Aboriginal Camp Sites on the Western Coast of Damper

Total Page:16

File Type:pdf, Size:1020Kb

Aboriginal Camp Sites on the Western Coast of Damper 93 ictpt.r.,) J','uclof/tcr:/c . 4- ABORIGINAL CAMP SITES ON THEWESTERN COAST OF DAMPER LAND, WESTERNAUSTRALIA by Kim Akerman * The Dampierland Peninsulalies to the north of Broome on the north-west coast of WesternAustralia. The peninsula is within 25" - 30" rainfall belt,with temperature varying between 70° F in July and85° Fin November/December. The low plateau that makes upthe peninsula has el basal locally layer of cretaceous silicifiedsandstone, overlain with occuring Pliestocene sand dunesand a thin sandy soil veneer. locally The area supports tropicalwoodland vegetation known as 'pindan'. Very little has been recordedabout the day-to-day life of the coastal people ofDampierland. W.D. Campbell visited Sunday Island in 1908 andwith W.H. Bird provided an account of the Aborigines inhabitingit in 1915. From this account Bad tribe and from discussions heldwith elderly men of the now resident at OneArm Point, it is clear thatalthough a maritime people the materialculture possessed allowed only a very limitedexploitation of the marineenvironment. Many of the items consideredvital to a-coastal exploiting time. group were absent. Harpoons were not 'used until contact Even now the harpoons useddiffer radically from those used on the northern and eastern coastsof Australia. There appears to be no word in thelanguage for harpoons and they are designated 'English harpoons'and 'Japanese harpoons', depending on their construction(Figure 1, a and b). The 'English harpoon' is an ironrod of 1.5cm diameter non-detachable single up to one meter inlength with a flattened is formed into an off- barbed tip. The other end of the rod mangrove wood pole set 'eye'. This end is lashed firmly onto .a abudffOurMetet-g in TengtitThe-'Japanese-harpoon! differs This in having a detachablebarbed head with a hollow base. is slipped over a onemeter.iron foreshaft which in turnis lashed securely to the mangrovewood shaft. The harpoon line of the former type is securedthrough the 'eye' of the iron rod and in the latter isattached directly to thedetatchable found by Thomson (1934: head. The indigenous harpoon type as fore- 237-62) has a shaft socketed toreceive the head and no preferred for shaft. Among theBad the 'Japanese harpoon' is turtle and the 'Englishharpoon' with its lance-like head, harpooned and the for dugong. Turtles tend to spin when rigid 'English' iron is morelikely to pull out. * Manuscript received March 1974. Kim Akerman is with theDepartment of Public Health,Derby, W.A. 44' 94 ID Workshops Map 1: [Sunday I. 0 Living areas Freshwater soak 0 Low seawarddunes "mircLarger stabel dunes -tin Cape Reef Berthole - Derby Coulomb James :70 Price Pt. 0 INDIAN OCEAN Broom No Peninsula The Dampierland 0 Map 2: '400 ---- Coutait Pt creek 0 200 metres concentration Map 3: Sketch map showing Point of camps in areaB (i) Coulomb Recent sites nearCoulomb Pt. English Harpoon 1 metre Japanese Harpoon used by theBad Figure 1: Modern harpoon types Figure 2: 1 metre A2......... A. red soilcliff beach Al sea level ., rlietStorleilisitcrqe.istliet relationship betweenAl and A2 sites Sketch showingstratigraphical 95 Nowadays there is little emphasis ongathering sea foods from the reef or beach environmentalthough 'shelling' and the gathering of clam meat isundertaken for commercial purposes. Fishing with lines and hooks (formerly not made or used) is undertaken on anirregular basis. Fishing was formerly done with long single pointed unbarbed spears or with special fishing boomerangs. After the coming of the pearling fleets, iron 'boomerangs' were used by menand women when fishing in the shallows. Turtles are taken throughout the year but the main months appear to be October and November when mating or 'married' turtles are common. The hunters usually watch for them from beaches on either side of tidal channels. The copulating