Appendix 2 - Vegetation Communities and Regional Ecosystems
Appendix 2 - Vegetation Communities and Regional Ecosystems
Appendix 2 - Vegetation Communities and Regional Ecosystems
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<strong>Vegetation</strong> <strong>Communities</strong> <strong>and</strong><br />
<strong>Regional</strong> <strong>Ecosystems</strong><br />
of<br />
The Torres Strait Isl<strong>and</strong>s,<br />
Queensl<strong>and</strong>, Australia.<br />
An Accompaniment to L<strong>and</strong> Zone,<br />
<strong>Vegetation</strong> Community <strong>and</strong><br />
<strong>Regional</strong> Ecosystem Maps.<br />
Final Report to<br />
Torres Strait <strong>Regional</strong> Authority<br />
L<strong>and</strong> & Sea Management Unit.<br />
by 3d Environmental<br />
Stanton, D.J., Fell, D.G. <strong>and</strong> Gooding, D.O.<br />
August, 2008
Executive Summary<br />
The Torres Strait region, lying between the tip of Cape York Peninsula <strong>and</strong> the south-western<br />
coast of Papua New Guinea, has long been recognised for its cultural <strong>and</strong> ecological<br />
uniqueness <strong>and</strong> diversity. The need to preserve <strong>and</strong> appropriately manage the cultural, social<br />
<strong>and</strong> environmental values identified throughout the region is now more than ever apparent<br />
<strong>and</strong> vital given the pressures imposed by a range of current <strong>and</strong> potentially threatening<br />
processes.<br />
Under funding from the Natural Heritage Trust administered through the Torres Strait<br />
<strong>Regional</strong> Authority L<strong>and</strong> <strong>and</strong> Sea Management Unit, a regional vegetation classification <strong>and</strong><br />
mapping survey of the Torres Strait Isl<strong>and</strong>s has been undertaken. The report <strong>and</strong><br />
accompanying maps present the first comprehensive assessment of the regions vegetation<br />
with previous studies either much broader in scale or focused on particular areas or isl<strong>and</strong>s.<br />
The information is intended to directly address priority issues identified in the Torres Strait<br />
<strong>Regional</strong> L<strong>and</strong> <strong>and</strong> Sea Management Strategy being; lack of information on terrestrial<br />
biodiversity ecology or biological process; <strong>and</strong> the lack of a spatial representation of<br />
vegetation communities (<strong>and</strong> regional ecosystems) at an appropriate scale for local l<strong>and</strong> use<br />
planning initiatives. Furthermore, the information provided in this study serves to provide<br />
baseline data layers to support the development of Pilot Sustainable L<strong>and</strong> Use Plans on six<br />
isl<strong>and</strong>s (Saibai, Boigu, Dauan, Iama, Masig, <strong>and</strong> Erub).<br />
The study focused on detailed stereoscopic interpretation of the available aerial photography,<br />
both recent <strong>and</strong> historical, supported by satellite imagery as a basis for vegetation community<br />
delineation. A field survey undertaken to provide floristic characterisation of representative<br />
vegetation communities was completed by two field ecologists between 16 October <strong>and</strong> 2<br />
December, 2007. The survey collected data at 1 372 survey locations over a total l<strong>and</strong> area of<br />
892 km 2 , supplementing 37 sites surveyed during previous data collection exercises (Neldner<br />
<strong>and</strong> Clarkson 2005), providing a spatial scale of sampling at scale of roughly 1:25 000. A<br />
secondary phase of field sampling was completed in July 2008 for Badu Isl<strong>and</strong>.<br />
In total, the study identified 158 remnant vegetation communities within 27 Broad <strong>Vegetation</strong><br />
Groups. These vegetation communities are classified into the regional ecosystem framework<br />
based on l<strong>and</strong>form association, structural type <strong>and</strong> floristic assemblage. Seventy-six regional<br />
ecosystems are identified in the study area, of which 10 are recognised as new ecosystem<br />
types for the Cape York Peninsula Bioregion, within which 218 regional ecosystems are<br />
currently recognised. This accounts for approximately one third of the total ecosystem<br />
diversity present in the bioregion within a recognised sub-region contributing less than 0.01%<br />
to the bioregions total l<strong>and</strong> area (12,050,307.0576 ha – IBRA Version 5). The vascular flora<br />
is similarly diverse with 1 330 vascular flora species known <strong>and</strong> including 196 naturalised<br />
species, seven species declared on the L<strong>and</strong> Protection Act 2002, <strong>and</strong> 31 species listed as<br />
endangered, vulnerable or rare under Queensl<strong>and</strong>’s Nature Conservation Act (Wildlife)<br />
Regulation 2006. The Torres Strait flora approximates 40% of the species known for the Cape<br />
York Peninsula bioregion <strong>and</strong> some 13% of the Queensl<strong>and</strong> vascular flora.<br />
The Isl<strong>and</strong>s that make up the Torres Strait sub-region are truly unique <strong>and</strong> biologically diverse<br />
terrestrial ecosystems which support outst<strong>and</strong>ing terrestrial biodiversity values much of which<br />
has been previously unrecognised. The findings identify a number of highly significant<br />
vegetation types, which include those with very restricted distribution within the study area,<br />
bioregionally endemic types, extensive wetl<strong>and</strong>s, <strong>and</strong> vegetation that provides important<br />
habitat for flora of national, state <strong>and</strong> regional significance. Furthermore, the vegetation <strong>and</strong><br />
flora exhibit evidence of the evolving <strong>and</strong> ongoing fragmentation of the biomes of northern<br />
Australia <strong>and</strong> New Guinea.<br />
3D Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008 i
Acknowledgments<br />
This project was funded with the assistance of the Federal Government’s Natural Heritage<br />
Trust (NHT) through the Torres Strait <strong>Regional</strong> Authority-L<strong>and</strong> <strong>and</strong> Sea Management Unit.<br />
The authors would like to acknowledge <strong>and</strong> thank the following people <strong>and</strong> organisations for<br />
their assistance with the project:<br />
• All isl<strong>and</strong> Prescribed Body Corporate (PBC) bodies <strong>and</strong> members who granted<br />
permission for access to traditional l<strong>and</strong>s;<br />
• All isl<strong>and</strong> Council Chairpersons, CEO’s <strong>and</strong> executive for coordination <strong>and</strong> logistical<br />
support throughout the survey;<br />
• Kaurerag field rangers particularly Mr. John Wigness <strong>and</strong> Mr. Kathawa Rattler for<br />
assistance in the field on Kaurerag country, <strong>and</strong> liaison support by Mr Milton Savage<br />
<strong>and</strong> Mr Eliza Wasaga;<br />
• TSRA L<strong>and</strong> <strong>and</strong> Sea Management Unit staff Damian Miley, Miya Isherwood, <strong>and</strong><br />
Vic McGrath for assistance with project management <strong>and</strong> cultural liaison. Ben<br />
Hanrahan <strong>and</strong> Marianne Helling provided valuable background information<br />
throughout;<br />
• Dr. Garrick Hitchcock for advice <strong>and</strong> guidance on issues pertaining to cultural<br />
protocols <strong>and</strong> ethnography, provision of background literature <strong>and</strong> review of the draft<br />
report;<br />
• Mary Bani of TSRA Native Title Office for assistance with introductory<br />
correspondence <strong>and</strong> advice on Native Title matters;<br />
• EPA Senior Botanist Eda Addicot <strong>and</strong> Dr John Neldner for advice <strong>and</strong> assistance on<br />
vegetation <strong>and</strong> <strong>Regional</strong> Ecosystem classification;<br />
• Barbara Waterhouse for provision of background information valuable to project<br />
planning <strong>and</strong> for botanical advice;<br />
• Peter Stanton for provision of comments on the draft report;<br />
• AQIS staff throughout Torres Strait;<br />
• Mr John Dowe for advice on palm distributions <strong>and</strong> identifications;<br />
• John <strong>and</strong> Linda Fell for accommodation on Zuna Isl<strong>and</strong><br />
• Keith <strong>and</strong> Moroma Fell for accommodation on Mabuiag Isl<strong>and</strong>.<br />
Cover Photographs<br />
1. Mangroves <strong>and</strong> salt pan on L<strong>and</strong> Zone 1, Horn Isl<strong>and</strong>.<br />
2. Semi deciduous vine forest on L<strong>and</strong> Zone 2, Erub.<br />
3. P<strong>and</strong>anus grassl<strong>and</strong> complex on L<strong>and</strong> Zone 3, Saibai.<br />
4. Vine thicket remnants on L<strong>and</strong> Zone 7, Saibai.<br />
5. Grassl<strong>and</strong> <strong>and</strong> vine thicket on L<strong>and</strong> Zone 8, Erub.<br />
6. Rainforest on L<strong>and</strong> Zone 12, Moa Isl<strong>and</strong>.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
ii
Table of Contents<br />
Executive Summary...................................................................................... i<br />
Acknowledgments....................................................................................... ii<br />
Table of Contents ........................................................................................iii<br />
1. Introduction ........................................................................................... 1<br />
1.1 Study Area Description....................................................................................1<br />
1.1.1 Study Location <strong>and</strong> Context...................................................................................1<br />
1.1.2 Climate ......................................................................................................................2<br />
1.1.3 Geology <strong>and</strong> Geomorphology ...............................................................................2<br />
2. Aims <strong>and</strong> Scope..................................................................................... 6<br />
3. Methods .................................................................................................. 7<br />
3.1 Desktop Literature Review..............................................................................7<br />
3.2 Image Base Compilation <strong>and</strong> Aerial Photograph Analysis ........................9<br />
3.3 Site Locations...................................................................................................10<br />
3.4 Field Survey Procedure..................................................................................17<br />
3.5 Classification of L<strong>and</strong> <strong>and</strong> <strong>Vegetation</strong>.........................................................18<br />
3.5.1 Non-Rainforest <strong>Vegetation</strong>...................................................................................19<br />
3.5.2 Classification of Rainforest <strong>Vegetation</strong>...............................................................19<br />
3.5.3 Classification of Remnant/Non-Remnant <strong>Vegetation</strong> .....................................20<br />
3.6 Scale of Survey.................................................................................................21<br />
3.7 Image Interpretation <strong>and</strong> Attribution Method ...........................................21<br />
3.8 Pre-clearing <strong>Vegetation</strong> Method...................................................................21<br />
3.9 Digital Processing <strong>and</strong> Accuracy..................................................................22<br />
3.10 Limitations <strong>and</strong> Constraints ..........................................................................22<br />
4.0 Results – Field Analysis ..................................................................... 24<br />
4.1 Classification of L<strong>and</strong> <strong>and</strong> <strong>Vegetation</strong>.........................................................24<br />
4.1.1 L<strong>and</strong> Zones .............................................................................................................24<br />
4.1.2 <strong>Vegetation</strong> <strong>Communities</strong> ......................................................................................24<br />
4.1.3 <strong>Regional</strong> <strong>Ecosystems</strong> .............................................................................................34<br />
5.0 Results Analysis <strong>and</strong> Discussion ...................................................... 40<br />
5.1 Clarifications on the Classification of L<strong>and</strong> Zones in the Study Area ....40<br />
5.1.1 L<strong>and</strong> Zone 1............................................................................................................40<br />
5.1.2 L<strong>and</strong> Zone 2............................................................................................................40<br />
5.1.3 L<strong>and</strong> Zone 3............................................................................................................41<br />
5.1.4 L<strong>and</strong> Zone 5............................................................................................................42<br />
5.1.5 L<strong>and</strong> Zone 7............................................................................................................45<br />
5.1.6 L<strong>and</strong> Zone 8............................................................................................................45<br />
5.1.7 L<strong>and</strong> Zone 12..........................................................................................................45<br />
5.2 <strong>Regional</strong> Ecosystem Descriptions <strong>and</strong> Rationale for Classification ........46<br />
5.2.1 <strong>Regional</strong> Ecosystem 3.1.1......................................................................................46<br />
5.2.2 <strong>Regional</strong> Ecosystem 3.1.2......................................................................................48<br />
5.2.3 <strong>Regional</strong> Ecosystem 3.1.4......................................................................................50<br />
5.2.4 <strong>Regional</strong> Ecosystem 3.1.5......................................................................................50<br />
5.2.5 <strong>Regional</strong> Ecosystem 3.1.6......................................................................................51<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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5.2.6 <strong>Regional</strong> Ecosystem 3.1.7 (New RE)....................................................................52<br />
5.2.7 <strong>Regional</strong> Ecosystem 3.2.2a....................................................................................54<br />
5.2.8 <strong>Regional</strong> Ecosystem 3.2.2b....................................................................................56<br />
5.2.9 <strong>Regional</strong> Ecosystem 3.2.3......................................................................................58<br />
5.2.10 <strong>Regional</strong> Ecosystem 3.2.4......................................................................................60<br />
5.2.11 <strong>Regional</strong> Ecosystem 3.2.5......................................................................................63<br />
5.2.12 <strong>Regional</strong> Ecosystem 3.2.6......................................................................................66<br />
5.2.13 <strong>Regional</strong> Ecosystem 3.2.7......................................................................................68<br />
5.2.14 <strong>Regional</strong> Ecosystem 3.2.8......................................................................................69<br />
5.2.15 <strong>Regional</strong> Ecosystem 3.2.10c ..................................................................................71<br />
5.2.17 <strong>Regional</strong> Ecosystem 3.2.14....................................................................................71<br />
5.2.18 <strong>Regional</strong> Ecosystem 3.2.15....................................................................................72<br />
5.2.19 <strong>Regional</strong> Ecosystem 3.2.19....................................................................................74<br />
5.2.20 <strong>Regional</strong> Ecosystem 3.2.24....................................................................................76<br />
5.2.21 <strong>Regional</strong> Ecosystem 3.2.25....................................................................................76<br />
5.2.22 <strong>Regional</strong> Ecosystem 3.2.26....................................................................................78<br />
5.2.23 <strong>Regional</strong> Ecosystem 3.2.27....................................................................................79<br />
5.2.24 <strong>Regional</strong> Ecosystem 3.2.28....................................................................................79<br />
5.2.26 <strong>Regional</strong> Ecosystem 3.3.5c ....................................................................................81<br />
5.2.27 <strong>Regional</strong> Ecosystem 3.3.6......................................................................................81<br />
5.2.28 <strong>Regional</strong> Ecosystem 3.3.7......................................................................................84<br />
5.2.29 <strong>Regional</strong> Ecosystem 3.3.9......................................................................................85<br />
5.2.30 <strong>Regional</strong> Ecosystem 3.3.10....................................................................................87<br />
5.2.31 <strong>Regional</strong> Ecosystem 3.3.12....................................................................................90<br />
5.2.32 <strong>Regional</strong> Ecosystem 3.3.13....................................................................................90<br />
5.2.33 <strong>Regional</strong> Ecosystem 3.3.14....................................................................................91<br />
5.2.34 <strong>Regional</strong> Ecosystem 3.3.17b..................................................................................92<br />
5.2.35 <strong>Regional</strong> Ecosystem 3.3.20c ..................................................................................93<br />
5.2.36 <strong>Regional</strong> Ecosystem 3.3.22....................................................................................94<br />
5.2.37 <strong>Regional</strong> Ecosystem 3.3.27....................................................................................95<br />
5.2.38 <strong>Regional</strong> Ecosystem 3.3.28....................................................................................97<br />
5.2.39 <strong>Regional</strong> Ecosystem 3.3.42....................................................................................98<br />
5.2.40 <strong>Regional</strong> Ecosystem 3.3.48b................................................................................102<br />
5.2.41 <strong>Regional</strong> Ecosystem 3.3.51..................................................................................103<br />
5.2.42 <strong>Regional</strong> Ecosystem 3.3.57..................................................................................103<br />
5.2.43 <strong>Regional</strong> Ecosystem 3.3.62..................................................................................105<br />
5.2.44 <strong>Regional</strong> Ecosystem 3.3.63..................................................................................107<br />
5.2.45 <strong>Regional</strong> Ecosystem 3.3.68 (New RE)................................................................108<br />
5.2.46 <strong>Regional</strong> Ecosystem 3.3.69 (New RE)................................................................110<br />
5.2.47 <strong>Regional</strong> Ecosystem 3.3.70 (New RE)................................................................111<br />
5.2.48 <strong>Regional</strong> Ecosystem 3.5.5....................................................................................112<br />
5.2.49 <strong>Regional</strong> Ecosystem 3.5.8c ..................................................................................112<br />
5.2.50 <strong>Regional</strong> Ecosystem 3.5.15..................................................................................113<br />
5.2.51 <strong>Regional</strong> Ecosystem 3.5.17a................................................................................116<br />
5.2.52 <strong>Regional</strong> Ecosystem 3.5.19a................................................................................117<br />
5.2.53 <strong>Regional</strong> Ecosystem 3.5.23x1..............................................................................117<br />
5.2.54 <strong>Regional</strong> Ecosystem 3.5.29..................................................................................119<br />
5.2.55 <strong>Regional</strong> Ecosystem 3.5.32 (New RE)................................................................119<br />
5.2.56 <strong>Regional</strong> Ecosystem 3.7.1x1b..............................................................................120<br />
5.2.57 <strong>Regional</strong> Ecosystem 3.8.4b..................................................................................121<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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5.2.58 <strong>Regional</strong> Ecosystem 3.8.5 (New RE)..................................................................124<br />
5.2.59 <strong>Regional</strong> Ecosystem 3.12.4..................................................................................128<br />
5.2.60 <strong>Regional</strong> Ecosystem 3.12.8..................................................................................130<br />
5.2.61 <strong>Regional</strong> Ecosystem 3.12.9..................................................................................132<br />
5.2.62 <strong>Regional</strong> Ecosystem 3.12.11................................................................................133<br />
5.2.63 <strong>Regional</strong> Ecosystem 3.12.13................................................................................135<br />
5.2.64 <strong>Regional</strong> Ecosystem 3.12.16................................................................................136<br />
5.2.65 <strong>Regional</strong> Ecosystem 3.12.18................................................................................138<br />
5.2.66 <strong>Regional</strong> Ecosystem 3.12.20................................................................................138<br />
5.2.67 <strong>Regional</strong> Ecosystem 3.12.21a..............................................................................140<br />
5.2.68 <strong>Regional</strong> Ecosystem 3.12.23................................................................................143<br />
5.2.69 <strong>Regional</strong> Ecosystem 3.12.29................................................................................145<br />
5.2.70 <strong>Regional</strong> Ecosystem 3.12.30................................................................................146<br />
5.2.71 <strong>Regional</strong> Ecosystem 3.12.31x1a (New RE)........................................................147<br />
5.2.72 <strong>Regional</strong> Ecosystem 3.12.33b..............................................................................150<br />
5.2.73 <strong>Regional</strong> Ecosystem 3.12.34c ..............................................................................151<br />
5.2.74 <strong>Regional</strong> Ecosystem 3.12.35 (New RE)..............................................................154<br />
5.2.75 <strong>Regional</strong> Ecosystem 3.12.36 (New RE)..............................................................160<br />
5.2.76 <strong>Regional</strong> Ecosystem 3.12.37 (New RE)..............................................................166<br />
5.2.77 <strong>Regional</strong> Ecosystem 3.12.38 (New RE)..............................................................167<br />
5.3 Retrospective Classifications.......................................................................169<br />
5.3.1 <strong>Regional</strong> Ecosystem 3.3.1c (Cleared).................................................................169<br />
5.4 Non-Remnant Classifications......................................................................170<br />
5.5 Other Classifications.....................................................................................173<br />
6.0 Spatial Extent of <strong>Regional</strong> <strong>Ecosystems</strong> .......................................... 173<br />
7.0 Significant <strong>Vegetation</strong> <strong>and</strong> Flora .................................................... 175<br />
7.1 Summary of Significant <strong>Vegetation</strong> ...........................................................175<br />
7.2 Summary of Flora .........................................................................................178<br />
7.2.1 <strong>Regional</strong> Flora ......................................................................................................178<br />
7.2.2 Introduced <strong>and</strong> Naturalised Flora.....................................................................179<br />
7.2.3 Significant Flora ...................................................................................................181<br />
8.0 Ecosystem Condition........................................................................ 186<br />
9.0 Recommendations............................................................................. 189<br />
9.1 Additional Survey Requirements ...............................................................189<br />
9.2 Future Opportunities....................................................................................189<br />
10. Bibliography....................................................................................... 191<br />
11. Appendices ........................................................................................ 196<br />
<strong>Appendix</strong> A1. Map Legend - <strong>Vegetation</strong> Communties....................................196<br />
<strong>Appendix</strong> A2. Map Legend – L<strong>and</strong> Zones .........................................................202<br />
<strong>Appendix</strong> B. Torres Strait Isl<strong>and</strong>s Flora Species List ......................................204<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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1. Introduction<br />
Three (3)d Environmental have been commissioned by the Torres Strait <strong>Regional</strong> Authority<br />
(TSRA) L<strong>and</strong> <strong>and</strong> Sea Management Unit to undertake a vegetation community <strong>and</strong> regional<br />
ecosystem assessment of the Torres Strait <strong>and</strong> Kaurareg Isl<strong>and</strong>s. The study is one of the major<br />
regional scale initiatives of the ‘L<strong>and</strong> <strong>and</strong> Sea Management Strategy for Torres Strait’ developed<br />
in late 2005 to co-ordinate the delivery of funding <strong>and</strong> programs through the National Heritage<br />
Trust (NHT) program. The major objectives of the Strategy are biodiversity conservation,<br />
sustainable use of natural resources, <strong>and</strong> community capacity building <strong>and</strong> institutional change<br />
(Torres Strait NRM Reference Group 2005). The study is third in a series of regional ecosystem<br />
assessments funded through this initiative. The first of these assessments, undertaken by<br />
Greening Australia (Freebody 2002) identified areas within the Torres Strait with outst<strong>and</strong>ing<br />
biodiversity values. Natural Resource Assessments (2003) completed vegetation survey on two<br />
isl<strong>and</strong>s (Mer <strong>and</strong> Moa) <strong>and</strong> identified their outst<strong>and</strong>ing conservation values.<br />
As a regional survey, this study presents by far the most comprehensive assessment of vegetation<br />
undertaken in the Torres Strait Isl<strong>and</strong>s to date <strong>and</strong> presents data in a regionally consistent<br />
framework. The information will directly inform priority issues identified in the Strategy, that is;<br />
lack of information on terrestrial biodiversity; ecological <strong>and</strong> biological processes; <strong>and</strong><br />
incomplete vegetation mapping at appropriate scale for use in l<strong>and</strong> use planning. Furthermore,<br />
the information within this study serves to provide baseline data layers to support the<br />
development of Sustainable L<strong>and</strong> Use Plans on six isl<strong>and</strong>s (Saibai, Boigu Dauan, Iama, Masig,<br />
<strong>and</strong> Erub). The l<strong>and</strong> use plans are a NHT initiative being concurrently delivered by the TSRA<br />
L<strong>and</strong> <strong>and</strong> Sea Management Unit.<br />
1.1 Study Area Description<br />
1.1.1 Study Location <strong>and</strong> Context<br />
The study area encompasses isl<strong>and</strong>s extending from the tip of Cape York Peninsula to within five<br />
kilometres (km) of the Papua New Guinea (PNG) coastline <strong>and</strong> encompasses some 35 000 km 2 of<br />
shallow open seas. Within this area are about one hundred <strong>and</strong> fifty isl<strong>and</strong>s of which 17 are<br />
inhabited <strong>and</strong> supporting approximately 8 000 indigenous people (about 20% of Australia’s total<br />
Torres Strait Isl<strong>and</strong>er population) (Arthur <strong>and</strong> Morphy 2005). Historically the isl<strong>and</strong>s within the<br />
region have been occupied for between 8 000 <strong>and</strong> 6 000 years with permanent isl<strong>and</strong> occupation<br />
occurring after 3 500-3 000 years BP (Rowe 2006). The recognition of the Kaurareg Isl<strong>and</strong>s<br />
acknowledges the traditional owners of the southern continental group of isl<strong>and</strong>s (the Kaurareg<br />
People). In future reference within this report, the Kaurareg Isl<strong>and</strong>s are recognised within the<br />
broader group referred to as the ‘The Torres Strait Isl<strong>and</strong>s’. The Isl<strong>and</strong>s, with regional context<br />
<strong>and</strong> isl<strong>and</strong> distribution shown in Figure 1, are located within Sub-region 3 (Cape York-Torres<br />
Strait) <strong>and</strong> the Barrier Reef Isl<strong>and</strong> sub-region of the Cape York Peninsula Bioregion. These can<br />
be characterised geographically into five major isl<strong>and</strong> groups being:<br />
• Eastern Group – Comprising Mer (Murray), Erub (Darnley), Ugar (Stephen), Dauar <strong>and</strong><br />
Waier (Mer Group) <strong>and</strong> Bramble Cay. These isl<strong>and</strong>s are of mostly volcanic in origin<br />
comprising mainly basic volcanic <strong>and</strong> igneous basement rocks. The latter isl<strong>and</strong> is a<br />
coral cay;<br />
• Central Group – Comprising Warraber (Sue), Poruma (Coconut), Masig (Yorke), Sassie<br />
are low s<strong>and</strong>y isl<strong>and</strong>s (often with some basement rock exposure) developed on coral<br />
platforms while Naghir (Mt Ernest) <strong>and</strong> Iama (Yam) Isl<strong>and</strong>s are generally volcanic in<br />
origin;<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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• Top Western Group - Saibai, Boigu, <strong>and</strong> Dauan Isl<strong>and</strong>s. Saibai <strong>and</strong> Boigu are<br />
comprised dominantly of alluvial muds overlying old coral platforms. These isl<strong>and</strong>s are<br />
low, swampy, <strong>and</strong> dominated by mangroves <strong>and</strong> saltpans with difficult access to interior<br />
areas. Dauan is on granite basement forming low hills with steep rocky interior areas<br />
which are topographically accessible;<br />
• Near Western –Moa, Badu <strong>and</strong> Mabuiag Isl<strong>and</strong>s comprised predominantly of old<br />
volcanic <strong>and</strong> granite rocks. Also includes a number of small uninhabited isl<strong>and</strong>s <strong>and</strong><br />
islets; <strong>and</strong><br />
• Inner – Waibene (Thursday), Kirriri (Hammond), Ngurapai (Horn), Paliliug (Goods),<br />
Zuna (Entrance), Tuesday, Maiwai (Wednesday), Giralug (Friday), Muralug (Prince of<br />
Wales), Morilug (Mt Adolphus-Little Adolphus), Possession <strong>and</strong> Albany Isl<strong>and</strong>s. These<br />
are topographically elevated cluster of continental isl<strong>and</strong>s comprising basement igneous<br />
<strong>and</strong> volcanic rock.<br />
Whilst geographical classification places these isl<strong>and</strong>s in a spatial context, geological typing of the<br />
isl<strong>and</strong>s has been undertaken in Section 1.1.3 for descriptive purposes.<br />
1.1.2 Climate<br />
The climate of the isl<strong>and</strong> group on a whole is tropical monsoonal with 90% of annual rainfall (1<br />
750-2 000 mm) occurring in the summer (December – April) period where winds are<br />
predominantly from the north-west <strong>and</strong> coinciding with highest astronomical spring tides. Strong<br />
south-easterly trade winds blow during the winter months (May – September) with moisture<br />
generated from ocean fetch falling in sporadic showers which tend to clear rapidly. The isl<strong>and</strong>s<br />
in general receive more than 1 600 mm of rainfall annually (Sattler <strong>and</strong> Williams 1999).<br />
Mean temperatures recorded over a 12-year period from the Horn Isl<strong>and</strong> meteorological station<br />
(1995-2007) record mean maximum temperatures of 28.6º for July, <strong>and</strong> 31.8º for November. For<br />
the same weather station <strong>and</strong> same period, the driest month on average is September with 2.8 mm<br />
of rainfall, <strong>and</strong> wettest is February with 499.5mm on average, <strong>and</strong> an average annual rainfall of<br />
1804.6 mm (BOM 2008). Records for historical weather stations are not readily available.<br />
1.1.3 Geology <strong>and</strong> Geomorphology<br />
The geology of the isl<strong>and</strong>s is presented in a number of regional reports on the isl<strong>and</strong> group, of<br />
which the major findings are summarised here in a broad regional overview. A more detailed<br />
analysis of the geology, geomorphology <strong>and</strong> l<strong>and</strong>form evolution of the isl<strong>and</strong> group is presented<br />
in Section 5.1 where l<strong>and</strong> zones (according to legislative definition) are described. The isl<strong>and</strong>s<br />
can be placed in five broad geological groupings described below.<br />
Isl<strong>and</strong>s Formed on Acidic Volcanic <strong>and</strong> Plutonic Basement: This is the most extensive<br />
geological grouping extending from the inner isl<strong>and</strong> group in the south; through the near western<br />
isl<strong>and</strong>s of Moa <strong>and</strong> Badu <strong>and</strong> Mabuiag; the central group with Iama <strong>and</strong> Gebar; <strong>and</strong> the top<br />
western group where Dauan forms the sole representative. This grouping represents the<br />
continuation of the Australian continental basement northwards to New Guinea, having its most<br />
northerly expression at Mabaduan Hill on the southern PNG coast (Loffler 1977).<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
2
Waral Kawa (Deliverance) Is.<br />
ARAFURA<br />
SEA<br />
0 15 30 45 60<br />
N O T E S:<br />
Kilometres<br />
(i) This figure has been produced for exclusive use<br />
of the client TSRA L<strong>and</strong> & Sea Management Unit <strong>and</strong> 3D Environmental<br />
TORRES<br />
Wassi Kussa R.<br />
Mai Kussa R.<br />
Giralag (Friday) Is.<br />
Papua New Guinea (Western Province)<br />
CORAL SEA<br />
Mabuiag Is.<br />
Badu Is.<br />
Kirriri (Hammond) Is.<br />
Palilag (Goods) Is.<br />
Boigu Is.<br />
Muralug (Prince of<br />
Wales) Is.<br />
Buru (Turnagain) Is.<br />
Moa Is.<br />
Zurath (Phipps) Is.<br />
Dauan Is.<br />
Warral (Hawksberry) Is.<br />
Cape York Peninsula<br />
Naghir (Mt Ernest) Is.<br />
Maiwaii (Wednesday) Is.<br />
Waibene (Thursday Is.)<br />
Zuna Is.<br />
Ngurapai (Horn) Is.<br />
Bamaga<br />
Saibai Is.<br />
Gebar Is.<br />
Mabaduan<br />
Iama (Yam) Is.<br />
Zagai (Dungeness) Is.<br />
Sassie Is.<br />
SOUTH<br />
Morilag (Mt Adolphus) Is.<br />
Somerset<br />
Tudu (Warrior) Is.<br />
Warraber (Sue) Islet<br />
STRAIT<br />
Poruma (Coconut) Is.<br />
PACIFIC<br />
Aureed Is.<br />
OCEAN<br />
Masig (Yorke) Is.<br />
Ugar (Stephens) Is.<br />
Figure 1. Study Area Location<br />
Client<br />
Scale<br />
1:900,000<br />
Erub (Darnley Is.)<br />
Torres Strait <strong>Regional</strong> Authority<br />
Dawar Is. Waier Is.<br />
Mer (Murray) Is.<br />
3D Environmental<br />
<strong>Vegetation</strong> Assessment<br />
& Mapping Specialists<br />
P. O. Box 959<br />
Kenmore, Qld 4069<br />
Phone: (07) 3411 9072; (07) 3878 4344<br />
Mobile: 0404 577 285; 0409 426 916<br />
www.3denvironmental.com.au<br />
File Path C:\3D Environmental\<br />
Drawn By DG Checked DF Torres\3d_TS_Maps_A3L.mxd Date<br />
25/03/08<br />
A3
Literature often refers to the string of continental isl<strong>and</strong>s extending northwards to PNG as the<br />
northern extension of Australia’s Great Dividing Range (Torres Strait NRM Reference Group<br />
2005). As the Great Dividing Range is a geographical rather than geological feature, dividing the<br />
watershed on Australia’s east coast into west flowing <strong>and</strong> east flowing streams (in a broad sense),<br />
the term is considered irrelevant to the isl<strong>and</strong>s.<br />
A range of lithologies are represented in this group with acid welded tuff, agglomerate, rhyolite<br />
<strong>and</strong> <strong>and</strong>esite of the Torres Strait Volcanics most extensive in the southern group of isl<strong>and</strong>s<br />
although extending through Moa, Mabuiag, <strong>and</strong> Gebar Isl<strong>and</strong>s (Willmott <strong>and</strong> Powell 1977). The<br />
volcanics have been variably intruded by the Badu Granite, a coarse biotite granite which forms<br />
the highest peaks on many of the isl<strong>and</strong>s including Banks Peak on Moa Isl<strong>and</strong>, the highest Peak<br />
in the isl<strong>and</strong> group at 399m, <strong>and</strong> Mount Cornwallis on Dauan at 242m. These later intrusive<br />
events have resulted in extensive horfeldsing of the rhyolite basement manifest in a number of<br />
extremely resistant knolls <strong>and</strong> ridgelines, most prominent on Moa Isl<strong>and</strong>.<br />
The larger isl<strong>and</strong>s in this geological group generally have well-developed coastal flats, often in<br />
broad embayments separated by coastal headl<strong>and</strong>s. The most extensive of these is located on<br />
Moa Isl<strong>and</strong> where an extensive area of residual s<strong>and</strong> forms a thin cover over the granite <strong>and</strong><br />
volcanic basement rock. Relict alluvial fans, generally deeply dissected, often fringe these<br />
residual areas <strong>and</strong> were once probably considerably more extensive. Similar features are noted<br />
on Muralug, <strong>and</strong> to a lesser extent on Horn Isl<strong>and</strong>.<br />
Coastal dunes are a common feature on the coastline of the acid volcanic isl<strong>and</strong>s, with younger<br />
prograding beach ridge systems pronounced in a number of locations. The best development of<br />
these features is on the south-west facing coastline of Muralug Isl<strong>and</strong>, as well as Friday Isl<strong>and</strong><br />
(see Swan 1981) where the dunes have developed aeolian (wind blown) features including<br />
blowouts <strong>and</strong> some broad deflation hollows. An extensive relict dune system is mapped on Badu<br />
Isl<strong>and</strong>, the extent of which has not been recognised in the previous studies of Willmott <strong>and</strong><br />
Powell (1977). The system is developed behind exposed embayments on the isl<strong>and</strong>s southeastern<br />
side, <strong>and</strong> is represented by a gently sloping broad s<strong>and</strong> ridge which tapers to a near<br />
uniform s<strong>and</strong> sheet on the dunes l<strong>and</strong>ward margins where it terminates against a series of low<br />
granite escarpments. Field evidence indicates that dune s<strong>and</strong> has pushed over the top of low<br />
granite saddles <strong>and</strong> headl<strong>and</strong>s in some locations, being strong evidence that the broad system is a<br />
relict feature from a period of transgressive dune building. The majority of the system is<br />
stabilised with vegetation ranging from sedgel<strong>and</strong> to eucalypt woodl<strong>and</strong>, which has resulted in a<br />
suppressed <strong>and</strong> evenly graded morphology. In the area to the south-west of the Badu township<br />
(in the vicinity of the current borefield), a large portion of the dunefield is in unstable form with<br />
the dominant surface area of the dune formed by exposed coarse silica s<strong>and</strong> demonstrating<br />
undulating morphologies which include shallow deflation basins, blowouts <strong>and</strong> low depositional<br />
mounds (see Photograph 1).<br />
The initiation of transgressive dune development is often linked to sea level rise (Hesp <strong>and</strong> Thom,<br />
1990) <strong>and</strong> it is feasible to conclude that the transgressive event on Badu can be linked to a sea<br />
level highst<strong>and</strong> inferred by Burne et al. (1995) as being 6 000 yrs B.P. It is also feasible to<br />
conclude that the dune has degraded to the suppressed <strong>and</strong> stable morphology manifest in todays<br />
l<strong>and</strong>scape in the period lapsed since this sea level high st<strong>and</strong>. The timing of the event responsible<br />
for dune destabilisation is unknown, although it is clear that it is relatively recent as the unstable<br />
area forms a broad deflational basin which truncates well-wooded <strong>and</strong> stable dunes to the<br />
immediate south. Orme (1990) suggests that periods of dune instability may be initiated by<br />
anthropogenic disturbance such as burning. It is considered possible that dune instability is coincident<br />
with the advent of permanent human occupation, prompted by indigenous l<strong>and</strong><br />
management practices.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
4
Photograph 1. A deflation scar in<br />
the early stages of stabilisation.<br />
Transgressive dune sequence - Near<br />
Western Isl<strong>and</strong> group.<br />
Extensive deposits of estuarine sediment are found on many of the isl<strong>and</strong> embayments,<br />
particularly on Muralug in the Port Lihou area, although broad estuarine sequences supporting<br />
mangroves are found on all of the larger isl<strong>and</strong>s. Many of the smaller isl<strong>and</strong>s including Iama,<br />
Gebar <strong>and</strong> Dauan have similar features developed to a lesser extent.<br />
Isl<strong>and</strong>s of Recent Basic Volcanics: This geologic grouping is exclusive to the Eastern Group of<br />
Isl<strong>and</strong>s including Mer (<strong>and</strong> associated islets), Erub <strong>and</strong> Ugar. These isl<strong>and</strong>s have resulted from<br />
recent Pleistocene Age (
Isl<strong>and</strong> Remnants of the Southern Papuan Lowl<strong>and</strong>s: The Fly platform is the largest tract of<br />
low lying country in Papua New Guinea (Loffler 1977), occupying nearly a third of the mainl<strong>and</strong>.<br />
Flat areas are poorly drained <strong>and</strong> swampy, terminating with extensive estuarine swampl<strong>and</strong>s on<br />
the southern coast. The isl<strong>and</strong>s of Boigu <strong>and</strong> Saibai represent remnants of this coastal plain,<br />
possibly separated from the mainl<strong>and</strong> through the erosive actions of major PNG river systems,<br />
which include the Pahoturi, the Mai Kussa, <strong>and</strong> the Wassi Kussa Rivers. Saibai Isl<strong>and</strong> forms the<br />
most elevated expression of this remnant coastal plain with gently domed inner alluvial regions<br />
broken by tidal swampl<strong>and</strong>s <strong>and</strong> marshes. Profiles in the alluvial system indicate up to a metre of<br />
grey silty clay loam at surface, often with vertic nature (cracking clays) passing into mottled<br />
heavy clay soils at depth. On Saibai, a well-developed lateritic profile is exposed on the northern<br />
coastline of the isl<strong>and</strong> on which the major settlement is developed. This laterite is suffering<br />
extreme erosion on the coastal fringe.<br />
Boigu represents a lower <strong>and</strong> swampier version of Saibai, with suppressed <strong>and</strong> fragmented<br />
alluvial remnants scattered across the isl<strong>and</strong>s interior, as well as on the developed northern<br />
coastal fringe. The majority of Boigu comprises marine swampl<strong>and</strong>s with limited l<strong>and</strong> available<br />
for development or settlement.<br />
Suppressed beach ridges occur on both Boigu <strong>and</strong> Saibai Isl<strong>and</strong>s. These are scattered around<br />
isl<strong>and</strong>s fringes forming low rises in mangrove forests. They are most extensive on the exposed<br />
southern coast of Boigu, <strong>and</strong> the south-eastern <strong>and</strong> north-western coast of Saibai.<br />
Coral Cays: This grouping represents a large number of smaller isl<strong>and</strong>s coral s<strong>and</strong> isl<strong>and</strong>s,<br />
mostly (although not restricted to) the central group of isl<strong>and</strong>s. The most prominent of these are<br />
Masig, Poruma, Aureed <strong>and</strong> Warraber although a large number of smaller cays are scattered<br />
throughout the isl<strong>and</strong> chain. These isl<strong>and</strong>s are formed on coral platforms <strong>and</strong> are extremely low<br />
lying, generally not more than 6m high (Willmott 1972). Heights for Warraber are reported as 2-<br />
8m above mean sea level (Hart et al. nd). In contrast to the continental <strong>and</strong> volcanic isl<strong>and</strong>s, the<br />
s<strong>and</strong> cays are relatively dynamic, shaped by prevailing tidal currents <strong>and</strong> subject to shifting<br />
shorelines in response to extreme weather events.<br />
Mangrove Isl<strong>and</strong>s: This is an interesting isl<strong>and</strong> grouping which is poorly referenced in available<br />
literature. The mangrove Isl<strong>and</strong>s of Buru <strong>and</strong> Zagai are built on coral platforms, although unlike<br />
coral cays, the isl<strong>and</strong>s are subject to complete tidal inundation. These Isl<strong>and</strong>s in the central isl<strong>and</strong><br />
group have no l<strong>and</strong> elevated above the higher tidal ranges <strong>and</strong> their entire above tidal expression<br />
is as a mangrove forest. Sassie Isl<strong>and</strong> has areas of elevated coral rubble <strong>and</strong> calcareous s<strong>and</strong>,<br />
although the interior is swampy <strong>and</strong> frequently inundated within the normal tidal range.<br />
2. Aims <strong>and</strong> Scope<br />
The study aims to document the nature of vegetation communities in the Torres Strait Isl<strong>and</strong><br />
Group through the provision of detailed description <strong>and</strong> mapping <strong>and</strong> placement of these<br />
communities into Queensl<strong>and</strong>’s regional ecosystem framework. The developed dataset provides<br />
baseline information suitable for sustainable l<strong>and</strong> use planning <strong>and</strong> for broader natural resource<br />
management planning, as well as providing a means to assess the regional conservation status of<br />
Torres Strait vegetation communities under relevant state <strong>and</strong> federal legislative process.<br />
The project scope extends to assessment of all isl<strong>and</strong>s with terrestrial biodiversity values. This<br />
includes documentation of the floristic composition, structure, <strong>and</strong> extent of all vegetation<br />
communities which have coverage under suitable remotely sensed imagery.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
6
3. Methods<br />
3.1 Desktop Literature Review<br />
A search of relevant literature <strong>and</strong> databases provided background information on the intensity<br />
<strong>and</strong> results of previous survey, the presence <strong>and</strong> distribution of vegetation communities <strong>and</strong> flora<br />
species in the broader region. Site data sourced from the Queensl<strong>and</strong> Herbarium’s CORVEG<br />
database provided information on the location of previous survey sites <strong>and</strong> data extracts sourced<br />
from HERBRECS <strong>and</strong> the CORVEG database provided information on flora species distribution.<br />
The method also included a review of previous studies completed by private organisations <strong>and</strong><br />
government agencies over relevant sections of the study area. Relevant publications included<br />
project specific reports, state government biodiversity planning studies, regional management<br />
strategies, as well as any useful academic studies.<br />
A regional perspective of the vegetation communities across the Torres Strait Isl<strong>and</strong>s is limited to<br />
the mapping carried out as part of the Cape York Peninsula L<strong>and</strong> Use Study (CYPLUS) in 1995<br />
(Neldner <strong>and</strong> Clarkson 1995). This work produced pre-clearing mapping at 1: 250 000 scale<br />
using Aerial Photograph Interpretation (API) only for isl<strong>and</strong>s north of Badu Isl<strong>and</strong> <strong>and</strong> a<br />
combination of API <strong>and</strong> limited ground-truthing. Using the analysis of that work by Neldner<br />
(1998), the regional analysis of vegetation prior to the current survey is as follows.<br />
Table 1. Extent of amalgamated broad vegetation groups in the Torres Strait isl<strong>and</strong>s (Neldner 1998).<br />
Amalgamated Broad <strong>Vegetation</strong> Groups<br />
Area<br />
(km 2 )<br />
% of total<br />
area<br />
Corymbia/Eucalyptus spp. dominated woodl<strong>and</strong>s, open-woodl<strong>and</strong>s <strong>and</strong><br />
open-forests<br />
231.7 25.9<br />
Melaleuca spp. low open-woodl<strong>and</strong>s, low woodl<strong>and</strong>s <strong>and</strong> tall shrubl<strong>and</strong>s 105.0 11.7<br />
Grassl<strong>and</strong>s <strong>and</strong> grassy open-woodl<strong>and</strong>s 59.7 6.7<br />
Closed-forests (excluding mangroves) 156.1 17.5<br />
Mangrove closed-forests 220.9 24.7<br />
Heathl<strong>and</strong>s 11.7 1.3<br />
Other communities (littoral vegetation, sedgel<strong>and</strong>s, saltpans <strong>and</strong> wetl<strong>and</strong>s) 108.1 12.1<br />
TOTAL 893.2 100.0<br />
Table 2. Percentage <strong>and</strong> area of each structural formation in Torres Strait Isl<strong>and</strong>s (Neldner 1998)<br />
Torres Strait Isl<strong>and</strong>s<br />
Structural Formation No. of map<br />
Area km 2 % of total area<br />
Woodl<strong>and</strong><br />
Low open-woodl<strong>and</strong><br />
Tall woodl<strong>and</strong><br />
Open woodl<strong>and</strong><br />
Closed-forest<br />
Open-heath<br />
Open-forest<br />
Closed-tussock grassl<strong>and</strong><br />
Tussock grassl<strong>and</strong><br />
Sparse-herbl<strong>and</strong><br />
Low closed-forest<br />
Low woodl<strong>and</strong><br />
Low open-forest<br />
Open-sedgel<strong>and</strong><br />
Tall shrubl<strong>and</strong><br />
Lakes <strong>and</strong> lagoons<br />
units<br />
7<br />
3<br />
-<br />
-<br />
7<br />
2<br />
5<br />
4<br />
1<br />
4<br />
9<br />
2<br />
1<br />
-<br />
1<br />
-<br />
233.2<br />
43.5<br />
-<br />
-<br />
212.0<br />
1.6<br />
11.0<br />
56.5<br />
3.3<br />
58.4<br />
183.1<br />
55.5<br />
18.0<br />
-<br />
0.6<br />
-<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
26.1<br />
4.9<br />
-<br />
-<br />
23.7<br />
0.2<br />
1.2<br />
6.3<br />
0.4<br />
6.5<br />
20.5<br />
6.2<br />
2.0<br />
-<br />
0.1<br />
-<br />
7
Structural Formation No. of map<br />
units<br />
Dwarf open-heath<br />
2<br />
Closed-sedgel<strong>and</strong><br />
2<br />
Tall open-shrubl<strong>and</strong><br />
-<br />
Closed-scrub<br />
1<br />
Closed herbl<strong>and</strong><br />
1<br />
Torres Strait Isl<strong>and</strong>s<br />
Area km 2 % of total area<br />
Freebody (2002) utilized the mapping data to assess the spatial distribution of each different<br />
vegetation community <strong>and</strong> to provide analysis of ‘rarity’ across the region. In a detailed review<br />
of isl<strong>and</strong> vegetation across the region incorporating 123 isl<strong>and</strong>s, Freebody (2002) reports 58<br />
vegetation units that have been mapped by the Queensl<strong>and</strong> Herbarium, with 34 units described as<br />
significant <strong>and</strong> representing 16% of the total terrestrial area of the Torres Strait. Significant<br />
vegetation units occur on at least 46 of the isl<strong>and</strong>s. Wannan <strong>and</strong> Bousi (2003) describe the<br />
vegetation <strong>and</strong> ecological values of Mer (Murray) <strong>and</strong> Moa Isl<strong>and</strong>s as part of a Natural Heritage<br />
Trust funded project Torres Strait Terrestrial Biodiversity Assessment for Sustainable<br />
Development.<br />
The extent of the known total flora of 1065 species as deduced from the Queensl<strong>and</strong> Herbarium<br />
Herbrecs database includes 154 (14%) introduced species (Neldner 1998, Freebody 2002), <strong>and</strong><br />
recognises the lack of systematic survey <strong>and</strong> collecting work. Despite these inadequacies, the<br />
table below from Neldner (1998) indicates a high floristic diversity within the Torres Strait Isl<strong>and</strong>s<br />
evidenced by the presence of 32% of the diversity of the vascular flora in 0.7% of the area of Cape<br />
York Peninsula (Neldner 1998).<br />
Table 3. Summary of the native vascular flora of the Torres Strait isl<strong>and</strong>s in comparison with Cape York<br />
Peninsula (from Neldner <strong>and</strong> Clarkson 1995 in Neldner 1998).<br />
Families<br />
Taxa<br />
Cape York<br />
Peninsula<br />
Families<br />
Taxa<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
9.5<br />
3.2<br />
-<br />
2.3<br />
2.1<br />
Pteridophytes Gymnosperms Angiosperms Total<br />
11<br />
26<br />
1<br />
1<br />
139<br />
977<br />
1.1<br />
0.4<br />
-<br />
0.3<br />
0.2<br />
155<br />
1,067<br />
Pteridophytes Gymnosperms Angiosperms Total<br />
30<br />
157<br />
5<br />
6<br />
183<br />
3,173<br />
218<br />
3,338<br />
Analysis of data extracted from Herbrecs 2007 lists 26 species listed as Endangered, Vulnerable<br />
<strong>and</strong> Rare (EVR) (see <strong>Appendix</strong> C). An online search of the Environment Protection Biodiversity<br />
<strong>and</strong> Conservation Act 1999 (EPBC Act) for the Torres Shire identifies 18 threatened flora species<br />
<strong>and</strong> the potential occurrence of one Threatened Ecological Community.<br />
Previously, much of the published information relevant to the regions natural <strong>and</strong> cultural history<br />
is available in ‘Bridge <strong>and</strong> Barrier’ (Walker 1972), which, in addition to a wealth of information<br />
on environmental, faunal <strong>and</strong> cultural topics, offers detailed analyses on aspects of plant<br />
biogeography. These include papers on; ecological comparisons of vegetation on either side of<br />
Torres Strait (Webb <strong>and</strong> Tracey 1972); species distribution patterns (Hoogl<strong>and</strong> 1972);<br />
biogeography of tropical eucalypts (Carr 1972) <strong>and</strong> distribution of Loranthaceae (Barlow 1972).<br />
Wace (1972) in his discussion on the plant geography around Torres Strait reflects how the<br />
aforementioned are: “based upon more or less insecure taxonomic foundations, <strong>and</strong><br />
acknowledged gaps in distributional data”, <strong>and</strong> further that “a common theme underlying all the<br />
papers is our almost total ignorance of past environments in the Torres Strait itself” (in Walker<br />
1972 pp. 198). The conclusions of Walker (1972), Mulrennan (1992), Mackey et al. (2006) <strong>and</strong><br />
Freebody (2002) all refer to a lack of taxonomic <strong>and</strong> distributional data required to determine the<br />
limits of most plants at a species level within the region the need for detailed biological surveys<br />
to inform planning <strong>and</strong> management of unique <strong>and</strong> fragile isl<strong>and</strong> natural <strong>and</strong> cultural values.<br />
8
Plant taxonomy <strong>and</strong> distributional data have been considerably advanced through initiatives such<br />
as CYPLUS <strong>and</strong> various taxonomic treatments.<br />
Studies of past environments have also developed an increasing body of literature. Palynological<br />
studies (Rowe 2006, Parr 2003, Barham 1999) <strong>and</strong> archaeological <strong>and</strong> anthropological<br />
investigations (David et al. 2004, David <strong>and</strong> Badugal 2006, Barham <strong>and</strong> Harris 1987, Barham et<br />
al. 2004, Shnukal 2004, McNiven 2008) offer an important cultural context for biodiversity<br />
assessment <strong>and</strong> elucidate anthropogenic influences on isl<strong>and</strong> biodiversity over a period of human<br />
occupation in the region of between 8 000 <strong>and</strong> 6 000 years (Rowe 2006) with permanent isl<strong>and</strong><br />
occupation occurring between around 3 800–2 500 years (BP) (David <strong>and</strong> Badugal 2006).<br />
3.2 Image Base Compilation <strong>and</strong> Aerial Photograph Analysis<br />
The initial stage of desktop assessment involved a compilation of remotely sensed imagery<br />
suitable for vegetation mapping purposes. Aerial photography was the preferred information<br />
base, allowing stereoscopic assessment of vegetation <strong>and</strong> l<strong>and</strong>form patterns <strong>and</strong> giving greater<br />
confidence to assignment of l<strong>and</strong> zone <strong>and</strong> vegetation structure classification. Historical aerial<br />
photography also provided a means to assess the pre-clearing distribution of vegetation<br />
communities in a large number of cases. Satellite imagery was used as a secondary means of<br />
vegetation community assessment where suitable aerial photography was not available, <strong>and</strong> was<br />
used as a base for photo-registration during digital processing, as well as a means of st<strong>and</strong>ardising<br />
vegetation mapping scales. A summary of aerial photography used in this assessment is provided<br />
in Table 4 below. Assessment of photograph quality relates to a subjective appraisal of image<br />
clarity, site coverage, shadow <strong>and</strong> cloud cover.<br />
Table 4. Aerial photography used for vegetation assessment purposes.<br />
Isl<strong>and</strong>/Isl<strong>and</strong><br />
Group<br />
Year Scale<br />
Schenckler Aerial Survey<br />
Negative Quality<br />
Buru 1999 1:12 000 Colour Excellent<br />
Mabuiag 1999 1:8 000 Colour Excellent<br />
Erub 1999 1:8 000 Colour Excellent<br />
Stephen 1999 1:4 000 Colour Excellent<br />
Iama 1999 1:4 000 Colour Excellent<br />
Yorke 1999 1:4 000 Colour Excellent<br />
Zagai 1999 1:16 000 Colour Excellent<br />
Ului 1999 1:8 000 Colour Excellent<br />
Zurat 1999 1:8 000 Colour Excellent<br />
Aureed 1999 1:9 000 Colour Excellent<br />
Warral 1999 1:16 000 Colour Excellent<br />
Deliverance 1999 1:4 000<br />
Commonwealth Flying<br />
Colour Excellent<br />
Murray 1988 1:30 000 B&W Moderate<br />
Dauan 1988 1:18 000 B&W Moderate<br />
Gabba 1988 1:25 000 Colour Excellent<br />
Deliverance 1971 1:42 000 B&W Moderate<br />
Adolphus 1973 1:34 000 B&W Poor<br />
Tudu 1973 1:12 000 B&W Excellent<br />
Moa<br />
Badu<br />
1974 1:34 000 B&W Poor<br />
Moa-Badu 1971 1:85 000 B&W Excellent<br />
Sassie, Burpa,<br />
Warraber<br />
1973 1:50 000<br />
State Flying<br />
B&W Moderate<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
9
Isl<strong>and</strong>/Isl<strong>and</strong><br />
Group<br />
Cooktown-Crab<br />
Isl<strong>and</strong> (Prince of<br />
Wales, Thursday<br />
Group)<br />
Torres Strait Isl<strong>and</strong><br />
– Coconut Isl<strong>and</strong><br />
Boigu Isl<strong>and</strong> 74<br />
Project Aerial<br />
Photography<br />
Saibai Isl<strong>and</strong><br />
Photography 1<br />
Year Scale Negative Quality<br />
1992 1:50 000<br />
Colour<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
Excellent<br />
1975 1:37 800 B&W Excellent<br />
1974 1:10 000 B&W Excellent<br />
1974 1:10 000 B&W Excellent<br />
Two sources of satellite imagery were provided to the project by TSRA. Of these, satellite<br />
imagery sourced from Ikononos was by far the most usable, supplied in a single false colour<br />
image for a number of the individual isl<strong>and</strong>s including Saibai <strong>and</strong> Boigu. Quickbird imagery for<br />
the majority of the larger continental isl<strong>and</strong>s, including the Inner <strong>and</strong> Near Western Isl<strong>and</strong><br />
Groups, was provided in a number of separate tiles. The full satellite image coverage of Muralug<br />
for example consisted of 40 individual unreferenced tiles of different sizes <strong>and</strong> shapes. The<br />
spectral signatures of these tiles lacked consistency, requiring a high degree of image<br />
manipulation to ensure spectral signatures could be matched between tiles, <strong>and</strong> matching could<br />
not always be achieved. Due to the enormous processing power required, it was not possible to<br />
load more than a limited number of tiles at any time, <strong>and</strong> this did not allow for an overview of the<br />
broader l<strong>and</strong>scape as is required in a regional mapping exercise. For this reason Quickbird<br />
imagery proved unsuitable for the supplied purpose other than to provide a basis for aerial<br />
photograph rectification. The data format provided for the Quickbird imagery resulted in<br />
considerable time being used to reference tiles, <strong>and</strong> added greatly to the time taken for the digital<br />
processing (8-10 days). The usefulness of both Ikononos <strong>and</strong> Quickbird imagery was hindered<br />
by considerable cloud cover <strong>and</strong> resulting shadow in some areas, particularly on Muralug, Dauan,<br />
Mabuiag <strong>and</strong> Saibai Isl<strong>and</strong>s.<br />
3.3 Site Locations<br />
Aerial photography was analysed stereoscopically in an initial phase of pre-survey interpretation<br />
designed specifically to:<br />
a) target a representative range of habitats within the study area;<br />
b) sample those communities that are useful for provision of reference condition, or ‘best<br />
type examples’ of specific vegetation types, <strong>and</strong>;<br />
c) direct detailed sampling towards those communities that could not be adequately<br />
categorised through API, or were considered critical to a range of significant flora<br />
species.<br />
Further sites were added opportunistically during the field survey to provide a more complete<br />
data coverage <strong>and</strong> allow a verification of the mapping units to st<strong>and</strong>ard herbarium procedure.<br />
The locations of field survey sites is spatially illustrated in Figure 2a to 2e. A summary of<br />
isl<strong>and</strong>s <strong>and</strong> sites provided in Table 5 indicates 1 372 sites completed during the field survey.<br />
This comprised 74 secondary level sites, 2 tertiary level sites <strong>and</strong> 1 296 quaternary level sites.<br />
1 Aerial photography for the southern portion of Saibai Isl<strong>and</strong> only.<br />
10
Table 5. Site survey effort in Stage 1 <strong>and</strong> broader study areas<br />
Isl<strong>and</strong><br />
Quaternary<br />
Sites<br />
Secondary Sites Tertiary Sites<br />
Total Sites per<br />
Isl<strong>and</strong><br />
Aureed* 3 - - 3<br />
Badu 2 43 4 - 47<br />
Boigu** 96 2 - 98<br />
Buru* 1 - - 1<br />
Dauan 50 6 - 56<br />
Erub (Darnley) 51 11 - 62<br />
Gaboy* 1 - - 1<br />
Giralug (Friday) 26 - - 26<br />
Gebar** 34 - - 34<br />
Iama (Yam) 30 4 - 34<br />
Keriri (Hammond)** 40 - - 40<br />
Layoak* 2 - - 2<br />
Masig (Yorke) 5 11 - 16<br />
Mabuiag 51 7 - 58<br />
Mawai (Wednesday) 21 - - 21<br />
Mer (Murray) 32 4 - 36<br />
Mer/Duaur* 10 - - 10<br />
Moa** 178 9 2 189<br />
Muralug (PoW)** 222 3 - 225<br />
Morilug (Little Adolphus)* 8 - - 8<br />
Morilug (Mt Adolphus)* 27 - - 27<br />
Naghir** 11 - - 11<br />
Ngurupai (Horn)** 65 - - 65<br />
Palilug (Goode) 9 - - 9<br />
Possession* 4 - - 4<br />
Saibai** 185 12 - 197<br />
Sassie** 9 1 - 10<br />
Tudu** 8 - - 8<br />
Waibene (Thursday) 13 - - 13<br />
Warraber (Sue)* 6 - - 6<br />
Warral (Hawkesbury)** 25 - - 25<br />
Zagai* 10 - - 10<br />
Zuna (Entrance) 20 - - 20<br />
Total Sites<br />
* indicates helicopter survey only<br />
1296 74 2 1372<br />
** indicates on ground sites supplemented by helicopter sites<br />
2 Badu Is. sites limited to Council managed l<strong>and</strong>s in close vicinity to community.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
11
Legend<br />
Waral Kawa (Deliverance) Is<br />
Quaternary<br />
Quaternary (Helicopter)<br />
Secondary<br />
Tertiary<br />
PAPUA NEW GUINEA<br />
Western Province<br />
TORRES<br />
0 15 30 45 60<br />
N O T E : S<br />
(i) his T plan has n produced bee r exclusive fo use<br />
of the ient cl <strong>and</strong> 3D Environmental<br />
Kilometres<br />
Boigu Is<br />
Buru (Turnagain) Is.<br />
Dauan Is<br />
CORAL SEA<br />
F igur e 2a . Surve y locati ons –<br />
Top Wester n Isl <strong>and</strong>s<br />
Client<br />
STRAIT<br />
To res Stra it Reg ional Aut hority<br />
Gebar Is.<br />
Saibai Is<br />
3D Environmental<br />
Vegetati on Ass essm ent<br />
& Mapping Specialists<br />
P. O. x Bo 95 9<br />
Kenmore, ld Q 69 40<br />
Phone: (07) 9072; 3411 (07) 3878 44 43<br />
M obil e: 404 0 7 57285<br />
; 0409 426 691<br />
www.3denv ironm ental.com .au<br />
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Legend<br />
Quaternary<br />
Ugar (Stephens) Is<br />
Quaternary (Helicopter)<br />
Secondary<br />
Tertiary<br />
0 5 10 15 20<br />
N O T E : S<br />
Kilometres<br />
(i) his T plan has n produced bee r exclusive fo use<br />
of the ient cl <strong>and</strong> 3D Environmental<br />
Erub (Darnley) Is<br />
Client<br />
Dawar<br />
F igur e 2b . Surve y locati ons – Easte rn sl<strong>and</strong>s I<br />
To res Stra it ion Reg al Aut hority<br />
Waier<br />
Mer (Murray) Isl<strong>and</strong>s<br />
3D Environmental<br />
Vegetati on Ass essm ent<br />
& Mapping Specialists<br />
P. O. x Bo 95 9<br />
Kenmore, ld Q 69 40<br />
Phone: (07) 9072; 3411 (07) 3878 44 43<br />
M obil e: 404 0 7 57285<br />
; 0409 426 691<br />
www.3denv ironm ental.com .au<br />
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Gebar Isl<strong>and</strong><br />
0 5 10 15 20<br />
N O T E : S<br />
Kilometres<br />
(i) his T plan has n produced bee r exclusive fo use<br />
of the ient cl <strong>and</strong> 3D Environmental<br />
Iama (Yam) Isl<strong>and</strong><br />
Bet - Bara Isl<strong>and</strong><br />
Sassie Isl<strong>and</strong><br />
Warraber (Sue) Islet<br />
Zagai Isl<strong>and</strong><br />
Tudu Isl<strong>and</strong><br />
Poruma (Coconut) Is<br />
Client<br />
STRAIT<br />
Aureed Isl<strong>and</strong><br />
F igur e 2c. Survey locati ons – Cent ralIsl<br />
<strong>and</strong>s<br />
To res Stra it ion Reg al Aut hority<br />
Legend<br />
Masig (Yorke) Isl<strong>and</strong>s<br />
Quaternary<br />
Quaternary (Helicop<br />
Secondary<br />
Tertiary<br />
3D Environmental<br />
Vegetati on Ass essm ent<br />
& Mapping Specialists<br />
P. O. x Bo 95 9<br />
Kenmore, ld Q 69 40<br />
Phone: (07) 9072; 3411 (07) 3878 44 43<br />
M obil e: 404 0 7 57285<br />
; 0409 426 691<br />
www.3denv ironm ental.com .au<br />
Scale<br />
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TORRES<br />
0 5 10 15 20<br />
N O T E : S<br />
Kilometres<br />
(i) his T plan has n produced bee r exclusive fo use<br />
of the ient cl <strong>and</strong> 3D Environmental<br />
Mabuiag Isl<strong>and</strong><br />
Badu Isl<strong>and</strong><br />
Warral Isl<strong>and</strong><br />
Moa Isl<strong>and</strong><br />
Client<br />
Naghir (Mt Ernest) Isl<strong>and</strong><br />
F igur e 2d . Surve y locati ons –<br />
Near estern W Isl <strong>and</strong>s<br />
To res Stra it ion Reg al Aut hority<br />
Legend<br />
Quaternary<br />
Quaternary (Helicop<br />
Secondary<br />
Tertiary<br />
3D Environmental<br />
Vegetati on Ass essm ent<br />
& Mapping Specialists<br />
P. O. x Bo 95 9<br />
Kenmore, ld Q 69 40<br />
Phone: (07) 9072; 3411 (07) 3878 44 43<br />
M obil e: 404 0 7 57285<br />
; 0409 426 691<br />
www.3denv ironm ental.com .au<br />
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Giralag (Friday) Isl<strong>and</strong><br />
Kirriri (Hammond) Isl<strong>and</strong><br />
Palilag (Goods0 Isl<strong>and</strong><br />
Muralug (Prince of<br />
Wales) Isl<strong>and</strong><br />
Waibene (Thursday) Isl<strong>and</strong><br />
0 5 10 15 20<br />
N O T E : S<br />
(i) his T plan has n produced bee r exclusi fove<br />
use<br />
of the ient cl <strong>and</strong> 3D Environmental<br />
Kilometres<br />
Ngurapai (Horn) Isl<strong>and</strong><br />
Maiwaii (Wednesday) Isl<strong>and</strong><br />
Zuna (Entrance0 Isl<strong>and</strong><br />
Possession Isl<strong>and</strong><br />
Client<br />
Cape York Peninsula<br />
F igur e 2e . Surve y locati ons – ner In Isl <strong>and</strong>s<br />
To res Stra it ion Reg al Aut hority<br />
Legend<br />
Quaternary<br />
Quaternary (Helico<br />
Secondary<br />
Tertiary<br />
Little Adolphus Isl<strong>and</strong><br />
Mount Adolphus Isl<strong>and</strong><br />
Albany Is.<br />
3D Environmental<br />
Vegetati on Ass essm ent<br />
& Mapping Specialists<br />
P. O. x Bo 95 9<br />
Kenmore, ld Q 69 40<br />
Phone: (07) 9072; 3411 (07) 3878 44 43<br />
M obil e: 404 0 7 57285<br />
; 0409 426 691<br />
www.3denv ironm ental.com .au<br />
Scale<br />
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3.4 Field Survey Procedure<br />
The execution of the field survey within the time <strong>and</strong> budgetary constraints of the project<br />
presented a number of logistical challenges. As a priority, protocols necessary to achieve access<br />
to isl<strong>and</strong> communities <strong>and</strong> native title l<strong>and</strong>s were developed in consultation <strong>and</strong> support of<br />
TSRA’s L<strong>and</strong> <strong>and</strong> Sea Management Unit <strong>and</strong> Native Title office. These consisted of an initial<br />
round of introductory letters to all isl<strong>and</strong> councils <strong>and</strong> Prescribed Body Corporate (PBC) bodies<br />
followed by phone or fax communication prior to the actual field visit where possible to organize<br />
time of arrival, accommodation etc. Meetings with appropriate community representatives <strong>and</strong><br />
AQIS officers were held on each isl<strong>and</strong> <strong>and</strong> served to advise <strong>and</strong> guide the survey team in regards<br />
to adherence to cultural protocols whilst on country. Where necessary <strong>and</strong> possible, cultural<br />
monitors accompanied the survey team.<br />
The requirement to achieve a regional overview within a short time frame <strong>and</strong> with consideration<br />
to budget necessitated a single <strong>and</strong> continuous field trip over a seven week period between 16<br />
October <strong>and</strong> 2 December 2007 wherein two ecologists aimed to access <strong>and</strong> describe as many<br />
representative vegetation communities as possible. Access to isl<strong>and</strong>s was achieved mainly by<br />
commercial air service (Aero Tropics) <strong>and</strong> also by charter plane <strong>and</strong> helicopter. The use of a<br />
survey vehicle on Moa, Erub, Thursday, Horn <strong>and</strong> Masig assisted site coverage although survey<br />
by walking traverses guided by stereoscopic use of aerial photography was the predominant mode<br />
of survey. A charter boat was used to access isl<strong>and</strong>s in the Inner Group particularly Muralug,<br />
Zuna, Friday, Hammond, <strong>and</strong> Wednesday. This provided a preliminary, although thorough<br />
assessment of vegetation in the study area that was supplemented by 11 hours of helicopter<br />
flying. The latter was an invaluable means of gaining a regional perspective of the isl<strong>and</strong>s,<br />
increasing site coverage <strong>and</strong> allowing the establishment of vegetation sites in otherwise<br />
inaccessible locations.<br />
Field survey method followed Queensl<strong>and</strong> Herbarium st<strong>and</strong>ards as identified in Neldner et al.<br />
(2005) using a combination of formalised secondary, tertiary <strong>and</strong> quaternary level sampling<br />
procedures, as well as informal site observation. Data relevant to requirements of Neldner et al.<br />
(2005) were modified to suit sampling requirements specific to the study <strong>and</strong> were entered into<br />
field notebooks. The core field information recorded included location, tenure, air photo <strong>and</strong> site<br />
photo references, l<strong>and</strong>form <strong>and</strong> geological features, <strong>and</strong> community structure. Complete species<br />
lists were compiled wherever these were considered appropriate <strong>and</strong> were not limited to<br />
secondary sites. Canopy height was meticulously measured at all sample locations using a<br />
clinometer <strong>and</strong> linear regression table, <strong>and</strong> canopy cover was recorded in the majority of sites<br />
using measured crown intercept transects. A Garmin GPS 60 (Geographic Positioning System)<br />
was used to accurately record map coordinates for the site locations (GDA94). Digital<br />
photographs of all sites as well as geological <strong>and</strong> l<strong>and</strong>form features <strong>and</strong> significant flora species<br />
were captured using a digital camera.<br />
Secondary sites of non-rainforest vegetation consisted of a 50m x 10m plot located along the<br />
contour with attempts made to avoid the sampling across vegetation community boundaries,<br />
which became difficult in some of the lineal vegetation communities. Bitterlich measurements,<br />
as described in Grosenbaugh (1952), were used to record community basal area at all sites except<br />
in highly linear communities where the method proved inappropriate. Full species lists for all<br />
strata were established during the secondary sampling procedure wherein the 500m 2 plot was<br />
intensively sampled followed by a detailed search of the vicinity. While the vicinity search was<br />
broadly defined by the extent of the basal area sweep, it was in all cases confined to the target<br />
community. The abundance of all species within the plot was recorded by stem counts <strong>and</strong> by a<br />
visually assessed abundance ranking.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
17
Data at rainforest sites were collected using a variable area 32 nearest neighbour method as<br />
consistent with data collected for the Cape York Bioregion (Stanton <strong>and</strong> Fell 2005). Tertiary<br />
sites were completed in a similar fashion to secondary procedure, except non-woody species were<br />
not recorded. Sites recorded at tertiary level consisted of full species lists in a search area<br />
established via a radial sweep of the Bitterlich device.<br />
Quaternary sites comprised a description of floristic structure, composition, <strong>and</strong> associated<br />
l<strong>and</strong>form. <strong>Vegetation</strong> communities were also recorded on walking traverses. Botanical voucher<br />
specimens were collected throughout the field survey to verify site floristics <strong>and</strong> enable<br />
identification of those species that were problematic. All material was pressed in the field before<br />
being packaged in ethanol as required under AQIS Quarantine Permit. A total of 740 vouchers<br />
were collected.<br />
3.5 Classification of L<strong>and</strong> <strong>and</strong> <strong>Vegetation</strong><br />
Photograph 3. Helicopter l<strong>and</strong>ing<br />
site Saibai Isl<strong>and</strong>.<br />
A vegetation type is defined as a unit of structurally <strong>and</strong> floristically similar vegetation, whilst a<br />
l<strong>and</strong> type is defined as a unit of structurally <strong>and</strong> floristically similar vegetation on a similar<br />
geology (Stanton <strong>and</strong> Morgan 1977, Sattler <strong>and</strong> Williams 1998). <strong>Vegetation</strong> types are referred to<br />
as ‘vegetation communities’ (VC) <strong>and</strong> are consistently referred to as such throughout this<br />
document, whilst l<strong>and</strong> types are incorporated into the broader RE classification. <strong>Vegetation</strong><br />
communities have been amalgamated to form ‘Broad <strong>Vegetation</strong> Groups’ (BVG’s) <strong>and</strong> are used<br />
to describe structurally similar vegetation groups, or in specific cases, vegetation groups<br />
controlled by similar ecological conditions. Broad <strong>Vegetation</strong> Groups are useful both as a means<br />
to spatially represent detailed floristic information, <strong>and</strong> to define associated ecological parameters<br />
including faunal habitat. The BVG is used as a primary subdivision to define a floristic/structural<br />
type. This is followed by an alpha suffix to define a specific VC. A VC code may be<br />
complemented by an appended code indicating particular structural attributes (e.g. a vine forest<br />
sub-canopy), or as an indicator of vegetation condition. Explanatory notes for vegetation coding<br />
are described in Section 4.1.<br />
<strong>Vegetation</strong> communities are assigned to RE’s on the basis of a three-part code of which the<br />
primary subdivision is bio-regional zone, followed by geology or l<strong>and</strong> zone, with specific floristic<br />
attributes providing the tertiary subdivision. <strong>Vegetation</strong> communities are often amalgamated to<br />
form RE’s, <strong>and</strong> these communities may retain autonomy through classification as a RE sub-unit.<br />
RE’s are assessed on a state wide basis for conservation significance, as regulated by<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
18
Queensl<strong>and</strong>’s <strong>Vegetation</strong> Management Act (1999), (VMA). The RE classification system<br />
requires detailed knowledge <strong>and</strong> underst<strong>and</strong>ing of both l<strong>and</strong>form <strong>and</strong> geology <strong>and</strong> these features<br />
have been described <strong>and</strong> classified in this report.<br />
3.5.1 Non-Rainforest <strong>Vegetation</strong><br />
<strong>Vegetation</strong> structure is classified according to the system of Neldner et al. (2005) modified from<br />
Specht (1970) <strong>and</strong> this classification has been applied consistently to vegetation throughout the<br />
field survey <strong>and</strong> broader flora study. Structural formation classes as qualified by Neldner et al.<br />
(2005) are detailed in Table 6.<br />
3.5.2 Classification of Rainforest <strong>Vegetation</strong><br />
The classification of rainforest vegetation is based on the classification of Walker <strong>and</strong> Hopkins<br />
(1990) which is adapted from Webb (1959). This classification describes rainforest in terms of<br />
several attributes including:<br />
1. Complexity of life forms including species diversity in a number of structural layers. The<br />
presence / absence of structural features including plank buttresses, banyans etc.<br />
Complexity is recorded as either simple, simple-complex, <strong>and</strong> complex;<br />
2. The leaf sizes of the dominant plants/strata. Leaf size options are macrophyll, mesophyll,<br />
notophyll, microphyll <strong>and</strong> nanophyll;<br />
3. The floristic composition of the dominant stratum including the tendency for one or more<br />
species to dominate or otherwise;<br />
4. Indicator growth forms including the presence of palms, moss etc.; <strong>and</strong><br />
5. Height <strong>and</strong> crown cover classes including the presence of emergents;<br />
6. Thicket is used to described stunted rainforest vegetation in which the canopy closes at 3-<br />
9 m (Webb, 1959);<br />
7. ‘Deciduous’ in reference to a rainforest st<strong>and</strong> means that the species in question, or at<br />
least certain individuals in the species population, completely lose their leaves for a time<br />
<strong>and</strong> that this behaviour is obligatory <strong>and</strong> fixed for the species (Webb, 1959).<br />
8. ‘Semi- deciduous’ indicates that most leafless species are truly deciduous, but that some<br />
are facultative, i.e. leaf-fall is controlled by the severity of the dry season, rather than by<br />
being obligate (Webb, 1959); <strong>and</strong><br />
9. ‘Semi-evergreen’ means that few or none the species are truly deciduous, <strong>and</strong> that most<br />
of those that shed their leaves do so incompletely depending on the severity of the dry<br />
season (Webb, 1959).<br />
It should be noted that in accordance with the classification of Walker <strong>and</strong> Hopkins (1990),<br />
emergents are classified as trees clearly above the dominant stratum whose crown cover is less<br />
than 5% of the total canopy cover. This classification of an emergent stratum is not extended to<br />
severely disturbed communities whose structural integrity has been compromised through human<br />
intervention.<br />
Table 6. Structural formation classes qualified by height for Non-Rainforest <strong>Vegetation</strong>: Neldner et al.<br />
2005) modified from Specht (1970).<br />
Projective Foliage<br />
Cover<br />
70-100% 30-70% 10-30% 30m tall closed-forest tall open-forest tall woodl<strong>and</strong> tall open-<br />
3 Growth form of the predominant layer (the ecologically dominant layer).<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
19
Projective Foliage<br />
Cover<br />
70-100% 30-70% 10-30%
3.6 Scale of Survey<br />
In vegetation survey, sampling scale is determined by sampling intensity, influenced by<br />
vegetation complexity <strong>and</strong> the areal extent of remnant vegetation. The Agricultural Organisation<br />
of the United Nations (FAO 1979) recommends 25 sites per km 2 for 1:10 000 scale soil survey,<br />
although Neldner et al. (2005) recommend a minimum of half of this sampling density for<br />
vegetation survey, dependant on the vegetation complexity <strong>and</strong> areal extent of remnant<br />
vegetation. Reference to Table 5 indicates 1 372 survey locations recorded during the initial<br />
phase of field survey, with an additional 34 sites recorded during previous mapping exercises<br />
(EPA Corveg sites). Resultant sampling equates to roughly 1:25 000 scale, based on a total l<strong>and</strong><br />
area of 892 km 2 <strong>and</strong> minimum site requirements as per Neldner et al. (2005). This data is suitable<br />
for incorporation into detailed state wide regional ecosystem assessments at present sampling<br />
intensity, although additional sites will be gathered during any subsequent survey phases.<br />
The spatial scale <strong>and</strong> accuracy of a mapping product is determined in part by the scale of the<br />
image base used for vegetation community delineation. Reference to Table 4 indicates<br />
considerable disparity between aerial photographic scales used in the assessment, ranging from<br />
1:4 000 scale on Iama Isl<strong>and</strong> to 1:85 000 on Moa. This disparity in spatial scales was addressed<br />
to a degree during the photo rectification process, whereby photographic line work was registered<br />
against satellite imagery at a st<strong>and</strong>ardised 1:25 000 scale, as required in the project brief. Whilst<br />
this process will have rectified disparities in spatial scale between isl<strong>and</strong>s to a large degree,<br />
variations in the scale of vegetation community delineation between isl<strong>and</strong>s as well as spatial<br />
accuracy of vegetation linework can be expected.<br />
3.7 Image Interpretation <strong>and</strong> Attribution Method<br />
Aerial photography was purchased as contact prints <strong>and</strong> subject to detailed stereoscopic<br />
assessment. The aim of stereoscopic analysis is to delineate consistently mappable units<br />
(polygons) of homogenous vegetation characterised through similarity of aerial photographic<br />
pattern or signature. During this process, geological <strong>and</strong> vegetation community boundaries were<br />
marked directly onto the aerial photography with removable white china ink, <strong>and</strong> a 0.25mm<br />
Rotring pen. The width of vegetation line work produced was between 0.25mm <strong>and</strong> 0.5mm with<br />
finer line work resulting in a more accurate delineation of vegetation community boundaries.<br />
Polygon attribution is based on a hierarchical system identifying l<strong>and</strong>form/geological affiliation,<br />
vegetation structure, <strong>and</strong> floristic composition. This stratification was consistent with basic rules<br />
of vegetation classification detailed in Section 3.5.<br />
Where suitable aerial photographic material was not available, satellite imagery was used as a<br />
base for vegetation community delineation with vegetation line work established directly on the<br />
digital image <strong>and</strong> incorporated into the broader spatial database. In the case of Saibai Isl<strong>and</strong>,<br />
where suitable aerial photographic coverage was available for only half of the isl<strong>and</strong>, the line<br />
work established during aerial photographic interpretation was extrapolated across the broader<br />
study area, over the top of available satellite imagery.<br />
3.8 Pre-clearing <strong>Vegetation</strong> Method<br />
The oldest available photographic imagery was utilised to establish pre-clearing vegetation<br />
communities within the study area. <strong>Vegetation</strong> line work was established on these photographs,<br />
attributed accordingly, <strong>and</strong> overlain with the recent satellite imagery to determine the extent of<br />
clearing. <strong>Vegetation</strong> polygons were clipped to cleared boundaries on recent imagery to produce a<br />
‘Remnant <strong>Vegetation</strong> Layer’.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
21
Historically cleared vegetation was attributed with a code indicative of its pre-clearing status, <strong>and</strong><br />
an appended designator of its current status, whether it be cleared or in varying stages of<br />
regrowth. Where no suitable historical photography was available, ecological <strong>and</strong> geological<br />
knowledge gathered throughout the course of the survey was used to reconstruct the original<br />
vegetation mosaic. Existing vegetation communities <strong>and</strong> community boundaries are extrapolated<br />
across areas of similar geology <strong>and</strong> l<strong>and</strong>form to re-construct the pre-clearing l<strong>and</strong>scape.<br />
Reconstructed polygons were attributed with a code to indicate pre-clearing status <strong>and</strong> appended<br />
with a symbol to designate current status <strong>and</strong>/or condition. A separate pre-clearing layer was<br />
generated from re-constructed vegetation community mapping, allowing an assessment of the<br />
relative impacts of past l<strong>and</strong> use practice on specific vegetation communities.<br />
3.9 Digital Processing <strong>and</strong> Accuracy<br />
The marked aerial photographs were scanned at a resolution of 300dpi. Each photo was then<br />
registered within ArcMap using the geo-registration extension against the supplied Satellite<br />
imagery at 1:25 000 scale or greater. Upon completion of photo registration, the identified<br />
boundaries were captured as line-work. Final editing was performed when all of the boundaries<br />
had been captured, prior to generation of polygons in ARC/INFO format.<br />
As described in Section 3.6, spatial accuracy is determined largely by the scale of the image base<br />
used for the mapping exercise, the thickness of the vegetation linework, <strong>and</strong> photographic<br />
distortion (RMS error). Although photo registration <strong>and</strong> rectification was undertaken on a<br />
spatially consistent satellite image base, variations in spatial accuracy will occur due to the wide<br />
range of aerial photographic scales used during the assessment. All vegetation line-work was<br />
approximately 0.5 mm wide on the aerial photography <strong>and</strong> as a general rule, 0.5 mm on aerial<br />
photography at 1:10 000 scale (as used on Saibai <strong>and</strong> Boigu) is equivalent to 500 mm on the<br />
ground, which is equivalent to an accuracy of +/- 5 m. On 1:85 000 scale photography as was<br />
used on Moa Isl<strong>and</strong>, an accuracy of +/- 85 m can be expected. St<strong>and</strong>ardisation of the spatial<br />
accuracy between individual isl<strong>and</strong>s was achieved to some degree during the registration process<br />
which utilised st<strong>and</strong>ardized satellite imagery at 1:25 000 scale. On isl<strong>and</strong>s where smaller scale<br />
photography was used during the vegetation mapping process, particular attention was paid to<br />
ensure the coastline <strong>and</strong> areas around urban settlement were mapped with a spatial accuracy of<br />
1:25 000 scale or greater.<br />
The RMS error obtained during the registration process varied from photo to photo <strong>and</strong> between<br />
isl<strong>and</strong>s, although was particularly high on mountainous isl<strong>and</strong>s such as Mabuiag which were<br />
captured with low level photography. RMS error was introduced by the considerable radial<br />
distortion of the l<strong>and</strong>scape on the peripheries of the photography. Once again, this distortion was<br />
significantly reduced during the linework rectification process by utilizing st<strong>and</strong>ardized scale<br />
satellite imagery. It should be noted that in areas of significant cloud cover on satellite imagery,<br />
the spatial accuracy of the linework cannot be guaranteed.<br />
3.10 Limitations <strong>and</strong> Constraints<br />
The survey objectives were largely achieved, however a number of limitations <strong>and</strong> constraints are<br />
worthy of mention.<br />
• As previously discussed, Quickbird imagery proved unsuitable for the supplied purpose<br />
other than to provide a basis for aerial photograph rectification. The spectral signatures<br />
of Quickbird tiles lacked consistency, requiring a high degree of image manipulation to<br />
ensure spectral signatures could be matched between tiles which in many cases could not<br />
be achieved. This process consumed considerable time <strong>and</strong> effort (approximately 80<br />
hours of GIS time) that was not accounted for in the project budget. Furthermore, cloud<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
22
cover on both satellite formats created significant information gaps, particularly on<br />
Muralug, Mabuiag, Dauan <strong>and</strong> Saibai Isl<strong>and</strong>s.<br />
• Due to unforeseen circumstances, introductory letters sent to Badu Isl<strong>and</strong> Council <strong>and</strong> the<br />
PBC were not received by the appropriate representatives. Therefore the acting PBC<br />
Chair, executive <strong>and</strong> members had no prior knowledge of the projects purpose, <strong>and</strong><br />
subsequently, access to Native Title l<strong>and</strong>s was denied. Access to the small extent of<br />
DOGIT l<strong>and</strong> was granted through Badu Council, however the lack of representative<br />
vegetation communities within the DOGIT l<strong>and</strong> deemed it necessary for a secondary field<br />
trip to be scheduled to cover the entirety of the isl<strong>and</strong>. Following liaison with<br />
representatives of Mura Badulgal (Torres Strait Isl<strong>and</strong>er) Corporation PBC Body, Badu<br />
Council <strong>and</strong> the TSRA L<strong>and</strong> <strong>and</strong> Sea Management Unit, a second field trip to Badu<br />
Isl<strong>and</strong> was carried out between 22 July <strong>and</strong> 29 July 2008. Access to all areas outside of<br />
Council duristiction was however once again denied on the basis that the PBC body was,<br />
at that time, not a functioning entity <strong>and</strong> could not therefore facilitate a process to secure<br />
the consent of traditional owners for the survey team to access Native Title l<strong>and</strong>s. The<br />
survey was therefore limited to a small portion of the DOGIT l<strong>and</strong> around Badu village.<br />
• Minimal field data was collected on a number of small isl<strong>and</strong>s including atolls throughout<br />
the study area. Whilst such isl<strong>and</strong>s are indeed small, a number supported terrestrial<br />
vegetation <strong>and</strong> would be worthy of inspection. These include the more remote isl<strong>and</strong>s<br />
such as Deliverance where review of documentation from previous studies has proved<br />
valuable to achieve a preliminary classification of vegetation communities. The use of<br />
helicopter survey enabled a rapid overview of vegetation structure. In a number of<br />
instances however, assessment of the floristic composition could not be achieved. These<br />
areas include (but are not limited to) rainforest on the steep terrain of Gebar, Mt.<br />
Adolphus, <strong>and</strong> Naghir Isl<strong>and</strong>s which are recommended for on ground assessment during<br />
future field work programs.<br />
• Throughout the survey, every attempt was made to collect detailed site based floristic<br />
data, <strong>and</strong> provide collections of voucher specimens for species not readily identified in<br />
the field, or for records of poorly collected taxa. A thorough analysis of this floristic data<br />
however remains outside of the project scope. Vouchers of a number of species<br />
necessary for full floristic descriptions of vegetation communities <strong>and</strong> regional<br />
ecosystems await identification <strong>and</strong> are referred to with collection numbers throughout.<br />
A detailed floristic analysis utilizing the taxonomic <strong>and</strong> distributional data collected<br />
during the survey in combination with pre-existing data would be a valuable future<br />
supplement to the study, <strong>and</strong> would result in a significant contribution to the current<br />
knowledge of plant biogeography of the region.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
23
4.0 Results – Field Analysis<br />
4.1 Classification of L<strong>and</strong> <strong>and</strong> <strong>Vegetation</strong><br />
4.1.1 L<strong>and</strong> Zones<br />
Aerial photographic analysis completed in conjunction with detailed field survey effort indicates<br />
11 broad geological/l<strong>and</strong>form associations in the study area relevant to l<strong>and</strong> zone classification as<br />
per Neldner et al. (2005) <strong>and</strong> Harris (undated). These are given a specific geological attribute in<br />
the mapping process to allow associations between l<strong>and</strong> zone <strong>and</strong> vegetation to be recognised,<br />
<strong>and</strong> RE’s classified. The l<strong>and</strong>form/geological associations relevant to l<strong>and</strong> zone classification<br />
that are recognised in the study area are identified in Table 7 below <strong>and</strong> spatially illustrated in<br />
accompanying maps 3a to 3e. The derivation of these classifications is discussed briefly in<br />
Section 5.1.<br />
Table 7. Geological types <strong>and</strong> l<strong>and</strong> zones identified in the Torres Strait Isl<strong>and</strong>s.<br />
Geological<br />
Geological Description<br />
Attribute<br />
E Estuarine muds, alluvium (saline <strong>and</strong> brackish alluvium), coastal s<strong>and</strong>s <strong>and</strong><br />
rock shelves subject to saltwater incursion.<br />
D Coastal dunes, cheniers, calcareous beach s<strong>and</strong>s (including atolls), beach<br />
ridges <strong>and</strong> associated swales.<br />
A Alluvial plains, alluvial fans (active), terraces <strong>and</strong> fluvial sediments.<br />
Excludes alluvial sediments affected by tidal/saltwater incursion.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
EPA L<strong>and</strong><br />
Zone<br />
T Remnant colluvial surfaces. 5<br />
As Residual s<strong>and</strong>y plains <strong>and</strong> s<strong>and</strong>y terraces. 5<br />
L Exposed duricrust 7<br />
B Basalt escarpments <strong>and</strong> terraces. 8<br />
V Volcanic cones formed on ash <strong>and</strong> scoria. 8<br />
G Granite hillslopes <strong>and</strong> footslopes including boulder talus <strong>and</strong> colluvium. 12<br />
Gd Diorite <strong>and</strong> Dacite. 12<br />
Mg Metamorphosed granitoid rocks including hornfels. 12<br />
R Rhyolites <strong>and</strong> associated fine grained volcanic rocks including tuff,<br />
ignimbrite <strong>and</strong> a range of other acid volcanic extrusive <strong>and</strong> intrusive rocks.<br />
4.1.2 <strong>Vegetation</strong> <strong>Communities</strong><br />
The VC’s identified within the study area, in relation to specific Broad <strong>Vegetation</strong> Groups<br />
(BVG’s) <strong>and</strong> l<strong>and</strong> zone affiliations are listed in Table 8 below with distribution maps presented<br />
in the accompanying maps 4a to 4e. One hundred <strong>and</strong> fifty eight VC’s are identified within 27<br />
BVG’s. It should be noted that this classification relates to remnant vegetation only <strong>and</strong><br />
classification of non-remnant vegetation communities is discussed in Section 6.1.3. It should be<br />
noted in respect to the vine forest <strong>and</strong> thicket communities, that relatively fine scale floristic <strong>and</strong><br />
1<br />
2<br />
3<br />
12<br />
24
structural variations have been differentiated between isl<strong>and</strong>s <strong>and</strong> isl<strong>and</strong> groups. This was<br />
possible due to the geographic isolation that isl<strong>and</strong>s impose on their inherent vegetation, giving<br />
confidence that fine scale floristic variations are consistently represented <strong>and</strong> delineated. These<br />
communities however represent a snapshot of the floristic <strong>and</strong> structural variation present within<br />
the isl<strong>and</strong> group <strong>and</strong> a large number of intermediate variations may be present.<br />
Table 8. <strong>Vegetation</strong> <strong>Communities</strong> in the Project Area.<br />
<strong>Vegetation</strong><br />
Community<br />
Description<br />
Evergreen/Semi-evergreen vine forest <strong>and</strong> vine thicket<br />
Geologies<br />
1a Evergreen notophyll vine forest + Acmenospermum claviflorum<br />
+ Syzygium puberulum + Ganophyllum falcatum + Arytera<br />
divaricata + Ficus microcarpa + *Mangifera indica.<br />
G<br />
1b Evergreen notophyll vine thicket (windsheared) + Manilkara<br />
kauki + Intsia bijuga + Pouteria sericea + Aglaia elaeagnoidea<br />
+ Garcinia warrenii + P<strong>and</strong>anus sp.<br />
G<br />
1c Evergreen notophyll vine thicket (windsheared) + Manilkara<br />
kauki + Celtis philippensis + Terminalia muelleri + Diospyros<br />
maritima + Thespesia populneiodes + Drypetes deplanchei.<br />
D<br />
1d Mesophyll/notophyll vine forest + Endi<strong>and</strong>ra glauca + Acacia<br />
polystachya + Syzygium bungadinnia + Canarium australianum<br />
+ Dysoxylum oppositifolium.<br />
GD, R<br />
1e Mesophyll/notophyll vine forest + Myristica insipida + G<br />
Maranthes corymbosa + Cryptocarya cunninghamii +<br />
1f<br />
Dysoxylum latifolium + Calophyllum sil +/- Arenga australasica.<br />
Complex notophyll vine forest + Pouteria sp. + Calophyllum sil<br />
+ Argyrodendron poly<strong>and</strong>rum + Palaquium galactoxylon +<br />
Acmenospermum claviflorum + Licuala ramsayi.<br />
G<br />
1g Evergreen notophyll vine thicket + Calophyllum sil + Syzygium<br />
br<strong>and</strong>erhorstii + Diospyros hebecarpa + Schefflera actinophylla<br />
+ Podocarpus grayae +Licuala ramsayi.<br />
G<br />
1h Evergreen notophyll vine thicket with Buchanania arborescens + R<br />
Drypetes deplanchei + Eleaodendron melanocarpum +<br />
1i**<br />
Endi<strong>and</strong>ra glauca + Elaeocarpus arnhemicus + Chionanthus<br />
ramiflora.<br />
Evergreen mesophyll vine forest + Horsfieldia australiana,<br />
Syzygium bamagense + Acmena hemilampra subsp. hemilampra<br />
+ Buchanania arborescens.<br />
A<br />
1j Tall evergreen notophyll vine forest + Syzygium angophoroides +<br />
Acmena hemilampra subsp. hemilampra + Acacia auriculiformis<br />
+ Syzygium forte subsp. forte + Podocarpus grayae<br />
Deciduous/Semi deciduous vine forest <strong>and</strong> vine thicket<br />
A<br />
2a Deciduous/Semi-deciduous vine forest + Erythrina variegata +<br />
Manilkara kauki + Terminalia subacroptera + Mimusops elengi<br />
+ Cordia subcordata.<br />
D<br />
2b Semi deciduous vine forest/thicket + Canarium australianum +<br />
Terminalia subacroptera + Bombax ceiba var. leiocarpum +<br />
Cochlospermum gillivraei + Cleistanthus peninsularis + Ficus<br />
virens var. sublanceolata.<br />
G,R<br />
2c Semi-deciduous vine thicket + Mimusops elengi + Acacia<br />
auriculiformis + Terminalia subacroptera + Diospyros spp. +/-<br />
Manilkara kauki +/- Melaleuca cajuputi subsp. platyphylla.<br />
A<br />
2d Semi deciduous vine forest + Tetrameles nudiflora + Canarium<br />
australianum + Ficus spp. + Bombax ceiba var. leiocarpum +/-<br />
Alstonia spectabilis.<br />
G<br />
2e Semi deciduous vine thicket + Terminalia subacroptera + Intsia<br />
bijuga + Hibiscus tiliaceus + Excoecaria agallocha + Thespesia<br />
populneoides + Cathormion umbellatum subsp. moniliforme.<br />
L<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
25
<strong>Vegetation</strong><br />
Community<br />
Description Geologies<br />
2f Semi-deciduous vine thicket + Canarium australianum +<br />
Manilkara kauki + Dalbergia densa var. australis + Buchanania<br />
arborescens + Sterculia sp. (Annan River L.J. Brass 20319) +<br />
Cochlospermum gillivraei.<br />
R<br />
2g Semi deciduous notophyll vine forest + Canarium australianum<br />
+ Terminalia subacroptera + Semecarpus australiensis +<br />
Buchanania arborescens + Acacia auriculiformis +/- Erythrina<br />
variegata +/- Welchiodendron longivalve +/- Parinari nonda +/-<br />
Chionanthus ramiflora.<br />
A<br />
2h Deciduous notophyll vine forest + Erythrina insularis +/-<br />
Antiaris toxicaria var. macrophylla+/- Terminalia subacroptera<br />
+/- Bombax ceiba var. leiocarpum +/- Canarium australianum +<br />
Acacia auriculiformis.<br />
G,R<br />
2i Semi deciduous notophyll vine thicket + Berrya javanica +<br />
Cupaniopsis anacardioides + Bombax ceiba var. leiocarpum +<br />
B<br />
Diospyros hebecarpa + Mimusops elengi + Melicope<br />
2j<br />
peninsularis.<br />
Semi-deciduous notophyll vine forest + Bombax ceiba var. B<br />
leiocarpum + Diospyros hebecarpa +/- Alectryon<br />
2k<br />
rep<strong>and</strong>odentatus + Cupaniopsis anacardiodes + Alstonia<br />
spectabilis +/- Melicope peninsularis.<br />
Deciduous vine forest + Gyrocarpus americanus + Bombax ceiba<br />
var. leiocarpum + Antiaris toxicaria var. macrophylla +<br />
Canarium australianum + Cathormion umbellatum subsp.<br />
B, GD, R<br />
monoliforme + Garuga floribunda var. floribunda +/-<br />
2l<br />
Adenanthera pavonina +/- Maranthes corymbosa.<br />
Semi-deciduous notophyll vine forest + Bombax ceiba var.<br />
leiocarpum + Gyrocarpus americanus + Garuga floribunda var.<br />
floribunda + Manilkara kauki + Diospyros maritima + Celtis<br />
philippensis.<br />
D<br />
2m Semi-deciduous notophyll vine forest + Milletia pinnata +<br />
Terminalia spp. + Diospyros maritima + Manilkara kauki +<br />
Aglaia elaeagnoidea + Pouteria obovata + Drypetes deplanchei<br />
+/- Erythrina spp.<br />
D<br />
2n Semi deciduous notophyll vine thicket + Canarium australianum<br />
+ Antiaris toxicaria var. macrophylla + Acacia auriculiformis +<br />
Terminalia subacroptera + Manilkara kauki + Bombax ceiba var.<br />
leiocarpum.<br />
G<br />
2o Semi deciduous notophyll vine forest + Acacia auriculiformis +<br />
Barringtonia calyptrata + Maranthes corymbosa + Syzygium<br />
forte subsp. forte + Bombax ceiba var. leiocarpum + Canarium<br />
australianum.<br />
MG<br />
2p Semi deciduous vine thicket (windsheared) + Bombax ceiba var.<br />
leiocarpum + Premna serratifolia + Acacia crassicarpa +<br />
D<br />
Manilkara kauki + Drypetes deplanchei + Terminalia<br />
2q<br />
subacroptera +/- Arenga australasica.<br />
Tall semi deciduous vine forest + Bombax ceiba var. leiocarpum<br />
+ Berrya javanica + Antiaris toxicaria var. macrophylla +<br />
Garuga floribunda var. floribunda + Canarium australianum +/-<br />
Albizia lebbeck +/- Syzygium bamagense +/- Maranthes<br />
corymbosa.<br />
Gd<br />
2r Semi deciduous vine forest + Sterculia quadrifida + Canarium Gd, G<br />
australianum + Cleistanthus peninsularis + Terminalia<br />
2s<br />
subacroptera + Antiaris toxicaria var. macrophylla +/-<br />
Paraserianthes toona + Alstonia actinophylla +/- Xanthoxylum<br />
rhetsa +/- Maniltoa lenticellata var. lenticellata.<br />
Semi-deciduous notophyll vine thicket (windsheared) + Pouteria G<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
26
<strong>Vegetation</strong><br />
Community<br />
Description<br />
sericea + Ficus virens var. sublanceolata + Schefflera<br />
actinophylla + Garcinia warrenii + Syzygium puberulum.<br />
Geologies<br />
2t Semi-deciduous notophyll vine forest <strong>and</strong> occasional thicket with<br />
Bombax ceiba var. leiocarpum + Canarium australianum +<br />
Terminalia spp. + Acacia polystachya.<br />
G, Gd, R<br />
2u Semi-deciduous vine forest + Manilkara kauki + Terminalia spp.<br />
+ Sterculia quadrifida + Premna serratifolia + Acacia<br />
crassicarpa + Drypetes deplanchei + Millettia pinnata.<br />
D<br />
2v Semi-deciduous vine thicket + Acacia polystachya <strong>and</strong> R<br />
2w<br />
Terminalia subacroptera.<br />
Deciduous vine thicket + Garuga floribunda var. floribunda+<br />
Gyrocarpus americanus + Bombax ceiba var. leiocarpum +/-<br />
Antiaris toxicaria var. macrophylla.<br />
B<br />
2x Deciduous vine thicket + Cochlospermum gillivraei + Bombax<br />
ceiba var. leiocarpum + Terminalia subacroptera +Sterculia<br />
quadrifida + Psydrax reticulata + Drypetes deplanchei.<br />
R<br />
2y Semi-deciduous vine thicket + Manilkara kauki + Terminalia<br />
subacroptera + Cordia subcordata + Premna serratifolia +<br />
Indeterminate species.<br />
D<br />
2z Low groved notophyll vine thicket + Sterculia quadrifida +<br />
Manilkara kauki + Eugenia reinwardtiana + P<strong>and</strong>anus sp.<br />
D<br />
2xx Semi-deciduous vine forest + Terminalia catappa + Acacia<br />
auriculiformis + Myristica insipida<br />
Swamp <strong>and</strong> riparian forest <strong>and</strong> forest complexes<br />
A<br />
3a Lophostemon suaveolens + Melaleuca quinquenervia + Syzygium<br />
angophoroides + Asteromyrtus brassii + Dillenia alata swamp<br />
forest complex<br />
A, As, D<br />
3b Medium to tall Melaleuca leucadendra +/- Melaleuca argentea +<br />
Syzygium forte subsp. forte + Dillenia alata open forest.<br />
A<br />
3c Tall Melaleuca dealbata / Melaleuca leucadendra open<br />
forest/Acacia sp. open forest / Mesophyll vine forest complex.<br />
A<br />
3d Evergreen mesophyll vine forest / Sclerophyll vine forest<br />
complex + Syzygium forte subsp. forte + Syzygium bamagense +<br />
A<br />
Horsfieldia Australiana +/- Melaleuca leucadendra +/-<br />
3e<br />
Lophostemon suaveolens. (1i/3b- 50/50)<br />
Melaleuca quinquenervia + P<strong>and</strong>anus sp. +/- Deplanchea D<br />
tetraphylla swamp forest/ Lophostemon suaveolens +/-<br />
3f<br />
Asteromyrtus brassii +/- Acacia crassicarpa +/- Deplanchea<br />
tetraphylla open swamp forest complex (7d/8b -50/50).<br />
Lophostemon suaveolens + Melaleuca leucadendra + Corymbia<br />
clarksoniana open forest.<br />
A<br />
3g Tall Melaleuca dealbata + Acacia crassicarpa + Acmena<br />
hemilampra + Deplanchea tetraphylla + Syzygium forte subsp.<br />
forte swamp forest complex.<br />
Welchiodendron dominant closed to open forests <strong>and</strong> woodl<strong>and</strong>s<br />
A<br />
4a Welchiodendron longivalve + Acacia polystachya +/- Terminalia<br />
subacroptera +/- Canarium australianum +/- Bombax ceiba var.<br />
leiocarpum open to closed forest.<br />
A, G, MG, Gd, R<br />
4b Welchiodendron longivalve low woodl<strong>and</strong>, low open woodl<strong>and</strong><br />
<strong>and</strong> tall open shrubl<strong>and</strong><br />
G, R<br />
4c Low Welchiodendron longivalve + Melaleuca dealbata open<br />
forest.<br />
Eucalypt dominant open forests <strong>and</strong> woodl<strong>and</strong>s<br />
G, A<br />
5a Corymbia novoguinensis +/- Corymbia stockeri subsp. As<br />
peninsularis woodl<strong>and</strong> <strong>and</strong> open forest.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
27
<strong>Vegetation</strong><br />
Community<br />
Description Geologies<br />
5b Corymbia clarksoniana + Corymbia nesophila +/- Corymbia<br />
tessellaris +/- Corymbia stockeri subsp. peninsularis +/-<br />
Welchiodendron longivalve woodl<strong>and</strong> <strong>and</strong> open forest.<br />
A, G, Mg<br />
5c Corymbia clarksoniana + Melaleuca stenostachya + Melaleuca<br />
viridiflora +/- Asteromyrtus symphyocarpa +/- Parinari nonda<br />
+/- Asteromyrtus brassii woodl<strong>and</strong>.<br />
A<br />
5d Low Corymbia clarksoniana + Melaleuca viridiflora +<br />
Welchiodendron longivalve + Asteromyrtus brassii + Acacia<br />
leptocarpa woodl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong> complex.<br />
R<br />
5e Low to medium Corymbia clarksoniana +/- Welchiodendron<br />
longivalve +/- Eucalyptus leptophleba open forest <strong>and</strong> woodl<strong>and</strong>.<br />
R, G<br />
5f Eucalyptus leptophleba +/- Acacia polystachya woodl<strong>and</strong> <strong>and</strong><br />
open forest.<br />
G<br />
5g Corymbia tessellaris + Acacia polystachya +/- Welchiodendron<br />
longivalve woodl<strong>and</strong> <strong>and</strong> open forest.<br />
A, G<br />
5h Corymbia spp. + Melaleuca saligna + Acacia crassicarpa +/-<br />
Eucalyptus platyphylla +/- Eucalyptus brassiana open forest.<br />
A<br />
5i Corymbia clarksoniana +/- Corymbia novoguinensis +/-<br />
Livistona muelleri woodl<strong>and</strong> <strong>and</strong> open forest.<br />
A, D<br />
5j Eucalyptus tetrodonta + Corymbia nesophila +/- Corymbia<br />
clarksoniana +/- Corymbia novoguinensis +/- Corymbia stockeri<br />
subsp. peninsularis open forest.<br />
AS, D<br />
5k Corymbia nesophila +/- Corymbia stockeri subsp. peninsularis<br />
+/- Eucalyptus tetrodonta woodl<strong>and</strong> <strong>and</strong> open forest.<br />
A, AS, D<br />
5l Corymbia stockeri subsp. peninsularis +/- Corymbia nesophila<br />
+/- Eucalyptus tetrodonta +/- Eucalyptus cullenii woodl<strong>and</strong>.<br />
G, GD, R<br />
5m Low Corymbia spp. (C. stockeri, C. nesophila, C. clarksoniana)<br />
+ Melaleuca stenostachya +/- Melaleuca viridiflora +/-<br />
Asteromyrtus symphyocarpa woodl<strong>and</strong>.<br />
A, D<br />
5n Eucalyptus platyphylla + Erythrophloeum chlorostachys +/-<br />
Corymbia nesophila +/- Corymbia novoguinensis +/- Eucalyptus<br />
tetrodonta +/- Corymbia stockeri subsp. peninsularis woodl<strong>and</strong><br />
<strong>and</strong> open forest.<br />
A, D<br />
5o Corymbia tessellaris +/- Corymbia clarksoniana woodl<strong>and</strong> <strong>and</strong><br />
open woodl<strong>and</strong>.<br />
A, D, GD<br />
5p Low Corymbia polycarpa/Corymbia novoguinensis + Acacia<br />
crassicarpa + Terminalia subacroptera +/- Sterculia quadrifida<br />
+/- Syzygium suborbiculare woodl<strong>and</strong> <strong>and</strong> open woodl<strong>and</strong>.<br />
D<br />
5q Low Corymbia stockeri subsp. peninsularis open forest. A, AS,D<br />
5r Corymbia nesophila woodl<strong>and</strong> <strong>and</strong> open forest. R<br />
5s Corymbia clarksoniana +/- Corymbia tessellaris woodl<strong>and</strong>. A, GD<br />
5t Eucalyptus platyphylla +/- Corymbia stockeri subsp. peninsularis<br />
+/- Corymbia nesophila +/- Corymbia clarksoniana woodl<strong>and</strong>.<br />
5u Eucalyptus platyphylla +/- Corymbia tessellaris woodl<strong>and</strong> <strong>and</strong><br />
open woodl<strong>and</strong>.<br />
5v Corymbia stockeri subsp peninsularis + Welchiodendron<br />
longivalve + Acacia polystachya +/- Corymbia tessellaris<br />
woodl<strong>and</strong> / open forest complex.<br />
Acacia dominant open forests <strong>and</strong> woodl<strong>and</strong>s<br />
6a Low to medium Acacia auriculiformis +/- Terminalia<br />
subacroptera +/- Antiaris toxicaria var. macrophylla +/- Bombax<br />
ceiba var. leiocarpum open forest / woodl<strong>and</strong> & occasional<br />
shrubl<strong>and</strong>.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
R<br />
A, G, R<br />
G<br />
G, R<br />
28
<strong>Vegetation</strong><br />
Community<br />
Description Geologies<br />
6b Low to medium Acacia auriculiformis +/- Parinari nonda +/-<br />
P<strong>and</strong>anus sp. +/- Semecarpus australiensis open forest/woodl<strong>and</strong><br />
(<strong>and</strong> occasional shrubl<strong>and</strong>).<br />
A<br />
6c Low Acacia crassicarpa + Terminalia subacroptera + Sterculia<br />
quadrifida + Manilkara kauki + Syzygium suborbiculare open<br />
forest <strong>and</strong> woodl<strong>and</strong>.<br />
D<br />
6d Low Acacia crassicarpa + Melaleuca spp. open forest. D<br />
6e Low Acacia polystachya + Alstonia actinophylla + Buchanania<br />
arborescens + Manilkara kauki + Pouteria sericea + Sterculia<br />
quadrifida open to closed forest.<br />
GD<br />
6f Acacia sp. closed shrubl<strong>and</strong> R<br />
6g Acacia crassicarpa +Asteromyrtus brassii open forest <strong>and</strong> low<br />
open forest.<br />
Melaleuca dominant open forests<br />
D<br />
7a Low Melaleuca cajuputi subsp. platyphylla open forest. A<br />
7b/7bs Melaleuca saligna open forest. A, D<br />
7c Tall Melaleuca dealbata + Corymbia clarksoniana open forest. A<br />
7d Melaleuca quinquenervia +/- Melaleuca saligna +/- Melaleuca<br />
cajuputi subsp. platyphylla +/- Lophostemon suaveolens open<br />
forest.<br />
A, D<br />
7e Low Melaleuca dealbata +/- Melaleuca saligna +/- Lophostemon<br />
suaveolens open forest.<br />
A, D<br />
7f/7fs Melaleuca leucadendra open forest. A, D<br />
7g Melaleuca dealbata woodl<strong>and</strong> <strong>and</strong> open forest. D<br />
Lophostemon dominant woodl<strong>and</strong> <strong>and</strong> open forest<br />
8a Lophostemon suaveolens +/- Melaleuca cajuputi subsp.<br />
platyphylla +/- P<strong>and</strong>anus sp. +/- Livistona muelleri woodl<strong>and</strong><br />
<strong>and</strong> open forest.<br />
8b Low Lophostemon suaveolens +/- Asteromyrtus brassii +/-<br />
Acacia crassicarpa +/- Melaleuca saligna +/- Deplanchea<br />
tetraphylla open forest <strong>and</strong> swamp forest.<br />
8c Low Lophostemon suaveolens + Corymbia clarksoniana +<br />
Asteromyrtus symphyocarpa + Melaleuca saligna + Melaleuca<br />
viridiflora +/- Corymbia latifolia open woodl<strong>and</strong>.<br />
Asteromyrtus/Neofabricia dominant open forests<br />
9a Asteromyrtus brassii + Syzygium angophoroides + Acmena<br />
hemilampra subsp. hemilampra +/- Acacia crassicarpa +/-<br />
Melaleuca quinquenervia open forest.<br />
9b Neofabricia myrtifolia + Parinari nonda + Sterculia quadrifida<br />
+ Terminalia muelleri +Milletia pinnata closed to open forest.<br />
Casuarina dominant woodl<strong>and</strong> <strong>and</strong> open forest<br />
10a Casuarina equisetifolia open forest + Diospyros maritima +<br />
Premna serratifolia + Milletia pinnata.<br />
10b Casuarina equisetifolia woodl<strong>and</strong> <strong>and</strong> open forest +/- Terminalia<br />
catappa woodl<strong>and</strong> <strong>and</strong> open forest.<br />
P<strong>and</strong>anus dominant woodl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong><br />
11a P<strong>and</strong>anus sp. +/- Melaleuca cajuputi subsp. platyphylla +/-<br />
Acacia leptocarpa +/- Melaleuca acacioides shrubl<strong>and</strong> <strong>and</strong> low<br />
woodl<strong>and</strong>.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
A<br />
A, D<br />
D<br />
As<br />
D<br />
D<br />
D<br />
A<br />
29
<strong>Vegetation</strong><br />
Community<br />
Description Geologies<br />
11b P<strong>and</strong>anus sp. +/- Melaleuca viridiflora open forest, woodl<strong>and</strong><br />
<strong>and</strong> shrubl<strong>and</strong>.<br />
B, D, A, G<br />
Palm dominant forest <strong>and</strong> woodl<strong>and</strong>s<br />
12a Livistona meulleri woodl<strong>and</strong>. G<br />
12b Low Nypa fruticans closed forest. E<br />
Melaleuca dominant shrubl<strong>and</strong>s <strong>and</strong> woodl<strong>and</strong>s<br />
13a Melaleuca viridiflora +/- P<strong>and</strong>anus sp. shrubl<strong>and</strong> <strong>and</strong> low<br />
woodl<strong>and</strong>.<br />
A, D, R<br />
13b Melaleuca cajuputi subsp. platyphylla +/- P<strong>and</strong>anus sp.<br />
shrubl<strong>and</strong>.<br />
A<br />
13c Melaleuca viridiflora + Asteromyrtus symphyocarpa +/- As. A<br />
13d<br />
Asteromyrtus brassii + /- Banksia dentata +/- Melaleuca saligna<br />
+/- Leucopogon ruscifolius shrubl<strong>and</strong>.<br />
Melaleuca saligna + Melaleuca viridiflora + Asteromyrtus<br />
symphyocarpa +/- Asteromyrtus brassii +/- Corymbia spp. +/-<br />
Banksia dentata low woodl<strong>and</strong>.<br />
A, AS<br />
13e Melaleuca acacioides shrubl<strong>and</strong>. A<br />
13f Low Melaleuca viridiflora + Corymbia clarksoniana woodl<strong>and</strong>. A<br />
13g Low Melaleuca saligna shrubl<strong>and</strong>. A<br />
13h Low Melaleuca arcana closed shrubl<strong>and</strong>. D<br />
13i Melaleuca stenostachya shrubl<strong>and</strong> +/- Melaleuca viridiflora low<br />
woodl<strong>and</strong>.<br />
A, AS, Gd,R<br />
13j Melaleuca acacioides +/- Melaleuca viridiflora open shrubl<strong>and</strong>. A<br />
Shrubl<strong>and</strong>s <strong>and</strong> shrubl<strong>and</strong> complexes<br />
14a Dwarf Welchiodendron longivalve + Alyxia spicata +/-<br />
Melaleuca viridiflora +/- Acacia spp. +/- Asteromyrtus brassii<br />
shrubl<strong>and</strong>.<br />
R<br />
14b Melaleuca cajuputi subsp. platyphylla + Acacia auriculiformis<br />
+/- Terminalia subacroptera open scrub <strong>and</strong> low open forest.<br />
A<br />
14c Welchiodendron longivalve shrubl<strong>and</strong>. R, Gd<br />
14d Cochlospermum gillivraei +/- Canarium australianum +/-<br />
Welchiodendron longivalve deciduous shrubl<strong>and</strong>.<br />
G, R<br />
14e Low open shrubl<strong>and</strong> with Baeckea frutescens, Melaleuca<br />
viridiflora <strong>and</strong> Asteromyrtus brassii.<br />
D<br />
14f Melaleuca viridiflora + Melaleuca stenostachya + G, R<br />
Welchiodendron longivalve + Acacia leptocarpa +/-<br />
14g<br />
Cochlospermum gillivraei shrubl<strong>and</strong>.<br />
Low Alyxia spicata + Manilkara kauki +/- Buchanania<br />
arborescens +/- Canarium australianum +/- Diospyros spp. +/-<br />
P<strong>and</strong>anus sp. low closed shrubl<strong>and</strong>/ rock pavement complex.<br />
G, R<br />
14h Acacia polystachya +/- Welchiodendron longivalve closed<br />
shrubl<strong>and</strong>.<br />
G<br />
14i Asteromyrtus brassii + Melaleuca saligna + Baeckea frutescens AS<br />
+ Leucopogon yorkensis + Leucopogon ruscifolius +/-<br />
14j<br />
Lophostemon suaveolens shrubl<strong>and</strong> <strong>and</strong> low shrubl<strong>and</strong>.<br />
Acacia brassii +/- Welchiodendron longivalve closed shrubl<strong>and</strong>. R<br />
14k Low Melaleuca stenostachya + Asteromyrtus symphyocarpa +<br />
Jacksonia thesioides + Melaleuca viridiflora shrubl<strong>and</strong>.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
R<br />
30
<strong>Vegetation</strong><br />
Community<br />
Description Geologies<br />
14l Low Melaleuca sp. (Zuna DGF9257+) + Welchiodendron<br />
longivalve + Corymbia spp. + Acacia brassii + Melaleuca<br />
stenostachya + Jacksonia thesioides shrubl<strong>and</strong>.<br />
R<br />
14m Grevillea striata + Acacia crassicarpa + Melaleuca viridiflora +<br />
Parinari nonda + P<strong>and</strong>anus sp. + Corymbia tessellaris<br />
shrubl<strong>and</strong>.<br />
A<br />
14n Acacia crassicarpa + Leucopogon ruscifolius +/- Neofabricia<br />
myrtifolia +/- Pouteria sericea +/- Psydrax banksii +/- Halfordia<br />
kendack shrubl<strong>and</strong> <strong>and</strong> open shrubl<strong>and</strong>.<br />
D<br />
14o Melaleuca saligna dominant riparian shrubl<strong>and</strong> complex. A<br />
14p Asteromyrtus brassii + Petalostigma pubescens + Melaleuca<br />
viridiflora + Asteromyrtus brassii + Acacia crassicarpa +<br />
Corymbia clarksoniana shrubl<strong>and</strong>.<br />
R<br />
14q Low Cycas sp. open shrubl<strong>and</strong>. D<br />
14r Acacia crassicarpa + P<strong>and</strong>anus sp. + Melaleuca viridiflora +/-<br />
Parinari nonda +/- Banksia dentata +/- Lophostemon suaveolens<br />
shrubl<strong>and</strong>.<br />
14s Low sparse Leucopogon ruscifolius + Acacia crassicarpa +<br />
Syzygium suborbiculare shrubl<strong>and</strong> with Corymbia novoguinensis<br />
emergents.<br />
14t Low sparse Cochlospermum gillivraei + Canarium australianum<br />
+ Eugenia reinwardtiana + Terminalia sp. + P<strong>and</strong>anus sp.<br />
shrubl<strong>and</strong>.<br />
14u Low Corymbia stockeri subsp. peninsualris + Welchiodendron<br />
longivalve open forest / Welchiodendron longivalve closed scrub/<br />
Deciduous shrubl<strong>and</strong>/rock pavement complex (5v/4a/18a/18d –<br />
30/40/20/10).<br />
14u Low Corymbia stockeri subsp. peninsularis + Welchiodendron<br />
longivalve open forest / Welchiodendron longivalve closed scrub /<br />
Deciduous shrubl<strong>and</strong> / rock pavement complex (5v/14c/18a/18d –<br />
30/40/20/10).<br />
14v Eucalyptus leptophleba + Grevillea parallela + Exocarpos<br />
latifolius + Terminalia sp. + Acacia crassicarpa shrubl<strong>and</strong>.<br />
14w Eucalyptus cullenii + Corymbia stockeri subsp. peninsularis<br />
woodl<strong>and</strong> +/- Eucalyptus tetrodonta + Welchiodendron<br />
14x<br />
longivalve + Melaleuca stenostachya shrubl<strong>and</strong> / Low Acacia<br />
brassii shrubl<strong>and</strong> / Deciduous shrubl<strong>and</strong> complex (5l/14x/14j/18a<br />
– 20/40/30/10).<br />
Eucalyptus tetrodonta + Welchiodendron longivalve + Melaleuca<br />
stenostachya open to sparse shrubl<strong>and</strong>.<br />
14y Low Premna serratifolia + Cordia subcordata +/- Pemphis<br />
acidula +/- Drypetes deplanchei shrubl<strong>and</strong>.<br />
Coastal headl<strong>and</strong> forest complexes<br />
15a Semi deciduous vine thicket / P<strong>and</strong>anus sp. open forest complex<br />
(2w/11a – 60-40).<br />
Coastal dune complexes<br />
16a Coastal foredune grassl<strong>and</strong>, herbl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong> complex.<br />
(17j/14y – 70/30)<br />
16b Coastal foredune grassl<strong>and</strong> / Casuarina equisetifolia +/-<br />
P<strong>and</strong>anus sp. +/- Acacia crassicarpa shrubl<strong>and</strong> complex (17j/<br />
10b/6c – 30/20/50).<br />
16c Coastal dune swale shrubl<strong>and</strong> / Low open forest complex +<br />
Cochlospermum gillivraei + Canarium australianum +<br />
Terminalia subacroptera + Acacia crassicarpa + Melaleuca<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
A<br />
D<br />
D<br />
G<br />
G<br />
D<br />
R<br />
R<br />
D<br />
B<br />
D<br />
D<br />
D<br />
31
<strong>Vegetation</strong><br />
Community<br />
saligna + Melaleuca acacioides (14t/7b – 70/30).<br />
Description Geologies<br />
16d Coastal dune shrubl<strong>and</strong> <strong>and</strong> vine forest complex (14t/2aa –<br />
70/30).<br />
D<br />
16e Corymbia tessellaris woodl<strong>and</strong> <strong>and</strong> open forest / shrubl<strong>and</strong> / vine<br />
thicket complex (5o/14t/2aa – 40/40/20).<br />
D<br />
16f Casuarina equisetifolia woodl<strong>and</strong> <strong>and</strong> open forest/vine thicket<br />
complex (10b/2aa – 60/40).<br />
D<br />
16g Low Acacia crassicarpa/Melaleuca dealbata open forest dune<br />
swale complex (6c/7g - 80/20).<br />
D<br />
16h Low groved notophyll vine thicket + Terminalia muelleri +<br />
Diospyros maritima + Premna serratifolia + Thespesia<br />
populneoides + Manilkara kauki (2y/17j – 80/20).<br />
D<br />
16i Low open shrubl<strong>and</strong> with Terminalia sp., Premna serratifolia,<br />
Diospyros maritima.<br />
D<br />
16j Low groved notophyll vine thicket/ grassl<strong>and</strong> <strong>and</strong> herbl<strong>and</strong><br />
complex (2z/17j - 80/20).<br />
D<br />
16k Coastal foredune grassl<strong>and</strong>, herbl<strong>and</strong>, woodl<strong>and</strong> <strong>and</strong> vine thicket<br />
complex (17j/17d/10b/2aa – 50/20/20/10).<br />
Grassl<strong>and</strong>s <strong>and</strong> grassl<strong>and</strong> complexes<br />
D<br />
17a Tall Ischaemum australe +/- Imperata cylindrica +/- Themeda<br />
tri<strong>and</strong>ra +/- Mnesithea rottboellioides +/- Heteropogon triticeus<br />
grassl<strong>and</strong>.<br />
A<br />
17b Themeda tri<strong>and</strong>ra +/- Imperata cylindrica +/- Mnesithea<br />
rottboellioides grassl<strong>and</strong>.<br />
B, V<br />
17c Open to closed tussock grassl<strong>and</strong> with emergent shrubs. GD, R<br />
17d Medium to tall Mnesithea rottboellioides + Heteropogon triticeus<br />
+ Cymbopogon spp. +/- Imperata cylindrica +/- Themeda<br />
tri<strong>and</strong>ra grassl<strong>and</strong>.<br />
A. AS. D, G, L<br />
17e Relic cultivated alluvial plains with anastomosing channel<br />
morphology.<br />
A<br />
17f Imperata cylindrica dominant grassl<strong>and</strong>. D<br />
17g Imperata/Themeda grassl<strong>and</strong> complex with emergent shrubs. A<br />
17h Imperata cylindrica + Themeda tri<strong>and</strong>ra grassl<strong>and</strong> / G<br />
17i<br />
Welchiodendron longivalve open forest <strong>and</strong> woodl<strong>and</strong> complex<br />
(17f/4a – 90/10).<br />
Low sedgel<strong>and</strong> with emergent shrubs <strong>and</strong> trees. AS, D<br />
17j Low Spinifex sericeus + Vigna marina + Ipomoea pes-caprae<br />
subsp. brasiliensis + Sesuvium portulacastrum grassl<strong>and</strong> <strong>and</strong><br />
forbl<strong>and</strong> complex.<br />
Rock pavement <strong>and</strong> pavement complexes<br />
D<br />
18a Deciduous shrubl<strong>and</strong> / Rock pavement complex. R<br />
18b Low Acacia brassii +/- Welchiodendron longivalve +/-<br />
Cochlospermum gillivraei shrubl<strong>and</strong>/ rock pavement complex<br />
(18a/14j -50/50).<br />
18c Welchiodendron longivalve +/- Acacia polystachya closed<br />
shrubl<strong>and</strong> / Low deciduous shrubl<strong>and</strong>/rock pavement complex<br />
(18a/14c – 50/50).<br />
18d Corymbia stockeri subsp. peninsularis + Welchiodendron<br />
longivalve + Psydrax banksii + Dodonoea sp. + Ficus sp. rock<br />
pavement complex.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
Gd, R<br />
G, R<br />
G<br />
32
<strong>Vegetation</strong><br />
Community<br />
Description Geologies<br />
Boulder slope vinel<strong>and</strong>/shrubl<strong>and</strong> complexes<br />
19a Open vinel<strong>and</strong>/deciduous shrubl<strong>and</strong>/boulder slope complex. G, Gd<br />
Wetl<strong>and</strong> complexes <strong>and</strong> mosaics<br />
20a Eleocharis dulcis closed sedgel<strong>and</strong>. A<br />
20b Open wetl<strong>and</strong> complex. D<br />
Successional vine forest communities<br />
21a Low vine forest <strong>and</strong> vine thicket with Barringtonia calyptrata +<br />
Macaranga involucrata var. mallotoides + Hibiscus tiliaceus +<br />
Semecarpus australiensis successional vine forest <strong>and</strong> thicket.<br />
Anthropogenically altered (secondary) vine forest <strong>and</strong> thicket<br />
22a Tall palm (Cocos nucifera) woodl<strong>and</strong> <strong>and</strong> open forest with<br />
mesophyll/notophyll vine forest sub-canopy of Myristica insipida<br />
<strong>and</strong> Lepidopetalum fructoglabrum.<br />
22b Semi deciduous vine thicket (secondary) + Buchanania<br />
arborescens + Manilkara kauki + Scolopia braunii + Drypetes<br />
deplanchei + Terminalia muelleri.<br />
Saline transitional communities<br />
23a Low Excoecaria agallocha + Hibiscus tiliaceus + Thespesia<br />
populneoides + Melaleuca cajuputi subsp. platyphylla open<br />
forest.<br />
23b Pemphis acidula +/- Terminalia subacroptera +/- Premna<br />
serratifolia closed shrubl<strong>and</strong>.<br />
23c Semi deciduous transitional vine forest + Xylocarpus granatum +<br />
Manilkara kauki.<br />
Mangrove forest, woodl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong> complexes<br />
D<br />
24a Mangrove closed <strong>and</strong> open forest, woodl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong><br />
complexes (24d/24c – 80/20).<br />
E<br />
24b Pemphis acidula + Osbornia octodonta closed shrubl<strong>and</strong>. E<br />
24c Avicennia marina subsp. eucalyptifolia open to closed forest. E<br />
24d Open to closed forest of Bruguiera gymnorhiza +/- Rhizophora<br />
stylosa.<br />
Samphire herbl<strong>and</strong>s <strong>and</strong> shrubl<strong>and</strong>s <strong>and</strong> salt pans<br />
E<br />
25a Dwarf halophytic shrubl<strong>and</strong> <strong>and</strong> saltpan. E<br />
25b Salt pan. E<br />
26a<br />
Samphire grassl<strong>and</strong>s<br />
Closed Sporobolus sp. grassl<strong>and</strong>. E<br />
26b Sporobolus sp. Grassl<strong>and</strong> / Chenopod forbl<strong>and</strong> <strong>and</strong> herbl<strong>and</strong><br />
complex (26a/25a - 50/50).<br />
Estuarine wetl<strong>and</strong> complexes <strong>and</strong> mosaics<br />
E<br />
27a Schoenoplectus sp. sedgel<strong>and</strong>. E<br />
27b Tall Schoenoplectus sp. Sedgel<strong>and</strong> / Estuarine wetl<strong>and</strong> complex. E<br />
*indicates pre-clearing community only<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
V<br />
B<br />
D<br />
E<br />
D<br />
33
Additional Descriptors: An appended indicator of condition may be applied. As an example a<br />
community code of 1ax, where ‘x’ is the appended condition indicator, represents a highly<br />
disturbed VC which has retained sufficient structural integrity to be classified as ‘remnant’<br />
according to the VMA (1999). The use of an appended ‘r’, or appended ‘d’ against VC7ba<br />
vegetation attribute is used to distinguish riparian occurrences <strong>and</strong> drainage depression<br />
occurrences respectively, which proved necessary for RE differentiation in this community.<br />
Pre-clearing Descriptors (including non-remnant vegetation types): Where vegetation has<br />
been cleared or disturbed to a degree that it can no longer be classified as remnant, the preclearing<br />
vegetation code is provided as the primary attribute, followed by an appended indicator<br />
of current status or condition. As an example, the code B2j(c) indicates a presently cleared area<br />
with a pre-clearing vegetation type of B2j. A list of current status indicators is provided in Table<br />
9.<br />
Table 9. Descriptors used to indicate pre-clearing vegetation <strong>and</strong> current vegetation status.<br />
Current Status<br />
Indicator<br />
Variation<br />
(Appended)<br />
(c) Native vegetation has been cleared <strong>and</strong> remains cleared. Generally, these areas<br />
are under housing or infrastructure development, or agricultural use.<br />
(b) Native vegetation has been cleared or disturbed <strong>and</strong> is currently occupied by<br />
Bamboo thicket.<br />
(e) Native vegetation has been cleared or disturbed <strong>and</strong> is currently occupied by<br />
exotic species (other than Bamboo).<br />
(r) Native vegetation has been previously cleared <strong>and</strong> is currently occupied by native<br />
regrowth (secondary vegetation) with non-remnant status.<br />
4.1.3 <strong>Regional</strong> <strong>Ecosystems</strong><br />
<strong>Vegetation</strong> communities have been classified into RE’s based on l<strong>and</strong>form association, structural<br />
type <strong>and</strong> floristic assemblage. Seventy six RE’s are identified in the study area detailed in Table<br />
10. This includes recognition of 10 new RE’s of which two are identified on the basis of preclearing<br />
extent. The spatial distribution of these RE’s is provided in accompanying maps 5a to<br />
5e. A spatial analysis on the extent of RE’s in the Torres Strait Isl<strong>and</strong> Sub-region presented in<br />
Section 6. Further description of RE’s including classification <strong>and</strong> derivation is provided in<br />
Section 5.2.<br />
Table 10. <strong>Regional</strong> <strong>Ecosystems</strong> in the Project Area.<br />
<strong>Regional</strong><br />
Ecosystem<br />
Component<br />
<strong>Vegetation</strong><br />
<strong>Communities</strong><br />
<strong>Regional</strong> Ecosystem Description 4 .<br />
<strong>Vegetation</strong><br />
Management Status<br />
L<strong>and</strong> Zone 1- Estuarine muds <strong>and</strong> alluvium subject to saltwater incursion<br />
3.1.1 24a (co) Closed forest of Rhizophora stylosa ± Not of Concern<br />
24b<br />
Bruguiera gymnorhiza. Occurs as outer<br />
24d<br />
12b<br />
mangroves.<br />
3.1.2 24c<br />
Avicennia marina ± Ceriops tagal low open Of Concern<br />
3.1.2b 23c<br />
24a (co)<br />
forest l<strong>and</strong>ward side of mangroves.<br />
3.1.4 23a Excoecaria agallocha ± Aegiceras<br />
corniculata closed scrub. Upper tidal reaches<br />
of rivers.<br />
Of Concern<br />
3.1.5 26a Sporobolus virginicus closed tussock Not of Concern<br />
4 Short description as per REDD Version 5.2, 2007<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
34
<strong>Regional</strong><br />
Ecosystem<br />
Component<br />
<strong>Vegetation</strong><br />
<strong>Communities</strong><br />
3.1.6 25a<br />
25b<br />
26b (co)<br />
3.1.7** 27a<br />
27b<br />
<strong>Regional</strong> Ecosystem Description 4 .<br />
26b (co) grassl<strong>and</strong>. Occurs on coastal plains.<br />
Sparse herbl<strong>and</strong> or bare saltpans. Associated<br />
with salt plains <strong>and</strong> saline flats.<br />
<strong>Vegetation</strong><br />
Management Status<br />
Not of Concern<br />
Schoenoplectus sp. estuarine wetl<strong>and</strong> mosaic. Not of Concern<br />
L<strong>and</strong> Zone 2 - Coastal Dunes, Cheniers <strong>and</strong> S<strong>and</strong> Sheets <strong>and</strong> associated Dune Swales.<br />
3.2.2a 1c<br />
Semi-deciduous vine thicket on coastal dunes Of Concern<br />
2p<br />
2y<br />
2z<br />
16d(co)<br />
16e(co)<br />
16f(co)<br />
16h(co)<br />
16j(co)<br />
16k(co)<br />
<strong>and</strong> beach ridges.<br />
3.2.2b** 2a<br />
Semi-deciduous notophyll vine forest <strong>and</strong> Of Concern<br />
2l<br />
thicket of prograding beach ridges of the<br />
2u<br />
9b<br />
Torres Strait Isl<strong>and</strong>s*.<br />
3.2.3 7g<br />
Melaleuca dealbata ± Acacia crassicarpa Of Concern<br />
7e<br />
open forest. Occurs in dune swales on the<br />
6d<br />
16g (co)<br />
west coast.<br />
3.2.4a 7f<br />
Melaleuca leucadendra ± M. dealbata open Of Concern<br />
3.2.4b 7d<br />
forest. In dune swales, <strong>and</strong> swampy areas.<br />
3.2.4c 8b<br />
3e (7d/8b)<br />
3.2.4d 7b<br />
16c (co)<br />
3.2.5a 6c<br />
Acacia crassicarpa ± Syzygium suborbiculare Not of Concern<br />
3.2.5b 5p<br />
± Parinari nonda woodl<strong>and</strong>. On beach<br />
3.2.5c 6g<br />
14t<br />
14v<br />
14q<br />
16c(co)<br />
16b(co)<br />
16d (co)<br />
16g (co)<br />
ridges.<br />
3.2.6a 10b<br />
Casuarina equisetifolia woodl<strong>and</strong>. Occurs on Of Concern<br />
16f(co)<br />
16b(co)<br />
16k(co)<br />
foredunes.<br />
3.2.6b 10b<br />
3.2.7 5i<br />
Corymbia intermedia or C. clarksoniana Not of Concern<br />
5o<br />
16e (co)<br />
woodl<strong>and</strong> in wet coastal areas.<br />
3.2.8 5k<br />
Corymbia nesophila ± C. novoguinensis ± Of Concern<br />
5n<br />
Eucalyptus spp. woodl<strong>and</strong> on old stabilised<br />
5m<br />
5q<br />
dunes.<br />
3.2.10c 5j Eucalyptus tetrodonta, Corymbia<br />
clarksoniana ± E. brassiana or<br />
Erythrophleum chlorostachys woodl<strong>and</strong> on<br />
Of Concern<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
35
<strong>Regional</strong><br />
Ecosystem<br />
Component<br />
<strong>Vegetation</strong><br />
<strong>Communities</strong><br />
<strong>Regional</strong> Ecosystem Description 4 .<br />
<strong>Vegetation</strong><br />
Management Status<br />
3.2.14 13h<br />
stabilised dunes.<br />
Melaleuca arcana low open forest.<br />
Associated with dune swamps.<br />
Of Concern<br />
3.2.15 13a<br />
Melaleuca viridiflora, Neofabricia myrtifolia Not of Concern<br />
8c<br />
17i<br />
woodl<strong>and</strong> on beach ridges.<br />
3.2.19a 14n<br />
Leucopogon yorkensis ± Asteromyrtus brassii Of Concern<br />
3.2.19b 14e<br />
open heath on old beach ridges.<br />
3.2.24 17j<br />
Closed herbl<strong>and</strong> of mixed graminoids <strong>and</strong> Of Concern<br />
17d<br />
17f<br />
16a(co)<br />
16b(co)<br />
16h(co)<br />
16k(co)<br />
forbs. Occurs on exposed foredunes.<br />
3.2.25 16i<br />
Sparse herbl<strong>and</strong> of mixed herbaceous species Of Concern<br />
14y<br />
16a(co)<br />
16j(co)<br />
on foredunes <strong>and</strong> beach ridges.<br />
3.2.26 14s Sparse herbl<strong>and</strong>/shrubl<strong>and</strong> <strong>and</strong> bare s<strong>and</strong><br />
areas. Predominantly on s<strong>and</strong> blows.<br />
Not of Concern<br />
3.2.27 20b Ephemeral <strong>and</strong> perennial lakes in coastal<br />
dunefields<br />
Of Concern<br />
3.2.28 2m Evergreen notophyll vine forest on beach<br />
ridges on coral atolls, shingle cays <strong>and</strong> s<strong>and</strong><br />
cays.<br />
Of Concern<br />
3.2.30 23b Pemphis acidula ± low closed forest.<br />
Restricted to coral atolls, shingle cays <strong>and</strong><br />
s<strong>and</strong> cays.<br />
Of Concern<br />
L<strong>and</strong> Zone3 - Alluvial plains, alluvial fans, terraces <strong>and</strong> fluvial sediments<br />
3.3.1c*** 2xx Closed semi-deciduous mesophyll vine forest.<br />
Mainly occurs on loamy alluvia (Pre-clearing<br />
classification only).<br />
Extinct (??)<br />
3.3.5c 1i<br />
Evergreen notophyll vine forest. Occurs on Not of Concern<br />
1j<br />
3d (co)<br />
alluvia on major watercourses.<br />
3.3.6 3c(co) Evergreen notophyll vine forest with Of Concern<br />
3d(co) Melaleuca leucadendra on swamps.<br />
3.3.7 2g<br />
Tall semi-deciduous notophyll/microphyll Not of Concern<br />
4a<br />
vine thicket (sic-forest). Occurs on colluvial<br />
6b<br />
plains.<br />
3.3.9 3a<br />
Lophostemon suaveolens open forest. Occurs Not of Concern<br />
3f<br />
8b<br />
on streamlines, swamps <strong>and</strong> alluvial terraces.<br />
3.3.10a 3b<br />
Melaleuca argentea <strong>and</strong> / or M. fluviatilis ± Not of Concern<br />
3.3.10b 14o/7br M. leucadendra open forest. Fringes streams<br />
3.3.10c 5h<br />
<strong>and</strong> creeks.<br />
3.3.10d 3g<br />
3.3.12 7d Melaleuca quinquenervia open forest.<br />
Associated with scattered coastal swamps.<br />
Of Concern<br />
3.3.13 7bs Melaleuca saligna ± Hakea pedunculata open<br />
forest. Occurs on edges of salt pans plains.<br />
Of Concern<br />
3.3.14 7b<br />
Melaleuca saligna ± M. viridiflora,<br />
Not of Concern<br />
7e<br />
Lophostemon suaveolens woodl<strong>and</strong> on<br />
13g<br />
drainage swamps.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
36
<strong>Regional</strong><br />
Ecosystem<br />
3.3.14b 7fs<br />
3.3.17b 5o<br />
5g<br />
Component<br />
<strong>Vegetation</strong><br />
<strong>Communities</strong><br />
5s<br />
<strong>Regional</strong> Ecosystem Description 4 .<br />
Corymbia clarksoniana, Erythrophleum<br />
chlorostachys woodl<strong>and</strong> on alluvial plains.<br />
3.3.20c 5b Corymbia clarksoniana ± Erythrophleum<br />
chlorostachys ± Melaleuca viridiflora<br />
woodl<strong>and</strong> on alluvial plains.<br />
3.3.22 5i<br />
Corymbia clarksoniana or C. novoguinensis<br />
3.3.27<br />
5c<br />
5k<br />
5q<br />
5m<br />
3.3.28 5u<br />
5n<br />
woodl<strong>and</strong> on alluvial plains.<br />
Corymbia nesophila ± Eucalyptus tetrodonta<br />
± Eucalyptus brassiana woodl<strong>and</strong> on alluvial<br />
sediments.<br />
Eucalyptus platyphylla ± Corymbia<br />
clarksoniana woodl<strong>and</strong> on alluvial <strong>and</strong><br />
<strong>Vegetation</strong><br />
Management Status<br />
Not of Concern<br />
Not of Concern<br />
Not of Concern<br />
Not of Concern<br />
Not of Concern<br />
3.3.42a 13a<br />
colluvial plains.<br />
Melaleuca viridiflora low woodl<strong>and</strong> in Not of Concern<br />
13c<br />
14m<br />
14r<br />
13f<br />
11b<br />
drainage areas.<br />
3.3.42c 13b<br />
3.3.48b 13d Melaleuca saligna ± M. viridiflora low open<br />
woodl<strong>and</strong> in drainage depressions.<br />
Not of Concern<br />
3.3.51 13e<br />
Melaleuca acacioides ± Hakea pedunculata Of Concern<br />
13j<br />
tall shrubl<strong>and</strong> on marine plains.<br />
3.3.57 17d<br />
Imperata cylindrica ± Mnesithea<br />
Of Concern<br />
17g<br />
rottboellioides closed tussock grassl<strong>and</strong> on<br />
coastal plains.<br />
3.3.62 17a<br />
Grassl<strong>and</strong>/sedgel<strong>and</strong> with P<strong>and</strong>anus spp. Of Concern<br />
17e<br />
11a<br />
Confined to Torres Strait Isl<strong>and</strong>s.<br />
3.3.63 20a Closed sedgel<strong>and</strong> dominated by Eleocharis<br />
dulcis. On seasonally flooded marine plains.<br />
Not of Concern<br />
3.3.65 20b Ephemeral lakes <strong>and</strong> lagoons on alluvial<br />
plains <strong>and</strong> depressions.<br />
Not of Concern<br />
3.3.68** 2c<br />
Semi-deciduous notophyll vine forest <strong>and</strong> Of Concern<br />
14b<br />
thicket on alluvial plains. Northern isl<strong>and</strong>s of<br />
the Torres Strait*.<br />
3.3.69** 7c<br />
Melaleuca dealbata +/- Corymbia<br />
Of Concern<br />
4d<br />
4c<br />
clarksoniana open forest on alluvial plains.<br />
3.3.70** 8a<br />
Lophostemon suaveolens +/- Melaleuca Of Concern<br />
7a<br />
cajuputi subsp. platyphylla +/- P<strong>and</strong>anus sp.<br />
+/- Livistona muelleri woodl<strong>and</strong> <strong>and</strong> open<br />
forest. Alluvial plains of northern Torres<br />
Strait Isl<strong>and</strong>s.<br />
L<strong>and</strong> Zone 5 – S<strong>and</strong>y plains <strong>and</strong> rises/ lateritic profiles <strong>and</strong> remnant alluvial/colluvial surfaces.<br />
3.5.5 5a Corymbia novoguinensis or C. nesophila ± C.<br />
tessellaris woodl<strong>and</strong> on northern Cape York<br />
Peninsula.<br />
Of Concern<br />
3.5.8c 5q Eucalyptus tetrodonta ± Corymbia hyl<strong>and</strong>ii<br />
subsp. peninsularis ± C. stockeri woodl<strong>and</strong><br />
on erosional plains <strong>and</strong> s<strong>and</strong>tone plateaus.<br />
Not of Concern<br />
3.5.15a 13a Melaleuca viridiflora ± Acacia spp. ± Not of Concern<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
37
<strong>Regional</strong><br />
Ecosystem<br />
3.5.15b<br />
Component<br />
<strong>Vegetation</strong><br />
<strong>Communities</strong><br />
13d<br />
13f<br />
13c<br />
17i<br />
<strong>Regional</strong> Ecosystem Description 4 .<br />
Asteromyrtus symphyocarpa low woodl<strong>and</strong><br />
on scattered coastal s<strong>and</strong> plains.<br />
<strong>Vegetation</strong><br />
Management Status<br />
3.5.17a 13i Melaleuca stenostachya +/- Melaleuca<br />
viridiflora low open woodl<strong>and</strong> on flat plains.<br />
Of Concern<br />
3.5.19a 14i Asteromyrtus lysicephala, Choriceras<br />
tricorne open heath on s<strong>and</strong> sheets.<br />
Not of Concern<br />
3.5.23x1 5j<br />
Eucalyptus tetrodonta ± Corymbia nesophila Of Concern<br />
5k<br />
± C. clarksoniana woodl<strong>and</strong> on undulating<br />
rises.<br />
3.5.29 17d Sorghum plumosum var. plumosum ±<br />
Themeda arguens closed tussock grassl<strong>and</strong> on<br />
erosional plains.<br />
Not of Concern<br />
3.5.32** 9a Asteromyrtus brassii + Syzygium<br />
angophoroides + Acmena hemilampra subsp.<br />
hemilampra open to closed forest on s<strong>and</strong>y<br />
rises*.<br />
L<strong>and</strong> Zone 7 – Exposed or shallowly covered duricrust<br />
Not of Concern<br />
3.7.1x1b 2e Semi-deciduous notophyll vine thicket on<br />
lateritic remnants. Northern Torres Strait<br />
Isl<strong>and</strong>s.<br />
Of Concern<br />
L<strong>and</strong> Zone 8 - Basalt escarpments <strong>and</strong> terraces/Volcanic cones formed on ash <strong>and</strong> scoria<br />
3.8.4b 17b Imperata cylindrica ± Mnesithea<br />
rottboellioides closed tussock grassl<strong>and</strong> on<br />
basalt vents & cones.<br />
Of Concern<br />
3.8.5a** 2i<br />
Semi-deciduous notophyll/microphyll vine Of Concern<br />
2j<br />
forest of the Torres Strait Isl<strong>and</strong> Sub-region*.<br />
3.8.5b** 2k<br />
3.8.5c** 2w<br />
3.8.5d** 21a<br />
3.8.5e** 15a<br />
L<strong>and</strong> Zone 12 – Acid volcanic <strong>and</strong> plutonic rocks including hornfelsed granite parent rocks<br />
3.12.4a 4a<br />
Notophyll vine forest of Welchiodendron Not of Concern<br />
4b<br />
14u (co)<br />
17h (co)<br />
longivalve on Torres Strait Isl<strong>and</strong>s.<br />
3.12.4b 1d<br />
3.12.8 5b<br />
Corymbia clarksoniana ± C. tessellaris open Not of Concern<br />
5s<br />
5e<br />
forest on coastal ranges <strong>and</strong> lowl<strong>and</strong>s.<br />
3.12.9 5g<br />
Corymbia tessellaris, C. clarksoniana open Not of Concern<br />
5o<br />
forest. Occurs on coastal ranges.<br />
3.12.11 5l<br />
Corymbia stockeri subsp. peninsularis ± Not of Concern<br />
5v<br />
Welchiodendron longivalve woodl<strong>and</strong> on<br />
14u (co)<br />
14w(co)<br />
Torres Strait Isl<strong>and</strong>s.<br />
3.12.13 5r Corymbia nesophila ± C. hyl<strong>and</strong>ii subsp.<br />
peninsularis woodl<strong>and</strong> on acid volcanic hills.<br />
Not of Concern<br />
3.12.16c 13i<br />
Melaleuca viridiflora, Asteromyrtus brassii Not of Concern<br />
14k<br />
woodl<strong>and</strong>. Associated with granitic hills.<br />
3.12.16d 14x<br />
14w(co)<br />
3.12.18 5f Eucalyptus leptophleba, Corymbia<br />
clarksoniana woodl<strong>and</strong> to open woodl<strong>and</strong> on<br />
Not of Concern<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
38
<strong>Regional</strong><br />
Ecosystem<br />
3.12.20<br />
3.12.21a<br />
3.12.23<br />
Component<br />
<strong>Vegetation</strong><br />
<strong>Communities</strong><br />
14c<br />
14d<br />
14h<br />
18c(co)<br />
2b<br />
2f<br />
2n<br />
2s<br />
2v<br />
2x<br />
14j<br />
14w(co)<br />
18b(co)<br />
6f<br />
3.12.29 17c<br />
12a<br />
3.12.30 17f<br />
17h(co)<br />
13.12.31x1a 14a<br />
14f<br />
14l<br />
3.12.33b<br />
3.12.34c<br />
3.12.35a**<br />
3.12.35b**<br />
3.12.35c**<br />
3.12.35d**<br />
3.12.35e**<br />
3.12.35f**<br />
3.12.36a**<br />
3.12.36b**<br />
14g<br />
19a<br />
11b<br />
18a<br />
18b (co)<br />
18c (co)<br />
18d<br />
14w (co)<br />
RR<br />
GG<br />
2t<br />
2h<br />
2d<br />
2o<br />
2q<br />
2r<br />
6a/6e<br />
1a<br />
1e<br />
1f<br />
1b<br />
1g<br />
1h<br />
3.12.37** 5t<br />
5u<br />
3.12.38** 5d<br />
14p<br />
13a<br />
<strong>Regional</strong> Ecosystem Description 4 .<br />
coastal hills.<br />
Evergreen notophyll vine forest dominated by<br />
Welchiodendron longivalve on headl<strong>and</strong>s.<br />
Deciduous vine thicket. Occurs on granite<br />
slopes mainly on the Great Dividing Range<br />
<strong>and</strong> offshore isl<strong>and</strong>s.<br />
Acacia brassii low open forest on acid<br />
volcanics on northern ranges <strong>and</strong> isl<strong>and</strong>s.<br />
Heteropogon triticeus ± Sarga plumosum<br />
closed tussock grassl<strong>and</strong> on continental<br />
isl<strong>and</strong>s.<br />
Imperata cylindrica ± Mnesithea<br />
rottboellioides closed tussock grassl<strong>and</strong> on<br />
steep slopes.<br />
Shrubl<strong>and</strong> on exposed coastal headl<strong>and</strong>s of<br />
the Torres Strait Isl<strong>and</strong>s.*<br />
Granite boulders covered with blue-green<br />
algae. Occurs on Black Mountain <strong>and</strong> Cape<br />
Melville.<br />
Rock pavements associated with hillslopes<br />
<strong>and</strong> footslopes of the Torres Strait Isl<strong>and</strong>s.*<br />
Semi-deciduous mesophyll/notophyll vine<br />
forest on granite slopes of the Torres Strait<br />
Sub-region.*<br />
Evergreen to complex evergreen mesophyll to<br />
notophyll vine forest <strong>and</strong> thicket on mountain<br />
ranges of Torres Strait Isl<strong>and</strong>s.<br />
Eucalyptus platyphylla +/- Corymbia<br />
stockerii +/- Corymbia clarksoniana<br />
woodl<strong>and</strong> to open woodl<strong>and</strong> on coastal hills.<br />
Melaleuca viridiflora ± Neofabricia<br />
myrtifolia low woodl<strong>and</strong> on granitic ranges.<br />
<strong>Vegetation</strong><br />
Management Status<br />
Of Concern<br />
Not of Concern<br />
Of Concern<br />
Of Concern<br />
Of Concern<br />
Of Concern<br />
Of Concern<br />
Of Concern<br />
Of Concern<br />
Of Concern<br />
Not of Concern<br />
Not of Concern<br />
*Preliminary description / **New regional ecosystem / *** Pre-clearing representation only / co = Component of<br />
<strong>Vegetation</strong> Complex where specific components of this VC are included in the RE.<br />
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5.0 Results Analysis <strong>and</strong> Discussion<br />
5.1 Clarifications on the Classification of L<strong>and</strong> Zones in the<br />
Study Area<br />
The following provides a brief analysis of the l<strong>and</strong> zone classifications used to derive RE’s in the<br />
area, including description of their component l<strong>and</strong>forms, rationale for classification, <strong>and</strong> their<br />
distribution.<br />
5.1.1 L<strong>and</strong> Zone 1<br />
As per the definition of Harris (nd.), this l<strong>and</strong> zone includes all alluvial deposits subject to<br />
periodic tidal inundation, including muds, s<strong>and</strong>s <strong>and</strong> rock bars inundated by brackish or marine<br />
waters. Whilst this is conceptually simple, L<strong>and</strong> Zone 1 does present some problem for<br />
interpretation due its relationship with L<strong>and</strong> Zone 3. There is often a continuum of l<strong>and</strong>form<br />
between these l<strong>and</strong> zones <strong>and</strong> differentiation is possible only through assessment of ground cover<br />
or shrub species. L<strong>and</strong> Zone 1 is recognisable through its association with sod grasses, sedges<br />
<strong>and</strong> chenopod forbs <strong>and</strong> in many cases, the upper tidal influence is marked by a low bench or rise,<br />
particularly on Boigu <strong>and</strong> Saibai Isl<strong>and</strong>s where low alluvial rises define the boundaries between<br />
tall tussock grassl<strong>and</strong>s <strong>and</strong> sod grassl<strong>and</strong>/salt flat vegetation. Saibai Isl<strong>and</strong> also demonstrates a<br />
continuum between freshwater <strong>and</strong> estuarine wetl<strong>and</strong> systems which proved problematic. The<br />
attenuated arms of tidal swamps that intrude into the isl<strong>and</strong>s central alluvial areas are dominated<br />
by mangroves forests on the seaward portions, merging seamlessly into mixed melaleuca <strong>and</strong><br />
mangrove communities fringing tall brackish sedge swamps, with inl<strong>and</strong> attenuations frequently<br />
represented by marginally brackish sedgel<strong>and</strong>s with scattered mangrove shrubs, vine thickets <strong>and</strong><br />
melaleuca dominant communities on the fringes. In these areas, the distinction between L<strong>and</strong><br />
Zone 1 <strong>and</strong> L<strong>and</strong> Zone 3 was subjective, based on field assessment of the degree of saltwater<br />
influence in particular portions of the wetl<strong>and</strong> system as observed in the late dry season. In all<br />
cases, attempts were made to apply a consistent approach to l<strong>and</strong> zone classifications, ensuring<br />
any future attempts to clarify these l<strong>and</strong> zone boundaries can be addressed on a regionally<br />
consistent basis. In summary, with reference to the definition provided by Harris (nd.), the<br />
classification of L<strong>and</strong> Zone 1 is best indicated by the nature of its constituent species. This l<strong>and</strong><br />
zone is recognised by a prominence of halophytic species including mangroves, salt tolerant<br />
grasses <strong>and</strong> sedges, <strong>and</strong> chenopod forbs.<br />
5.1.2 L<strong>and</strong> Zone 2<br />
This l<strong>and</strong> zone includes all l<strong>and</strong>forms composed of marine s<strong>and</strong>s <strong>and</strong> may include beach ridges,<br />
cheniers, degraded s<strong>and</strong> dunes, aeolian dune systems, <strong>and</strong> the calcareous s<strong>and</strong> deposits of coral<br />
cays. It also encompasses dune swales <strong>and</strong> associated freshwater wetl<strong>and</strong>s. The best developed<br />
occurrences are on the inner isl<strong>and</strong>s with extensive prograding dune systems found on the southwestern<br />
facing embayments of Muralug <strong>and</strong> Friday Isl<strong>and</strong>s. L<strong>and</strong> Zone 2 is developed on all of<br />
the larger isl<strong>and</strong>s to some degree, often manifest as a minor sliver of s<strong>and</strong> (beach ridge)<br />
immediately above the upper tidal limits. Extensive wind blown (aeolian) s<strong>and</strong> deposits well<br />
developed on Badu <strong>and</strong> Naghir (to a lesser degree) are also classified in this system. Marine<br />
s<strong>and</strong>s subject to tidal inundation, often occupied by mangrove species, are classified as L<strong>and</strong><br />
Zone 1.<br />
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40
5.1.3 L<strong>and</strong> Zone 3<br />
Difficulties with the distinction between L<strong>and</strong> Zone 1 <strong>and</strong> L<strong>and</strong> Zone 3 have been indicated<br />
previously in Section 5.1.1. L<strong>and</strong> Zone 3 in this study includes all transported alluvial material<br />
except those affected by tidal inundation; older sediment <strong>and</strong> colluvial profiles affected by deep<br />
weathering, laterisation <strong>and</strong> clay alteration, <strong>and</strong>; residual sediments. The major l<strong>and</strong>forms<br />
associated with L<strong>and</strong> Zone 3 include piedmont fans <strong>and</strong> outwash plains; fluvial sediments <strong>and</strong><br />
terraces associated with drainage channels, <strong>and</strong>; alluvial sediments associated with freshwater<br />
swamps. Problematic areas which concern the distinction between L<strong>and</strong> Zone 3 <strong>and</strong> L<strong>and</strong> Zone 5<br />
on Moa <strong>and</strong> Muralug Isl<strong>and</strong>s are described in Section 5.1.4.<br />
The most extensive occurrences of L<strong>and</strong> Zone 3 are associated with gently overlapping alluvial<br />
fans <strong>and</strong> outwash plains on Muralug <strong>and</strong> Moa Isl<strong>and</strong>s. This is not surprising considering that due<br />
to their considerable size, these isl<strong>and</strong>s have a well-developed drainage network which is lacking<br />
on many of the smaller isl<strong>and</strong>s in the study area. The composition of the alluvial plains depends<br />
largely on provenance, with alluvium derived from finer grained acid volcanic rocks generally<br />
being silty <strong>and</strong> poorly drained. Coarser granitoid rocks produce s<strong>and</strong>ier alluvial types which are<br />
relatively well-drained, often supporting luxuriant riparian vine-forest vegetation. On the southeastern<br />
side of Muralug Isl<strong>and</strong> where the dominant geology is diorite, relatively fertile clay rich<br />
alluvial plains have developed. The soil associated with these plains is mildly vertic (shrink <strong>and</strong><br />
swell) with a well-drained upper soil profile <strong>and</strong> gentle gilgai micro-topography. The geological<br />
code TQH characterises the majority of the fringing coastal plains on the larger isl<strong>and</strong>s, indicating<br />
an undifferentiated unit comprising Tertiary, Quaternary <strong>and</strong> Holocene age sediments. In the<br />
majority of cases (particularly on Horn <strong>and</strong> Muralug Isl<strong>and</strong>), coastal plains are formed by low<br />
angle, evenly graded alluvial fans which slope to tidal margins without any abrupt variation in<br />
topography. Local sea level provides a control on the base level of erosion, influencing the angle<br />
of the fringing alluvial fan, the rate of sedimentation, <strong>and</strong> the depth of fan incision. It is evident<br />
that the dominant control on the distribution of surficial sediments on these fans is sheetwash <strong>and</strong><br />
alluvial process rather than being residual sediment weathered insitu. On this account, the<br />
majority of the more extensive coastal plains are classified as LZ3 features rather than LZ5 as<br />
might be otherwise inferred. A relative sea level fall would reactivate alluvial process, initiating a<br />
new episode of fan incision <strong>and</strong> erosion, forming a transient sequence of relict alluvial surfaces.<br />
As discussed in Section 5.1.4, relict alluvial surfaces are present in some locations on the larger<br />
isl<strong>and</strong>s, possible testament to a recent sea level fall as inferred by Burne et al (1995). The<br />
possibility that the alluvial covering on these broad coastal plains is surficial, overlying deeply<br />
weathered sediments from previous depositional cycles, or bedrock weathered insitu should be<br />
considered. Until in-depth soil profiling <strong>and</strong> geomorphic studies are undertaken on these coastal<br />
plains, it is not possible to confirm their true nature <strong>and</strong> l<strong>and</strong> zone classification can only be based<br />
on visible geomorphic character.<br />
As previously mentioned in Section 1.1.3, remnants of the Fly Platform, manifest as s<strong>and</strong>y clay<br />
rises on Saibai <strong>and</strong> Boigu Isl<strong>and</strong>s are described as Quaternary age by Wilmott et al. (1972),<br />
although broad physiographic groupings of Paijmans et al. (1971) classify the isl<strong>and</strong>s as part of<br />
the Tertiary age Oriomo Plateau. Evidence produced from sediment coring undertaken by<br />
Barham (1999) support early Pleistocene age for these features, based both on observation of<br />
ferruginous pisoliths within the soil profile <strong>and</strong> experimental results. It is therefore not<br />
inappropriate to classify these broad clay plains as L<strong>and</strong> Zone 5 features, although this<br />
reclassification has not been implemented in this study, due largely to the poorly constrained<br />
definition of what constitutes a LZ5 feature. For the purpose of this study, the majority of the<br />
alluvial l<strong>and</strong>form on Saibai (<strong>and</strong> all of Boigu) has been classified as L<strong>and</strong> Zone 3, corresponding<br />
to the coastal plain of Bleaker (1983) on the adjacent PNG coast, which shares similarities in both<br />
l<strong>and</strong>form <strong>and</strong> vegetation, <strong>and</strong> is classified as a Holocene feature (Blake <strong>and</strong> Ollier, 1970). The<br />
lateritised sediments on the coastal margins of Saibai are classified as L<strong>and</strong> Zone 7 features <strong>and</strong><br />
are described in the following section.<br />
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5.1.4 L<strong>and</strong> Zone 5<br />
The classification of L<strong>and</strong> Zone 5 presents one of the most problematic aspects of l<strong>and</strong><br />
classification in the exercise, due largely to its relationship with more recent alluvial features <strong>and</strong><br />
its often subtle characteristics which are not always immediately obvious. The L<strong>and</strong> Zone is<br />
most extensive on Moa <strong>and</strong> Muralug Isl<strong>and</strong>s, <strong>and</strong> discussion on the provenance of these features<br />
is provided below. Minor areas have been classified on Wednesday <strong>and</strong> Friday Isl<strong>and</strong>s, <strong>and</strong> a<br />
number of lateritised colluvial terraces on the south western side of Dauan have also been<br />
recognised in this category, <strong>and</strong> are described briefly towards the end of the section.<br />
Photograph 4. Extensive alluvial<br />
plains (L<strong>and</strong> Zone 3) on Saibai<br />
Isl<strong>and</strong> supporting P<strong>and</strong>anus. The<br />
sinuous red-brown feature is a<br />
desiccated sedge swamp. Dauan<br />
Isl<strong>and</strong> is visible in the far right<br />
background of the photograph.<br />
Rationale for the classification of L<strong>and</strong> Zone 5 on Moa Isl<strong>and</strong>, considers the broad physiography<br />
<strong>and</strong> l<strong>and</strong>form development of the isl<strong>and</strong>, <strong>and</strong> is described based largely on field observation. The<br />
present day morphology has been heavily influenced by the intrusion of the Badu Granite (Cub)<br />
into the Torres Strait Volcanics (Ct) in the Late Carboniferous period. This intrusion altered the<br />
mineral structure of the earlier volcanic rocks through extreme heating (hornfelsing) which<br />
hardened them, <strong>and</strong> resulted in a rock type that is resistant to weathering. The Badu granite in<br />
contrast, being coarse grained <strong>and</strong> fresh, was relatively susceptible to both physical <strong>and</strong> chemical<br />
breakdown. This differing susceptibility to erosion created an erosion gradient, particularly along<br />
granite contacts <strong>and</strong> the Badu Granite was eroded at a much faster rate than the more resilient<br />
Torres Strait Volcanics. Preferential erosion of the granite resulted in the deposition of significant<br />
quantities of coarse granite s<strong>and</strong>, which are well-preserved as thick, gently undulating s<strong>and</strong> plains<br />
in the present Moa l<strong>and</strong>scape (incorporated in part into the l<strong>and</strong>form type AS). Active deposition<br />
on these s<strong>and</strong> plains has largely ceased <strong>and</strong> they have been classified as L<strong>and</strong> Zone 5 features in<br />
this exercise in recognition of their relict status. It is however clear that these s<strong>and</strong> plains are<br />
likely to be of Quaternary age, <strong>and</strong> are significantly younger than the erosional plain which<br />
occupies more central parts of the isl<strong>and</strong>. Preferential erosion of the younger granite pluton has<br />
resulted in the broadly semi-circular rim of hardened volcanic rock evident on the southern <strong>and</strong><br />
eastern margins of the isl<strong>and</strong>, which has channelled the bulk of the sedimentation towards the<br />
northwest into a broad topographic depression, where the best preserved <strong>and</strong> developed examples<br />
of these relicts s<strong>and</strong> plains are located.<br />
There is strong evidence in the present l<strong>and</strong>scape to suggest that the extremely rapid erosion <strong>and</strong><br />
deposition that resulted in formation of the s<strong>and</strong> plains slowed, or, that sediment deposition was<br />
re-directed. A considerable proportion of broad plain indicated as AS is clearly an erosional<br />