turtles are easily approached and harpooned. Dugong on the other hand migrate from areasnorth of Sunday Island south during March/May and at this time, aretaken often. The heavy emphasis on the large marine animals atpresent is nor reflected in surface sites to be describedand there appears to be a radical change inthe exploitation methoas used by the Dampierlanders. Description of sites The sites described here lie along a coastalstretch of some ten miles in lengthimmediately north of James Price Point. In 1971 W.H. Butler conducted a fauna surveyof the area on behalf of the Departmentof Fisheries and Fauna. On this survey artifacts similar to thosedescribed were collected and forwarded to the Western Australia Museum(W.H. Butler, personal communication). At present the coastal strip running from Coulomb Point to Cape Bertholet is aFisheries and Fauna Reserve. The coast here is rugged with beach frontsvarying between 100 and 500 rosters in width. TheFe beaches abut either on to large fixed sand dunes or onto terra rossa cliffs up to thirty meters in height.. Thesites which appear to belong to three different phases I havedesignated Al, A2 and B. Sites designated as Al and Al. appear to beconsiderably older than thOse that fall into the B category. On all three types of sites concentrationsof mollusc shells are evident. In fact, these shell concentrations are the main indications that there has beenaboriginal activity in the area. It appears that rock oysters (Crassostreasp), trochus (Trochus lineatus), ark shells (Arcidaesp), abalone (two species of HaZiotis, H. ovina and H. asinina) andsmall pearl oysters (Pinctada sp and Pteria sp) were themain shell fish gathered, although many shells belonging to other genera were found damaged on sites but in muchlesser quantities. 96 Gastropods were usually found tohave one or more of their whorls damaged - evidenceof the method of extraction the dorsal of the animal. Trochus shells, however, usually had half of their spires removed tofacilitate extraction of the animal. As well as the smaller molluscsthe large shells of trumpet shells (Syrinx auranus)and bailer shells (tdeloamphora), are common althoughusually damaged. Whole shells of the bailer shell usually have thecolumella and interior whorls .removed to convert the outer bodywhorls into a large bowl. Occasional specimens were seen with ahole punched in the side.of the body whorl opposite the aperture,allowing the columella to be grasped as a handle(Davidson 1937:200). Both Al and A2 are associated withthe red soil cliffs and fossilized dunes. Al sites have sparse shellaccumulations usually about small hearth zones. Hearths are characterized by a scatter of either burntsandstone lumps or baked antbed. There is a crude lithic industryusing silcretes which are exposed at sealevel on the western side of Dampierland, (this sandstone/silcrete stratum is wellexposed on the eastern coast of thepeninsula and appears to dip gently to the west). Boulders of silcrete were obtainedfrom creek washouts. Crude flakes with largeplain'striking platforms and sharp edges were used asknives and scrapers. Cores were also used aschoppers; otherwise there is no,evidence of any refined stone or shellindustry. Sites in the Al category do not appearto have any vertical accumulation and liedirectly above the disconformity between the sand stone and thered earth cliffs (Figure 2). A2 sites are found on the topsof the cliffs and appear to be up to 1-1.5 meters indepth. The shell accumulations are interbedded in theterra rossa soils. As hearth accumulations of the same speciesof shells appear, there begun seem to be indicationsthat specialized gathering had species to take place, Small concentrations of individual are found embeddedin the cliff face. The most striking introduction,however, is the refined lithic technology which hasproduced long simple blade points in with some marginal trimming. These blades are 3 to 12 cm length. Dortsb (L972: 65-710 described asimilar industry in the Chichester Ranges of WesternAustralia. At the Chichester Ranges, however, the blades areflaked from black, fine grained Dortch appear cherty siltstone. The techniques describeiby Dampierland to be the same asthose used for blade production on ground edge axes (Figure 3). As well as these points, rare of both pebble and bifacecoroid types have been introduced, pebbles. along with anvils made onsilcrete or shelly conglomerate All implements are madeof either silcrete or conglomerate. No artifacts made of basalt ordolerite have been noted, cm B. A- ground edge with slightmarginal trimming Heavily battered Blade points axe made or silcrete Small grindingplague of ferriginous grit. Thistype of grindstone isassociated 0 4 with bailer shellimplements <2277.- D. points Plain bladeswith flake vc(272212:32r1 F. 402 E. made 0 4 Nosed scraper Figure 5: Chopping implement on brokenflake made on a flake Figure 6: offramjcm Pebble anvil stoneof shelly associated with conglomerate food. oPentng trochusshells for 98 On the A2 sites a shelltechnology appears to have begun. Extremely brittle Melo shell bowls areweathered out of the cliff and one weathered ground bailershell knife/chisel was found. This was the only'shell knifefound associated with the cliff allow some top sites. Although sites in the Al and A2 category impressions of the prehistoriclife of the Dampierlanders, two sites in particular cover the contactand early post-contact era, which allow greaterinsights into the ecology of thestrand dwellers. These I have classed as B sites. B sites differ radically intheir location from A sites lying directly on stablized sanddunes about one mile apart. The first B (i) is on Point Coulomb,the other B (ii), on the south bank of a creek mouth, onemile to the north (Map 2). The sites lie between the first lowseaward dunes and extend east to the tops of thelarger stabilized dunes. On both sites it is possible toobserve that some specialization in food collection hastaken place. Separate hearths are often associated with oneparticular mollusc species, usually trochas, abalone or ark shells, Rock oyster shells are Also by far the commonest beingscattered over the entire area. at both sites it is possible to seethe remainof turtle.
Recommended publications
  • Building Nature's Safety Net 2008
    Building Nature’s Safety Net 2008 Progress on the Directions for the National Reserve System Paul Sattler and Martin Taylor Telstra is a proud partner of the WWF Building Nature's Map sources and caveats Safety Net initiative. The Interim Biogeographic Regionalisation for Australia © WWF-Australia. All rights protected (IBRA) version 6.1 (2004) and the CAPAD (2006) were ISBN: 1 921031 271 developed through cooperative efforts of the Australian Authors: Paul Sattler and Martin Taylor Government Department of the Environment, Water, Heritage WWF-Australia and the Arts and State/Territory land management agencies. Head Office Custodianship rests with these agencies. GPO Box 528 Maps are copyright © the Australian Government Department Sydney NSW 2001 of Environment, Water, Heritage and the Arts 2008 or © Tel: +612 9281 5515 Fax: +612 9281 1060 WWF-Australia as indicated. www.wwf.org.au About the Authors First published March 2008 by WWF-Australia. Any reproduction in full or part of this publication must Paul Sattler OAM mention the title and credit the above mentioned publisher Paul has a lifetime experience working professionally in as the copyright owner. The report is may also be nature conservation. In the early 1990’s, whilst with the downloaded as a pdf file from the WWF-Australia website. Queensland Parks and Wildlife Service, Paul was the principal This report should be cited as: architect in doubling Queensland’s National Park estate. This included the implementation of representative park networks Sattler, P.S. and Taylor, M.F.J. 2008. Building Nature’s for bioregions across the State. Paul initiated and guided the Safety Net 2008.