feature, with shallow residual s<strong>and</strong>s overlying granite basement which protrudes as numerous<br />
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42
corestones above the surface of what is an otherwise flat leached s<strong>and</strong>y plain. Residual terraces<br />
composed of coarse granite s<strong>and</strong>, being remnants of the former depositional l<strong>and</strong>form, are limited<br />
to marginal areas of the erosional plain <strong>and</strong> have clearly retreated in their extent. This l<strong>and</strong>scape<br />
almost certainly results from a much earlier period of weathering <strong>and</strong> is clearly a more typical<br />
L<strong>and</strong> Zone 5 feature.<br />
Photograph 5. Deeply weathered<br />
granite basement on erosional plain<br />
(L<strong>and</strong>form AS) on Moa Isl<strong>and</strong>.<br />
Changes in rates of sedimentation can be attributed to either shifts in climatic regime, or as a<br />
gradual cessation as l<strong>and</strong>forms lower through denudation over time, <strong>and</strong> both of these<br />
mechanisms may have been partly responsible for a change in regime from deposition to erosion.<br />
A change in base level may also have contributed to the shifting regime. Pleistocene (122ka) sea<br />
level is reported to have been 5 m higher than present in the Cape York Peninsula region (Burne<br />
et al. 1995) <strong>and</strong> a drop in sea levels may have contributed to a shift in the regime from coastal<br />
plain deposition to erosion. An area of extremely weathered s<strong>and</strong> dune on the broad erosional<br />
plain provides a clear indication of higher sea levels in the past. It should be noted that this<br />
contrasts dramatically with the findings of Rowe (2007), who postulates on the basis of the pollen<br />
record, that sediment deposition rates in the last 2 500 years have increased dramatically due to<br />
anthropogenic disturbance (l<strong>and</strong>scape burning) facilitating extensive freshwater swamp formation<br />
(expansion) on Moa Isl<strong>and</strong>. At least in the geomorphic sense, there is no evidence for this.<br />
Through whatever mechanism, this shift in sedimentary regime has resulted in a number of<br />
features on the north-west coastal plain which are considered unique to the isl<strong>and</strong>. Several low<br />
s<strong>and</strong>y rises on the north-western side of the isl<strong>and</strong> support open forest vegetation comprising<br />
Melaleuca quinquenervia, Syzygium angophoroides <strong>and</strong> Acmena hemilampra subsp. hemilampra.<br />
If l<strong>and</strong>scape position is ignored, these forests would normally be classified as swamp forests,<br />
typically occupying the lower permanently wet portions of the l<strong>and</strong>scape. That these<br />
communities occupy low s<strong>and</strong>y rises presents some problems for l<strong>and</strong>scape interpretation. The<br />
residual rises may represent relict s<strong>and</strong> dunes, although are too degraded for this to be<br />
demonstrated clearly. <strong>Vegetation</strong> on these rises is also significantly different from communities<br />
on weathered dunes in other locations, with sparse shrubl<strong>and</strong>s being more typical. With this<br />
considered, it is possible that the forest communities (mapped as VC9a) represent remnants of<br />
former swampl<strong>and</strong>s that have been subject to a topographic reversal <strong>and</strong> now occupy the raised<br />
portions of the erosional plain. In any case, from a l<strong>and</strong>scape sense, there is little alternative to<br />
classify these low rises as L<strong>and</strong> Zone 5 features.Furthermore, l<strong>and</strong>form systems similar to the one<br />
described on Moa are identified on Muralug behind Big Buttertin Beach. In this area, coarse<br />
s<strong>and</strong>y terraces are scattered across a coastal plain where thin recent alluvial deposits overly a<br />
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deeply leached kaolin profile. The classification of this coastal plain remains problematic,<br />
dependant largely on the depth of the recent alluvial cover. In the absence of any detailed soil<br />
auger sampling on these plains, visible surficial morphology provides the only sound basis for<br />
classification. As such, the classification places them within L<strong>and</strong> Zone 3. Future soil sampling<br />
efforts would be required to increase confidence in L<strong>and</strong> Zone classification in these areas, in<br />
particular, determination of the depth of recent alluvial cover. The s<strong>and</strong>y terraces rising above<br />
these gently sloping plains are often characterised by basal exposures of laterite <strong>and</strong> as such, are<br />
classified within L<strong>and</strong> Zone 5. It should however be considered likely that the s<strong>and</strong>y overburden<br />
is a superficial Quaternary deposit which, similar to Moa Isl<strong>and</strong>, has been stripped in adjacent<br />
areas.<br />
Photograph 6. Exposed laterite<br />
profile at the base of a remnant s<strong>and</strong><br />
plain on Muralug Isl<strong>and</strong>.<br />
On Wednesday <strong>and</strong> Friday Isl<strong>and</strong>s, L<strong>and</strong> Zone 5 is recognised in midslope positions, typically on<br />
eroded <strong>and</strong> deeply weathered terraces. Iron stained kaolin cements the detrital sediment on<br />
Wednesday Isl<strong>and</strong>, <strong>and</strong> erosion gullies have incised the l<strong>and</strong>form, generated through excessive<br />
surface run-off over a relatively impermeable substrate. The l<strong>and</strong>form on Wednesday Isl<strong>and</strong><br />
corresponds roughly to an area of deeply weathered s<strong>and</strong>stone reported in the vicinity by Wilmott<br />
(1977), however this s<strong>and</strong>stone outcrop was not observed during the traverse. Although in a<br />
similar topographic location on Friday Isl<strong>and</strong>, the facilitation of deep sediment weathering by the<br />
high permeability of the constituent coarse granitic sediment has favoured a period of relative<br />
l<strong>and</strong>form stability. This stability has allowed preservation of relict alluvial features, although<br />
these features may be considerably younger than Tertiary age.<br />
The classification of L<strong>and</strong> Zone 5 extends northward to Dauan Isl<strong>and</strong> where series of truncated<br />
colluvial terraces fringe the base of the piedmont slope on the isl<strong>and</strong>s western side, mapped as<br />
l<strong>and</strong>form type ‘T’. Examination of cuttings on these features exposed on drainage incisions<br />
demonstrates a strong lateritic horizon at approximately 60cm depth in the soil profile in some<br />
areas. These features have been classified with L<strong>and</strong> Zone 5 on account of their long term<br />
stability <strong>and</strong> weathering history.<br />
In summary, the classification of L<strong>and</strong> Zone 5 within the Torres Strait Isl<strong>and</strong>s applies to<br />
extensive erosional plains <strong>and</strong> remnant s<strong>and</strong> plains identified on Moa <strong>and</strong> Muralug Isl<strong>and</strong>s,<br />
weathered alluvial remnants associated with gully heads on Friday <strong>and</strong> Wednesday Isl<strong>and</strong>s, <strong>and</strong><br />
minor areas associated with lateritised colluvial terraces on Dauan. Extensive coastal plains on<br />
the north-west side of Horn Isl<strong>and</strong> <strong>and</strong> to a lesser extent Wednesday <strong>and</strong> Friday Isl<strong>and</strong>s lack some<br />
of the geomorphic <strong>and</strong> l<strong>and</strong>form features described for Moa <strong>and</strong> Muralug, which makes L<strong>and</strong><br />
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Zone classification more robust. Thin surficial layers of alluvial sediment <strong>and</strong> fine silica s<strong>and</strong> are<br />
present on some coastal plains on the inner isl<strong>and</strong>s although these are generally extremely<br />
shallow with the majority of the fringing coastal plain being influenced by alluvial process which<br />
is continuing in the present geomorphic regime.<br />
5.1.5 L<strong>and</strong> Zone 7<br />
A minor area of mapped as L<strong>and</strong> Zone 7 (geol. prefix T) underlies the settlement on Saibai<br />
Isl<strong>and</strong>, forming the most topographically elevated portion of the isl<strong>and</strong>. This l<strong>and</strong>form is<br />
currently undergoing significant l<strong>and</strong>ward erosion through undercutting <strong>and</strong> collapse of the iron<br />
cemented hard-pan layer, most actively during the summer periods where northerly trade winds<br />
prevail. The inclusion of this feature under the classification of L<strong>and</strong> Zone 7 is based on the<br />
lateritic exposure evident on the coastline, directed under advice from the Queensl<strong>and</strong> Herbarium,<br />
<strong>and</strong> has not been validated through formalised soil profiles or geomorphic analysis. Due to the<br />
long history of settlement, this l<strong>and</strong>form is largely devoid of remnant vegetation.<br />
5.1.6 L<strong>and</strong> Zone 8<br />
Photograph 7. Slabby exposure of<br />
lateritic duricrust on the coastal<br />
fringe of Saibai township.<br />
L<strong>and</strong> Zone 8 poses few problems for classification, being restricted to the eastern group of isl<strong>and</strong>s<br />
including Mer, Erub <strong>and</strong> Ugar. L<strong>and</strong>forms associated with L<strong>and</strong> Zone 8, which include<br />
Pleistocene flow basalts <strong>and</strong> associated volcanic ejecta, have been adequately characterised in the<br />
introductory sections of this report (Section 1.1.3) <strong>and</strong> require little expansion in this section.<br />
Basaltic terraces <strong>and</strong> pavements subject to tidal inundation, supporting mangrove communities in<br />
some locations have been classified as L<strong>and</strong> Zone 1.<br />
5.1.7 L<strong>and</strong> Zone 12<br />
L<strong>and</strong> zone 12 occupies a considerable proportion of the combined isl<strong>and</strong> mass, <strong>and</strong> as previously<br />
described in Section 1.1.3 (i.e. Isl<strong>and</strong>s Formed on Acidic Volcanic <strong>and</strong> Plutonic Basement),<br />
extends through all isl<strong>and</strong> groupings with the exception of the eastern group. This is a relatively<br />
simple group to define, including all igneous <strong>and</strong> volcanic rocks greater than Cainozoic in age,<br />
<strong>and</strong> as such extends to all basement outcrop in the Torres Strait Isl<strong>and</strong>s other than Pleistocene<br />
basalt. There is however significant chemical <strong>and</strong> structural variation within the grouping <strong>and</strong> in<br />
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45
an attempt to better describe the l<strong>and</strong>scape <strong>and</strong> provide a more comprehensive ecological<br />
analysis, a number of l<strong>and</strong> zone sub-groupings have been recognised.<br />
Sub-groupings, as listed in Table 7, are characterised in respect to a rock types specific<br />
ecological properties. Rhyolite (R), which is extensive on the inner group of isl<strong>and</strong>s (including<br />
Muralug), is generally the least fertile grouping, being fine grained, <strong>and</strong> resilient to weathering.<br />
Granites weather to form s<strong>and</strong>y soils which are relatively well-drained, <strong>and</strong> can be relatively<br />
fertile depending on the percentage of iron <strong>and</strong> magnesium rich mineral in the parent rock. The<br />
Badu Granite, which comprises a significant proportion of the Badu, Moa, Dauan <strong>and</strong> Iama l<strong>and</strong><br />
masses, is relatively rich in biotite <strong>and</strong> derived soils are of moderate fertility (as a generalisation).<br />
By definition, diorite is richer in iron <strong>and</strong> magnesium rich minerals than both granite <strong>and</strong> rhyolite,<br />
<strong>and</strong> derived soils are of moderate fertility. This feature is a useful indicator to assist<br />
differentiation of forest types, for example, some of the best-developed examples of vine forest<br />
on foothills occupy diorite knolls <strong>and</strong> talus slopes on the south eastern-side of Muralug Isl<strong>and</strong>.<br />
A final classification recognises altered acid plutonic rocks classified as MG, <strong>and</strong> is indicative of<br />
rocks that have been hardened through superheating during subsequent intrusive events. These<br />
rocks, generally termed hornfels, are extremely resistant to weathering <strong>and</strong> often manifest in the<br />
l<strong>and</strong>scape as rock piles <strong>and</strong> knolls comprised of boulder talus as on Moa Isl<strong>and</strong>. Although a<br />
metamorphic rock on a generic level, hornfels is grouped within L<strong>and</strong> Zone 12 in recognition of<br />
the limited chemical change parent material undergoes during the heating process.<br />
5.2 <strong>Regional</strong> Ecosystem Descriptions <strong>and</strong> Rationale for<br />
Classification<br />
This section provides descriptive notes on the occurrence <strong>and</strong> characteristics of RE’s in the study<br />
area. Features of each RE are discussed in relation to component vegetation communities with<br />
recognition of some marked structural <strong>and</strong> floristic variations which may occur within individual<br />
RE’s. It should also be noted that individual vegetation communities may be recorded in a range<br />
of regional ecosystems dependant on geological association.<br />
5.2.1 <strong>Regional</strong> Ecosystem 3.1.1<br />
Description: Closed forest of Rhizophora stylosa ± Bruguiera gymnorhiza. Occurs as outer<br />
mangroves.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 24a (co), 24b, 24d, 12b<br />
Reference Sites: 41 Quaternary<br />
This is a highly complex <strong>and</strong> variable RE occupying intertidal areas, generally on the seaward<br />
fringe of mangroves where tidal exchange is greatest, although may be attenuated well inl<strong>and</strong><br />
along estuarine drainage systems. All isl<strong>and</strong>s sampled with the exception of the Coral Cays have<br />
some development of this regional ecosystem on their shorelines, although the most extensive<br />
occurs on the northern isl<strong>and</strong>s of Saibai <strong>and</strong> Boigu, as well as mangrove isl<strong>and</strong>s of Zagai, Buru<br />
<strong>and</strong> Sassie. The major component is open to closed forest although a range of structural<br />
variations including closed shrubl<strong>and</strong>, mangrove woodl<strong>and</strong> <strong>and</strong> low open forest have been<br />
included in the classification. As such, VC24a the major component of this RE is described as a<br />
mangrove forest, woodl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong> complex. <strong>Vegetation</strong> Community 24d is a purer<br />
expression of RE3.1.1 mapped on the mangrove tidal isl<strong>and</strong>s of Sassie <strong>and</strong> Buru.<br />
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The mapping of VC24a as a complex reflects limitations in vegetation sampling which<br />
concentrated on terrestrial biodiversity values as required within the project scope. <strong>Vegetation</strong><br />
sampling was insufficient to describe all floristic <strong>and</strong> structural components of this complex with<br />
confidence. Wherever possible, VC24c is separated from the mangrove complex to allow<br />
differentiation of RE3.1.2, which is discussed in following sections. There is however<br />
considerable complexing of this RE which is evident in the spatial data, particularly on the<br />
northern isl<strong>and</strong>s. This RE also includes small areas of Nypa forest on North-West Creek mapped<br />
as VC12b, <strong>and</strong> limited occurrences of Pemphis acidula <strong>and</strong> Osbornia octodonta dominated low<br />
closed forest on intertidal areas of Iama Isl<strong>and</strong> <strong>and</strong> Sassie Isl<strong>and</strong> (VC24b).<br />
This RE represents the best development of mangrove habitat in the Torres Strait. It provides<br />
important habitat for estuarine crocodiles, <strong>and</strong> may provide habitat for the vulnerable listed<br />
butterfly Hypochrysops apollo, <strong>and</strong> two other jewel butterflies H. narcissus <strong>and</strong> H. apelles (EPA<br />
2007). The occurrence of Nypa forest on Muralug is significant <strong>and</strong> representing an extension of<br />
geographical range north from the Jardine River mouth <strong>and</strong> is the only known occurrence<br />
between Cape York <strong>and</strong> PNG. The ecosystem also provides an important cultural resource<br />
supporting traditional hunting <strong>and</strong> fishing practises <strong>and</strong> is fundamental to marine biodiversity <strong>and</strong><br />
fisheries.<br />
Photograph 8. Tall open forest with<br />
dominant Bruguiera sp. on Boigu<br />
Isl<strong>and</strong> (RE3.1.1). Canopy height of<br />
this community exceeded 35m.<br />
Photograph 9. A grove of Nypa<br />
Palm (Nypa fruticans) on North-<br />
West Creek, Muralug Isl<strong>and</strong><br />
represents the most northern<br />
occurrence of the palm in Australian<br />
territory.<br />
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5.2.2 <strong>Regional</strong> Ecosystem 3.1.2<br />
Description: Avicennia marina ± Ceriops tagal low open forest l<strong>and</strong>ward side of mangroves<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 24c, 23c, 24a<br />
Reference Sites: 14 Quaternary<br />
<strong>Vegetation</strong> Community 24c: This regional ecosystem is extensive on the l<strong>and</strong>ward fringe of<br />
mangrove forest complexes, typically on the forest boundary between halophytic forbl<strong>and</strong><br />
(RE3.1.6) <strong>and</strong> Sporobolus grassl<strong>and</strong>s (RE3.1.5). The major occurrences are on the northern<br />
isl<strong>and</strong>s of Saibai <strong>and</strong> Boigu where they are mapped as a component of mangrove complex type<br />
VC24a, although smaller areas are present on the majority of isl<strong>and</strong>s sampled <strong>and</strong> have been<br />
individually differentiated. The dominant canopy tree is Avicennia marina subsp. eucalyptifolia<br />
with the canopy varying markedly in both height <strong>and</strong> structure. The majority of communities<br />
sampled were woodl<strong>and</strong>s, although tall open forests with canopy heights exceeding 30m were<br />
common on Boigu Isl<strong>and</strong>. This RE has been mapped separately wherever convenient, although it<br />
has been included in a broader complex with RE3.1.1 in the majority of areas.<br />
Photograph 10. A specimen of<br />
Avicennia marina subsp.<br />
eucalyptifolia exceeding 35m. Tall<br />
open forest (RE3.1.2) on Boigu<br />
Isl<strong>and</strong>.<br />
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Photograph 11. Mangrove<br />
woodl<strong>and</strong> dominated by Avicennia<br />
marina subsp. eucalyptifolia on<br />
Boigu Isl<strong>and</strong> (RE3.1.2).<br />
<strong>Vegetation</strong> Community 23c: The interior of Sassie Isl<strong>and</strong> hosts a unique ecosystem, mapped<br />
here as VC23c. The community is recognised in the sub-grouping of RE3.2.1b due to its limited<br />
aerial extent <strong>and</strong> lack of a more appropriate RE classification. This community provides a<br />
significant floristic departure from other VC’s allocated to this group <strong>and</strong> its floristic association<br />
presents features transitional between a mangrove <strong>and</strong> vine forest community. The canopy,<br />
which attains heights of 25m or greater, is dominated by the deciduous mangrove species<br />
Xylocarpus granatum with Manilkara kauki a co-dominant species. Due to difficult access, the<br />
community was observed from helicopter only <strong>and</strong> its shrub <strong>and</strong> ground cover composition in<br />
unknown. Investigation of similar Xylocarpus dominated forests, which form a fringe to vine<br />
forests on the isl<strong>and</strong>s southern coast, suggest that it occupies raised ridges of coral rubble above<br />
the height of average maximum tidal inundation.<br />
Photograph 12. The deciduous<br />
crowns of Xylocarpus granatum<br />
clearly visible in contrast to the<br />
evergreen nature of surrounding<br />
mangrove communities. Interior<br />
areas of Sassie Isl<strong>and</strong>.<br />
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5.2.3 <strong>Regional</strong> Ecosystem 3.1.4<br />
Description: Excoecaria agallocha ± Aegiceras corniculata closed scrub. Upper tidal reaches<br />
of rivers.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 23a<br />
Reference Sites: 10 Quaternary<br />
This RE is extensive on Saibai Isl<strong>and</strong>, particularly on the brackish l<strong>and</strong>ward attenuations of tidal<br />
inlets where it forms a fringing community.<br />
<strong>Vegetation</strong> Community 23a: The dominant component VC23a is classified as a saline<br />
transitional community on account of its requirement for brackish conditions. Dominant canopy<br />
species are Excoecaria agallocha, Avicennia marina subsp. eucalyptoides, Bruguiera sp.,<br />
Hibiscus tiliaceus <strong>and</strong> Thespesia populneoides. The type merges with VC2c in some locations<br />
where scattered vine forest species including Terminalia subacroptera may occur in the canopy<br />
together with Acacia leptocarpa. Melaleuca cajuputi subsp. platyphylla may also be a prominent<br />
canopy species in some locations. Typical understorey species include Clerodendron inerme,<br />
Acanthus ilicifolius, <strong>and</strong> Cynanchum carnosum with Acrostichum aureum dominating the<br />
groundcover.<br />
5.2.4 <strong>Regional</strong> Ecosystem 3.1.5<br />
Photograph 13. VC23a fringing<br />
brackish sedge swamps on Saibai<br />
Isl<strong>and</strong>. Excoecaria agallocha,<br />
Hibiscus tiliaceus <strong>and</strong> Thespesia<br />
populneoides form the dominant<br />
canopy species in this narrow fringe.<br />
Description: Sporobolus virginicus closed tussock grassl<strong>and</strong>. Occurs on coastal plains.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 26a, 26b(co)<br />
Reference Sites: 16 Quaternary<br />
Sporobolus virginicus dominant grassl<strong>and</strong>s (VC26a) are extensive on the northern isl<strong>and</strong>s of<br />
Boigu <strong>and</strong> Saibai where they occupy the l<strong>and</strong>ward fringe on mangrove forest communities, often<br />
complexing with salt flats <strong>and</strong> halophytic forbl<strong>and</strong>s where they are mapped as VC26b.<br />
Associated species include Tecticornia australasica, Cynanchum carnosum, <strong>and</strong> Sesuvium<br />
portulacastrum. On margins Acrostichum aureum <strong>and</strong> Eleocharis dulcis may occur. Emergent<br />
shrubs to 1m may occur <strong>and</strong> include Avicennia marina, Bruguiera parviflora, Clerodendron<br />
inerme, Excoecaria agollocha, Thespesia populneoides <strong>and</strong> Wollastonia biflora. The community<br />
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also forms a component of VC26b, mapped as a complex of sporobulus grassl<strong>and</strong> <strong>and</strong> chenopod<br />
forbl<strong>and</strong>. On Boigu Isl<strong>and</strong>, Sporobolus grassl<strong>and</strong>s are seasonally burnt as traditional practice. It<br />
is postulated that burning prevents mangrove invasion, <strong>and</strong> by doing so, assists in the long-term<br />
maintenance of habitat diversity, also maintaining access for traditional prawning practices <strong>and</strong><br />
hunting of introduced deer.<br />
Photograph 14. Recently burnt<br />
(Oct. 2007) Sporobolus grassl<strong>and</strong><br />
with open forest of Avicennia marina<br />
subsp. eucalyptifolia in background.<br />
Boigu Isl<strong>and</strong>.<br />
5.2.5 <strong>Regional</strong> Ecosystem 3.1.6<br />
Description: Sparse herbl<strong>and</strong> or bare saltpans. Associated with salt plains <strong>and</strong> saline flats.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 25a, 25b, 26b (co)<br />
Reference Sites: 16 Quaternary<br />
RE3.1.6 is the dominant ecosystem in the northern isl<strong>and</strong> group with relatively extensive areas<br />
also occurring on the mid western isl<strong>and</strong>s of Moa <strong>and</strong> inner isl<strong>and</strong>s of Muralug <strong>and</strong> Horn. The<br />
RE manifests in response to hyper-saline conditions, a result of repetitive tidal wetting <strong>and</strong><br />
subsequent evaporation.<br />
<strong>Vegetation</strong> Community 25a & 25b: The dominant floristic components of VC25a & VC25b<br />
are halophytic forbs including Tecticornia australasica, Halosarcia sp., Sarcocornia<br />
quinqueflora subsp. quinqueflora <strong>and</strong> Suaeda australis. Where these species form a prominent<br />
ground cover, they are mapped as VC25a. Areas of this RE, mapped as VC25b, lack any<br />
significant ground cover due to persistent salt scalding. Evaporite crusts may form in the lower<br />
depressions of these areas during dryer periods. The RE provides estuarine wetl<strong>and</strong> habitat<br />
values. Small areas of VC25a form a componet of the estuarine complex VC26b.<br />
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5.2.6 <strong>Regional</strong> Ecosystem 3.1.7 (New RE)<br />
Photograph 15. An evaporite crust<br />
on a saltpan on Saibai Isl<strong>and</strong> where<br />
the formation is mapped as VC25b.<br />
Photograph 16. Saltpan vegetation<br />
on Horn Isl<strong>and</strong> with clumps of the<br />
halophytic forbs Tecticornia<br />
australasica <strong>and</strong> Halorsarcia sp. in<br />
the foreground. These areas are<br />
mapped as VC25a.<br />
Preliminary Description: Preliminary Description – Schoenoplectus spp. Sedgel<strong>and</strong>s<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 27a, 27b<br />
Reference Sites: 9 Quaternary<br />
This grouping is described as a new RE for the bioregion, restricted to isl<strong>and</strong> remnants of the Fly<br />
Platform. The community has two variants being a low open sedgel<strong>and</strong> of Schoenoplectus<br />
littoralis mapped as VC27a, <strong>and</strong> a taller sedgel<strong>and</strong> mosaic mapped as VC27b.<br />
<strong>Vegetation</strong> Community 27a: The variant 27a is prominent on both Saibai <strong>and</strong> Boigu Isl<strong>and</strong> <strong>and</strong><br />
occupies drainage depressions on tidal flats in which variations in salinity depend on seasonal<br />
rainfall. During the wet season, these depressions accumulate freshwater, which progressively<br />
evaporates during drier periods to increase salinity. During the driest periods of the year, the<br />
wetl<strong>and</strong>s are characterised by desiccated sedges including Schoenoplectus littoralis <strong>and</strong><br />
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Eleocharis dulcis often with an evaporate accumulation in drainage low points. These systems<br />
are dynamic <strong>and</strong> seasonal variations in species composition may lead to confusion with VC25b.<br />
The system does however appear unique to these northern isl<strong>and</strong>s <strong>and</strong> as such warrants<br />
recognition as a separate ecosystem. The habitat exhibits high integrity although there may be<br />
minor impacts associated with grazing of feral deer, although seasonal hunting controls this<br />
population. The extent of similar ecosystems on the Fly Platform of mainl<strong>and</strong> PNG is unknown<br />
yet likely to be associated with the Wunji L<strong>and</strong> System (CSIRO 1971). The RE provides<br />
important estuarine wetl<strong>and</strong> habitat values with likely habitat for estuarine crocodile, migratory<br />
waders, Jabiru <strong>and</strong> Sauras Crane <strong>and</strong> a cultural resource for traditional fishing <strong>and</strong> hunting.<br />
<strong>Vegetation</strong> Community 27b: The taller variant (VC27b) is restricted to Saibai Isl<strong>and</strong> where it<br />
occurs as a brackish wetl<strong>and</strong> comprising extensive areas of tall sedgel<strong>and</strong> mosaiced with open<br />
areas of brackish water. The community forms where freshwater swampl<strong>and</strong>s mix with estuarine<br />
waters, generally on the l<strong>and</strong>ward margins of mangrove forest complexes. Classification within<br />
L<strong>and</strong> Zone 1 is based on the regular tidal mixing, <strong>and</strong> the prominence of mangrove vegetation on<br />
the community margins. The community was originally mapped within the Map Unit 190 of<br />
Neldner <strong>and</strong> Clarkson (1995) <strong>and</strong> has been incorporated into RE3.3.63. The original description<br />
recognises that 48% of the community occurs on saline tidal flats.<br />
Photograph 17. Tall sedgel<strong>and</strong>/open<br />
wetl<strong>and</strong> mosaic on the l<strong>and</strong>ward<br />
margins of mangrove forest complex<br />
(VC27b). Saibai Isl<strong>and</strong>.<br />
Photograph 18. Low sedgel<strong>and</strong>/<br />
wetl<strong>and</strong> communities on seasonal<br />
drainage depression. VC27a on<br />
Boigu Isl<strong>and</strong>.<br />
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5.2.7 <strong>Regional</strong> Ecosystem 3.2.2a<br />
Description: Semi-deciduous vine thicket on coastal dunes <strong>and</strong> beach ridges<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 1c, 2p, 2y, 2z, 16d(co), 16e(co), 16f(co), 16h(co), 16j(co), 16k(co)<br />
Reference Sites: 2 secondary, 9 Quaternary<br />
This classification is restricted to true thickets, which according to definition adopted in this study<br />
have canopy heights less than 9m. These communities are often floristically similar to RE3.2.1x1<br />
although the much lower stature warrants differentiation. They are also relatively widespread,<br />
mapped on most of the larger continental isl<strong>and</strong>s in the Torres Strait Area. The RE comprises<br />
VC1c, VC2p, VC2y, a dominant component of VC16j <strong>and</strong> components of a number of coastal<br />
foredune complexes.<br />
<strong>Vegetation</strong> Community 1c: VC1c is an evergreen thicket of windswept foredunes. Manilkara<br />
kauki forms the dominant (<strong>and</strong> often sole) canopy species. Associated species include Celtis<br />
philippensis, Terminalia muelleri, Diospyros maritima, Thespesia populneiodes, Drypetes<br />
deplanchei, Mimusops elengi, Smilax australis, Capparis sepiaria <strong>and</strong> Flagellaria indica. The<br />
stature is influenced by coastal exposure which limits canopy height. It is prominent on Erub<br />
with a minor occurrence mapped on Masig Isl<strong>and</strong>.<br />
Photograph 19. Low windswept<br />
evergreen vine thicket (VC1c) on the<br />
exposed south-eastern coast of Erub.<br />
The thicket is dominated by<br />
Manilkara kauki.<br />
<strong>Vegetation</strong> Community 2p: The major occurrence of VC2p is on Moa Isl<strong>and</strong>, where it occupies<br />
foredune locations on broad coastal dune systems to the south of Saveka Point. In this location<br />
the community can be best described as a groved thicket with clumped trees reaching average<br />
canopy heights of 8m interspersed with bare areas of windblown s<strong>and</strong>. Bombax ceiba var.<br />
leiocarpum, Premna serratifolia, Acacia crassicarpa <strong>and</strong> Manilkara kauki are the dominant<br />
canopy species with emergents of Bombax to 15m height. Subdominant taxa are Drypetes<br />
deplanchei, Pouteria sericea <strong>and</strong> Celtis philippensis with the associated species Acacia<br />
polystachya, Diospyros compacta, Exocarpos latifolius, Aglaia elaeagnoidea, Canarium<br />
australianum, Carallia brachiata, Ficus virens, Cupaniopsis anacardioides, Semecarpus<br />
australiensis, Terminalia meulleri, Sterculia quadrifida, Arenga australasica <strong>and</strong><br />
Cochlospermum gillivraei. Arenga australasica (Vulnerable EPBC, NCA) is a prominent species<br />
in the sub-canopy layer on Moa Isl<strong>and</strong>. It is not likely that this unique feature can be extended to<br />
any mapped example of this community on other isl<strong>and</strong>s.<br />
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Photograph 20. The broken canopy<br />
typical of VC2p, Moa Isl<strong>and</strong>.<br />
Arenga australasica is a prominent<br />
sub-canopy component of this<br />
thicket community.<br />
<strong>Vegetation</strong> Community 2y: The major occurrences of vine thicket type 2y (VC2y) were not<br />
sampled during the survey other than an overview of the community provided by a helicopter<br />
flight over Sassie Isl<strong>and</strong>, <strong>and</strong> some notes of the community provided in the ICC report (Freebody,<br />
2002) on the central portions of Deliverance Isl<strong>and</strong>. From this overview, the community has<br />
described as a semi-deciduous notophyll vine thicket with canopy heights of 3-6m dominated by<br />
Premna serratifolia, Manilkara kauki, <strong>and</strong> Terminalia sp. (Freebody, 2002). Extensive<br />
occurrences of the type appear restricted to Deliverance <strong>and</strong> Sassie Isl<strong>and</strong>s although minor,<br />
possibly unrepresentative areas are present on Tudu Isl<strong>and</strong>.<br />
Photograph 21. An example of<br />
VC2y on the eastern end of Sassie<br />
Isl<strong>and</strong>. The community forms a<br />
fringe between mangroves <strong>and</strong><br />
coastline.<br />
<strong>Vegetation</strong> Community 2z/16j: <strong>Vegetation</strong> community 2z forms the dominant component of<br />
the foredune complex type 16j, which is mapped as a complex of notophyll vine thicket <strong>and</strong><br />
foredune grassl<strong>and</strong>/shrubl<strong>and</strong> complex. <strong>Vegetation</strong> community 2z conforms reasonably with the<br />
RE type description, being typified by an uneven canopy composed of deciduous notophyll <strong>and</strong><br />
occasional microphyll species. Constituent species are Sterculia quadrifida, Eugenia<br />
reinwardtiana, Manilkara kauki, Guettardia speciosa, Terminalia subacroptera.,<br />
Cochlospermum gillivraei, Acacia crassicarpa, Premna serratifolia, Aglaia elaeagnoidea,<br />
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Drypetes deplanchei, Diospyros maritima, Psydrax banksii, Elaeodendron melanocarpum,<br />
Capparis sepiaria, Turraea pubescens, Gyrocarpus americanus , Morinda citrifolia, Opilia<br />
armentacea, Capparis quiniflora, Cyclophyllum maritimum, Micromelum minutum, Pleurostylia<br />
opposita, Exocarpos latifolius, Tabernaemontana orientalis, Salacia chinensis, Alectryon<br />
reticulatus, Breynia cernua, Cayratia cardiophylla, Miliusa brahei <strong>and</strong> P<strong>and</strong>anus tectorius. The<br />
communities uneven appearance is accentuated by the groved nature of the community which has<br />
scattered clumps of trees <strong>and</strong> shrubs relatively well-spaced <strong>and</strong> separated by bare s<strong>and</strong> or sparse<br />
tussock grasses <strong>and</strong> herbs. The community is represented in Photograph 22.<br />
5.2.8 <strong>Regional</strong> Ecosystem 3.2.2b<br />
Photograph 22. The typical<br />
structure of VC2z as a component of<br />
complex type 16j. Near Western<br />
Isl<strong>and</strong> Group.<br />
Preliminary Description: Semi-deciduous vine thicket on coastal dunes <strong>and</strong> beach ridges<br />
Preliminary Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 2a, 2l, 2u, 9b<br />
Reference Sites: 2 Secondary (Saibai SA1, SA94); 21 Quaternary<br />
This vegetation group sits uncomfortably in any current RE classifications groupings for Cape<br />
York Peninsula <strong>and</strong> has thus been proposed as a new RE type specific to the Torres Strait Isl<strong>and</strong>s.<br />
The proposed RE comprises four vegetation communities broadly described as semi-deciduous<br />
notophyll vine forests. The constituent communities are described briefly in the following<br />
section.<br />
<strong>Vegetation</strong> Community 2a: VC2a is restricted to the northern isl<strong>and</strong> group, with the best<br />
developed expression of the type on the south-eastern coastal margins of Saibai Isl<strong>and</strong>, although<br />
scattered occurrences are also found on the southern coast of Boigu Isl<strong>and</strong> <strong>and</strong> Gebar Isl<strong>and</strong>. The<br />
community occupies calcareous s<strong>and</strong> ridges, is deciduous in nature, <strong>and</strong> has maximum canopy<br />
heights of 35m in the better-developed examples. Erythrina variegata often dominates the<br />
uneven canopy with a mix of other deciduous species such as Terminalia subacroptera, Cordia<br />
subcordata, <strong>and</strong> Milletia pinnata <strong>and</strong> with evergreen species such as Manilkara kauki, Mimusops<br />
elengi <strong>and</strong> Aglaia elaeagnoidea. Associated canopy species are Acacia auriculiformis, P<strong>and</strong>anus<br />
sp., Excoecaria agollocha, Guettardia speciosa, Premna serratifolia, Drypetes deplanchei,<br />
Exocarpos latifolius, Diospyros maritima, Diospyros compacta, Ficus virens, Garcinia warrenii,<br />
Carallia brachiata, Buchanania arborescens, Pouteria obovata, Sterculia quadrifida, Garuga<br />
floribunda var. floribunda, Hibiscus tiliaceus, <strong>and</strong> Terminalia catappa. The occasional presence<br />
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of Heritiera littoralis, Xylocarpus granatum <strong>and</strong> Excoecaria agollocha is associated with an often<br />
sharp transition to mangrove forest.<br />
On the southern coasts of Saibai <strong>and</strong> Boigu this RE occupies the most elevated parts of the<br />
l<strong>and</strong>scape <strong>and</strong> therefore has been a focus for traditional settlement. Parts of the coast continue to<br />
provide seasonal living <strong>and</strong> camping sites for traditional owners being accessed only by boat.<br />
The vegetation is likely to also provide important ethno-botanical resources. The occurrence of<br />
*Cocus nucifera <strong>and</strong> *Bambusa vulgaris may be associated with past <strong>and</strong> present areas of<br />
settlement.<br />
Photograph 23. Deciduous crowns<br />
of Erythrina variegata in a welldeveloped<br />
example of VC2a. Southeastern<br />
margins on Saibai Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 2l: A single example of VC2l was located on a broad degraded s<strong>and</strong><br />
dune on the north-eastern side of Erub. Although restricted in area, this community was wellpreserved<br />
with minimum canopy disturbance <strong>and</strong> an intact ground <strong>and</strong> shrub layer. The canopy,<br />
which ranges from 12-25m, is dominated by Bombax ceiba var. leiocarpum <strong>and</strong> Garuga<br />
floribunda var. floribunda with Gyrocarpus americanus <strong>and</strong> Diospyros maritima. Associated<br />
species are Diospyros hebecarpa, Drypetes deplanchei, Celtis philippensis <strong>and</strong> Manilkara kauki.<br />
Pre-clearing mapping indicates that this community has always had a highly restricted occurrence<br />
<strong>and</strong> is unique to Erub. VC2l supports the Alectryon rep<strong>and</strong>odentatus (E) <strong>and</strong> the rare listed<br />
Neololeba atra.<br />
Photograph 24. The deciduous<br />
crowns of Garuga floribunda var.<br />
floribunda, Bombax ceiba var.<br />
leiocarpum <strong>and</strong> Gyrocarpus<br />
americanus clearly visible in the<br />
canopy of VC2l. Erub Isl<strong>and</strong>.<br />
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<strong>Vegetation</strong> community 2u: VC2u is the dominant variant in this proposed RE, being mapped on<br />
prograding dune s<strong>and</strong>s in a number of locations including Muralug, Moa <strong>and</strong> Warral Isl<strong>and</strong>s, as<br />
well as having a preserved example in the eastern group of isl<strong>and</strong>s on Dauar Islet. The canopy<br />
ranges from 12 to 30m, with characteristic species Mimusops elengi, Sterculia quadrifida <strong>and</strong><br />
Terminalia sp. although Manilkara kauki is always present. VC2u supports the vulnerable<br />
species Dendrobium biggibum (Cooktown Orchid) <strong>and</strong> Psydrax reticulata.<br />
Photograph 25. Well preserved <strong>and</strong><br />
developed example of VC2u on<br />
Wongai Beach, Muralug Isl<strong>and</strong>. The<br />
dark green canopy is dominated by<br />
Manilkara kauki.<br />
<strong>Vegetation</strong> Community 9b: VC9b was sampled to quaternary level on Muralug Isl<strong>and</strong> where it<br />
formed restricted groves on a broad dune amongst a broader area eucalypt dominant woodl<strong>and</strong>s.<br />
The canopy is composed of species similar to VC2u, although Neofabricia myrtifolia is a<br />
dominant to co-dominant species. Mapping indicates that this vine forest variation has a limited<br />
distribution in the Torres Strait Isl<strong>and</strong>s.<br />
5.2.9 <strong>Regional</strong> Ecosystem 3.2.3<br />
Description: Melaleuca dealbata ± Acacia crassicarpa open forest. Occurs in dune swales on<br />
the west coast.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 7g, 7e, 6d, 16g (co)<br />
Reference Sites: 8 Quaternary Sites<br />
Melaleuca dealbata has relatively restricted distribution in the mapping area, confined mostly to<br />
the Inner Isl<strong>and</strong>s <strong>and</strong> Near Western isl<strong>and</strong>s of Muralug <strong>and</strong> Moa. Where it occurs on coastal<br />
dunes, it is generally restricted to narrow linear swales which are relatively difficult to represent<br />
in a spatial sense due to scale, although where possible, these communities have been<br />
differentiated. Three vegetation communities <strong>and</strong> one vegetation complex comprise the<br />
representation of this RE in the isl<strong>and</strong> group <strong>and</strong> these are described below.<br />
<strong>Vegetation</strong> Community 7g: The best development of the RE is represented by VC7g, which is a<br />
common dune swale community on the south-west side of Muralug (see Photograph 26). To the<br />
immediate north of North-West Beach (Site PWS42) an extensive occurrence of this community<br />
occupies a dune swale complex with Melaleuca dealbata open forest occupying the dune swales,<br />
<strong>and</strong> lower Melaleuca dealbata woodl<strong>and</strong> inhabiting the dune crests. The dune crests support a<br />
dense grassy groundcover, whilst swales, being seasonal swamps, are largely devoid of<br />
vegetation. To the south, this community separates into a dune complex with crests composed of<br />
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Acacia crassicarpa woodl<strong>and</strong> (RE3.2.5) with associated Syzygium suborbiculare, Sterculia<br />
quadrifida, Grevillea parallela, <strong>and</strong> Parinari nonda. Melaleuca dealbata forest is attenuated<br />
along the dune swales. This complex of vegetation types has been mapped as VC16g.<br />
<strong>Vegetation</strong> Community 7e: <strong>Vegetation</strong> community 7e (see Photograph 27) is a lower variant<br />
of the RE, mapped on Moa Isl<strong>and</strong> in a back dune swale to the south of Saveka Point. The variant<br />
is characterised by a mixed canopy of dominant Melaleuca dealbata with Lophostemon<br />
suaveolens <strong>and</strong> Melaleuca saligna. Mapped distributions indicate that this type, potentially a new<br />
RE sub-type, has an extremely limited occurrence.<br />
<strong>Vegetation</strong> Community 6d: <strong>Vegetation</strong> community 6e, located on Possession Isl<strong>and</strong>, was<br />
sampled by helicopter reconnaissance only. Observations indicate that the dominant canopy<br />
comprises Acacia crassicarpa with a mix of Melaleuca species which may include Melaleuca<br />
dealbata <strong>and</strong> Melaleuca cajuputi. The community occupies a dune swale <strong>and</strong> through brief<br />
observation appears to occupy a swampier l<strong>and</strong>form than the previously described communities.<br />
Photograph 26. <strong>Vegetation</strong><br />
community 7g, occupying a dune<br />
swale at site PWS42.<br />
Photograph 27. <strong>Vegetation</strong><br />
Community 7e on Moa Isl<strong>and</strong>.<br />
Melaleuca dealbata forms the<br />
dominant canopy with Lophostemon<br />
suaveolens <strong>and</strong> Melaleuca saligna<br />
forming sub-dominant canopy<br />
components.<br />
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5.2.10 <strong>Regional</strong> Ecosystem 3.2.4<br />
Description: Melaleuca leucadendra ± M. dealbata open forest. In dune swales <strong>and</strong> swamps..<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 7b, 7d, 7f, 3e, 16c (co)<br />
Reference Sites: 4 Secondary Sites (PWQ4, MO66, MO20, BAS39), 17 Quaternary Sites<br />
Melaleuca leucadendra dominant communities are a relatively frequent community on dune<br />
swale systems of the Inner <strong>and</strong> Near Western Isl<strong>and</strong> groups. The extent of this RE is somewhat<br />
broadened by a range of Melaleuca dominant communities. These communities provide valuable<br />
wetl<strong>and</strong> (palustrine) habitat <strong>and</strong> may be inundated for a number of months over the wet season.<br />
<strong>Vegetation</strong> Community 7b: Melaleuca saligna forms the dominant canopy in VC7b, which is a<br />
relatively widespread community in dune swale systems on Moa Isl<strong>and</strong> where it is mapped as RE<br />
sub-type 3.2.4d. Remnants of it are also recognised on Mabuiag Isl<strong>and</strong> where it has been<br />
extensively cleared for residential development. It is ecologically <strong>and</strong> structurally similar to<br />
VC7f although canopy heights are often significantly lower, in the range of 15 to 20m. There is<br />
currently no RE or RE subtype classification that comfortably accommodates this vegetation<br />
community <strong>and</strong> it is suggested that an additional RE sub-type be erected to provide a suitable<br />
classification. Dependant on studies of the broader CYP bio-region, a sufficient extent of this<br />
community may be recognised to warrant an individual RE classification. A complex of VC7b<br />
<strong>and</strong> 14t (RE3.2.5) recognised near Kubin on Moa Isl<strong>and</strong> as complex type 16c (sites MOQ118 to<br />
MOQ120) appears to be similarly unique.<br />
<strong>Vegetation</strong> Community 7d: Melaleuca quinquenervia forms the dominant canopy component<br />
of VC7d (sampled at Site MOQ66), which is restricted to a broad swale south of Saveka Point on<br />
Moa Isl<strong>and</strong>. The community is mapped as RE sub-type 3.2.4b in this exercise, based on<br />
recommendations from the Queensl<strong>and</strong> Herbarium. Sub-dominant canopy species in this<br />
community include Lophostemon suaveolens, Melaleuca saligna <strong>and</strong> Melaleuca cajuputi <strong>and</strong><br />
canopy heights attain 20m. The sub canopy is dominated by Livistona muelleri <strong>and</strong> includes<br />
Lophostemon suaveolens, Melaleuca quinquenervia, Acacia crassicarpa <strong>and</strong> a host of epiphytes<br />
such as Myrmecodia platytyrea subsp. antoinii, Dendrobium triamellatum, Dischidia major <strong>and</strong><br />
Hydnophytum moseleyanum var. moseleyanum. A sparse understorey comprises Acacia<br />
leptocarpa, Melaleuca quinquenervia, Acacia crassicarpa, Livistona muelleri <strong>and</strong> Glochidion<br />
disparipes. Similar communities are classified as RE sub-type 3.2.4b in current mapping<br />
databases (REDD, Version 5.2, 2007) <strong>and</strong> this occurrence has been similarly classified. The<br />
extent of such communities in the Torres Strait Isl<strong>and</strong>s appears however to be extremely<br />
restricted.<br />
Photograph 28. Low open forest<br />
with dominant Melaleuca saligna<br />
(VC7b) in a dune swale on Moa<br />
Isl<strong>and</strong> (MOQ122).<br />
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Photograph 29. Open forest with<br />
dominant Melaleuca quinquenervia<br />
(VC7d) in a dune swale on Moa<br />
Isl<strong>and</strong> (MOS66).<br />
Photograph 30. Extensive swamp<br />
forest of Melaleuca quinquenervia<br />
(VC7d) nestled in deflationary<br />
hollow (LZ2). Near Western Isl<strong>and</strong><br />
Group.<br />
<strong>Vegetation</strong> Community 7f: VC7f forms what would probably be considered the type example<br />
of RE3.2.4 (classified in this exercise as RE3.2.4a) comprising a tall open forest of Melaleuca<br />
leucadendra (canopy 30-35m). In its best development sampled behind Long Beach on Muralug<br />
(Site PWQ4) the sub-canopy is extremely sparse comprising Livistona muelleri, Melaleuca<br />
saligna, Melaleuca cajuputi <strong>and</strong> Ficus virens. Well-developed examples also occur on Friday<br />
Isl<strong>and</strong> (Site FQ3) where the understorey of the features Livistona muelleri, Glochidion<br />
apodogynum, Cyclophyllum maritimum, Alstonia spectabilis, Mimusops elengi, Breynia cernua,<br />
Acacia polystachya, P<strong>and</strong>anus tectorius, Gymnosporia inermis, <strong>and</strong> Vitex acuminata.<br />
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Photograph 31. Tall open forest of<br />
Melaleuca leucadendra (VC7f) at its<br />
maximum development behind Long<br />
Beach on Muralug Isl<strong>and</strong> (Site<br />
PWQ4)<br />
<strong>Vegetation</strong> Community 3e: Lophostemon suaveolens dominant forests on coastal dunes are not<br />
common in the study area although representative communities are present on Badu Isl<strong>and</strong> where<br />
they form swamp forests on broad deflation plains. In these communities, Deplanchea<br />
tetraphylla, Asteromyrtus brassii, Acmena hemilampra subsp. hemilampra <strong>and</strong> Acacia<br />
crassicarpa are prominent canopy associates. These communities are recognised as RE sub-type<br />
3.2.4c (REDD Version 5.2, 2007) <strong>and</strong> have been similarly classified here. The community often<br />
forms broad, poorly defined mosaics <strong>and</strong> complexes with Melaleuca quinquenervia dominant<br />
swamp forest (VC7d/RE3.2.4b). The shrub layer supports Macaranga involucrata subsp.<br />
mallotoides with a groundcover dominated by Blechnum indicum, Scleria sp. <strong>and</strong> Canavalia<br />
papuana.<br />
Photograph 32. Tall open forest of<br />
Lophostemon suaveolens <strong>and</strong><br />
Deplanchea tetraphylla in complex<br />
with Melaleuca quinquenervia<br />
dominant open forest on Badu Isl<strong>and</strong><br />
(VC3e).<br />
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5.2.11 <strong>Regional</strong> Ecosystem 3.2.5<br />
Description: Acacia crassicarpa ± Syzygium suborbiculare ± Parinari nonda woodl<strong>and</strong>. On<br />
beach ridges.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 6c, 5p, 6g, 14v, 14t, 14q, 16c(co),16d(co), 16b(co), 16g(co)<br />
Reference Sites: 10 Quaternary Sites. (Includes MO118, NAQ9, NAQ6, FRQ2).<br />
Acacia crassicarpa dominant communities are common on prograding coastal dune <strong>and</strong> beach<br />
ridge systems, particularly on Muralug within the Inner Isl<strong>and</strong> Group. <strong>Vegetation</strong> communities<br />
comprising RE3.2.5 are structurally <strong>and</strong> floristically variable, ranging from tall shrubl<strong>and</strong>s to low<br />
open woodl<strong>and</strong>s, often with a mix of associated shrubl<strong>and</strong> <strong>and</strong> woodl<strong>and</strong> species. Acacia<br />
crassicarpa may form a sub-dominant component of some of the communities grouped under this<br />
classification.<br />
<strong>Vegetation</strong> Community 6c: The type example of this RE is VC6c, represented as RE3.2.5a in<br />
the RE mapping, is common on prograding beach ridge complexes typically found on the west<br />
coast of Muralug. The dominant canopy comprises Acacia crassicarpa which is generally<br />
associated with a number of vine forest <strong>and</strong> woodl<strong>and</strong> species such as Sterculia quadrifida,<br />
Terminalia subacroptera, Syzygium suborbiculare, Parinari nonda, Cochlospermum gillivraei,<br />
Neofabricia myrtifolia, Grevillea parallela, <strong>and</strong> Melaleuca viridiflora. The community typically<br />
forms a low open woodl<strong>and</strong> community with bare s<strong>and</strong> clearly visible between canopy trees on<br />
account of the sparse ground cover. Due to the frequent, although repetitive change in edaphic<br />
conditions across these dune sequences, these communities are commonly mapped as<br />
components of coastal dune complexes, as has been applied with VC16b, VC16d <strong>and</strong> VC16g.<br />
<strong>Vegetation</strong> Community 5p: <strong>Vegetation</strong> community 5p has been mapped wherever Corymbia<br />
species, (generally Corymbia novoguinensis, Corymbia clarksoniana or less commonly C.<br />
tessellaris), form prominent emergents or canopy components, represented as RE subtype 3.2.5b.<br />
Typically, Corymbia components are sparse, scattered as sub-dominant or co-dominant<br />
components of the canopy layer with species such as Parinari nonda, Sterculia quadrifida,<br />
Acacia crassicarpa, Canarium australianum <strong>and</strong> Alphitonia excelsa otherwise typical of VC6c.<br />
A Long-Fruited Bloodwood thought to be Corymbia polycarpa was collected on Muralug <strong>and</strong><br />
Horn Isl<strong>and</strong>s 5 . The community is represented in Photograph 34.<br />
<strong>Vegetation</strong> Community 6g: The broad system of stabilised transgressive dunes to the southwest<br />
of the Badu Isl<strong>and</strong> township host this relatively well-developed acacia dominant open forest<br />
type. Canopy heights are may reach 28m in some locations although communities of much lower<br />
stature (12-15m) are a more typical representation. Acacia crassicarpa dominates the canopy<br />
with Asteromyrtus brassii forming a prominent co-dominant to sub-dominant canopy species. A<br />
range of associated species including Melaleuca dealbata <strong>and</strong> Corymbia novoguinensis may be<br />
scattered sparsely throughout the canopy structure. In some locations, Asteromyrtus brassii may<br />
dominate the canopy although such areas are generally restricted. The predominant sub-canopy<br />
comprises Asteromyrtus brassii, Acmena hemilampra subsp. hemilampra, <strong>and</strong> Lophostemon<br />
suaveolens with characteristic species of the shrub layer including Astermomyrtus brassii,<br />
Dodonaea poly<strong>and</strong>ra, Endi<strong>and</strong>ra glauca, Halfordia kendack, Exocarpos latifolius, Psydrax<br />
banksii, Litsea glutinosa, Deplanchea tetraphylla, <strong>and</strong> Breynia oblongifolia. A dense low shrub/<br />
groundcover layer of Lom<strong>and</strong>ra banksii is a general feature of this community in association with<br />
Alyxia spicata, Lithomyrtus obtusa, Shizaea dichotoma <strong>and</strong> Panicum sp. As with the majority of<br />
acacia dominant communities, VC6g is indicative of past disturbance <strong>and</strong> may be a seral stage in<br />
a successional sequence from shrubl<strong>and</strong> to eucalypt woodl<strong>and</strong>. Alternatively, the forest type may<br />
be indicative of a severe fire scarring within a former eucalypt dominant community that is in a<br />
5 (DGF9219+DJS, DGF9221+DJS)<br />
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elatively advanced stage of recovery. Community 6g is recognised as sub-type variant RE3.2.5c<br />
on account of atypical structural features <strong>and</strong> geomorphic association. Representation is provided<br />
in Photograph 35.<br />
Photograph 33. Acacia crassicarpa<br />
dominant woodl<strong>and</strong> (VC6c) as a<br />
component of VC16d. Muralug (Site<br />
PWQ48).<br />
Photograph 34. Low open<br />
woodl<strong>and</strong> of Acacia crassicarpa,<br />
Grevillea parallela <strong>and</strong> Corymbia<br />
spp. typical of VC5p. This<br />
photograph is taken at Site PWQ71<br />
to the North of Bampfield Head on<br />
Muralug.<br />
Photograph 35. Well-developed<br />
Acacia crassicarpa dominant open<br />
forest with associated Asteromyrtus<br />
brassii (VC6g). Stabilised<br />
transgressive dunes system. Near<br />
Western Isl<strong>and</strong> Group.<br />
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<strong>Vegetation</strong> Community 14t/16c: This VC is represented on Moa Isl<strong>and</strong> as a component of dune<br />
complex type 16c (Site MO118), as well as a number of examples mapped individually on<br />
Muralug Isl<strong>and</strong> (PWO47). The community represents a sparse shrubl<strong>and</strong> with dominant species<br />
including Cochlospermum gillivraei, Canarium australianum, Eugenia reinwardtiana,<br />
Terminalia subacroptera with P<strong>and</strong>anus sp. dominating in some areas. In the complex type 16c,<br />
the shrubl<strong>and</strong> component occupies dune crests, separated by Melaleuca saligna/Melaleuca<br />
acacioides open forest in narrow dune swales. The community is represented in Photograph 36.<br />
Photograph 36. Shrubl<strong>and</strong> VC14t<br />
occupying beach ridges on Moa<br />
Isl<strong>and</strong> at site MOQ118.<br />
<strong>Vegetation</strong> Community 14v: Shrubl<strong>and</strong> community 14v is confined to Naghir Isl<strong>and</strong> where it<br />
manifests on exposed crests of aeolian dunes. Shrubs are generally low <strong>and</strong> sparse, dominated by<br />
Grevillea parallela, Acacia crassicarpa, Acacia polystachya, Terminalia subacroptera,<br />
Exocarpos latifolius <strong>and</strong> occasionally Eucalyptus leptophleba over a ground cover of<br />
Heteropogon triticeus <strong>and</strong> the exotic Hyptis suaveolens. A similar shrubl<strong>and</strong> forms a component<br />
of VC16e on the aeolian dune system of Friday Isl<strong>and</strong>. The shrubl<strong>and</strong> is represented in<br />
Photograph 37, taken at Site NAQ9. Due to its considerable departure from the RE3.2.25 type<br />
description, the inclusion of this community as an RE subtype should be considered. Disjunct<br />
populations of Eucalyptus leptophleba on Naghir represent the northern limit of the species<br />
geographical range.<br />
Photograph 37. Shrubl<strong>and</strong> type<br />
VC14v on exposed crests of aeolian<br />
dunes on Naghir Isl<strong>and</strong> (NAQ9). The<br />
dominant shrub in this location is<br />
Eucalyptus leptophleba.<br />
.<br />
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<strong>Vegetation</strong> Community 14q: A species of Cycas thought to be a disjunct population of Cycas<br />
badensis forms a low shrubl<strong>and</strong> on low parallel dunes on the north-west coast of Moa Isl<strong>and</strong><br />
where it is mapped as VC14q. The community was observed during a helicopter survey <strong>and</strong><br />
although not sampled on the ground, is relatively extensive, continuous, <strong>and</strong> readily differentiated<br />
as a discrete vegetation unit. The community is represented in Photograph 38.<br />
5.2.12 <strong>Regional</strong> Ecosystem 3.2.6<br />
Description: Casuarina equisetifolia woodl<strong>and</strong>. Occurs on foredunes.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 10a, 16e(co) 16f (co), 16b (co), 10b<br />
Reference Sites: 3 Secondary (Masig; YO5, YO6, YO16), 7 Quaternary Sites.<br />
Photograph 38. Cycas badensis<br />
forming a shrubl<strong>and</strong> community on<br />
low parallel dunes. North –west coast<br />
of Moa Isl<strong>and</strong> (VC14q).<br />
Casuarina equisetifolia forms a prominent woodl<strong>and</strong> community on foredunes throughout many<br />
of the isl<strong>and</strong>s in the study area, both on continental isl<strong>and</strong>s <strong>and</strong> coral cays. It is apparent through<br />
examination of a considerable number of Casuarina dominant communities throughout the study<br />
area that structural variations to this community occur, <strong>and</strong> the current descriptions provide an<br />
inadequate account of these variations.<br />
In a similar fashion to VC5p, frequent edaphic change across prograding dune systems has often<br />
resulted in a complexing of this RE with associated dune shrubl<strong>and</strong> <strong>and</strong> woodl<strong>and</strong> communities.<br />
These complexes are classified as VC16b <strong>and</strong> VC16f, the latter being a particularly welldeveloped<br />
example on the south coast of Friday Isl<strong>and</strong> where Casuarina equisetifolia woodl<strong>and</strong><br />
complexes with vine thicket (RE3.2.2). <strong>Vegetation</strong> community 10b provides what would<br />
generally be considered a typical representation of RE3.2.6, (represented in the RE attributes as<br />
RE3.2.6a) where Casuarina equisetifolia forms a woodl<strong>and</strong> community over a ground cover of<br />
sprawling herbs <strong>and</strong> grasses typical of foredune communities. Such examples are best<br />
represented on the west coast of Muralug (on Bampfield <strong>and</strong> Long Beach) where woodl<strong>and</strong>s<br />
typically reach 30m height <strong>and</strong> mix with scattered coastal vine forest species trees, most<br />
commonly Terminalia catappa. This would represent the maximum development of the type,<br />
<strong>and</strong> more typical examples on coastal foredunes would rarely reach an average canopy height of<br />
greater than 20m.<br />
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Photograph 39. Maximum<br />
development of VC10b on<br />
Bampfield Beach where Casuarina<br />
equisetifolia mixes with vine forest<br />
species.<br />
Photograph 40. <strong>Vegetation</strong> complex<br />
16f on Friday Isl<strong>and</strong> where<br />
Casuarina woodl<strong>and</strong> complexes with<br />
notophyll vine thicket. The Acacia<br />
in foreground right is Acacia oraria.<br />
Casuarina dominant communities which occur on the central group of isl<strong>and</strong>s <strong>and</strong> coral cays in<br />
particular, are poorly represented in the literature. Open forest of Casuarina equisetifolia forms<br />
the dominant vegetation type of Masig <strong>and</strong> Kodel Isl<strong>and</strong>s. Canopy heights ranging from 18 to<br />
25m are typical over a dense sub-canopy of vine forest species (height range of 10 to 15m)<br />
dominated by Diospyros maritima, Pouteria obovata, Aglaia elaeagnoidea, Diospyros compacta,<br />
Cyclophyllum maritimum <strong>and</strong> Terminalia subacroptera. Previous classification efforts have<br />
recognised the vine forest component only; however repeated measurement over three detailed<br />
sites in this survey clearly indicates that PFC of Casuarina is typically 60 to 80% with basal area<br />
measurement of 8-10m 2 /ha. This structural variation, represented as VC10a, is resticted to coral<br />
cays in the central isl<strong>and</strong> ground where they have been assigned to RE sub-type 3.2.6b.<br />
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Photograph 41. Open forest of<br />
Casuarina equisetifolia with a vine<br />
forest sub-canopy on Masig. The<br />
community is rapidly being<br />
fragmented to accommodate<br />
exp<strong>and</strong>ing sewerage infrastructure<br />
requirements.<br />
5.2.13 <strong>Regional</strong> Ecosystem 3.2.7<br />
Description: Corymbia intermedia or C. clarksoniana woodl<strong>and</strong> in wet coastal areas.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5i, 5o, 16e (co)<br />
Reference Sites: 8 Quaternary<br />
<strong>Vegetation</strong> Community 5i: <strong>Vegetation</strong> Community 5i, representing a ‘type community’ for<br />
RE8.3.7 is restricted largely to the Inner Isl<strong>and</strong> Group with sampled communities on Muralug,<br />
Horn, <strong>and</strong> Wednesday Isl<strong>and</strong>s. Corymbia clarksoniana forms an open forest community at sites<br />
PW3 (Muralug) <strong>and</strong> H17 (Horn), with a canopy height range of 18 to 23m <strong>and</strong> a typical sub<br />
canopy composed of Neofabricia myrtifolia, Acacia crassicarpa <strong>and</strong> Parinari nonda.<br />
<strong>Communities</strong> on Wednesday Isl<strong>and</strong> mapped as VC5i (Site WEQ13 <strong>and</strong> WEQ15) are dominated<br />
by Corymbia novoguinensis with a sparse sub canopy of Parinari nonda, Acacia crassicarpa <strong>and</strong><br />
Livistona muelleri (see Photograph 42). The shrub layer is well-defined <strong>and</strong> dominated by<br />
Jacksonia thesioides, Alyxia spicata, Parinari nonda, Acacia crassicarpa, Psydrax reticulata (V),<br />
Premna dallachyana, Syzygium suborbiculare, Psychotria poliostemma, Breynia oblongifolia,<br />
Psydrax banksii, Terminalia subacroptera, Smilax australis <strong>and</strong> Lithomyrtus retusa.<br />
<strong>Vegetation</strong> Community 5o/16e: A sub-type of this RE is represented by woodl<strong>and</strong> an open<br />
forest communities composed of Corymbia tessellaris. This sub-type was poorly sampled,<br />
although clearly visible as community on younger dune sequences on the north-west facing<br />
embayments of Muralug during helicopter <strong>and</strong> charter boat survey where it is mapped as VC5o.<br />
The community was also sampled as a component of VC16e, a woodl<strong>and</strong>/shrubl<strong>and</strong> complex on<br />
younger aeolian dune systems on Friday Isl<strong>and</strong> (Photograph 43) where an open shrub layer<br />
comprised Acacia crassicarpa, Sterculia quadrifida, Alstonia spectabilis, Alstonia actinophylla,<br />
Croton arnhemicus, Stephania japonica, Premna serratifolia, Mallotus nesophila, Canarium<br />
australianum, Smilax australis <strong>and</strong> Atalaya sericopetala.<br />
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5.2.14 <strong>Regional</strong> Ecosystem 3.2.8<br />
Photograph 42. VC5i on<br />
Wednesday Isl<strong>and</strong> (WEQ15) with<br />
dominant canopy composed of<br />
Corymbia novoguinensis.<br />
Photograph 43. VC16e forms a<br />
complex of woodl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong><br />
communities on Friday Isl<strong>and</strong>. The<br />
woodl<strong>and</strong> community is composed<br />
of Corymbia tessellaris which are<br />
visible on the skyline (Site FR2).<br />
Description: Corymbia nesophila ± C. novoguinensis ± Eucalyptus spp. woodl<strong>and</strong> on old<br />
stabilised dunes.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5k, 5n, 5m, 5q<br />
Reference Sites: 2 Quaternary<br />
<strong>Vegetation</strong> Community 5k: Corymbia nesophila dominant communities on coastal dunes are<br />
restricted in the mapping area. The RE would most typically be represented by VC5k (on coastal<br />
dunes), which is limited to a number of minor areas that have not been adequately ground truthed.<br />
<strong>Vegetation</strong> Community 5n: It is mapped as a number of disjunct occurrences on weathered<br />
(Pleistocene?) dune systems on the west coast of Muralug. In the representative Site PWQ40,<br />
Eucalyptus platyphylla forms the dominant canopy tree, ranging in height from 21-27m, with<br />
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Erythrophleum chlorostachys a sub-dominant component. Corymbia clarksoniana occasionally<br />
reaches the canopy <strong>and</strong> is co-dominant with Erythrophleum chlorostachys in the sub canopy.<br />
Photograph 44. <strong>Vegetation</strong><br />
Community 5n at Site (PWQ40) on<br />
Muralug Isl<strong>and</strong>. Eucalyptus<br />
platyphylla forms the dominant<br />
canopy species.<br />
<strong>Vegetation</strong> Community 5m & 5q: Variant VC5m is restricted to the north-coast of Wednesday<br />
Isl<strong>and</strong> on weathered back-dune situations. It forms a low woodl<strong>and</strong> community with dominant<br />
Corymbia stockeri subsp. peninsularis at heights of 10-12m. Acacia crassicarpa forms a sparse<br />
sub-canopy layer over a mid dense shrub layer of Cochlospermum gillivraei <strong>and</strong> Melaleuca<br />
stenostachya at 3-6m. The degraded dune feature which hosts this community merges l<strong>and</strong>ward<br />
with a s<strong>and</strong>y alluvial plain with negligible change in community floristics or structure. The open<br />
forest form of this community. Where Corymbia stockeri subsp. peninsularis forms an open<br />
forest, generally in absence of the dense shrub layer, the community is mapped as VC5q.<br />
Photograph 45. Low woodl<strong>and</strong> to<br />
open forest of Corymbia stockeri<br />
subsp. peninsularis (VC5q) on a<br />
weathered backdune situation.<br />
Wednesday Isl<strong>and</strong> at Site WEQ3.<br />
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5.2.15 <strong>Regional</strong> Ecosystem 3.2.10c<br />
Description: Eucalyptus tetrodonta, Corymbia clarksoniana ± E. brassiana or Erythrophleum<br />
chlorostachys woodl<strong>and</strong> on stabilised dunes.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5j<br />
Reference Sites: 2 Secondary Sites (PWS6, PWS69)<br />
<strong>Vegetation</strong> Community 5j: <strong>Regional</strong> Ecosystem 3.2.10c occurs only on the western coast of<br />
Muralug Isl<strong>and</strong> where older dune systems are well preserved <strong>and</strong> relatively extensive. The RE is<br />
typified by VC5j which provides a mix of species relatively representative of the RE type<br />
description. Eucalyptus tetrodonta dominates the canopy which reaches heights of greater than<br />
30m in most communities. Corymbia nesophila forms a sub-dominant to co-dominant canopy<br />
component in some communities with Corymbia novoguinensis <strong>and</strong> Corymbia clarksoniana<br />
locally prominent, although more abundant in sub-canopy layers. Erythrophleum chlorostachys<br />
is nearly always present in varying quantities. Sub-canopy species are relatively variable<br />
although Erythrophleum chlorostachys, Corymbia clarksoniana <strong>and</strong> Neofabricia myrtifolia are<br />
typical <strong>and</strong> were present in the sub-canopies of most communities sampled. The characteristic<br />
understorey is composed of Xylomelum scottianum, Acacia leptocarpa, Acacia platycarpa,<br />
Acacia crassicarpa, Acacia polystachya, Melaleuca viridiflora, Neofabricia myrtifolia,<br />
Planchonia careya, Grevillea parallela, Jacksonia thesioides, Leucopogon ruscifolius, Alphitonia<br />
excelsa, Syzygium suborbiculare with associated vine thicket species such as Cupaniopsis<br />
anacardioides, Sterculia quadrifida, Mallotus nesophila <strong>and</strong> Drypetes deplanchei.<br />
5.2.17 <strong>Regional</strong> Ecosystem 3.2.14<br />
Description: Melaleuca arcana low open forest. Associated with dune swamps.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: D13h<br />
Reference Sites: HI15<br />
Photograph 46. Tall open forest of<br />
Eucalyptus tetrodonta on degraded<br />
s<strong>and</strong> dunes at Site PWS6 (Muralug<br />
Isl<strong>and</strong>).<br />
<strong>Vegetation</strong> Community 13h: <strong>Regional</strong> Ecosystem 3.2.14 is restricted to a single occurrence on<br />
Horn Isl<strong>and</strong>, expressed as a low closed shrubl<strong>and</strong> which forms a semi-circular swamp within a<br />
broader relict dune system. Melaleuca arcana is the dominant species forming a shrub layer<br />
rarely exceeding 1.5m. The ground cover is dominated by Restionaceae spp. The occurrence of<br />
M. arcana in this locality represents an extension of geographical range north from the Jardine<br />
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River. The community is therefore unique in the Torres Strait regional context with future<br />
consideration to fire management requirements important for its long-term preservation.<br />
5.2.18 <strong>Regional</strong> Ecosystem 3.2.15<br />
Photograph 47. A low swamp<br />
shrubl<strong>and</strong> of Melaleuca arcana. Site<br />
HI15 on Horn Isl<strong>and</strong>.<br />
Photograph 48. Melaleuca arcana.<br />
Site HI15 on Horn Isl<strong>and</strong>.<br />
Description: Melaleuca viridiflora, Neofabricia myrtifolia woodl<strong>and</strong> on beach ridges.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: D8c, D13a, D17i<br />
Reference Sites: 1 Secondary (BAS20), 1 Quaternary (PWQ5)<br />
Two VC’s are classified under this ecosystem, of which VC13a is the most prominent.<br />
Characteristics of these vegetation communities are summarised below.<br />
<strong>Vegetation</strong> Community 13a: Melaleuca viridiflora shrubl<strong>and</strong> <strong>and</strong> low woodl<strong>and</strong> occupies<br />
extensive areas on the broad degraded s<strong>and</strong> dunes of Badu Isl<strong>and</strong>. The community in this<br />
location forms a low woodl<strong>and</strong> of 8 to 12m height dominated by Melaleuca viridiflora with<br />
scattered Asteromyrtus brassii <strong>and</strong> rare Corymbia novoguinensis. The sparse shrub layer is<br />
composed of Banksia dentata, P<strong>and</strong>anus sp., <strong>and</strong> scattered Acacia crassicarpa. Ground covers<br />
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are similarly sparse, dominated by Dapsilanthus spathaceus <strong>and</strong> a range of scattered herbs such<br />
as Drosera spatulata, Eriocaulon sp. <strong>and</strong> Dianella sp. In the better developed deflationary s<strong>and</strong><br />
sheets on Badu Isl<strong>and</strong>, the community forms a sparse shrubl<strong>and</strong>, verging on a sedgel<strong>and</strong> in areas<br />
where deflation has scoured the overlying s<strong>and</strong> sheet to its erosional base level (on the capillary<br />
fringe of the water table). Several examples of this community are also represented on Horn<br />
Isl<strong>and</strong> in association with a low dune-swale complex, where the structural <strong>and</strong> floristic affinities<br />
are similar to the examples on Badu Isl<strong>and</strong>.<br />
In some locations on Badu Isl<strong>and</strong> the Melaleuca shrub layer becomes very sparse, <strong>and</strong> the<br />
structural formation grades to a Dapsilanthus spathaceus dominant sedgel<strong>and</strong> generally with<br />
scattered emergent shrubs. These areas are mapped as VC17i, although are retained within the<br />
broader group of RE3.2.15.<br />
Photograph 49. Low woodl<strong>and</strong> of<br />
Melaleuca viridiflora (VC13a)<br />
occupying degraded s<strong>and</strong> dunes on<br />
Badu Isl<strong>and</strong> (BAS20).<br />
<strong>Vegetation</strong> Community 8c: A variant of the RE, represented as VC8c was mapped on the<br />
tapering slope of an old dune system on Muralug Isl<strong>and</strong>. The canopy of this community was<br />
dominated by Lophostemon suaveolens with Corymbia clarksoniana, Asteromyrtus<br />
symphyocarpa, Melaleuca saligna <strong>and</strong> Melaleuca viridiflora scattered evenly throughout.<br />
Melaleuca viridiflora, P<strong>and</strong>anus sp., <strong>and</strong> Banksia dentata formed the dominant sub-canopy<br />
component. Corymbia latifolia (shown in Photograph 50) was recorded in this community <strong>and</strong><br />
in adjoining woodl<strong>and</strong>s of E. tetrodonta <strong>and</strong> C. nesophila on old beach ridges. The species is<br />
known previously from a collection housed at the NSW Herbarium (T. Bean pers. comm. Jan 08).<br />
Its occurrence on Muralug <strong>and</strong> on Zuna verifies a considerable extension of the geographical<br />
extent being otherwise known only from the Northern Territory <strong>and</strong> West Kimberley Region<br />
(Brooker et al. 1994) <strong>and</strong> south west Papua (Conn et al. 2006+). Due to the extremely limited<br />
size of this community, it has been classified under RE3.2.15, in the absence of a more suitable<br />
classification.<br />
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5.2.19 <strong>Regional</strong> Ecosystem 3.2.19<br />
Photograph 50. Corymbia latifolia<br />
(DGF9199+DJS) forms a scattered<br />
canopy tree in VC8b on Muralug<br />
(Site PWQ5).<br />
Description: Leucopogon yorkensis ± Asteromyrtus brassii open heath on old beach ridges.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 14n, 14e,<br />
Reference Sites: 2 Quaternary (PO4, HI14, MO148)<br />
<strong>Vegetation</strong> communities 14n <strong>and</strong> 14e provide representation for RE3.2.19. These communities<br />
have a scattered distribution, with small areas mapped on Horn, Possession, Muralug <strong>and</strong> Moa<br />
Isl<strong>and</strong>s where they occupy deeply leached s<strong>and</strong> deposits of relict beach ridges.<br />
<strong>Vegetation</strong> Community 14n: This community is classified as RE3.2.19a based on advice<br />
provided by the Queensl<strong>and</strong> Herbarium. On Horn Isl<strong>and</strong>, the community represents a shrubl<strong>and</strong><br />
dominated by Acacia crassicarpa, Neofabricia myrtifolia, Leucopogon ruscifolius, L. yorkensis,<br />
<strong>and</strong> Cochlospermum gillivraei. These species form a relatively uneven shrubl<strong>and</strong> canopy from 4<br />
to 8m tall <strong>and</strong> with a scattered low shrub layer of Pouteria sericea, Psydrax banksii, Exocarpos<br />
latifolius, Myrsine sp., Alyxia spicata, Breynia oblongifolia, P<strong>and</strong>anus sp., Jacksonia thesioides,<br />
Drypetes deplanchei <strong>and</strong> Notelaea ovata. The groundcover is sparse of Lom<strong>and</strong>ra banksii,<br />
Aristida sp., <strong>and</strong> Dianella bambusifolia. Sterculia quadrifida <strong>and</strong> Premna serratifolia are<br />
associated with a number of additional shrubs including Grevillea parallela <strong>and</strong> Pouteria sericea<br />
which join the mix of species on Possession Isl<strong>and</strong>. Representative examples of this community<br />
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are also mapped on Badu Isl<strong>and</strong> where the community occupies a broad dune formation. On<br />
Badu, Leucopogon ruscifolius <strong>and</strong> Acacia crassicarpa form the dominant sparse shrubby canopy,<br />
although scattered emergents of Corymbia novoguinensis <strong>and</strong> Syzygium suborbiculare are<br />
occasionally present. The representation on Badu Isl<strong>and</strong> occupies an unstable transgressive dune<br />
sequence (as discussed in Section 1.1.3 <strong>and</strong> shown in Photograph 1) <strong>and</strong> appears to be a<br />
transitional to better developed open forest <strong>and</strong> woodl<strong>and</strong> types on more stable dune formations.<br />
A representative community on Possession Isl<strong>and</strong> is shown in Photograph 51.<br />
<strong>Vegetation</strong> Community 14e: A single representative unit of VC14e has been mapped on Moa<br />
Isl<strong>and</strong> where it is represented as RE sub-type 3.2.19b. This community is structurally dissimilar<br />
to the RE type description, <strong>and</strong> has been assigned to RE3.2.19 in the absence of a more suitable<br />
classification. The community is a dwarf open shrubl<strong>and</strong> dominated by Leucopogon ruscifolius<br />
with co-dominant Melaleuca viridiflora <strong>and</strong> subdominant Asteromyrtus brassii <strong>and</strong> Baeckea<br />
frutescens. Associated species are Banksia dentata, Acacia crassicarpa, Alyxia spicata <strong>and</strong><br />
Exocarpos latifolius. The epiphytes Dischidia major <strong>and</strong> Myrmecodia platytyrea subsp. antoinii<br />
are abundant throughout. Ground cover, dominated by Dapsilanthus spathaceus, Schoenus<br />
sparteus, Lom<strong>and</strong>ra banksii <strong>and</strong> Dianella bambusifolia is sparse, with areas of bare s<strong>and</strong> between<br />
the scattered shrubs. The community occupies a deeply leached s<strong>and</strong> sheet, which forms a low<br />
rise above the Tertiary s<strong>and</strong> plain on which it sits, interpreted to be a relict s<strong>and</strong> dune based on its<br />
position in the l<strong>and</strong>scape <strong>and</strong> broad crescent shape. The VC is illustrated in Photograph 52.<br />
Photograph 51. A relatively<br />
extensive occurrence of VC14n<br />
(RE3.2.19) on Possession Isl<strong>and</strong>.<br />
Photograph 52. Sparse low<br />
shrubl<strong>and</strong> 14e (RE3.2.19) on relict<br />
dune. Moa Isl<strong>and</strong> (MO148).<br />
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5.2.20 <strong>Regional</strong> Ecosystem 3.2.24<br />
Description: Closed herbl<strong>and</strong> of mixed graminoids <strong>and</strong> forbs. Occurs on exposed foredunes<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 17d, 17j, 16a (co), 16b (co), 16h (co), 16k (co)<br />
Reference Sites: 3 Secondary (YOS02, YOS13, YOS16), 1 Quaternary (TU8)<br />
<strong>Regional</strong> Ecosystem 3.2.24 forms an almost universal cover on the majority of coastal foredune<br />
communities sampled, although its best development is often associated with s<strong>and</strong> cay isl<strong>and</strong>s of<br />
the eastern group, particularly on foredune communities where s<strong>and</strong> actively accumulates.<br />
<strong>Vegetation</strong> Community 17j is the dominant component of this ecosystem forming an open to<br />
closed grassl<strong>and</strong> <strong>and</strong> forbl<strong>and</strong> complex composed of species including Spinifex sericeus, Vigna<br />
marina, Ipomoea pes-capre subsp. brasiliensis, Cassytha filiformis <strong>and</strong> a range of halophytic<br />
forbs such as Sesuvium portulacastrum. Grasses including Mnesithea rottboellioides <strong>and</strong><br />
Heteropogon triticeus form a prominent ground cover where the community is mapped as<br />
VC17d, although such grassl<strong>and</strong> areas are often an indication of prior disturbance.<br />
The representation of this RE as a homogenous ecosystem is rare due to the fine scale ecotonal<br />
change across foredune systems evident in the majority of locations. This ecosystem typically<br />
complexes with RE3.2.25 (VC14y) where it merges on the leaward side of dunes with low<br />