    [Show full text]
  • Bardi Plants an Annotated List of Plants and Their Use
    H.,c H'cst. /lust JIus lH8f), 12 (:J): :317-:359 BanE Plants: An Annotated List of Plants and Their Use by the Bardi Aborigines of Dampierland, in North-western Australia \!o\a Smith and .\rpad C. Kalotast Abstract This paper presents a descriptive list of the plants identified and used by the BarcE .\borigines of the Dampierland Peninsula, north~\q:stern Australia. It is not exhaust~ ive. The information is presented in two wavs. First is an alphabetical list of Bardi names including genera and species, use, collection number and references. Second is a list arranged alphabetically according to botanical genera and species, and including family and Bardi name. Previous ethnographic research in the region, vegetation communities and aspects of seasonality (I) and taxonomy arc des~ cribed in the Introduction. Introduction At the time of European colonisation of the south~west Kimberley in the mid­ nineteenth century, the Bardi Aborigines occupied the northern tip of the Dam­ pierland Peninsula. To their east lived the island-dwelling Djawi and to the south, the ~yulnyul. Traditionally, Bardi land ownership was based on identification with a particular named huru, translated as home, earth, ground or country. Forty-six bum have been identified (Robinson 1979: 189), and individually they were owned by members of a family tracing their ownership patrilineally, and known by the bum name. Collectively, the buru fall into four regions with names which are roughly equivalent to directions: South: Olonggong; North-west: Culargon; ~orth: Adiol and East: Baniol (Figure 1). These four directional terms bear a superficial resemblance to mainland subsection kinship patterns, in that people sometimes refer to themselves according to the direction in which their land lies, and indeed 'there are.
    [Show full text]
  • Dampierland 2
    Dampierland 2 Dampierland 2 (DL2 – Pindanland subregion) GORDON GRAHAM SEPTEMBER 2001 Subregional description and biodiversity • Adansonia gregorii (boab), Bauhinia cunninghamii and Grevillea striata (beefwood) grassy low open- values woodland. • Corymbia dampieri low open-woodland with Acacia spp. Shrubs and Triodia pungens (soft spinifex) and Description and area Triodia bitextura hummock grasses. • Eucalyptus brevifolia (snappy gum) low open- There are four basic components to the subregion. These woodland with Triodia spp. (spinifex) hummock comprise; grasses or sometimes a hummock grassland without • Quaternary sandplain overlying Jurassic and trees. Mesozoic sandstones with Pindan. There are • Acacia ancistrocarpa (Fitzroy wattle) and/or Acacia hummock grasslands on hills. eriopoda (Broome pindan wattle) and/or Acacia • Quaternary marine deposits on coastal plains, with monticola (Gawar) tall shrubland with Triodia mangal, samphire – Sporobolus spp. grasslands, intermedia (lobed spinifex) and Triodia pungens Melaleuca alsophila low forests, and Spinifex spp. – (soft spinifex) hummock grasses. Crotalaria spp. strand communities. • Grevillea refracta +/- Hakea lorea corkwood open- • Quaternary alluvial plains associated with the shrubland with Triodia pungens (soft spinifex) Permian and Mesozoic sediments of Fitzroy Trough hummock grasses. support tree savannahs of ribbon grass (Chrysopogon • Triodia pungens (soft spinifex) and/or Triodia spp.) – bluegrass (Dichanthium spp.) grasses with schinzii hummock grassland wooded with low trees scattered coolibah (Eucalyptus microtheca) - and Acacia spp. Shrubs. Bauhinia cunninghamii. There are riparian forests of river red gum (Eucalyptus camaldulensis) and Cadjeput (Melaleuca spp.) fringe drainages. Dominant land use (see Appendix B, key b) The climate is described as dry hot tropical and semi-arid with summer rainfall. The average annual rainfall is (ix) Grazing – Native pastures between 450 – 700 mm, slightly lower than the Fitzroy (xi) UCL and Crown reserves Trough subregion.