shrubl<strong>and</strong>. In such locations, the community is mapped as complex 16a. It also mixes with a<br />
range of other ecosystems including RE3.2.2 <strong>and</strong> RE3.2.6 represented in the mapping as complex<br />
types 16b <strong>and</strong> 16k. The RE provides an important rookery for sea turtles.<br />
5.2.21 <strong>Regional</strong> Ecosystem 3.2.25<br />
Photograph 53. Typical structure of<br />
RE3.2.24 (VC17j) on Masig Isl<strong>and</strong><br />
(YOS2).<br />
Description: Sparse herbl<strong>and</strong> of mixed herbaceous species on foredunes <strong>and</strong> beach ridges.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 16i, 14y, 16a (co), 16j (co)<br />
Reference Sites: 1 secondary (YOS4), 1 Quaternary (TU8)<br />
<strong>Regional</strong> Ecosystem 3.2.25 is composed of VC16i <strong>and</strong> VC14y, forming low sparse shrubl<strong>and</strong>s<br />
<strong>and</strong> shrubl<strong>and</strong>s respectively. The ecosystem generally occurs on foredune locations in<br />
association with <strong>and</strong> immediately l<strong>and</strong>ward of RE3.2.24 (VC17j) often complexing with this<br />
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community where it is mapped as complex 16a, <strong>and</strong> with microphyll vine thicket where it is<br />
mapped as VC16j. The two dominant components, VC16i <strong>and</strong> VC14y, are discussed briefly<br />
below.<br />
<strong>Vegetation</strong> Community 16i: <strong>Vegetation</strong> community 16i represents open tussock grassl<strong>and</strong> with<br />
emergent shrubs, verging on a sparse shrubl<strong>and</strong> in some locations. Ground cover is composed of<br />
Heteropogon triticeus <strong>and</strong> Cymbopogon sp. with emergent shrubs, ranging in height from 1-2m,<br />
typical of adjacent vine thicket communities <strong>and</strong> including Premna serratifolia, Terminalia<br />
subacroptera <strong>and</strong> Cordia subcordata. The community, which has been mapped exclusively on<br />
Tudu Isl<strong>and</strong>, is most likely the result of repetitive burning practice which has pushed back vine<br />
thicket margins. The community is represented in Photograph 54.<br />
It is of note that Haddon (1888) described the vegetation of Tudu on account of a visit there in<br />
1888 where “The interior of the isl<strong>and</strong> is flat, <strong>and</strong> supports a vegetation of bushes <strong>and</strong> coarse<br />
grass. In one spot only, about one-third from the northern end, are there a few fairly large trees,<br />
……. There are only a few young coconut palms” (Haddon 1888). An earlier account by Dumont<br />
d’Urville in 1840 in Haddon (1888) refers to Tudu as “a bank of s<strong>and</strong> almost at sea level, on the<br />
north point is a clump of trees, the rest of this miserable l<strong>and</strong> is saline, marshy, covered with<br />
grasses <strong>and</strong> shrubs that afford scarcely any shade”.<br />
Photograph 54. Open tussock<br />
grassl<strong>and</strong> with emergent shrubs on<br />
Tudu Isl<strong>and</strong> (VC16i).<br />
<strong>Vegetation</strong> Community 14y: <strong>Vegetation</strong> community 14y typically occupies a narrow fringe<br />
between foredune grassl<strong>and</strong> <strong>and</strong> taller open forest communities in backdune localities, in places<br />
ecotonal to this transition. The community is largely restricted to coral cays where it forms a<br />
complex with the foredune grassl<strong>and</strong> community VC17j, <strong>and</strong> is frequently mapped as a<br />
component of vegetation complex VC16a. Shrubl<strong>and</strong> is the dominant structural formation with a<br />
height range of 0.5m to 2m <strong>and</strong> projected canopy cover of 25% to 60%. Typical canopy species<br />
include Cordia dichotoma, Premna serratifolia <strong>and</strong> Drypetes deplanchei. These species form<br />
cover to a sparse ground cover typical of VC17j. <strong>Vegetation</strong> community 14y is not represented<br />
as a homogenous polygon in the mapping data.<br />
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5.2.22 <strong>Regional</strong> Ecosystem 3.2.26<br />
Photograph 55. Low open<br />
shrubl<strong>and</strong> community 14y on Masig<br />
Isl<strong>and</strong> (YOS4). The community has<br />
been mapped as a component of VC<br />
16a.<br />
Description: Sparse herbl<strong>and</strong>/shrubl<strong>and</strong> <strong>and</strong> bare s<strong>and</strong> areas. Predominantly on s<strong>and</strong> blows<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 14s<br />
Survey Locations: 1 Secondary Site (BAS35)<br />
<strong>Vegetation</strong> Community 14s: <strong>Vegetation</strong> community 14s, providing the only representation of<br />
RE3.2.26, is restricted to Badu Isl<strong>and</strong> where it forms a low sparse shrubl<strong>and</strong>. The dominant<br />
shrub layer forms an uneven upper stratum ranging in height from 0.5m to 1m with a total cover<br />
rarely exceeding 10%. Leucopogon ruscifolius forms the dominant component of the shrub layer<br />
with scattered Acacia crassicarpa, Leucopogon yorkensis, Syzygium suborbiculare, Exocarpos<br />
latifolius, Alyxia spicata, Melaleuca viridiflora <strong>and</strong> P<strong>and</strong>anus conicus. The groundcover forms<br />
5% combined cover dominated by Dapsilanthus spathaceus, with associated species such as<br />
Xyris complanata, Lom<strong>and</strong>ra banksii, Evolvulus alsinoides, Tricoryne elatior, Cassytha<br />
pubescens, Gompholobium sp. (DGF9707+), Tephrosia sp. (DGF9710+), Myrtella obtusa, <strong>and</strong><br />
Drosera spatulata. Emergents of Corymbia novoguinensis to 6m are scattered throughout the<br />
community. This community occupies a unique geomorphic situation, being restricted to the<br />
outer gently undulating slopes of a broad deflationary hollow within a stabilising transgressive<br />
dune system.<br />
Photograph 56. Low sparse<br />
shrubl<strong>and</strong> type 14s on Badu Isl<strong>and</strong>.<br />
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5.2.23 <strong>Regional</strong> Ecosystem 3.2.27<br />
Description: Ephemeral <strong>and</strong> perennial lakes in coastal dunefields.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 20b<br />
Survey Locations: No Representative Sites.<br />
A number of small perennial swamps are mapped on Badu Isl<strong>and</strong>, occupying deflationary<br />
hollows with a broad dune complex. The example represented in Photograph 57 occupies a<br />
degraded s<strong>and</strong> sheet on the l<strong>and</strong>ward margins of a transgressional dunefield. An association with<br />
fringing forests of Melaleuca quinquenervia is typical. Further survey is recommended to<br />
provide for full characterisation of these communities.<br />
Photograph 57. Shallow ephemeral<br />
<strong>and</strong> occasional seasonal open<br />
waterbodies are scattered across the<br />
Badu Isl<strong>and</strong> s<strong>and</strong> dunes <strong>and</strong> sheets.<br />
5.2.24 <strong>Regional</strong> Ecosystem 3.2.28<br />
Description: Evergreen notophyll vine forest on beach ridges on coral atolls, shingle cays <strong>and</strong><br />
s<strong>and</strong> cays.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 2m<br />
Survey Locations: 3 Secondary Sites (YO1, YO8, YO9)<br />
<strong>Vegetation</strong> Community 2m: <strong>Vegetation</strong> Community 2m, is mapped exclusively on coral cays<br />
of the central group of isl<strong>and</strong>s. Whilst floristically similar to VC2u (RE3.2.1x1), the community<br />
has been differentiated largely on a geographical basis. <strong>Vegetation</strong> Community 2u is restricted to<br />
parallel dune systems of continental isl<strong>and</strong>s while 2m dominates the calcareous s<strong>and</strong> of the coral<br />
cays. Differentiated from the type are Casuarina equisetifolia dominant open forests with vine<br />
forest sub-canopies previously mapped under this classification on Masig. The dominant canopy,<br />
which forms heights of 18 to 25m is composed of a mix of deciduous <strong>and</strong> evergreen species <strong>and</strong><br />
it is suggested that an amendment to the RE type description from evergreen to semi-deciduous<br />
should be considered. Dominant species include Milletia pinnata, Terminalia subacroptera,<br />
Diospyros maritima, Manilkara kauki, Aglaia elaeagnoidea, Pouteria obovata, Drypetes<br />
deplanchei with scattered Erythrina variegata. The latter species forms the dominant canopy on<br />
Gaboy Isl<strong>and</strong>. Highly disturbed examples of the type, sampled on Tudu <strong>and</strong> Aureed Isl<strong>and</strong>s, are<br />
generally dominated exclusively by Manilkara kauki, the likely result of selective indigenous<br />
l<strong>and</strong> management practice. <strong>Vegetation</strong> on these isl<strong>and</strong>s are reported to be heavily impacted by<br />
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firewood harvesting to service the Trepang industry (see Shnukal 2004). The vegetation<br />
community is represented in Photograph 58 overleaf.<br />
5.2.25 <strong>Regional</strong> Ecosystem 3.2.30<br />
Photograph 58. The sub-canopy<br />
structure of VC2m on Masig Isl<strong>and</strong><br />
at Site YO1.<br />
Description: Pemphis acidula ± low closed forest. Restricted to coral atolls, shingle cays <strong>and</strong><br />
s<strong>and</strong> cays.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 23b<br />
Reference Sites: 2 Quaternary<br />
<strong>Vegetation</strong> Community 23b: This shrubl<strong>and</strong>/low closed forest community is mapped on Tudu,<br />
Sassie, <strong>and</strong> Iama Isl<strong>and</strong>. It is recognised as a saline transitional type, providing indication that<br />
some overlap between LZ1 <strong>and</strong> LZ2 exists. On Tudu, it is typified by a closed shrubl<strong>and</strong> with<br />
canopy heights of 6m - 8m, forming an extensive l<strong>and</strong>ward fringe to mangroves <strong>and</strong> appearing to<br />
be confined to s<strong>and</strong> dunes (LZ2) above the average maximum tidal limit. A minor area on the<br />
north-west side of Iama mixes with the low mangrove shrub Osbornia octodonta on a coral<br />
platform at upper tidal limits. L<strong>and</strong> zone classification schemes adhered to in this survey<br />
consider this community as occurring within LZ1, although the floristic assemblage <strong>and</strong> l<strong>and</strong>form<br />
are considered consistent with those provided in the RE type description (REDD Version 5.2,<br />
2007). For the purposes of this study, the community has been mapped as RE3.2.30 in all<br />
occurrences, although clarification on the l<strong>and</strong> zone affinities of this community are required.<br />
Photograph 59. The light green crowns of<br />
Pemphis acidula (VC23b) forming an<br />
extensive fringe to mangrove communities<br />
on Tudu Isl<strong>and</strong>.<br />
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5.2.26 <strong>Regional</strong> Ecosystem 3.3.5c<br />
Description: Evergreen notophyll vine forest. Occurs on alluvium on major watercourses.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 1i, 1j, 3d (co)<br />
Reference Sites: 4 Secondary (MO48, MO76, MO107, MO106)<br />
<strong>Regional</strong> ecosystem 3.3.5 is composed of VC1i <strong>and</strong> VC1j, restricted to Moa Isl<strong>and</strong> where they<br />
occur on well-drained s<strong>and</strong>y alluvium of the larger watercourses <strong>and</strong> are representative<br />
communities of the RE sub-type 3.3.5c. The communities, which represent distinctive structural<br />
variations, are mapped as components of vegetation complex 3d. Maximum development of the<br />
RE occurs on Tutalia Creek where evergreen mesophyll vine forest (VC1i) <strong>and</strong> evergreen<br />
notophyll vine forest (VC1j) form a broad complex on the well-developed s<strong>and</strong>y flood plain<br />
alluvials on the lower reaches of Tutalia Creek. <strong>Vegetation</strong> community 1j is unique to Moa<br />
Isl<strong>and</strong> <strong>and</strong> is not known to occur on Cape York Peninsula.<br />
<strong>Vegetation</strong> Community 1i: This tall evergreen mesophyll gallery forest occupies the welldrained<br />
<strong>and</strong> seasonally inundated s<strong>and</strong>y banks on the lower reaches of Tutalia Creek, with minor<br />
occurrences also recorded in a number of other riparian situations on Moa Isl<strong>and</strong>. Canopy<br />
heights of 40m were regularly observed in this community with typical species including<br />
Horsfieldia australiana, Syzygium bamagense <strong>and</strong> Acmena hemilampra subsp. hemilampra<br />
although Maranthes corymbosa <strong>and</strong> Buchanania arborescens are prominent in some localities.<br />
The sub-canopy assemblage includes Licuala ramsayi, <strong>and</strong> P<strong>and</strong>anus spp. with Arenga<br />
australasica recorded at site MO83. The community is shown in Photograph 60. <strong>Vegetation</strong><br />
Community 1i is a prominent component of the complex type 3d.<br />
<strong>Vegetation</strong> Community 1j: <strong>Vegetation</strong> community 1j is a tall forest, reaching heights of 35m,<br />
with dominance shared between Acmena hemilampra subsp. hemilampra <strong>and</strong> Syzygium<br />
angophoroides. Associated canopy species include Acacia auriculiformis, Syzygium forte subsp.<br />
forte, Calophyllum sil <strong>and</strong> Buchanania arborescens. The sub-canopy is dominated by<br />
Podocarpus grayae with prominent P<strong>and</strong>anus sp., Buchanania arborescens <strong>and</strong> Calophyllum sil,<br />
Horsfieldia australiana, Endi<strong>and</strong>ra glauca, Carallia brachiata, <strong>and</strong> Deplanchea tetraphylla.<br />
Shrub layers are variable although a typical assemblage in better-developed locations may<br />
include Halfordia kendack, Atractocarpus sessilis, Podocarpus grayae, Endi<strong>and</strong>ra glauca,<br />
Salacia disepala, Dysoxylum oppositifolium, Cyclophyllum maritimum, Cryptocarya bamagana,<br />
Polyscias australiana, Haplosticanthus fruticosus, Psydrax sp. (DGF8955+), Polyalthia<br />
nitidissima <strong>and</strong> Cryptocarya cunninghamii.<br />
The community occupies the s<strong>and</strong>y flood overflow deposit on the lower reaches of Tutalia Creek,<br />
peripheral to the main flood channel on which maximum development of riparian rainforest<br />
occurs. The community is illustrated in Photograph 61.<br />
5.2.27 <strong>Regional</strong> Ecosystem 3.3.6<br />
Description: Evergreen notophyll vine forest with Melaleuca leucadendra on swamps.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 3c, 3d (co)<br />
Reference Sites: 3 Secondary (MO76, MO107, MO48)<br />
<strong>Regional</strong> Ecosystem 3.3.6 is represented by the vine forest/open forest mosaic of VC3c, <strong>and</strong> as a<br />
component of forest complex type 3d. These communities occupy swampy depressions <strong>and</strong> flood<br />
overflow channels on well-drained granitic alluvium. Characteristics of these communities are<br />
discussed briefly below.<br />
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<strong>Vegetation</strong> Complex 3c: <strong>Vegetation</strong> Complex 3c occupies a series of broad swampy drainage<br />
depressions on Moa Isl<strong>and</strong>. Tall mesophyll vine forest <strong>and</strong> Melaleuca open forest form a mosaic<br />
with roughly equal contribution to total canopy cover by both components, which have a canopy<br />
height range of 35m to 40m. The canopy of the tall open forest component is dominated by<br />
Melaleuca dealbata with Melaleuca leucadendra occurring in some locations (MO48). Subcanopy<br />
species are typically swamp tolerant <strong>and</strong> may include Dillenia alata, Gmelina<br />
dalrympleana, Horsfieldia australiana, Calophyllum sil, Acacia polystachya <strong>and</strong> P<strong>and</strong>anus sp.<br />
The type is restricted to Moa Isl<strong>and</strong> in broad drainage depressions. The community is shown in<br />
Photograph 62.<br />
The vine forest component occupies elevated loamy s<strong>and</strong> rises within the drainage swamp <strong>and</strong> is<br />
best described as a tall evergreen mesophyll vine forest. A canopy height range of 30 to 45m is<br />
typical with a diverse floristic composition dominated by Syzygium angophoroides, Acacia<br />
auriculiformis, Buchanania arborescens <strong>and</strong> Syzygium bamagense. Additional species are<br />
Syzygium forte subsp. forte, Gmelina dalrympleana, Terminalia sericocarpa, Maranthes<br />
corymbosa, Vitex acuminata, *Mangifera indica, Carallia brachiata, Calophyllum sil, Ficus<br />
drupacea <strong>and</strong> Acacia polystachya. The sub-canopy <strong>and</strong> shrub layers support Arenga<br />
australasica, P<strong>and</strong>anus spp., <strong>and</strong> Licuala ramsayi. The vine forest component of RE3.3.6 is<br />
illustrated in Photograph 63.<br />
<strong>Regional</strong> ecosystem 3.3.6 also forms a component of complex type VC3d, where it mixes with<br />
evergreen mesophyll forest type VC1i.<br />
Photograph 60. Tall evergreen<br />
mesophyll vine forest (VC3i)<br />
forming gallery forest on Tutalia<br />
Creek.<br />
<strong>Vegetation</strong> Complex 3d: Complex type 3d (VC3d) is mapped on Tutalia Creek (MO107) <strong>and</strong><br />
tributaries (Moa Isl<strong>and</strong>), as well as minor occurrence associated with a perennial drainage feature<br />
south of Saveka Point. Although riparian forest complexes, the lower reaches of these<br />
watercourses, which typically host these communities, form broad swampy flood overflow<br />
channels, <strong>and</strong> as such, are represented as swampl<strong>and</strong> ecosystems rather than specialist riparian<br />
forests. The open forest component of this complex, which is dominated by Melaleuca<br />
leucadendra (<strong>and</strong> occasionally Lophostemon suaveolens, provides representation for RE3.3.6,<br />
with the evergreen mesophyll vine forest component represented <strong>and</strong> previously described as<br />
VC1i (RE3.3.5c). The structural formation is consistent with the representation provided in<br />
VC3c with canopy heights of the Melaleuca leucadendra dominant open forest attaining 45m <strong>and</strong><br />
a range of vine forest species forming the sub-canopy <strong>and</strong> shrub layers.<br />
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Photograph 61. Tall notophyll<br />
forest VC1j on lower reaches on<br />
Tutalia Creek, Moa Isl<strong>and</strong> (MO106).<br />
Photograph 62. Tall open forest<br />
(swamp forest) of Melaleuca<br />
leucadendra on Moa Isl<strong>and</strong>.<br />
Component of VC3c.<br />
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5.2.28 <strong>Regional</strong> Ecosystem 3.3.7<br />
Photograph 63. Complex subcanopy<br />
features of the vine forest<br />
component of VC3c with prominent<br />
Arenga australasica. The large<br />
canopy tree in the foreground is<br />
Syzygium bamagense.<br />
Description: Tall semi-deciduous notophyll/microphyll vine thicket. Occurs on colluvial plains.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 2g, 4a<br />
Reference Sites: 1 Quaternary (G14)<br />
This RE is confined to Gebar Isl<strong>and</strong> as scattered pockets withint a broader grassl<strong>and</strong> community.<br />
The community also occurs as a perennial fringe to a deeply incised drainage line. The canopy,<br />
ranging in height from 15 to 25m, includes Canarium australianum, Terminalia subacroptera,<br />
Semecarpus australiensis, Buchanania arborescens <strong>and</strong> Acacia auriculiformis as dominant<br />
species. Erythrina variegata, Welchiodendron longivalve, Parinari nonda <strong>and</strong> Chionanthus<br />
ramiflora form subdominant canopy components. The sub canopy was not sampled intensively<br />
due to time restrictions. Also included in this category are isolated pockets of Welchiodendron<br />
longivalve open forest occupying the same l<strong>and</strong>form, which are thought to be fire disturbed<br />
variants of the better developed VC2g. Where these forests form discrete units, they are mapped<br />
as VC4a. Traditional burning practice has had a major structural impact on this community, most<br />
likely leading to a significant reduction in its original extent <strong>and</strong> floristic complexity.<br />
Photograph 64. Sub canopy<br />
structure of VC2g on Gebar Isl<strong>and</strong>,<br />
where it occupies loamy alluvial<br />
soils.<br />
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5.2.29 <strong>Regional</strong> Ecosystem 3.3.9<br />
Description: Lophostemon suaveolens open forest. Occurs on streamlines, swamps <strong>and</strong> alluvial<br />
terraces.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 3a, 3f, 8b<br />
Reference Sites: 2 Secondary (MOA16, BAS1); 5 Quaternary<br />
The RE classification 3.3.9 incorporates VC3a, VC3f <strong>and</strong> VC8b. These VC’s are considered<br />
atypical of the RE type description. These component vegetation communities are described<br />
briefly below.<br />
<strong>Vegetation</strong> Community 3a: <strong>Vegetation</strong> Community 3a on Moa Isl<strong>and</strong>, occupies the swampy<br />
channels of major drainage features, typically on lower stream reaches. The community is often<br />
narrow <strong>and</strong> linear, becoming more extensive on swampy areas where coarse alluvial s<strong>and</strong> has<br />
been deposited. Lophostemon suaveolens forms the dominant open forest canopy, attaining<br />
heights of 25m, although it is accompanied by Melaleuca quinquenervia, Syzygium<br />
angophoroides <strong>and</strong> Asteromyrtus brassii. The sub-canopy features Dillenia alata, Gmelina<br />
dalrympleana, <strong>and</strong> Acacia crassicarpa with a diverse shrub layer which includes Melastoma<br />
malabathricum subsp. malabathricum, Polyscias australianum, Chionanthus ramiflora,<br />
Flagellaria indica, Syzygium angophoroides, Diospyros hebecarpa, Rhodamnia australis,<br />
Deplanchea tetraphylla, Livistona muelleri, Carallia brachiata, Acmena hemilampra subsp.<br />
hemilampra, Terminalia sp., Litsea breviumbellata, Maranthes corymbosa, Tabernaemontana<br />
orientalis, <strong>and</strong> Macaranga involucrata var. mallotoides. Gahnia sp., Lom<strong>and</strong>ra banksii <strong>and</strong><br />
Lindsaea ensifolia form the dominant ground cover. The community merges downstream with<br />
VC3d which occupies the thicker deposits of fluvial s<strong>and</strong>.<br />
Photograph 65. VC3a at Site<br />
MO16 (Moa Isl<strong>and</strong>). Lophostemon<br />
suaveolens forms the dominant<br />
canopy.<br />
<strong>Vegetation</strong> Community 3f: The only described representation of VC3f is on Badu Isl<strong>and</strong> where<br />
it occupyies broad swampy drainage lines <strong>and</strong> <strong>and</strong> shallow depressions formed on loamy granitic<br />
alluvium. The community typically forms on the upper reaches of drainage lines in broad gully<br />
heads where a number of low angle alluvial fans coalesce. Lophostemon suaveolens forms the<br />
dominant canopy, reaching heights of 30m, with co-dominant to sub-dominant Melaleuca<br />
leucadendra. Corymbia clarksoniana forms a minor canopy component (5-10%) where the<br />
community was sampled <strong>and</strong> Parinari nonda occasionally reaches canopy height. The subcanopy<br />
is of Acacia leptocarpa, Acacia crassicarpa, Carallia brachiata, Dillenia alata <strong>and</strong><br />
P<strong>and</strong>anus sp., with Banksia dentata, Gmelina dalrympleana, P<strong>and</strong>anus sp., Rhodamnia australis<br />
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<strong>and</strong> Dillenia alata representing the most prominent shrub species with a height range of 3m to<br />
8m. The ground cover is typically dense with Ischeamum australe, Ischeamum sp., Imperata<br />
cylindrica, Heteropogon triticeus, Melastoma malabathricum subsp. malabathricum, <strong>and</strong><br />
Crotalaria calycina. The community is represented in Photograph 66.<br />
<strong>Vegetation</strong> Community 8b: <strong>Vegetation</strong> community 8b is located on a coastal outwash plain to<br />
the south of Saveka Point. The community forms a low open forest with Lophostemon<br />
suaveolens forming the dominant canopy. Sub-dominant species are typically Melaleuca saligna,<br />
Asteromyrtus brassii <strong>and</strong> Acacia crassicarpa. The sparse to mid-dense sub-canopy layer is<br />
dominated by Livistona muelleri, Pleomele angustifolia <strong>and</strong> Dodonaea poly<strong>and</strong>ra over a sparse<br />
shrub layer of Polyscias australianum, Litsea breviumbellata, Endi<strong>and</strong>ra glauca, Rhodomyrtus<br />
macrocarpa, Wilkiea rigidifolia, Alyxia spicata, Buchanania arborescens, Psydrax banksii,<br />
Calophyllum sil, Halfordia kendack, <strong>and</strong> Smilax australis. Lom<strong>and</strong>ra banksii dominates the<br />
ground cover. The alluvial substrate comprises coarse s<strong>and</strong> derived from alluvial outwash across<br />
a narrow swampy flood plain. Both drainage capacity <strong>and</strong> fertility can be considered moderate.<br />
Photograph 66. Open forest type 3f<br />
at Site BAS1 (Badu Isl<strong>and</strong>).<br />
Lophostemon suaveolens <strong>and</strong><br />
Melaleuca leucadendra form the<br />
dominant canopy species.<br />
Photograph 67. Low open forest of<br />
Lophostemon suaveolens, Melaleuca<br />
saligna, Asteromyrtus brassii <strong>and</strong><br />
Acacia crassicarpa (VC8b) at Moa<br />
Site MO72.<br />
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5.2.30 <strong>Regional</strong> Ecosystem 3.3.10<br />
Description: Melaleuca argentea <strong>and</strong>/or M. fluviatilis ± M. leucadendra open forest. Fringes<br />
streams <strong>and</strong> creeks.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 3b, 3g, 5h, 7f, 14o<br />
Reference Sites: 5 Quaternary<br />
<strong>Vegetation</strong> Community 7f: The dominant component of this RE is VC7f representing an open<br />
to tall open forest of Melaleuca leucadendra. It occurs commonly as a riparian fringe on major<br />
drainage features, extending to broader flood overflow plains in some locations. On riparian<br />
areas <strong>and</strong> associated overflow channels, Melaleuca leucadendra forms the canopy ranging in<br />
height from 15m in poorly developed communities on Warral Isl<strong>and</strong>, to greater than 30m on welldrained<br />
flood overflow channels on Muralug. <strong>Vegetation</strong> Community 7f is also represented by a<br />
woodl<strong>and</strong> variant extending away from the riparian margins across a silty flood plain (PW81).<br />
This Melaleuca leucadendra dominant community has a mixed sub-canopy layer of which<br />
Melaleuca saligna <strong>and</strong> Corypha utan are components. The occurrence of the latter species is a<br />
significant extension of range north from the Dulhunty River (Forster 1996) although the most<br />
northerly vouchered material at BRI is from near Aurukun (P. Forster pers. comm. March 2008).<br />
It also occurs in the Northern Territory. Similar communities on drainage swamps are<br />
represented as RE3.3.14b (VC7fs).<br />
Photograph 68. Open forest of<br />
Melaleuca leucadendra (VC7f) on<br />
flood overflow of North-West Ck,<br />
Muralug Isl<strong>and</strong> (PW58).<br />
Photograph 69. Disjunct population<br />
of Corypha utan forming a subcanopy<br />
component of Melaleuca<br />
leucadendra woodl<strong>and</strong> (VC7f).<br />
Muralug Isl<strong>and</strong> Site PW81.<br />
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<strong>Vegetation</strong> Complex 3b: <strong>Vegetation</strong> community 3b (RE3.3.10a) forms a tall open forest<br />
complex on Moa Isl<strong>and</strong> where it is restricted to narrow drainage lines incised into coarse s<strong>and</strong>y<br />
plains. A canopy height range of 28 to 38m is typical comprising Melaleuca argentea <strong>and</strong><br />
Melaleuca leucadendra, although occasionally accompanied by vine forest species including<br />
Syzygium forte subsp. forte becoming more prominent in the sub-canopy. Dominant sub-canopy<br />
species include Dillenia alata, Parinari nonda, Acacia auriculiformis, Buchanania arborescens,<br />
Euroschinus falcatus var. angustifolius <strong>and</strong> P<strong>and</strong>anus sp. The community is represented in<br />
Photograph 70. The community provides habitat for the vulnerable Voacanga gr<strong>and</strong>iflora.<br />
Photograph 70. Riparian open forest<br />
(RE3.3.10a) at Site MO4, Moa<br />
Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 3g: Broad swampy drainage lines carved into degraded s<strong>and</strong> dunes on<br />
Badu Isl<strong>and</strong> are habitat for swamp forest type VC3g. The drainage lines that host this community<br />
originate as swampy depressions nestled within broad s<strong>and</strong> sheets <strong>and</strong> become gradually more<br />
incised as water flux increases downstream. The depth of drainage incision, which may be up to<br />
3m, <strong>and</strong> seasonal water flow has resulted in the classification of these forests within LZ3 rather<br />
than LZ2, as might otherwise be applied if drainage away from the swamp was impeded to any<br />
degree. Melaleuca dealbata forms the dominant canopy of this community, reaching heights of<br />
30m, with associated species including Lophostemon sauveolens, Acmena hemilampra subsp.<br />
hemilampra, Syzygium forte subsp. forte, Syzygium angophoroides, Deplanchea tetraphylla,<br />
Gmelina dalrympleana <strong>and</strong> Acacia crassicarpa. Carallia brachiata, Dillenia alata <strong>and</strong> Gmelina<br />
dalrympleana are prominent as sub-canopy species. The shrub layer is dominated by the vine<br />
forest species Polyscias australiana, Wilkiea rigidifolia, Syzygium fibrosum, Chionanthus<br />
ramiflora, Cryptocarya brassii, Macaranga involucrata var. mallotoides, Rhodamnia australis,<br />
Dysoxylum oppositifolium, Tabernaemontana orientalis, Litsea breviumbellata, Endi<strong>and</strong>ra<br />
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glauca, Rhodamnia macrocarpa, Sterculia quadrifida, Haplosticanthus fruticosus <strong>and</strong> Litsea<br />
glutinosa. The community often forms in complex with Melaleuca leucadendra dominant<br />
riparian communities (VC3b) <strong>and</strong> is mapped in this exercise as sub-type variant 3.3.10d.<br />
Photograph 71. Tall open<br />
riparian forest type 3g on Badu<br />
Isl<strong>and</strong> (Site BDQ25).<br />
<strong>Vegetation</strong> Community 7b/14o: <strong>Regional</strong> Ecosystem sub-type 3.3.10b, represented by VC7b, is<br />
dominated by Melaleuca saligna, which forms a prominent low open forest fringe to major<br />
drainage lines on Muralug. Melaleuca acacioides may be associated with the sub-canopy of this<br />
VC on brackish river reaches. <strong>Vegetation</strong> Community 14o represents a riparian shrubl<strong>and</strong> variant<br />
of this RE sub-type mapped on the middle reaches of North-West Creek (Muralug Isl<strong>and</strong>).<br />
Classification of this system is based largely on aerial photographic interpretation <strong>and</strong> brief aerial<br />
inspection. As such, the specific characteristics of this community are poorly known although<br />
Melaleuca saligna <strong>and</strong> Acacia spp. are inferred as the dominant species.<br />
Photograph 72. <strong>Vegetation</strong><br />
Community 5h at Site HI57, Horn<br />
Isl<strong>and</strong> with Eucalyptus brassiana in<br />
the background.<br />
<strong>Vegetation</strong> Community 5h: <strong>Vegetation</strong> Community 5h represents a mixed riparian forest type<br />
classified under RE sub-type 3.3.10c. The dominant canopy, always in open forest formation,<br />
ranges in height from 15 to 23m <strong>and</strong> is composed of Melaleuca saligna, Corymbia stockeri subsp.<br />
peninsularis, Corymbia clarksoniana, Eucalyptus brassiana <strong>and</strong> Eucalyptus platyphylla.<br />
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Melaleuca leucadendra is also prominent in location. Melaleuca saligna forms the dominant<br />
sub-canopy component in association with Dillenia alata <strong>and</strong> Deplanchea tetraphylla. The<br />
community occupies swampy flood overflow plains, often associated with relict dune systems,<br />
<strong>and</strong> has been mapped only on Horn Isl<strong>and</strong>. A representative community is shown in Photograph<br />
72. The occurrence of Eucalyptus brassiana in this VC on Horn Isl<strong>and</strong> is a new record for the<br />
study area.<br />
5.2.31 <strong>Regional</strong> Ecosystem 3.3.12<br />
Description: Melaleuca quinquenervia open forest. Associated with scattered coastal swamps.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 7d<br />
Reference Sites: 2 Quaternary (MO148a, MO148b)<br />
<strong>Vegetation</strong> Community 7d: <strong>Regional</strong> Ecosystem 3.3.12 is represented by VC7b which is<br />
restricted to the broad erosional plain on the north-west side of Moa Isl<strong>and</strong> occurring as a number<br />
of sparsely scattered swampl<strong>and</strong> communities amongst a broader residual s<strong>and</strong> plain (LZ5).<br />
Melaleuca quinquenervia forms the dominant canopy species in a community which ranges<br />
structurally from open forest to shrubl<strong>and</strong>, depending largely on fire history. The ground cover is<br />
dominated by Dapsilanthus spathaceus, Schoenus sp. <strong>and</strong> P<strong>and</strong>anus sp.<br />
5.2.32 <strong>Regional</strong> Ecosystem 3.3.13<br />
Photograph 73. A Melaleuca<br />
quinquenervia swampl<strong>and</strong> formed on<br />
the broader residual s<strong>and</strong> plain.<br />
Description: Melaleuca saligna ± Hakea pedunculata open forest. Occurs on edges of salt pans.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 7bs<br />
Reference Sites: 2 Quaternary<br />
<strong>Vegetation</strong> Community 7bs: This RE, characterised by VC7bs is restricted largely to Horn<br />
Isl<strong>and</strong>, with occurrences also on Muralug. The community is represented by an open forest,<br />
generally low in stature with a canopy height range of 10 to 18m. The dominant canopy is<br />
formed by Melaleuca saligna although it mixes with Livistona muelleri, in some cases with<br />
Livistona dominating the canopy. The sub-canopy is often sparse, although Livistona muelleri<br />
<strong>and</strong> P<strong>and</strong>anus sp. are locally prominent. The l<strong>and</strong>form hosting this community is restricted to<br />
outwash plains on the margins of salt flats true to the type description. Where this community<br />
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occurs on drainage swamps, it has been classified as RE3.3.14 (VC7b), which is discussed in the<br />
following section.<br />
5.2.33 <strong>Regional</strong> Ecosystem 3.3.14<br />
Photograph 74. Livistona muelleri<br />
forming a prominent sub-canopy<br />
layer to Melaleuca saligna open<br />
forest (VC7bs). Horn Isl<strong>and</strong> Site<br />
HI5.<br />
Description: Melaleuca saligna ± M. viridiflora, Lophostemon suaveolens woodl<strong>and</strong> on<br />
drainage swamps.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 7b, 7e, 13g, 7fs<br />
Reference Sites: 9 Quaternary<br />
<strong>Regional</strong> Ecosystem 3.3.14 represents Melaleuca saligna dominant open forests occurring in<br />
drainage swamps. There is some degree of overlap with RE3.3.13 which occupies outwash plains<br />
adjacent to salt flats, most prominently on Horn Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 7b: Although occurring on the same L<strong>and</strong> Zone, RE3.3.14 has been<br />
classified where VC7b occurs in drainage depressions <strong>and</strong> represents a much more extensive<br />
expression of Melaleuca saligna dominant open forest, occurring on the majority of isl<strong>and</strong>s in the<br />
Inner Isl<strong>and</strong> Group, as well as Mabuiag <strong>and</strong> Moa Isl<strong>and</strong>. Whilst Melaleuca saligna is the<br />
dominant canopy species, it mixes with Melaleuca leucadendra, Livistona muelleri <strong>and</strong> Alstonia<br />
spectabilis on Friday Isl<strong>and</strong>. The sub-canopy is generally sparse, although Livistona muelleri <strong>and</strong><br />
P<strong>and</strong>anus sp. are generally prominent.<br />
<strong>Vegetation</strong> Community 13g & 7e: The RE classification also includes VC13g <strong>and</strong> VC7e,<br />
occurring on Zuna <strong>and</strong> Moa Isl<strong>and</strong>s respectively. <strong>Vegetation</strong> Community 13g represents a low<br />
closed shrubl<strong>and</strong> of Melaleuca saligna which forms a narrow (although mappable) fringe to an<br />
Eleocharis dominated swampl<strong>and</strong> community on Zuna Isl<strong>and</strong>. <strong>Vegetation</strong> Community 7e<br />
represents an open forest community with a canopy composed of Melaleuca dealbata, Melaleuca<br />
saligna <strong>and</strong> Livistona muelleri. The community, which occupies a broad drainage depression on<br />
the south coast of Moa Isl<strong>and</strong>, was identified during helicopter survey <strong>and</strong> was not subject to<br />
detailed on-ground investigation.<br />
<strong>Vegetation</strong> Community 7fs: Minor areas of Melaleuca leucadendra dominant swamp forest<br />
was observed during helicopter traverse fringing saline flats on Badu Isl<strong>and</strong>. This community,<br />
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mapped as VC7fs, has not been adequately ground truthed <strong>and</strong> requires further description. This<br />
representation has been mapped as RE3.3.14b.<br />
5.2.34 <strong>Regional</strong> Ecosystem 3.3.17b<br />
Photograph 75. Melaleuca saligna<br />
dominant open forest on a drainage<br />
swamp on Zuna Isl<strong>and</strong> (ZQ9).<br />
Description: Corymbia clarksoniana, Erythrophleum chlorostachys woodl<strong>and</strong> on alluvial plains.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5o, 5g, 5s<br />
Reference Sites: 1 Secondary (POW82), 1 Quaternary.<br />
<strong>Vegetation</strong> Community 5o: <strong>Vegetation</strong> Community 5o on alluvium provides the dominant<br />
representation of RE3.3.17b, restricted to the broad alluvial flats near Port Lihou on Muralug<br />
Isl<strong>and</strong>. The community occupies an unusual l<strong>and</strong>form situation, occurring on the alluvial aprons<br />
of a number of diorite knolls which protrude above the general surface of the surrounding alluvial<br />
plain. The derived soils are relatively fertile, clay rich, <strong>and</strong> have mild vertic properties<br />
manifesting in subdued gilgai morphology. Corymbia tessellaris forms the dominant canopy<br />
with associated Corymbia clarksoniana attaining canopy heights of 27m. Ground cover is<br />
composed of dense tussock grasses of which Themeda tri<strong>and</strong>ra is most prominent, although it<br />
also includes Ischaemum australe <strong>and</strong> Imperata cylindrica. The community has been classified<br />
with sub-type RE3.3.17b, which provides representation most consistent with the REDD (Version<br />
5.2, 2007).<br />
<strong>Vegetation</strong> Community 5g: <strong>Vegetation</strong> community 5g on alluvium represents a Corymbia<br />
tessellaris dominant open forest with small areas mapped on Warral Isl<strong>and</strong> <strong>and</strong> Friday Isl<strong>and</strong>.<br />
The community occurs most commonly on s<strong>and</strong>y alluvial soils derived from granite where it<br />
mixes with a range of vine forest species, making it distinct from VC5o which typically<br />
represents grassy woodl<strong>and</strong>. Limited floristic <strong>and</strong> structural information was gathered on this<br />
community.<br />
<strong>Vegetation</strong> Community 5s: <strong>Vegetation</strong> community 5s forms restricted areas of Corymbia<br />
clarksoniana <strong>and</strong> Corymbia tessellaris dominant low open woodl<strong>and</strong> on Muralug Isl<strong>and</strong>. Species<br />
associated with the sub-canopy of this community include Livistona muelleri <strong>and</strong> Acacia<br />
leptocarpa. This community is separated from VC5o by stature <strong>and</strong> l<strong>and</strong>form. <strong>Vegetation</strong><br />
community 5s forms a stunted community on silty poorly drained alluvial outwash, whilst 5o<br />
occupies more fertile soils derived from diorite <strong>and</strong> has developed considerably greater stature.<br />
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5.2.35 <strong>Regional</strong> Ecosystem 3.3.20c<br />
Photograph 76. Woodl<strong>and</strong> type 5o<br />
on alluvial soils. Muralug Isl<strong>and</strong> at<br />
Site PW82.<br />
Photograph 77. Corymbia<br />
tessellaris dominant open forest on<br />
alluvial flat (Friday Isl<strong>and</strong> Site<br />
FR21).<br />
Description: Corymbia clarksoniana ± Erythrophleum chlorostachys ± Melaleuca viridiflora<br />
woodl<strong>and</strong> on alluvial plains.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5b<br />
Reference Sites: 12 Quaternary<br />
<strong>Vegetation</strong> Community 5b: <strong>Vegetation</strong> Community 5b is the dominant woodl<strong>and</strong> an open forest<br />
community on Moa Isl<strong>and</strong> where it occupies silty alluvial outwash plains <strong>and</strong> piedmont fans,<br />
typically derived from granite, hornfels <strong>and</strong> metamorphic lithologies. The community is mapped<br />
as the newly described RE subtype 3.3.20c which is represented as a woodl<strong>and</strong> to open forest,<br />
with canopy heights ranging from 18 to 27m. Corymbia clarksoniana tends to dominate the<br />
canopy, although associated canopy species may include Corymbia nesophila, Corymbia<br />
tessellaris, Corymbia stockeri subsp. peninsularis <strong>and</strong> Welchiodendron longivalve.<br />
Welchiodendron is often well represented in the canopy <strong>and</strong> shrub layers which may also<br />
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comprise Planchonia careya, Melaleuca viridiflora, Acacia leptocarpa <strong>and</strong> Cycas sp. The Cycas<br />
is thought to be the endemic C. badensis.<br />
5.2.36 <strong>Regional</strong> Ecosystem 3.3.22<br />
Photograph 78. Typical structure of<br />
VC5b which represents the dominant<br />
woodl<strong>and</strong> <strong>and</strong> open forest<br />
community on Moa Isl<strong>and</strong> (Site<br />
MO94).<br />
Description: Corymbia clarksoniana or C. novoguinensis woodl<strong>and</strong> on alluvial plains.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5i, 5c<br />
Reference Sites: 1 Quaternary (Zuna ZQ6)<br />
<strong>Vegetation</strong> Community 5i: The major occurrences of this RE are on degraded s<strong>and</strong> dunes where<br />
they have been mapped as RE3.2.7. Small areas of VC5i occupy s<strong>and</strong>y alluvial wash on the<br />
margins of a drainage depression on Zuna Isl<strong>and</strong>, which represent the only mapped areas of this<br />
RE in the study area. This occurrence forms an open forest with relatively even canopy heights<br />
in the 18 to 23m range. Corymbia clarksoniana dominates the canopy, with Lophostemon<br />
suaveolens, Livistona muelleri <strong>and</strong> Parinari nonda associated. Livistona muelleri has a tendency<br />
to form dense groves in some areas which have been incorporated into the broader VC. The subcanopy<br />
is relatively dense (up to 40% PFC) <strong>and</strong> composed of Melaleuca viridiflora, Lophostemon<br />
suaveolens, Livistona muelleri, <strong>and</strong> P<strong>and</strong>anus sp. The shrub layer features Livistona muelleri,<br />
Acacia leptocarpa, Acacia brassii, Acacia simsii, Acacia crassicarpa, Ficus opposita, Dodonaea<br />
poly<strong>and</strong>ra <strong>and</strong> P<strong>and</strong>anus sp. Tall graminoids form the dominant ground cover comprising<br />
Ischaemum australe, Heteropogon triticeus, Mnesithea rottboellioides <strong>and</strong> Imperata cylindrica.<br />
The community merges with Melaleuca saligna open forest (RE3.3.17) where the ground<br />
becomes increasingly swampy.<br />
<strong>Vegetation</strong> Community 5c: This classification also includes VC5c where Corymbia<br />
clarksoniana forms a low woodl<strong>and</strong> community with co-dominant canopy species including<br />
Parinari nonda, Melaleuca viridiflora, Welchiodendron longivalve <strong>and</strong> P<strong>and</strong>anus sp. The subcanopy<br />
layers (typically an S1 layer) are typically dominated by Melaleuca viridiflora <strong>and</strong><br />
P<strong>and</strong>anus sp. This community is restricted to Moa Isl<strong>and</strong> where it occupies alluvial fans,<br />
although its occurrence is more extensive on the s<strong>and</strong>y alluvial plains of L<strong>and</strong> Zone 5.<br />
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5.2.37 <strong>Regional</strong> Ecosystem 3.3.27<br />
Photograph 79. A dense grove of<br />
Livistona muelleri within VC5i.<br />
Zuna Isl<strong>and</strong> Site ZQ6.<br />
Photograph 80. <strong>Vegetation</strong><br />
Community 5c recorded at Site<br />
MO99, Moa Isl<strong>and</strong>.<br />
Description: Corymbia nesophila ± Eucalyptus tetrodonta ± Eucalyptus brassiana woodl<strong>and</strong> on<br />
alluvial sediments.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5k, 5q, 5m<br />
Reference Sites: 2 Secondary, 18 Quaternary<br />
Three VC’s are represented under this category.<br />
<strong>Vegetation</strong> Community 5k: <strong>Vegetation</strong> Community 5k forms the dominant variant, being<br />
relatively extensive on the Inner Isl<strong>and</strong> Group <strong>and</strong> particularly well-developed <strong>and</strong> extensive on<br />
Horn <strong>and</strong> Muralug Isl<strong>and</strong>s. The community generally forms an open forest community with<br />
canopy heights ranging from 18 to 27m. Corymbia nesophila forms the dominant canopy species<br />
in most locations, although it mixes with Corymbia stockeri subsp. peninsularis <strong>and</strong> Eucalyptus<br />
tetrodonta in the majority of communities sampled. Erythrophleum chlorostachys forms a codominant<br />
canopy component in some locations on Muralug Isl<strong>and</strong> (Site PW78) <strong>and</strong> Corymbia<br />
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latifolia occasionally reaches the canopy (PQ63). Sub-canopy is variable although a general<br />
assemblage of species includes Melaleuca stenostachya, Neofabricia myrtifolia, Alphitonia<br />
excelsa, Xylomelum scottianum, Acacia polystachya, Livistona muelleri <strong>and</strong> Capparis arborea.<br />
Shrub layers are typically composed of Melaleuca viridiflora, Melaleuca stenostachya,<br />
Xylomelum scottianum, Acacia simsii, Persoonia falcata, Jacksonia thesioides, Acacia simsii,<br />
Acacia platycarpa, Banksia dentata, Melaleuca nervosa, Planchonia careya <strong>and</strong> Acacia<br />
leptocarpa. The ground cover generally comprises a range of grasses including Heteropogon<br />
triticeus, Panicum trichoides, Themeda tri<strong>and</strong>ra, Imperata cylindrica, Eriachne pallescens <strong>and</strong><br />
Eragrostis spartinoides.<br />
Photograph 81. A typical example<br />
of open forest type 5k on alluvium<br />
represented at Site PW15. The<br />
canopy in this community is<br />
dominated by Corymbia nesophila.<br />
<strong>Vegetation</strong> Community 5q: <strong>Vegetation</strong> community 5q forms a lower open forest variant of this<br />
RE. The community is restricted to the Inner Isl<strong>and</strong> Group with best development occurring on<br />
Muralug, Wednesday <strong>and</strong> Horn Isl<strong>and</strong>s. The general canopy ranges in height from 15 to 21m <strong>and</strong><br />
is dominated by Corymbia stockeri subsp. peninsularis with Corymbia nesophila <strong>and</strong> Corymbia<br />
clarksoniana commonly associated canopy species. The shrub layer is variable although in open<br />
forest communities on s<strong>and</strong>ier substrates, the shrub layer tends to be dominated by Acacia spp.<br />
<strong>and</strong> Jacksonia thesioides.<br />
<strong>Vegetation</strong> Community 5m: On siltier soils, the open forest structure is replaced by woodl<strong>and</strong><br />
<strong>and</strong> occasionally open woodl<strong>and</strong> with a sub-canopy layer dominated by a range of myrtaceous<br />
shrubs including Melaleuca stenostachya, Melaleuca viridiflora <strong>and</strong> Asteromyrtus symphyocarpa.<br />
In these locations, the community is mapped as VC5m, being prominent on Wednesday, Friday,<br />
<strong>and</strong> Horn Isl<strong>and</strong>s. It merges with VC 13d (RE3.3.48) in some areas where Melaleuca saligna<br />
forms a prominent sub-canopy component, particularly on Horn Isl<strong>and</strong> where VC5m <strong>and</strong> VC13d<br />
tend to mosaic. As a general rule applied, VC5m was classified where Corymbia stockeri subsp.<br />
peninsularis forms a clear canopy layer above sub-canopy strata. Where Corymbia stockeri is a<br />
component of the canopy that is subdominant to Melaleuca saligna (or associated Melaleuca<br />
spp.), or forms an emergent layer, the community is classified with VC13d.<br />
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5.2.38 <strong>Regional</strong> Ecosystem 3.3.28<br />
Photograph 82. Low woodl<strong>and</strong><br />
variant of VC5m at Site PW7 where<br />
Corymbia nesophila is a codominant<br />
canopy species with<br />
Corymbia stockeri subsp.<br />
peninsularis.<br />
Description: Eucalyptus platyphylla ± Corymbia clarksoniana woodl<strong>and</strong> on alluvial <strong>and</strong><br />
colluvial plains.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5u, 5n<br />
Reference Sites: 3 Quaternary<br />
<strong>Regional</strong> Ecosystem 3.3.28 is represented by two VC’s, both restricted to Muralug Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 5u: <strong>Vegetation</strong> Community 5u, surveyed by helicopter at Site PW116,<br />
represents a woodl<strong>and</strong> community with dominant Eucalyptus platyphylla with an estimated<br />
canopy heights range of 18 to 23m. The sub-canopy is relatively sparse, <strong>and</strong> is composed of<br />
Livistona muelleri <strong>and</strong> scattered Melaleuca viridiflora. Melaleuca spp. forms the dominant shrub<br />
layer over an open grassy ground cover. The community occupies a broad alluvial outwash plain<br />
on the l<strong>and</strong>ward margins of a coastal dune/estuarine wetl<strong>and</strong> complex.<br />
Photograph 83. <strong>Vegetation</strong><br />
Community 5u. Alluvial flat behind<br />
a coastal dune complex. Muralug<br />
Site 116.<br />
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<strong>Vegetation</strong> Community 5n: This community is restricted to alluvial terraces on North-West<br />
Creek where it forms an extensive flood plain type. Eucalyptus platyphylla dominates the canopy<br />
attaining maximum heights of 27m, with sub-dominant species including Eucalyptus tetrodonta,<br />
Corymbia nesophila <strong>and</strong> Erythrophleum chlorostachys. Sub-canopy is generally sparse, although<br />
Erythrophleum chlorostachys is prominent in association with Eucalyptus spp. <strong>and</strong> Corymbia<br />
spp. typical of the canopy. Ground cover is dominated by Heteropogon contortus, Imperata<br />
cylindrica <strong>and</strong> Themeda tri<strong>and</strong>ra. The community is represented in Photograph 84.<br />
5.2.39 <strong>Regional</strong> Ecosystem 3.3.42<br />
Description: Melaleuca viridiflora low woodl<strong>and</strong> in drainage areas.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 13a, 13b, 13c, 14b, 14m, 14r, 11b<br />
Reference Sites: 23 Quaternary<br />
Photograph 84. <strong>Vegetation</strong><br />
community 5n on an alluvial terrace<br />
of North-West Creek. The<br />
community, sampled in this location<br />
is located at PW061.<br />
<strong>Vegetation</strong> communities falling under the classification of RE3.3.42 form one of the most<br />
extensive <strong>and</strong> variable vegetation groups in the Torres Strait Isl<strong>and</strong>s. Melaleuca viridiflora forms<br />
the pivotal species in a group whose distribution <strong>and</strong> ecology is largely controlled by soil<br />
drainage <strong>and</strong> to a lesser extent, soil fertility.<br />
<strong>Vegetation</strong> Community 13a: <strong>Vegetation</strong> Community 13a represents the most abundant of the<br />
variations, common on the Inner Isl<strong>and</strong> <strong>and</strong> Near Western Isl<strong>and</strong> groups, with a floristic<br />
composition <strong>and</strong> structural form that is largely consistent with the type description of RE sub-unit<br />
3.3.42a. Melaleuca viridiflora dominantes the shrub layer with heights between 4m to 10m.<br />
P<strong>and</strong>anus sp. is a common sub-dominant species <strong>and</strong> a range of myrtaceous species may be<br />
associated, although at no stage are these associated species dominant. The community also<br />
includes scattered shrubl<strong>and</strong>s of Melaleuca acacioides on Moa Isl<strong>and</strong> which mix on the margins<br />
of salt flats <strong>and</strong> mangrove wetl<strong>and</strong>s. It occupies areas of limited surface drainage, generally on<br />
silty outwash plains with infertile clay loam soils.<br />
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Photograph 85. Shrubl<strong>and</strong><br />
dominated by Melaleuca viridiflora<br />
with scattered emergents of Parinari<br />
nonda <strong>and</strong> Corymbia clarksoniana.<br />
Site MO7 (Moa Isl<strong>and</strong>).<br />
<strong>Vegetation</strong> Community 13c: <strong>Vegetation</strong> Community 13c represents a shrubl<strong>and</strong>, canopy<br />
heights ranging from 3m to 6m, dominated by Melaleuca viridiflora, Asteromyrtus symphyocarpa<br />
<strong>and</strong> Banksia dentata. Hakea pedunculata <strong>and</strong> Melaleuca saligna may be associated although<br />
they are always sub-dominant shrub components, <strong>and</strong> Melaleuca acacioides may occur on<br />
community on saltpan margins. The secondary shrub layer is typically sparse, comprising species<br />
characteristic of the upper stratum <strong>and</strong> the ground cover is dominated by sedges, typically not<br />
forming more than 30% total cover. Melaleuca viridiflora is consistently represented by a<br />
distinctive variety represented as a low <strong>and</strong> generally poorly formed shrub with thick leathery<br />
leaves <strong>and</strong> distinctive red buds on growing points. The VC is consistent with the description<br />
provided for sub-type RE3.3.42a (REDD, Version 5.2, 2007) <strong>and</strong> it has been mapped as such.<br />
The major distribution of VC13j is on the larger isl<strong>and</strong>s of the Inner Isl<strong>and</strong> Group (Muralug <strong>and</strong><br />
Horn) <strong>and</strong> Moa Isl<strong>and</strong>, where it occupies poorly drained alluvial flats, typically on the peripheral<br />
margins of outwash plains where sediments are dominantly silts <strong>and</strong> clays. A superficial coating<br />
of fine white residual silica s<strong>and</strong> is often visible on the soil surface. This VC is also recorded on<br />
LZ5.<br />
Photograph 86. <strong>Vegetation</strong><br />
Community 13c on Muralug Isl<strong>and</strong><br />
(Site PW057).<br />
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<strong>Vegetation</strong> Community 13f: <strong>Vegetation</strong> Community 13f is recognised where Melaleuca<br />
viridiflora forms a canopy with sub-dominant to co-dominant Corymbia spp., typically in<br />
shrubl<strong>and</strong> to low woodl<strong>and</strong>s structural formation. A range of Corymbia species may be present<br />
include Corymbia stockeri subsp. peninsularis, Corymbia nesophila <strong>and</strong> Corymbia clarksoniana.<br />
Parinari nonda is locally abundant as a canopy <strong>and</strong> sub-canopy species <strong>and</strong> Banksia dentata <strong>and</strong><br />
Asteromyrtus symphyocarpa often form a prominent sub-canopy layer. Ground cover is variable<br />
although as a general rule, with Themeda tri<strong>and</strong>ra dominant in areas of better soil drainage,<br />
giving way to sedges as drainage becomes increasingly impeded. The community often merges<br />
with VC5c which occupies a similar l<strong>and</strong>scape position, although Melaleuca viridiflora<br />
represents a sub-canopy species in VC5c, only occasionally reaching canopy height. The major<br />
occurrences of this community are on Moa <strong>and</strong> Badu Isl<strong>and</strong>s. This community is extensively<br />
mapped in association with LZ5 on Moa Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 14m: Mixed shrubl<strong>and</strong> on Hammond Isl<strong>and</strong> forms VC14m. It is<br />
structurally a tall shrubl<strong>and</strong>, although it forms occasional woodl<strong>and</strong>, with an uneven upper<br />
stratum ranging in height from 5m to 12m. The community is consistent with RE3.3.42a <strong>and</strong> is<br />
represented within this sub-type in this exercise. Melaleuca viridiflora is a co-dominant canopy<br />
species mixing with Acacia crassicarpa, Grevillea parallela, Parinari nonda <strong>and</strong> P<strong>and</strong>anus sp.<br />
Corymbia tessellaris forms an emergent species reaching heights of 15m. Ground cover is<br />
dominated by grasses which include Imperata cylindrica <strong>and</strong> Heteropogon triticeus. The<br />
community occupies silty alluvial soils (alluvial fan) forming a corridor between granite<br />
footslopes with vine forest, <strong>and</strong> salt pan. It is likely that the structure <strong>and</strong> floristic composition of<br />
this community is heavily influenced by fire, <strong>and</strong> the community had been recently burnt at the<br />
time of survey. The community is represented in Photograph 87.<br />
Photograph 87. <strong>Vegetation</strong><br />
Community 14m on Hammond<br />
Isl<strong>and</strong> (Site HA12).<br />
<strong>Vegetation</strong> Community 14r: <strong>Vegetation</strong> Community 14r has a restricted distribution, confined<br />
to Moa Isl<strong>and</strong>, on coastal plains to the south of Saveka Point (St Paul’s) where it is represented<br />
under the broad sub-unit of RE3.3.42a. Canopy height ranges from 6m to 9m, represented<br />
structurally as a shrubl<strong>and</strong> to low woodl<strong>and</strong>. The upper stratum is mixed, comprising a relatively<br />
even proportion of Acacia crassicarpa, Melaleuca viridiflora <strong>and</strong> P<strong>and</strong>anus sp. Associated<br />
species include Parinari nonda, Banksia dentata <strong>and</strong> Lophostemon suaveolens which form subdominant<br />
canopy components <strong>and</strong> are always present. Banksia dentata is the dominant species in<br />
the secondary shrub layer. Ground cover is relatively dense with well-developed tussock grasses<br />
dominated by Ischaemum australe. The community, an example of which is represented in<br />
Photograph 88, is developed on silty alluvial outwash plains on the l<strong>and</strong>ward fringe of a broad<br />
coastal dune system.<br />
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Photograph 88. Low<br />
woodl<strong>and</strong>/shrubl<strong>and</strong> community 14r<br />
on Moa Isl<strong>and</strong>. The photograph is<br />
taken at Site MO65.<br />
<strong>Vegetation</strong> Community 11b: P<strong>and</strong>anus dominant shrubl<strong>and</strong>s <strong>and</strong> low woodl<strong>and</strong>s are prominent<br />
on drainage swamps <strong>and</strong> seepage zones is a range of localities, although they are most prominent<br />
on Dauan <strong>and</strong> Mabuiag Isl<strong>and</strong>. These communities generally form tall shrubl<strong>and</strong>s, mixing with<br />
Melaleuca viridiflora in some locations on Mabuiag Isl<strong>and</strong>, <strong>and</strong> have been classified as VC11b.<br />
These communities present some classification difficulties, having frequently developed in<br />
response to disturbance which may include intense fire or removal of previous canopy layers by<br />
mechanical disturbance. In the broader l<strong>and</strong>scape of the Torres Strait Isl<strong>and</strong>s, this community<br />
appears relatively stable being maintained by regular fire <strong>and</strong> remnant status is warranted. It<br />
should be noted that this community has been distinguished from the broad expanse of P<strong>and</strong>anus<br />
dominant woodl<strong>and</strong> occupying alluvial systems on Saibai Isl<strong>and</strong>. This VC has been classified<br />
under the broad RE sub-type 3.3.42a<br />
Photograph 89. A P<strong>and</strong>anus<br />
dominant low woodl<strong>and</strong> occupying a<br />
freshwater seepage zone on Dauan<br />
Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 13b: North of Mabuiag Isl<strong>and</strong>, Melaleuca viridiflora is replaced by<br />
Melaleuca cajuputi subsp. platyphylla as the dominant Melaleuca species. Melaleuca cajuputi<br />
forms extensive shrubl<strong>and</strong>s <strong>and</strong> low open forests on Saibai Isl<strong>and</strong>, <strong>and</strong> Boigu Isl<strong>and</strong> to a lesser<br />
extent. The shrubl<strong>and</strong> VC13b is restricted to Saibai Isl<strong>and</strong> where it forms a vegetation unit that is<br />
structurally similar to VC13a, although based on floristic affinities to vegetation communities<br />
associated with the northern Torres Strait Isl<strong>and</strong>s (Saibai in particular), has been assigned to the<br />
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new RE sub-type 3.3.42c. <strong>Vegetation</strong> Community 13b is represented with a general canopy<br />
height range from 3m to 6m, occasionally reaching 10m where ground becomes swampy.<br />
Melaleuca cajuputi forms the dominant shrubl<strong>and</strong> species although it mixes with P<strong>and</strong>anus sp.<br />
<strong>and</strong> Acacia leptocarpa. Acacia auriculiformis may represent a prominent canopy component<br />
where the shrubl<strong>and</strong> community fringes brackish wetl<strong>and</strong>s, merging with mixed shrubl<strong>and</strong> type<br />
14b. The ground cover is frequently dominated by Acrostichum aureum in these locations. The<br />
community occupies soil types which range from moist brackish clays to hardened silty clay<br />
loams with mound <strong>and</strong> hummock micro-topography as at Site SAS066.<br />
5.2.40 <strong>Regional</strong> Ecosystem 3.3.48b<br />
Photograph 90. <strong>Vegetation</strong><br />
Community 13b (RE3.3.42c) at Site<br />
SAS066 (Saibai Isl<strong>and</strong>).<br />
Description: Melaleuca saligna ± M. viridiflora low open woodl<strong>and</strong> in drainage depressions.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 13d<br />
Reference Sites: 20 Quaternary<br />
<strong>Vegetation</strong> Community 13d: <strong>Vegetation</strong> Community 13d has an extensive distribution on<br />
coastal outwash plains of the Inner <strong>and</strong> Near Western Isl<strong>and</strong> groups where it frequently mosaics<br />
with woodl<strong>and</strong>s (VC5m) <strong>and</strong> other shrubl<strong>and</strong> communities (13a, 13c). Melaleuca saligna is the<br />
characteristic <strong>and</strong> generally dominant species in the upper stratum, forming a shrubl<strong>and</strong> to low<br />
woodl<strong>and</strong> community with a height range from 5 to 9m. Associated canopy species include<br />
Melaleuca viridiflora (long drooping leaf variety), Asteromyrtus symphyocarpa, Asteromyrtus<br />
brassii <strong>and</strong> Banksia dentata. Corymbia stockeri subsp. peninsularis <strong>and</strong> Corymbia nesophila are<br />
occasional canopy components, forming an emergent layer in some locations, <strong>and</strong> merging with<br />
woodl<strong>and</strong> type 5m with increasing dominance of Corymbia spp. The shrub layer is frequently<br />
dominated by Asteromyrtus symphyocarpa <strong>and</strong> Banksia dentata with P<strong>and</strong>anus sp. locally<br />
prominent. Ground cover layers are typically sparse, dominated by a range of sedges <strong>and</strong> grasses,<br />
typically forming a cover of less than 30%. VC13d occupies poorly drained alluvial outwash<br />
plains, often with a superficial film of white residual s<strong>and</strong> at surface, rather than drainage<br />
swamps. The community is classified as the new RE sub-unit of 3.3.48b, distinctive from the<br />
more typical occurrences of RE3.3.48 which are described as being associated with drainage<br />
depressions. It is represented in Photograph 91 overleaf.<br />
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5.2.41 <strong>Regional</strong> Ecosystem 3.3.51<br />
Photograph 91. A relatively welldeveloped<br />
example of VC13d at Site<br />
H1011 (Horn Isl<strong>and</strong>). The shrub<br />
layer is poorly developed in this<br />
location.<br />
Description: Melaleuca acacioides ± Hakea pedunculata tall shrubl<strong>and</strong> on marine plains.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 13e, 13j<br />
Reference Sites: 6 Quaternary<br />
<strong>Regional</strong> Ecosystem 3.3.51, represented as VC13e <strong>and</strong> VC13j frequently forms a narrow fringe to<br />
mangrove communities on many of the larger isl<strong>and</strong>s including isl<strong>and</strong>s of both the Inner <strong>and</strong> Near<br />
Western Groups.<br />
<strong>Vegetation</strong> Community 13e: <strong>Vegetation</strong> Community 13e is the dominant representation of this<br />
ecosystem, forming a tall closed shrubl<strong>and</strong> (scrub) with Melaleuca acacioides on Horn Isl<strong>and</strong>,<br />
Muralug Isl<strong>and</strong>, <strong>and</strong> Moa Isl<strong>and</strong>. These are relatively simple communities, generally lacking a<br />
distinctive sub-canopy layer, with a ground cover dominated by salt tolerant sedges <strong>and</strong> grasses<br />
including Fimbristylis dichotoma <strong>and</strong> occasionally Sporobolus virginicus.<br />
<strong>Vegetation</strong> Community 13j: <strong>Vegetation</strong> Community 13j represents an open shrubl<strong>and</strong> variant<br />
restricted to a single mappable occurrence on Muralug Isl<strong>and</strong> behind Port Lihou. Canopy heights<br />
range from 3m to 6m with PFC generally less than 20%. Melaleuca acacioides forms the<br />
dominant shrub layer with associated species including Hakea pedunculata <strong>and</strong> Leucopogon<br />
ruscifolius. The Vulnerable listed orchid Dendrobium bigibbum was recorded in this community.<br />
5.2.42 <strong>Regional</strong> Ecosystem 3.3.57<br />
Description: Imperata cylindrica ± Mnesithea rottboellioides closed tussock grassl<strong>and</strong> on<br />
coastal plains.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 17d, 17g<br />
Reference Sites: 6 Quaternary<br />
Grassl<strong>and</strong>s mapped under the classification of RE3.3.57 fall in a generic group, <strong>and</strong> were difficult<br />
to differentiate on a floristic level due to lack of fertile specimens at the time of survey (late dry<br />
season).<br />
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Photograph 92. Tall closed<br />
shrubl<strong>and</strong> of Melaleuca acacioides<br />
(VC13e) on the margins of a salt flat<br />
(Site HI01, Horn Isl<strong>and</strong>).<br />
Photograph 93. Open shrubl<strong>and</strong><br />
with dominant Melaleuca<br />
acacioides. <strong>Vegetation</strong> community<br />
13j on Muralug Isl<strong>and</strong> (Site PW83).<br />
<strong>Vegetation</strong> Community 17d: <strong>Vegetation</strong> Community 17d provides reference to a floristically<br />
undifferentiated grassl<strong>and</strong> classification with a range of species including Imperata cylindrica,<br />
Themeda tri<strong>and</strong>ra, Heteropogon triticeus <strong>and</strong> Mnesithea rottboellioides. The community has<br />
scattered occurrences throughout the study area with the best developed examples being located<br />
on Moa Isl<strong>and</strong> <strong>and</strong> Gebar Isl<strong>and</strong>, generally on relatively well-drained, s<strong>and</strong>y loam soils. These<br />
grassl<strong>and</strong>s have developed in response to repetitive anthropogenic burning <strong>and</strong> the fire disclimax<br />
vegetation types are often evident scattered throughout the community as discontinuous <strong>and</strong><br />
isolated remnants. The community is represented in Photograph 94 overleaf.<br />
<strong>Vegetation</strong> Community 17g: <strong>Vegetation</strong> Community 17g has been mapped in a single location<br />
on Muralug where the dominant Themeda tri<strong>and</strong>ra <strong>and</strong> Imperata cylindrica grassl<strong>and</strong> community<br />
mosaics with Melaleuca nervosa shrubl<strong>and</strong>. The shrubl<strong>and</strong> component represents shrubby<br />
thickening in the absence of regular fire.<br />
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5.2.43 <strong>Regional</strong> Ecosystem 3.3.62<br />
Photograph 94. Grassl<strong>and</strong>s on a<br />
broad alluvial plain on Gebar Isl<strong>and</strong>.<br />
The community in this location<br />
represents a fire climax community<br />
with vine forest (the original<br />
vegetation type) clearly visible in the<br />
background.<br />
Description: Grassl<strong>and</strong>/sedgel<strong>and</strong> with P<strong>and</strong>anus spp. Confined to Torres Strait Isl<strong>and</strong>s.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 17a, 17e, 11a<br />
Reference Sites: 3secondary (SA15, SA21, BO16), 33 Quaternary<br />
This RE comprises a mosaic of grassl<strong>and</strong>, shrubl<strong>and</strong> <strong>and</strong> low woodl<strong>and</strong> types, confined mostly to<br />
Northern Isl<strong>and</strong>s group with extensive areas on Saibai Isl<strong>and</strong>. More restricted <strong>and</strong> scattered areas<br />
occur on Boigu, <strong>and</strong> isolated examples are also represented on Hammond <strong>and</strong> Moa Isl<strong>and</strong>s (Inner<br />
<strong>and</strong> Near Western Isl<strong>and</strong> Groups respectively). The RE is endemic to the Torres Strait.<br />
<strong>Vegetation</strong> Community 17a: The dominant component of this ecosystem is VC17a, generally<br />
developed as a closed tussock grassl<strong>and</strong> dominated by Ischaemum australe with associated<br />
species Imperata cylindrica, Themeda tri<strong>and</strong>ra, Mnesithea rottboellioides, V<strong>and</strong>asia retusa, <strong>and</strong><br />
Derris trifoliata. Species associated with brackish margins include Fimbristylis ferruginea,<br />
Acrostichum aureum, <strong>and</strong> Cynanchum carnosum. Characteristic emergent shrubs are Acacia<br />
leptocarpa, Melaleuca cajuputi subsp. platyphylla, P<strong>and</strong>anus sp. Livistona muelleri, Antidesma<br />
parviflorum, Acacia auriculiformis <strong>and</strong> less commonly Dillenia alata on the Northern Isl<strong>and</strong><br />
Group. This VC is represented in Photograph 95.<br />
<strong>Vegetation</strong> Community 17e: <strong>Vegetation</strong> Community 17e represents anthropogenically<br />
disturbed areas on Saibai Isl<strong>and</strong> which have re-established native grass cover. These<br />
communities are clearly identifiable on aerial photography due to their intricate <strong>and</strong> precisely<br />
constructed furrow <strong>and</strong> ridge morphology, indicative of prior cultivation. Barham (1999)<br />
identifies this feature as former prehistoric tropical field systems with characteristic physical<br />
traces of relict agricultural mounds <strong>and</strong> ditches. Barham <strong>and</strong> Harris (1985), in Barham (1999)<br />
report that the field systems on Saibai were partly in use as late as 1945 with detailed mapping<br />
carried out as part of archeological investigations indicating previous use of some 650 ha of l<strong>and</strong><br />
area. High cultural values are therefore assciated with this vegetation. This community is<br />
composed of grass species typical of VC17a, although they lack the prominent emergent shrub<br />
layer. A representative community is illustrated in Photograph 96.<br />
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Photograph 95. Remnants of the<br />
grassl<strong>and</strong> community 17a (VC17a)<br />
are scattered amongst the broader<br />
mosaic of salt flat <strong>and</strong> mangrove<br />
communities on Boigu Isl<strong>and</strong>.<br />
Photograph 96. The intricate<br />
pattern of irrigation channels carved<br />
into the alluvial l<strong>and</strong>scape are<br />
diagnostic of VC17e. These are<br />
visible in the photo foreground.<br />
<strong>Vegetation</strong> Community 11a: P<strong>and</strong>anus sp. forms the dominant component of VC11a, a tall<br />
shrubl<strong>and</strong>/low woodl<strong>and</strong> community that is most extensive on Saibai Isl<strong>and</strong>, with minor<br />
occurrences also on Hammond <strong>and</strong> Moa Isl<strong>and</strong>s. P<strong>and</strong>anus sp. forms the dominant component of<br />
the upper stratum which has a height range of 4m to 10m, <strong>and</strong> PFC generally between 10% <strong>and</strong><br />
40%. Associated canopy species include Melaleuca cajuputi subsp. platyphylla, Dillenia alata<br />
<strong>and</strong> Livistona muelleri, the latter often manifest as a canopy emergent. The secondary shrub layer<br />
is frequently dominated by Melaleuca cajuputi subsp. platyphylla, Acacia leptocarpa <strong>and</strong> low<br />
P<strong>and</strong>anus shrubs. Melaleuca acacioides forms a component of the secondary shrub layer on<br />
Hammond Isl<strong>and</strong>. In the majority of communities sampled, the ground cover is dominated by<br />
Ischaemum australe although Sarga sp. is locally prominent on Hammond Isl<strong>and</strong>. The<br />
development of this unique ecosystem is undoubtedly linked to soil type, as well as an ongoing<br />
fire practice. Whilst the RE is largely confined to the Northern Isl<strong>and</strong>s of the Torres Strait<br />
associated with isolated Pleistocene alluvial remnants of the Papuan Fly Platform, scattered<br />
occurrences of the type on the Inner <strong>and</strong> Near Western Isl<strong>and</strong> Groups provides some indication<br />
that similar l<strong>and</strong> use practice was being applied across the broader Torres Strait Isl<strong>and</strong> area.<br />
Detailed examination of soil profiles was not undertaken during the study, although some<br />
considerable differences in soil physical properties is expected between isl<strong>and</strong> groups where this<br />
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RE is supported, which provides some evidence that this community is shaped largely by l<strong>and</strong><br />
management practice. The community is widespread on the Morehead-Kiunga area of the PNG<br />
lowl<strong>and</strong>s <strong>and</strong> is identified in the Bula <strong>and</strong> Mibini L<strong>and</strong> Systems (CSIRO 1971).<br />
5.2.44 <strong>Regional</strong> Ecosystem 3.3.63<br />
Photograph 97. Typical<br />
representation of P<strong>and</strong>anus sp.<br />
shrubl<strong>and</strong>/woodl<strong>and</strong> (VC11a) on<br />
Saibai Isl<strong>and</strong> (Site SA021).<br />
Description: Closed sedgel<strong>and</strong> dominated by Eleocharis dulcis. Occurs on seasonally flooded<br />
marine plains.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 20a<br />
Reference Sites: 12 Quaternary (Saibai, Zuna)<br />
<strong>Vegetation</strong> Community 20a: VC20a is extensive only on Saibai Isl<strong>and</strong>, with minor areas<br />
mapped on the Inner Isl<strong>and</strong> Group (Zuna <strong>and</strong> Muralug Isl<strong>and</strong>s). The Saibai communities form an<br />
extensive system of broad shallow swamps attenuated well into the isl<strong>and</strong>s alluvial interior.<br />
These swamps possess a dense cover of Eleocharis sp. which was dry at the time of survey. A<br />
dramatic response to seasonal rainfall would be expected however, prompting vigorous new<br />
growth. These are generally brackish wetl<strong>and</strong> communities, merging with mangrove swamps <strong>and</strong><br />
salt pans on estuarine margins. In this regard, seasonal desiccation of these communities would<br />
be facilitated in part by salinity which increases dramatically as the soil dries, to be flushed<br />
during seasonal rainfall events. The community further manifests within a constructed wetl<strong>and</strong><br />
on Boigu Isl<strong>and</strong> <strong>and</strong> has a very restricted occurrence on Zuna. The latter is a circular swamp<br />
dominated by Eleocharis surrounded by shrubl<strong>and</strong> of Melaleuca saligna (VC13g).<br />
Representation is provide in Photograph 98.<br />
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5.2.45 <strong>Regional</strong> Ecosystem 3.3.68 (New RE)<br />
Photograph 98. An extensive sedge<br />
swamp with dominant Eleocharis sp.<br />
on Saibai Isl<strong>and</strong>. The wooded<br />
fringes are dominated by mangrove<br />
spp. <strong>and</strong> Melaleuca cajuputi subsp.<br />
platyphylla.<br />
Description: Semi-deciduous notophyll vine forest <strong>and</strong> thicket on alluvial plains. Northern<br />
isl<strong>and</strong>s of the Torres Strait.*<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 2c, 14b<br />
Reference Sites: 4 Secondary (Saibai SA40, SA43, SA80, BO8)<br />
A new RE, under the classification of RE3.3.68, has been erected to accommodate two VC’s<br />
which are restricted to the Northern Isl<strong>and</strong> Group. These communities, represented by vine forest<br />
classification 2c on Saibai Isl<strong>and</strong> <strong>and</strong> closed shrubl<strong>and</strong> type 14b an Boigu Isl<strong>and</strong>, occupy a unique<br />
l<strong>and</strong>form situation with no similar representation in either the broader isl<strong>and</strong> group or bio-region.<br />
<strong>Vegetation</strong> Community 2c: <strong>Vegetation</strong> community 2c is confined to Saibai Isl<strong>and</strong> where it<br />
occupies hard clayey alluvium on the margins of brackish swamps, generally as discontinuous<br />
pockets in the structural range of semi-deciduous vine thicket to semi-deciduous vine forest.<br />
Representative areas are also located on sinuous slivers on alluvium in the eastern portion of the<br />
isl<strong>and</strong>, which form low rises above tidal salt pans. The canopy is typically broken <strong>and</strong> uneven,<br />
ranging in height from 5 to 18m. Dominant species are Mimusops elengi, Terminalia<br />
subacroptera, Diospyros calycantha, Acacia auriculiformis, Manilkara kauki, Heritiera littoralis,<br />
Hibiscus tiliaceus, Excoecaria agollocha <strong>and</strong> Thespesia populneoides. Livistona benthamii <strong>and</strong><br />
Ptychosperma elegans are rare emergents <strong>and</strong> Melaleuca cajuputi subsp. platyphylla may also be<br />
locally prominent often on margins. Sub-canopy species are Mimusops elengi, Drypetes<br />
deplanchei <strong>and</strong> Cupaniopsis anacardioides with vines such as Flagellaria indica <strong>and</strong> Opilia<br />
armentacea common at Site SA80. It merges with transitional forest type VC23a, on brackish<br />
swamp margins, differentiated by the general prominence of mangrove species including<br />
Excoecaria agallocha <strong>and</strong> Avicennia marina in the transitional types. A representative<br />
photograph is provided in Photograph 99.<br />
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Photograph 99. Maximum<br />
development of VC2c on Saibai<br />
Isl<strong>and</strong> (Site SA80) with Livistona<br />
benthamii prominent in the subcanopy.<br />
Ptychosperma elegans in<br />
background left.<br />
<strong>Vegetation</strong> Community 14b: VC14b is restricted to Boigu Isl<strong>and</strong> where remnants are scattered<br />
across a large portion of the isl<strong>and</strong>s l<strong>and</strong>scape. The community is represented as a tall open scrub<br />
to low open forest with an upper stratum dominated by Acacia auriculiformis, Melaleuca cajuputi<br />
subsp. platyphylla <strong>and</strong> Terminalia subacroptera. A range of vine thicket species including<br />
Hibiscus tiliaceus, Mimusops elengi, Thespesia populneoides, Drypetes deplanchei <strong>and</strong><br />
Excoecaria agallocha generally form a sub-dominant component of the canopy. Prominent shrub<br />
species include Capparis lucida, Gymnosporia inermis, Chionanthus ramiflora, Drypetes<br />
deplanchei, Ximenia americanus <strong>and</strong> Diospyros littoralis. Thin wiry lianes such as Flagellaria<br />
indica, Opilia armentacea, Derris trifoliata <strong>and</strong> Cynanchum carnosum are abundant <strong>and</strong> may<br />
form part of the groundcover with Acrostichum aureum. The community occupies silty alluvial<br />
deposits that form low rises above a l<strong>and</strong>scape otherwise dominated by salt pans <strong>and</strong> estuarine<br />
wetl<strong>and</strong>s. These rises are rarely more that 0.5m above the maximum tidal levels, <strong>and</strong> from field<br />
observation, the community margins are rapidly retreating with succession by mangrove<br />
shrubl<strong>and</strong>s. A representative example is shown in Photograph 100. The rare species<br />
Tristiropsis acutangula (Sapindaceae) which occurs in the understorey as a sapling shrub is not<br />
previously known north of Cape York Peninsula (Lockerbie) (Herbrecs 2007) however occurs in<br />
Papua New Guinea (Conn et al. 2006).<br />
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5.2.46 <strong>Regional</strong> Ecosystem 3.3.69 (New RE)<br />
Photograph 100. Low open forest<br />
type 14b on a low alluvial rise<br />
amongst broader estuarine wetl<strong>and</strong><br />
vegetation.<br />
Preliminary Description: Melaleuca dealbata +/- Corymbia clarksoniana open forest on<br />
alluvial plains.<br />