    [Show full text]
  • Hummock Grasslands Biome Climate Adaptation Flagship Working Paper #13D
    CLIMATE ADAPTATION FLAGSHIP The implications of climate change for biodiversity conservation and the National Reserve System: hummock grasslands biome Climate Adaptation Flagship Working Paper #13D Anita K Smyth, David W Hilbert, Simon Ferrier, Michael Dunlop, Tom Harwood, Kristen J Williams, Cameron S Fletcher and David Gobbett September 2012 National Library of Australia Cataloguing-in-Publication entry Title: The implications of climate change for biodiversity conservation and the National Reserve System: hummock grasslands biome / Anita K Smyth ISBN: 978-1-4863-0216-1 (pdf) Series: CSIRO Climate Adaptation Flagship working paper series; 13D. Other Climate Adaptation Flagship, Dave W Hilbert, Simon Ferrier, Authors/Contributors: Mike Dunlop, Tom Harwood, Kristen J Williams, Cameron S Fletcher and David Gobbett Enquiries Enquiries regarding this document should be To contact the lead author of the report: addressed to: Michael Dunlop Anita K Smyth Land-water-biodiversity-climate Analyst Data Facilitator (Partnerships, Licensing & Communications) CSIRO Ecosystem Sciences TERN Eco-informatics Facility GPO Box 1700, Black Mountain, ACT 2601 AUSTRALIA Level 12, Schulz Building, The University of Adelaide, 5005, AUSTRALIA [email protected] [email protected] Enquiries about the Climate Adaptation Flagship or the Working Paper series should be addressed to: Working Paper Coordinator CSIRO Climate Adaptation Flagship [email protected] Citation Smyth AK, Hilbert DW, Ferrier S, Dunlop M, Harwood T, Williams KJ, Fletcher CS and Gobbett D (2012) The implications of climate change for biodiversity conservation and the National Reserve System: hummock grasslands biome. CSIRO Climate Adaptation Flagship Working Paper No. 13D. www.csiro.au/resources/CAF-working-papers Copyright and disclaimer © 2012 CSIRO To the extent permitted by law, all rights are reserved and no part of this publication covered by copyright may be reproduced or copied in any form or by any means except with the written permission of CSIRO.
    [Show full text]
  • North Australian Pastoralists and Graziers Are Ready for Contractual Biodiversity Conservation
    North Australian pastoralists and graziers are ready for contractual biodiversity conservation Romy Greiner Charles Darwin University 28 April 2014 All photographs taken by the presenter unless otherwise attributed Purpose of the research . Develop a grazing industry perspective: Snapshot of what graziers and pastoralists think. Conservation for enterprise/income diversification? What conservation models would work? Where? How? What are preferred contractual conditions? . Establish foundation for a strategic industry position on potential supply of environmental services. Enhance the ability of potential investors to understand the needs of pastoralists. Support market formation and negotiations about the provision of contractual biodiversity conservation by pastoralists. Research area Bioregions as per colloquial reference but aligned with interim biogeographic regionalisation for Australia, version 7 (DE, 2013); E.U.=’Einasleigh Uplands’; V.R.D.=’Victoria River District’. ‘Einasleigh Uplands’ also includes directly adjacent areas of Cape York and Desert Uplands; ‘Gulf Plains’ also includes Mount Isa Inlier and parts of Mitchell Grass Downs; ‘Barkly’ comprises western parts of Mitchell Grass Downs, Davenport Murchison Ranges and eastern parts of Tanami; ‘Sturt’ also includes western parts of Gulf Falls and Uplands; Victoria River District’ comprises Ord Victoria Plain and Victoria Bonaparte; ‘Kimberley’ comprises Northern Kimberley, Central Kimberley and Dampierland. Survey response Total QLD NT WA (n=104) (n=61) (n=25) (n=18) Property