Status: Not of Concern (VMS status requires review)<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 7c, 4d<br />
Reference Sites: 1 Secondary (MO49), 1 Quaternary<br />
<strong>Vegetation</strong> Community 7c: <strong>Vegetation</strong> Community 7c is restricted to coastal areas north of St<br />
Paul’s, Moa Isl<strong>and</strong>. The community is described as a tall open forest, with canopy heights<br />
ranging from 27 to 35m, composed of Melaleuca dealbata <strong>and</strong> Corymbia clarksoniana in<br />
relatively equal proportions. Sub-canopy comprises scattered trees to 18m including Corymbia<br />
clarksoniana, Livistona muelleri <strong>and</strong> Acacia crassicarpa. The community had been recently<br />
burnt at the time of survey <strong>and</strong> shrub layers <strong>and</strong> ground cover were sparse. Imperata cylindrica<br />
formed the dominant regenerating grass species. This community occupies a well-drained, thick<br />
sequence of alluvial outwash which has been heavily dissected by erosion gullies in some<br />
locations. The floristic composition of this community appears unique in a bio-regional context<br />
<strong>and</strong> a new RE code of RE 3.3.69 has been assigned following discussion with the Queensl<strong>and</strong><br />
Herbarium. This community has been heavily fragmented <strong>and</strong> a dominant proportion of the<br />
l<strong>and</strong>form that it occupies has been cleared.<br />
<strong>Vegetation</strong> Community 4d: <strong>Vegetation</strong> community 4d represents a minor component of the<br />
l<strong>and</strong>scape adjacent to VC7c, differing structurally as a low open forest community dominated by<br />
Welchiodendron longivalve <strong>and</strong> Melaleuca dealbata. Limited floristic information was gathered<br />
in relation to this community. Although similar to VC7d, it has been highly fragmented by<br />
clearing <strong>and</strong> infrastructure development. Due to its restricted size <strong>and</strong> similar l<strong>and</strong>form<br />
association, this VC has been included as a subtype of the proposed new RE3.3.69.<br />
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5.2.47 <strong>Regional</strong> Ecosystem 3.3.70 (New RE)<br />
Photograph 101. Tall open forest of<br />
Corymbia clarksoniana <strong>and</strong><br />
Melaleuca dealbata (VC7c) on Moa<br />
Isl<strong>and</strong> (Site MO48).<br />
Description: Lophostemon suaveolens +/- Melaleuca cajuputi subsp. platyphylla +/- P<strong>and</strong>anus<br />
sp. +/- Livistona muelleri woodl<strong>and</strong> <strong>and</strong> open forest. Alluvial plains of northern Torres Strait<br />
Isl<strong>and</strong>s.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 8a, 7a<br />
Reference Sites: 2 Secondary (Saibai SA20, SA61); 10 Quaternary<br />
The RE classification 3.3.70 incorporates two distinctive vegetation communities most<br />
commonly associated with the alluvial remnants of the Fly Platform on Saibai Isl<strong>and</strong>, although<br />
with minor occurrences extending southwards onto Moa Isl<strong>and</strong>. These communities are<br />
composed of VC8a <strong>and</strong> VC7b.<br />
<strong>Vegetation</strong> Community 8a/7b: <strong>Vegetation</strong> Community 8a is confined to Saibai Isl<strong>and</strong> where<br />
Lophostemon suaveolens forms an open forest community. It forms scattered groves throughout<br />
the more extensive Ischaemum spp. grassl<strong>and</strong>s (see RE3.3.62) which occupy the broad gently<br />
domed alluvial plains in the isl<strong>and</strong>s interior. Canopy heights range from 10-18m <strong>and</strong> associated<br />
canopy species may include Melaleuca cajuputi subsp. platyphylla, Livistona muelleri <strong>and</strong><br />
P<strong>and</strong>anus sp. although all three of these species are more prominent in the sub-canopy <strong>and</strong> shrub<br />
layers together with Acacia leptocarpa. Ground cover is generally dominated by Ischaemum<br />
australe, Imperata cylindrica <strong>and</strong> V<strong>and</strong>asia retusa. Upper trunks <strong>and</strong> branches support the<br />
epiphytes Myrmecodia platytyrea subsp. antoinii, Hydnophytum mosleyanum var. moseleyanum,<br />
Dischidia nummularia <strong>and</strong> D. major. Melaleuca cajuputi subsp. platyphylla occasionally<br />
separates from this community to form a discrete low open forest unit, particularly on swampier<br />
alluvial plain margins, unit classified as VC7a. In recognition of the association with the broader<br />
Lophostemon suaveolens open forest communities, VC7a has been classified as a component of<br />
RE3.3.70.<br />
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5.2.48 <strong>Regional</strong> Ecosystem 3.5.5<br />
Photograph 102. Low open forest<br />
of Lophostemon suaveolens.<br />
Alluvial plains of Saibai Isl<strong>and</strong>.<br />
Description: Corymbia novoguinensis or C. nesophila ± C. tessellaris woodl<strong>and</strong> on northern<br />
Cape York Peninsula.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5a<br />
Reference Sites: 4 Quaternary (MO5, MO15, MO23, MO153).<br />
<strong>Vegetation</strong> Community 5a: <strong>Regional</strong> Ecosystem 3.5.5, represented as VC5a in this mapping<br />
exercise, is restricted to Moa Isl<strong>and</strong>. Where surveyed, the community presents as an open forest<br />
with a canopy height range of 18m to 25m dominated by Corymbia novoguinensis. Associated<br />
canopy species typically include Parinari nonda, Lophostemon suaveolens, Acacia crassicarpa<br />
<strong>and</strong> Melaleuca viridiflora although these species are never dominant. The sub-canopy, which<br />
ranges from 10 to 15m is typified by Parinari nonda, Lophostemon suaveolens, Livistona<br />
muelleri, Acacia crassicarpa, Welchiodendron longivalve, Melaleuca viridiflora <strong>and</strong> Syzygium<br />
suborbiculare. Ground cover is typically grassy although species were not identified due to lack<br />
of fertile material. The open forest community occupies the s<strong>and</strong>y remnants of a former<br />
depositional surface. These remnants form low, flat or gently undulating rises above a<br />
surrounding erosional plain, although scattered examples are found in a number of locations on<br />
the isl<strong>and</strong>. The community is represented in Photograph 103 overleaf.<br />
5.2.49 <strong>Regional</strong> Ecosystem 3.5.8c<br />
Description: Eucalyptus tetrodonta ± Corymbia hyl<strong>and</strong>ii subsp. peninsularis ± C. stockeri<br />
woodl<strong>and</strong> on erosional plains <strong>and</strong> s<strong>and</strong>tone plateaus.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5q<br />
Reference Sites: 2 Quaternary (FRQ9, WEQ9)<br />
Minor areas of RE3.5.8c are represented on Wednesday <strong>and</strong> Friday Isl<strong>and</strong>s where the community<br />
is characteristed as a low woodl<strong>and</strong> or low open woodl<strong>and</strong> of Corymbia stockerii subsp.<br />
peninsularis (VC5q). Melaleuca stenostachya is the typical sub-canopy dominant, although<br />
occasionally forms the canopy in areas of low soil moisture <strong>and</strong> fertility where it is differentiated<br />
as VC13i (RE3.5.7). A number of intermediate structural phases between woodl<strong>and</strong> <strong>and</strong><br />
shrubl<strong>and</strong> may exist, passing through open woodl<strong>and</strong> community 5m, although this community is<br />
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not differentiated from the broader woodl<strong>and</strong>/shrubl<strong>and</strong> complex. This RE is associated with<br />
deeply weathered terraces <strong>and</strong> remnant alluvial features, typically in lower mid-slope locations.<br />
More detailed analysis of these associated l<strong>and</strong>forms is provided in Section 5.1.4.<br />
5.2.50 <strong>Regional</strong> Ecosystem 3.5.15<br />
Photograph 103. <strong>Vegetation</strong><br />
Community 5a at Site MO23.<br />
Photograph 104. Typical<br />
representation of VC5q occurring on<br />
a deeply weathered alluvial feature<br />
(FRQ9).<br />
Description: Melaleuca viridiflora ± Acacia spp. ± Asteromyrtus symphyocarpa low woodl<strong>and</strong><br />
on scattered coastal s<strong>and</strong> plains.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 13d, 13c, 13a, 13f, 17i<br />
Reference Sites: 1 Secondary (MO19), 12 Quaternary (Moa & Muralug)<br />
<strong>Regional</strong> Ecosystem 3.5.15 exists as a mosaic of Melaleuca viridiflora dominant shrubl<strong>and</strong> <strong>and</strong><br />
low woodl<strong>and</strong> VC’s, largely restricted to Moa Isl<strong>and</strong> with small areas also mapped on Muralug.<br />
These VC’s occupy residual s<strong>and</strong>y plains, formed on deeply weathered granite on Moa, <strong>and</strong> clays<br />
on Muralug, <strong>and</strong> their formation is largely a response to infertile soils <strong>and</strong> poor drainage.<br />
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<strong>Vegetation</strong> Community 13d: <strong>Vegetation</strong> Community 13d, represented as a newly erected subtype<br />
RE3.5.15a, forms a somewhat better developed community with canopy heights to 8m <strong>and</strong><br />
canopy cover typically ranging from 40% to 60%. Melaleuca saligna is the characterising upper<br />
stratum species, which is typically co-dominant with Melaleuca viridiflora <strong>and</strong> Asteromyrtus<br />
symphyocarpa. Banksia dentata forms an occasional shrub layer, in association with species<br />
otherwise typical of the canopy. An emergent layer dominated by Corymbia spp. (typically<br />
Corymbia stockeri subsp. peninsularis or Corymbia nesophila) is commonly formed. The type<br />
occupies s<strong>and</strong>y plain areas, with soils better drained than VC13c. Numerous granite corestones<br />
area apparent scattered across the surface where the community was sampled at MO21.<br />
Illustration of VC13d is provided in Photograph 105.<br />
<strong>Vegetation</strong> Community 13c: The dominant community on Moa Isl<strong>and</strong> is VC13c, which forms a<br />
low sparse shrubl<strong>and</strong>, with shrub cover with a general range from 10% to 20%, <strong>and</strong> heights of the<br />
upper stratum ranging from 3m to 6m. Melaleuca viridiflora <strong>and</strong> Asteromyrtus symphyocarpa<br />
form the dominant shrub species, with associated <strong>and</strong> occasionally co-dominant shrubs including<br />
Asteromyrtus brassii <strong>and</strong> Banksia dentata. Melaleuca saligna <strong>and</strong> Leucopogon ruscifolius are<br />
occasional shrub species. Ground cover is typically sparse <strong>and</strong> dominated by Dapsilanthus<br />
spathaceus. In comparison to VC13a on alluvium, where this community occurs on remnant<br />
surfaces, the Melaleuca viridiflora variety is typically a longer (pendulous) leaf variety. A<br />
representative photograph is provided in Photograph 106. The community is described under<br />
RE sub-type 3.3.15b<br />
<strong>Vegetation</strong> Community 13f/13a: <strong>Vegetation</strong> Community 13f is recognised where Melaleuca<br />
viridiflora forms a canopy with sub-dominant to co-dominant Corymbia spp. This community<br />
forms a mosaic with Melaleuca viridiflora dominant woodl<strong>and</strong> (VC13a) on remnant alluvial<br />
plains on Moa Isl<strong>and</strong>. <strong>Vegetation</strong> Community 13f is typically a tall shrubl<strong>and</strong> to low woodl<strong>and</strong>,<br />
with an upper stratum height ranging from 7 to 10m. Canopy cover varies although cover of ><br />
40% is typical. The suite of Corymbia spp. that may be present include Corymbia stockeri subsp.<br />
peninsularis, Corymbia nesophila <strong>and</strong> Corymbia clarksoniana. Parinari nonda is locally<br />
abundant as a canopy <strong>and</strong> sub-canopy species <strong>and</strong> Banksia dentata <strong>and</strong> Asteromyrtus<br />
symphyocarpa often form a prominent sub-canopy layer. Ground cover is variable although as a<br />
general rule, with Themeda tri<strong>and</strong>ra dominant in areas of better soil drainage, giving way to<br />
sedges as drainage becomes increasingly impeded. The community often merges with VC5c<br />
which occupies a similar l<strong>and</strong>scape position, although Melaleuca viridiflora represents a subcanopy<br />
species in VC5c, only occasionally reaching canopy height (refer to Photograph 107).<br />
Photograph 105. <strong>Vegetation</strong><br />
Community 13d on residual plain with<br />
outcropping granite corestone.<br />
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Photograph 106. <strong>Vegetation</strong><br />
Community 13c on residual s<strong>and</strong><br />
plain. Moa Isl<strong>and</strong> Site M019.<br />
Photograph 107. Low woodl<strong>and</strong> of<br />
Melaleuca viridiflora <strong>and</strong> Corymbia<br />
clarksoniana (VC13f) on remnant<br />
s<strong>and</strong> plain at site MO112.<br />
<strong>Vegetation</strong> Community 17i: <strong>Vegetation</strong> Community 17i is a relatively extensive formation<br />
associated with residual s<strong>and</strong> plains on north-west side of Moa Isl<strong>and</strong> where it is represented as<br />
RE sub-type 3.3.15b, in recognition of its association with VC13c. The community was not<br />
sampled on the ground, being observed from helicopter, although some indication of its<br />
constituent species can be ascertained from Site MO149 where a swampl<strong>and</strong> within the broader<br />
VC17i community was sampled <strong>and</strong> where Dapsilanthus spathaceus formed the dominant ground<br />
cover, typical of other open shrubl<strong>and</strong> communities on the broader residual plain. Low emergent<br />
shrubs including Melaleuca viridiflora, P<strong>and</strong>anus sp. <strong>and</strong> Asteromyrtus brassii to 1m are<br />
associated with the community. This community has been assigned to the new RE sub-unit of<br />
RE3.5.15b (based on Herbarium recommendations) in recognition of its distinctive floristic <strong>and</strong><br />
structural characteristics, <strong>and</strong> its association with the broader mosaic of shrubl<strong>and</strong> <strong>and</strong> low<br />
woodl<strong>and</strong> communities comprising RE3.5.15.<br />
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5.2.51 <strong>Regional</strong> Ecosystem 3.5.17a<br />
Description: Melaleuca stenostachya +/_ Melaleuca viridiflora on flat plains.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: VC13i<br />
Reference Sites: 2 Quaternary (MO025, MO028)<br />
Photograph 108. Mosaic of<br />
sedgel<strong>and</strong> <strong>and</strong> low open forest<br />
(VC17i, VC9a) communities on<br />
residual s<strong>and</strong> sheets in the north west<br />
of Moa Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 13i: Mapped areas of VC 13i on L<strong>and</strong> Zone 5 are restricted to Friday<br />
<strong>and</strong> Wednesday Isl<strong>and</strong>s where it is represented as a shrubl<strong>and</strong>, or rarely as low woodl<strong>and</strong>, with a<br />
canopy dominated by Melaleuca stenostachya. Associated canopy species include Asteromyrtus<br />
symphyocarpa, Melaleuca viridiflora with Corymbia stockeri subsp. peninsularis frequently<br />
forming an emergent tree layer, becoming dominant where it merges with VC5m. This<br />
community occupies deeply weathered alluvial deposits, generally on gully heads where older<br />
alluvial l<strong>and</strong>forms are preserved as incised terraces. Derivation of these l<strong>and</strong>form features is<br />
described briefly in Section 5.1.5.<br />
Photograph 109. Tall shrubl<strong>and</strong> of<br />
Melaleuca stenostachya with<br />
emergent Corymbia spp. on deeply<br />
weathered alluvial remnants.<br />
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5.2.52 <strong>Regional</strong> Ecosystem 3.5.19a<br />
Description: Asteromyrtus lysicephala, Choriceras tricorne open heath on s<strong>and</strong> sheets.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 14i<br />
Reference Sites: 2 Quaternary (MO025, MO028)<br />
<strong>Vegetation</strong> Community 14i: <strong>Vegetation</strong> Community 14i is the only component of RE3.5.19,<br />
represented as sub-type 3.5.19a. The community is floristically atypical <strong>and</strong> has been placed in<br />
this category for convenience in the absence of more suitable category. Residual s<strong>and</strong> rises on<br />
Moa Isl<strong>and</strong> host the only representation of VC14i identified in the study area. The community<br />
manifests as a shrubl<strong>and</strong> <strong>and</strong> occasional low open forest with a general canopy height from 4m to<br />
8m, <strong>and</strong> emergents to 10m. Asteromyrtus brassii is the dominant species in the upper stratum,<br />
accompanied by Melaleuca saligna, Lophostemon suaveolens, <strong>and</strong> Acacia crassicarpa.<br />
Lophostemon suaveolens forms the dominant emergent species. The lower shrub layer achieves<br />
up to 50% cover featuring Leucopogon ruscifolius, Baeckea frutescens, Exocarpos latifolius,<br />
Melaleuca viridiflora, Alyxia spicata, Banksia dentata <strong>and</strong> Lom<strong>and</strong>ra banksii features in the<br />
groundcover. The floristic similarities to VC8b must be recognised, although VC14i represents a<br />
generally lower, shrubbier version on residual s<strong>and</strong> rather than recent fluvial deposits as in VC8b.<br />
The associated l<strong>and</strong>form is severely leached humic s<strong>and</strong> which forms low rises above an<br />
erosional plain. As discussed in Section 5.1.5, the provenance of these low s<strong>and</strong> rises is<br />
uncertain, possibly representing old dunes or remnant fluvial deposits.<br />
5.2.53 <strong>Regional</strong> Ecosystem 3.5.23x1<br />
Photograph 110. <strong>Vegetation</strong><br />
Community 14i on residual s<strong>and</strong><br />
rise. Site MO25.<br />
Description: Eucalyptus tetrodonta ± Corymbia nesophila ± C. clarksoniana woodl<strong>and</strong> on<br />
undulating rises.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5k, 5j<br />
Reference Sites: 4 Quaternary (Muralug)<br />
<strong>Regional</strong> Ecosystem 3.5.23x1 is represented by two VC’s, with occurrences restricted to Muralug<br />
Isl<strong>and</strong>.<br />
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<strong>Vegetation</strong> Community 5j: <strong>Vegetation</strong> Community 5j represents a tall open forest, with a<br />
canopy height range of 23 to 35m, dominated by Eucalyptus tetrodonta <strong>and</strong> Corymbia nesophila.<br />
The sub-canopy, which attains a height of 18m is dominated by Corymbia stockeri subsp.<br />
peninsularis. Typical species of the upper shrub layer include Xylomelum scottianum, Acacia<br />
platycarpa, Persoonia falcata, P<strong>and</strong>anus spiralis, Grevillea parallela while the sparse lower<br />
shrub layer comprises Alyxia spicata, Jacksonia thesioides, Parinari nonda, Acacia leptocarpa<br />
<strong>and</strong> Syzygium suborbiculare. This community occupies low residual s<strong>and</strong> rises which are<br />
scattered across the coastal plain on Muralug Isl<strong>and</strong> with the community description coming from<br />
SitePWQ25. The community is illustrated in Photograph 111.<br />
<strong>Vegetation</strong> Community 5k: <strong>Vegetation</strong> Community 5k occupies remnant alluvial terraces in<br />
scattered locations on Muralug. It is similar to VC5j, although the canopy is typically lower, <strong>and</strong><br />
Eucalyptus tetrodonta is sparsely scattered or absent. The dominant canopy is composed of<br />
Corymbia nesophila <strong>and</strong> Corymbia stockeri subsp. peninsularis which generally form an open<br />
forest, <strong>and</strong> occasionally woodl<strong>and</strong> in some locations <strong>and</strong> Erythrophleum chlorostachys, Corymbia<br />
novoguinensis <strong>and</strong> Corymbia tessellaris in some locations. Parinari nonda often forms a subcanopy<br />
dominant with typical shrubs in a sparse understorey being layer Neofabricia myrtifolia,<br />
Melaleuca viridiflora, Banksia dentata, Acacia simsii <strong>and</strong> Jacksonia thesioides. Representation<br />
is provided in Photograph 112.<br />
Photograph 111. Woodl<strong>and</strong> VC5j<br />
on remnant alluvial terrace.<br />
Photograph 112. Low s<strong>and</strong> rise on<br />
Muralug supporting Eucalyptus<br />
tetrodonta <strong>and</strong> Corymbia nesophila<br />
open forest, Site PWQ25.<br />
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5.2.54 <strong>Regional</strong> Ecosystem 3.5.29<br />
Description: Sorghum plumosum var. plumosum ± Themeda arguens closed tussock grassl<strong>and</strong><br />
on erosional plains.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 17d<br />
Reference Sites: 1 Quaternary (MO86)<br />
<strong>Vegetation</strong> Community 17d: Grassl<strong>and</strong> community 17d represents the generic grassl<strong>and</strong> type<br />
on a range of L<strong>and</strong> Zone associations. On LZ5, Moa Isl<strong>and</strong> provides for the only representation.<br />
The community (at MO86) is dominated by Themeda tri<strong>and</strong>ra <strong>and</strong> Heteropogon triticeus with a<br />
range of emergent shrubs, the most prominent being Planchonia careya, Cycas badensis,<br />
Parinari nonda <strong>and</strong> Cochlospermum gillivraei. The grassl<strong>and</strong> is a fire climax community, with<br />
scattered vine forest remnants clumped on low granite mounds which protrude above the<br />
undulating s<strong>and</strong> plain, offering some protection from fire. It should be noted that this grassl<strong>and</strong><br />
community has been stable for long periods <strong>and</strong> its extent has changed little in the past 35 years,<br />
based on the 1974 photographs which were used to assist the mapping exercise.<br />
5.2.55 <strong>Regional</strong> Ecosystem 3.5.32 (New RE)<br />
Photograph 113. Grassl<strong>and</strong><br />
community 17d on undulating s<strong>and</strong>y<br />
plain, Site MO86, Moa Isl<strong>and</strong>.<br />
Preliminary Description: Asteromyrtus brassii + Syzygium angophoroides + Acmena<br />
hemilampra subsp. hemilampra open forest. Residual s<strong>and</strong> rises <strong>and</strong> sheets.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 9a<br />
Reference Sites: 1 Secondary (MO29), 2 Quaternary.<br />
<strong>Vegetation</strong> Community 9a: This community is expressed on Moa Isl<strong>and</strong> where it presents a<br />
number of discontinuous, broadly linear occurrences across a broad erosional plain.<br />
Asteromyrtus brassii, Syzygium angophoroides, Acmena hemilampra subsp. hemilampra, Acacia<br />
crassicarpa <strong>and</strong> Melaleuca quinquenervia form the dominant canopy constituents of an open<br />
forest community with a canopy height range of 15m to 20m. The sub-canopy <strong>and</strong> shrub layers<br />
tend to merge ranging in height from 2m to 10m comprising Leucopogon ruscifolius, Exocarpos<br />
latifolius, Lithomyrtus obtusa, Livistona muelleri, Acacia crassicarpa, Polyscias australiana,<br />
Breynia oblongifolia, Baeckea frutescens, Alyxia spicata, Lophostemon suaveolens, Dillenia<br />
alata, Banksia dentata, P<strong>and</strong>anus sp., Endi<strong>and</strong>ra glauca, <strong>and</strong> Myrsine urceolata. The ground<br />
cover is dominated by Lom<strong>and</strong>ra banksii.<br />
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This community presents some difficulty for classification in a l<strong>and</strong>form sense. The low s<strong>and</strong>y<br />
rises that it occupies are scattered across a broader erosional surface <strong>and</strong> their provenance is not<br />
clear. It is considered that these features may represent relict beach ridges, although their<br />
morphology has been degraded to a degree that confirmation of this is not possible. The low rises<br />
also support forest communities that are atypical of degraded dune systems examined in other<br />
locations, more typically occupied by stunted shrubl<strong>and</strong>s. That the vegetation community<br />
comprises species typically associated with swampl<strong>and</strong>s is also puzzling when it is considered<br />
that the ridges are elevated above the surrounding erosional plain <strong>and</strong> provide reasonable<br />
drainage. Given that the surrounding l<strong>and</strong>form is erosional presents the possibility that these<br />
features are the result of a topographic reversal <strong>and</strong> the forest communities represent former<br />
swampl<strong>and</strong>s on a previous depositional surface. The species composition of the forest gives<br />
some support to this possibility. Without the ability to positively identify these features, they<br />
have been classified with the broader erosional plain as LZ5 features. A new RE is proposed to<br />
accommodate this community under the preliminary classification of RE3.5.4x6.<br />
5.2.56 <strong>Regional</strong> Ecosystem 3.7.1x1b<br />
Photograph 114. Open forest<br />
dominated by Asteromyrtus brassii<br />
<strong>and</strong> Syzygium angophoroides (VC9a)<br />
at Site MO108.<br />
Description: Closed semi-deciduous mesophyll vine forest. Mainly occurs on loamy alluvia.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 2e<br />
Reference Sites: 2 Quaternary<br />
<strong>Vegetation</strong> Community 2e: The lateritic profile that provides an elevated base for the Saibai<br />
Isl<strong>and</strong> township presents a significant puzzle in respect to pre-clearing vegetation association.<br />
With out any similar examples of lateritic profiles in the study area, let alone a fully vegetated<br />
one, the pre-clearing l<strong>and</strong>scape can only be re-constructed from remnants associated with this<br />
l<strong>and</strong>form. It should also be considered that with the considerable history of traditional occupation,<br />
the vegetated l<strong>and</strong>scape has most likely undergone a number of transformations in an area that<br />
was central to pre-european occupation. The only remnant of native vegetation on the laterite<br />
plateau exists in the form of a scrubby vine thicket community, mapped as L2e, which has been<br />
reduced to two marginal slivers along the access road to the Saibai cemetery. These slivers<br />
comprise a low semi-deciduous vine thicket with canopy species represented by Thespesia<br />
populneoides, Terminalia subacroptera, Cathormion umbellatum subsp. monoliforme,<br />
Dendrolobium umbellatum, Intsia bijuga, Hibiscus tiliaceus, Manilkara kauki, Milletia pinnata,<br />
Cordia subcordata <strong>and</strong> Lysiphyllum bipinnata.<br />
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That this community is marginal to estuarine wetl<strong>and</strong> communities is manifest in the prominence<br />
of a deciduous mangrove species (Excoecaria agallocha) in the canopy. The central areas of this<br />
l<strong>and</strong>form were likely to have formed a much better developed thicket community than is<br />
represented in contemporary remnants, with a prominence of species including Terminalia<br />
subacroptera <strong>and</strong> Acacia auriculiformis. It is possible that clues to the original floristic<br />
composition of this l<strong>and</strong>form may be present on the mainl<strong>and</strong> PNG coastline, although no such<br />
communities are documented in available literature. Although highly degraded <strong>and</strong> extremely<br />
limited in size, the continuity with adjacent remnant estuarine l<strong>and</strong>scapes affords this community<br />
remnant status. This community has been assigned to a preliminary RE classification based on<br />
Herbarium recommendations. Further review into the bio-regional occurrence of this RE is<br />
required.<br />
5.2.57 <strong>Regional</strong> Ecosystem 3.8.4b<br />
Photograph 115. Remnants of vine<br />
thicket community 2e reduced to<br />
narrow slivers on roadside margins.<br />
Description: Imperata cylindrica ± Mnesithea rottboellioides closed tussock grassl<strong>and</strong> on basalt<br />
vents & cones.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 17b, 17b(e)<br />
Reference Sites: 3 Secondary (ER006, ER021, MU030), 13 Quaternary<br />
Native grassl<strong>and</strong>s form a considerable portion of the major basaltic isl<strong>and</strong>s, <strong>and</strong> these are<br />
represented as RE3.8.4b, in recognition of their geographic seperation from basaltic grassl<strong>and</strong>s in<br />
the south of the bioregion. Some floristic variation from the type description is present in the<br />
surveyed communities.<br />
Grassl<strong>and</strong>s on Erub Isl<strong>and</strong> extend from the upper slopes to the coastal margins <strong>and</strong> form a broad<br />
complex with vine forest communities which are generally restricted to gully lines <strong>and</strong> sheltered<br />
locations. Two secondary sites were surveyed on Erub (ER06 <strong>and</strong> ER021), both of these located<br />
on basaltic coastal headl<strong>and</strong>s <strong>and</strong> both were dominated by Themeda tri<strong>and</strong>ra achieving between<br />
70-80% cover. Additional groundcover species are *Passiflora foetida, Anisomeles malabarica,<br />
Cissus maritima, Ipomoea pes-capre subsp. brasiliensis, <strong>and</strong> Jacquemontia paniculata. Scattered<br />
low stunted shrubs of Wrightia pubescens subsp. penicillata, Litsea glutinosa, Morinda citrifolia<br />
<strong>and</strong> Flueggea virosa subsp. melanthesoides may occur with occasional emergents of<br />
Barringtonia calyptrata to 10m. Lantana is usually abundant on margins often within emerging<br />
shrubl<strong>and</strong>s dominated by Macaranga tanarius.<br />
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Away from the coastal headl<strong>and</strong>s Imperata cylindrica was often the dominant species <strong>and</strong> the<br />
tendency for it to mosaic with Themeda tri<strong>and</strong>ra meant that differentiation based on species<br />
composition could not be completed with any degree of confidence. As such, VC17b describes a<br />
mosaic of grassl<strong>and</strong> species which may include Themeda tri<strong>and</strong>ra, Imperata cylindrica <strong>and</strong><br />
Mnesithea rottboellioides, restricted to basic volcanic rock types.<br />
Photograph 116. <strong>Vegetation</strong><br />
Community 17b with dominant<br />
Themeda tri<strong>and</strong>ra (Site ER021, Erub<br />
Isl<strong>and</strong>).<br />
Secondary level survey was completed at sites considered from on ground examination to be in<br />
good condition, however data from a number of additional Quaternary sites indicate the general<br />
condition of the grassl<strong>and</strong> on Erub to be extremely variable. Large areas, generally on the<br />
margins of vine forest communities are dominated by Lantana camara where they are mapped as<br />
VC17b(e), or have been invaded by a range of colonising native shrubs where they have been<br />
represented as VC17b(r). Typical regenerating species include Micromelum minutum, Litsea<br />
glutinosa, Cupaniopsis anacardioides, Wrightia pubescens subsp. penicillata, Melicope<br />
peninsularis, Flagellaria indica, Jacquemontia paniculata, Annonaceae (DGF8739+), Abutilon<br />
sp., Rubiaceae (DGF8741+), Thespesia populneoides, Ficus opposita, Barringtonia racemosa,<br />
Atalaya sericopetala, Tabernaemontana orientalis, Morinda citrifolia, Clerodendron sp. <strong>and</strong><br />
Garuga floribunda var. floribunda. Exotics such as *Senna alata, *Calopogonium mucunoides,<br />
*Sida retusa, *Sida rhombifolia, *Macroptilium atropurpurea, *Clitoria ternata <strong>and</strong> *Bambusa<br />
spp. are frequent.<br />
Considerable areas have also been subject to severe topsoil erosion which has thinned the ground<br />
cover <strong>and</strong> these areas are represented as VC17b(s). In all cases, these communities have been<br />
represented with remnant status. In the case of VC17b(e) <strong>and</strong> VC17b(s) remnant status has been<br />
recognised given that an applied l<strong>and</strong> management practice (i.e. appropriate fire regimes) is<br />
capable of quickly re-establishing natural condition.<br />
Native grassl<strong>and</strong> communities on Mer Isl<strong>and</strong> were similar to those on Erub although they<br />
generally demonstrated considerably more species diversity. At Site MU030, groundcover<br />
composition was as follows; Mnesithea rottboellioides (40%), Themeda tri<strong>and</strong>ra (21%),<br />
Imperata cylindrica (19%), Ipomoea pes-capre subsp. brasiliensis (13%), Premna dallachyana<br />
(4%), Anisomeles malabrica (2%), Desmodium sp. (DGF8812+) (1%), Wedelia biflora (
Photograph 117. Grassl<strong>and</strong><br />
community V17b on Mer Isl<strong>and</strong> with<br />
emergent shrubs prominent<br />
(MU030).<br />
The literature suggests considerable conjecture about the provenance of grassl<strong>and</strong>s on these<br />
isl<strong>and</strong>s. Draffan et al. (1983) in Freebody (2002), <strong>and</strong> Stocker (1978), refer to the use of fire in<br />
vine forest areas (with a closed canopy) on Erub <strong>and</strong> Mer Isl<strong>and</strong>s causing habitat alteration <strong>and</strong> a<br />
reduction of the total area of closed forest to fire climax grassl<strong>and</strong>s. The results of this study<br />
however indicate that the grassl<strong>and</strong> community on Mer occupies a cinder cone, which imposes<br />
unique edaphic conditions on vegetation communities in the form of extreme drainage. The<br />
considerable number of volcanic vents <strong>and</strong> basalt regolith on Australia’s north-eastern region that<br />
naturally support grassl<strong>and</strong>s in much wetter or similar climates (e.g. Seven Sisters near<br />
Yungaburra, Mount Fox <strong>and</strong> Clump Point in Queensl<strong>and</strong>’s wettest coastal location), offer<br />
evidence to suggest that the grassl<strong>and</strong>s on these isl<strong>and</strong>s were not necessarily preceded by vine<br />
forest. The extremely fresh nature of many of the volcanic structures apparent on the Dauar<br />
Cone, <strong>and</strong> to lesser extent the Mer Cone, largely disproves any theory of rainforest succession to<br />
grassl<strong>and</strong>. Historical annotations by Haddon (1901) provide clear evidence that the l<strong>and</strong>scape<br />
dynamic has changed little in the period of European influence. An extract from Haddon quotes<br />
“the cresentic valley, crater, or “big valley” Aupaut, being formed in a porous volcanic ash, is<br />
somewhat arid; the vegetation consists of coarse grass, low scrub <strong>and</strong> scattered coconut palms<br />
<strong>and</strong> presents a marked contrast to the remainder of the isl<strong>and</strong>; the steep slopes are unusually<br />
bare” (Haddon 1901 Part 1, Chapter 3, pp30).<br />
Similarly, the argument that Erub (<strong>and</strong> Mer) once supported a blanketing vine forest community<br />
that was cleared <strong>and</strong> burnt to produce the grassl<strong>and</strong> mosaic that is apparent in today’s l<strong>and</strong>scape<br />
is questionable. Whilst there is no doubt that fire controls vine forest distribution to a<br />
considerable extent, ecotonal changes upslope along gully lines from tall vine forest (VC2k) to<br />
vine thicket (VC2w), to grassl<strong>and</strong> (VC17b) observed during the study indicates the considerable<br />
role the natural environment plays in vine forest distribution. It is unlikely that the upper slopes<br />
of Erub ever supported luxuriant vine forest due to the relative dryness of the climate <strong>and</strong> the<br />
extreme soil drainage on these upper slope areas. It should thus be stated that whilst removal of<br />
fire as a l<strong>and</strong> management tool may not have any marked effect long term effect on vine forest<br />
distribution, it will certainly result in considerable degredation of these restricted grassl<strong>and</strong><br />
communities through lantana invasion. Very hot late dry season fires burnt upslope are likely to<br />
cause a retreat of vine forest margins with subsequent invasion by lantana.<br />
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5.2.58 <strong>Regional</strong> Ecosystem 3.8.5 (New RE)<br />
Description: Preliminary Description; Semi deciduous <strong>and</strong> Deciduous Notophyll Vine Forest.<br />
Basaltic Isl<strong>and</strong>s of the Torres Strait.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 2i, 2j, 2k, 2w, 15a, 21a, 22a<br />
Reference Sites: 10 Secondary (ER02, MU11, MU01, ER44, ER20, ER12, ER11, ER34, MU09,<br />
ER45), 74 Quaternary.<br />
RE 3.8.5 describes vine forests formed on basalt, typical of the Torres Strait Eastern Isl<strong>and</strong> Group<br />
including Mer, Erub, <strong>and</strong> Ugar Isl<strong>and</strong>s. A new RE classification (RE3.8.5) is provided in<br />
recognition of their unique structural <strong>and</strong> floristic characterics, distinct from basaltic vine forests<br />
typical of mainl<strong>and</strong> areas. This is a variable grouping <strong>and</strong> the degree of floristic <strong>and</strong> structural<br />
variation warrants a range of RE sub-types to be described. Six sub-types are described under the<br />
classifications of VC2i, VC2j, VC2k, VC2w <strong>and</strong> VC15a. The Endangered shrub <strong>and</strong> small tree<br />
Alectryon rep<strong>and</strong>odentatus is previously known from four Queensl<strong>and</strong> Herbarium collections on<br />
Mer <strong>and</strong> also from semi deciduous mesophyll vine forest at Lockerbie, Cape York (L<strong>and</strong>sberg<br />
<strong>and</strong> Clarkson 2004). Survey records indicate that it is a very common species that is pervasive in<br />
both canopy <strong>and</strong> sub-canopy layers throughout this regional ecosystem, on both Mer <strong>and</strong> Erub. It<br />
also occurs in VC1a on Dauan Isl<strong>and</strong>. A highly disjunct population of Chrysophyllum roxburgii<br />
previously noted on the isl<strong>and</strong> by Freebody (2002) was vouchered during the survey. The species<br />
was not recorded elsewhere on the isl<strong>and</strong>. A disjunct population of Canarium vitiense was also<br />
recorded on Erub from this RE.<br />
<strong>Vegetation</strong> Community 2i: The initial sub-type is represented by VC2i, classified as RE3.8.5a<br />
(based on Herbarium advice), which occurs on the steep basaltic escarpments on Erub Isl<strong>and</strong>.<br />
This community is a thicket, with canopy heights ranging from 6 to 10m, <strong>and</strong> emergents to 15m.<br />
The dominant canopy comprises (in order of decreasing dominance) Berrya javanica,<br />
Cupaniopsis anacardioides, Diospyros hebecarpa, Aglaia elaeagnoidea, Melicope peninsularis,<br />
Bombax ceiba var. leiocarpum, Drypetes deplanchei, Mimusops elengi <strong>and</strong> Manilkara kauki. The<br />
sole emergent species is typically Bombax ceiba var. leiocarpum. This is a restricted community<br />
limited to a number of steep sheltered gully lines <strong>and</strong> coastal escarpments where some protection<br />
from fire is afforded.<br />
Photograph 118. Notophyll vine<br />
thicket type 2i on a steep basaltic<br />
escarpment at Site ER013.<br />
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<strong>Vegetation</strong> Community 2j: <strong>Vegetation</strong> Community 2j is the dominant vine forest type on both<br />
Mer <strong>and</strong> Erub Isl<strong>and</strong>s, <strong>and</strong> is also represented under the sub-unit of RE3.8.5a. The best<br />
representation is formed on gentle basalt slopes to the north east of the airport on Erub where the<br />
community mixes with VC2k. Well-preserved remnants of this community were difficult to find<br />
on Mer, although the best type example was located adjacent to the workers accommodation at<br />
Site MU01 where the canopy <strong>and</strong> internal forest structure was surprisingly well-preserved. In<br />
this location, a general canopy height range of 15m to 18m was typical with emergents reaching<br />
28m. The canopy species comprised Bombax ceiba var. leiocarpum, Diospyros hebecarpa,<br />
Alectryon rep<strong>and</strong>odentatus (E), Adenanthera pavonina, Wrightia pubescens subsp. penicillata,<br />
<strong>and</strong> Antiaris toxicaria var. macrophylla. Bombax ceiba var. leiocarpum always forms the<br />
emergent layer. On Erub Isl<strong>and</strong>, Cupaniopsis anacardioides forms a dominant to co-dominant<br />
canopy species with Diospyros hebecarpa (refer to Site ER12). It is therefore considered unusual<br />
that this species is not recorded as either a canopy or sub-canopy species on Mer. The typical<br />
canopy structure of this VC is highly broken, often with significant canopy gaps extending to<br />
near ground level. The uneven nature of this canopy can only be attributed to disturbance in<br />
some form, possible with extreme wind as a major contributing factor.<br />
<strong>Vegetation</strong> Community 2k: <strong>Vegetation</strong> community 2k, represented by RE sub-unit 3.8.5b, was<br />
sampled to secondary level at Site ER011 <strong>and</strong> represents the maximum development of vine<br />
forest observed on the basaltic isl<strong>and</strong>s. This tall deciduous forest formation is restricted to Erub<br />
Isl<strong>and</strong> where it occupies sheltered pockets, generally within broader areas of VC2j. The canopy,<br />
which typically ranges from 25m to 38m, has an open feel due to the deciduous canopy although<br />
measured crown cover is typically > 80%. The dominant canopy species (in order of decreasing<br />
dominance) are Gyrocarpus americanus, Cathormion umbellatum subsp. monoliforme, Garuga<br />
floribunda var. floribunda, Antiaris toxicaria var. macrophylla, Mimusops elengi, Wrightia<br />
laevis, Diospyros hebecarpa <strong>and</strong> Bombax ceiba var. leiocarpum. The sub-canopy is relatively<br />
open (30 – 50%) with dominant species including Diospyros hebecarpa, Celtis philippensis,<br />
Alectryon rep<strong>and</strong>odentatus (E) <strong>and</strong> Manilkara kauki.<br />
Photograph 119. The best<br />
development of VC2j on Murray<br />
Isl<strong>and</strong> at Site MU01.<br />
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Photograph 120. Tall deciduous<br />
vine forest community 2k at site<br />
ER011 on Erub Isl<strong>and</strong>. The<br />
prominent tree is Gyrocarpus<br />
americanus.<br />
<strong>Vegetation</strong> Community 2w: Deciduous vine thicket on basalt is characterised by VC2w,<br />
occurring on both Erub <strong>and</strong> Mer Isl<strong>and</strong>s. A separate sub-typing of RE3.8.5c is used to describe<br />
this distinctive community which is associated with exposed basaltic escarpments on Erub <strong>and</strong><br />
Maer Isl<strong>and</strong>s. The community forms a canopy with a height range of 6m to 8m that is typified by<br />
species similar to VC2k described above. Besides an obvious difference in canopy height, the<br />
distinction between VC2k <strong>and</strong> VC2w is also an ecological one, with VC2w typically on drier<br />
sites such as steep exposed escarpments or as narrow attenuations upslope along gully lines<br />
within broader grassl<strong>and</strong> communities. Canopy species include Antiaris toxicaria var.<br />
macrophylla, Garuga floribunda var. floribunda, Gyrocarpus americanus, Terminalia<br />
subacroptera <strong>and</strong> scattered Bombax ceiba var. leiocarpum. The sparse sub-canopy comprises<br />
Cleistanthus peninsularis, Drypetes deplanchei, Eugenia reinwardtiana, <strong>and</strong> Alectryon<br />
rep<strong>and</strong>odentatus (E). Ground cover comprises abundant slender vines <strong>and</strong> low shrubs which<br />
form a sparse cover over a substrate typically composed of basalt talus.<br />
Photograph 121. Vine thicket type<br />
2w at site ER34 with the deciduous<br />
nature of the canopy clearly evident.<br />
<strong>Vegetation</strong> Community 15a: <strong>Vegetation</strong> community 15a represents a complex of vine thicket<br />
<strong>and</strong> low open forest mapped on the steep south-eastern basaltic escarpment of Mer. The<br />
components, which comprise vine thicket type 2w <strong>and</strong> an undescribed low open forest of<br />
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P<strong>and</strong>anus sp, contribute roughly equal portions to the complex which was left undifferentiated<br />
due to limitations with photographic scale <strong>and</strong> the steep slopes which made remote interpretation<br />
<strong>and</strong> accurate representation extremely difficult. The vine thicket component VC2w has been<br />
previously described although in this situation, P<strong>and</strong>anus sp. may form a minor component of the<br />
canopy <strong>and</strong> the sub-canopy is typically dominated by evergreen species with Manilkara kauki<br />
particularly prominent. P<strong>and</strong>anus sp. forms the canopy of the low open forest component,<br />
accompanied by occasional trees which include Hibiscus tiliaceus, <strong>and</strong> Barringtonia calyptrata.<br />
The relatively even canopy is occasionally interrupted by emergent trees such as Bombax ceiba<br />
var. leiocarpum. This is a community that has been shaped by extreme environmental conditions,<br />
clearly evident in the strongly windswept crowns of the vine thicket complex component, which<br />
occupies the more exposed positions on the escarpment. The vegetation complex is represented<br />
under the sub-type classification of RE 3.8.5e.<br />
Photograph 122. Vine thicket<br />
component (VC2w) of the coastal<br />
headl<strong>and</strong> complex type VC15a.<br />
Photograph 123. Low open forest<br />
of P<strong>and</strong>anus sp. which forms<br />
component of VC15a on Mer.<br />
<strong>Vegetation</strong> Community 21a: Successional forests are recognised in sheltered positions on the<br />
western portion of Mer Isl<strong>and</strong>, occupying gully lines incised into the main cinder cone. This<br />
community forms a dense thicket to low closed forest, generally with canopy heights in the 6m to<br />
12m range, with dominant upper stratum species including Cerbera manghas, Macaranga<br />
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tanarius, Hibiscus tiliaceus, Mangifera indica, Barringtonia calyptrata, Myristica insipida,<br />
Pouteria obovata, Alstonia spectabilis, Premna dallachyana with vines such as Mucuna gigantea<br />
<strong>and</strong> Entada phaseoloides. Bombax ceiba var. leiocarpum may be present as a sparse emergent in<br />
the more advanced successional stages. The development of these communities is controlled by<br />
both fire <strong>and</strong> edaphic conditions. It should also be noted that whilst the climax stage of this VC is<br />
possibly VC2j, the extreme drainage conditions imposed by the porous cinder substrate is likely<br />
to limit successional forest development <strong>and</strong> it is expected that even advanced successional stages<br />
are likely to be extremely depauperate both in stature <strong>and</strong> floristics. Cessation of regular burning<br />
will possibly facilitate the expansion of depauperate thickets at the expense of grassl<strong>and</strong>s. The<br />
contemporary fire regimes of the isl<strong>and</strong> were not discussed in detail with the local community.<br />
Evidence from historical photographs (1988) indicates that these communities are in a state of<br />
relative stability. The timing <strong>and</strong> intensity of fires is an important l<strong>and</strong> management issue<br />
requiring additional investigation in relevance to the management of invase weeds particularly<br />
Lantana. This community is represented as RE sub-type 3.8.5d.<br />
5.2.59 <strong>Regional</strong> Ecosystem 3.12.4<br />
Photograph 124. Early stage<br />
successional forest on Mer Isl<strong>and</strong><br />
forming a low closed thicket with<br />
dominant Macaranga tanarius.<br />
Description: Notophyll vine forest of Welchiodendron longivalve on Torres Strait Isl<strong>and</strong>s.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 4a, 4b, 4c, 1d, 17h (co)<br />
Reference Sites: 3 Secondary (MO003, MA030, MA043)<br />
<strong>Regional</strong> Ecosystem 3.12.4 is an endemic yet extensive community in the study area occurring on<br />
granite <strong>and</strong> rhyolite hillslopes <strong>and</strong> footslopes, reaching its northern limits on Gebar Isl<strong>and</strong> in the<br />
Central Isl<strong>and</strong> Group.<br />
<strong>Vegetation</strong> Community 4a: <strong>Regional</strong> Ecosystem 3.12.4 is formed dominantly by VC4a, which<br />
is represented in the coverage as sub-type RE3.12.4a. This VC is an amalgam of two forest types<br />
that, due to frequency of variation <strong>and</strong> similarity in photographic signature, could not be<br />
differentiated with confidence on either aerial photography or satellite imagery. The canopy<br />
height of VC4a is highly variable, although generally ranging from 8 to 20m. The dominant<br />
floristic component is Welchiodendron longivalve although this species mixes to varying degrees<br />
with a range of vine forest species. On Moa <strong>and</strong> Muralug Isl<strong>and</strong>s, Welchiodendron longivalve<br />
closed forest <strong>and</strong> semi-deciduous vine forest communities form mosaics that separate into<br />
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distinctive structural components. On Mabuiag <strong>and</strong> Hammond Isl<strong>and</strong>s, Welchiodendron forms a<br />
canopy with evergreen species <strong>and</strong> this grouping has also been included in VC4a. A<br />
representative assemblage of canopy species in this VC includes Welchiodendron longivalve as a<br />
dominant to sub-dominant species with Acacia polystachya, Endi<strong>and</strong>ra glauca, Canarium<br />
australianum, Psydrax sp. (DGF8884+), Syzygium bungadinnia, Dysoxylum oppositifolium,<br />
Alphitonia excelsa, Sterculia quadrifida, Parinari nonda, Canarium australianum, Pouteria<br />
sericea, Gyrocarpus americanus, Drypetes deplanchei <strong>and</strong> Bombax ceiba var. leiocarpum.<br />
<strong>Vegetation</strong> Community 4b: <strong>Vegetation</strong> Community 4b forms a low woodl<strong>and</strong> variant of this<br />
RE with typical examples on Gebar <strong>and</strong> Mabuiag with a well-developed grassy ground cover.<br />
Small areas on Moa Isl<strong>and</strong> where Welchiodendron mixes with Melaleuca dealbata on loamy<br />
granite slopes are represented as VC4c. The RE also forms a component of vegetation grassl<strong>and</strong><br />
complex 17h. <strong>Vegetation</strong> Community 17h represents a grassl<strong>and</strong> complex behind St Paul’s<br />
Village (Moa Isl<strong>and</strong>) where, through the process of repetitive burning, Welchiodendron dominant<br />
open forest has retreated into sheltered pockets along gully lines within a broader grassl<strong>and</strong><br />
community.<br />
Photograph 125. Welchiodendron<br />
longivalve dominant closed forest on<br />
Mabuiag Isl<strong>and</strong> (MA003).<br />
Photograph 126. Low<br />
Welchiodendron longivalve<br />
dominant woodl<strong>and</strong> on acid volcanic<br />
footslopes (VC4b-Gebar Isl<strong>and</strong>).<br />
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<strong>Vegetation</strong> Community 1d: <strong>Vegetation</strong> Community 1d, represented in the mapping as sub-type<br />
RE13.12.4b, is a variation restricted to the Torres Strait Isl<strong>and</strong>s. The community occupies<br />
sheltered gully lines, most abundantly on Mabuiag Isl<strong>and</strong>, although scattered occurrences have<br />
been mapped on Gebar <strong>and</strong> Warral Isl<strong>and</strong>s. Only the Mabuiag Isl<strong>and</strong> forests have been<br />
adequately ground truthed <strong>and</strong> classification of this community on other isl<strong>and</strong>s is based largely<br />
on l<strong>and</strong>scape position <strong>and</strong> photographic signatures. The canopy is relatively even, ranging from<br />
18 to 25m, <strong>and</strong> canopy cover is greater than 80%.<br />
Evergreen species dominate the canopy with a minor deciduous component present in some<br />
locations. Typical canopy species in order of decreasing dominance include Endi<strong>and</strong>ra glauca,<br />
Syzygium bungadinnia, Buchanania arborescens, Acacia polystachya, Dysoxylum oppositifolium,<br />
Canarium australianum, Pouteria sericea, Sterculia quadrifida, Schefflera actinophylla,<br />
Myristica insipida, Carallia brachiata, Clerodendron sp., Rhodomyrtus macrocarpa,<br />
Cryptocarya exfoliata, *Mangifera indica, Calophyllum sil, Elaeodendron melanocarpum,<br />
Terminalia subacroptera <strong>and</strong> Maranthes corymbosa. The sub-canopy ranges in height from 10 to<br />
15m <strong>and</strong> includes species otherwise typical of the canopy, plus several additional species<br />
including Chionanthus ramiflora, Arytera bifoliolata, Cryptocarya exfoliata <strong>and</strong> Pouteria<br />
obovata. Ground cover is typically sparse, with abundant rock talus <strong>and</strong> scattered epiphytes<br />
dominated by Drynaria quercifolia. The community merges upslope from gully walls into<br />
Welchiodendron <strong>and</strong> Acacia polystachya dominant open forest.<br />
5.2.60 <strong>Regional</strong> Ecosystem 3.12.8<br />
Photograph 127. The distinctive<br />
bark of Syzygium bungadinnia which<br />
is a prominent canopy component of<br />
VC1d.<br />
Description: Corymbia clarksoniana ± C. tessellaris open forest on coastal ranges <strong>and</strong> lowl<strong>and</strong>s.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5b, 5s, 5e<br />
Reference Sites: 28 Quaternary<br />
<strong>Regional</strong> Ecosystem 3.12.8 is represented by VC5b, VC5s <strong>and</strong> VC5e. <strong>Vegetation</strong> Community 5b<br />
forms the dominant woodl<strong>and</strong> <strong>and</strong> open forest type on footslopes <strong>and</strong> colluvial slopes of Moa<br />
Isl<strong>and</strong>. <strong>Vegetation</strong> Community 5s on granitic l<strong>and</strong>forms is relatively more restricted, occurring<br />
most abundantly on Hammond Isl<strong>and</strong> of the Inner Isl<strong>and</strong> Group.<br />
<strong>Vegetation</strong> Community 5b: The typical structure of VC5b is woodl<strong>and</strong> <strong>and</strong> occasional open<br />
forest with canopy heights ranging from 23 to 27m. Corymbia clarksoniana forms the dominant<br />
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canopy species in most locations, accompanied by a mixed range of Corymbia spp. including<br />
Corymbia dallachyana, C. tessellaris, C. novoguinensis <strong>and</strong> C. nesophila. Welchiodendron is<br />
locally abundant, although it is more commonly a sub-canopy tree, <strong>and</strong> Melaleuca dealbata<br />
reaches the canopy in some locations. Dense groves of Cycas badensis form a prominent shrub<br />
layer in some locations, particularly on colluvial slopes <strong>and</strong> ground cover is typically grassy with<br />
Heteropogon triticeus <strong>and</strong> Themeda tri<strong>and</strong>ra the dominant species.<br />
<strong>Vegetation</strong> Community 5s: <strong>Vegetation</strong> Community 5s on granitic footslopes presents a more<br />
typical expression of RE3.12.8 than VC5b. The community forms woodl<strong>and</strong> to open forest with<br />
canopy heights ranging from 23 to 27m. Corymbia clarksoniana dominates the canopy with<br />
Corymbia tessellaris forming a sub-dominant canopy component. Sub-canopy <strong>and</strong> shrub layers<br />
are typically sparse <strong>and</strong> ground cover is grassy with dominant Themeda tri<strong>and</strong>ra. Similar to its<br />
occurrence on alluvial soils, VC5s is associated with more fertile edaphic conditions, <strong>and</strong><br />
occupies diorite footslopes where it occurs on Hammond Isl<strong>and</strong>.<br />
Photograph 128. A typical<br />
expression of VC5b on granitic<br />
footslopes of Moa Isl<strong>and</strong>.<br />
Photograph 129. Woodl<strong>and</strong><br />
community 5s on diorite footslope.<br />
Hammond Isl<strong>and</strong> Site HA18.<br />
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<strong>Vegetation</strong> Community 5e: Windswept south-east facing slopes of Thursday Isl<strong>and</strong> provide the<br />
only representation of VC5e in the study area. The community forms a low open forest, typically<br />
with a windswept even canopy structure with an average height of 15m. Corymbia clarksoniana<br />
forms the dominant canopy species, with Corymbia nesophila <strong>and</strong> Eucalyptus leptophleba subdominant.<br />
Welchiodendron longivalve occasionally reaches the canopy although it is more<br />
common as a sub-canopy tree. Livistona muelleri, Acacia leptocarpa <strong>and</strong> Deplanchea tetraphylla<br />
are associated canopy species although are they generally more common in the sub-canopy. The<br />
shrub layer is typically sparse comprising Acacia simsii <strong>and</strong> Pogonolobus reticulatus with ground<br />
cover dominated by sedges <strong>and</strong> tussock grasses<br />
5.2.61 <strong>Regional</strong> Ecosystem 3.12.9<br />
Photograph 130. Low open forest<br />
community 5e at Site TI08,<br />
Thursday Isl<strong>and</strong>.<br />
Description: Corymbia tessellaris, C. clarksoniana open forest. Occurs on coastal ranges.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5g, 5o<br />
Reference Sites: 13 Quaternary<br />
Limited floristic or structural sampling was undertaken in this RE, which is represented by VC’s<br />
5g <strong>and</strong> 5o. The communities occur most commonly on the inner group with mapped examples on<br />
Hammond, Warral <strong>and</strong> Muralug Isl<strong>and</strong>s.<br />
<strong>Vegetation</strong> Community 5g: <strong>Vegetation</strong> Community 5g (on granite lithologies) represents an<br />
open forest community with dominant Corymbia tessellaris often associated with<br />
Welchiodendron longivalve over a sparse sub-canopy of vine forest species. Vine forest species<br />
are generally dominated by Acacia polystachya, Syzygium suborbiculare, Parinari nonda,<br />
Carallia brachiata <strong>and</strong> deciduous vine forest species including Canarium australianum. Welldeveloped<br />
examples were observed on Warral Isl<strong>and</strong> where they dominated the footslope<br />
communities, merging upslope with Acacia polystachya <strong>and</strong> Welchiodendron longivalve<br />
dominant shrubl<strong>and</strong>s. Some good examples also occur on sheltered gully lines in the central<br />
portion of Muralug Isl<strong>and</strong>. Eucalyptus cullenii was associated with this community in a number<br />
of Muralug localities.<br />
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Photograph 131. Lighter coloured<br />
crowns of Corymbia tessellaris in<br />
VC5g forming a mosaic with vine<br />
forest community 2q on central<br />
portions of Muralug Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 5o: <strong>Vegetation</strong> community 5o (on granitoid lithologies) represents a<br />
much simpler community, typically a grassy open woodl<strong>and</strong> with a range of associated shrubl<strong>and</strong><br />
species including Grevillea parallela, P<strong>and</strong>anus sp. <strong>and</strong> Livistona muelleri. This community has<br />
most likely been heavily influenced by a frequent burning regime. <strong>Vegetation</strong> community 5o was<br />
sampled to quaternary level at Hammond Isl<strong>and</strong> Site HA009.<br />
5.2.62 <strong>Regional</strong> Ecosystem 3.12.11<br />
Photograph 132. Grassy woodl<strong>and</strong><br />
community VC5o on Hammond<br />
Isl<strong>and</strong> with dominant Corymbia<br />
tessellaris.<br />
Description: Corymbia stockeri subsp. peninsularis ± Welchiodendron longivalve woodl<strong>and</strong> on<br />
Torres Strait Isl<strong>and</strong>s.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5l, 5v, 14w(co), 14u(co)<br />
Reference Sites: 33 Quaternary<br />
<strong>Regional</strong> Ecosystem 13.12.11 is the dominant ecosystem on acid volcanic <strong>and</strong> granitic ranges of<br />
the Inner Isl<strong>and</strong> Group. The RE is formed by VC5l, which also forms components of the<br />
vegetation complex 14g.<br />
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<strong>Vegetation</strong> Community 5l: <strong>Vegetation</strong> Community 5l is typically a woodl<strong>and</strong> <strong>and</strong> occasionally<br />
open forest community with canopy heights generally ranging from 12m to 23m. The canopy is<br />
dominated by Corymbia stockeri subsp. peninsularis in the majority of occurrences although<br />
mixes with Eucalyptus cullenii, Eucalyptus tetrodonta <strong>and</strong> Corymbia nesophila occur on Muralug<br />
Isl<strong>and</strong>. Welchiodendron longivalve is a prominent sub-canopy <strong>and</strong> occasional canopy species.<br />
Shrub layers are typically sparse although Acacia brassii, Acacia leptocarpa, Welchiodendron<br />
longivalve, Cochlospermum gillivraei <strong>and</strong> Grevillea parallela are scattered throughout. Ground<br />
cover is formed by a mosaic of grasses <strong>and</strong> exposed acid volcanic rock with Imperata cylindrica<br />
<strong>and</strong> Heteropogon triticeus the dominant species. In complex type 14w, VC5l mosaics with<br />
shrubl<strong>and</strong>s of Acacia brassii <strong>and</strong> Welchiodendron longivalve although it has not been<br />
differentiated due to scale of complex variation. Minor areas of this RE are represented as VC5m<br />
on Horn Isl<strong>and</strong> where Melaleuca stenostachya forms a dense sub-canopy to Corymbia stockeri<br />
subsp. peninsularis.<br />
Photograph 133. Woodl<strong>and</strong><br />
structure of VC5l on Muralug Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 5v: This community is a relatively extensive VC restricted to granite<br />
hills <strong>and</strong> footslopes on Badu Isl<strong>and</strong>. Corymbia stockerii subsp. peninsularis forms the dominant<br />
canopy species with a height range of 20m to 28m. Welchiodendron longivalve is a co-dominant<br />
species, often separating into copses in sheltered location. Associated canopy species include<br />
Acacia polystachya <strong>and</strong> scattered Corymbia tessellaris. Welchiodendron longivalve forms the<br />
dominant sub-canopy species, mixing with Acacia polystachya, Terminalia subacroptera <strong>and</strong><br />
Psydrax banksii. Cycas badensis is a dominant shrub species on the footslopes. The natural<br />
variability in both the structure <strong>and</strong> floristic composition of the community is imposed by the<br />
irregularity of the granite boulder slopes on which the community has developed. The<br />
community remains poorly sampled due to access restrictions imposed during the field survey.<br />
More comprehensive vegetation survey on Badu would greatly benefit the description of this VC.<br />
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5.2.63 <strong>Regional</strong> Ecosystem 3.12.13<br />
Photograph 134. <strong>Vegetation</strong><br />
community 5v on Badu Isl<strong>and</strong>.<br />
Description: Corymbia nesophila ± C. hyl<strong>and</strong>ii subsp. peninsularis woodl<strong>and</strong> on acid volcanic<br />
hills.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5r<br />
Reference Sites: 5 Quaternary<br />
<strong>Vegetation</strong> Community 5r: <strong>Vegetation</strong> Community 5r, which provides representation for<br />
RE3.12.13 occurs in a number of scattered occurrences on the Inner Isl<strong>and</strong> Group. Small areas<br />
are mapped on sheltered upper slope positions on Zuna, Thursday <strong>and</strong> Muralug Isl<strong>and</strong>s. Site<br />
location TI14 on Thursday Isl<strong>and</strong> presents a typical community with canopy heights of 21m to<br />
27m in a woodl<strong>and</strong> <strong>and</strong> occasional open forest form. The canopy is dominated by Corymbia<br />
nesophila <strong>and</strong> C. stockeri subsp. peninsularis with an open sub-canopy <strong>and</strong> a sparse shrub layer<br />
comprising Grevillea parallela, Acacia leptocarpa <strong>and</strong> Pogonolobus reticulatus <strong>and</strong> a grassy<br />
ground cover dominated by Themeda tri<strong>and</strong>ra. On Zuna the canopy is lower with a diverse shrub<br />
layer dominated by Jacksonia thesioides, associated Acacia brassii, Livistona muelleri,<br />
Xylomelum scottianum, Melaleuca stenostachya, <strong>and</strong> Acacia simsii.<br />
Photograph 135. Woodl<strong>and</strong> of<br />
Corymbia nesophila on upper slope<br />
on diorite. Thursday Isl<strong>and</strong> Site<br />
TQ14.<br />
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5.2.64 <strong>Regional</strong> Ecosystem 3.12.16<br />
Description: Melaleuca viridiflora, Asteromyrtus brassii woodl<strong>and</strong>. Associated with granitic<br />
hills.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 14k, 13i, 14x, 14w (co)<br />
Reference Sites: 2 Secondary (ZS14, PWS11), 2 Quaternary (PWQ10, HAQ17a)<br />
Small areas of this RE are scattered throughout the inner isl<strong>and</strong> group, with minor areas also<br />
mapped on Moa Isl<strong>and</strong> <strong>and</strong> some extensive areas also represented on Muralug. The low<br />
shrubl<strong>and</strong> (VC14k) blankets a broad topographic depression in the central portion of Zuna Isl<strong>and</strong><br />
with VC13i much less extensive. The RE is typically manifest as a shrubl<strong>and</strong> <strong>and</strong> rarely low<br />
woodl<strong>and</strong> with Melaleuca stenostachya forming a prominent component of the canopy species.<br />
Structurally <strong>and</strong> floristic similarities are shared with coastal headl<strong>and</strong> shrubl<strong>and</strong>s (refer to<br />
RE3.12.31x1a) although differentiation is based largely on ecological controls. Whilst extreme<br />
exposure is the limiting factor in development of shrubl<strong>and</strong>s on exposed coastal headl<strong>and</strong>s, the<br />
development of RE3.12.16 is limited largely by soil infertility <strong>and</strong> moisture. Both VC14k <strong>and</strong><br />
VC13i are assigned to RE sub-type 3.12.16c whilst VC14x, represents the RE sub-type 3.12.16d.<br />
<strong>Vegetation</strong> community 14x occupies an extensive portion the rocky central interior of Muralug<br />
Isl<strong>and</strong> as component of the complex VC14w.<br />
<strong>Vegetation</strong> Community 14k: <strong>Vegetation</strong> community 14k is resticted to a broad topographic<br />
depression in the central portion of Zuna Isl<strong>and</strong>, occupying an area of skeletal soil formed on hard<br />
white acid volcanic rocks (rhyolite). The infertility of this substrate is the dominant control on<br />
shrubl<strong>and</strong> development. Melalueca stenostachya forms the dominant component of the<br />
shrubl<strong>and</strong> which has a general canopy height of 1.5 to 2m with sub-dominant to co-dominant<br />
species including Melaleuca viridiflora, Asteromyrtus symphyocarpa, Asteromyrtus brassii <strong>and</strong><br />
Jacksonia thesioides. The canopy is relatively even although is frequently broken with areas of<br />
unvegetated acid volcanic rubble.<br />
Photograph 136. Shrubl<strong>and</strong> type<br />
14k in a broad topographic<br />
depression on Zuna Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 13i: <strong>Vegetation</strong> community 13i represents near pure st<strong>and</strong>s of<br />
Melaleuca stenostachya, growing in shrubl<strong>and</strong> or low woodl<strong>and</strong> formation on acid volcanic<br />
rocks. The type is represented in only a few locations on Moa, Muralug <strong>and</strong> Hammond Isl<strong>and</strong>s<br />
with small areas forming on low rises in the acid volcanic basement, or on colluvial slopes where<br />
a thin thin blanket of poorly drained silty soils is retained. Typical of the occurrence of M.<br />
stenostachya in other communities, the species indicates extremely infertile edaphic condition.<br />
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Photograph 137. Low rise in acid<br />
volcanic basement at PWQ10<br />
supporting Melaleuca stenostachya<br />
low woodl<strong>and</strong> (VC13i).<br />
<strong>Vegetation</strong> Community 14x: <strong>Vegetation</strong> community 14x (RE 3.12.16d) forms the dominant<br />
component of VC14w, the latter being an extensive shrubl<strong>and</strong>, low woodl<strong>and</strong> <strong>and</strong> pavement<br />
complex on Muralug Isl<strong>and</strong>. The community, which is not represented individually in the<br />
mapping exercise, forms a low open shrubl<strong>and</strong> with shrub heights ranging from 1.5 to 3m, <strong>and</strong><br />
scattered emergents to 8m. The shrub layer is dominated by Melaleuca stenostachya, Corymbia<br />
stockeri subsp. peninsularis, Eucalyptus cullenii, Eucalyptus tetrodonta, Welchiodendron<br />
longivalve, Acacia sp. (DGF9191+), <strong>and</strong> Cochlospermum gillivraei. Eucalyptus cullenii <strong>and</strong><br />
Corymbia stockeri form the dominant emergent species. The ground cover is generally sparse<br />
interspersed with abundant bare rocky areas. Typical species are Heteropogon triticeus, Carissa<br />
ovata, Melaleuca stenostachya, Heamodorum coccineum, Cheilanthes sp., Themeda tri<strong>and</strong>ra,<br />
Evolvulus alsinoides, Schoenus sparteus, Eriachne pallescens, <strong>and</strong> Alloteropsis semialata.<br />
Photograph 138. Low open<br />
shrubl<strong>and</strong> VC14x (RE3.12.26a).<br />
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5.2.65 <strong>Regional</strong> Ecosystem 3.12.18<br />
Description: Eucalyptus leptophleba, Corymbia clarksoniana woodl<strong>and</strong> to open woodl<strong>and</strong> on<br />
coastal hills.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5f<br />
Reference Sites: 4 Quaternary.<br />
<strong>Vegetation</strong> Community 5f: <strong>Vegetation</strong> Community 5f is restricted to Naghir Isl<strong>and</strong>, <strong>and</strong><br />
provides the only representation of the RE in the study area. The community occupies welldrained<br />
granitic soils of the footslope <strong>and</strong> colluvial apron on the isl<strong>and</strong>s western side. Eucalyptus<br />
leptophleba forms the dominant canopy component of this open forest community which<br />
possesses a relatively even canopy at 20 to 25m height with Acacia polystachya an occasional<br />
associated species. The sub-canopy is relatively sparse featuring Dodonaea poly<strong>and</strong>ra <strong>and</strong><br />
Pleomele angustifolia, although the community hosts a well-developed shrub layer at 3m to 8m<br />
<strong>and</strong> 50% cover composed of Dodonaea poly<strong>and</strong>ra, Polyscias elegans, Micromelum minutum,<br />
Canarium australianum, Grewia oxyphylla, Psychotria poliostemma, Diospyros compacta <strong>and</strong><br />
Dalbergia densa var. australis. This community is highly disjunct, forming Australia’s most<br />
northerly occurrence of Eucalyptus leptophleba. The only other recognised occurrence of the<br />
species in the Torres Strait Isl<strong>and</strong>s is confined to scattered populations located on Thursday<br />
Isl<strong>and</strong>. Macgillivray (1852, 11, p. 39) (in Haddon 1888) in his account of a visit to Torres Strait<br />
<strong>and</strong> Naghir makes reference to E. leptophleba as follows…. “the small Eucalypti growing<br />
between the hill <strong>and</strong> the brushes is the most northern limit of that Australian genus known to me”.<br />
5.2.66 <strong>Regional</strong> Ecosystem 3.12.20<br />
Photograph 139. Eucalyptus<br />
leptophleba open forest on a granite<br />
colluvial Apron. Naghir Isl<strong>and</strong> Site<br />
NA05.<br />
Description: Evergreen notophyll vine forest dominated by Welchiodendron longivalve on<br />
headl<strong>and</strong>s.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 14c, 14d, 14h, 18c(co)<br />
Reference Sites: 22 Quaternary<br />
<strong>Regional</strong> Ecosystem 3.12.20 representing Welchiodendron longivalve dominant shrubl<strong>and</strong> is<br />
formed by VC14c <strong>and</strong> VC14f. These shrubl<strong>and</strong> communities occupy coastal escarpments<br />
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exposed to prevailing trade winds <strong>and</strong> this element of exposure, combined with skeletal soils,<br />
limitsd the development of these community to shrubl<strong>and</strong>s. Strong wind shearing of the canopy<br />
is generally apparent.<br />
<strong>Vegetation</strong> Community 14c/14d: <strong>Vegetation</strong> Community 14c is the dominant expression of this<br />
community, with extensive occurrences on exposed hillslopes of most of the larger continental<br />
isl<strong>and</strong>s. The community is particularly abundant on the Inner Isl<strong>and</strong> Group where it extends from<br />
coastal escarpments well upslope to exposed ridge crests <strong>and</strong> peaks, mixing with Acacia brassii<br />
shrubl<strong>and</strong>s (VC14j) on Muralug Isl<strong>and</strong>. The general canopy height for this community is less<br />
than 8m in accordance with classification as a shrubl<strong>and</strong> although communities with an upper<br />
stratum of less than 1m have also been included. Welchiodendron longivalve is the dominant<br />
species with associated Acacia polystachya, Cochlospermum gillivraei, Melaleuca stenostachya,<br />
Alyxia spicata, Terminalia subacroptera, Psydrax reticulata (V), Diospyros reticulata, Drypetes<br />
deplanchei <strong>and</strong> Premna dallachyana. Where deciduous thicket species, typically<br />
Cochlospermum gillivraei <strong>and</strong> Terminalia spp., dominate the canopy, the community is<br />
represented as VC14d. Psydrax reticulata is particularly prominent as a canopy or sub-canopy<br />
species.<br />
Photograph 140. Windsheared<br />
shrubl<strong>and</strong>s of Welchiodendron<br />
longivalve forming a mosaic with<br />
rock pavement on exposed coastal<br />
escarpment of Naghir Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 14h: This is an Acacia polystachya dominant variant of RE3.12.20,<br />
mapped largely on Warral Isl<strong>and</strong> although possibly more extensive than mapping currently<br />
indicates. The canopy comprises generally >50% cover of Acacia polystachya with co-dominant<br />
to sub-dominant Welchiodendron longivalve in a closed shrubl<strong>and</strong> to low open forest formation.<br />
The sub-canopy features of this community were not sampled intensively during the survey. The<br />
community is a prominent component of the complex type VC18c.<br />
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5.2.67 <strong>Regional</strong> Ecosystem 3.12.21a<br />
Photograph 141. The brilliant<br />
green canopy features of Acacia<br />
polystachya in VC14f. Warral<br />
Isl<strong>and</strong>.<br />
Description: Deciduous vine thicket. Occurs on granite slopes mainly on the Great Dividing<br />
Range <strong>and</strong> offshore isl<strong>and</strong>s.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 2b, 2f, 2n, 2s, 2v, 2x<br />
Reference Sites: 3 Secondary (DA01, DA32, DA47), 18 Quaternary<br />
<strong>Regional</strong> Ecosystem 3.12.21 represents a diverse array of floristic <strong>and</strong> structural variations of<br />
semi-deciduous <strong>and</strong> deciduous vine thicket mapped individually in the <strong>Vegetation</strong> Community<br />
Classifications 2b, 2f, 2x, 2n, 2v <strong>and</strong> 2s. This RE also comprises components of the<br />
vegetacomplexes 18c <strong>and</strong> 14d. The features of the major VC’s are discussed briefly below. All<br />
component VC’s are described under the sub-unit RE 3.12.21a. <strong>Vegetation</strong> 2v, being an Acacia<br />
polystachya dominant variation, is poorly sampled <strong>and</strong> as such, is not included in the vegetation<br />
descriptions.<br />
<strong>Vegetation</strong> Community 2b: This is a floristically uniform community on the granite boulder<br />
footslopes of Dauan Isl<strong>and</strong>. The community, which was nearly fully deciduous at the time of<br />
survey, forms a semi-deciduous notophyll vine thicket <strong>and</strong> occasional low closed forest.<br />
Dominant canopy species include Canarium australianum, Cochlospermum gillivraei, Bombax<br />
ceiba var. leiocarpum, Cleistanthus peninsularis, Cupaniopsis anacardioides, Pouteria sericea,<br />
Ficus virens var. sublanceolata, Terminalia subacroptera, Elaeocarpus arnhemicus <strong>and</strong><br />
Manilkara kauki. The understorey is diverse comprising Glycosmis trifoliata, Dimorphocalyx<br />
australiensis, Salacia disepala, Psydrax reticulata, Cyclophyllum maritimum, Cupaniopsis<br />
anacardioides, Memecylon pauciflorum, Cliestanthus peninsularis, Micromelum minutum,<br />
Ganophyllum falcatum, Cryptocarya exfoliata, Litsea glutinosa, Tabernaemontana orientalis,<br />
Eugenia reinwardtiana, Drypetes deplanchei, Diospyros reticulatus, Aidia racemosa, Capparis<br />
sepiaria, Ixora timorensis, Exocarpos latifolius, Cathormion umbellatum subsp. monoliforme,<br />
Celtis philippensis, Murraya ovatifoliolata, Cryptocarya exfoliata, Litsea glutinosa, Diospyros<br />
reticulatus, Chionanthus ramiflora, Pleomele angustifolia, Macaranga tanarius, Pouteria<br />
sericea, <strong>and</strong> Ficus obliqua var. obliqua. Thin wiry vines are numerous such as Gymnosporia<br />
inermis, Trophis sc<strong>and</strong>ens, Cissus sp., Flagellaria indica, Cansjera leptostachya, Hoya australe<br />
subsp. sanae <strong>and</strong> Jasminum elongata.<br />
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Photograph 142. Vine Thicket<br />
Community 2b at Site DA01 (Dauan<br />
Isl<strong>and</strong>).<br />
<strong>Vegetation</strong> Community 2f: Small areas of low deciduous vine thicket, typically with canopy<br />
heights ranging from 3m to 6m, are found on the steep exposed rocky headl<strong>and</strong>s of Horn <strong>and</strong><br />
Adolphus Isl<strong>and</strong>. The communities form a patchwork with sclerophyll shrubl<strong>and</strong> communities,<br />
<strong>and</strong> are attenuated attenuated upslope along gully lines where some shelter from the elements is<br />
afforded. The dominant canopy is occupied by a range of species which include, in order of<br />
decreasing dominance; Buchanania arborescens, Millettia pinnata, Sterculia sp. (Annan River),<br />
Terminalia subacroptera, Cochlospermum gilivraei <strong>and</strong> Pouteria sericea. Sub-canopy <strong>and</strong><br />
ground covers are poorly developed on account of the low stature <strong>and</strong> rocky substrate.<br />
Additional site survey would benefit the characterisation of this community.<br />
Photograph 143. Low semideciduous<br />
notophyll vine thicket<br />
(VC2f) on exposed slopes of Horn<br />
Isl<strong>and</strong> (Site HI26).<br />
<strong>Vegetation</strong> Community 2n: <strong>Vegetation</strong> Community 2n is the dominant structural variation on<br />
Iama Isl<strong>and</strong> where it occupies wind-exposed footslopes on granite. The community is typically<br />
lower than VC2b <strong>and</strong> has a much more even <strong>and</strong> wind sheared canopy structure. The community<br />
was sampled at Sites YA014, YA017, YA019, YA20, YA23 <strong>and</strong> YA25 where typical canopy<br />
species included in order of decreasing dominance Canarium australianum, Antiaris toxicaria<br />
var. macrophylla, Gyrocarpus americanus, Terminalia subacroptera, Manilkara kauki, Acacia<br />
auriculiformis, Diospyros reticulata, Sterculia sp. (Annan River) <strong>and</strong> Premna dallachyana.<br />
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The understorey is diverse featuring Memecylon pauciflorum, Dimorphocalyx australiensis,<br />
Drypetes deplanchei, Eugenia reinwardtiana, Exocarpos latifolius, Micromelum minutum,<br />
Murraya ovatifoliolata, Glycosmis trifoliata, Turraea pubescens, Manilkara kauki, Litsea<br />
glutinosa, Cryptocarya exfoliata, Wrightia pubescens subsp penicillata, Diospyros hebecarpa,<br />
Chionanthus ramiflora, Cupaniopsis anacardioides, Ixora timorensis, Streblus brunonianus,<br />
Luvunga monophylla, Miliusa traceyi, Diospyros compacta, Alyxia spicata, Aidia racemosa,<br />
Micromelum minutum, Arytera bifoliolata, <strong>and</strong> Intsia bijuga. Typical vines are Capparis<br />
quiniflora, Derris trifoliata, Trophis sc<strong>and</strong>ens, Opilia armentacea, Flagellaria indica, Secamone<br />
elliptica, <strong>and</strong> Salacia disepala.<br />
<strong>Vegetation</strong> Community 2s: This vine thicket variant occupies windsheared upper slope<br />
positions on Dauan Isl<strong>and</strong>. Limited floristic information was gathered for this community due to<br />
its occurrence on a precipitous slope, which greatly limited the ability to sample safely. Thus the<br />
community description pertains largely to canopy features which were recorded though<br />
observation. The canopy is relatively even with strong wind shearing <strong>and</strong> typical height<br />
estimated at 8m. Dominant canopy species comprised Ficus virens var. sublanceolata, Pouteria<br />
sericea, Shefflera actinophylla, Pouteria obovata, Garcinia warrenii, Syzygium puberulum, Ficus<br />
microcarpa, Acmenosperma claviflorum, Ficus destruens, Terminalia subacroptera, Myristica<br />
insipida, Canarium australianum, Arytera divaricata, Aglaia elaeagnoidea <strong>and</strong> Drypetes<br />
deplanchei.<br />
Photograph 144. <strong>Vegetation</strong><br />
Community 2n on footslopes at Site<br />
YA019, Iama Isl<strong>and</strong>.<br />
Photograph 145. <strong>Vegetation</strong><br />
Community 2s demonstrating<br />
typically wind sheared canopy<br />
structure on steep south-east facing<br />
upper slopes of Dauan Isl<strong>and</strong>.<br />
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<strong>Vegetation</strong> Community 2x: A representation of a fully deciduous vine thicket community, with<br />
occurrence restricted to upper slopes on Mabuiag Isl<strong>and</strong> where it occupies acid volcanic talus,<br />