    [Show full text]
  • Australia's 89 Bioregions (PDF
    ARC Arnhem Coast ARP Arnhem Plateau TIW AUA Australian Alps AVW Avon Wheatbelt BBN Brigalow Belt North DARWIN ! ARC BBS Brigalow Belt South BEL Ben Lomond ITI DAC PCK ARP BHC Broken Hill Complex CEA BRT Burt Plain CAR Carnarvon ARC CEA Central Arnhem DAB CYP CEK Central Kimberley CER Central Ranges NOK VIB CHC Channel Country CMC Central Mackay Coast GUC COO Coolgardie GFU STU COP Cobar Peneplain COS Coral Sea CEK CYP Cape York Peninsula OVP DAB Daly Basin DAC Darwin Coastal DAL WET GUP EIU DAL Dampierland DEU Desert Uplands DMR Davenport Murchison Ranges COS DRP Darling Riverine Plains DMR TAN EIU Einasleigh Uplands MII ESP Esperance Plains GSD EYB Eyre Yorke Block FIN Finke FLB Flinders Lofty Block CMC FUR Furneaux BRT GAS Gascoyne PIL DEU GAW Gawler MGD BBN GES Geraldton Sandplains GFU Gulf Fall and Uplands MAC GID Gibson Desert LSD GID GSD Great Sandy Desert GUC Gulf Coastal GUP Gulf Plains CAR GAS CER FIN CHC GVD Great Victoria Desert HAM Hampton ITI Indian Tropical Islands SSD JAF Jarrah Forest KAN Kanmantoo KIN King GVD LSD Little Sandy Desert STP BBS MUR SEQ MAC MacDonnell Ranges MUL MAL Mallee ! BRISBANE MDD Murray Darling Depression YAL MGD GES Mitchell Grass Downs STP MII Mount Isa Inlier MUL Mulga Lands NUL MUR Murchison NAN Nandewar GAW NET NCP Naracoorte Coastal Plain SWA COO NAN NET New England Tablelands AVW HAM BHC DRP NNC NSW North Coast FLB NOK Northern Kimberley ! COP PERTH NSS NSW South Western Slopes MDD NNC NUL Nullarbor MAL EYB OVP Ord Victoria Plain PCK Pine Creek JAF ESP SYB PSI PIL Pilbara ADELAIDE ! ! PSI Pacific
    [Show full text]
  • Taxonomic Assessment of Diporiphora (Reptilia: Agamidae) Dragon Lizards from the Western Arid Zone of Australia
    Zootaxa 3518: 1–24 (2012) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA Copyright © 2012 · Magnolia Press Article ISSN 1175-5334 (online edition) urn:lsid:zoobank.org:pub:45D8F963-B9CA-4386-B54D-6C6E6AE72C63 Taxonomic assessment of Diporiphora (Reptilia: Agamidae) dragon lizards from the western arid zone of Australia PAUL DOUGHTY1,3, LUKE KEALLEY1 & JANE MELVILLE2 1Department of Terrestrial Zoology, Western Australian Museum, 49 Kew St, Welshpool, Western Australia, Australia. 2 Department of Sciences, GPO Box 666, Museum Victoria, Melbourne, Victoria, Australia 3Corresponding author email: [email protected] Abstract Members of the genus Diporiphora are slender perching agamid lizards from Australasia, with a conservative morphology and some outstanding taxonomic issues. Here we assess morphological variation in the morphologically similar D. pin- dan, D. valens, and D. winneckei from the western deserts of Australia. A reassessment of morphological differences that included the presence or absence of a gular fold, revealed D. pindan to be much more widely distributed than previously thought, occurring as far south as the northern Pilbara and east to the Tanami Desert. Examination of D. valens specimens revealed a north-south split within the Pilbara, with specimens conspecific with the types from the Hamersley Range in the southern Pilbara, whereas recently collected specimens from the Chichester and Roebourne regions in the northern Pilbara differ morphologically, and are described as a new species. Examination of the type of D. winneckei and topotypic material indicates that populations referable to this species are confined to the eastern arid zone. The isolated far western population of ‘D. winneckei’ from the Carnarvon Basin differs in morphology from the eastern arid zone D.