complexing with rock pavement shrubl<strong>and</strong> (VC18c) <strong>and</strong> bare rock pavement. Where sampled on<br />
Mabuiag Isl<strong>and</strong> at Site MO047, the canopy comprised Bombax ceiba var. leiocarpum, Terminalia<br />
subacroptera, Cochlospermum gillivraei, Sterculia quadrifida, Cleistanthus peninsularis,<br />
Drypetes deplanchei <strong>and</strong> Melicope peninsularis at a height of 8m. Sub-canopy species although<br />
sparse may include Pouteria sericea, Garcinia warrenii, Syzygium puberulum, Acmenosperma<br />
claviflorum, Myristica insipida, Arytera divaricata, Aglaia elaeagnoidea, <strong>and</strong> Drypetes<br />
deplanchei. Photographic illustration is provided in Photograph 146.<br />
5.2.68 <strong>Regional</strong> Ecosystem 3.12.23<br />
Photograph 146. Typical structure<br />
of VC2x at Site MO45, Mabuiag<br />
Isl<strong>and</strong>.<br />
Description: Acacia brassii low open forest on acid volcanics on northern ranges <strong>and</strong> isl<strong>and</strong>s.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 14j, 14w (co), 18b (co), 6f<br />
Reference Sites: 16 Quaternary<br />
Acacia brassii dominant shrubl<strong>and</strong>s are prominent on the continental isl<strong>and</strong>s being particularly<br />
extensive on the rocky interior of Muralug Isl<strong>and</strong> <strong>and</strong> on Mabuiag Isl<strong>and</strong>. These communities are<br />
represented individually or as components of broader shrubl<strong>and</strong> <strong>and</strong> rock pavement mosaics. The<br />
RE comprises a number of VC’s which are discussed briefly below.<br />
<strong>Vegetation</strong> Community 14j <strong>and</strong> Complex 14w: <strong>Vegetation</strong> Community 14j forms the<br />
dominant expression of this RE <strong>and</strong> is mapped on rocky acid volcanic ridgelines <strong>and</strong> hillslopes of<br />
the Inner Isl<strong>and</strong> Group, being particularly prominent on Muralug Isl<strong>and</strong>. Extensive areas are also<br />
represented on Mabuiag Isl<strong>and</strong>. The community represents a shrubl<strong>and</strong> of typically 1.5 to 5m tall<br />
dominated by Acacia brassii. Associated species include a range of shrubs such as<br />
Cochlospermum gillivraei, Melaleuca stenostachya <strong>and</strong> Welchiodendron longivalve although in<br />
no circumstance do these shrubs dominate the upper stratum. Melaleuca viridiflora may be<br />
locally prominent on Mabuiag where the type merges with VC14a. This community forms<br />
extensive complexes with Eucalypt shrubl<strong>and</strong>s, Welchiodendron shrubl<strong>and</strong>s <strong>and</strong> deciduous<br />
shrubl<strong>and</strong>s on Muralug Isl<strong>and</strong> where it is mapped as a component of the shrubl<strong>and</strong> complex type<br />
VC14w. The coomunity is also major component of the pavement complex type VC18b.<br />
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<strong>Vegetation</strong> Community 6f: The steep wind exposed peak of Mt. Adolphus hosts a windswept<br />
closed shrubl<strong>and</strong> of Acacia sp. Due to difficulties with l<strong>and</strong> access permission, this community<br />
could only be observed remotely from helicopter. As such, confirmation of the acacia to species<br />
level was not achievable. This community is placed into RE3.12.23 as a preliminary measure<br />
subject to on-ground floristic assessment. The shrubl<strong>and</strong> forms a narrow fringe between rock<br />
pavement on the eastern facing escarpment of Mt. Adolphus <strong>and</strong> well-developed evergreen vine<br />
forest on the mountains leeward side.<br />
Photograph 147. Acacia brassii<br />
dominant community 14j as a<br />
component of the shrubl<strong>and</strong> complex<br />
14w on Muralug Isl<strong>and</strong> (Site PoW<br />
45).<br />
Photograph 148. Acacia brassii<br />
dominant shrubl<strong>and</strong> as type 14j on<br />
Mabuiag Isl<strong>and</strong>. The type separates<br />
into VC18b where the ratio of<br />
rock/shrubl<strong>and</strong> is greater than 1:1<br />
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5.2.69 <strong>Regional</strong> Ecosystem 3.12.29<br />
Photograph 149. Acacia sp.<br />
shrubl<strong>and</strong> type 6f. Well-developed<br />
evergreen vine forest (VC1a) is<br />
clearly visible on the sheltered<br />
margins of this shrubl<strong>and</strong>.<br />
Description: Heteropogon triticeus ± Sarga plumosum closed tussock grassl<strong>and</strong> on continental<br />
isl<strong>and</strong>s<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 17c, 12a<br />
Reference Sites: 18 Quaternary<br />
<strong>Regional</strong> Ecosystem 3.12.29 is relatively extensive throughout the Torres Strait continental<br />
isl<strong>and</strong>s where it typically occupies exposed coastal headl<strong>and</strong>s <strong>and</strong> footslopes on granite <strong>and</strong> acid<br />
volcanic rocks. The RE is represented by VC17c <strong>and</strong> VC12a, the latter being an atypical<br />
expression of the type.<br />
<strong>Vegetation</strong> Community 17c: This classification provides a generic representation of grassl<strong>and</strong><br />
communities on acid volcanic <strong>and</strong> acid plutonic lithologies. The constituent grass species are<br />
variable dependant on soil type, exposure <strong>and</strong> derivation. <strong>Communities</strong> on Dauan are composed<br />
dominantly of Cymbopogon refractus <strong>and</strong> Heteropogon triticeus with a range of shrub species<br />
forming an emergent layer including P<strong>and</strong>anus sp., Psydrax sp., Cochlospermum gillivraei,<br />
Syzygium suborbiculare <strong>and</strong> Parinari nonda. These communities are fire controlled, derived<br />
from repetitive burning of colluvial footslopes which has caused an upslope retreat of the vine<br />
forest margins. Associated soils are generally well-drained s<strong>and</strong> <strong>and</strong> gravel loams mixed with<br />
granite detritus.<br />
In wind-exposed locations on skeletal soils, grassl<strong>and</strong>s represent a climax community with<br />
species composition <strong>and</strong> structure influenced by prevailing climatic <strong>and</strong> edaphic conditions rather<br />
than human induced l<strong>and</strong>scape changes. Themeda tri<strong>and</strong>ra forms the dominant species in such<br />
locations often interspersed with scattered shrubs <strong>and</strong> bare rock pavement. It should be noted that<br />
a range of RE sub-types are represented under this classification although no attempt has been<br />
made to separate these on a floristic or l<strong>and</strong>scape process basis. Considerable field survey will be<br />
required to confidently differentiate <strong>and</strong> typify these variations.<br />
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Photograph 150. A typical<br />
expression of VC17c on Dauan<br />
Isl<strong>and</strong> where it occupies a regularly<br />
burnt granite boulder footslope.<br />
<strong>Vegetation</strong> Community 12a: This community represents an atypical expression of RE3.12.29<br />
forming grassy woodl<strong>and</strong> of Livistona muelleri on the colluvial footslopes of Dauan Isl<strong>and</strong>.<br />
Similar to VC17c, repetitive burning of the footslopes has resulted in an upslope retreat of the<br />
vine forest margins, although in this community, the fire tolerance of Livistona muelleri has<br />
resulted in the retention of this species as vine forest margins have retreated. It should be noted<br />
that the palm forms a scattered emergent in a limited number of vine thicket communities<br />
examined on the isl<strong>and</strong>. This community has been classified under RE13.12.29 due to its<br />
extremely limited extent <strong>and</strong> similarity in community derivation to the more extensive VC17c.<br />
5.2.70 <strong>Regional</strong> Ecosystem 3.12.30<br />
Photograph 151. Livistona muelleri<br />
grassy woodl<strong>and</strong> (VC12b) on granite<br />
colluvial footslopes of Dauan Isl<strong>and</strong>.<br />
Description: Imperata cylindrica ± Mnesithea rottboellioides closed tussock grassl<strong>and</strong> on steep<br />
slopes.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 17f, 17h (co)<br />
Reference Sites: No reference sites<br />
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The extensive mosaic of grassl<strong>and</strong> <strong>and</strong> low closed forest on steep granite hillslopes on Moa Isl<strong>and</strong><br />
provides the only mapped representation of this RE in the exercise. More intensive field survey<br />
is likely to result in additional representation. Several areas mapped as RE13.12.29 may be more<br />
appropriately represented under this RE.<br />
<strong>Vegetation</strong> Community 17f: The Moa Isl<strong>and</strong> example forms an extensive grassl<strong>and</strong> complex<br />
dominated by Imperata cylindrica. Closed forest communities of Welchiodendron are restricted<br />
to fire protected gullies <strong>and</strong> boulder piles where they are represented as RE3.12.4, although due<br />
to scale limitations, these could not be adequately differentiated from the broader grassl<strong>and</strong><br />
system. The grassl<strong>and</strong>/Welchiodendron open forest complex is represented as VC17h. The<br />
current representation of this RE is clearly influenced by repetitive firing of the slopes which has<br />
caused retreat of the once dominant closed forest communities in favour of Imperata dominant<br />
grassl<strong>and</strong>. This community is in a state of relative stability with little change in areal extent<br />
indicated between 1974 aerial photography <strong>and</strong> recent satellite imagery.<br />
5.2.71 <strong>Regional</strong> Ecosystem 3.12.31x1a (New RE)<br />
Photograph 152. Grassl<strong>and</strong><br />
community 17h with a stark fire<br />
controlled boundary between<br />
grassl<strong>and</strong> <strong>and</strong> open forest. The<br />
similarity to grassl<strong>and</strong> communities<br />
on Dauan are notable, however Moa<br />
Isl<strong>and</strong> examples are dominated by<br />
Imperata cylindrica.<br />
Preliminary Description: Shrubl<strong>and</strong> on exposed coastal headl<strong>and</strong>s of the Torres Strait Isl<strong>and</strong>s.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 14a, 14f, 14l, 14g<br />
Reference Sites: 1 Secondary (MA02), 22 Quaternary Sites.<br />
A new <strong>Regional</strong> Ecosystem is erected to represent shrubl<strong>and</strong> communities formed on coastal<br />
headl<strong>and</strong>s, whose development has been shaped by elements of extreme wind exposure <strong>and</strong><br />
skeletal soil development. These communities are generally located on south-east facing<br />
headl<strong>and</strong>s which are exposed to the prevailing south east trade winds. Scattered communities<br />
may also occur on exposed ridgelines away from the immediate coast.<br />
<strong>Vegetation</strong> Community 14a: The dominant representation for this group is provided by VC14a<br />
which occurs on the majority of continental isl<strong>and</strong> groups including the Central group, the Near<br />
Western Group, <strong>and</strong> Muralug Isl<strong>and</strong> on the Inner Isl<strong>and</strong> Group. The community is represented as<br />
a shrubl<strong>and</strong> to dwarf open shrubl<strong>and</strong> with canopy heights ranging from 0.5m to 1.5m. Several<br />
examples with prostrate shrubs were also included in this classification. The dominant canopy<br />
comprises Melaleuca viridiflora <strong>and</strong> Welchiodendron longivalve, generally in equal proportion.<br />
Asteromyrtus brassii is present in some locations but is rarely prominent. Lithomyrtus retusa is<br />
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prominent as a secondary shrub layer, occasionally reaching the upper strata. Additional<br />
characteristic species are Psydrax reticulata, Alyxia spicata, Acacia brassii, Jacksonia thesioides,<br />
Acacia leptocarpa, Acacia simsii, Cochlospermum gillivraei, Parinari nonda, Pogonolobus<br />
reticulatus, Asteromyrtus symphyocarpa, Exocarpos latifolius, <strong>and</strong> Melaleuca stenostachya.<br />
Groundcover is dominated by stunted shrubs with a minor contribution to cover from Dianella<br />
sp., Themeda tri<strong>and</strong>ra, Cassytha filiformis, Aristida sp., Schoenus sp., Thaumastochloa sp.,<br />
Phyllanthus sp., Alloteropsis semialata <strong>and</strong> the Gompholobium pinnatum. The community is<br />
restricted to rhyolite headl<strong>and</strong>s on infertile skeletal soils.<br />
Photograph 153. <strong>Vegetation</strong><br />
Community 14a on Mabuiag Isl<strong>and</strong><br />
Site MA2.<br />
Photograph 154. Dwarf<br />
shrubl<strong>and</strong>/grassl<strong>and</strong> complexes with<br />
prostrate Melaleuca viridiflora<br />
shrubs have also been included in<br />
VC14a. Site MO69 on Moa Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 14f: <strong>Vegetation</strong> Community 14f is represented only on the southern<br />
footslopes of Thursday Isl<strong>and</strong>. This is a slightly more developed community, forming a<br />
shrubl<strong>and</strong> at 1.5 to 3m tall composed of a mixed range of species including Melaleuca viridiflora,<br />
Welchiodendron longivalve, Cochlospermum gillivraei, Grevillea parallela <strong>and</strong> Melaleuca<br />
stenostachya. Corymbia spp. may be present as emergents. The community grades upslope into<br />
woodl<strong>and</strong> community 5e.<br />
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Photograph 155. Shrubl<strong>and</strong><br />
community 14f on Thursday Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 14l: The inner isl<strong>and</strong>s of Zuna, Horn <strong>and</strong> Hammond host VC14l, which<br />
similar to VC14a, occupies steep coastal headl<strong>and</strong>s directly exposed to prevailing south-easterly<br />
trade winds. The community is manifest as a low shrubl<strong>and</strong> to shrubl<strong>and</strong>, typically 1m to 1.5m<br />
tall with an upper shrub layer composed of, in order of decreasing dominance, Melaleuca<br />
viridiflora, Acacia brassii, Lithomyrtus retusa, Welchiodendron longivalve, Jacksonia thesioides,<br />
Corymbia nesophila, Asteromyrtus symphyocarpa, Melaleuca stenostachya, Alyxia spicata,<br />
Acacia simsii, Halfordia kendack, <strong>and</strong> Psydrax reticulata. This community is structurally similar<br />
to VC14a although a more diverse upper stratum warrants recognition as an individual<br />
community.<br />
Photograph 156. Low windswept<br />
shrubl<strong>and</strong> community 14l on<br />
exposed coastal escarpments of Zuna<br />
Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 14g: The shrubl<strong>and</strong> complex 14g is most prominent on exposed granite<br />
boulder footslopes on Dauan Isl<strong>and</strong> although a minor area has also been differentiated on Iama<br />
Isl<strong>and</strong>. The upper stratum of this community forms a dense shrubby thicket that is generally<br />
impenetrable, with a typical height of not greater than 1.5m. Species representative of the<br />
dominant upper stratum (S1 layer) include Buchanania arborescens, Manilkara kauki, Alyxia<br />
spicata <strong>and</strong> Pouteria sericea. On Iama, the unit includes coastal vine thicket species such as<br />
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Manilkara kauki, Terminalia subacroptera, Canarium australianum, Eugenia reinwardtiana,<br />
Sarcostemma viminale subsp. brunonianus, Alyxia spicata, <strong>and</strong> Drypetes deplanchei.<br />
Emergents of P<strong>and</strong>anus sp. to 8m are scattered throughout the complex. Similar to other<br />
communities within this grouping, the community has formed in response to extreme wind<br />
exposure <strong>and</strong> skeletal soils. This community is not florisitically typical of this proposed new RE,<br />
lacking Melaleuca spp. as a dominant component. It does however occupy a similar ecological<br />
niche to VC’s 14a, 14f <strong>and</strong> 14l <strong>and</strong>, due to its extremely limited areal extent, has been placed<br />
within this grouping in the absence of a more suitable one.<br />
5.2.72 <strong>Regional</strong> Ecosystem 3.12.33b<br />
Photograph 157. Windswept<br />
shrubl<strong>and</strong> community 14g on<br />
exposed granite footslopes of Dauan<br />
Isl<strong>and</strong>. Site DA041.<br />
Description: Granite boulders covered with blue-green algae. Occurs on Black Mountain <strong>and</strong><br />
Cape Melville.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 19a, 11a<br />
Reference Sites: 4 Quaternary<br />
<strong>Vegetation</strong> Community 19a: The most extensive occurrence of RE3.12.33 is mapped on Dauan<br />
Isl<strong>and</strong> where it occupies extensive areas of hillslope, generally in a mid-slope position. Smaller<br />
areas are mapped on Hammond <strong>and</strong> Muralug Isl<strong>and</strong>s. The community is best described as an<br />
open granite boulder field with scattered vine forest shrubs, low trees <strong>and</strong> occasional vine thicket.<br />
Woody cover is typically less than 5% comprising Canarium australianum, Ficus microcarpa,<br />
Cochlospermum gillivraei <strong>and</strong> Tetrameles nudiflora. Sprawling mats <strong>and</strong> low towers of the vine<br />
Aristolochia acuminata are locally prominent <strong>and</strong> ground cover of Drynaria quercifolia,<br />
Asplenium sp. <strong>and</strong> Sarcostemma viminale subsp. brunonianus are occasionally present in<br />
sheltered pockets. This community represents a significant geographical departure from<br />
mainl<strong>and</strong> Cape York Peninsula examples at Black Mountain <strong>and</strong> Cape Melville. Small areas of<br />
P<strong>and</strong>anus woodl<strong>and</strong> are also recognised within this RE <strong>and</strong> are discussed below.<br />
<strong>Vegetation</strong> Community 11a: P<strong>and</strong>anus dominant woodl<strong>and</strong> on granite headl<strong>and</strong>s are scattered<br />
throughout a large number of the larger continental isl<strong>and</strong>s. In the majority of examples, these<br />
communities have been too small to represent individually <strong>and</strong> thus consumed within a broader<br />
vegetation complex. The communities on Dauan, represented as VC11a (on granite) are<br />
sufficiently developed to allow classification as an individual VC. The extremely limited spatial<br />
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extent of this community greatly restricts the ability to classify it appropriately within the RE<br />
framework as as such, it has been place within the broader RE3.12.33b grouping in recognition of<br />
its similarity in l<strong>and</strong>form <strong>and</strong> edaphic condition.<br />
5.2.73 <strong>Regional</strong> Ecosystem 3.12.34c<br />
Photograph 158. A typical granite<br />
boulder field on Dauan Isl<strong>and</strong><br />
providing representation of<br />
RE13.12.33b.<br />
Photograph 159. P<strong>and</strong>anus<br />
woodl<strong>and</strong>s (Type 11a) on granite<br />
headl<strong>and</strong>s of Dauan Isl<strong>and</strong>.<br />
Preliminary Description: Rock pavements associated with hillslopes <strong>and</strong> footslopes of the<br />
Torres Strait Isl<strong>and</strong>s.*<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 18a, 18b (co), 18c (co), 18d, 14w (co), RR, RG<br />
Reference Sites: 13 Quaternary<br />
This RE classification provides for representation of a range of rock pavements <strong>and</strong> rock<br />
pavement shrubl<strong>and</strong>s that have a considerable extent on a number of continental isl<strong>and</strong>s. Whilst<br />
RE3.12.34 presents a suitable classification in a structural sense, the type description is<br />
geographically confined to the Melville Range <strong>and</strong> Black Mountain cannot be applied to the<br />
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Torres Strait situation without modification of the original type description, or description as an<br />
RE sub-type. As such, this community has been described under RE sub-type 3.12.34c as<br />
advised by the Queensl<strong>and</strong> Herbarium. <strong>Vegetation</strong> community 18a forms a homogenous polygon<br />
of RE3.12.4c, whilst VC18b, VC18c <strong>and</strong> 14w are mapped as complexes of a number of different<br />
RE’s. Small areas of rock, devoid of vegetation <strong>and</strong> mapped under units RR <strong>and</strong> RG, are also<br />
included in this classification.<br />
<strong>Vegetation</strong> Community 18a: <strong>Vegetation</strong> community 18a is widespread on the rockier<br />
continental isl<strong>and</strong>s, being particularly prominent on Mabuiag, Hawkesbury <strong>and</strong> Muralug where it<br />
occurs on areas of skeletal soil. The community comprises a complex of bare rock interspersed<br />
with shrubl<strong>and</strong>, the latter typically occupying cracks <strong>and</strong> crevices where sufficient moisture <strong>and</strong><br />
nutrient (from skeletal soil formation) is provided to allow shrubl<strong>and</strong> development. The<br />
shrubl<strong>and</strong> component typical comprises deciduous vine thicket species ranging in height from 1.5<br />
to 6m, with an average cover (including bare pavement areas) typically less than 5%. Dominant<br />
species include Cochlospermum gillivraei, Canarium australianum, Terminalia sp., Psydrax<br />
banksii, Psydrax reticulata, Dalbergia densa var. australis, Secamone elliptica, Acacia<br />
polystachya, Carissa ovata, Acacia polystachya, Ziziphus oenopolia, Capparis arborea <strong>and</strong><br />
occasional Welchiodendron longivalve. Bare pavements are scattered throughout the broader<br />
shrubl<strong>and</strong> mosaic.<br />
<strong>Vegetation</strong> community 18a is a prominent component of a number of vegetation complexes<br />
including VC18b where it mosaics with VC14j (RE3,12,23); VC18c where it mosaics with<br />
VC14h (RE3.12.20), <strong>and</strong>; VC14w where it complexes with a range of woodl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong><br />
types including VC5l (RE3.12.11), VC14c (RE3.12.20) <strong>and</strong> VC14w (3.12.16d).<br />
Photograph 160. A mosaic of<br />
deciduous shrubl<strong>and</strong> <strong>and</strong> granite<br />
boulders forming a represention of<br />
VC18a on Warral Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Complex 18b/18c: Shrubl<strong>and</strong> /rock pavement complex type 18b is particularly<br />
prominent on the rocky acid volcanic slopes of Mabuiag Isl<strong>and</strong>. This complex comprises a<br />
mosaic of Acacia brassii low shrubl<strong>and</strong> (VC14j/RE3.12.23) <strong>and</strong> deciduous shrubl<strong>and</strong>/ bare rock<br />
pavement complex (VC18a/RE3.12.34c). The Acacia brassii shrubl<strong>and</strong> component of this<br />
complex, forms a low windswept closed shrubl<strong>and</strong> typically 0.5 to 1.5 m tall with prostrate<br />
examples in the most exposed locations. The type has been more thoroughly described in relation<br />
to RE3.12.23 (see Section 5.2.68) whilst the deciduous shrubl<strong>and</strong> component is typical of<br />
VC18a described above. <strong>Vegetation</strong> community 18c is largely confined to Warral Isl<strong>and</strong> in the<br />
Near Western Isl<strong>and</strong> group where VC18a mosaics with low open forest <strong>and</strong> shrubl<strong>and</strong> dominated<br />
by Acacia polystachya <strong>and</strong> Welchiodendron longivalve (VC14h/RE3.12.20).<br />
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Photograph 161. Bare pavements<br />
with scattered Cochlospermum<br />
gillivraei forming a mosaic with<br />
Acacia brassii shrubl<strong>and</strong> in VC18b<br />
(Mabuiag Isl<strong>and</strong>) providing<br />
representation for RE13.12.34c.<br />
<strong>Vegetation</strong> Community 18d: Shrubl<strong>and</strong> /rock pavement complex type 18d is mapped on the<br />
rocky granite knolls of Badu Isl<strong>and</strong>, forming extensive pavements <strong>and</strong> rock piles on the isl<strong>and</strong>s<br />
interior. Due to access constraints, this community was sparsely sampled <strong>and</strong> as such, the<br />
description provided here may not represent the communities full range of floristic <strong>and</strong> structural<br />
variations. Further sampling of this pavement type is warranted should future access to the isl<strong>and</strong><br />
for the purpose of vegetation survey be granted. The community characteristically occupies<br />
rocky knolls with scattered shrubs utilising fractures, crevices <strong>and</strong> overhangs for nutrient <strong>and</strong><br />
shelter. Corymbia stockerii subsp. peninsularis is the dominant shrub species reaching heights of<br />
6m. Associated shrub species include Acacia polystachya, Psydrax banksii, <strong>and</strong> Welchiodendron<br />
longivalve. A secondary shrub layer forms at a height of 0.5m to 1.5m, dominated by Alyxia<br />
spicata, Ficus sp. <strong>and</strong> Dodonoea poly<strong>and</strong>ra. The total combined canopy cover of the two shrub<br />
layers is typically < 5%, with bare rock exposure forming >90% of the total ground cover.<br />
Photograph 162. Rock pavement<br />
type 18d.<br />
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5.2.74 <strong>Regional</strong> Ecosystem 3.12.35 (New RE)<br />
Preliminary Description: Semi-deciduous mesophyll/notophyll vine forest on granite slopes of<br />
the Torres Strait Sub-region.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 2d, 2h, 2o, 2q, 2r, 2t, 6a, 6e<br />
Reference Sites: 8 Secondary (YAO4, YA05, MO003, PW085, PW093, HA05, YA18, YA21)<br />
To provide an adequate ecological grouping for the deciduous <strong>and</strong> semi deciduous vine forest<br />
communities in the Torres Strait, it is necessary to erect an additional RE to accommodate a<br />
diverse array of vine forest types that characterise the steep granitic <strong>and</strong> acid volcanic slopes of<br />
many of the continental isl<strong>and</strong>s. These forests extend from the Northern Isl<strong>and</strong> Group, being<br />
particularly abundant on Dauan, through the central group on Iama <strong>and</strong> Gebar, the Near Western<br />
Group <strong>and</strong> the Inner Isl<strong>and</strong> Group. Vine forest communities often vary subtly between isl<strong>and</strong>s<br />
<strong>and</strong> as such, minor floristic or structural variations can be represented with relative confidence<br />
due to the ecological isolation imposed by isl<strong>and</strong> boundaries. The constituent vegetation<br />
communities of newly described RE3.12.35 are described below.<br />
<strong>Vegetation</strong> Community 2d: VC 2d is mapped on the steep, boulder strewn mid to upper slopes<br />
of Dauan Isl<strong>and</strong>, demonstrating a marked structural contrast to the thickets of the lower slopes.<br />
Canopy heights in this community range from 18 to 25m <strong>and</strong> constituent species are both<br />
deciduous <strong>and</strong> semi-deciduous consistent with its structural classification as a semi-deciduous<br />
vine forest. Dominant canopy species include Tetrameles nudiflora, Alstonia spectabilis,<br />
Ganophyllum falcatum, Bombax ceiba var. leiocarpum, Canarium australianum, Ficus virens<br />
var. sublanceolata, Ficus microcarpa <strong>and</strong> *Mangifera indica. Sub-canopy species were not<br />
sampled in detail although Gossia floribunda was abundant in some locations, <strong>and</strong> hemiepiphytes<br />
including Asplenium nidus, Drynaria quercifolia <strong>and</strong> Microsorum punctatum are<br />
prominent. The community is notable for the diversity of epiphytic plants including Dendrobium<br />
litorale, Bulbophyllum spp., <strong>and</strong> Dischidia littoralis, listed as Vulnerable (NCA, 1992), which<br />
was particularly abundant. With reference to Herbrecs data <strong>and</strong> Stanton <strong>and</strong> Fell (2005), the<br />
occurrence of Tetrameles nudiflora represents a considerable extension of geographical range<br />
north from Schram Creek, although Hyl<strong>and</strong> et al. (2003) record it from northern Torres Strait. Its<br />
presence on Dauan on steep granitic boulder slopes is considered unusual, as it is more<br />
commonly associated with seasonally flooded lowl<strong>and</strong> alluvial terraces e.g. Claudie River<br />
(RE3.3.1). This species also occurs throughout lowl<strong>and</strong> PNG (Conn et al. 2006+).<br />
Photograph 163. In foreground, the<br />
deciduous crowns of Tetrameles<br />
nudiflora in flower are clearly visible<br />
in the canopy of VC2d.<br />
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<strong>Vegetation</strong> Community 2h: This community is mapped on rocky granite <strong>and</strong> rhyolite footslopes<br />
of Iama Isl<strong>and</strong> where it presents as a deciduous vine forest. The typical canopy is irregular,<br />
ranging in height from 12 to 25m, with a cover generally greater than 80%. The majority of<br />
crowns were fully deciduous at the time of survey resulting in a forest with an ‘open’ feel <strong>and</strong> a<br />
number of sub-canopy species were also deciduous. Dominant canopy species include Erythrina<br />
insularis, Antiaris toxicaria var. macrophylla, Terminalia subacroptera, Canarium australianum,<br />
Bombax ceiba var. leiocarpum, Acacia auriculiformis, <strong>and</strong> Manilkara kauki. The sub-canopy<br />
which ranges in height from 8 to 15m is relatively open comprising Diospyros reticulatus,<br />
Manilkara kauki, Exocarpos latifolius, Capparis quiniflora, Diospyros compacta <strong>and</strong> Celtis<br />
philippensis. The shrub layer is typically sparse <strong>and</strong> comprises species including Murraya<br />
ovatifoliolata, Glycosmis trifoliata, Jasminum elongata, Trophis sc<strong>and</strong>ens, Eugenia<br />
reinwardtiana, Grewia oxyphylla, Diospyros reticulata, Manilkara kauki, Flagellaria indica,<br />
Drypetes deplanchei, Exocarpos latifolius, Pleomele angustifolia, Opilia armentacea,<br />
Jacquemontia paniculata, Memecylon pauciflorum, Cupaniopsis flagelliformis var. flagelliformis,<br />
Aglaia elaeagnoidea, Salacia disepala, Diospyros compacta, Triflorensia australis, Litsea<br />
glutinosa, Archidendron gr<strong>and</strong>iflorum, Stephania japonica, Cissus maritima, Macaranga<br />
tanarius, Micromelum minutum <strong>and</strong> *Passiflora foetida. The community has been assigned the<br />
sub-type grouping of RE3.12.35a following Herbarium recommendations.<br />
Photograph 164. Deciduous vine<br />
thicket type 2h at Site YA05, Iama<br />
Isl<strong>and</strong>.<br />
<strong>Vegetation</strong> Community 2o: Rocky granitic knolls on Moa Isl<strong>and</strong> present habitat for VC2o,<br />
which in context of the Torres Strait Isl<strong>and</strong>s, is a well-developed semi-deciduous to semievergreen<br />
vine forest type. The community is represented unde the sub-type classification of<br />
RE3.12.35c, based on herbarium recommendations. This is a tall community with a canopy<br />
height range of 23 to 35m <strong>and</strong> a typically diverse floristic assemblage which includes (in order of<br />
decreasing dominance) Maranthes corymbosa, Buchanania arborescens, Cryptocarya sp.<br />
(DGF8917+), Acacia auriculiformis, Syzygium forte subsp. forte, Barringtonia calyptrata,<br />
Gmelina dalrympleana, Polyscias elegans, Bombax ceiba var. leiocarpum, Sterculia quadrifida,<br />
Endi<strong>and</strong>ra glauca, Carallia brachiata, Commersonia bartramia, Mimusops elengi, Canarium<br />
australianum, Myristica insipida, Beilschmiedia obtusifolia, <strong>and</strong> *Mangifera indica on the<br />
community margins.<br />
The sub-canopy comprises species typical of the canopy with additional species including<br />
Endi<strong>and</strong>ra glauca, Polyscias elegans, Cleistanthus peninsularis, Garcinia warrenii, Cryptocarya<br />
hypospodia, Rhodomyrtus macrocarpa, Polyalthia australis, Ptychosperma elegans <strong>and</strong><br />
Myristica insipida. Shrub layers are evergreen <strong>and</strong> relatively well-developed with species<br />
including Pleomele angustifolia, Drypetes deplanchei, Cliestanthus peninsularis, Flagellaria<br />
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indica, Salacia disepala., Morinda citrifolia, Smilax calophylla, Ganophyllum falcatum,<br />
Cryptocarya hypospodia, Alstonia actinophylla, Chionanthus ramiflora, Diospyros sp. (Mt White<br />
P.I. Forster PIF 14415), Melicope peninsularis, Micromelum minutum, Cryptocarya exfoliata,<br />
Opilia armentacea, Cupaniopsis anacardioides, Macaranga tanarius, Premna dallachyana,<br />
Dischidia ovata, Litsea breviumbellata <strong>and</strong> Cyclophyllum brevipes. The Rare listed species<br />
Archidendron hirsutum was a prominent component of the shrub layer.<br />
Photograph 165. Sub-canopy<br />
structure of VC2o on Moa Isl<strong>and</strong><br />
(Site MO003).<br />
<strong>Vegetation</strong> Community 2q: The best development of the RE3.12.35 is provided by VC2q,<br />
restricted to Muralug Isl<strong>and</strong> with notable communities found in the Port Lihou area on the<br />
southern coastal flats. In this location, the community occupies a number of rocky diorite knolls<br />
which protrude above a broad alluvial plain. The canopy is dominated by deciduous species with<br />
a height range of 25 to 40m. Typical canopy species include Berrya javanica, Bombax ceiba var.<br />
leiocarpum, Albizia lebbeck, Antiaris toxicaria var. macrophylla, Canarium australianum,<br />
Maranthes corymbosa, Terminalia complanata, Garuga floribunda var. floribunda, Cordia myxa,<br />
Buchanania arborescens, Beilschmiedia obtusifolia, Ficus virens var. sublanceolata, Aidia<br />
racemosa, Indigator fordii, Myristica insipida, Aidia racemosa <strong>and</strong> Lagerstroemia archeriana.<br />
The shrub layer is relatively open which highlights the impressive stature of this forest. The<br />
luxuriant development of this community in this location is undoubtedly assisted by the inherent<br />
fertility of the diorite, which has weathered to feed a black soil plain that forms a broad apron<br />
around the rocky l<strong>and</strong>forms. The record of Indigator fordii represents a highly disjunct<br />
occurrence of an extremely rare species known previously from only four to six trees on the<br />
southern slopes of the McIlwraith Range (see Halford 2002). Cheek (2007) recommends a<br />
conservation status of Critically Endangered under IUCN criteria by virtue of its vulnerability to<br />
stochastic change because it occurs at a single location with a population of fewer than 50<br />
individuals. The community is represented under the sub-type of RE3.12.35d based on<br />
Herbarium recommendations.<br />
<strong>Vegetation</strong> community 2r: The community is restricted to Hammond Isl<strong>and</strong> where it occupies<br />
boulder slopes formed on diorite, <strong>and</strong> is classified under the sub-type of RE3.12.35e. The canopy<br />
is typically broken, ranging in height from 10m to 28m, with ridgeline <strong>and</strong> some disturbed lower<br />
slope communities verging on vine thickets. The floristic feature which distinguishes VC2r from<br />
other communities in this group is the prominence of Alstonia actinophylla as a canopy species,<br />
although the full range of species may include Paraserianthes toona, Vitex acuminata, Canarium<br />
australianum, Buchanania arborescens, Sterculia quadrifida, Acacia polystachya, Maniltoa<br />
lenticellata var. lenticellata, Cleistanthus peninsularis, Cryptocarya cunninghamii, Maranthes<br />
corymbosa, Calophyllum sil, Endi<strong>and</strong>ra impressicosta, Zanthoxylum rhetsa <strong>and</strong> Endi<strong>and</strong>ra<br />
glauca. Where the community has been subject to disturbance, such as on wind exposed<br />
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idgelines, Acacia polystachya may form a low closed canopy, <strong>and</strong> these variations have mapped<br />
as VC6e, although incorporated into the broader RE classification. <strong>Vegetation</strong> community 6e is<br />
represented under the sub-type of RE3.12.35f with VC6a, which is discussed below. The<br />
community is illustrated in Photograph 167.<br />
Photograph 166. A well-developed<br />
example of VC2q on Muralug<br />
Isl<strong>and</strong>. Diorite talus is clearly visible<br />
on the ground surface.<br />
Photograph 167. The footslope<br />
margins of VC2r on Hammond<br />
Isl<strong>and</strong> with emergent Alstonia<br />
actinophylla visible in the<br />
background.<br />
<strong>Vegetation</strong> Community 2t: <strong>Vegetation</strong> community 2t is a rather poorly constrained type due to<br />
limited floristic sampling across its mapped range which is extensive throughout the Inner Isl<strong>and</strong><br />
Group including portions of the Inner Western Group <strong>and</strong> Mt. Adolphus Isl<strong>and</strong>. It is likely that<br />
further floristic sampling within this VC would result in a number of additional types being<br />
recognised. At present, VC2t represents the default vine forest community for the Inner Isl<strong>and</strong><br />
Group, comprising vine forest communities classified largely through informal observation that<br />
cannot be classified adequately through lack of floristic data. The community has been assigned<br />
the sub-type grouping of RE3.12.35a following Herbarium recommendations. The description of<br />
this VC is based largely on descriptions from Naghir Isl<strong>and</strong> (NAQ02), although in the majority of<br />
mapped areas, it is expected that the dominant species which include Bombax ceiba var.<br />
leiocarpum, Canarium australianum <strong>and</strong> Terminalia subacroptera remain relatively constant.<br />
The community on Naghir forms a closed forest community with canopy range of 20m to 25m<br />
tall comprising in order of decreasing abundance Bombax ceiba var. leiocarpum, Terminalia<br />
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subacroptera., Acacia polystachya, Erythrina variegata., Buchanania arborescens, Canarium<br />
australianum, Sterculia quadrifida, Manilkara kauki, Gyrocarpus americanus, Antiaris toxicaria<br />
var. macrophylla, Ficus virens <strong>and</strong> Ganophyllum falcatum. The sub-canopy forms a height of 12<br />
to 18m. composed of Buchanania arborescens, Chionanthus ramiflora, Drypetes deplanchei,<br />
Atalaya sericopetala, Diospyros maritima, Celtis philippensis with a typical shrub layer formed<br />
by Chionanthus ramiflora, Drypetes deplanchei, Memecylon pauciflorum, Cupaniopsis<br />
anacardioides, Atalaya sericopetala, Capparis sepiaria, Diospyros sp. (DGF9121+), Diospyros<br />
maritima, Micromelum minutum, Celtis philippensis, Cryptocarya exfoliata, Diospyros compacta,<br />
Exocarpos latifolius, Salacia disepala, Elaeodendron melanocarpum, Pleomele angustifolia,<br />
Murraya ovatifoliolata, Ganophyllum falcatum, Cliestanthus peninsularis, Phyllanthus novaeholl<strong>and</strong>iae,<br />
Wrightia pubescens subsp. penicillata <strong>and</strong> Miliusa brahei.<br />
Photograph 168. Typical subcanopy<br />
structure of VC2t on Naghir<br />
Isl<strong>and</strong> (Site NAQ02).<br />
<strong>Vegetation</strong> Community 6a: <strong>Vegetation</strong> Community 6a, represented in Photograph 169, is<br />
restricted largely to Iama Isl<strong>and</strong>, with a minor occurrence also mapped on Gebar to the immediate<br />
north-west. In conjunction with the previously mentioned VC6e, the community is classified<br />
under the sub-type of RE3.12.35f. The canopy of this community presents a height range from<br />
12 to 23m, typically broken <strong>and</strong> dominated by Acacia auriculiformis with scattered deciduous<br />
vine forest species including Canarium australianum, Terminalia subacroptera, Bombax ceiba<br />
var. leiocarpum, <strong>and</strong> Diospyros hebecarpa. The sub-canopy is relatively open, comprising vine<br />
forest species including Cupaniopsis anacardioides, Terminalia subacroptera, Diospyros<br />
hebecarpa, Micromelum minutum, <strong>and</strong> Wrightia pubescens subsp penicillata. Sub dominant <strong>and</strong><br />
associated species include Bombax ceiba var. leiocarpum, Canarium australianum, Cryptocarya<br />
exfoliata, Antiaris toxicaria var. macrophylla, Acacia auriculiformis, Aidia racemosa, Opilia<br />
armentacea, *Mangifera indica, Psydrax sp. <strong>and</strong> Manilkara kauki.<br />
The understorey is diverse with Salacia chinensis, Micromelum minutum, Wrightia pubescens<br />
subsp. penicillata, Pleomele angustifolia, Cupaniopsis anacardioides, Diospyros compacta,<br />
Cryptocarya exfoliata, Litsea glutinosa, Memecylon pauciflorum, Exocarpos latifolius, Secamone<br />
elliptica, Terminalia subacroptera, Diospyros maritima, Tabernaemontana orientalis, Litsea<br />
glutinosa, Opilia armentacea, Psydrax sp., Breynia cernua, Ixora timorensis, Trophis sc<strong>and</strong>ens,<br />
Luvunga monophylla, Arytera bifoliolata, Jasminum sp., Turraea pubescens, Flagellaria indica,<br />
Streblus brunonianus, Drypetes deplanchei, Garcinia warrenii, Diospyros hebecarpa, Diospyros<br />
reticulata, Chionanthus ramiflora, Archidendron gr<strong>and</strong>iflorum, Murraya ovatifoliolata,<br />
Macaranga tanarius, Drypetes deplanchei, Phaleria oct<strong>and</strong>ra, Capparis quiniflora, Antidesma<br />
parvifolium, Eugenia reinwardtiana, <strong>and</strong> Dalbergia densa var. australis.<br />
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It is envisaged, as is the general case with most Acacia dominant forests, that this community has<br />
developed in response to disturbance. The nature of this disturbance is unknown, although the<br />
forest community would be expected to burn in hot conditions, with evidence from old charred<br />
stumps that it is occasionally burnt, largely in a wildfire regime. It is understood that gardens<br />
occurred on hillsides of the interior <strong>and</strong> that people would cut down the trees in a garden area,<br />
then burn them <strong>and</strong> move on the following year (Kepa/Hitchcock pers. com 2008). Further<br />
evidence is offered by Haddon (1901, pp 25) who recounts the observations by Jukes (1847 pp.<br />
155-7) where: “On Turtle-backed Isl<strong>and</strong> we found a few small groves of cocoa-nut trees near a<br />
group of huts, with a little thicket of bamboo; <strong>and</strong> near the centre of the isl<strong>and</strong>, following a little<br />
path through a matted wood, rendered impervious by creepers, we came [on]. . .a little circular<br />
plot of ground, not more than four or five yards in diameter; but it had evidently been dug,<br />
though in a crude manner, <strong>and</strong> in it were set several young plantain-trees, one or two other<br />
plants, <strong>and</strong> two trailing plants…which we afterwards found were a kind of yam”.<br />
It is therefore likely that a combination of both human disturbance, wind <strong>and</strong> fire played a role in<br />
the development of this forest type. That this community is found only on Iama Isl<strong>and</strong> presents<br />
another puzzle. The nearby continental isl<strong>and</strong>s of Mabuiag <strong>and</strong> Gebar are dominated by<br />
Welchiodendron forests, although not a single individual of this plant was found on Iama. It is<br />
clear that despite a close proximity, forests on Iama has developed independently from forest<br />
types on neighbouring isl<strong>and</strong>s.<br />
The high biodiversity values that this ecosystem attracts on the basis of its uniqueness in the subregional,<br />
regional <strong>and</strong> national contexts, is further strengthened by its provision of habitat for<br />
Luvunga monophylla (Rutaceae). The occurrence on Iama Isl<strong>and</strong> is a new record for Queensl<strong>and</strong><br />
extending geographical range eastwards from the eastern Arnhem coast of the Northern Territory.<br />
This multi-stemmed shrub of the understorey occurs in coastal vine thickets of the East<br />
Kimberley, Northern Territory <strong>and</strong> also from the Philippines with records from Timor (Hyl<strong>and</strong> et<br />
al. 1995). Luvunga is of tribe Citreae (Rutaceae: subfam. Aurantioideae) <strong>and</strong> the the sole<br />
Australian representative of the Citrus subtribe ‘Triphasiinae’ (Mabberley 1998). It was first<br />
collected in the Sir Edward Pellew Group, Gulf of Carpentaria, in December 1802 by Robert<br />
Brown during Flinders Investigator circumnavigation of Australia with additional collections<br />
gathered a few months later in Timor by J.B.L.C.T. Leschenault de la Tour on Baudin’s voyage<br />
(Mabberley 1998). Luvunga is relatively common in its habitat on Iama among rocky boulder<br />
slopes <strong>and</strong> hillcrests. The species is of ‘least concern’ according to NT legislation.<br />
Photograph 169. The internal forest<br />
structure of VC6a (RE3.12.35f) on<br />
Iama Isl<strong>and</strong> (YA18).<br />
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5.2.75 <strong>Regional</strong> Ecosystem 3.12.36 (New RE)<br />
Preliminary Description: Evergreen to complex evergreen mesophyll to notophyll vine forest<br />
<strong>and</strong> thicket on mountain ranges of Torres Strait Isl<strong>and</strong>s.<br />
Status: Of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 1a, 1e, 1f, 1b, 1g, 1h<br />
Reference Sites: 3 Secondary (DA20, MO82, MO150)<br />
A new RE has been erected to accommodate evergreen vine forest <strong>and</strong> thicket communities of the<br />
Torres Strait Isl<strong>and</strong>s. Representation of vine forests is provided by VC1a, VC1e <strong>and</strong> VC1f, being<br />
thes most luxuriant development of vine forest in the isl<strong>and</strong> group <strong>and</strong> are assigned to the subtype<br />
RE3.12.36a. A number of evergreen vine thicket communities are also described under this<br />
classification, recognised under the sub-type RE3.12.6b. On Cape York Peninsula, evergreen<br />
forest on granitic upper slopes is recognised on Mt Cook <strong>and</strong> south into the ranges of the northern<br />
Wet Tropics Bioregion, on upl<strong>and</strong> areas of the Melville Range, <strong>and</strong> on the granitic upl<strong>and</strong>s of the<br />
McIlwraith Range. The communities recognised in the study area display significant floristic<br />
differences to the previously described Cape York RE’s <strong>and</strong> warrant individual recognition.<br />
These communities are mapped on a number of the more mountainous isl<strong>and</strong>s including Moa,<br />
Dauan, <strong>and</strong> Mt. Adolphus.<br />
<strong>Vegetation</strong> Community 1a: <strong>Vegetation</strong> Community 1a is mapped on the steep upper boulder<br />
slopes of Mt Cornwallis on Dauan Isl<strong>and</strong> where it forms an evergreen notophyll vine forest. The<br />
canopy is relatively low at 15 to 25m height <strong>and</strong> is windswept in exposed locations. Dominant<br />
canopy species include Ganophyllum falcatum, Arytera divaricata, Mangifera indica, Ficus<br />
microcarpa, Alstonia spectabilis, Celtis paniculata, Syzygium puberulum, Calophyllum sil,<br />
Buchanania arborescens, Dysoxylum oppositifolium, Acmenospermum claviflorum, Schefflera<br />
actinophylla, Endi<strong>and</strong>ra impressicosta, Cryptocarya cunninghamii <strong>and</strong> Ficus destruens. Amongst<br />
the sub-canopy species, Garcinia warrenii, Endi<strong>and</strong>ra impressicosta, Garcinia dulcis,<br />
Cupaniopsis anacardioides, Aglaia elaeagnoidea <strong>and</strong> Ficus virens var. sublanceolata were<br />
frequent. The shrub layer <strong>and</strong> ground cover was relatively complex with associated species<br />
including Pleomele angustifolia, Capparis lucida, Haplosticanthus fruticosus, Zanthoxylum<br />
rhetsa, Macaranga tanarius, Litsea glutinosa, Leea indica, Memecylon pauciflorum,<br />
Archidendron gr<strong>and</strong>iflorum, Ptychosperma macarthurii, Trophis sc<strong>and</strong>ens, Chionanthus<br />
ramiflora, Glycosmis trifoliata, Alectryon rep<strong>and</strong>odentatus (E), <strong>and</strong> Smilax australis. Epiphytes,<br />
climbing epiphytes <strong>and</strong> ferns are particularly abundant in response to the permanently moist<br />
upl<strong>and</strong> environment with ferns such as Nephrolepis biserrata, Drynaria qeurcifolia, Drynaria<br />
sparsisora <strong>and</strong> Pyrrosia longifolia. Epiphyic orchids are a feature together with abundant Hoya<br />
<strong>and</strong> Dischidia species.<br />
The RE provides the only known ‘Australian’ habitat of Dischidia littoralis (Vulnerable NCA)<br />
(Forster <strong>and</strong> Liddle 1993) which was recollected on the survey (<strong>and</strong> also from Mabuiag Isl<strong>and</strong>).<br />
The record of Alectryon rep<strong>and</strong>odentatus (Endangered NCA, Vulnerable IUCN) in the shrub<br />
layer is significant, being an extension of range <strong>and</strong> habitat for a species otherwise previously<br />
known in Australian territory only from the basaltic eastern isl<strong>and</strong>s <strong>and</strong> Lockerbie (Cape York)<br />
although it is widespread in PNG (see Conn et al. 2006+). The prominence of Mangifera indica<br />
(Mango) in the upper stratum of this forest also requires mention, as the species appears to be<br />
long established <strong>and</strong> naturalised. Information from traditional owners on Dauan Isl<strong>and</strong> suggests<br />
that the species was established as a potential food source for when under attack, the population<br />
retreated to the mountain tops.<br />
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Photograph 170. Evergreen<br />
notophyll vine forest near the<br />
summit of Mt Cornwallis. The<br />
boulder covered in epiphytes is<br />
typical.<br />
<strong>Vegetation</strong> Community 1e: <strong>Vegetation</strong> Community 1e which was sampled at Site MO82 occurs<br />
on the footslopes of Banks Peak (Moa Isl<strong>and</strong>), occupying often steep sheltered slopes with<br />
southern aspect <strong>and</strong> formed on coarse biotite granite. Weathering of the granite has produced a<br />
well-drained <strong>and</strong> relatively fertile s<strong>and</strong>y loam soil which has favoured development of a welldeveloped<br />
mesophyll vine forest. The canopy has a height range of 23 to 35m with the dominant<br />
species being Myristica insipida, Dysoxylum latifolium, Cryptocarya cunninghamii, Sterculia<br />
shillinglawii subsp. shillinglawii <strong>and</strong> Calophyllum sil. Canopy sub dominants include Maranthes<br />
corymbosa, Semecarpus australiensis, Aglaia tomentosa, Mimusops elengi, Buchanania<br />
arborescens, Aidia racemosa <strong>and</strong> Endi<strong>and</strong>ra glauca. Sub-canopy species are typified by<br />
Endi<strong>and</strong>ra glauca, Cryptocarya cunninghamii, Sterculia shillinglawii subsp. shillinglawii,<br />
Carallia brachiata, Cryptocarya hypospodia, Arenga australasica (V), Calophyllum sil, Psydrax<br />
sp. (DGF8955+), Epipremum pinnatum, <strong>and</strong> Entada rheedii.<br />
Photograph 171. Arenga<br />
australasica is prominent in the sub<br />
canopy <strong>and</strong> shrub layers in VC1e<br />
(Site MO083).<br />
Shrub layers are relatively well-developed <strong>and</strong> diverse with a complex array of species which<br />
include Arenga australasica (V), Ptychosperma macarthurii, Hydriastele wendl<strong>and</strong>iana,<br />
Flagellaria indica, Cryptocarya cunninghamii, Psydrax sp. (DGF8955+), Sterculia shillinglawii<br />
subsp. shillinglawii (R), Aglaia tomentosa, Calophyllum sil, Endi<strong>and</strong>ra glauca, Cryptocarya<br />
hypospodia, Arytera divaricata, Dysoxylum latifolium, Smilax calophylla, Archidendron hirsutum<br />
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(R), Wilkiea rigidifolia, Archidendron gr<strong>and</strong>iflorum, Mallotus philippensis, Glycosmis trifoliata,<br />
Barringtonia calyptrata, Macaranga involucrata var. mallotoides, Polyscias macgillivraei,<br />
Atractocarpus sessilis, Salacia disepala, Chionanthus ramiflora, Micromelum minutum,<br />
Cryptocarya hypospodia, Arytera divaricata, Arytera bifoliolata, Phaleria oct<strong>and</strong>ra,<br />
Mischocarpus lachnocarpus, Polyalthia australis, <strong>and</strong> Pleomele angustifolia.<br />
The prominence of Arenga australasica, listed as Vulnerable under both EPBC (1999) <strong>and</strong> the<br />
NCA (1992) is a noteworthy feature of this forest, along with additional rare <strong>and</strong> threatened<br />
species listed in the type description <strong>and</strong> a number of species at the limit of geographical range in<br />
Australian territory.<br />
<strong>Vegetation</strong> Community 1f: The upper slopes of Banks Peak on Moa Isl<strong>and</strong>, at an elevation of<br />
399m, host a tall well-developed notophyll vine forest which presents a complex array of<br />
structural features. This community, represented as VC1f, presents the best-developed example<br />
of vine forest in the study area <strong>and</strong> is described as a complex notophyll vine forest. Canopy<br />
heights in this community vary depending on exposure although canopies observed on sheltered<br />
leeward slopes attain heights of greater than 30m. The sub-dominant stratum form a number of<br />
poorly differentiated layers which tend to merge in places, <strong>and</strong> it is these layers that present the<br />
greatest life form complexity. Typical canopy species include Calophyllum sil, Argyrodendron<br />
poly<strong>and</strong>rum, Cryptocarya cunninghamii, Syzygium br<strong>and</strong>erhorstii, Syzygium buettnerianum,<br />
Archidendron hirsutum (Rare), Anthocarapa nitidula, Pouteria obovata, Acmenospermum<br />
claviflorum, Canarium vitiense, Gomph<strong>and</strong>ra australiana, Pouteria sp. (DGF9168+), Syzygium<br />
forte subsp. forte, Maranthes corymbosa, Palaquium galatoxylon, Ficus microcarpa, Horsfieldia<br />
australiana, Licuala ramsayi <strong>and</strong> Maniltoa lenticellata var. lenticellata.<br />
The sub-canopy layer which ranges in height from 12 to 18m is dominated by Licuala ramsayi<br />
with associated species including Cryptocarya cunninghamii, Psydrax sp. (DGF8955+),<br />
Ptychosperma elegans, P<strong>and</strong>anus zea, Pouteria obovata, Canarium vitiense, Buchanania<br />
arborescens, Aglaia sapindina, Epipremnum pinnatum, Pouteria sp. (DGF9168+), Maranthes<br />
corymbosa, Podocarpus grayae, Meiogyne sp. (DGF9718+), Pimeleodendron amboinicum (R)<br />
<strong>and</strong> Maniltoa lenticellata var. lenticellata. Shrub layers, typically 1.5 to 10m are typified by<br />
Meiogyne sp. (9718+), Pimeleodendron amboinicum, Cryptocarya cunninghamii, Licuala<br />
ramsayi, Codiaeum variegatum var. moluccanum, Atractocarpus sessilis, Acmenosperma<br />
claviflorum, P<strong>and</strong>anus zea, Piper caninum, Polyscias australiana, Psydrax sp. (DGF9154+),<br />
Flagellaria indica, Pouteria obovata, Diospyros sp. (DGF9160+), Aglaia sapindina,<br />
Gomph<strong>and</strong>ra australiana, Myristica insipida, Polyscias macgillivraei, Chionanthus ramiflora,<br />
Salacia chinensis <strong>and</strong> Maniltoa lenticellata var. lenticellata.<br />
Photograph 172. Aerial view of<br />
VC1f on Banks Peak showing.<br />
Licuala ramsayi visible in canopy.<br />
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This habitat is unique in the national <strong>and</strong> regional context. The micro-climatic <strong>and</strong> edaphic<br />
conditions provide a permanently moist ‘upl<strong>and</strong>’ habitat exhibiting important floristic evidence of<br />
biological connectivity with mesothermal upl<strong>and</strong>s of the south <strong>and</strong> neighbouring PNG. Although<br />
further research <strong>and</strong> analysis is warranted utilising the survey data set, preliminary evidence<br />
reveals populations of a number of mesic taxa known previously north to the Lockerbie forests<br />
<strong>and</strong>/or Muralug. These include but are not limited to Acmenosperma claviflorum, Aglaia<br />
sapindina, Aglaia tomentosa, Argyrodendron poly<strong>and</strong>rum, Atractocarpus sessilis,<br />
Pimeleodendron amboinicum, Cryptocarya cunninghamii, Licuala ramsayi, Canarium vitiense,<br />
Codiaeum variegatum var. moluccana, Endi<strong>and</strong>ra impressicosta, Epipremum amplissimum,<br />
Gomph<strong>and</strong>ra australiana, Maniltoa lenticellata var. lenticellata, Neolitsea brassii, Palaquium<br />
galactoxylon, P<strong>and</strong>anus zea, Podocarpus grayae, Polyscias australiana, Sterculia shillinglawii<br />
subsp. shillinglawii, Syzygium bamagense, Syzygium puberulum, <strong>and</strong> Terminalia complanata.<br />
Colections of Pouteria sp. (DGF9168+DJS) one of the dominant canopy rainforest trees on<br />
Banks Peak, <strong>and</strong> Meiogyne sp. (Moa Is. DGF9718+DJS), are currently unplaced in the<br />
Queensl<strong>and</strong> Flora <strong>and</strong> await Herbarium determination. The occurrence of Podocarpus represents<br />
the occurrence of a relictual Godwanan taxon <strong>and</strong> its northern extent of distribution.<br />
Photograph 173. The complex subcanopy<br />
structure of VC1f on Banks<br />
Peak (MO150) showing Licuala<br />
ramsayi <strong>and</strong> the stilt roots of a<br />
P<strong>and</strong>anus species thought to be<br />
P<strong>and</strong>anus zea.<br />
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<strong>Vegetation</strong> Community 1b: This community is represented as a windsheared evergreen vine<br />
thicket <strong>and</strong> occasional forest formed on exposed granite boulder footslopes of Dauan Isl<strong>and</strong>. The<br />
canopy height is variable depending on position in relation to rock boulders. Taller communities<br />
typically form in sheltered crevasses where the canopy may reach 12m. In exposed locations, the<br />
canopy may be significantly lower. Dominant canopy species include Manilkara kauki, Intsia<br />
bijuga, Pouteria sericea, Garcinia warrenii, Aglaia elaeagnoidea, Chionanthus ramiflora,<br />
Diospyros reticulatus, Drypetes deplanchei, Ptychosperma macarthurii, Buchanania<br />
arborescens, P<strong>and</strong>anus sp., Ficus microcarpa, <strong>and</strong> Pouteria obovoidea. A shrub layer ranging in<br />
height from 0.5m to 3m is the dominant sub-canopy stratum. Typical species of this shrub layer<br />
include Trophis sc<strong>and</strong>ens, Alyxia spicata, Cleistanthus peninsularis, Tabernaemontana<br />
orientalis, Glycosmis trifoliata, Cupaniopsis anacardioides, Aglaia elaeagnoidea, Flagellaria<br />
indica <strong>and</strong> Smilax australis.<br />
Photograph 174. The typical<br />
internal structure of VC1b on Dauan<br />
Isl<strong>and</strong> (DA04).<br />
<strong>Vegetation</strong> Community 1g: <strong>Vegetation</strong> Community 1b represents a windsheared evergreen<br />
notophyll vine thicket that is restricted to exposed, elevated <strong>and</strong> steep escarpments on Moa<br />
Isl<strong>and</strong>. The type description is obtained from Site MA151 on Banks Peak where sheltered<br />
leeward slopes host the much better developed VC1f. The typical canopy is even at 6m to 8m<br />
height with representative species comprising Podocarpus grayae, Anthocarapa nitidula,<br />
Diospyros hebecarpa, Syzygium bungadinnia, Dillenia alata, Licuala ramsayi, Ptychosperma<br />
elegans, Calophyllum sil, P<strong>and</strong>anus zea, Cryptocarya cunninghamii, Buchanania arborescens,<br />
Rhodomyrtus macrocarpa, Psydrax sp. (DGF9154+), Pouteria obovata, Antiaris toxicaria var.<br />
macrophylla, Schefflera actinophylla, Canarium vitiense, Acacia auricauliformis <strong>and</strong> Polyscias<br />
elegans. As with the majority of the windsheared thicket types, the sub-canopy is sparse although<br />
a range of species including Atractocarpus sessilis, Codiaeum variegatum, Aglaia sapindina,<br />
Wilkiea rigidifolia, Neolitsea brassii, Sterculia quadrifida, Mischocarpus lachnocarpus, Litsea<br />
breviumbellata, Hydnophytum mosleyanum var. moselyanum, Helicia australasica, Syzygium<br />
buettnerianum (R), <strong>and</strong> Sterculia sp. (Annan River) were recorded in the sub-canopy <strong>and</strong> shrub<br />
layers.<br />
<strong>Vegetation</strong> Community 1h: An extremely restricted notophyll thicket community that is<br />
confined to the steep upper slopes of Mabuiag Isl<strong>and</strong>. The community is structurally similar to<br />
VC1g although floristic composition varies significantly. The dominant canopy, which ranges<br />
from 6m to 8m comprises Buchanania arborescens, Drypetes deplanchei, Elaeodendron<br />
melanocarpum, Endi<strong>and</strong>ra glauca, Elaeocarpus arnhemicus, Chionanthus ramiflora, Dysoxylum<br />
oppositifolium, Cliestanthus peninsularis, Rhodomyrtus macrocarpa, Canarium australianum,<br />
Ganophyllum falcatum, Calophyllum sil, *Mangifera indica <strong>and</strong> Arytera divaricata. The sub-<br />
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canopy forms a poorly defined stratum ranging in height from 1.5m to 6m <strong>and</strong> is composed of<br />
Haplosticanthus fruticosus, Rhodomyrtus macrocarpa, Pleomele angustifolia, Diospyros<br />
hebecarpa, Streblus brunonianus, Arytera bifoliolata, Cyclophyllum maritimum, Flagellaria<br />
indica, Psychotria sp., Diospyros sp. (Bamaga B.P.Hyl<strong>and</strong> 2517), Ganophyllum falcatum,<br />
Phaleria oct<strong>and</strong>ra, Arytera divaricata, Salacia disepala, Cryptocarya exfoliata, Elaeodendron<br />
melanocarpum, Dendrobium discolor <strong>and</strong> Secamone elliptica. Drynaria quercifolia forms the<br />
dominant ground cover.<br />
<strong>Vegetation</strong> Community 1h represents a much drier thicket type that VC1g <strong>and</strong> this is reflected in<br />
the species composition. The limited height development of this community, <strong>and</strong> possibly its<br />
species composition is also influenced by the mobile acid volcanic talus slope, which it occupies.<br />
Photograph 175. The internal<br />
structure of windsheared notophyll<br />
vine thicket type 1g. Site MA151.<br />
Photograph 176. The steep<br />
windward slope of Banks Peak<br />
demonstrating the evergreen <strong>and</strong><br />
windsheared structure of VC1g.<br />
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5.2.76 <strong>Regional</strong> Ecosystem 3.12.37 (New RE)<br />
Photograph 177. Evergreen<br />
notophyll thicket VC1h on Mabuiag<br />
Isl<strong>and</strong>. Site MA48.<br />
Preliminary Description: Eucalyptus platyphylla +/- Corymbia stockerii +/- Corymbia<br />
clarksoniana woodl<strong>and</strong> to open woodl<strong>and</strong> on coastal hills.<br />
Status (Preliminary): Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5t, 5u<br />
Reference Sites: 8 Quaternary.<br />
A new RE has been erected to incorporate Eucalyptus platyphylla dominant communities that are<br />
manifest on coastal headl<strong>and</strong>s <strong>and</strong> footslopes of the Inner Isl<strong>and</strong> Group. The RE comprises VC5t<br />
<strong>and</strong> VC5u, restricted to Horn <strong>and</strong> Muralug Isl<strong>and</strong>s respectively.<br />
<strong>Vegetation</strong> Community 5t: This community is mapped exclusively on Horn Isl<strong>and</strong>, where it<br />
represents a relatively extensive woodl<strong>and</strong> <strong>and</strong> open forest community on the isl<strong>and</strong>s eastern side.<br />
The canopy of this community ranges from 18 to 27m <strong>and</strong> comprises (in order of decreasing<br />
abundance) Eucalyptus platyphylla, Corymbia stockeri subsp. peninsularis, Corymbia nesophila<br />
<strong>and</strong> Welchiodendron longivalve. The community often demonstrates a relatively well-developed<br />
shrub layer composed of Welchiodendron longivalve <strong>and</strong> Acacia spp. Limited floristic sampling<br />
was undertaken in this community <strong>and</strong> further structural survey would aid its description.<br />
Photograph 178. <strong>Vegetation</strong><br />
Community 5t on the eastern side of<br />
Horn Isl<strong>and</strong>.<br />
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<strong>Vegetation</strong> Community 5u: Similar to VC5t, community 5u was subject to limited structural<br />
sampling, with community description ascertained largely from quaternary observation. The<br />
structural characteristics were however relatively distinctive, forming localised areas of open to<br />
sparse woodl<strong>and</strong>, mostly restricted to acid volcanic coastal headl<strong>and</strong>s on Muralug Isl<strong>and</strong>. Canopy<br />
heights are estimated at 18m to 25m with canopy cover generally less than 25%. The dominant<br />
canopy species is Eucalyptus platyphylla with scattered Corymbia tessellaris <strong>and</strong> associated but<br />
uncommon Eucalytpus cullenii. The shrub layer is sparse, generally comprising Cochlospermum<br />
gillivraei <strong>and</strong> Acacia spp. with ground cover formed by Themeda tri<strong>and</strong>ra interspersed with rock<br />
pavement <strong>and</strong> talus. A broad area of this community was identified on the south-western portion<br />
of Badu Isl<strong>and</strong> (see Garnett <strong>and</strong> Jackes 1983). Due to the paucity of the field survey effort on<br />
Badu Isl<strong>and</strong>, coupled with the broad scale of the aerial photography used for the interpretation,<br />
the location <strong>and</strong> extent of this community could not be verified.<br />
Photograph 179. <strong>Vegetation</strong><br />
Community 5u on acid volcanic<br />
headl<strong>and</strong>. Muralug Site PW038.<br />
5.2.77 <strong>Regional</strong> Ecosystem 3.12.38 (New RE)<br />
Description: Corymbia clarksoniana + Corymbia stockerii + Corymbia nesophila low mixed<br />
woodl<strong>and</strong> of Torres Strait Isl<strong>and</strong>s.<br />
Status: Not of Concern<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 5d, 14p, 13a<br />
Reference Sites: 5 Quaternary<br />
<strong>Regional</strong> Ecosystem 3.12.38 is new RE classification restricted entirely to Moa Isl<strong>and</strong> where it<br />
occupies skeletal soils formed on hard white acid volcanic rock. The constituent VC’s comprise<br />
shrubl<strong>and</strong> <strong>and</strong> low woodl<strong>and</strong> expressions as described below in VC’s 5d <strong>and</strong> 14p. Small areas of<br />
Melaleuca viridiflora woodl<strong>and</strong> separate from this community <strong>and</strong> are also included under this<br />
classification.<br />
Vegation Community 5d: This community represents low woodl<strong>and</strong> comprising a mix of<br />
species from a range of genera. The canopy forms with a height range between 6m <strong>and</strong> 10m with<br />
cover typically 25% to 40%. Constituent species include Corymbia clarksoniana, Corymbia<br />
nesophila, Corymbia stockeri subsp. peninsularis, Asteromyrtus brassii, Melaleuca viridiflora,<br />
Melaleuca stenostachya, Petalostigma pubescens, Acacia leptocarpa <strong>and</strong> Welchiodendron<br />
longivalve. The relative contribution that these species make to total canopy cover varies<br />
although Corymbia spp. is always a canopy component. Secondary shrub layers are variable<br />
although Melaleuca viridiflora, Melaleuca stenostachya <strong>and</strong> Petalostigma pubescens are<br />
generally abundant. Grasses form a sparse cover over a typically skeletal substrate. Where<br />
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Corymbia spp. contribute less than 10% to the total canopy cover or are present as an emergent<br />
layer only, the community is represented as VC14p. The VC is represented in Photograph 180.<br />
Photograph 180. <strong>Vegetation</strong><br />
community 5d on acid volcanic soils.<br />
Corymbia spp. make a significant<br />
contribution to total canopy cover at<br />
this site (MO046).<br />
<strong>Vegetation</strong> Community 14p: <strong>Vegetation</strong> Community 14p (Photograph 181) mosaics with<br />
VC5d, <strong>and</strong> separation of these communities is based largely on the relative contribution<br />
Corymbia species make to the total canopy cover. The upper shrub layer typically forms at 3m to<br />
6m <strong>and</strong> is composed of Melaleuca viridiflora as a dominant with Corymbia clarksoniana, Acacia<br />
leptocarpa, Petalostigma pubescens <strong>and</strong> Asteromyrtus brassii as sub-dominant species. Acacia<br />
crassicarpa, Parinari nonda <strong>and</strong> Petalostigma pubescens are occasional canopy associates.<br />
Shrub layers are typically sparse comprising species typical of the canopy. Grasses form a sparse<br />
cover over a typically skeletal substrate. Emergents of Corymbia clarksoniana, Corymbia<br />
nesophila <strong>and</strong> Corymbia stockeri subsp. peninsularis may be present although by definition<br />
contribute less than 5% to the total canopy cover. In some locations, areas of pure Melaleuca<br />
viridiflora may separate out from the mixed shrubl<strong>and</strong>, where it is mapped as VC13a. In these<br />
locations, the community is captured within RE3.12.26x1, recognising the continuum of floristic<br />
variations occurring within the VC.<br />
Photograph 181. <strong>Vegetation</strong><br />
Community 14p at Moa Isl<strong>and</strong> Site<br />
MO124.<br />
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5.3 Retrospective Classifications<br />
L<strong>and</strong>forms suitable for human occupation have largely been cleared on the majority of inhabited<br />
isl<strong>and</strong>s <strong>and</strong> as such, the vegetation communities that once occupied these areas have been heavily<br />
impacted. Alluvial l<strong>and</strong>forms have been used almost exclusively for inhabitation <strong>and</strong> agricultural<br />
purpose <strong>and</strong> small alluvial pockets on the majority of the larger inhabited isl<strong>and</strong>s have been<br />
totally cleared with limited evidence of the floristic composition or structure of pre-disturbance<br />
vegetation types. Similarly, the elevated Tertiary remnant on the northern coast of Saibai Isl<strong>and</strong><br />
presents the most suitable area for human occupation on the isl<strong>and</strong> <strong>and</strong> has been heavily impacted<br />
by human activities. In these areas, evidence of the pre-disturbance vegetation communities can<br />
only be gathered from floristic evidence manifest in the contemporary l<strong>and</strong>scape. Two VC’s <strong>and</strong><br />
associated RE’s in the study area are presumed to be regionally extinct <strong>and</strong> these are described<br />
briefly below.<br />
5.3.1 <strong>Regional</strong> Ecosystem 3.3.1c (Cleared)<br />
Description: Closed semi-deciduous mesophyll vine forest. Mainly occurs on loamy alluvia<br />
Status: Presumed Extinct<br />
<strong>Vegetation</strong> <strong>Communities</strong>: 2xx(e), 2xx(c), 2xx(b)<br />
Reference Sites: 2 Quaternary (Dauan - DA15, 43)<br />
<strong>Vegetation</strong> Community 2xx: <strong>Vegetation</strong> community 2xx provides an example of retrospective<br />
vegetation classification with type, which is classified as mesophyll vine forest on alluvia,<br />
mapped as an RE only in pre-clearing status. All well-developed alluvial flats on isl<strong>and</strong>s such as<br />
Erub, Dauan, <strong>and</strong> Iama have been cleared <strong>and</strong> probably have been under human occupation for<br />
long periods prior to European settlement. Indications of the pre-clearing status of these flats can<br />
only be gained from examination of scattered non-remnant communities retained (although most<br />
likely highly modified) on gully lines <strong>and</strong> as scattered remnant trees. For this reason, the<br />
description of this community should be considered indicative. Isolated strips of VC2xx(e) on<br />
Dauan are currently occupied on swampy alluvium by Acacia auriculiformis, Terminalia cattapa,<br />
Myristica insipida <strong>and</strong> a range of exotic species including Mangifera indica <strong>and</strong> Cocos nucifera.<br />
The pre-clearing representation of this community is proposed to comprise a similar native<br />
species assemblage, although it is conceded that the original species assemblage is likely to be<br />
considerably more diverse. A new RE sub-type (RE3.3.1c) has been used to accommodate <strong>and</strong><br />
describe this pre-clearing community. In in the Torres Strait Isl<strong>and</strong>s, any natural occurrence is<br />
apparently extinct.<br />
Photograph 182. Semi-deciduous<br />
mesophyll vine forest dominated by<br />
Terminalia cattapa, Mangifera<br />
indica <strong>and</strong> Cocos nucifera (2xx(e))<br />
on Dauan Isl<strong>and</strong> (Site DA43).<br />
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5.4 Non-Remnant Classifications<br />
The following provides a brief explanation for, <strong>and</strong> characterisation of the non-remnant<br />
vegatation communities mapped in the Torres Strait Isl<strong>and</strong>s.<br />
Bamboo: Bamboo groves <strong>and</strong> thickets are prominent on a number of isl<strong>and</strong>s although<br />
particulary abundant on the Eastern Isl<strong>and</strong> Group of Mer, Erub <strong>and</strong> Ugar. On these isl<strong>and</strong>s,<br />
bamboo groves mosaic with adjacent vine forest communities, either spreading from former<br />
traditional garden areas on margins or as discrete groves within the forest communities. These<br />
communities are also prominent on the continental isl<strong>and</strong>s of Moa <strong>and</strong> Mabuiag, although no<br />
such examples were recognised on the Kaurareg Isl<strong>and</strong>s (Inner Isl<strong>and</strong> Group). The communities<br />
are represented as the pre-disturbance vegetation type with an appended (b).<br />
The historical record as reviewed by McNiven (2008) reveals the existence of bamboo groves<br />
throughout the Torres Strait, more specifically in the eastern isl<strong>and</strong>s in 1793, the western isl<strong>and</strong>s<br />
in 1845, <strong>and</strong> on Kirriri (Hammond) in 1867, with indications that groves continued to be<br />
established in the late nineteenth century <strong>and</strong> that the material was utilized extensively for<br />
material items (Shnukal, 2004a in McNiven 2008). Contemporary use of this important resource<br />
was observed during the field survey on Erub where large canes of the introduced Bambusa<br />
vulgaris cut for structural building purposes were lashed <strong>and</strong> soaked in the sea before use. This<br />
robust species is the most likely bamboo to form the communities mapped in this exercise<br />
although a number of species are recorded for the region (see McNiven 2008). The native<br />
Neololeba atra (listed as Rare under the Nature Conservation Act), occurs in the Wet Tropcs,<br />
Iron Range-McIlwraith <strong>and</strong> Lockerbie areas of north-eastern Queensl<strong>and</strong> <strong>and</strong> also in Papua New<br />
Guinea <strong>and</strong> New Britain (Hyl<strong>and</strong> et al. 2003). It is known from the Torres Strait from Mer,<br />
Naghir, Ugar <strong>and</strong> Iama (EPA 2007), <strong>and</strong> from Badu <strong>and</strong> Moa Isl<strong>and</strong>s (Fell pers. obs.) however is<br />
generally restricted to the understorey <strong>and</strong> rainforest margins <strong>and</strong> does not form mappable<br />
communities.<br />
EX: <strong>Communities</strong> Dominated by Exotic Species (other than bamboo): <strong>Communities</strong><br />
dominated by exotic species other than bamboo, are represented with an appended (e). This<br />
classification extends to a range of communities <strong>and</strong> species including extensive areas of tall<br />
closed forest of *Mangifera indica (Mango) or *Delonix regia (Poinciana) on a number of<br />
isl<strong>and</strong>s, most prominently Mer <strong>and</strong> Erub, where such communities have been designated as nonremnant<br />
vegetation. Former grassl<strong>and</strong> areas on Mer <strong>and</strong> Erub Isl<strong>and</strong>s dominated by *Lantana<br />
camara are similarly designated with an appended (e) although in such cases, remnant status has<br />
been designated given that natural condition of these areas can be restored relatively easily<br />
through appropriate fire regime.<br />
Photograph 183. Bamboo groves<br />
on a basalt headl<strong>and</strong> within broader<br />
vine forest communities. Erub<br />
Isl<strong>and</strong>.<br />
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RE: Native Regrowth <strong>Communities</strong>: Native regrowth communities are recognised on the<br />
majority of isl<strong>and</strong> groups that have been subject to human occupation where they have been noted<br />
with an appended (R). These communities result from the clearing, or partial clearing of natural<br />
vegetation that is in varying stages of recovery to a natural condition. On Erub, such<br />
communities are often represented by groves of Barringtonia calyptrata on the margins of<br />
remnant vine forest vegetation, <strong>and</strong> on Boigu or Iama as mangrove shrubl<strong>and</strong>.<br />
Non-Remnant <strong>Communities</strong> of Local Cultural Significance: Anthropogenically altered<br />
forests with development influenced by intensive cultural l<strong>and</strong> use covered extensive areas of<br />
Mer, Erub <strong>and</strong> Masig. The broad structural characteristics of the communities, being VC22a <strong>and</strong><br />
VC22b are described below, followed by brief discussion on their likely derivation.<br />
<strong>Vegetation</strong> Community 22a: <strong>Vegetation</strong> community 22a, found on Murray <strong>and</strong> Erub Isl<strong>and</strong>s,<br />
are typically represented by tall groves of Cocos nucifera below which a closed forest has<br />
formed. This closed forest component has a general canopy height range of 15 to 23m,<br />
comprising predominantly native species (Mango being an exception), although the species<br />
assemblage is heavily skewed in favour of traditional food trees such as Syzygium br<strong>and</strong>erhorstii<br />
<strong>and</strong> Syzygium bungadinnia (on Mer Isl<strong>and</strong>). A typical canopy assemblage (or sub canopy below<br />
the dominant stratum of Cocos nucifera) on Erub (Site ER30) comprised Syzygium<br />
br<strong>and</strong>erhorstii, Myristica insipida, Cocos nucifera, Alectryon rep<strong>and</strong>odentatus (E), Diospyros<br />
hebecarpa, Cupaniopsis anacardioides, Mangifera indica, Bombax ceiba var. leiocarpum,<br />
P<strong>and</strong>anus sp., Canarium vitiense <strong>and</strong> Mimusops elengi. Other prominent species may include<br />
Alstonia spectabilis, Cerbera manghas, <strong>and</strong> Semecarpus australiensis. An unusual feature noted<br />
in this community on both Mer <strong>and</strong> Erub is the prominence of Lepidopetalum fructoglabrum in<br />
the sub-canopy <strong>and</strong> shrub layers of a large number of these forest types. This species is not<br />
recorded in any other vine forest community examined. Where mapped, the majority of these<br />
areas are on level topography with a sparse understorey <strong>and</strong> free of the surface rock that is<br />
otherwise abundant on hillslope situations.<br />
Photograph 184. A tall specimen of<br />
Syzygium bungadinnia mixing with Cocos<br />
nucifera in the canopy of VC22a (Site<br />
MU028, Mer Isl<strong>and</strong>).<br />
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Field evidence suggests that areas mapped as VC22a on Murray <strong>and</strong> Erub Isl<strong>and</strong>s, were once<br />
utilised as traditional garden sites where cultivation of food trees such as Syzygium br<strong>and</strong>erhorstii<br />
<strong>and</strong> Mangifera indica occurred under coconut groves. In some instances old rotting Coconut<br />
stumps were observed in the understorey. Detailed knowledge of l<strong>and</strong> use histories throughout<br />
Mer is undoubtedly held within the traditional owner clan groups <strong>and</strong> this is an essential<br />
foundation toward further ecological underst<strong>and</strong>ing of these systems. The role Torres Strait<br />
isl<strong>and</strong>er people have had in shaping the vegetation communities of the Torres Strait (see Parr <strong>and</strong><br />
Carter 2003, Carter 2004, McNiven 2007, Rowe 2007, Barham 1999) is evident through the<br />
length of continuous occupation +2,500 years BP which relied on l<strong>and</strong> <strong>and</strong> marine resource<br />
exploitation inclusive of extensive garden cultivations.<br />
In respect to Mer Isl<strong>and</strong>, Haddon (1935) states ‘ the great lava stream extends with an undulating<br />
surface from the central cone to the north-western end of the isl<strong>and</strong>, <strong>and</strong> forms a fertile tablel<strong>and</strong><br />
which is bounded by a steep slope. The disintegrated lava forms a reddish brown soil in which<br />
coconut palms grow in profusion, <strong>and</strong> the natives have their gardens of bananas, yams <strong>and</strong> sweet<br />
potatoes. There are also wild mangoes <strong>and</strong> other wild fruit <strong>and</strong> other trees’. Carter (2004)<br />
makes reference to the observations of Yonge (1930) where large areas of the more fertile parts of<br />
the isl<strong>and</strong> supported extensive tropical horticulture, <strong>and</strong> further comments that “the eastern<br />
interior tablel<strong>and</strong> currently supports dense vine thicket, groves of bamboo, wild mango trees <strong>and</strong><br />
secondary woodl<strong>and</strong> regrowth interspersed with garden plots” (Carter 2004, pp 165). It is<br />
apparent that a period of stability (or change in l<strong>and</strong> usage) has allowed for the development of<br />
VC22a on both Mer <strong>and</strong> Erub.<br />
<strong>Vegetation</strong> Community 22b: <strong>Vegetation</strong> Community 22b on Masig is represented as a low<br />
notophyll/microphyll vine thicket dominated by species which include Buchanania arborescens,<br />
Drypetes deplanchei, <strong>and</strong> Terminalia subacroptera. This community is reported by local people<br />
to represent former traditional garden areas that have long since regenerated to a relatively stable<br />
vine thicket dominated by native species. Whilst a number of similar communities, controlled<br />
<strong>and</strong> maintained by natural process, are present in other isl<strong>and</strong> locations, the communities on<br />
Masig lack sufficent cover of the original canopy for classification as remnant vegetation.<br />
In summary, the modification of the natural environment by the indigenous cultures of the Torres<br />
Strait over centuries is recognised in both VC22a <strong>and</strong> VC22b <strong>and</strong> although classified as nonremnant<br />
vegetation, such areas retain significant cultural values with l<strong>and</strong> ownership boundaries<br />
well defined within the local community.<br />
Photograph 185. Anthropogenically<br />
altered vine thicket<br />
VC22b on Masig (Site YOS7).<br />
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5.5 Other Classifications<br />
Areas Represented as R: Areas labelled R represent bare rock pavement formed on volcanic,<br />
granitoid or basaltic lithologies. Such areas lack soil development in any form <strong>and</strong> are generally<br />
found in exposed <strong>and</strong> precipitous locations, often at the base of coastal escarpments immediately<br />
above the intertidal zone. These areas are typically devoid of vegetation due to extreme exposure<br />
to both wind <strong>and</strong> salt spray, although stunted shrubs, herbs <strong>and</strong> grasses may occupy rock fractures<br />
where some shelter is provided. Due to extremely steep terrain, these communities are likely to<br />
be under-represented in the mapping with many areas obscured by steep slopes.<br />
6.0 Spatial Extent of <strong>Regional</strong> <strong>Ecosystems</strong><br />
The spatial analysis of regional ecosystems presented in Table 11 below, which compares preclearing<br />
extent with contemporary representation, enables the area of current vegetation cover to<br />
be compared to the pre-clearing extent. Results indicate that 98.9% of remnant vegetation cover<br />
remains. The most extensive loss of remnant vegetation cover is attributable to the following<br />
RE’s.<br />
• RE 3.7.1x1, a vine thicket type which is now restricted to narrow fragments adjacent to<br />
roadsides on ironstone exposures on the northern shores of Saibai Isl<strong>and</strong> (0.4% remains<br />
in remnant condition;<br />
• RE 3.2.28, Evergreen notophyll vine forest on beach ridges on coral atolls, shingle cays<br />
<strong>and</strong> s<strong>and</strong> cays (45.4% remaining). Heavily impacted on Aureed, Warraber, <strong>and</strong> Masig;<br />
• RE 3.3.69, Melaleuca dealbata <strong>and</strong> Corymbia clarksoniana open forest on alluvial plains<br />
restricted to Moa (47% remaining);<br />
• RE 3.8.5, Semi deciduous <strong>and</strong> deciduous vine thicket restricted to Erub <strong>and</strong> Mer (58.8%<br />
remaining). Heavily fragmented through past native gardening with significant areas<br />
have been replaced by bamboo;<br />
• RE 3.12.13, Corymbia nesophila ± C. hyl<strong>and</strong>ii subsp. peninsularis woodl<strong>and</strong> on acid<br />
volcanic hills, restricted to Thursday, Zuna <strong>and</strong> Muralug (66.7% remaining);<br />
• RE 3.2.6, Casuarina equisetifolia woodl<strong>and</strong> of coastal foredunes (67.5% remaining).<br />
Heavily impacted community on foreshores in a number of isl<strong>and</strong> groups;<br />
• RE 3.2.15, Melaleuca viridiflora, Neofabricia myrtifolia woodl<strong>and</strong> on beach ridges<br />
occurring on Badu, Horn <strong>and</strong> Muralug (77.1% remaining). Nearly all of the clearing of<br />
this RE is associated with increased urbanization on Badu including clearing for airstrips<br />
(old <strong>and</strong> new); <strong>and</strong><br />
• RE 3.3.57, Tussock grassl<strong>and</strong> on coastal plains of Moa, Gebar <strong>and</strong> Muralug (77.5%<br />
remaining). A fire disclimaz community that has been impacted by clearing on Moa<br />
Isl<strong>and</strong> (St Pauls).<br />
Table 11. Analysis of pre-clearing regional ecosystems in the Torres Strait Isl<strong>and</strong> region.<br />
<strong>Regional</strong><br />
Ecosystem<br />
Pre-clearing Area<br />
(ha)<br />
Area (2007 Coverage-ha) % Remaining<br />
L<strong>and</strong> Zone 1- Estuarine muds <strong>and</strong> alluvium subject to saltwater incursion<br />
3.1.1 17908.8 17886.3 99.8<br />
3.1.2 4327.01 4326.62 99.8<br />
3.1.4 20.02 20.02 100<br />
3.1.5 346.11 341.74 98.7<br />
3.1.6 3325.38 3319.27 99.8<br />
3.1.7 954.12 953.13 99.9<br />
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<strong>Regional</strong><br />
Ecosystem<br />
Pre-clearing Area<br />
(ha)<br />
Area (2007 Coverage-ha) % Remaining<br />
L<strong>and</strong> Zone 2 - Coastal Dunes, Cheniers <strong>and</strong> S<strong>and</strong> Sheets <strong>and</strong> associated Dune Swales.<br />
3.2.2 368.12 264.4 71.8<br />
3.2.3 111.962 109.18 97.5<br />
3.2.4 320.32 313.43 97.8<br />
3.2.5 646.21 561.16 86.8<br />
3.2.6 285.81 193.148 67.5<br />
3.2.7 605.45 599.41 99.0<br />
3.2.8 60.44 60.44 100.0<br />
3.2.10 128.89 128.99 100.0<br />
3.2.14 0.46 0.46 100.0<br />
3.2.15 967.02 745.1 77.1<br />
3.2.19 167.83 160.08 95.4<br />
3.2.24 359.16 296.23 82.5<br />
3.2.25 39.84 35.76 89.8<br />
3.2.26 80.1 80.1 100.0<br />
3.2.27 4.27 4.27 100.0<br />
3.2.28 188.80 85.72 45.4<br />
3.2.30 3.14 3.14 100.0<br />
L<strong>and</strong> Zone 3 - Alluvial plains, alluvial fans, terraces <strong>and</strong> fluvial sediments<br />
3.3.1c 8.03 0 0.0<br />
3.3.5c 103.83 103.83 100.0<br />
3.3.6 46.97 46.97 100.0<br />
3.3.7 18.09 10.95 100.0<br />
3.3.9 179.77 179.77 100.0<br />
3.3.10 476.21 467.00 98.0<br />
3.3.12 33.75 33.75 100.0<br />
3.3.13 55.47 55.47 100.0<br />
3.3.14 208.75 204.32 97.8<br />
3.3.17b 185.33 182.05 98.23<br />
3.3.20c 1143..37 1120.68 98.0<br />
3.3.22 553.72 537.6 97.08<br />
3.3.27 2277.73 2201.02 96.6<br />
3.3.28 253.21 227.39 89.8<br />
3.3.42 2999.52 2931.18 97.7<br />
3.3.48 1124.00 1112.13 98.9<br />
3.3.51 111.72 111.72 100.0<br />
3.3.57 273.07 211.61 77.5<br />
3.3.62 1331.87 1290.36 96.9<br />
3.3.63 105.7 105.7 100.0<br />
3.3.68 90.02 90.02 100.0<br />
3.3.69 139.82 65.60 46.9<br />
3.3.70 148.41 144.254 97.1<br />
L<strong>and</strong> Zone 5 – S<strong>and</strong>y plains <strong>and</strong> rises/ Lateritic profiles <strong>and</strong> remnant alluvial/colluvial surfaces.<br />
3.5.5 2110.88 2110.88 100.0<br />
3.5.8 73.37 73.37 100.0<br />
3.5.15 3273.32 3273.32 100.0<br />
3.5.17a 10.44 10.44 100.0<br />
3.5.19 229.93 229.93 100.0<br />
3.5.23x1 115.54 115.54 100.0<br />
3.5.29 59.26 59.26 100.0<br />
3.5.32 228.21 228.21 100.0<br />
L<strong>and</strong> Zone 7 – Exposed or shallowly covered duricrust<br />
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<strong>Regional</strong><br />
Ecosystem<br />
Pre-clearing Area<br />
(ha)<br />
Area (2007 Coverage-ha) % Remaining<br />
3.7.1x1b 19.19 0.77 0.4<br />
L<strong>and</strong> Zone 8 - Basalt escarpments <strong>and</strong> terraces/Volcanic cones formed on ash <strong>and</strong> scoria<br />
3.8.4 530.45 519.3 97.9<br />
3.8.5 484.00 284.67 58.8<br />
L<strong>and</strong> Zone 12 – Acid volcanic <strong>and</strong> plutonic rocks including hornfelsed granite parent rocks<br />
3.12.4 6049.01 5896.87 97.5<br />
3.12.8 1664.26 1628.43 97.8<br />
3.12.9 785.84 779.46 99.2<br />
3.12.11 7998.49 7798.93 97.5<br />
3.12.13 360.49 240.37 66.7<br />
3.12.16 1795.76 1786.14 99.46<br />
3.12.18 96.83 96.83 100.0<br />
3.12.20 5660.53 5660.53 100.0<br />
3.12.21a 365.18 328.58 89.9<br />
3.12.23 2252.69 2252.69 100.0<br />
3.12.29 927.73 909.03 97.9<br />
3.12.30 489.68 488.15 99.7<br />
13.12.31x1a 1408.50 1408.39 100.0<br />
3.12.33 29.36 29.36 100.0<br />
3.12.34 1833.99 1833.99 100.0<br />
3.12.35 1156.18 1092.06 94.45<br />
3.12.36 494.78 491.68 99.9<br />
3.12.37 503.42 474.70 94.3<br />
3.12.38 1661.64 1661.5 100.0<br />
Total 84613.2 83684.85 98.9<br />
7.0 Significant <strong>Vegetation</strong> <strong>and</strong> Flora<br />
7.1 Summary of Significant <strong>Vegetation</strong><br />
The following section identifies vegetation types which have a restricted occurrence in the study<br />
area, recognising a number of vegetation communities potentially unique to the Torres Strait<br />
Isl<strong>and</strong>s. <strong>Vegetation</strong> which provides habitat to significant flora species including EVR’s, disjunct<br />
populations <strong>and</strong> species at the limits of geographical range are also recognized.<br />
1. <strong>Regional</strong> Ecosystem 3.1.1 (Closed forest of Rhizophora stylosa ± Bruguiera gymnorhiza)<br />
is described as a highly complex <strong>and</strong> variable RE occupying intertidal areas, generally on<br />
the seaward fringe of mangroves where tidal exchange is greatest. This RE includes<br />
small areas of Nypa forest on North-West Creek (Muralug) mapped as VC12a. The<br />
occurrence of Nypa forest on Muralag represents an extension of geographical range of<br />
the species north from the Jardine River mouth, being the only known occurrence<br />
between Cape York <strong>and</strong> PNG.<br />
2. <strong>Regional</strong> Ecosystem 3.1.7 is a previously unrecognised unit describing Schoenoplectus<br />
spp. sedgel<strong>and</strong>s in brackish estuarine environments. This ecosystem unit incorporates<br />
low open sedgel<strong>and</strong> (VC 27a) <strong>and</strong> tall sedgel<strong>and</strong>/estuarine wetl<strong>and</strong> mosaics (VC 27b), the<br />
latter forming where freshwater drainage mixes with estuarine waters, generally on the<br />
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l<strong>and</strong>ward margins of mangrove forest complexes. The RE is confined to Saibai <strong>and</strong><br />
Boigu Isl<strong>and</strong>s <strong>and</strong> is not currently recognised on mainl<strong>and</strong> areas of Cape York.<br />
3. The complexity of vine forest types on s<strong>and</strong> dunes within the isl<strong>and</strong> group is remarkable,<br />
warranting recognition as a single broad RE unit distinct from those identified in the<br />
existing RE schema. The new RE is formed by the VC’s 2a, 2l, 2u, <strong>and</strong> 9b, occurring on<br />
nearly all isl<strong>and</strong> groups with best developed type examples represented on Saibai, Boigu,<br />
Erub, Muralug, Moa, Warral <strong>and</strong> Sassie Isl<strong>and</strong>s. These communities are semi-deciduous<br />
in nature with structural variation between vine thicket <strong>and</strong> vine forest, <strong>and</strong> occupy<br />
calcareous beach ridges, as distinct from the coralline s<strong>and</strong> deposits of the atolls which<br />
provide habitat for RE3.2.28. A unique expression (VC23c) occurs on inacessible parts<br />
of Sassie Isl<strong>and</strong> where coral rubble ridges provides habitat for tall transitional vine forest<br />
types. On Saibai Isl<strong>and</strong>, parts of the coast supporting this habitat continue to provide<br />
seasonal living <strong>and</strong> camping sites for traditional owners <strong>and</strong> are likely to also provide<br />
important ethnobotanical resources. The occurrence of *Cocus nucifera <strong>and</strong> *Bambusa<br />
spp. may be associated with settlement areas. The Erub occurrence of the RE provides<br />
habitat for the listed Alectryon rep<strong>and</strong>odentatus (Endangered, NCA 1992) <strong>and</strong> Neololeba<br />
atra (Rare, NCA 1992). On Muralug Isl<strong>and</strong>, VC2u provides habitat for the vulnerable<br />
Cooktown Orchid (Dendrobium biggibum) <strong>and</strong> the Vulnerable listed (yet widespread)<br />
Psydrax reticulata. Populations of the Endangered vine Muelleragia timorensis are<br />
likely.<br />
4. The occurrence of RE 3.2.2b (Semi-deciduous vine thicket on coastal dunes <strong>and</strong> beach<br />
ridges) on Moa Isl<strong>and</strong>, mapped as VC2p, provides the only known s<strong>and</strong> dune habitat for<br />
the Vulnerble palm Arenga australasica in the Torres Strait. This is also known habitat<br />
for the Endangered vine Muelleragia timorensis, <strong>and</strong> disjunct populations of Aristolochia<br />
chalmersii.<br />
5. <strong>Regional</strong> Ecosystem 3.2.10c (Eucalyptus tetrodonta, Corymbia clarksoniana ± E.<br />
brassiana or Erythrophleum chlorostachys woodl<strong>and</strong> on stabilised dunes - VC5j) is<br />
resticted to the western coast of Muralug Isl<strong>and</strong> where older dune systems are wellpreserved<br />
<strong>and</strong> relatively extensive. This Eucalyptus tetrodonta dominant habitat<br />
represents the most northerly geographical limit of E. tetrodonta in Queensl<strong>and</strong>.<br />
Additionally the ecosystem provides habitat for highly disjunct occurrences of Corymbia<br />
latifolia.<br />
6. The newly described RE3.3.2x1 accommodates a unique variety of Semi-deciduous<br />
mesophyll/notophyll vine forest on alluvium, restricted to flood prone alluvial plains of<br />
the Northern Isl<strong>and</strong> Group. It incorporates VC2c on Saibai Isl<strong>and</strong> <strong>and</strong> closed<br />
shrubl<strong>and</strong>/vine thicket type 14b an Boigu Isl<strong>and</strong>. These communities occupy a unique<br />
l<strong>and</strong>form situation with no similar representation in either the broader isl<strong>and</strong> group or the<br />
Cape York Peninsula Bioregion. The representative communities are under imminent<br />
threat of extinction through sea level rise.<br />
7. The tall evergreen notophyll vine forest type VC1j is represented only on the s<strong>and</strong>y<br />
alluvial soils of Tutalia Creek on Moa Isl<strong>and</strong>. The unique floristic assemblage which is<br />
dominated by Acmena hemilampa subsp. hemilampra, Syzygium angophoroides <strong>and</strong><br />
associated Acacia auriculiformis, Syzygium forte subsp. forte, Calophyllum sil <strong>and</strong><br />
Buchanania arborescens has no known comparable communities on Cape York<br />
Peninsula. The adjoining evergreen mesophyll vine forest (VC1i) on stream alluvia is<br />
similarly unique in the Torres Strait region. The community has floristic affinities (on<br />
account of abundant Horsfieldia in the canopy) to riparian vine forests on swampy<br />
alluvium associated with the lower catchment of the Lockhart River <strong>and</strong> tributaries.<br />
Provision of habitiat for P<strong>and</strong>anus zea, listed as ‘Rare’ under provisions of the NCA is an<br />
additional significant habitat feature.<br />
8. The mixed riparian forest type mapped as VC5h is restricted to Horn Isl<strong>and</strong> where it<br />
occupies swampy flood overflow plains carved into relict dune systems. The dominant<br />
canopy, always in open forest formation, ranges in height from 15 to 23m <strong>and</strong> is<br />
composed of Melaleuca saligna, Corymbia stockeri subsp. peninsularis, Corymbia<br />
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clarksoniana, Eucalyptus brassiana <strong>and</strong> Eucalptus platyphylla. This presents an unusual<br />
floristic assemblage <strong>and</strong> the record of Eucalyptus brassiana provides an extension of<br />
geographic limit of the species north from Cape York. The community provides for the<br />
only record of the species within the study area.<br />
9. The Melaleuca quinquinervia dominant RE 3.3.12 (VC7d) is restricted in the Torres<br />
Strait to Moa <strong>and</strong> Badu Isl<strong>and</strong>s forming the most northerly known occurrence of the<br />
species on Badu. On Moa it occurs on the broad erosional plain of the north-west, <strong>and</strong> on<br />
Badu in deflation hollows <strong>and</strong> broad swales of old dune surfaces. On both isl<strong>and</strong>s, M.<br />
quinquinervia occurs in sparsely scattered swampl<strong>and</strong>s.<br />
10. <strong>Regional</strong> Ecosystem 3.2.14 (VC13h) is restricted to a single occurrence on Horn Isl<strong>and</strong>,<br />
where it is expressed as a low closed shrubl<strong>and</strong> dominated by Melaleuca arcana. The<br />
community forms a semi-circular swamp within a broader relict dune system <strong>and</strong><br />
represents an extension of geographical range of the species north from the Jardine River.<br />
The community is therefore unique in the Torres Strait regional context.<br />
11. <strong>Regional</strong> ecosystem 3.3.18x1, incorporating VC7c <strong>and</strong> VC4d is restricted to coastal areas<br />
north of St. Pauls, Moa Isl<strong>and</strong> where it is represented as a tall open forest of Melaleuca<br />
dealbata <strong>and</strong> Corymbia clarksoniana in relatively equal proportions. The floristic<br />
composition of this community appears unique in a bio-regional context, <strong>and</strong> its spatial<br />
extent is extremely limited. This community has been heavily fragmented by past<br />
l<strong>and</strong>use practice <strong>and</strong> a dominant proportion of the l<strong>and</strong>form that it once occupied has<br />
been cleared, highlighting the urgency to recognise the unique nature of this community.<br />
12. <strong>Regional</strong> ecosystem 3.3.62a* (VC11a) comprises a mosaic of grassl<strong>and</strong>, shrubl<strong>and</strong> <strong>and</strong><br />
low woodl<strong>and</strong> types, confined mostly to Northern Isl<strong>and</strong>s group. The most extensive<br />
representation is provided on Saibai Isl<strong>and</strong>, although scattered areas also occur on Boigu,<br />
<strong>and</strong> southern representation is provided on Hammond <strong>and</strong> Moa Isl<strong>and</strong>s (Inner <strong>and</strong> Near<br />
Western Isl<strong>and</strong> Groups respectively). The community is confined to Torres Strait Region<br />
although extensive areas occur on the coastal plains of neighbouring PNG. Large areas<br />
of the unit are former prehistoric tropical field systems with characteristic physical traces<br />
of relict agricultural mounds <strong>and</strong> ditches indicating high cultural values (see Barham<br />
1999).<br />
13. The proposed creation of a new RE3.5.32 (VC9a) recognises the unique combination of<br />
Asteromyrtus brassii, Syzygium angophoroides <strong>and</strong> Acmena hemilampra subsp.<br />
hemilampra open forest on residual s<strong>and</strong> rises <strong>and</strong> sheets. The unusual l<strong>and</strong>form<br />
association of these more typically swamp dwelling species is unique to Moa Isl<strong>and</strong>, <strong>and</strong><br />
provides an unusual floristic variation of vegetation on a L<strong>and</strong> Zone 5 feature.<br />
14. Native gassl<strong>and</strong>s classified within RE3.8.4 (VC17b) on basalt vents & cones are<br />
restricted to the major basaltic isl<strong>and</strong>s of Erub <strong>and</strong> Mer, forming a considerable portion of<br />
the isl<strong>and</strong>s terrestrial habitat. Special significance is assigned to these communities,<br />
considering both the uniqueness of the volcanic l<strong>and</strong>scape, <strong>and</strong> the rarity of basaltic<br />
grassl<strong>and</strong> types in the broader bioregional area. Similar communities are represented<br />
near Hopevale in the south of the CYP bioregion. These ecosytems have long histories<br />
of anthropogenic management, although edaphic condition provides a fundamental<br />
control on their development. Underst<strong>and</strong>ing the impact of incremental l<strong>and</strong> use change,<br />
evidenced today by shrub <strong>and</strong> lantana invasion <strong>and</strong> erosion, is vital for determining<br />
appropriate management strategies.<br />
15. The proposed new <strong>Regional</strong> Ecosystem 3.12.1x1 (Semi-deciduous mesophyll/notophyll<br />
vine forest on granite slopes of the Torres Strait Sub-region) comprises a floristically<br />
diverse group of vegetation mapping units (2d, 2h, 2o, 2q, 2r, 6e) occurring on steep<br />
granitic <strong>and</strong> acid volcanic slopes of the larger continental isl<strong>and</strong>s. The most extensive<br />
occurrences are are recognised on Dauan, Iama <strong>and</strong> Gebar Isl<strong>and</strong>s, <strong>and</strong> on the Near<br />
Western <strong>and</strong> Inner Isl<strong>and</strong> Group. <strong>Vegetation</strong> community 2d, which is found on the steep<br />
boulder strewn mid to upper slopes of Dauan Isl<strong>and</strong>, supports disjunct populations of<br />
Tetrameles nudiflora <strong>and</strong> Nothocnide rep<strong>and</strong>a, <strong>and</strong> is notable for its diversity of<br />
epiphytic plants including the ‘Vulnerable’ Dischidia littoralis. <strong>Vegetation</strong> community<br />
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177
2o on the sheltered slopes of Moa provides habitat for Archidendron hirsutum (Rare) <strong>and</strong><br />
disjunct populations of Polyalthia australis. The best development of the ecosystem is<br />
provided on Muralug Isl<strong>and</strong> as VC2q where it occupies a series of rocky diorite knolls<br />
protruding above a broad alluvial plain. The type supports restricted occurrences of<br />
Terminalia complanata, Albizia lebbeck, Cordia myxa, Lagerstroemia archeriana <strong>and</strong><br />
Indigator fordii. The latter represents the highly disjunct occurrence of an extremely rare<br />
species, previously known from only four to six trees on the southern slopes of the<br />
McIlwraith Range.<br />
16. <strong>Regional</strong> Ecosystem 3.12.3x1 (VC6a) is a proposed new RE, accounting for Acacia<br />
auriculiformis open forest with vine forest understorey. This unique community is<br />
restricted to Iama Isl<strong>and</strong> (VC6a) with a minor occurrence also mapped on Gebar. High<br />
biodiversity values are given to this community given its uniqueness in the national,<br />
regional <strong>and</strong> local contexts, <strong>and</strong> through provision of habitat for a highly disjunct<br />
population of Luvunga monophylla (Rutaceae), being a new record for Queensl<strong>and</strong>.<br />
17. <strong>Regional</strong> Ecosystem 3.12.5x1 is proposed as a new RE recognising a unique expression<br />
of evergreen to complex evergreen mesophyll to notophyll vine forest <strong>and</strong> thicket on<br />
mountain ranges of Torres Strait Isl<strong>and</strong>s. The proposed new ecosystem represents a<br />
diverse range of floristic <strong>and</strong> structural variations that have been previously<br />
unrecognised. This ecosystem is extremely undersampled in regard to its botanical <strong>and</strong><br />
faunal diversity <strong>and</strong> warrants more detailed investigation of these components in future<br />
studies. The likelihood of finding significant new botanical <strong>and</strong> faunal records within<br />
this community can be regarded as extremely high.<br />
18. <strong>Vegetation</strong> Community 5f (proposed as a component of RE3.12.18) is restricted to<br />
Naghir Isl<strong>and</strong>, occupying the well-drained granitic soils of the footslope <strong>and</strong> colluvial<br />
apron on the isl<strong>and</strong>s western side. This community provides Australia’s most northerly<br />
occurrence of Eucalyptus leptophleba, <strong>and</strong> is highly significant for this reason. The<br />
occurrence of this community is well-removed from examples on northern Cape York<br />
Peninsula, with the only other recognised occurrence of the species in the Torres Strait<br />
Group confined to scattered trees on Thursday Isl<strong>and</strong>. The taxon also occurs on the<br />
windswept coastal dunes of Naghir (RE3.2.25) as a component of VC14t.<br />
Whilst the signifigance of regional ecosystems can be assessed on an individual basis, the values<br />
of the broader mosaic of vegetation across the Torres Strait Sub-region, including its complexity,<br />
diversity <strong>and</strong> connectivity should also be considered highly significant. The study revealed 77<br />
regional regional ecosystems in the Torres Strait study area, accounting for approximately one<br />
third of the currently documented ecosystem diversity in the broader bioregion within a<br />
recognised sub-region contributing less than 0.01% to the bioregions total l<strong>and</strong> area<br />
(12,050,307.0576 ha – IBRA Version 5). Of the isl<strong>and</strong>s represented, the diversity of the<br />
vegetation on Moa Isl<strong>and</strong> which ranges from upl<strong>and</strong> complex rainforests, well-developed gallery<br />
rain forests, expansive plains with a variety of woodl<strong>and</strong>, heathl<strong>and</strong>, shrubl<strong>and</strong> <strong>and</strong> swampl<strong>and</strong><br />
forms, provides biodiversity values that are unlikely to be matched on any mainl<strong>and</strong> conservation<br />
area. At present, much of this l<strong>and</strong>scape is free from degradation associated with invasive species<br />
<strong>and</strong> other impacts such as development.<br />
7.2 Summary of Flora<br />
7.2.1 <strong>Regional</strong> Flora<br />
An analysis of the field survey data in combination with EPA Corveg <strong>and</strong> Herbrecs data <strong>and</strong><br />
previous studies for the study area identifies a vascular flora of 1,330 species (<strong>Appendix</strong> B) 6 .<br />
6<br />
Analysis includes Herbrecs data from Albany Isl<strong>and</strong> which was not part of mapping area. Includes subspecies <strong>and</strong><br />
varieties.<br />
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This includes 196 (15%) naturalised species. A breakdown of the flora into major groups<br />
together with a broad comparison to regional floras is provided in Table 12 below.<br />
Table 12. Summary of the native vascular flora of the Torres Strait Isl<strong>and</strong>s in comparison Cape York<br />
Peninsula (from Neldner <strong>and</strong> Clarkson 1995 in Neldner 1998) <strong>and</strong> Great Barrier Reef Continental Isl<strong>and</strong>s<br />
(from Batianoff <strong>and</strong> Dilleward 1997) <strong>and</strong> Queensl<strong>and</strong> Flora (Bostock <strong>and</strong> Holl<strong>and</strong> 2007).<br />
Families<br />
Taxa<br />
Cape York<br />
Peninsula<br />
Families 7<br />
Taxa<br />
Great Barrier<br />
Reef Continental<br />
Isl<strong>and</strong>s 8<br />
15<br />
39<br />
30<br />
157<br />
Pteridophytes Gymnosperms Angiosperms Total<br />
1<br />
1<br />
158<br />
1,289<br />
174<br />
1,329<br />
Pteridophytes Gymnosperms Angiosperms Total<br />
5<br />
6<br />
183<br />
3,173<br />
218<br />
3,338<br />
Pteridophytes Gymnosperms Angiosperms Total<br />
Families<br />
25<br />
5<br />
165<br />
195<br />
Taxa<br />
97<br />
7<br />
2,091<br />
2,195<br />
Qld Flora 9 Pteridophytes Gymnosperms Angiosperms Total<br />
Taxa 396 70 9,424 9,890<br />
In comparison to the Cape York Peninsula bioregion, the Torres Strait Isl<strong>and</strong>s support a high<br />
floristic diversity as evidenced by the presence of approximately 40% of the diversity of the vascular<br />
flora in 0.01% of the l<strong>and</strong> area. On a statewide basis, the Torres Strait supports some 13% of the<br />
Queensl<strong>and</strong> vascular flora. Taxa such as Cycas scratchelyana, Dendrobium litorale, Dischidia<br />
littoralis, Globba marantina, Grastidium insigne, Ischaemum polystachyum, <strong>and</strong> Vrydagzynea<br />
elongata reach their southern limit of distribution in the study area whilst Croton waterhousea,<br />
Cycas badensis, <strong>and</strong> Secamone auriculata are Torres Strait endemics. Floristic diversity reflects on<br />
the remarkable ecosystem diversity within the study area. Further analysis of the survey data in<br />
combination with available datasets is outside the scope of the current project however is<br />
necessary to allow comparisons of individual isl<strong>and</strong>s, <strong>and</strong> to assess the spatial distribution of<br />
taxonomic groups across the Straits.<br />
7.2.2 Introduced <strong>and</strong> Naturalised Flora<br />
The account of the introduced flora remains an underestimation despite the significant<br />
contributions by Waterhouse as part of ongoing AQIS work throughout the region <strong>and</strong> other<br />
collectors. The figure of 15%, which consitutes the proportion of the naturalised flora within the<br />
total flora, contrasts with; the National flora (13-15%) (Bean 1996); the Queensl<strong>and</strong> Flora<br />
(15.6%) (Bostock <strong>and</strong> Holl<strong>and</strong> 2007); the Northern Territory flora (5.2%) (Bowman et al. 1988);<br />
Cape York Peninsula flora (7.4%) (Neldner 1998); <strong>and</strong> the Great Barrier Reef Contiental Isl<strong>and</strong>s<br />
flora (9.8%) (Batianoff <strong>and</strong> Dillewaard 1997). Eight species are listed as Declared on the L<strong>and</strong><br />
Protection (Pest <strong>and</strong> Stock Route Management) Act 2002 (see Table 13). A summary of invasive<br />
species with the potential to invade native ecosystems provided in Table 14 below is informed by<br />
personal communication with Barbara Waterhouse.<br />
7 Cape York flora utilises Henderson (2002).<br />
8 Batianoff <strong>and</strong> Dilleward (1997) identify 552 continental isl<strong>and</strong>s along the east coast of Queensl<strong>and</strong> within the Great<br />
Barrier Reef Marine Park (GBRMP), a total l<strong>and</strong> area of about 1,627 km2.<br />
9 Bostock <strong>and</strong> Holl<strong>and</strong> (2007).<br />
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Table 13. Summary of declared species listed on the L<strong>and</strong> Protection Act 2002.<br />
Class Declared Species Comments<br />
2 Bellyache Bush (Jatropha gosypifolia) Badu Isl<strong>and</strong>. Notes in Herbrecs (2007) from<br />
Waterhouse collections indicate that it occurs as an<br />
ornamental in gardens <strong>and</strong> as wild plants in small<br />
populations of 5-10 plants that have grown from<br />
discarded garden water adjacent to beach <strong>and</strong> mangrove<br />
at northeast end of settlement <strong>and</strong> around council dump.<br />
2 Pond Apple (Annona glabra)<br />
Weed of National Significance.<br />
Boigu Isl<strong>and</strong>. Small populations in township.<br />
Horn Isl<strong>and</strong>. Two collections from from s<strong>and</strong> <strong>and</strong><br />
gravel storage area adjacent to Eilkam Holiday Park in<br />
disturbed site adjacent to Melaleuca woodl<strong>and</strong> <strong>and</strong><br />
mangroves.<br />
Thursday Is. Record from approx. 100m north of<br />
Torres Shire Water Supply sign on track between Sadie's<br />
Beach <strong>and</strong> Waiben.<br />
Muralug. Isolated occurrences reported.<br />
2 Prickly Pear (Opuntia stricta) Horn Is. Isolated occurrences<br />
Hammond Is. Isolated occurrences<br />
Moa Is (St Pauls). Isolated occurrences<br />
2 Americans Rats Tail Grass (Sporobolus<br />
jacquemontia)<br />
Lantana (Lantana camara)<br />
Weed of National Significance.<br />
3<br />
3<br />
2<br />
Singapore Daisy (Sphagneticola<br />
trilobata)<br />
Thursday Is. Single record from town area.<br />
Erub. Widespread<br />
Mer. Widespread<br />
Masig. Naturalised <strong>and</strong> originating from garden plants.<br />
Warraber. Isolated occurrence<br />
Albany. Isolated occucrence<br />
Dauan. Infestation of several hundred square metres<br />
occupying lower slope of hillside behind church.<br />
Erub. Spreading from garden plants.<br />
Moa (Kubin). Spreading from garden plants on edge of<br />
town area.<br />
Badu. Occurs in a number of situations such as on track<br />
verges to water treatment plant <strong>and</strong> behing quarry. Also<br />
in swamp forest <strong>and</strong> stream banks near town.<br />
Sicklepod (Senna obtusifolia, S. tora) Ugar. Isolated occurrence.<br />
Thursday. Isolated occurrence.<br />
Table 14. Summary of highly invasive species.<br />
Species Isl<strong>and</strong><br />
Gloriosa Lilly (Gloriosa superba) Masig, Erub, Mer, Poruma<br />
Grader Grass (Themeda quadrivalvis) Dauan, Erub, Gebar, Masig, Saibai, Thursday<br />
Barleria prionitis Boigu<br />
Leucaena (Leucaena leucocephala) Boigu, Hammond, Horn, Naghir, Mer, Moa, Muralug, Saibai,<br />
Thursday, Ugar, Warraber<br />
Japanese Sunflower (Tithonia diversifolia) Ugar<br />
Praxelis (Praxelis clematidea) Mabuiag, Masig, Moa, Thursday, Badu, Mer, Horn<br />
Siratro (Macroptlium atropurpurea) Badu, Erub, Thursday<br />
Desmodium tortuosum Iama, Masig, Mer, Muralug, Saibai, ugar, Thursday<br />
Poinciana (Delonix regia) Erub, Mer<br />
Sensitive Weed (Mimosa pudica) Badu, Mabuiag, Saibai<br />
Althernanthera brasiliana Widespread<br />
Khaki Weed (Alternanthera pungens) Mer, Erub, Saibai, Thursday<br />
Mission Grass (Pennisetum penicellata) Horn, Masig, Poruma<br />
Tecoma stans Mabuiag<br />
Snake Weed (Stachytarpheta jamaicensis) Badu, Erub, Mer, Poruma, Masig, Mabuiag, Thursday, Goods,<br />
Moa, Hammond<br />
Cashew (Anacardium occidentale) Badu, Horn<br />
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Species Isl<strong>and</strong><br />
Ipomoea hederifolia Iama, Poruma, Erub, Mer, Moa, Mabuiag, Naghir, Ugar,<br />
Thursday<br />
Agave sisalana Dauan, Iama, Masig, Moa<br />
Castor Oil Bush (Ricinus communis) Poruma, Mer<br />
Angelonia salicariifolia Badu, Boigu, Erub, Hammond, Horn, Moa, Muralug, Saibai<br />
7.2.3 Significant Flora<br />
The field survey recorded a number of significant flora species. Thirteen of the 31 EVR species<br />
known for the study area were recorded with one new record for Queensl<strong>and</strong> <strong>and</strong> some 50 new<br />
records for the Torres Strait. The latter includes disjunct occurrences, <strong>and</strong> numerous range<br />
extensions within the Torres Strait sub-region.<br />
A summary of all EVR species records for the Torres Strait provided in Table 15 is derived from<br />
an analysis of Herbrecs (2007 extract) data, previous relevant studies <strong>and</strong> is supplemented by<br />
survey data. Survey records of EVR’s including brief notes on habitat <strong>and</strong> distribution are<br />
summarised in Table 16 below. Table 17 lists some significant (non-EVR) flora records.<br />
Photo 186. Disjunct occurrence of<br />
Chrysophyllum roxburghii in nonremnant<br />
vegetation on Mer.<br />
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Table 15. Summary of EVR flora records for Torres Strait Isl<strong>and</strong>s (Source: Herbrecs data Oct. 2007<br />
extract). Bold denotes taxa also recorded on 3D field survey, X denotes new records based on 3D survey<br />
results.<br />
NCA<br />
EPBC<br />
Botanical_Name<br />
Albany<br />
Badu<br />
Booby<br />
Dauan<br />
Erub<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
G.Woody<br />
Iama<br />
E - Alectryon<br />
rep<strong>and</strong>odentatus<br />
X X 4<br />
E - Costus potierae 2 2<br />
E - Muellerargia<br />
timorensis<br />
2 1 1 1 1 1 2 1 1<br />
V V Arenga<br />
australasica<br />
1 X X<br />
V - Cissus aristata 1<br />
V V Dendrobium<br />
bigibbum<br />
1 2 1<br />
V V Dendrobium<br />
johannis<br />
1 1<br />
V V Dendrobium<br />
superbiens<br />
x<br />
1<br />
V V Dischidia littoralis 1 X<br />
V V Germainia capitata 2 3<br />
V V Hydriastele costata 1<br />
V - Psydrax reticulata X X X X 3 X X 2 X<br />
R - Apluda mutica 1 2 1<br />
R - Archidendron<br />
hirsutum<br />
X 1<br />
R - Cadetia wariana 3<br />
R Chrysophyllum<br />
roxburghii<br />
X<br />
R - Diospyros<br />
(Bamaga<br />
sp. X X X<br />
R -<br />
B.P.Hyl<strong>and</strong> 2517)<br />
Eremochloa ciliaris 4 1<br />
R - Fatoua villosa 1 5 1<br />
R - Globba marantina 1 3<br />
R - Hoya revoluta 3<br />
R - Lepturus geminatus 1<br />
R - Lobelia<br />
douglasiana<br />
1<br />
R - Neololeba atra X X 1 1 2 X 1 1<br />
R - Operculina brownii 1 1 2 1 2<br />
R - P<strong>and</strong>anus zea X<br />
R - Pimeliodendron<br />
amboinicum<br />
X<br />
R - Secamone<br />
auriculata<br />
1<br />
R - Sterculia<br />
shillinglawii subsp<br />
shillinglawii<br />
X<br />
R - Syzygium aqueum 1<br />
R - Syzygium<br />
buettnerianum<br />
1<br />
Kirriri<br />
Masig<br />
Mer<br />
Moa<br />
Naghir<br />
Horn<br />
Pumpkin<br />
Saibai<br />
Tudu<br />
Ugar<br />
182<br />
Waiben<br />
Warraber<br />
Warral
Table 16. Summary of survey records for EVR flora<br />
Previously Survey Records /<br />
EVR Taxa Records in Torres <strong>Vegetation</strong><br />
Straits<br />
<strong>Communities</strong><br />
Alectryon rep<strong>and</strong>odentatus 4 collections from Erub – 2i, 2j, 22a<br />
- Endangered<br />
Mer<br />
Mer – 2j, 2j(e), 21a,<br />
22a, 2j/15a, 2j (x)<br />
Dauan -1a<br />
Muelleragia timorensis -<br />
Endangered<br />
Dischidia littoralis -<br />
Vulnerable<br />
Arenga australasica –<br />
Vulnerable<br />
(NB. Confirmation of<br />
specimens required with<br />
possibility of A.<br />
microcarpa)<br />
Psydrax reticulata -<br />
Vulnerable<br />
Dendrobium biggibum -<br />
Vulnerable<br />
Archidendron hirsutum -<br />
Rare<br />
Chysophyllum roxburghii -<br />
Rare<br />
Diospyros sp. (Bamaga<br />
B.P.Hyl<strong>and</strong> 2517) -Rare<br />
Dauan, Iama, Mer,<br />
Moa, Pumpkin,<br />
Tuda, Waiben<br />
Notes<br />
Widespread <strong>and</strong> common<br />
species in all forms of vine<br />
forest <strong>and</strong> vine thicket <strong>and</strong><br />
regrowth on Mer <strong>and</strong> Erub.<br />
Survey record from Mt<br />
Cornwallis on Dauan<br />
extends range eastwards.<br />
- Not recorded on survey<br />
however known from<br />
coastal vine thickets.<br />
Requires wet or post wet<br />
season surveys.<br />
Dauan Dauan - 1a Common on upper slopes<br />
of Mt Cornwallis with a<br />
tentative record from<br />
Moa, Dauan,<br />
Naghir<br />
Neololeba atra - Rare Moa<br />
Erub<br />
Naghir<br />
Waiben, Warral,<br />
Muralug, Iama,<br />
Badu, Moa,<br />
Naghir, Horn,<br />
Zuna<br />
Erub, Hammond,<br />
Horn<br />
Moa – 1e, 2p, 3c, 3d<br />
Naghir – 2a, 2v<br />
Dauan – 1a<br />
Muralug – 2u, 16d<br />
Mabuiag – 2x, 4a, 18a<br />
Friday – 4g, 7b<br />
Moa – 4b, 14a, 14d<br />
Wednesday – 5i, 5q,<br />
14c<br />
Hammond – 6e<br />
Mt Adolphus – 14c<br />
Zuna – 14g, 14l<br />
Warral – 18a, 18d<br />
Mabuiag.<br />
New record for Naghir.<br />
Recorded from Moa in<br />
beach scrub, foothill vine<br />
forest <strong>and</strong> mountain vine<br />
forest on Moa. Previously<br />
known from Mt Cornwallis<br />
on Dauan (Herbrecs).<br />
Common shrub/small tree<br />
on acid volcanics <strong>and</strong><br />
granites recorded<br />
throughout continental<br />
isl<strong>and</strong>s.<br />
Muralug – 13j, 13k Coastal vine thicket <strong>and</strong><br />
Melaleuca woodl<strong>and</strong>s<br />
Muralug, Horn, Zuna, Moa,<br />
Moa, Badu Moa – 1e, 1f, 2o, 3d, 4a<br />
Badu - 4a<br />
Mer Mer – Non remnant<br />
Previosly reported<br />
on Moa by<br />
Wannan.<br />
Mabuiag – 4a<br />
Moa – 1a<br />
Badu – 4a<br />
Moa – 1i, 2o, 3d<br />
Badu – 4a<br />
Dauan – 7a<br />
Mer – 2j<br />
Iama, Erub, Naghir<br />
Wednesday, Hammond.<br />
Occasional in footslope <strong>and</strong><br />
upl<strong>and</strong> vine forest.<br />
Understorey of<br />
Welchiodendron dominated<br />
closed forests, footslope<br />
<strong>and</strong> upl<strong>and</strong> rainforest.<br />
P<strong>and</strong>anus zea - Rare Moa Moa – 1g, 1f, 3c, 3d In best development of<br />
ENVF on swampy <strong>and</strong><br />
riverine alluvium <strong>and</strong><br />
upl<strong>and</strong> granite.<br />
Pimeliodendron Moa Moa – 1e In best development of<br />
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EVR Taxa<br />
Previously<br />
Records in Torres<br />
Straits<br />
Survey Records /<br />
<strong>Vegetation</strong><br />
<strong>Communities</strong><br />
Notes<br />
amboinicum - Rare ENVF on upl<strong>and</strong> granite.<br />
Sterculia shillinglawii<br />
subsp shillinglawii - Rare<br />
Moa Moa – 1e, 3c SDNVF granite footslopes<br />
& swampy alluvium.<br />
Table 17. Summary of significant (non-EVR) Flora Records<br />
Species Known Distribution Survey Records<br />
Pending New Records for<br />
Qld <strong>and</strong> Cook<br />
Luvunga monophylla Kimberley, NT, Timor Iama – 2n, 6a<br />
Corymbia latifolia Single record from Muralug (NSW<br />
Herbarium), NT, WA, SW Papua<br />
(Conn et al. 2008).<br />
Muralug – 5k, 5n, 8c<br />
Zuna – 5l<br />
Peltophorum pterocarpum NT Erub (New record for Cook)<br />
Some New Records for<br />
Torres Strait<br />
Known Northern Distribution Survey Records<br />
Aglaia sapindina Lockerbie, PNG Moa - 1f<br />
Anthocarapa nitidula Lockerbie, M<strong>and</strong>uban (PNG) Moa - 1g,1f, 3c<br />
Aristolochia chalmersii Laura Basin Masig - 2m<br />
Mabuiag - 2u<br />
Iama - 6a<br />
Arytera divaricata Lockerbie, PNG Dauan - 1a, 2s<br />
Moa - 1e<br />
Mabuiag -1i<br />
Hammond - 4b<br />
Carissa ovata Hyl<strong>and</strong> et al. (2003) record northern Muralug - 4a, 14g<br />
limit at Bathurst Bay. No Herbrecs<br />
record for study area. Corveg record<br />
from Inner group.<br />
Friday – 5l<br />
Clausena brevistyla Jardine, Lockerbie Moa - 2v<br />
Cordia myxa Mer Muralug – 2q<br />
Corypha utan Aurukun Muralug – 5n<br />
Cupaniopsis flagelliformis Lockerbie Hammond – 2r, 4b, 6e<br />
var. flagelliformis<br />
Iama – 2h<br />
Muralug - 2q, 4b<br />
Badu – 4a<br />
Dysoxylum latifolium Lockerbie Moa – 1e, 4a<br />
Hammond – 4b<br />
Eucalyptus brassiana CYP Horn – 5h<br />
Eucalyptus tetrodonta CYP. No Herbrecs collections but Muralug – 5j, 5k, 5l, 5n, 14j<br />
community type previously mapped on<br />
Muralug by Neldner & Clarkson<br />
(1995).<br />
Zuna – 5l, 14g<br />
Endi<strong>and</strong>ra impressicosta Iron Range, Lockerbie, PNG Dauan – 1a<br />
Muralug - 2q<br />
Hammond - 2r<br />
Erythroxylum sp. (Mosquito North east coast - Cape York Friday - 6a,<br />
Creek J.R.Clarkson 9991+)<br />
Hammond - 4a<br />
Garcinia sp. (Claudie River Iron Range<br />
Moa – 1f<br />
L.J.Brass 19658)<br />
Moa<br />
Gomph<strong>and</strong>ra australiana Lockerbie, PNG Moa – 1e, 1f, 3c<br />
Harpullia arborea Lockerbie, PNG Erub - 22a<br />
Dauan – 1a,<br />
Muralug – 2q<br />
Moa – 1e, 1f<br />
Helicretes semiglabra Pascoe River (also PNG) Saibai – 13b<br />
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Species Known Distribution Survey Records<br />
Horsfieldia australiana Lockerbie, Badu (Garnett & Jackes), Moa – 1i, 3c, 3d<br />
PNG<br />
Badu – 3e, 3g<br />
Indigator fordii Highly disjunct. Known from 6 plants<br />
in southern Mcilwraith.<br />
Muralug – 2q<br />
Lagerstroemia archeriana Lockerbie Muralug – 2q<br />
Livistona benthamii Lockerbie, PNG Saibai – 2c;<br />
Badu -<br />
Melaleuca arcana Jardine Horn – 13a, 13h<br />
Miliusa horsfieldii Lockerbie Muralug – 2q<br />
Neolitsea brassii Lockerbie, PNG Moa – 1g, 3d<br />
Notelaea longifolia Lockerbie Friday- 4a<br />
Mabuiag – 2x, 4a<br />
Muralug – 4a, 4b<br />
Horn – 5i, 14n<br />
Wednesday – 14c<br />
Nypa fruticans Jardine mouth, PNG Muralug – 24c<br />
Palaquium galatoxylon Lockerbie, PNG Moa – 1f<br />
P<strong>and</strong>anus zea Lockerbie Moa – 1g, 1f, 3c, 3d<br />
Pimeliodendron amboinicum Lockerbie, PNG Moa – 1f<br />
Polyalthia australis Lockerbie Moa – 1f<br />
Sterculia shillinglawii subsp.<br />
shillinglawii<br />
Lockerbie, PNG Moa – 1e<br />
Tetrameles nudiflora Schram Creek (Herbrecs). Also PNG<br />
(Conn et al. 2008).<br />
Range Extensions within TSI<br />
Dauan – 2b<br />
10<br />
Acmena hemilampra subsp. Badu (Garnett & Jackes 1983) Moa – 1i, 1j, 3a, 9a<br />
hemilampra<br />
Badu – 3e, 3g, 6g<br />
Adenanthera pavonina Mer Erub, Dauan, Muralug<br />
Aglaia tomentosa (material Moa Muralug – 2q<br />
currently being assessed for<br />
Moa – 1e, 2o, 3c<br />
A. ferruginea by Pannel)<br />
Dauan – 1a<br />
Hammond – 2r, 4a<br />
Albizia lebbeck Waiben, Mer Muralug – 2q<br />
Antidesma parvifolium Albany, Friday, Moa, Gebar Saibai – 2c<br />
Atalaya sericopetala Single collection from Gebar Naghir – 2t, 2u<br />
Erub – 2k, 17b<br />
Moa – 2o, 4a<br />
Muralug – 16d<br />
Friday – 16e<br />
Diospyros sp. (Bamaga Previously reported on Moa by Moa – 1e<br />
B.P.Hyl<strong>and</strong> 2517)<br />
Wannan.<br />
Badu - 4a<br />
Mabuiag – 1d, 1h, 4a<br />
Glycosmis trifoliata Dauan, Moa, Ugar Badu – 4a<br />
Erub – 2k<br />
Iama – 2h, 2u, 2n, 6a<br />
Saibai – 2c<br />
Mabuiag – 2x<br />
Mer – 2j<br />
Rhodamnia australis Lockerbie, Moa Mabuiag – 1d, 2x<br />
Moa – 3a<br />
Triflorensia australis Dauan, Moa Saibai – 2c<br />
Toechima daemellianum Albany Is. Moa – 3c<br />
Voacanga gr<strong>and</strong>iflora Moa Moa – 2v, 3d<br />
Badu – 4a<br />
10 Preliminary-further analysis required.<br />
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185
8.0 Ecosystem Condition<br />
The notion of the ‘naturalness’ or ‘integrity’ of the Torres Strait Isl<strong>and</strong> region can be attributed to<br />
factors such its isolation in combination with underlying climatic conditions, geomorphic history<br />
<strong>and</strong> edaphic controls, but must also acknowledge the influences on the l<strong>and</strong>scape associated with<br />
long-term human occupation. The concept of ‘constructed l<strong>and</strong>scapes’ whereby Indigenous<br />
Australian’s intentionally manipulated their environment through a number of processes is<br />
explored in the Torres Strait Isl<strong>and</strong>s by McNiven (2008), on Saibai Isl<strong>and</strong> by Barham (1999), on<br />
Moa <strong>and</strong> Badu Isl<strong>and</strong>s by Rowe (2006), <strong>and</strong> on coastal north-east Cape York Peninsula by Hynes<br />
<strong>and</strong> Chase (1982). It is not the intention to elaborate on these findings other than to identify the<br />
occurrence of the more readily recognisable aspects of disturbance as they affect or appear to<br />
affect ecosystem condition <strong>and</strong> distribution as observed during this study, <strong>and</strong> to offer brief<br />
descriptive comment. Additional work, which combines the ecological, geomorphological,<br />
archaeological <strong>and</strong> anthropological disciplines, is required to compliment the existing body of<br />
knowledge in this field, <strong>and</strong> the preliminary discussions provided here.<br />
The more obvious anthropogenically altered l<strong>and</strong>scapes have been identified in Section 5.4 <strong>and</strong><br />
include bamboo groves, which are prominent on the eastern basaltic isl<strong>and</strong>s of Mer, Erub <strong>and</strong><br />
Ugar where they commonly form mosaic with vine forest <strong>and</strong> vine thicket communities, <strong>and</strong> have<br />
been identified in the mapping as such. Bamboo groves also occur on the continental isl<strong>and</strong>s of<br />
Moa, Iama, Mabiaug <strong>and</strong> Gebar. The mapping also identifies the extent of vegetation which is<br />
dominated by exotic or naturalised species other than bamboo, <strong>and</strong> recognises extensive areas of<br />
tall closed forest of Mangifera indica (Mango) or Delonix regia (Poinciana), <strong>and</strong> former<br />
grassl<strong>and</strong> areas more recently invaded by Lantana camara (Lantana). Again, the occurrence of<br />
these types is most prominent on Mer <strong>and</strong> Erub where distinctive regrowth formations under tall<br />
<strong>and</strong> senescing Cocos nucifera (Coconut) groves, thought to be old garden sites, were also<br />
observed <strong>and</strong> are discussed in Section 5.2.57.<br />
McNiven (2008) identifies species such as yams (Dioscorea spp.), taro (Colocasia esculenta),<br />
bananas (Musa spp.), sugarcane (Saccharum spp.) <strong>and</strong> sweet potatoes (Ipomoea spp.) as ‘plant<br />
inclusions’ defined as “the strategic addition or translocation of certain ‘exotic’ plants <strong>and</strong><br />
animals to areas”. In contrast to these species, which are often associated with gardens <strong>and</strong><br />
margins of heavily disturbed areas, are species such as Poinciana, Mango <strong>and</strong> Coconut which, by<br />
way of their dispersal <strong>and</strong> adaptive qualities, occur in sufficient quantities to form distinct <strong>and</strong><br />
mappable vegetation communities. Low shrubl<strong>and</strong> <strong>and</strong> vine thicket on Masig Isl<strong>and</strong> mapped in<br />
VC22b, is recognised from analysis of aerial photography in combination with field survey <strong>and</strong><br />
local input as advanced regeneration of former traditional gardens.<br />
Regrowth vegetation, the result of past clearing or partial clearing of natural vegetation, in<br />
varying stages of recovery, is recognised on the majority of isl<strong>and</strong> groups that have been subject<br />
to human occupation <strong>and</strong> are represented in the mapping as the Unit ‘Re’. The derivation of<br />
regrowth examples observed on Erub, where Barringtonia calyptrata groves occur on the<br />
margins of remnant vine forest vegetation, are unclear, however regenerating mangrove<br />
shrubl<strong>and</strong>s on Boigu <strong>and</strong> Iama are the result of recent mechanical actions. On Boigu Isl<strong>and</strong>,<br />
mangrove shrubl<strong>and</strong>s shown in Photographs 187 <strong>and</strong> 188 are a result of l<strong>and</strong> reclamation<br />
initiatives. Contemporary evidence of vegetation clearance (vine forest/thicket on beach ridges)<br />
for traditional gardens is noted Boigu Isl<strong>and</strong> in RE 3.2.2b (see photograph 189). Examples of<br />
larger scale remnant vegetation clearing on Masig Isl<strong>and</strong> (in RE 3.2.6) are associated with recent<br />
major infrastructure developments. Prehistoric gardens on Saibai described by Barham (1999)<br />
are recognised within a discrete mapping unit (VC1e) as distinct from the extensive <strong>and</strong><br />
widespread P<strong>and</strong>anus associated grassl<strong>and</strong> communities (VC11a).<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
186
Photograph 187. Regrowth<br />
mangrove shrubl<strong>and</strong>s on Boigu<br />
Isl<strong>and</strong>.<br />
Photograph 188. Bunding on Boigu Isl<strong>and</strong> for<br />
the purpose of l<strong>and</strong> reclamation.<br />
Photograph 189. Recent clearing of<br />
semi-deciduous vine forest on a dune<br />
flanked by mangroves on Boigu<br />
Isl<strong>and</strong>.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
187
Note should also be made to the impact of the bech-de-mer industry on fragile isl<strong>and</strong><br />
environments. The dem<strong>and</strong>s of the industry for a constant supply of wood to fuel trepang boilers<br />
<strong>and</strong> smokehouses <strong>and</strong> to service beacon fires used to guide passage to working boats throughout<br />
the late 1880’s resulted in isl<strong>and</strong> ecosystems being heavily denuded (Shnukal 2004). On Masig,<br />
incidents such as the cutting of wongai (Manilkara kauki) st<strong>and</strong>s for trepang drying, to fuel<br />
mission steamers, <strong>and</strong> for slipway <strong>and</strong> boat building are reported severely depleted important<br />
seasonal food recources (Shnukal 2004), while the deforestation of Uthu, Yarpar <strong>and</strong> Auridh<br />
contributed to relocation of inhabitants (Teske, 1991 in Shnukal 2004).<br />
The use of fire is evident on the majority of isl<strong>and</strong>s surveyed <strong>and</strong> there is no doubt that its<br />
ongoing use has been fundamental in shaping <strong>and</strong> modifying vegetation cover <strong>and</strong> influencing<br />
habitat diversity across the isl<strong>and</strong>s. McNiven (2008) notes the ethnographic record of Haddon<br />
(1935) where fire use forms an integral part of garden preparation <strong>and</strong> l<strong>and</strong> cleaning in the late<br />
1800’s <strong>and</strong> evidence of fire is also in the pollen <strong>and</strong> phytolith record (Rowe 2006, Parr <strong>and</strong> Carter<br />
2003).<br />
Observations made during the field survey of late season burning of isolated patches of<br />
Sporobolus grassl<strong>and</strong>s surrounded by mangroves on Boigu Isl<strong>and</strong> (see Photograph 13, RE3.1.5)<br />
are evidence of targeted actions to manage grassl<strong>and</strong> ecosystems, possibly to maintain access for<br />
fishing <strong>and</strong> hunting through halting the invasion of mangrove shrubs. Similarly, widespread<br />
annual burning on Saibai Isl<strong>and</strong> appears to maintain open P<strong>and</strong>anus grassl<strong>and</strong>s <strong>and</strong> facilitates<br />
hunting of introduced deer. Field observations from the more remote eastern areas of Saibai<br />
however reveals that succession of grassl<strong>and</strong> to dense shrubl<strong>and</strong>s of Melaleuca cajuputi subsp.<br />
platyphylla <strong>and</strong> Acacia leptocarpa may be occurring in the absence of fire. The phenomenon of<br />
rapid l<strong>and</strong>scape change from grassl<strong>and</strong> to melaleuca dominant shrubl<strong>and</strong>s <strong>and</strong> woodl<strong>and</strong>s is<br />
reported in similar l<strong>and</strong>scapes of southwest Papua where the primary disturbance agent is<br />
believed to be Rusa Deer (Cervus timorensis) (Bartolo et al. 2002, Stronach, 2000). Rusa Deer<br />
are known to occur on Saibai, Boigu <strong>and</strong> on Muralug. Aerial surveys conducted by AQIS in<br />
November 2007 estimate 60 deer on Boigu, <strong>and</strong> 100 on Saibai (Tim Kerlin, pers. comm. June<br />
2008).<br />
Eden (1974) investigated environmental <strong>and</strong> human factors affecting widespread areas of savanna<br />
<strong>and</strong> grassl<strong>and</strong> in southern Papua New Guinea <strong>and</strong> indicated that these ecosystems, over part of<br />
their extent, result from the combined effects of shifting cultivation <strong>and</strong> burning. The influence<br />
of past climatic fluctuations on the origins of these formations are unclear, however, their<br />
maintenance appears to be attributable to human activities, in particular burning (Eden 1974).<br />
Evidence from a number of isl<strong>and</strong>s, particularly Moa <strong>and</strong> Dauan, indicates fire has been a<br />
significant control on the distribution of native grassl<strong>and</strong>, particularly on footslope positions<br />
where the vine forest margins have retreated upslope through repetitive burning. Analysis of the<br />
aerial photo record shows that extensive grassl<strong>and</strong> complexes dominated by Imperata cylindrica<br />
(VC17a) on Moa Isl<strong>and</strong>, an inferred result of repetitive burning, are relatively stable with little<br />
change in areal extent between 1971 <strong>and</strong> the present.<br />
While the influence of fire in the present l<strong>and</strong>scape is considered similar to that of aboriginal<br />
burning practices on mainl<strong>and</strong> Cape York Peninsula, it is evident that the fundamental conditions<br />
of climate, soil fertility, drainage <strong>and</strong> topography also exhibit substantial control on the<br />
vegetation complexity <strong>and</strong> ecology of the isl<strong>and</strong>s. This observation is particularly so for Moa <strong>and</strong><br />
can be extended to the majority of the larger continental isl<strong>and</strong>s including Badu <strong>and</strong> Muralug,<br />
which support outst<strong>and</strong>ing biodiversity values.<br />
In comparison to Cape York Peninsula, where coastal <strong>and</strong> sub-coastal grassl<strong>and</strong>s are under<br />
pressure from exotic weeds <strong>and</strong> from woodl<strong>and</strong> <strong>and</strong> rainforest encroachment associated with<br />
reduced burning frequency <strong>and</strong> intensity (Neldner et al. 1997, Russell-Smith et al. 2002), the<br />
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Saibai Isl<strong>and</strong> grassl<strong>and</strong>s <strong>and</strong> other examples identified on Torres Strait Isl<strong>and</strong>s are in very good<br />
condition. Weed infestations generally associated with grazing pressure, high populations of feral<br />
pigs, <strong>and</strong> agricultural development on Cape York Peninsula are absent from the isl<strong>and</strong><br />
environments. The exceptions are the grassl<strong>and</strong> formations on the basaltic isl<strong>and</strong>s, where a<br />
discussion on the role of fire is provided in previous sections (Sections 5.2.58 <strong>and</strong> 5.2.59). On<br />
Erub <strong>and</strong> to a lesser extent on Mer, the implications of large-scale Lantana infestations in terms of<br />
its influence on fire behavior on rainforest margins are significant. Lantana’s ability to suppress<br />
cool fires yet burn fiercely under severe conditions, promotes serious damage to rainforest<br />
margins, <strong>and</strong> leads to a permanent loss of habitat by its ability to then invade damaged areas<br />
(Stanton <strong>and</strong> Fell 2005).<br />
9.0 Recommendations<br />
9.1 Additional Survey Requirements<br />
The recommendations offered below refer to future survey <strong>and</strong> analysis that will significant<br />
benefit the underst<strong>and</strong>ing of the vegetation on the isl<strong>and</strong>s. Due to constraints placed on field<br />
verification, the vegetation on Badu Isl<strong>and</strong> remains as significant knowledge gap <strong>and</strong> relatively<br />
low confidence is applicable to vegetation mapping over the majority of the isl<strong>and</strong>. Completion<br />
of field survey on the isl<strong>and</strong> is likely to reveal a number of undescribed <strong>and</strong> unique vegetation<br />
communities. A number of vegetation communities, remain poorly characterised as a result of<br />
time <strong>and</strong> budget restrictions <strong>and</strong> are listed below for future consideration.<br />
• Badu Isl<strong>and</strong>;<br />
• Gebar Isl<strong>and</strong> <strong>and</strong> Naghir Isl<strong>and</strong> where steep gully vine forests remain poorly<br />
characterised;<br />
• Floristic assessment of vine forests <strong>and</strong> thickets of Waier <strong>and</strong> Dauar (Mer Group) would<br />
benefit characterisation on vine forests in the region;<br />
• Ugar Isl<strong>and</strong> was not visited in the survey due to time/budgetary constraints <strong>and</strong> would<br />
benefit from further structural <strong>and</strong> floristic assesment;<br />
• Deliverance Isl<strong>and</strong>, the most westerly isl<strong>and</strong> in the Torres Strait, was not visited during<br />
the field survey due to time/budgetary constraints. Further assessment would increase the<br />
underst<strong>and</strong>ing of ecology on this remote <strong>and</strong> potentially unique isle;<br />
• A large number of small, vegetated isl<strong>and</strong> atolls <strong>and</strong> cays have limited field survey<br />
coverage <strong>and</strong> remain poorly described. <strong>Vegetation</strong> on the coral cay isl<strong>and</strong>s is poorly<br />
sampled in relation to the larger continental isl<strong>and</strong>s; <strong>and</strong><br />
• Mt Adolphus Isl<strong>and</strong> remains enigmatic, with a number of potentially unique forest types<br />
requiring description. Negotiation with traditonal l<strong>and</strong>owners will be required prior to<br />
future access.<br />
9.2 Future Opportunities<br />
In addition to the above, a number of the possible initiatives identified in Section 4 of the L<strong>and</strong><br />
<strong>and</strong> Sea Management Strategy for Torres Strait are supported. The majority relate to l<strong>and</strong>scapes,<br />
biodiversity <strong>and</strong> species management <strong>and</strong> build on the extensive data set developed as part of the<br />
RE mapping project.<br />
1. Undertake surveys involving local isl<strong>and</strong> parataxonomists <strong>and</strong> botanists/ecologists,<br />
etnotaxonomists/anthropologists to document traditional <strong>and</strong> contemporary ecological<br />
knowledge including plant names, plant use <strong>and</strong> l<strong>and</strong> management practises. Using the<br />
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189
vegetation community data set as a base, spatially identify culturally significant<br />
environmental l<strong>and</strong>scapes;<br />
2. Identify <strong>and</strong> determine the status of culturally important species <strong>and</strong> instigate appropriate<br />
management actions as required;<br />
3. Undertake further analysis of vegetation data set to map out wetl<strong>and</strong> types, riparian <strong>and</strong><br />
other sensitive vegetation types;<br />
4. Using the flora <strong>and</strong> vegetation data set undertake additional targeted surveys of<br />
threatened <strong>and</strong> significant flora species <strong>and</strong> develop habitat maps to spatially identify<br />
known <strong>and</strong> potential populations. Use this information to inform <strong>and</strong> determine the<br />
regional status of national <strong>and</strong> state species listed under legislation. Prioritise flora<br />
species for management <strong>and</strong> protection within Torres Strait <strong>and</strong> to develop recovery <strong>and</strong><br />
monitoring programs for selected species <strong>and</strong> habitats;<br />
5. Using the flora <strong>and</strong> vegetation data set undertake additional analysis on weed distribution<br />
as a resource to develop pest management plans toward management of highly invasive<br />
weeds;<br />
6. Commission research into fire ecology of grassl<strong>and</strong>s on Mer, Erub <strong>and</strong> Saibai <strong>and</strong><br />
develop fire management plans for priorty isl<strong>and</strong>s;<br />
7. Develop culturally appropriate individual isl<strong>and</strong> l<strong>and</strong> management guides incorporating<br />
vegetation maps <strong>and</strong> flora assessments suitable for use as a resource for isl<strong>and</strong> councils,<br />
l<strong>and</strong> <strong>and</strong> sea rangers <strong>and</strong> schools;<br />
8. Support publication of the findings of the current project.<br />
Photo 190. Authors David Stanton (left) <strong>and</strong> David Fell.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
190
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Neldner, V.J., Wilson, B.A., Thompson, E.J. <strong>and</strong> Dillewaard, H.A. (2005). Methodology for<br />
survey <strong>and</strong> mapping of regional ecosystems <strong>and</strong> vegetation communities in Queensl<strong>and</strong>.<br />
Version 3.1. Environmental Protection Agency, Brisbane.<br />
http://www.epa.qld.gov.au/publications?id=1418.<br />
Orme, A. R. (1990). The Instability of Holocene coastal dunes: The case of the Morro Dunes,<br />
California. In K. F. Nordstrom, N. Psuty, R. W. G. Carter (eds) Coastal dunes: form <strong>and</strong><br />
process’. John Wiley <strong>and</strong> Sons, Chichester, pp. 315 – 336.<br />
Paijmans, K., Blake, D.H. <strong>and</strong> Bleeker, P. (1971). L<strong>and</strong> Systems of the Morehead-Kiunga Area,<br />
In L<strong>and</strong> Resources of the Morehead-Kiunga Area, Papua New Guinea. L<strong>and</strong> Research<br />
Series No. 29, CSIRO 1971.<br />
Parr, J.F. <strong>and</strong> Carter, M. (2003). "Phytolith <strong>and</strong> starch analysis of sediment samples from two<br />
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History <strong>and</strong> Archaeobotany 12(2): 131-141.<br />
Rowe, C. (2007). A palynological investigation of Holocene vegetation change in Torres Strait,<br />
seasonal tropics of northern Australia. Palaeogeography, palaeoclimatology,<br />
Palaeoecology 251: 83-103.<br />
Russell-Smith, J., Stanton, P.J., Whitehead, P.J., Edwards, A.C. (2004). Rain forest invasion of<br />
eucalypt-dominated woodl<strong>and</strong> savanna, Iron Range, north-eastern Australia: I.<br />
Successional processes. Journal of Biogeography 31 (8), 1293–1303.<br />
Russell-Smith, J., Stanton, P.J. Edwards, A.C., Whitehead, P.J. (2004). Rain forest invasion of<br />
eucalypt-dominated woodl<strong>and</strong> savanna, Iron Range, north-eastern Australia: II. Rates of<br />
l<strong>and</strong>scape change. Journal of Biogeography 31 (8), 1305–1316.<br />
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ISSN 1440-4788.<br />
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Growth <strong>and</strong> Biodiversity. Oxford University Press, Melbourne.<br />
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of Mineral Resources, Geology <strong>and</strong> Geophysics. Australian Government Publishing<br />
Service, Canberra.<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
195
11. Appendices<br />
<strong>Appendix</strong> A1. Map Legend - <strong>Vegetation</strong> Communties<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
196
Client<br />
Scale<br />
Legend<br />
Evergreen vine forest <strong>and</strong> vine thicket<br />
1a, Evergreen notophyll vine forest + Acmenospermum claviflorum + Syzigium puberulum + Ganophyllum falcatum + Arytera divaricata +<br />
Ficus microcarpa + *Mangifera indica.Granite ranges.<br />
1b, Evergreen notophyll vine thicket (windsheared) + Manilkara kauki + Intsia bijuga + Pouteria sericea + Aglaia eleagnoidea + Garcinia<br />
warrenii + P<strong>and</strong>anus sp. Granite footslopes.<br />
1c, Evergreen notophyll vine thicket (windsheared) + Manilkara kauki + Celtis philippensis + Terminalia muelleri + Diospyros maritima +<br />
Thespesia populniodes + Drypetes deplanchei.Coastal dunes.<br />
1d, Mesophyll/notophyll vine forest + Endi<strong>and</strong>ra glauca + Acacia polystachya + Syzygium bungadinia + Canarium australianum + Dysoxylum<br />
oppositifolium. Granite <strong>and</strong> rhyolite slopes<br />
1e, Mesophyll/notophyll vine forest + Myristica insipida + Maranthes corymbosa + Cryptocarya cunninghamii + Dysoxylum latifolium +<br />
Calophyllum sil +/- Arenga australasica. Granite footslopes.<br />
1f, Complex notophyll vine forest + Pouteria sp. + Calophyllum sil sp. + Argyrodendron poly<strong>and</strong>rum + Palaquim galactoxylon<br />
+ Acmenospermum claviflorum + Licuala ramsayii. Upper slopes on granite.<br />
1g, Evergreen notophyll vine thicket + Calophyllum sil + Syzygium br<strong>and</strong>erhorstii + Diospyros hebecarpa + Schefflera actinophylla +<br />
Podocarpus grayae +Licuala ramsayi. Upper slopes on granite.<br />
1h, Evergreen notophyll vine thicket with Buchanania arborescens + Drypetes deplanchei + Eleaodendron melanocarpum + Endi<strong>and</strong>ra<br />
glauca + Elaeocarpus arnhemicus + Chionanthus ramiflora. Talus slopes on rhyolite.<br />
1i. Evergreen mesophyll vine forest + Horsfieldia australiana, Syzygium bamagense + Acmena hemilampra subsp. hemilampra +<br />
Buchanania arborescens<br />
1j, Tall evergreen notophyll vine forest + Syzygium angophoroides+Acmena hemilampra + Acacia aulacocarpa +Syzygium<br />
forte subsp. forte + Podocarpus greyae<br />
Deciduous/Semi deciduous vine forest <strong>and</strong> vine thicket<br />
2a, Deciduous/Semi-deciduous vine forest + Erythrina variegata + Manilkara kauki + Terminalia subacroptera + Mimusops elengii + Cordia<br />
subcordata.Calcareous beach ridges.<br />
2b, Semi deciduous vine forest/thicket + Canarium australianum + Terminalia subacroptera + Bombax ceiba var. leiocarpum +<br />
Cochlospermum gillivreai + Cleistanthus peninsularis + Ficus virens var. sublanceolata. Footslopes on granite <strong>and</strong> rhyolite.<br />
2c, Semi-deciduous vine thicket + Mimusops elengii + Acacia auricauliformis + Terminalia subactroptera + Diospyros spp. +/- Manilkara kauki<br />
+/- Melaleuca cajuputi subsp. platyphylla. Alluvial plains<br />
2d, Semi deciduous vine forest + Tetrameles nudiflora + Canarium australianum + Ficus spp. + Bombax ceiba var. leiocarpum +/- Alstonia<br />
spectabilis. Granite slopes.<br />
2e, Semi deciduous vine thicket + Terminalia subacroptera + Intsia bijuga + Hibiscus tiliaceus + Excoecaria agallocha + Thespesia populneoides<br />
+ Cathormion umbellatum subsp. moniliforme.<br />
2f, Semi-deciduous vine thicket + Canarium australianum + Manilkara kauki + Dalbergia densa var. australis + Buchanania arborescens +<br />
Sterculia sp. (Annan River L.J. Brass 20319) + Cochlospermum gillivraei. Coastal escarpments on rhyolite.<br />
2g, Semi deciduous notophyll vine forest + Canarium australianum + Terminalia subacroptera + Semecarpus australiensis + Buchanania<br />
arborescens + Acacia auricauliformis +/- Erythrina variegata +/- Welchiodendron longivalve +/- Parinari nonda +/- Chionanthus ramiflora<br />
2h, Deciduous notophyll vine forest + Erythrina insularis +/- Antiaris toxicaria var. macrophylla+/- Terminalia subacroptera +/- Bombax ceiba<br />
var. leiocarpum +/- Canarium australianum + Acacia auricauliformis. Granite <strong>and</strong> rhyolite footslopes.<br />
2i, Semi deciduous notophyll vine thicket + Berrya javanica + Cupaniopsis anacardioides + Bombax ceiba var. leicocarpum + Diospyros<br />
hebecarpa + Mimusops elengii + Melicope peninsularis. Basalt escarpments.<br />
2j, Semi-deciduous notophyll vine forest +Bombax ceiba var. leicocarpum + Diospyros hebecarpa +/- Alectryon rep<strong>and</strong>odentatus +<br />
Cupaniopsis anacardiodes + Alstonia spectabilis +/- Melicope peninsularis. Basalt hills.<br />
2k, Deciduous vine forest + Gyrocarpus americanus + Bombax ceiba var. leiocarpum + Antiaris toxicarya var. macrophylla + Canarium<br />
australianum + Cathormion umbellatum subsp. monoliforme + Garuga floribunda var. floribunda +/- Adenanthera pavonina +/- Maranthes<br />
corymbosa .Basalt footslopes.<br />
2l, Semi-deciduous notophyll vine forest + Bombax ceiba var. leiocarpum + Gyrocarpus americanus + Garuga floribunda var. floribunda<br />
+ Manilkara kauki + Diospyros maritima + Celtis philippensis. Coastal dune.<br />
2m, Semi-deciduous notophyll vine forest + Milletia pinnata + Terminalia spp. + Diospyros maritima + Manilkara kauki + Aglaia eleagnoidea<br />
+ Pouteria obovata + Drypetes deplanchei +/- Erythrina spp. Coral cays.<br />
2n, Semi deciduous notophyll vine thicket + Canarium australianum + Antiaris toxicarya var. macrophylla + Acacia auricauliformis + Terminalia<br />
subacroptera + Manilkara kauki + Bombax ceiba var. leiocarpum. Granite headl<strong>and</strong>s.<br />
2o, Semi deciduous notophyll vine forest + Acacia sp. (DGF8919+) + Barringtonia calyptrata + Maranthes corymbosa + Syzygium forte subsp.<br />
forte + Bombax ceiba var. leicarpum + Canarium australianum. Footslopes on metagranite.<br />
2p, Semi deciduous vine thicket (windsheared) + Bombax ceiba var. leiocarpum + Premna serratifolia + Acacia crassicarpa + Manikara kauki<br />
+ Drypetes deplanchei + Terminalia subacroptera +/- Arenga australasica. Coastal dunes.<br />
2q, Tall semi deciduous vine forest + Bombax ceiba var. leiocarpum + Berrya javanica + Antiaris toxicarya var. macrophylla + Garuga<br />
floribunda var. floribunda + Canarium australianum +/- Albizia lebbeck +/- Syzygium bamagense +/- Maranthes corymbosa.<br />
Diorite knolls <strong>and</strong> footslopes.<br />
2r, Semi deciduous vine forest + Sterculia quadrifida + Canarium australianum + Cleistanthus peninsularis + Terminalia subacroptera +<br />
Antiaris toxicarya var. macrophylla +/- Paraserianthes toona + Alstonia actinophylla +/- Xanthoxylon rhetsa +/- Maniltoa lenticellata var.<br />
lenticellata. Diorite footslopes.<br />
2s, Semi-deciduous notophyll vine thicket (windsheared) + Pouteria sericea + Ficus virens var. sublanceolata + Schefflera actinophylla +<br />
Garcinea warrenii + Syzygium puberulum. Granite hillslopes.<br />
2t, Semi-deciduous notophyll vine forest <strong>and</strong> occasional thicket with Bombax ceiba var. leiocarpum + Canarium australianum + Terminalia spp.<br />
+ Acacia polystachya.<br />
2u, Semi-deciduous vine forest + Manilkara kauki + Terminalia spp. + Sterculia quadrifida + Premna serratifolia + Acacia crassicarpa<br />
+ Drypetes deplanchei + Millettia pi¤ata. Coastal dunes.<br />
2v, Semi-deciduous vine thicket + Acacia polystachya <strong>and</strong> Terminalia subacroptera. Coastal headl<strong>and</strong>s on rhyolite <strong>and</strong> granite.<br />
2w, Deciduous vine thicket + Garuga floribunda var. floribunda+ Gyrocarpus americana + Bombax ceiba var. leiocarpum +/- Antiaris<br />
toxicarya var. macrophylla. Escarpments on basalt <strong>and</strong> scoria cones.<br />
2x, Deciduous vine thicket + Cochlospermum gillivraei + Bombax ceiba var. leiocarpum + Terminalia subacroptera +Sterculia quadrifida<br />
+ Psydrax reticulata + Drypetes deplanchei. Acid volcanic pavements.<br />
2y, Semi-deciduous vine thicket + Manilkara kauki + Terminalia subacroptera + Cordia subcordata + Premna serratifolia + Indeterminate<br />
species. Coral cays.<br />
2z, Low groved notophyll vine thicket + Sterculia quadrifida + Manilkara kauki + Eugenia reinwardtiana + P<strong>and</strong>anus sp. Beach ridges.<br />
Legend- <strong>Vegetation</strong> <strong>Communities</strong> <strong>and</strong> Broad<br />
<strong>Vegetation</strong> Groups of the Torres Strait Isl<strong>and</strong>s<br />
Torres Strait <strong>Regional</strong> Authority<br />
3D Environmental<br />
<strong>Vegetation</strong> Assessment<br />
& Mapping Specialists<br />
P. O. Box 959<br />
Kenmore, Qld 4069<br />
Phone: (07) 3411 9072; (07) 3878 4344<br />
Mobile: 0404 577 285; 0409 426 916<br />
www.3denvironmental.com.au<br />
File Path C:\3D Environmental\<br />
Drawn By DG Checked DS Torres\3d_TS_Maps_legend.mxd Date<br />
28/08/08<br />
A3
Swamp <strong>and</strong> riparian forest complexes<br />
Acacia dominant open forests <strong>and</strong> woodl<strong>and</strong>s<br />
Legend- <strong>Vegetation</strong> <strong>Communities</strong> <strong>and</strong> Broad<br />
<strong>Vegetation</strong> Groups of the Torres Strait Isl<strong>and</strong>s<br />
Client<br />
Scale<br />
Legend<br />
3a, Lophostemon suaveolens + Melaleuca quinquenervia + Syzygium angophoroides + Asteromyrtus brassii + Dillenia alata swamp forest<br />
complex. Alluvial depressions, drainage lines <strong>and</strong> dune swales.<br />
3b, Medium to tall Melaleuca leuc<strong>and</strong>endra +/- Melaleuca argentea + Syzygium forte subsp. forte + Dillenia alata open forest.<br />
Fluvial s<strong>and</strong>s <strong>and</strong> silts.<br />
3c, Tall Melaleuca dealbata / Melaleuca leucadendra open forest/Acacia sp. open forest / Mesophyll vine forest complex. Seasonal swamps.<br />
3d, Evergreen mesophyll vine forest / Sclerophyll vine forest complex + Syzygium forte subsp. forte + Syzygium bamagense + Horsfieldia<br />
Australiana +/- Melaleuca leucadendra +/- Lophostemon suaveolens. (1i/3b- 50/50)<br />
3e, Melaleuca quinquenervia + P<strong>and</strong>anus sp. +/- Deplanchea tetraphylla swamp forest/ Lophostemon suaveolens +/- Asteromyrtus brassii<br />
+/- Acacia crassicarpa +/- Deplanchea tetraphylla open swamp forest complex (7d/8b -50/50).<br />
3f, Lophostemon suaveolens + Melaleuca leucadendra + Corymbia clarksoniana open forest.<br />
3g, Tall Melaleuca dealbata + Acacia crassicarpa + Acmena hemilampra + Deplanchea tetraphylla + Syzygium forte subsp. forte swamp<br />
forest complex.<br />
Welchidendron dominant closed to open forests <strong>and</strong> wo<br />
4a, Welchiodendron longivalve + Acacia polystachya +/- Terminalia subacroptera +/- Canarium australianum +/- Bombax ceiba var.<br />
leiocarpum open to closed forest.<br />
4b, Welchiodendron longivalve low woodl<strong>and</strong>, low open woodl<strong>and</strong> <strong>and</strong> tall open shrubl<strong>and</strong><br />
4c, Low Welchiodendron longivalve + Melaleuca dealbata open forest. Granite footslopes <strong>and</strong> peidmont fans.<br />
Eucalypt dominant open forests <strong>and</strong> woodl<strong>and</strong>s<br />
5a, Corymbia novoguinensis +/- Eucalyptus stockeri subsp. peninsularis woodl<strong>and</strong> <strong>and</strong> open forest. Remnant s<strong>and</strong>y plains.<br />
5b, Corymbia clarksoniana + Corymbia nesophila +/- Corymbia tessellaris +/- Corymbia stockerii subsp. Peninsularis +/- Welchidendron<br />
longivalve woodl<strong>and</strong> <strong>and</strong> open forest. Alluvial, remnant s<strong>and</strong>y plains <strong>and</strong> granite footslopes.<br />
5c, Corymbia clarksoniana + Melaleuca stenostachya + Melaleuca viridiflora +/- Asteromyrtus symphiocarpa +/- Parinari nonda +/-<br />
Asteromyrtus brassii woodl<strong>and</strong>. Alluvial plains <strong>and</strong> s<strong>and</strong>y rises.<br />
5d, Low Corymbia clarksoniana + Melaleuca viridiflora + Welchiodendron longivalve + Asteromyrtus brassii + Acacia leptocarpa woodl<strong>and</strong><br />
<strong>and</strong> shrubl<strong>and</strong> complex. Acid volcanic hills.<br />
5e, Low to medium Corymbia nesophila +/- Welchiodendron longivalve +/- Eucalyptus leptophleba open forest <strong>and</strong> woodl<strong>and</strong>.<br />
Acid volcanic hillslopes.<br />
5f, Eucalyptus leptophleba +/- Acacia polystachya woodl<strong>and</strong> <strong>and</strong> open forest. Granite footslopes.<br />
5g, Corymbia tessellaris + Acacia polystachya +/- Welchiodendron longivalve woodl<strong>and</strong> <strong>and</strong> open forest. Granite hillslopes <strong>and</strong> s<strong>and</strong>y alluvium.<br />
5h, Corymbia spp. + Melaleuca saligna + Acacia crassicarpa +/- Eucalyptus platyphylla +/- Eucalyptus brassiana open forest.<br />
Swampy drainage lines.<br />
5i, Corymbia clarksoniana +/- Corymbia novoguinensis +/- Livistona muelleri woodl<strong>and</strong> <strong>and</strong> open forest. Coastal dunes <strong>and</strong><br />
s<strong>and</strong>y alluvial outwash.<br />
5j, Eucalyptus tetrodonta + Corymbia nesophila +/- Corymbia clarksoniana +/- Corymbia novoguinensis +/- Corymbia stockeri subsp.<br />
peninsularis open forest. Coastal dunes <strong>and</strong> remnant s<strong>and</strong>y plains.<br />
5k, Corymbia nesophila +/- Corymbia stockeri subsp. peninsularis +/- Eucalyptus tetrodonta woodl<strong>and</strong> <strong>and</strong> open forest. Alluvial plains,<br />
s<strong>and</strong>y rises <strong>and</strong> stabilised dunes.<br />
5l, Corymbia stockeri subsp. peninsularis +/- Corymbia nesophila +/- Eucalyptus tetrodonta +/- Eucalyptus cullenii woodl<strong>and</strong>.<br />
Hillslopes on rhyolite <strong>and</strong> granite.<br />
5m, Low Corymbia spp. (C. stockeri, C. nesophila, C. clarksoniana) + Melaleuca stenostachya +/- Melaleuca viridiflora +/- Asteromyrtus<br />
symphiocarpa woodl<strong>and</strong>. Alluvial outwash <strong>and</strong> degraded dunes.<br />
5n, Eucalyptus platyphylla + Erythrophloeum chlorostachys +/- Corymbia nesophila +/- Corymbia novoguinensis +/- Eucalyptus tetrodonta<br />
+/- Corymbia stockeri subsp. peninsularis woodl<strong>and</strong> <strong>and</strong> open forest. Alluvial terraces <strong>and</strong> degraded dunes.<br />
5o, Corymbia tessellaris +/- Corymbia clarksoniana woodl<strong>and</strong> <strong>and</strong> open woodl<strong>and</strong>. Coastal dunes, alluvial plains <strong>and</strong> acid volcanic hillslopes.<br />
5p, Low Corymbia polycarpa/Corymbia novoguinensis + Acacia crassicarpa + Teminalia subacroptera +/- Sterculia quadrifida +/- Syzygium<br />
suborbiculare woodl<strong>and</strong> <strong>and</strong> open woodl<strong>and</strong>. Coastal dunes<br />
5q, Low Corymbia stockeri subsp. peninsularis open forest. Alluvial plains <strong>and</strong> degraded dunes<br />
5r, Corymbia nesophila woodl<strong>and</strong> <strong>and</strong> open forest. Acid volcanic hills, alluvial plains <strong>and</strong> residual s<strong>and</strong>s.<br />
5s, Corymbia clarksoniana +/- Corymbia tessellaris woodl<strong>and</strong>. Acid volcanic hillslopes <strong>and</strong> coastal alluvial plains.<br />
5t, Eucalyptus platyphylla +/- Corymbia stockeri subsp. peninsularis +/- Corymbia nesophila +/- Corymbia clarksoniana woodl<strong>and</strong>.<br />
Alluvial plains <strong>and</strong> acid volcanic hillslopes (<strong>and</strong> minor coastal dunes).<br />
5u, Eucalyptus platyphylla +/- Corymbia tessellaris woodl<strong>and</strong> <strong>and</strong> open woodl<strong>and</strong>. Coastal dunes, alluvial plains <strong>and</strong> acid<br />
volcanic/plutonic headl<strong>and</strong> <strong>and</strong> hillslopes.<br />
5v, Eucalytpus stockerii sub.sp peninsularis + Welchidendron longivalve + Acacia polystachya +/- Corymbia tessellaris woodl<strong>and</strong>/<br />
open forest complex. Granite hills.<br />
6a, Low to medium Acacia auricauliformis +/- Terminalia subacroptera +/- Antiaris toxicarya var. macrophylla +/- Bombax<br />
ceiba var. leiocarpum open forest/woodl<strong>and</strong>/ (<strong>and</strong> occasional shrubl<strong>and</strong>).Granite hillslopes<br />
6b, Low to medium Acacia auricauliformis +/- Parinari nonda +/- P<strong>and</strong>anus sp. +/- Semecarpus australiensis open forest/woodl<strong>and</strong><br />
(<strong>and</strong> occasional shrubl<strong>and</strong>). Coastal alluvial plains<br />
6c, Low Acacia crassicarpa + Terminalia subacroptera + Sterculia quadrifida + Manilkara kauki + Syzygium suborbiculare open forest<br />
<strong>and</strong> woodl<strong>and</strong>. Beach ridges.<br />
6d, Low Acacia crassicarpa + Melaleuca spp. open forest. Dune swales.<br />
6e, Low Acacia polystachya + Alstonia actinophylla + Buchanania arborescens + Manilkara kauki + Pouteria sericea + Sterculea quadrifida<br />
open to closed forest. Exposed slopes on diorite.<br />
6f, Acacia sp. closed shrubl<strong>and</strong>. Acid volcanic escarpments.<br />
6g, Acacia crassicarpa +Asteromyrtus brassii open forest <strong>and</strong> low open forest. Coastal dunes.<br />
Torres Strait <strong>Regional</strong> Authority<br />
3D Environmental<br />
<strong>Vegetation</strong> Assessment<br />
& Mapping Specialists<br />
P. O. Box 959<br />
Kenmore, Qld 4069<br />
Phone: (07) 3411 9072; (07) 3878 4344<br />
Mobile: 0404 577 285; 0409 426 916<br />
www.3denvironmental.com.au<br />
File Path C:\3D Environmental\<br />
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Melaleuca dominant open forests<br />
Client<br />
Scale<br />
Legend<br />
7a, Low Melaleuca cajuputi subsp. platyphylla open forest. Alluvial plains <strong>and</strong> drainage depressions.<br />
7b, Melaleuca saligna open forest. Alluvial plains, drainage depressions <strong>and</strong> dune swales.<br />
7br, Melaleuca saligna open forest. Riparian fringes on alluvium.<br />
7bs, Melaleuca saligna open forest. Alluvial margins of salt pans<br />
7c, Tall Melaleuca dealbata + Corymbia clarksoniana open forest. Alluvial plains<br />
7d, Melaleuca quinquenervia +/- Melaleuca saligna +/- Melaleuca cajuputi subsp. platyphylla +/- Lophostemon suaveolens open forest.<br />
Coastal dunes <strong>and</strong> alluvial swamps.<br />
7e, Low Melaleuca dealbata +/- Melaleuca saligna +/- Lophostemon suaveolens open forest. Dune swales.<br />
7f/7fs, Melaleuca leucadendra open forest. Seasonal swamps <strong>and</strong> riparian margins.<br />
7g, Melaleuca dealbata woodl<strong>and</strong> <strong>and</strong> open forest. Coastal dune complexes<br />
Lophostemon dominant woodl<strong>and</strong> <strong>and</strong> open forest<br />
8a, Lophostemon suaveolens +/- Melaleuca cajuputi subsp. platyphylla +/- P<strong>and</strong>anus sp. +/- Livistona muelleri woodl<strong>and</strong> <strong>and</strong> open forest.<br />
Alluvial remnants of the Fly Platform.<br />
8b, Low Lophostemon suaveolens +/- Melaleuca saligna + Asteromyrtus brassii + Acacia crassicarpa open forest. S<strong>and</strong>y alluvial soils.<br />
8c, Low Lophostemon suaveolens + Corymbia clarksoniana + Asteromyrtus symphiocarpa + Melaleuca saligna + Melaleuca viridiflora<br />
+/- Corymbia latifolia open woodl<strong>and</strong>. Degraded dune margins.<br />
Asteromyrtus/Neofabricia dominant open forests<br />
9a, Asteromyrtus brassii + Syzygium angophoroides + Acmena hemilampra subsp. hemilampra +/- Acacia crassicarpa +/- Melaleuca<br />
quinquenervia open forest. S<strong>and</strong>y rises erosional plain.<br />
9b, Neofabricia myrtifolia + Parinari nonda + Sterculia quadrifida + Terminalia muelleri +Milletia pinnata closed to open forest. Coastal dunes<br />
Casuarina dominant woodl<strong>and</strong> <strong>and</strong> open forest<br />
10a, Casuarina equisetifolia open forest + Diospyros maritima + Premna serratifolia + Milletia pinnata. Coral cays<br />
10b, Casuarina equisetifolia woodl<strong>and</strong> <strong>and</strong> open forest +/- Terminalia catappa woodl<strong>and</strong> <strong>and</strong> open forest. Coastal foredune<br />
P<strong>and</strong>anus dominant woodl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong><br />
11a, P<strong>and</strong>anus sp. +/- Melaleuca catjaputi subsp. platyphylla +/- Acacia leptocarpa +/- Melaleuca acacioides shrubl<strong>and</strong> <strong>and</strong> low<br />
woodl<strong>and</strong>. Alluvial plains (Quaternary <strong>and</strong> Pleistocene).<br />
11b, P<strong>and</strong>anus sp. +/- Melaleuca viridiflora open forest, woodl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong>. Seepage zones on alluvium, dune swales<br />
<strong>and</strong> granite headl<strong>and</strong>s.<br />
Palm dominant forest <strong>and</strong> woodl<strong>and</strong>s<br />
12a, Livistona meulleri woodl<strong>and</strong>. Granite footslopes.<br />
12b, Low Nypa fruiticans closed forest. Brackish tidal areas<br />
Melaleuca dominant shrubl<strong>and</strong>s <strong>and</strong> woodl<strong>and</strong>s<br />
13a, Melaleuca viridiflora +/- P<strong>and</strong>anus sp. shrubl<strong>and</strong> <strong>and</strong> low woodl<strong>and</strong>. Alluvial plains, residual s<strong>and</strong>s, acid volcanic slopes<br />
<strong>and</strong> coastal dunes.<br />
13b, Melaleuca cajuputi subsp. platyphylla +/- P<strong>and</strong>anus sp. shrubl<strong>and</strong>. Alluvial plains.<br />
13c, Melaleuca viridiflora + Asteromyrtus symphiocarpa +/-Asteromyrtus brassii + /- Banksia dentata +/- Melaleuca saligna<br />
+/- Leucopogon ruscifolius shrubl<strong>and</strong>. Alluvial soils <strong>and</strong> residual s<strong>and</strong> plains.<br />
13d, Melaleuca saligna + Melaleuca viridiflora + Asteromyrtus symphiocarpa +/- Asteromyrtus brassii +/- Corymbia spp.<br />
+/- Banksia dentata low woodl<strong>and</strong>. Alluvial outwash plains, residual s<strong>and</strong>s <strong>and</strong> coastal dunes.<br />
13e, Melaleuca acacioides shrubl<strong>and</strong>. Alluvial outwash on saline margins.<br />
13f, Low Melaleuca viridiflora + Corymbia clarksoniana woodl<strong>and</strong>. Alluvial plains <strong>and</strong> residual s<strong>and</strong>s.<br />
13g, Low Melaleuca saligna shrubl<strong>and</strong>. Seasonal swamps.<br />
13h, Low Melaleuca arcana closed shrubl<strong>and</strong>. Dune swamps.<br />
13i, Melaleuca stenostachya shrubl<strong>and</strong> +/- Melaleuca viridiflora low woodl<strong>and</strong>. Alluvial plains <strong>and</strong> granite headl<strong>and</strong>s.<br />
13j, Melaleuca acacioides +/- Melaleuca viridiflora open shrubl<strong>and</strong>. Alluvial outwash on saline margins.<br />
Shrubl<strong>and</strong>s <strong>and</strong> shrubl<strong>and</strong> complexes<br />
14a, Dwarf Welchiodendron longivalve + Alyxia spicata +/- Melaleuca viridiflora +/- Acacia spp. +/- Asteromyrtus brassii shrubl<strong>and</strong>.<br />
Coastal headl<strong>and</strong>s <strong>and</strong> ridgelines.<br />
14b, Melaleuca catjaputi subsp. platyphylla + Acacia auricauliformis +/- Terminalia subacroptera open scrub <strong>and</strong> low open forest.<br />
Alluvial remnants of the Fly Platform.<br />
14c, Welchiodendron longivalve shrubl<strong>and</strong>. Escarpments <strong>and</strong> hillslopes on rhyolite <strong>and</strong> granite<br />
14d, Cochlospermum gillivraei +/- Canarium australianum +/- Welchiodendron longivalve deciduous shrubl<strong>and</strong>. Coastal headl<strong>and</strong>s on<br />
acid volcanic rocks<br />
14e, Low open shrubl<strong>and</strong> with Baeckea frutescens, Melaleuca viridiflora <strong>and</strong> Asteromyrtus brassii. Residual s<strong>and</strong> dunes.<br />
14f, Melaleuca viridiflora + Melaleuca stenostachya + Welchiodendron longivalve + Acacia leptocarpa +/- Cochlospermum gillivraei<br />
shrubl<strong>and</strong>. Coastal headl<strong>and</strong>s on rhyolite <strong>and</strong> granite.<br />
14g, Low Alyxia spicata + Manilkara kauki +/- Buchanania arborescens +/- Canarium australianum +/- Diospyros spp. +/-<br />
P<strong>and</strong>anus sp. low closed shrubl<strong>and</strong>/ rock pavement complex.<br />
14h, Acacia polystachya +/- Welchiodendron longivalve closed shrubl<strong>and</strong>. Granite hillslopes<br />
14i, Asteromrytus brassii + Melaleuca saligna + Baeckea frutescens + Leucopogon yorkensis + Leucopogon ruscifolius +/- Lophostemon<br />
suaveolens shrubl<strong>and</strong> <strong>and</strong> low shrubl<strong>and</strong>. Residual s<strong>and</strong> plains.<br />
14j, Acacia brassii +/- Welchiodendron longivalve closed shrubl<strong>and</strong>. Acid volcanic pavements.<br />
Legend- <strong>Vegetation</strong> <strong>Communities</strong> <strong>and</strong> Broad<br />
<strong>Vegetation</strong> Groups of the Torres Strait Isl<strong>and</strong>s<br />
Torres Strait <strong>Regional</strong> Authority<br />
3D Environmental<br />
<strong>Vegetation</strong> Assessment<br />
& Mapping Specialists<br />
P. O. Box 959<br />
Kenmore, Qld 4069<br />
Phone: (07) 3411 9072; (07) 3878 4344<br />
Mobile: 0404 577 285; 0409 426 916<br />
www.3denvironmental.com.au<br />
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A3
Shrubl<strong>and</strong>s <strong>and</strong> shrubl<strong>and</strong> complexes (Continued)<br />
Client<br />
Scale<br />
Legend<br />
14k, Low Melaleuca stenostachya + Asteromyrtus symphiocarpa + Jacksonia thesioides + Melaleuca viridiflora shrubl<strong>and</strong>.<br />
Acid volcanic pavements.<br />
14l, Low Melaleuca sp. (Zuna DGF9257+) + Welchiodendron longivalve + Corymbia spp. + Acacia brassii + Melaleuca stenostachya<br />
+ Jacksonia thesioides shrubl<strong>and</strong>. Coastal headl<strong>and</strong>s on acid volcanic <strong>and</strong> igneous rocks.<br />
14m, Grevillea striata + Acacia crassicarpa + Melaleuca viridiflora + Parinari nonda + P<strong>and</strong>anus sp. + Corymbia tessellaris<br />
shrubl<strong>and</strong>. Alluvial plains.<br />
14n, Acacia crassicarpa + Leucopogon ruscifolius +/- Neofabricia myrtifolia +/- Pouteria sericea +/- Psydrax banksii +/- Halfordia<br />
kendack shrubl<strong>and</strong> <strong>and</strong> open shrubl<strong>and</strong>.<br />
14o, Melaleuca saligna dominant riparian shrubl<strong>and</strong> complex. Riparian alluvial fringes <strong>and</strong> gravel beds.<br />
14p, Asteromyrtus brassii + Petalostigma pubescens + Melaleuca viridiflora + Asteromyrtus brassii + Acacia crassicarpa +<br />
Corymbia clarksoniana shrubl<strong>and</strong>. Acid volcanic hills.<br />
14q, Low Cycas sp. open shrubl<strong>and</strong>. Relict beach ridges.<br />
14r, Acacia crassicarpa + P<strong>and</strong>anus sp. + Melaleuca viridiflora +/- Parinari nonda +/- Banksia dentata +/- Lophostemon suaveolens<br />
shrubl<strong>and</strong>. Coastal outwash plains.<br />
14s, Low sparse Leucopogon ruscifolius + Acacia crassicarpa + Syzygium sub-orbiculare shrubl<strong>and</strong> with Corymbia<br />
novoguinensis emergents.<br />
14t, Low sparse shrubl<strong>and</strong> of Cochlospermum gillivraei, Canarium australianum, Eugenia reinwardtiana, Terminalia sp. with<br />
P<strong>and</strong>anus sp. Coastal dunes.<br />
14u, Low Corymbia stockerii subsp. stockerii + Welchiodendron longivalve open forest/ Welchidendron longivalve closed scrub/<br />
deciduous shrubl<strong>and</strong>/rock pavement complex (5v/4a/18a/18d – 30/40/20/10)<br />
14v, Eucalyptus leptophleba + Grevillea parallela + Exocarpos latifolius + Terminalia sp. + Acacia crassicarpa shrubl<strong>and</strong>. Aeolian dunes.<br />
14w, Eucalyptus cullenii + Corymbia stockeri subsp. peninsularis woodl<strong>and</strong> +/- Eucalyptus tetrodonta + Welchiodendron longivalve<br />
+ Melaleuca stenostachya shrubl<strong>and</strong> / Low Acacia brassii shrubl<strong>and</strong>/ Deciduous shrubl<strong>and</strong> complex (5l/14x/14j/18a – 20/40/30/10).<br />
14x, Eucalyptus tetrodonta + Welchiodendron longivalve + Melaleuca stenostachya open to sparse shrubl<strong>and</strong>. Acid volcanic pavements.<br />
14y, Low Premna serratifolia + Cordia subcordata +/-Pemphis acidula +/-Drypetes deplanchei shrubl<strong>and</strong>.<br />
Coastal headl<strong>and</strong> forest complexes<br />
15a, Semi deciduous vine thicket / P<strong>and</strong>anus sp. open forest complex. Basalt escarpment.<br />
Coastal dune complexes<br />
16a, Coastal foredune grassl<strong>and</strong>, herbl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong> complex. (17j/14y – 70/30).<br />
16b, Coastal foredune grassl<strong>and</strong>/ Casuarina equisetifolia +/- P<strong>and</strong>anus sp. +/- Acacia crassicarpa shrubl<strong>and</strong> complex.<br />
(17j/ 10b/6c – 30/20/50).<br />
16c, Coastal dune swale shrubl<strong>and</strong>/Low open forest complex + Cochlospermum gillivraei + Canarium australianum + Terminalia<br />
subacroptera + Acacia crassicarpa + Melaleuca saligna + Melaleuca acacioides. (14t/7b – 70/30)<br />
16d, Coastal dune shrubl<strong>and</strong> <strong>and</strong> vine forest complex (14t/2z – 70/30).<br />
16e, Corymbia tessellaris woodl<strong>and</strong> <strong>and</strong> open forest/ shrubl<strong>and</strong>/ vine thicket complex (5o/14t/2z– 40/40/20)<br />
16f, Casuarina equisetifolia woodl<strong>and</strong> <strong>and</strong> open forest/vine thicket complex (10b/2z – 60/40).<br />
16g, Low Acacia crassicarpa/ Melaleuca dealbata open forest dune swale complex (6c/7g - 80/20).<br />
16h, Low groved notophyll vine thicket + Terminalia muelleri + Diospyros maritima + Premna serratifolia + Thespesia populneoides<br />
+ Manilkara kauki (2y/17j – 80/20).<br />
16j, Low groved notophyll vine thicket/ grassl<strong>and</strong> <strong>and</strong> herbl<strong>and</strong> complex.(2z/17j - 80/20)<br />
16k, Coastal foredune grassl<strong>and</strong>, herbl<strong>and</strong>, woodl<strong>and</strong> <strong>and</strong> vine thicket complex. (17j/17d/10b/1c – 50/20/20/10).<br />
Grassl<strong>and</strong>s <strong>and</strong> grassl<strong>and</strong> complexes<br />
17a, Tall Ischeamum australe +/- Imperata cylindrica +/- Themeda tri<strong>and</strong>ra +/- Mnesithea rottboellioides +/- Heteropogon triticeus<br />
grassl<strong>and</strong>. Alluvial remnants of the Fly Platform.<br />
17b, Themeda sp. +/- Imperata cylindrica +/- Mnesithea rottboellioides grassl<strong>and</strong>. Basalt hillslopes<br />
17be, Themeda sp. +/- Imperata cylindrica +/- Mnesithea rottboellioides grassl<strong>and</strong> (Lantana degraded). Basalt hillslopes<br />
17bs, Themeda sp. +/- Imperata cylindrica +/- Mnesithea rottboellioides grassl<strong>and</strong> (severe erosion). Basalt hillslopes<br />
17c, Open to closed tussock grassl<strong>and</strong> with emergent shrubs. Coastal headl<strong>and</strong>s<br />
17d, Medium to tall Mnesithea rottboellioides + Heteropogon triticeus + Cymbopogon spp. +/- Imperata cylindrica +/- Themeda<br />
tri<strong>and</strong>ra grassl<strong>and</strong>. Alluvial <strong>and</strong> residual plains, coastal dunes <strong>and</strong> granite footslopes.<br />
17e, Relict cultivated alluvial plains with anastomosing channel morphology. Alluvial remnants of the Fly Platform.<br />
17f, Imperata cylindrica dominant grassl<strong>and</strong>. Coastal dunes.<br />
17g, Imperata/Themeda grassl<strong>and</strong> complex with emergent shrubs. Alluvial plains.<br />
17h, Imperata cylindrica + Themeda tri<strong>and</strong>ra grassl<strong>and</strong>/Welchiodendron longivalve open forest <strong>and</strong> woodl<strong>and</strong> complex.<br />
Fire degraded granite slopes.<br />
17i, Low sedgel<strong>and</strong> with emergent shrubs <strong>and</strong> trees. Residual s<strong>and</strong> plains <strong>and</strong> degraded dunes.<br />
17j, Low Spinifex sericeus+ Vigna marina+Ipomoea pes-caprae + Sesuvium portulacastrum grassl<strong>and</strong> <strong>and</strong> forbl<strong>and</strong> complex<br />
Rock pavement complexes<br />
18a, Deciduous shrubl<strong>and</strong>/Rock pavement complex. Rocky slopes on acid volcanic <strong>and</strong> plutonic rocks.<br />
18b, Low Acacia brassii +/- Welchiodendron longivalve +/- Cochlospermum gillivraei shrubl<strong>and</strong>/ rock pavement complex (18a/14j -50/50).<br />
18c, Welchiodendron longivalve +/- Acacia polystachya closed shrubl<strong>and</strong> / Low deciduous shrubl<strong>and</strong>/rock pavement complex<br />
(18a/14c – 50/50)<br />
18d, Corymbia stockerii subsp. peninsularis + Welchidendron longivalve + Psydrax banksi + Dodonoea sp. + Ficus platypoda<br />
rock pavement complex.<br />
Boulder slope vinel<strong>and</strong>/shrubl<strong>and</strong> complexes<br />
19a, Open vinel<strong>and</strong>/deciduous shrubl<strong>and</strong>/boulder slope complex. Granite talus <strong>and</strong> boulder slopes.<br />
Wetl<strong>and</strong> complexes <strong>and</strong> mosaics<br />
20a, Eleaocharis dulcis closed sedgel<strong>and</strong>.Seasonal swamps.<br />
20b, Open wetl<strong>and</strong> complex. Perennial swamps.<br />
Legend- <strong>Vegetation</strong> <strong>Communities</strong> <strong>and</strong> Broad<br />
<strong>Vegetation</strong> Groups of the Torres Strait Isl<strong>and</strong>s<br />
Torres Strait <strong>Regional</strong> Authority<br />
3D Environmental<br />
<strong>Vegetation</strong> Assessment<br />
& Mapping Specialists<br />
P. O. Box 959<br />
Kenmore, Qld 4069<br />
Phone: (07) 3411 9072; (07) 3878 4344<br />
Mobile: 0404 577 285; 0409 426 916<br />
www.3denvironmental.com.au<br />
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Legend<br />
Successional vine forest communities<br />
21a, Low vine forest <strong>and</strong> vine thicket with Barringtonia calyptrata + Macaranga involucrata + Hibiscus tiliaceus + Semecarpus<br />
australiensis successional vine forest <strong>and</strong> thicket. Basaltic cones.<br />
Anthropogenically altered (secondary) vine forest an<br />
22a, Tall palm (Cocos nucifera) woodl<strong>and</strong> <strong>and</strong> open forest with mesophyll/notophyll vine forest sub-canopy of Myristica insipida <strong>and</strong><br />
Lepidopetalum fructoglabrum. Basalt terraces<br />
22b, Semi deciduous vine thicket + Buchanania arborescens + Manilkara kauki + Scolopia braunii + Drypetes deplanchei +<br />
Terminalia muelleri. Relict gardens of coral cays.<br />
Saline transitional communities<br />
23a, Low Excoecaria agallocha + Hibiscus tiliaceus + Thespesia populneoides + Melaleuca cajuputi subsp. platyphylla open forest.<br />
Saline margins of alluvial plains.<br />
23b, Pemphis acidula +/- Terminalia subacroptera +/- Premna serratifolia closed shrubl<strong>and</strong>. Calcareous s<strong>and</strong>s.<br />
23c, Semi deciduous transitional vine forest + Xylocarpus granatum + Manilkara kauki. Calcareous beach ridges.<br />
Mangrove forest, woodl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong> complexes<br />
24a, Mangrove closed <strong>and</strong> open forest, woodl<strong>and</strong> <strong>and</strong> shrubl<strong>and</strong> complexes (24d/24c – 80/20).<br />
24b, Pemphis acidula + Osbornia octodonta closed shrubl<strong>and</strong>.<br />
24c, Avicennia marina subsp. eucalyptifolia open to closed forest. Saline alluvial soils.<br />
24d, Open to closed forest of Bruguiera gymnorhiza +/- Rhizophora stylosa. Intertidal coral platforms.<br />
Samphire herbl<strong>and</strong>s <strong>and</strong> shrubl<strong>and</strong>s <strong>and</strong> salt pans.<br />
25a, Dwarf halophytic shrubl<strong>and</strong> <strong>and</strong> saltpan. Hypersaline muds.<br />
25b, Salt pan. Hypersaline muds.<br />
Samphire grassl<strong>and</strong>s<br />
26a, Closed Sporobulus sp. grassl<strong>and</strong>.<br />
26b, Sporobulus sp. grassl<strong>and</strong>/Chenopod forbl<strong>and</strong> <strong>and</strong> herbl<strong>and</strong> complex<br />
Estuarine wetl<strong>and</strong> complexes <strong>and</strong> mosaics<br />
27a, Schoenoplectus sp. sedgel<strong>and</strong>.<br />
27b, Tall Schoenoplectus sp. sedgel<strong>and</strong>/ wetl<strong>and</strong> complex<br />
Tidal Lagoon<br />
Tidal Lagoon<br />
Rock<br />
R, Rock<br />
Artificial wetl<strong>and</strong><br />
Artificial wetl<strong>and</strong><br />
Exotic species<br />
Ex, <strong>Communities</strong> dominated by exotic species<br />
Bamboo, Bamboo thicket<br />
Reclaimed l<strong>and</strong><br />
RL, Reclaimed l<strong>and</strong><br />
Regrowth<br />
Re, Regrowth<br />
Cleared<br />
Cl, Cleared<br />
Legend- <strong>Vegetation</strong> <strong>Communities</strong> <strong>and</strong> Broad<br />
<strong>Vegetation</strong> Groups of the Torres Strait Isl<strong>and</strong>s<br />
Client<br />
Scale<br />
Torres Strait <strong>Regional</strong> Authority<br />
3D Environmental<br />
<strong>Vegetation</strong> Assessment<br />
& Mapping Specialists<br />
P. O. Box 959<br />
Kenmore, Qld 4069<br />
Phone: (07) 3411 9072; (07) 3878 4344<br />
Mobile: 0404 577 285; 0409 426 916<br />
www.3denvironmental.com.au<br />
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<strong>Appendix</strong> A2. Map Legend – L<strong>and</strong> Zones<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
202
Legend - L<strong>and</strong> Zones of the Torres Strait Isl<strong>and</strong>s<br />
L<strong>and</strong> Zone<br />
L<strong>and</strong> Zone 1<br />
E. Estuarine muds including saline <strong>and</strong> brackish alluvium.<br />
L<strong>and</strong> Zone 2<br />
D. Coastal dunes, cheniers, calcareous beach s<strong>and</strong>s (including atolls), beach ridges <strong>and</strong> associated swales.<br />
L<strong>and</strong> Zone 3<br />
A. Alluvial plains, alluvial fans, terraces <strong>and</strong> fluvial sediments.<br />
L<strong>and</strong> Zone 5<br />
AS. Residual s<strong>and</strong>y plains <strong>and</strong> s<strong>and</strong>y terraces<br />
L. Exposed duricrust<br />
T. Remnant colluvial surfaces.<br />
L<strong>and</strong> Zone 8<br />
B. Basalt escarpments <strong>and</strong> terraces<br />
V. Volcanic cones formed on ash <strong>and</strong> scoria<br />
L<strong>and</strong> Zone 12<br />
G. Granite hillslopes <strong>and</strong> footslopes including boulder talus <strong>and</strong> colluvium.<br />
GD. Diorite hills <strong>and</strong> knolls<br />
MG. Metamorphosed granitoid rocks including hornfels<br />
R. Acid volcanic hillslopes <strong>and</strong> footslopes including rhyolites <strong>and</strong> dacites.<br />
Client<br />
Scale<br />
Legend- L<strong>and</strong> Zones of the<br />
Torres Strait Isl<strong>and</strong>s<br />
Torres Strait <strong>Regional</strong> Authority<br />
3D Environmental<br />
<strong>Vegetation</strong> Assessment<br />
& Mapping Specialists<br />
P. O. Box 959<br />
Kenmore, Qld 4069<br />
Phone: (07) 3411 9072; (07) 3878 4344<br />
Mobile: 0404 577 285; 0409 426 916<br />
www.3denvironmental.com.au<br />
File Path C:\3D Environmental\<br />
Drawn By DG Checked DS Torres\3d_TS_Maps_legend.mxd Date<br />
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A3
<strong>Appendix</strong> B. Torres Strait Isl<strong>and</strong>s Flora Species List 11<br />
Family_Name Botanical_Name BRI C’veg 3DE<br />
Pteridiophytes<br />
Adiantaceae Adiantum atroviride Bostock X<br />
Adiantum philippense L. X X<br />
Cheilanthes caudata R.Br. X<br />
Cheilanthes contigua Baker X<br />
Cheilanthes nitida (R.Br.) P.S.Green X X<br />
Cheilanthes nudiuscula (R.Br.) T.Moore X X<br />
Cheilanthes prenticei Luerss. X<br />
Cheilanthes pumilio (R.Br.) F.Muell. X<br />
Cheilanthes tenuifolia (Burm.f.) Sw. X X<br />
Doryopteris concolor (Langsd. & Fisch.) Kuhn X X<br />
Aspleniaceae Asplenium nidus L. X X<br />
Blechnaceae Blechnum indicum X<br />
Stenochlaena palustris (Burm.f.) Bedd. X X<br />
Davalliaceae Davallia denticulata (Burm.f.) Mett. var. denticulata X X<br />
Humata pectinata (Sm.) Desv. X<br />
Gleicheniaceae Dicranopteris linearis (Burm.f.) Underw. var. linearis X<br />
Lindsaeaceae Lindsaea brachypoda (Baker) Salomon X<br />
Lindsaea ensifolia Sw. subsp. ensifolia X X<br />
Lindsaea media R.Br. X X<br />
Nephrolepidaceae Nephrolepis obliterata (R.Br.) J.Sm. X X<br />
Ophioglossaceae Helminthostachys zeylanica (L.) Kaulf. X X<br />
Ophioglossum sp. X<br />
Parkeriaceae Ceratopteris thalictroides (L.) Brongn. X X<br />
Polypodiaceae Drynaria quercifolia (L.) J.Sm. X X<br />
Drynaria sparsisora (Desv.) T.Moore X X<br />
Lecanopteris sinuosa (Wall. ex Hook.) Copel. X<br />
Microsorum grossum (Langsd. & Fisch.) S.B.Andrews X<br />
Microsorum punctatum (L.) Copel. X X<br />
Pyrrosia lanceolata (L.) Farw. X X<br />
Pyrrosia longifolia (Burm.f.) C.V.Morton X X<br />
Pteridaceae Acrostichum speciosum Willd. X X<br />
Schizaeaceae Lygodium flexuosum (L.) Sw. X X<br />
Lygodium microphyllum (Cav.) R.Br. X X<br />
Schizaea dichotoma (L.) Sm. X X<br />
Selaginellaceae Selaginella ciliaris (Retz.) Spring X<br />
Selaginella longiciliata Hieron. X<br />
Thelypteridaceae Cyclosorus interruptus (Willd.) H.Ito X X<br />
Vittariaceae Vittaria elongata Sw. X<br />
Vittaria ensiformis Sw. X X<br />
11 Preliminary pending identification of all survey records; Nomenclature follows Bostock <strong>and</strong> Holl<strong>and</strong> (2007); *<br />
denotes naturalized species; BRI denotes Qld Herbarium Aug 2007 Herbrecs extract; Cveg denotes EPA Corveg<br />
records; 3DE denotes 3d Environmental 2007/2008 survey records.<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Gymnosperms<br />
Podocarpaceae Podocarpus grayae de Laub. X X<br />
Angiosperms<br />
Acanthaceae Acanthus ilicifolius L. X X<br />
Asystasia australasica F.M.Bailey X X<br />
Asystasia gangetica (L.) T.Anderson subsp. gangetica* X<br />
Barleria cristata L.* X<br />
Barleria prionitis L.* X<br />
Brunonialis acaulis X<br />
Brunoniella australis (Cav.) Bremek. X X<br />
Dicliptera ciliata Decne. X<br />
Dicliptera glabra Decne. X<br />
Dipteracanthus bracteatus (R.Br.) Nees X X<br />
Dipteracanthus prostratus (Poir.) Nees* X<br />
Graptophyllum pictum (L.) Griff. X<br />
Hygrophila angustifolia R.Br. X<br />
Hypoestes floribunda R.Br. X X<br />
Nelsonia campestris R.Br. X<br />
Pseuderanthemum variabile (R.Br.) Radlk. X X<br />
Ruellia tuberosa L.* X<br />
Ruellia tweediana Griseb.* X<br />
Staurogyne leptocaulis subsp. decumbens R.M.Barker X<br />
Thunbergia arnhemica F.Muell. X<br />
Agavaceae Agave sisalana Perrine* X X<br />
Agave vivipara L. var. vivipara* X<br />
Cordyline cannifolia X<br />
Aizoaceae Sesuvium portulacastrum (L.) L. X X<br />
Trianthema portulacastrum L.* X X<br />
Amaranthaceae Achyranthes aspera L. X X<br />
Alternanthera angustifolia R.Br. X<br />
Alternanthera brasiliana (L.) Kuntze cv. Rubiginosa* X<br />
Alternanthera brasiliana (L.) Kuntze* X<br />
Alternanthera denticulata R.Br. X<br />
Alternanthera ficoidea (L.) P.Beauv.* X X<br />
Alternanthera micrantha (Benth.) Domin X<br />
Alternanthera nana R.Br. X X<br />
Alternanthera pungens Kunth* X X<br />
Alternanthera sessilis (L.) R.Br. ex DC.* X<br />
Alternanthera sp. X<br />
Amaranthus blitum L.* X<br />
Amaranthus hybridus L.* X<br />
Amaranthus interruptus R.Br. X<br />
Amaranthus sp. X<br />
Amaranthus undulatus R.Br. X<br />
Amaranthus viridis L.* X<br />
Celosia argentea L.* X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Cyathula prostrata (L.) Blume X<br />
Deeringia amaranthoides (Lam.) Merr. X X<br />
Gomphrena breviflora F.Muell. X<br />
Gomphrena celosioides Mart.* X X<br />
Gomphrena conferta Benth. X<br />
Gomphrena flaccida R.Br. X<br />
Ptilotus distans subsp. capensis Benl X<br />
Amaryllidaceae Crinum angustifolium R.Br. X X<br />
Crinum uniflorum F.Muell. X X<br />
Proiphys amboinensis (L.) Herb. X X<br />
Anacardiaceae Anacardium occidentale L.* X X<br />
Buchanania arborescens (Blume) Blume X X X<br />
Mangifera indica L.* X X<br />
Semecarpus australiensis Engl. X X<br />
Annonaceae Annona glabra L.* (Class 2) X<br />
Annonaceae sp. 12 X<br />
Meiogyne sp. (Moa Isl<strong>and</strong> DGFell 9718 + DJ Stanton) X X<br />
Desmos wardianus (F.M.Bailey) Jessup X X<br />
Haplostichanthus fruticosus Jessup X X<br />
Meiogyne cylindrocarpa subsp. trichocarpa Jessup X X<br />
Melodorum leichhardtii X<br />
Melodorum scabridulum Jessup X<br />
Miliusa brahei X<br />
Miliusa horsefieldii X<br />
Miliusa traceyi Jessup X X<br />
Polyalthia australis X<br />
Uvaria concava Teijsm. & Binn. X<br />
Uvaria rufa Blume X X<br />
Apiaceae Centella asiatica (L.) Urb. X X<br />
Apocynaceae Alstonia actinophylla (A.Cunn.) K.Schum. X X X<br />
Alstonia spectabilis R.Br. subsp. spectabilis X X<br />
Alyxia spicata R.Br. X X X<br />
Brachystelma glabriflorum (F.Muell.) Schltr. X<br />
Calotropis gigantea (L.) W.T.Aiton* X<br />
Carissa laxiflora Benth. X X<br />
Carissa ovata X X<br />
Catharanthus roseus (L.) G.Don* X X<br />
Cerbera manghas L. X X<br />
Cynanchum brachystelmoides P.I.Forst. X<br />
Cynanchum carnosum (R.Br.) Schltr. X X<br />
Cynanchum leptolepis (Benth.) Domin X<br />
Dischidia littoralis Schltr. (Vulnerable) X X<br />
Dischidia major (Vahl) Merr. X X<br />
Dischidia nummularia R.Br. X X X<br />
12 M.Lawrie 122, Mer. Noted as an edible fruit tree. Possibly naturalized.<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Dischidia ovata Benth. X X X<br />
Hoya australis R.Br. ex Traill subsp. australis X X<br />
Hoya australis subsp. sanae (F.M.Bailey) K.D.Hill X X<br />
Hoya revoluta Wight ex Hook.f. (Rare) X X<br />
Ichnocarpus frutescens (L.) W.T.Aiton X<br />
Marsdenia connivens P.I.Forst. X<br />
Marsdenia tricholepis (Schltr.) P.I.Forst. X<br />
Marsdenia velutina R.Br. X<br />
Marsdenia viridiflora subsp. tropica P.I.Forst. X<br />
Parsonsia velutina R.Br. X X<br />
Sarcostemma viminale subsp. brunonianum (Wight & X X X<br />
Arn.) P.I.Forst.<br />
Secamone auriculata Blume (Rare) X X<br />
Secamone elliptica R.Br. X X<br />
Secamone lineata Blume X<br />
Tabernaemontana orientalis R.Br. X X<br />
Tabernaemontana p<strong>and</strong>acaqui Lam. X X X<br />
Tylophora benthamii Tsiang X X<br />
Tylophora erecta F.Muell. ex Benth. X<br />
Voacanga gr<strong>and</strong>ifolia (Miq.) Rolfe X X<br />
Wrightia pubescens subsp. penicillata (F.M.Bailey) X X<br />
Ngan<br />
Wrightia saligna (R.Br.) F.Muell. ex Benth. X X<br />
Wrightia versicolor S.T.Blake X X<br />
Aquifoliaceae Ilex arnhemensis subsp. ferdin<strong>and</strong>i (Harms) Pedley X X<br />
Araceae Alocasia macrorrhizos (L.) G.Don X<br />
Amorphophallus paeoniifolius (Dennst.) Nicolson X X<br />
Epipremnum pinnatum (L.) Engl. X X<br />
Epipremnum amplissimum X<br />
Typhonium brownii Schott X<br />
Typhonium flagelliforme (Lodd.) Blume X<br />
Typhonium weipanum A.Hay X<br />
Araliaceae Polyscias australiana (F.Muell.) Philipson X X<br />
Polyscias elegans (C.Moore & F.Muell.) Harms X X<br />
Polyscias macgillivrayi (Seem.) Harms X X<br />
Polyscias scutellaria (Burm.f.) Fosberg X<br />
Schefflera actinophylla (Endl.) Harms X X<br />
Trachymene tenuifolia (Domin) B.L.Burtt X X<br />
Arecaceae Arenga australasica (H.Wendl. & Drude) S.T.Blake X X<br />
(Vulnerable)<br />
Cocos nucifera* X<br />
Corypha utan X<br />
Hydriastele costata F.M.Bailey (Vulnerable) X<br />
Hydriastele wendl<strong>and</strong>iana X<br />
Licuala ramsayi X<br />
Livistona benthamii X<br />
Livistona muelleri F.M.Bailey X X X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Metroxylon sagu X<br />
Normanbya sp. (DGFell 9751 + DJStanton) X<br />
Nypa fruticans X<br />
Ptychosperma elegans (R.Br.) Blume X X<br />
Ptychosperma macarthurii X<br />
Aristolochiaceae Aristolochia acuminata Lam. X X<br />
Aristolochia chalmersii (Endangered) X<br />
Pararistolochia sp. X<br />
Paristolochia sp. (DGF9651+DJS) 13 X<br />
Asteraceae Acanthospermum hispidum DC.* X X<br />
Acmella gr<strong>and</strong>iflora var. brachyglossa (Benth.) X<br />
13 Requires confirmation<br />
R.K.Jansen<br />
Ageratum conyzoides L. subsp. conyzoides* X X<br />
Allopterigeron filifolius (F.Muell.) Dunlop X X<br />
Bidens bipinnata L.* X X<br />
Bidens pilosa L.* X X<br />
Bidens sp. X<br />
Blainvillea dubia Specht X<br />
Blumea diffusa R.Br. ex Benth. X<br />
Blumea lacera (Burm.f.) DC. X<br />
Blumea saxatilis Zoll. & Moritzi X X X<br />
Cosmos caudatus Kunth* X<br />
Cyanthillium cinereum (L.) H.Rob. X X X<br />
Eclipta prostrata (L.) L. X X<br />
Eleutheranthera ruderalis (Sw.) Sch.Bip.* X<br />
Emilia sonchifolia (L.) DC. var. sonchifolia* X X<br />
Epaltes australis Less. X X<br />
Glossocardia bidens (Retz.) Veldkamp X X<br />
Peripleura diffusa (N.T.Burb.) G.L.Nesom X X<br />
Phacellothrix cladochaeta (F.Muell.) F.Muell. X X<br />
Pluchea indica (L.) Less. X X<br />
Praxelis clematidea R.M.King & H.Rob.* X X<br />
Pseudelephantopus spicatus (B.Juss. ex Aubl.) X<br />
C.F.Baker*<br />
Pterocaulon redolens (Willd.) Fern.-Vill. X X<br />
Pterocaulon sphacelatum (Labill.) F.Muell. X X<br />
Sphaeranthus africanus L. X<br />
Sphagneticola trilobata (L.) Pruski* (Class 3) X X<br />
Synedrella nodiflora (L.) Gaertn.* X X<br />
Tithonia diversifolia (Hemsl.) A.Gray* X<br />
Tridax procumbens L.* X X<br />
Vernonia junghuhniana J.Kost.* X<br />
Wedelia biflora X<br />
Wedelia longipes Klatt X<br />
Wedelia spilanthoides F.Muell. X X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Wollastonia biflora (L.) DC. X X<br />
Xanthium occidentale Bertol.* X<br />
Zinnia violacea Cav.* X<br />
Avicenniaceae Avicennia marina (Forssk.) Vierh. X X<br />
Avicennia marina subsp. australasica (Walp.) J.Everett X X<br />
Avicennia marina subsp. eucalyptifolia (Valeton) X X X<br />
J.Everett<br />
Bataceae Batis argillicola P.Royen X<br />
Bignoniaceae Deplanchea tetraphylla (R.Br.) F.Muell. X X<br />
Dolich<strong>and</strong>rone alternifolia (R.Br.) Seem. X<br />
Dolich<strong>and</strong>rone heterophylla X<br />
P<strong>and</strong>orea p<strong>and</strong>orana (Andrews) Steenis X X<br />
Tecoma stans (L.) Juss. ex Kunth var. stans* X X<br />
Bombacaceae Bombax ceiba var. leiocarpum A.Robyns X X X<br />
Camptostemon schultzii Mast. X X<br />
Boraginaceae Argusia argentea (L.f.) Heine X X<br />
Carmona retusa (Vulnerable) X<br />
Cordia dichotoma G.Forst. X X<br />
Cordia myxa X<br />
Cordia subcordata Lam. X X<br />
Heliotropium vagum Craven X<br />
Brassicaceae Rorippa eustylis (F.Muell.) L.A.S.Johnson X X<br />
Brownlowiaceae Berrya javanica X<br />
Indigator fordii X<br />
Burmanniaceae Burmannia juncea Sol. ex R.Br. X<br />
Burseraceae Canarium australianum F.Muell. var. australianum X X X<br />
Garuga floribunda Decne. var. floribunda X X<br />
Canarium vitiense X<br />
Byblidaceae Byblis liniflora Salisb. X<br />
Byttneriaceae Abroma molle DC. X<br />
Commersonia bartramia 14 X<br />
Melochia corchorifolia L. X<br />
Waltheria indica L. X X<br />
Cactaceae Opuntia stricta (Haw.) Haw.* (Class 2) X<br />
Caesalpiniaceae Bauhinia mon<strong>and</strong>ra Kurz* X<br />
Caesalpinia bonduc (L.) Roxb. X X<br />
Cassia fistula L.* X X<br />
Chamaecrista absus (L.) H.S.Irwin & Barneby var. X<br />
absus<br />
Chamaecrista mimosoides (L.) Greene X<br />
Chamaecrista nomame (Siebold) H.Ohashi var. nomame X<br />
Chamaecrista rotundifolia (Pers.) Greene var. X<br />
rotundifolia*<br />
Delonix regia (Bojer ex Hook.) Raf.* X X<br />
Erythrophleum chlorostachys (F.Muell.) Baill. X X X<br />
14 Requires confirmation against Moa Is. Collection, Commersonia sp. (DGF8919a+)<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Intsia bijuga (Colebr.) Kuntze X X<br />
Lysiphyllum binatum (Blanco) de Wit X X<br />
Maniltoa lenticellata C.T.White var. lenticellata X X<br />
Peltophorum pterocarpum X<br />
Senna alata (L.) Roxb.* X X<br />
Senna gaudichaudii (Hook. & Arn.) H.S.Irwin & X<br />
Barneby<br />
Senna obtusifolia (L.) H.S.Irwin & Barneby* (Class 2) X<br />
Senna occidentalis (L.) Link* X X<br />
Senna surattensis (Burm.f.) H.S.Irwin & Barneby X<br />
Senna tora (L.) Roxb.* (Class 2) X<br />
Campanulaceae Isotoma gulliveri F.Muell. X<br />
Lobelia dioica R.Br. X<br />
Lobelia douglasiana F.M.Bailey (Rare) X<br />
Lobelia stenophylla Benth. X<br />
Wahlenbergia caryophylloides P.J.Sm. X X<br />
Wahlenbergia gracilis (G.Forst.) A.DC. X X<br />
Cannaceae Canna indica L.* X X<br />
Capparaceae Capparis canescens Banks ex DC. X X X<br />
Capparis lucida (DC.) R.Br. ex Benth. X X<br />
Capparis quiniflora DC. X X<br />
Capparis sepiaria L. X X<br />
Capparis sp. X<br />
Caricaceae Carica papaya* X<br />
Caryophyllaceae Polycarpaea corymbosa var. torrensis Pedley X<br />
Casuarinaceae Allocasuarina littoralis (Salisb.) L.A.S.Johnson X X<br />
Casuarina equisetifolia L. subsp. equisetifolia X<br />
Casuarina equisetifolia subsp. incana (Benth.) X X<br />
L.A.S.Johnson<br />
Celastraceae Elaeodendron melanocarpum F.Muell. X X<br />
Gymnosporia inermis Merr. & L.M.Perry X X<br />
Pleurostylia opposita (Wall.) Alston X X<br />
Salacia chinensis L. X X<br />
Salacia disepala (C.T.White) Ding Hou X X<br />
Siphonodon pendulus F.M.Bailey X X X<br />
Ceratophyllaceae Ceratophyllum demersum L. X<br />
Chenopodiaceae Salsola kali L. X X<br />
Tecticornia australasica (Moq.) Paul G.Wilson X X<br />
Chrysobalanaceae Maranthes corymbosa Blume X X<br />
Parinari nonda F.Muell. ex Benth. X X X<br />
Cleomaceae Cleome aculeata L.* X<br />
Cleome gyn<strong>and</strong>ra L.* X<br />
Cleome tetr<strong>and</strong>ra var. pentata Hewson X<br />
Cleome viscosa L. X X<br />
Clusiaceae Calophyllum australianum F.Muell. ex Vesque X X<br />
Calophyllum inophyllum L. X X<br />
Calophyllum sil Lauterb. X X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Garcinia sp. (DGF9722+DJS) 15 X<br />
Garcinia sp. (Claudie River L.J.Brass 19658) X X<br />
Garcinia warrenii F.Muell. X X<br />
Colchicaceae Schelhammera multiflora X<br />
Cocholospermaceae Cochlospermum gillivraei Benth. X X X<br />
Colchicaceae Gloriosa superba L.* X X<br />
Combretaceae Lumnitzera sp. X X<br />
Lumnitzera littorea (Jack) F.Voigt X X<br />
Lumnitzera racemosa Willd. X X X<br />
Quisqualis indica L.* X<br />
Terminalia arenicola Byrnes X X<br />
Terminalia catappa L. X X<br />
Terminalia complanata X<br />
Terminalia muelleri Benth. X X X<br />
Terminalia sericocarpa F.Muell. X X<br />
Terminalia subacroptera Domin X X<br />
Commelinaceae Aneilema siliculosum R.Br. X<br />
Cartonema baileyi F.M.Bailey X<br />
Cartonema parviflorum Hassk. X<br />
Cartonema spicatum R.Br. X<br />
Cartonema spicatum var. humile Hassk. X<br />
Commelina benghalensis L.* X X<br />
Commelina diffusa Burm.f. X X<br />
Commelina ensifolia R.Br. X X<br />
Commelina sp. X<br />
Cyanotis axillaris (L.) D.Don X<br />
Murdannia gigantea (Vahl) G.Brueckn. X<br />
Murdannia graminea (R.Br.) G.Brueckn. X X<br />
Murdannia vaginata (L.) G.Brueckn.* X<br />
Tradescantia spathacea Sw.* X<br />
Convolvulaceae Erycibe coccinea (F.M.Bailey) Hoogl<strong>and</strong> X X<br />
Evolvulus alsinoides (L.) L. X X X<br />
Evolvulus alsinoides var. decumbens (R.Br.) Ooststr. X X<br />
Ipomoea abrupta R.Br. X<br />
Ipomoea aquatica Forssk. X<br />
Ipomoea carnea subsp. fistulosa (Mart. ex Choisy) X<br />
15 Requires determination<br />
D.F.Austin*<br />
Ipomoea eriocarpa R.Br. X<br />
Ipomoea graminea R.Br. X<br />
Ipomoea hederifolia L.* X<br />
Ipomoea macrantha Roem. & Schult. X X<br />
Ipomoea mauritiana Jacq. X X<br />
Ipomoea nil (L.) Roth* X<br />
Ipomoea pes-caprae subsp. brasiliensis (L.) Ooststr. X X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Ipomoea plebeia R.Br. X X<br />
Ipomoea polymorpha Roem. & Schult. X<br />
Ipomoea quamoclit L.* X<br />
Ipomoea tiliacea (Willd.) Choisy X<br />
Ipomoea triloba L.* X<br />
Jacquemontia paniculata (Burm.f.) Hallier f. var. X X<br />
paniculata<br />
Merremia dissecta (Jacq.) Hallier f.* X<br />
Merremia hirta (L.) Merr. X<br />
Merremia quinata (R.Br.) Ooststr. X X<br />
Merremia umbellata (L.) Hallier f. X<br />
Merremia umbellata (L.) Hallier f. subsp. umbellata X<br />
Operculina brownii Ooststr. (Rare) X<br />
Operculina riedeliana (Oliv.) Ooststr. X<br />
Operculina turpethum (L.) Silva Manso X<br />
Polymeria sp. (Aurukun J.R.Clarkson 4320) X<br />
Polymeria subhirsuta Domin X<br />
Xenostegia tridentata (L.) D.F.Austin & Staples X X X<br />
Costaceae Costus potierae F.Muell. (Endangered) X<br />
Cucurbitaceae Citrullus lanatus (Thunb.) Matsum. & Nakai var. X X<br />
lanatus*<br />
Cucumis sp. X<br />
Cucumis melo L. X X<br />
Diplocyclos palmatus (L.) C.Jeffrey X X<br />
Lagenaria siceraria (Molina) St<strong>and</strong>l.* X<br />
Luffa aegyptiaca Mill. X<br />
Muellerargia timorensis Cogn. (Endangered) X<br />
Mukia maderaspatana (L.) M.Roem. X X<br />
Neoalsomitra capricornica (F.Muell.) Hutch. X X<br />
Zehneria mucronata (Blume) Miq. X<br />
Cycadaceae Cycas badensis K.D.Hill X X<br />
Cycas scratchleyana F.Muell. X X<br />
Cymodoceaceae Halodule uninervis (Forssk.) Asch. X<br />
Thalassodendron ciliatum (Forssk.) Hartog X<br />
Cyperaceae Abildgaardia ovata (Burm.f.) Kral X<br />
Bulbostylis barbata (Rottb.) C.B.Clarke X X<br />
Cyperus angustatus R.Br. X<br />
Cyperus aquatilis R.Br. X X<br />
Cyperus castaneus Willd. X<br />
Cyperus compressus L.* X<br />
Cyperus cuspidatus Kunth X<br />
Cyperus decompositus (R.Br.) F.Muell. X X<br />
Cyperus dietrichiae Boeck. var. dietrichiae X<br />
Cyperus haspan L. subsp. haspan X X<br />
Cyperus iria L. X X<br />
Cyperus javanicus Houtt. X X<br />
Cyperus metzii (Hochst. ex Steud.) Mattf. & Kuek.* X<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Cyperus pedunculatus (R.Br.) J.Kern X<br />
Cyperus polystachyos Rottb. var. polystachyos X X<br />
Cyperus pumilus L. X<br />
Cyperus rotundus L.* X<br />
Cyperus scaber (R.Br.) Boeck. X<br />
Cyperus scariosus R.Br. X<br />
Cyperus sp. (Cape York J.R.Clarkson+ 8126) X<br />
Cyperus sp. (Mission Beach N.Byrnes MB14) X<br />
Cyperus sphacelatus Rottb.* X<br />
Cyperus squarrosus L. X<br />
Cyperus stoloniferus Retz. X<br />
Cyperus tetracarpus Boeck. X<br />
Cyperus zollingeri Steud. X<br />
Eleocharis dulcis (Burm.f.) Trin. ex Hensch. X X<br />
Eleocharis geniculata (L.) Roem. & Schult. X<br />
Eleocharis spiralis (Rottb.) Roem. & Schult. X X<br />
Fimbristylis acicularis R.Br. X X<br />
Fimbristylis aestivalis (Retz.) Vahl var. aestivalis X<br />
Fimbristylis bisumbellata (Forssk.) Bubani X<br />
Fimbristylis cinnamometorum (Vahl) Kunth X<br />
Fimbristylis cymosa R.Br. X<br />
Fimbristylis dichotoma (L.) Vahl X X<br />
Fimbristylis ferruginea (L.) Vahl X X<br />
Fimbristylis furva R.Br. X<br />
Fimbristylis insignis Thwaites X<br />
Fimbristylis lanceolata C.B.Clarke X<br />
Fimbristylis littoralis Gaudich. X<br />
Fimbristylis modesta S.T.Blake X<br />
Fimbristylis polytrichoides (Retz.) R.Br. X<br />
Fimbristylis rara R.Br. X<br />
Fimbristylis recta F.M.Bailey X X<br />
Fimbristylis signata S.T.Blake X<br />
Fimbristylis simplex S.T.Blake X<br />
Fimbristylis tristachya R.Br. X<br />
Fuirena ciliaris (L.) Roxb. X X<br />
Gahnia aspera (R.Br.) Spreng. X X<br />
Hypolytrum compactum Nees & Meyen X X<br />
Lipocarpha microcephala (R.Br.) Kunth X<br />
Rhynchospora exserta C.B.Clarke X<br />
Rhynchospora heterochaeta S.T.Blake X X<br />
Rhynchospora leae C.B.Clarke X<br />
Rhynchospora longisetis R.Br. X<br />
Rhynchospora pterochaeta F.Muell. X<br />
Schoenoplectus litoralis (Schrad.) Palla X X<br />
Schoenoplectus validus (Vahl) A.Love & D.Love X X<br />
Schoenus calostachyus (R.Br.) Roem. & Schult. X X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Schoenus falcatus R.Br. X<br />
Schoenus punctatus R.Br. X<br />
Schoenus sparteus R.Br. X X X<br />
Scleria brownii Kunth X X<br />
Scleria laxa R.Br. X X<br />
Scleria levis Retz. X<br />
Scleria lithosperma var. linearis Benth. X<br />
Scleria mackaviensis Boeck. X X<br />
Scleria pergracilis (Nees) Kunth X<br />
Scleria polycarpa Boeck. X X<br />
Scleria pygmaea R.Br. X<br />
Scleria rugosa R.Br. X<br />
Scleria sumatrensis (DGFell 9702+DJStanton) 16 X<br />
Scleria tricuspidata S.T.Blake X<br />
Tricostularia undulata (Thwaites) J.Kern X<br />
Datiscaceae Tetrameles nudiflora X<br />
Dilleniaceae Dillenia alata (R.Br. ex DC.) Martelli X X<br />
Tetracera daemeliana F.Muell. X X<br />
Dioscoreaceae Dioscorea bulbifera L. var. bulbifera X X<br />
Dioscorea esculenta (Lour.) Burkill* X<br />
Dioscorea pentaphylla var. papuana Burkill X X<br />
Dioscorea transversa R.Br. X X X<br />
Dracaenaceae Pleomele angustifolia (Medik.) N.E.Br. X X X<br />
Sansevieria trifasciata Prain* X<br />
Droseraceae Drosera burmanni Vahl X X<br />
Drosera indica L. X X<br />
Drosera lanata K.Kondo X<br />
Drosera spatulata X<br />
Ebenaceae Diospyros calycantha O.Schwarz X X<br />
Diospyros compacta (R.Br.) Kosterm. X X X<br />
Diospyros hebecarpa A.Cunn. ex Benth. X X<br />
Diospyros humils X<br />
Diospyros littoralis X<br />
Diospyros maritima Blume X X<br />
Diospyros sp. X X<br />
Diospyros sp. (Kur<strong>and</strong>a L.J.Webb+ 7265A) X<br />
Diospyros sp. (Mt White P.I.Forster PIF14415) X X<br />
Elaeocarpaceae Elaeocarpus arnhemicus F.Muell. X X<br />
Elatinaceae Bergia ammannioides Roxb. X<br />
Ericaceae Leucopogon ruscifolius R.Br. X X<br />
Leucopogon yorkensis Pedley X X X<br />
Eriocaulaceae Eriocaulon clarksonii G.J.Leach X<br />
Eriocaulon depressum R.Br. ex Sm. X X<br />
Eriocaulon fistulosum R.Br. ex Sm. X<br />
16 Requires confirmation<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
214
Family_Name Botanical_Name BRI C’veg 3DE<br />
Eriocaulon nanum R.Br. X<br />
Erythroxylaceae Erythroxylum sp. (Mosquito Creek J.R.Clarkson 9991+) X<br />
Euphorbiaceae Acalypha lanceolata Willd. X X<br />
Acalypha wilkesiana Muell.Arg.* X X<br />
Chamaesyce atoto (G.Forst.) Croizat X X<br />
Chamaesyce hirta (L.) Millsp.* X X<br />
Chamaesyce macgillivrayi (Boiss.) D.C.Hassall X<br />
Chamaesyce micradenia (Boiss.) D.C.Hassall X<br />
Chamaesyce mitchelliana (Boiss.) D.C.Hassall X X<br />
Chamaesyce prostrata (Aiton) Small* X<br />
Chamaesyce vachellii (Hook. & Arn.) Hara X X<br />
Claoxylon hillii Benth. X X<br />
Codiaeum variegatum (L.) A.Juss. var. variegatum* X X<br />
Codiaeum variegatum var. moluccanum (Decne.) X X<br />
Muell.Arg.<br />
Croton arnhemicus Muell.Arg. X X X<br />
Croton multicaulis P.I.Forst. subsp. multicaulis X<br />
Croton waterhouseae P.I.Forst. X<br />
Dimorphocalyx australiensis C.T.White X X<br />
Euphorbia cyathophora Murr* X X<br />
Euphorbia heterophylla L.* X X<br />
Euphorbia plumerioides Teijsm. & Binn. X<br />
Euphorbia tannensis Spreng. subsp. tannensis X X<br />
Euphorbiaceae sp. X<br />
Excoecaria agallocha L. X X X<br />
Jatropha gossypiifolia L.* (Class 2) X<br />
Macaranga involucrata var. mallotoides (F.Muell.) X X<br />
L.M.Perry<br />
Macaranga tanarius (L.) Muell.Arg. X X<br />
Mallotus dispersus P.I.Forst. X<br />
Mallotus ficifolius (Baill.) Pax & K.Hoffm. X X<br />
Mallotus mollissimus (Geiseler) Airy Shaw X<br />
Mallotus nesophilus X<br />
Mallotus philippensis (Lam.) Muell.Arg. X X X<br />
Mallotus polyadenos F.Muell. X<br />
Mallotus rep<strong>and</strong>us (Willd.) Muell.Arg. X<br />
Mallotus resinosus (Blanco) Merr. X<br />
Manihot esculenta Crantz* X X<br />
Microstachys chamaelea (L.) A.Juss. ex Hook.f. X<br />
Pimeleodendron amboinicum (Rare) X<br />
Ricinus communis L.* X<br />
Tragia finalis P.I.Forst. X X<br />
Fabaceae Abrus precatorius L. subsp. precatorius X X X<br />
Aeschynomene americana L. var. americana* X<br />
Aeschynomene indica L. X<br />
Alysicarpus ovalifolius (Schumach.) J.Leonard* X<br />
Alysicarpus schomburgkii Schindl. X<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
215
Family_Name Botanical_Name BRI C’veg 3DE<br />
Alysicarpus vaginalis (L.) DC.* X<br />
Aphyllodium schindleri Pedley X<br />
Calopogonium mucunoides Desv.* X X<br />
Canavalia cathartica Thouars X<br />
Canavalia papuana Merr. & L.M.Perry X X<br />
Canavalia rosea (Sw.) DC. X X X<br />
Centrosema molle Mart. ex Benth.* X<br />
Clitoria ternatea L.* X X<br />
Crotalaria brevis Domin X<br />
Crotalaria calycina Schrank X X X<br />
Crotalaria goreensis Guill. & Perr.* X X X<br />
Crotalaria humifusa Graham ex Benth. X<br />
Crotalaria medicaginea Lam. var. medicaginea X X<br />
Crotalaria<br />
Niyomdham<br />
montana var. angustifolia (Gagnep.) X X<br />
Crotalaria pallida var. obovata (G.Don) Polhill* X X<br />
Crotalaria retusa L. var. retusa* X<br />
Crotalaria sessiliflora var. anthylloides (Lam.) X<br />
17 Requires determination<br />
A.A.Ansari & Thoth.<br />
Crotalaria sp. (Torres Strait J.R.Clarkson 2044) X<br />
Cullen badocanum (Blanco) Verdc. X<br />
Dalbergia densa var. australis Prain X X X<br />
Dendrolobium arbuscula (Domin) H.Ohashi X<br />
Dendrolobium umbellatum (L.) Benth. var. umbellatum X X<br />
Derris rubrocalyx Verdc. subsp. rubrocalyx X X<br />
Derris sp. (Claudie River L.J.Webb+ 8348) X X<br />
Derris trifoliata Lour. X X<br />
Desmodium gangeticum (L.) DC. X<br />
Desmodium heterocarpon (L.) DC. var. heterocarpon X<br />
Desmodium heterocarpon var. strigosum Meeuwen X<br />
Desmodium pullenii Pedley X<br />
Desmodium scorpiurus (Sw.) Desv.* X<br />
Desmodium tortuosum (Sw.) DC.* X X<br />
Desmodium trichostachyum Benth. X<br />
Desmodium triflorum (L.) DC.* X<br />
Erythrina insularis F.M.Bailey X X<br />
Erythrina variegata L. X X<br />
Erythrina vespertilio Benth. X X<br />
Flemingia parviflora X X<br />
Galactia muelleri Benth. X X<br />
Galactia sp. (Andoom A.Morton 1149) X<br />
Galactia tenuiflora (Spreng.) Willd. ex Wight & Arn. X X<br />
Glycine tomentella Hayata X X<br />
Gompholobium sp. (Tozers Gap C.H.Gittins 1030) X<br />
Gompholobium sp. (DGFell 9709+DJStanton) 17 X<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Indigofera colutea (Burm.f.) Merr. X<br />
Indigofera gl<strong>and</strong>ulosa Willd. X<br />
Indigofera linifolia (L.f.) Retz. X X<br />
Indigofera polygaloides M.B.Scott X<br />
Indigofera praatensis X<br />
Indigofera tinctoria L.* X<br />
Indigofera trifoliata L. X<br />
Jacksonia thesioides A.Cunn. ex Benth. X X X<br />
Macroptilium atropurpureum (DC.) Urb.* X X<br />
Macroptilium lathyroides (L.) Urb.* X X<br />
Macroptilium lathyroides var. semierectum (L.) Urb.* X<br />
Millettia pinnata (L.) Panigrahi X X X<br />
Mimosa pudica var. unijuga (Walp. & Duchass.)<br />
Griseb.*<br />
X X<br />
Mucuna gigantea (Willd.) DC. X X<br />
Mucuna pruriens var. utilis (Wall. ex Wight) Baker ex X<br />
Burck*<br />
Ormocarpum orientale (Spreng.) Merr. X<br />
Pachyrhizus erosus (L.) Urb.* X<br />
Pterocarpus indicus Willd. X<br />
Pueraria montana var. lobata (Willd.) Maesen & X<br />
S.M.Almeida*<br />
Pycnospora lutescens (Poir.) Schindl. X<br />
Rhynchosia acuminatissima Miq. X X<br />
Rhynchosia minima (L.) DC. X X<br />
Rhynchosia minima var. australis (Benth.) C.Moore X<br />
Sesbania cannabina (Retz.) Poir. var. cannabina X X<br />
Smithia conferta Sm. X<br />
Sophora tomentosa subsp. australis Yakovlev X X<br />
Stylosanthes hamata (L.) Taub.* X X<br />
Stylosanthes humilis Kunth* X X<br />
Stylosanthes scabra Vogel* X X<br />
Tephrosia sp. X<br />
Tephrosia filipes Benth. subsp. filipes X X<br />
Tephrosia juncea Benth. X X<br />
Tephrosia laxa Domin X<br />
Tephrosia maculata Merr. & L.M.Perry X<br />
Tephrosia sp. (Muddy Bay P.I.Forster+ PIF15313) X<br />
Teramnus labialis (L.f.) Spreng.* X<br />
Uraria picta (Jacq.) Desv. X<br />
V<strong>and</strong>asina retusa (Benth.) Rauschert X X<br />
Vigna sp. X<br />
Vigna adenantha (G.Mey.) Marechal, Mascherpa & X<br />
Stainier*<br />
Vigna marina (Burm.) Merr. X X<br />
Vigna radiate var. sublobata (Roxb.) Verdc. X<br />
Vigna vexillata var. angustifolia (Schumach. & Thonn.) X<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Baker<br />
Vigna vexillata var. youngiana F.M.Bailey X<br />
Zornia areolata Mohlenbr. X<br />
Zornia dyctiocarpa var. filifolia (Domin) S.T.Reynolds X<br />
& A.E.Holl<strong>and</strong><br />
Zornia muelleriana Mohlenbr. subsp. muelleriana X<br />
Zornia muriculata Mohlenbr. subsp. muriculata X<br />
Zornia ramosa S.T.Reynolds & A.E.Holl<strong>and</strong> X<br />
Flacourtiaceae Flacourtia jangomas (Lour.) Raeusch.* X<br />
Flacourtia sp. (Shiptons Flat L.W.Jessup+ GJD3200) X X<br />
Scolopia braunii (Klotzsch) Sleumer X X<br />
Flagellariaceae Flagellaria indica L. X X X<br />
Goodeniaceae Goodenia debilis A.E.Holl<strong>and</strong> & T.P.Boyle X<br />
Goodenia pilosa (R.Br.) Carolin X<br />
Lechenaultia filiformis R.Br. X<br />
Scaevola taccada (Gaertn.) Roxb. X X<br />
Velleia sp. X<br />
Haemodoraceae Haemodorum coccineum R.Br. X X X<br />
Haloragaceae Gonocarpus acanthocarpus (Brongn.) Orchard X<br />
Myriophyllum sp. X<br />
Helicteraceae Helicteres isora L. X<br />
Helicretes semiglabra (F. muell.) F.M. Bailey X<br />
Caesia parviflora R.Br. var. parviflora X<br />
Hemerocallidaceae Dianella caerulea Sims X X<br />
Dianella caerulea var. aquilonia R.J.F.Hend. X<br />
Dianella caerulea var. vannata R.J.F.Hend. X X<br />
Dianella longifolia R.Br. X X<br />
Dianella odorata Blume X<br />
Dianella pavopennacea var. major R.J.F.Hend. X X X<br />
Hern<strong>and</strong>iaceae Gyrocarpus americanus Jacq. subsp. americanus X X<br />
Hern<strong>and</strong>ia nymphaeifolia (C.Presl) Kubitzki X<br />
Hugoniaceae Hugonia jenkinsii X<br />
Hydrocharitaceae Enhalus sp. X<br />
Enhalus acoroides (L.f.) Royle X<br />
Halophila minor (Zoll.) Hartog X<br />
Hypoxidaceae Curculigo ensifolia R.Br. var. ensifolia X<br />
Johnsoniaceae Caesia setifera Baker X<br />
Tricoryne anceps subsp. pterocaulon (Baker) Thongp. X X X<br />
Juncaginaceae Triglochin dubium R.Br. X<br />
Lamiaceae Anisomeles malabarica (L.) R.Br. ex Sims X X<br />
Baslicum polystachyon X<br />
Callicarpa brevistyla Munir X<br />
Callicarpa c<strong>and</strong>icans (Burm.f.) Hochr. X X<br />
Clerodendrum sp. X<br />
Clerodendrum costatum R.Br. X<br />
Clerodendrum floribundum R.Br. X X<br />
Clerodendrum inerme (L.) Gaertn. X X<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Clerodendrum longiflorum var. glabrum Munir X X<br />
Faradaya splendida F.Muell. X<br />
Glossocarya hemiderma (F.Muell. ex Benth.) Benth. & X X<br />
Hook.f. ex B.D.Jacks.<br />
Gmelina dalrympleana (F.Muell.) H.J.Lam X X X<br />
Gmelina philippensis Cham.* X<br />
Hyptis suaveolens (L.) Poit.* X X X<br />
Leucas decemdentata (Willd.) Sm. X<br />
Ocimum basilicum L.* X<br />
Ocimum tenuiflorum L. X<br />
Orthosiphon aristatus (Blume) Miq. X<br />
Platostoma longicorne (F.Muell.) A.J.Paton X<br />
Plectranthus amboinicus (Lour.) Spreng.* X<br />
Plectranthus parviflorus Willd. X X<br />
Plectranthus scutellarioides (L.) R.Br. X X<br />
Premna acuminata R.Br. X X X<br />
Premna dallachyana Benth. X X<br />
Premna serratifolia L. X X<br />
Salvia misella Kunth* X<br />
Vitex helogiton K.Schum. X X<br />
Vitex rotundifolia L.f. X X<br />
Vitex trifolia L. var. trifolia X X<br />
Lauraceae Beilschmiedia obtusifolia X<br />
Cassytha filiformis L. X X X<br />
Cryptocarya bamagana X<br />
Cryptocarya brassii C.K.Allen X X<br />
Cryptocarya cunninghamii Meisn. X X<br />
Cryptocarya exfoliata C.K.Allen X X<br />
Cryptocarya hypospodia F.Muell. X X<br />
Cryptocarya triplinervis R.Br. X X<br />
Endi<strong>and</strong>ra glauca R.Br. X X X<br />
Endi<strong>and</strong>ra impressicosta X<br />
Litsea breviumbellata C.K.Allen X X<br />
Litsea glutinosa (Lour.) C.B.Rob. X X<br />
Neolitsea brassii X<br />
Laxmanniaceae Eustrephus latifolius R.Br. ex Ker Gawl. X X X<br />
Lom<strong>and</strong>ra banksii (R.Br.) Lauterb. X X X<br />
Lom<strong>and</strong>ra multiflora (R.Br.) Britten subsp. multiflora X X<br />
Thysanotus banksii R.Br. X<br />
Thysanotus tuberosus R.Br. subsp. tuberosus X<br />
Lecythidaceae Barringtonia acutangula (L.) Gaertn. subsp. acutangula X X<br />
Barringtonia calyptrata (R.Br. ex Miers) R.Br. ex X X<br />
F.M.Bailey<br />
Barringtonia racemosa X<br />
Planchonia careya (F.Muell.) R.Knuth X X X<br />
Lentibulariaceae Utricularia sp. X X<br />
Utricularia bifida L. X<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Utricularia caerulea L. X<br />
Utricularia chrysantha R.Br. X<br />
Loganiaceae Mitrasacme connata R.Br. X<br />
Mitrasacme pygmaea R.Br. X<br />
Mitreola petiolata (J.F.Gmel.) Torr. & Gray X<br />
Strychnos lucida R.Br. X X<br />
Loranthaceae Amyema villiflora (Domin) Barlow subsp. villiflora X<br />
Amyema congener X<br />
Amylotheca dictyophleba (F.Muell.) Tiegh. X<br />
Decaisnina angustata (Barlow) Barlow X<br />
Dendrophthoe curvata (Blume) Miq. X<br />
Dendrophthoe glabrescens (Blakely) Barlow X X<br />
Diplatia tomentosa Barlow X<br />
Lythraceae Ammannia multiflora Roxb. X<br />
Lagerstroemia speciosa (L.) Pers.* X<br />
Pemphis acidula J.R.Forst. & G.Forst. X X<br />
Sonneratia alba Sm. X X<br />
Malpighiaceae Ryssopterys timorensis (Blume) A.Juss. X X<br />
Malvaceae Abelmoschus manihot subsp. tetraphyllus (Roxb. ex X<br />
Hornem.) Borss.Waalk.*<br />
X<br />
Abelmoschus moschatus subsp. tuberosus (Span.) X X<br />
Borss.Waalk.<br />
Abutilon albescens Miq. X X<br />
Abutilon auritum X<br />
Abutilon indicum (L.) Sweet X X<br />
Abutilon sp. X X<br />
Gossypium barbadense L.* X<br />
Hibiscus meraukensis Hochr. X X X<br />
Hibiscus normanii F.Muell. X<br />
Hibiscus rosasinensis L.* X X<br />
Hibiscus sabdariffa L.* X<br />
Hibiscus tiliaceus L. X X<br />
Hibiscus vitifolius L. X<br />
Malvastrum corom<strong>and</strong>elianum (L.) Garcke subsp. X<br />
corom<strong>and</strong>elianum*<br />
Sida acuta Burm.f.* X X<br />
Sida cordifolia L.* X<br />
Sida pusilla Cav. X<br />
Sida rhombifolia L.* X X<br />
Thespesia populnea (L.) Sol. ex Correa X X<br />
Thespesia populneoides (Roxb.) Kostel. X X<br />
Urena lobata L.* X X<br />
Melastomataceae Melastoma malabathricum L. subsp. malabathricum X X<br />
Osbeckia chinensis L. X X<br />
Ptern<strong>and</strong>ra coerulescens Jack X<br />
Meliaceae Aglaia brownii Pannell X X<br />
Aglaia elaeagnoidea (A.Juss.) Benth. X X<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Aglaia sapindina X<br />
Aglaia tomentosa Teijsm. & Binn. X X<br />
Anthocarapa nitidula X<br />
Dysoxylum acutangulum subsp. foveolatum (Radlk.) X X<br />
Mabb.<br />
Dysoxylum oppositifolium F.Muell. X X<br />
Dysoxylum latifolium X<br />
S<strong>and</strong>oricum koetjape (Burm.f.) Merr.* X<br />
Turraea pubescens Hellen. X X<br />
Vavaea amicorum Benth. X X<br />
Xylocarpus granatum K.D.Koenig X X<br />
Xylocarpus moluccensis (Lam.) M.Roem. X X<br />
Xylocarpus rumphii (Kostel.) Mabb. X X<br />
Memecylaceae Memecylon pauciflorum Blume var. pauciflorum X X<br />
Menispermaceae Hypserpa decumbens (Benth.) Diels X X<br />
Pachygone ovata (Poir.) Hook.f. & Thomson X X<br />
Stephania japonica (Thunb.) Miers X X<br />
Stephania japonica (Thunb.) Miers var. japonica X X<br />
Stephania japonica var. timoriensis (DC.) Forman X X<br />
Tinospora smilacina Benth. X X X<br />
Menyanthaceae Nymphoides sp. X<br />
Nymphoides aurantiaca (Dalzell) Kuntze X<br />
Nymphoides exiliflora (F.Muell.) Kuntze X<br />
Nymphoides triangularis Aston X<br />
Villarsia sp. (Laura C.Dalliston CC18) X<br />
Mimosaceae Acacia aulacocarpa A.Cunn. ex Benth. X<br />
Acacia auriculiformis A.Cunn. ex Benth. X X<br />
Acacia brassii Pedley X X X<br />
Acacia crassicarpa A.Cunn. ex Benth. X X X<br />
Acacia holosericea X<br />
Acacia humifusa A.Cunn. ex Benth. X X<br />
Acacia leptocarpa A.Cunn. ex Benth. X X X<br />
Acacia oraria F.Muell. X X<br />
Acacia platycarpa F.Muell. X X<br />
Acacia polystachya A.Cunn. ex Benth. X X X<br />
Acacia simsii A.Cunn. ex Benth. X X X<br />
Adenanthera pavonina L. X X<br />
Albizia lebbeck (L.) Benth. X X<br />
Archidendron gr<strong>and</strong>iflorum (Sol. ex Benth.) I.C.Nielsen X X<br />
Archidendron hirsutum I.C.Nielsen (Rare) X X<br />
Cathormion umbellatum subsp. moniliforme (DC.)<br />
Brummitt<br />
X X<br />
Entada phaseoloides (L.) Merr. X X<br />
Entada rheedii Spreng. X X<br />
Leucaena leucocephala (Lam.) de Wit subsp. X X<br />
leucocephala*<br />
Mimosa pudica var. unijuga (Walp. & Duchass.) X X<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Griseb.*<br />
Paraserianthes toona (F.M.Bailey) I.C.Nielsen X X X<br />
Molluginaceae Glinus oppositifolius (L.) A.DC. X X<br />
Mollugo pentaphylla L.* X X<br />
Monimiaceae Wilkiea rigidifolia (A.C.Sm.) Whiffin & Foreman X X<br />
Moraceae Antiaris toxicaria var. macrophylla (R.Br.) Corner X X<br />
Fatoua villosa (Thunb.) Nakai (Rare) X<br />
Ficus sp. X<br />
Ficus drupacea Thunb. var. drupacea X X<br />
Ficus fraseri Miq. X<br />
Ficus microcarpa L.f. X X<br />
Ficus microcarpa var. hillii (F.M.Bailey) Corner X X<br />
Ficus obliqua G.Forst. X X<br />
Ficus opposita Miq. X X<br />
Ficus opposita var. aculeata (Miq.) R.J.F.Hend. X<br />
Ficus racemosa X<br />
Ficus superba var. henneana (Miq.) Corner X X<br />
Ficus virens Aiton X<br />
Ficus virens var. sublanceolata (Miq.) Corner X X<br />
Streblus brunonianus X<br />
Trophis sc<strong>and</strong>ens (Lour.) Hook. & Arn. subsp. sc<strong>and</strong>ens X X<br />
Moringaceae Moringa oleifera Lam.* X<br />
Myristicaceae Horsfieldia australiana X<br />
Myristica insipida R.Br. var. insipida X X<br />
Myrsinaceae Aegiceras corniculatum (L.) Blanco X X X<br />
Myrsine urceolata R.Br. X X X<br />
Myrtaceae Acmena hemilampra (F.Muell. ex F.M.Bailey) Merr. & X X<br />
L.M.Perry subsp. hemilampra<br />
Acmenosperma claviflorum X<br />
Asteromyrtus brassii (Byrnes) Craven X X<br />
Asteromyrtus symphyocarpa (F.Muell.) Craven X X X<br />
Baeckea frutescens L. X X<br />
Corymbia clarksoniana X X<br />
Corymbia latifolia X<br />
Corymbia nesophila (Blakely) K.D.Hill & X X X<br />
L.A.S.Johnson<br />
Corymbia novoguinensis (D.J.Carr & S.G.M.Carr)<br />
K.D.Hill & L.A.S.Johnson<br />
X X X<br />
Corymbia polycarpa (F.Muell.) K.D.Hill & X X<br />
L.A.S.Johnson<br />
Corymbia stockeri (D.J.Carr & S.G.M.Carr) K.D.Hill &<br />
L.A.S.Johnson subsp. stockeri<br />
X<br />
Corymbia stockeri subsp. peninsularis (K.D.Hill & X<br />
L.A.S.Johnson) A.R.Bean<br />
X X<br />
Corymbia tessellaris (F.Muell.) K.D.Hill & X X X<br />
L.A.S.Johnson<br />
Eucalyptus brassiana X<br />
Eucalyptus cullenii Cambage X X X<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Eucalyptus leptophleba F.Muell. X X<br />
Eucalyptus platyphylla F.Muell. X X X<br />
Eucalyptus tetrodonta X<br />
Eugenia reinwardtiana (Blume) DC. X X<br />
Gossia floribunda (A.J.Scott) N.Snow & Guymer X X<br />
Lithomyrtus obtusa (Endl.) N.Snow & Guymer X X X<br />
Lithomyrtus retusa X X<br />
Lophostemon suaveolens (Sol. ex Gaertn.) Peter X X<br />
G.Wilson & J.T.Waterh.<br />
Melaleuca acacioides F.Muell. X X X<br />
Melaleuca arcana X<br />
Melaleuca argentea X<br />
Melaleuca cajuputi subsp. platyphylla Barlow X X<br />
Melaleuca dealbata S.T.Blake X X<br />
Melaleuca leucadendra (L.) L. X X<br />
Melaleuca nervosa X<br />
Melaleuca quinquenervia (Cav.) S.T.Blake X X<br />
Melaleuca saligna Schauer X X X<br />
Melaleuca sp. (Zuna DGF9257+) 18 X<br />
Melaleuca stenostachya S.T.Blake X X X<br />
Melaleuca viridiflora Sol. ex Gaertn. var. viridiflora X X X<br />
Neofabricia myrtifolia (Gaertn.) Joy Thomps. X X X<br />
Osbornia octodonta F.Muell. X X<br />
Rhodamnia australis A.J.Scott X X<br />
Rhodomyrtus macrocarpa Benth. X X<br />
Syzygium angophoroides (F.Muell.) B.Hyl<strong>and</strong> X X<br />
Syzygium aqueum (Burm.f.) Alston (Rare) X X<br />
Syzygium bamagense B.Hyl<strong>and</strong> X X<br />
Syzygium br<strong>and</strong>erhorstii Lauterb. X X<br />
Syzygium buettnerianum (K.Schum.) Nied. (Rare) X X<br />
Syzygium bungadinnia (F.M.Bailey) B.Hyl<strong>and</strong> X X<br />
Syzygium<br />
L.M.Perry<br />
fibrosum (F.M.Bailey) T.G.Hartley & X X<br />
Syzygium forte (F.Muell.) B.Hyl<strong>and</strong> subsp. forte X X<br />
Syzygium puberulum Merr. & L.M.Perry X X<br />
Syzygium<br />
L.M.Perry<br />
suborbiculare (Benth.) T.G.Hartley & X X X<br />
Welchiodendron longivalve (F.Muell.) Peter G.Wilson X X X<br />
& J.T.Waterh.<br />
Nyctaginaceae Boerhavia sp. X<br />
Boerhavia albiflora Fosberg var. albiflora X<br />
Boerhavia dominii Meikle & Hewson X<br />
Boerhavia mutabilis R.Br. X X<br />
Pisonia aculeata L. X X<br />
Pisonia gr<strong>and</strong>is R.Br. X<br />
18 Requires determination<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
223
Family_Name Botanical_Name BRI C’veg 3DE<br />
Nymphaeaceae Nymphaea violacea Lehm. X<br />
Olacaceae Ximenia americana L. X X<br />
Oleaceae Chionanthus ramiflora Roxb. X X<br />
Jasminum didymum G.Forst. subsp. didymum X X<br />
Jasminum elongatum (Bergius) Willd. X X<br />
Notelaea longifolia X<br />
Onagraceae Ludwigia hyssopifolia (G.Don) Exell* X X<br />
Ludwigia octovalvis (Jacq.) P.H.Raven X X<br />
Ludwigia perennis L. X<br />
Opiliaceae Cansjera leptostachya Benth. X X<br />
Opilia amentacea Roxb. X X X<br />
Orchidaceae Arthrochilus irritabilis F.Muell. X<br />
Arthrochilus sabulosus D.L.Jones X<br />
Bulbophyllum sp. X X<br />
Cadetia maideniana (Schltr.) Schltr. X<br />
Cadetia wariana Schltr. (Rare) X X<br />
Chiloschista phyllorhiza (F.Muell.) Schltr. X<br />
Crepidium marsupichilum (Upton) Szlach. X<br />
Dendrobium canaliculatum X X<br />
Dendrobium bigibbum Lindl. (Vulnerable) X X X<br />
Dendrobium discolor X<br />
Dendrobium johannis Rchb.f. (Vulnerable) X X<br />
Dendrobium litorale Schltr. X X<br />
Dendrobium smillieae F.Muell. X<br />
Dendrobium trilamellatum J.J.Sm. X X X<br />
Dendrobium x lavarackianum M.A.Clem. X<br />
Dendrobium x superbiens Rchb.f. (Vulnerable) X<br />
Diplocaulobium glabrum (J.J.Sm.) Kraenzl. X<br />
Dockrillia calamiformis (Lodd.) M.A.Clem. & X<br />
D.L.Jones<br />
Empusa habenarina (F.Muell.) M.A.Clem. & D.L.Jones X<br />
Eria fitzalanii F.Muell. X<br />
Grastidium insigne (Blume) M.A.Clem. & D.L.Jones X<br />
Grastidium luteocilium (Rupp) Rauschert X<br />
Habenaria elongata R.Br. X<br />
Habenaria propinquior Rchb.f. X<br />
Luisia teretifolia Gaudich. X<br />
Nervilia sp. X<br />
Nervilia holochila (F.Muell.) Schltr. X<br />
Nervilia peltata B.Gray & D.L.Jones X<br />
Nervilia plicata (Andrews) Schltr. X<br />
Pholidota imbricata Hook. X<br />
Taeniophyllum sp. (DGF9319+) 19 X<br />
Vrydagzynea elongata Blume X<br />
Oxalidaceae Biophytum petersianum Klotzsch X<br />
19 Requires determination<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
224
Family_Name Botanical_Name BRI C’veg 3DE<br />
P<strong>and</strong>anaceae P<strong>and</strong>anus sp. X X<br />
P<strong>and</strong>anus conicus X<br />
P<strong>and</strong>anus tectorius Parkinson X X<br />
P<strong>and</strong>anus zea (Rare) X<br />
Passifloraceae Adenia heterophylla (Blume) Koord. X X<br />
Adenia heterophylla subsp. australis (R.Br. ex DC.) X X<br />
W.J.de Wilde<br />
Passiflora aurantia G.Forst. var. aurantia X X<br />
Passiflora foetida L.* X X X<br />
Passiflora suberosa L.* X X<br />
Pedaliaceae Josephinia imperatricis Vent. X X<br />
Pentaphylacaceea Ternstroemia cherryi X<br />
Petiveriaceae Rivina humilis L.* X X<br />
Phyllanthaceae Actephila venusta P.I.Forst. X X<br />
Antidesma bunius (L.) Spreng. X X<br />
Antidesma ghaesembilla Gaertn. X X<br />
Antidesma parvifolium Thwaites & F.Muell. X X<br />
Breynia cernua (Poir.) Muell.Arg. X X X<br />
Breynia oblongifolia (Muell.Arg.) Muell.Arg. X X<br />
Bridelia finalis P.I.Forst. X X<br />
Bridelia tomentosa Blume X X<br />
Cleistanthus apodus Benth. X X<br />
Cleistanthus peninsularis Airy Shaw & B.Hyl<strong>and</strong> X X<br />
Cleistanthus xerophilus Domin X X<br />
Flueggea virosa subsp. melanthesoides (F.Muell.) X X X<br />
G.L.Webster<br />
Glochidion apodogynum X<br />
Glochidion disparipes Airy Shaw X X<br />
Phyllanthus amarus Schumach.* X<br />
Phyllanthus novae-holl<strong>and</strong>iae Muell.Arg. X X<br />
Phyllanthus reticulatus Poir. X X<br />
Phyllanthus sp. X<br />
Phyllanthus virgatus G.Forst. X X X<br />
Sauropus <strong>and</strong>rogynus (L.) Merr.* X<br />
Picrodendraceae Petalostigma pubescens X<br />
Piperaceae Piper caninum Blume X X<br />
Piper sarmentosum Roxb.* X<br />
Pittosporaceae Bursaria incana Lindl. X X<br />
Pittosporum ferrugineum subsp. linifolium (A.Cunn.) X X<br />
L.W.Cayzer, Crisp & I.Telford<br />
Pittosporum ferrugineum W.T.Aiton subsp. ferrugineum X X<br />
Pittosporum venulosum F.Muell. X X<br />
Plumbaginaceae Aegialitis annulata R.Br. X X<br />
Plumbago zeylanica L. X<br />
Poaceae Alloteropsis cimicina (L.) Stapf X X<br />
Alloteropsis semialata (R.Br.) Hitchc. X X X<br />
Apluda mutica L. (Rare) X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Aristida dominii B.K.Simon X<br />
Aristida holathera Domin var. holathera X X<br />
Aristida perniciosa Domin X<br />
Aristida utilis F.M.Bailey var. utilis X<br />
Arthraxon castratus (Griff.) V.Naray. ex Bor X<br />
Arundinella nepalensis Trin. X X X<br />
Arundinella setosa Trin. X X<br />
Arundo donax L.* X<br />
Axonopus compressus (Sw.) P.Beauv.* X X<br />
Bambusa sp. X X<br />
Bambusa vulgaris Schrad.* X X<br />
Bothriochloa bladhii (Retz.) S.T.Blake X X<br />
Bothriochloa bladhii (Retz.) S.T.Blake subsp. bladhii X<br />
Bothriochloa pertusa (L.) A.Camus* X X<br />
Capillipedium parviflorum (R.Br.) Stapf X X<br />
Cenchrus brownii Roem. & Schult.* X<br />
Cenchrus echinatus L.* X X<br />
Cenchrus elymoides var. brevisetosus B.K.Simon X<br />
Chionachne cyathopoda (F.Muell.) F.Muell. ex Benth. X<br />
Chloris gayana Kunth* X X<br />
Chloris inflata Link* X X<br />
Chrysopogon aciculatus (Retz.) Trin.* X<br />
Chrysopogon elongatus (R.Br.) Benth. X<br />
Chrysopogon setifolius Stapf X<br />
Cleistochloa subjuncea C.E.Hubb. X<br />
Coix lacryma-jobi L.* X<br />
Cymbopogon ambiguus A.Camus X X X<br />
Cymbopogon bombycinus (R.Br.) Domin X X<br />
Cymbopogon globosus Henrard X<br />
Cynodon dactylon (L.) Pers. var. dactylon* X X<br />
Dactyloctenium aegyptium (L.) Willd.* X<br />
Dactyloctenium radulans (R.Br.) P.Beauv. X X<br />
Dichanthium aristatum (Poir.) C.E.Hubb.* X<br />
Dichanthium fecundum S.T.Blake X<br />
Digitaria sp. X X<br />
Digitaria bicornis (Lam.) Roem. & Schult. X<br />
Digitaria ciliaris (Retz.) Koeler* X X<br />
Digitaria ctenantha (F.Muell.) Hughes X<br />
Digitaria gibbosa (R.Br.) P.Beauv. X<br />
Digitaria ramularis (Trin.) Henrard X X<br />
Digitaria setigera Roth ex Roem. & Schult. X<br />
Echinochloa colona (L.) Link* X X<br />
Ectrosia agrostoides Benth. X<br />
Ectrosia lasioclada (Merr.) S.T.Blake X<br />
Ectrosia leporina R.Br. X X<br />
Eleusine indica (L.) Gaertn.* X X<br />
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226
Family_Name Botanical_Name BRI C’veg 3DE<br />
Elionurus citreus (R.Br.) Munro ex Benth. X<br />
Eragrostis amabilis (L.) Wight & Arn. ex Nees* X<br />
Eragrostis brownii (Kunth) Nees ex Wight X X<br />
Eragrostis cumingii Steud. X<br />
Eragrostis pubescens (R.Br.) Steud. X<br />
Eragrostis spartinoides Steud. X X<br />
Eragrostis unioloides (Retz.) Nees ex Steud. X<br />
Eremochloa bimaculata X<br />
Eremochloa ciliaris (L.) Merr. (Rare) X X<br />
Eriachne armitii F.Muell. ex Benth. X<br />
Eriachne burkittii Jansen X<br />
Eriachne ciliata R.Br. X<br />
Eriachne humilis W.Hartley X<br />
Eriachne obtusa R.Br. X<br />
Eriachne pallescens R.Br. X X<br />
Eriachne pallescens R.Br. var. pallescens X X<br />
Eriachne squarrosa R.Br. X<br />
Eriachne triseta Nees ex Steud. X X<br />
Eriochloa fatmensis (Hochst. & Steud.) Clayton X<br />
Eriochloa procera (Retz.) C.E.Hubb. X X<br />
Eriochloa pseudoacrotricha (Stapf ex Thell.) J.M.Black X<br />
Eulalia sp. (Sabai Isl<strong>and</strong> J.R.Clarkson 7801) X<br />
Eulalia mackinlayi X<br />
Germainia capitata Balansa & Poitr. (Vulnerable) X<br />
Heterachne gulliveri X<br />
Heteropogon contortus (L.) P.Beauv. ex Roem. & X X X<br />
Schult.<br />
Heteropogon triticeus (R.Br.) Stapf X X X<br />
Imperata cylindrica (L.) Raeusch. X X X<br />
Ischaemum australe R.Br. var. australe X X<br />
Ischaemum australe var. villosum (R.Br.) Benth. X X<br />
Ischaemum fragile R.Br. X X<br />
Ischaemum muticum L. X<br />
Ischaemum polystachyum J.Presl X<br />
Ischaemum rugosum Salisb. var. rugosum X<br />
Ischaemum rugosum var. segetum (Trin.) Hack. X<br />
Ischaemum triticeum R.Br. X<br />
Ischaemum tropicum B.K.Simon X<br />
Leptaspis banksii R.Br. X<br />
Leptochloa fusca (L.) Kunth subsp. fusca X X<br />
Leptochloa simoniana N.Snow X<br />
Lepturus geminatus C.E.Hubb. (Rare) X<br />
Lepturus repens (G.Forst.) R.Br. X<br />
Megathyrsus maximus (Jacq.) B.K.Simon & X X<br />
S.W.L.Jacobs var. maximus*<br />
Melinis minutiflora P.Beauv.* X<br />
Melinis repens (Willd.) Zizka* X X<br />
3d Environmental – Torres Strait <strong>Regional</strong> Ecosystem Mapping Project – August 2008<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Mnesithea formosa (R.Br.) de Koning & Sosef X X<br />
Mnesithea granularis (L.) de Koning & Sosef X<br />
Mnesithea rottboellioides (R.Br.) de Koning & Sosef X X X<br />
Neololeba atra (Lindl.) (Rare) X X<br />
Ophiuros exaltatus (L.) Kuntze X<br />
Oplismenus aemulus (R.Br.) Roem. & Schult. X X<br />
Oplismenus burmannii (Retz.) P.Beauv. X X<br />
Oplismenus compositus (L.) P.Beauv. X<br />
Panicum laevinode Lindl. X<br />
Panicum mindanaense Merr. X<br />
Panicum seminudum Domin var. seminudum X<br />
Panicum seminudum var. cairnsianum Domin X<br />
Panicum trichoides Sw. X X<br />
Paspalidium distans (Trin.) Hughes X X<br />
Paspalum distichum L. X<br />
Paspalum scrobiculatum L. X X<br />
Paspalum vaginatum Sw. X X<br />
Pennisetum ciliare (L.) Link* X<br />
Pennisetum pedicellatum subsp. unispiculum Brunken* X<br />
Pennisetum pedicellatum Trin. subsp. pedicellatum* X<br />
Pennisetum setigerum (Vahl) Wipff* X<br />
Perotis rara R.Br. X<br />
Phragmites australis (Cav.) Trin. ex Steud. X X<br />
Phragmites karka (Retz.) Trin. ex Steud. X X<br />
Pseudopogonatherum contortum (Brongn.) A.Camus X X<br />
Pseudopogonatherum irritans (R.Br.) A.Camus X<br />
Pseudoraphis spinescens (R.Br.) Vickery X<br />
Rottboellia cochinchinensis (Lour.) Clayton* X X<br />
Saccharum officinarum L.* X X<br />
Sacciolepis indica (L.) Chase X<br />
Sarga angustum (S.T.Blake) Spangler X<br />
Sarga plumosum (R.Br.) Spangler X X X<br />
Schizachyrium fragile (R.Br.) A.Camus X X X<br />
Schizachyrium pachyarthron C.A.Gardner X<br />
Sehima nervosum (Rottler) Stapf X<br />
Setaria apiculata (Scribn. & Merr.) K.Schum. X<br />
Setaria australiensis (Scribn. & Merr.) Vickery X<br />
Setaria pumila subsp. pallidefusca (Schumach.) X<br />
B.K.Simon*<br />
Setaria surgens Stapf X X<br />
Sorghum halepense (L.) Pers.* X<br />
Sorghum nitidum (Vahl) Pers. forma nitidum X X<br />
Sorghum nitidum forma aristatum C.E.Hubb. X<br />
Spinifex longifolius R.Br. X X<br />
Sporobolus jacquemontii Kunth* (Class 2) X<br />
Sporobolus lenticularis S.T.Blake X<br />
Sporobolus pulchellus R.Br. X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Sporobolus virginicus (L.) Kunth X X X<br />
Thaumastochloa heteromorpha X<br />
Thaumastochloa major S.T.Blake X X<br />
Thaumastochloa monolifera X<br />
Thaumastochloa pubescens (Benth.) C.E.Hubb. X<br />
Themeda arguens (L.) Hack. X X<br />
Themeda intermedia (Hack.) Bor* X<br />
Themeda quadrivalvis (L.) Kuntze* X<br />
Themeda tri<strong>and</strong>ra Forssk. X X<br />
Thuarea involuta (G.Forst.) R.Br. ex Roem. & Schult. X X<br />
Urochloa distachya (L.) Nguyen* X<br />
Urochloa holosericea (R.Br.) R.D.Webster X<br />
Urochloa holosericea (R.Br.) R.D.Webster subsp. X<br />
holosericea<br />
Urochloa mosambicensis (Hack.) D<strong>and</strong>y* X<br />
Urochloa mutica (Forssk.) Nguyen* X<br />
Urochloa panicoides var. pubescens (Kunth) Bor* X<br />
Urochloa piligera (F.Muell. ex Benth.) R.D.Webster X<br />
Urochloa pubigera (Roem. & Schult.) R.D.Webster X<br />
Urochloa ramosa (L.) R.D.Webster* X<br />
Urochloa subquadripara (Trin.) R.D.Webster* X<br />
Vacoparis laxiflorum (F.M.Bailey) Spangler X<br />
Whiteochloa airoides (R.Br.) Lazarides X<br />
Polygalaceae Polygala exsquarrosa Adema X<br />
Polygala longifolia Poir. X<br />
Polygala rhinanthoides Sol. ex Benth. X<br />
Polygala sp. (Portl<strong>and</strong> Roads L.Pedley 2757) X<br />
Salomonia ciliata (L.) DC. X<br />
Polygonaceae Antigonon leptopus Hook. & Arn.* X<br />
Muehlenbeckia zippelii (Meisn.) Danser X<br />
Portulacaceae Cal<strong>and</strong>rinia gracilis Benth. X<br />
Portulaca australis Endl. X<br />
Portulaca oleracea L.* X<br />
Portulaca pilosa L.* X<br />
Portulaca tuberosa Roxb. X<br />
Talinum triangulare (Jacq.) Willd.* X<br />
Proteaceae Banksia dentata L.f. X X X<br />
Grevillea coriacea McGill. X X<br />
Grevillea parallela Knight X X X<br />
Hakea pedunculata X X<br />
Helicia australasica F.Muell. X X<br />
Persoonia falcata X<br />
Xylomelum scottianum (F.Muell.) F.Muell. X X X<br />
Ptaeroxylaceae Harrisonia brownii A.Juss. X X<br />
Putranjivaceae Drypetes deplanchei (Brongn. & Gris) Merr. X X X<br />
Restionaceae Dapsilanthus<br />
L.A.S.Johnson<br />
elatior (R.Br.) B.G.Briggs & X X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Dapsilanthus<br />
L.A.S.Johnson<br />
spathaceus (R.Br.) B.G.Briggs & X X<br />
Leptocarpus sp. X X<br />
Rhamnaceae Alphitonia excelsa (A.Cunn. ex Fenzl) Reissek ex X<br />
Benth.<br />
X<br />
Alphitonia obtusifolia X<br />
Colubrina asiatica Brongn. X X<br />
Ziziphus oenopolia (L.) Mill. X X X<br />
Rhizophoraceae Bruguiera cylindrica (L.) Blume X X<br />
Bruguiera exaristata Ding Hou X X<br />
Bruguiera gymnorhiza (L.) Savigny X X<br />
Bruguiera parviflora (Roxb.) Wight & Arn. ex Griff. X X<br />
Carallia brachiata (Lour.) Merr. X X<br />
Ceriops tagal (Perr.) C.B.Rob. X X X<br />
Rhizophora apiculata Blume X X<br />
Rhizophora stylosa Griff. X X<br />
Rubiaceae Aidia racemosa (Cav.) Tirveng. X X<br />
Antirhea ovatifolia (M.E.Jansen) Chaw X X<br />
Atractocarpus sessilis (F.Muell.) Puttock X X<br />
Cyclophyllum brevipes (Merr. & L.M.Perry) X X<br />
S.T.Reynolds & R.J.F.Hend.<br />
Cyclophyllum maritimum S.T.Reynolds & R.J.F.Hend. X X X<br />
Dentella repens (L.) J.R.Forst. & G.Forst. X<br />
Everistia vacciniifolia S.T.Reynolds & R.J.F.Hend. X X<br />
Guettarda speciosa L. X X<br />
Hydnophytum moseleyanum Becc. var. moseleyanum X X<br />
Ixora timorensis Decne. X X X<br />
Mitracarpus hirtus (L.) DC.* X<br />
Morinda citrifolia L. X X<br />
Morinda reticulata Benth. X X X<br />
Myrmecodia platytyrea subsp. antoinii (Becc.) X X<br />
C.R.Huxley & Jebb<br />
Oldenl<strong>and</strong>ia biflora L. X<br />
Oldenl<strong>and</strong>ia corymbosa L. var. corymbosa* X<br />
Oldenl<strong>and</strong>ia galioides (F.Muell.) F.Muell. X X<br />
Pavetta australiensis Bremek. var. australiensis X X<br />
Pavetta brownii Bremek. var. brownii X<br />
Pavetta brownii var. glabrata S.T.Reynolds X X<br />
Pogonolobus reticulatus F.Muell. X X X<br />
Psilanthus brassii (J.-F.Leroy) A.P.Davis X<br />
Psychotria coelospermum X<br />
Psychotria loniceroides Sieber ex DC. X X<br />
Psychotria nesophila F.Muell. X X<br />
Psychotria poliostemma Benth. X X<br />
Psydrax banksii S.T.Reynolds & R.J.F.Hend. X X<br />
Psydrax graciliflora (Merr. & L.M.Perry) S.T.Reynolds<br />
& R.J.F.Hend.<br />
X X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Psydrax lamprophylla forma latissima S.T.Reynolds &<br />
R.J.F.Hend.<br />
X X<br />
Psydrax odorata (G.Forst.) A.C.Sm. & S.P.Darwin X X<br />
Psydrax reticulata (C.T.White) S.T.Reynolds & X X<br />
R.J.F.Hend. (Vulnerable)<br />
Richardia scabra L.* X<br />
Scyphiphora hydrophylacea Gaertn. X X<br />
Spermacoce brachystema R.Br. ex Benth. X X<br />
Spermacoce papuana F.Muell. X<br />
Spermacoce remota Lam.* X<br />
Spermacoce sp. X<br />
Spermacoce sp. (Lorim Point A.Morton AM1237) X<br />
Timonius timon (Spreng.) Merr. var. timon X X<br />
Triflorensia australis (Benth.) S.T.Reynolds X X<br />
Ruppiaceae Ruppia sp X<br />
Rutaceae Acronychia imperforata X<br />
Acronychia sp. (Batavia Downs J.R.Clarkson+ 8511) X<br />
Clauesena brevistyla X<br />
Glycosmis trifoliata (Blume) Spreng. X X<br />
Halfordia kendack (Montrouz.) Guillaumin X X X<br />
Luvunga monophylla X<br />
Melicope peninsularis T.G.Hartley X X<br />
Melicope rubra (Lauterb. & K.Schum.) T.G.Hartley X<br />
Micromelum minutum (G.Forst.) Wight & Arn. X X X<br />
Murraya ovatifoliolata X<br />
Murraya paniculata (L.) Jack X X<br />
Zanthoxylum parviflorum Benth. X<br />
Zanthoxylum rhetsa (Roxb.) DC. X X<br />
Santalaceae Exocarpos latifolius R.Br. X X X<br />
Sapindaceae Alectryon reticulatus X<br />
Alectryon rep<strong>and</strong>odentatus Radlk. (Endangered) X X<br />
Alectryon tomentosus (F.Muell.) Radlk. X X<br />
Allophylus cobbe (L.) Blume X X<br />
Arytera bifoliolata S.T.Reynolds X X<br />
Arytera divaricata X<br />
Arytera pseudofoveolata H.Turner X<br />
Atalaya australiana Leenh. X<br />
Atalaya sericopetala S.T.Reynolds X X<br />
Cupaniopsis anacardioides (A.Rich.) Radlk. X X<br />
Cupaniopsis flagelliformis subsp. flagelliformis X<br />
Dictyoneura obtusa Blume X X<br />
Dodonaea poly<strong>and</strong>ra Merr. & L.M.Perry X X X<br />
Dodonaea viscosa Jacq. subsp. viscosa X X<br />
Ganophyllum falcatum Blume X X X<br />
Harpullia arborea X<br />
Jagera pseudorhus (A.Rich.) Radlk. var. pseudorhus X X<br />
Lepidopetalum fructoglabrum Welzen X X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Mischocarpus lachnocarpus (F.Muell.) Radlk. X X<br />
Mischocarpus stipitatus S.T.Reynolds X X<br />
Toechima daemelianum (F.Muell.) Radlk. X X<br />
Tristiropsis acutangula (Rare) X<br />
Sapotaceae Chrysophyllum roxburgii X<br />
Manilkara kauki (L.) Dubard X X<br />
Mimusops elengi L. X X<br />
Palaquium galactoxylon X<br />
Pouteria myrsinodendron (F.Muell.) Jessup X<br />
Pouteria obovata (R.Br.) Baehni X X<br />
Pouteria sericea (Aiton) Baehni X X X<br />
Pouteria sp. (DGFell 9168+DJStanton) X<br />
Pouteria unmackiana (F.M.Bailey) Erlee X<br />
Scrophulariaceae Adenosma caerulea R.Br. X<br />
Angelonia salicariifolia Bonpl.* X<br />
Buchnera gracilis R.Br. X<br />
Buchnera linearis R.Br. X X<br />
Buchnera ramosissima R.Br. X<br />
Buchnera tetragona R.Br. X<br />
Limnophila fragrans (G.Forst.) Seem. X<br />
Lindernia antipoda (L.) Alston X<br />
Lindernia ciliata (Colsm.) Pennell X<br />
Lindernia crustacea (L.) F.Muell. X<br />
Lindernia scapigera R.Br. X<br />
Lindernia tenuifolia (Colsm.) Alston X<br />
Mecardonia procumbens (Mill.) Small* X X<br />
Scoparia dulcis L.* X X<br />
Striga curviflora (R.Br.) Benth. X<br />
Striga parviflora (R.Br.) Benth. X<br />
Simaroubaceae Brucea javanica (L.) Merr. X X<br />
Smilacaceae Smilax australis R.Br. X X X<br />
Smilax calophylla Wall. ex A.DC. X X<br />
Smilax glyciphylla X<br />
Solanaceae Capsicum annuum var. glabriusculum (Dunal) Heiser & X<br />
Pickersgill*<br />
Capsicum frutescens L.* X<br />
Datura inoxia Mill.* X<br />
Datura wrightii Regel* X<br />
Lycianthes shanesii (F.Muell.) A.R.Bean X<br />
Physalis angulata L.* X<br />
Physalis pubescens L.* X<br />
Solanum seaforthianum Andrews* X X<br />
Solanum viridifolium Dunal X X<br />
Sparrmanniaceae Corchorus aestuans L. X X<br />
Grewia breviflora Benth. X X<br />
Grewia latifolia X X<br />
Grewia oxyphylla Burret X X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Grewia retusifolia X X<br />
Triumfetta pent<strong>and</strong>ra A.Rich.* X<br />
Triumfetta rhomboidea Jacq.* X X<br />
Stackhousiaceae Stackhousia intermedia F.M.Bailey X<br />
Stackhousia viminea Sm. X<br />
Stemonuraceae Gomph<strong>and</strong>ra australiana X<br />
Sterculiaceae Argyrodendron poly<strong>and</strong>rum L.S.Sm. X X<br />
Heritiera littoralis Dry<strong>and</strong>. X X<br />
Sterculia quadrifida R.Br. X X<br />
Sterculia shillinglawii subsp. shillinglawii (Rare) X<br />
Sterculia sp. (Annan River L.J.Brass 20319) X X<br />
Stylidiaceae Stylidium alsinoides R.Br. X X<br />
Stylidium schizanthum F.Muell. X<br />
Stylidium tenerum Spreng. X<br />
Surianaceae Suriana maritima L. X X<br />
Taccaceae Tacca leontopetaloides (L.) Kuntze X X X<br />
Thymelaeaceae Phaleria oct<strong>and</strong>ra (L.) Baill. X X<br />
Thecanthes cornucopiae (Vahl) Wikstr. X<br />
Wikstroemia indica (L.) C.A.Mey. X X X<br />
Turneraceae Turnera ulmifolia L.* X<br />
Ulmaceae Celtis paniculata (Endl.) Planch. X X<br />
Celtis philippensis Blanco var. philippensis X X<br />
Trema tomentosa (Roxb.) Hara var. tomentosa X<br />
Trema tomentosa var. aspera (Brongn.) Hewson X X<br />
Urticaceae Laportea interrupta (L.) Chew X<br />
Nothocnide rep<strong>and</strong>a (Blume) Blume X<br />
Pipturus argenteus (G.Forst.) Wedd. X X<br />
Pouzolzia zeylanica (L.) Benn. X<br />
Verbenaceae Lantana camara L.* X X<br />
Stachytarpheta jamaicensis (L.) Vahl* X X<br />
Violaceae Hybanthus enneaspermus (L.) F.Muell. X X X<br />
Viscaceae Viscum articulatum Burm.f. X<br />
Vitaceae Ampelocissus acetosa (F.Muell.) Planch. X X<br />
Cayratia acris (F.Muell.) Domin X X<br />
Cayratia cardiophylla Jackes X X<br />
Cayratia clematidea (F.Muell.) Domin X X<br />
Cayratia maritima Jackes X X<br />
Cayratia trifolia (L.) Domin X X<br />
Cissus adnata Roxb. X X<br />
Cissus aristata Blume (Vulnerable) X<br />
Cissus opaca F.Muell. X X<br />
Cissus reniformis Domin X X<br />
Cissus repens Lam. X X<br />
Leea indica (Burm.f.) Merr. X X<br />
Xyridaceae Xyris complanata R.Br. X X X<br />
Zingiberaceae Alpinia caerulea (R.Br.) Benth. X X<br />
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Family_Name Botanical_Name BRI C’veg 3DE<br />
Alpinia sp. X<br />
Curcuma australasica Hook.f. X X X<br />
Globba marantina L. (Rare) X<br />
Kaempferia sp. (Murray Isl<strong>and</strong> M.Lawrie 5) X<br />
Zingiber officinale Roscoe* X<br />
Zingiber zerumbet (L.) Sm.* X<br />
Zygophyllaceae Tribulopis sol<strong>and</strong>ri R.Br. X<br />
Tribulus cistoides L. X X<br />
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