    [Show full text]
  • Using Generalised Dissimilarity Modelling and Targeted Field Surveys to Gap-Fill an Ecosystem Surveillance Network
    bioRxiv preprint doi: https://doi.org/10.1101/2020.06.01.107391; this version posted June 2, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. 1 Using generalised dissimilarity modelling and targeted field surveys 2 to gap-fill an ecosystem surveillance network 3 4 Greg R. Guerin1,2*, Kristen J. Williams3, Emrys Leitch1,2, Andrew J. Lowe1, Ben Sparrow1,2 5 6 1School of Biological Science, The University of Adelaide, Adelaide, South Australia 5005, 7 Australia 8 2Terrestrial Ecosystem Research Network 9 3CSIRO Land and Water, Canberra, Australian Capital Territory 2601, Australia 10 11 *Email: [email protected] 12 1 bioRxiv preprint doi: https://doi.org/10.1101/2020.06.01.107391; this version posted June 2, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. 13 Abstract 14 1. When considering which sites or land parcels complement existing conservation or 15 monitoring networks, there are many strategies for optimising ecological coverage in the 16 absence of ground observations. However, such optimisation is often implemented 17 theoretically in conservation prioritisation frameworks and real-world implementation is 18 rarely assessed, particularly for networks of monitoring sites. 19 2. We assessed the performance of adding new survey sites informed by predictive modelling 20 in gap-filling the ecological coverage of the Terrestrial Ecosystem Research Network’s 21 (TERN) continental network of ecosystem surveillance plots, Ausplots.
    [Show full text]
  • Part B: Terrestrial Environments Overview
    Part B: Terrestrial Environments Norm McKenzie, Tony Start, Andrew Burbidge, Kevin Kenneally and Neil Burrows Overview The Kimberley extends from sub-humid to semi-arid areas and covers a variety of different geological basements. These differences are reflected in the distinctive geomorphologies, soil, landscapes and biotas of the north, central, south and eastern Kimberley, and have determined their different land-use histories and contemporary land condition. In these terms, five biogeographical regions (10 subregions) are recognised in the Kimberley (Thackway and Cresswell 1995, McKenzie et al. 2003), that provide a framework for planning and action. In this section, we review the information base then characterise the bioregions to identify their different contributions to Kimberley diversity (treated here as a mosaic of regional ecosystems). Then we summarise the biodiversity values of Kimberley ecosystems and identify special features, communities, clades and species that should be a particular focus for management because of rarity, special value, vulnerability or imminent risk. Next, we review the condition and trend of the ecosystems in each bioregion, and provide a schematic model of the soil nutrient, hydrological and inter-species processes that maintain the compositional diversity of savanna because it is the matrix in which all of the Kimberley’s other ecosystems and special features are set. Finally, we identify priority management needs, particularly strategic actions that will mitigate degrading processes throughout the Kimberley and protect or rehabilitate whole suites of ecosystems and species. Healthy country is more productive, both in economic and biodiversity terms (Whitehead et al. 2000, Start 2003). The most cost effective conservation strategy is to protect, restore and maintain functional landscapes and systems, rather than trying to preserve small remnants or focussing only on localised, patch-scale remedial actions such as site restoration.
    [Show full text]
  • Multi-Locus Phylogeny and Taxonomic Revision of Uperoleia Toadlets
    Zootaxa 2902: 1–43 (2011) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2011 · Magnolia Press ISSN 1175-5334 (online edition) Multi-locus phylogeny and taxonomic revision of Uperoleia toadlets (Anura: Myobatrachidae) from the western arid zone of Australia, with a description of a new species RENEE A. CATULLO1,4, PAUL DOUGHTY2, J. DALE ROBERTS3 & J. SCOTT KEOGH1 1Evolution, Ecology & Genetics, Research School of Biology, The Australian National University, Canberra, ACT, 0200 AUSTRALIA 2Department of Terrestrial Zoology, Western Australian Museum, 49 Kew Street, Welshpool WA 6106, AUSTRALIA 3School of Animal Biology M092, University of Western Australia, nedlands, WA 6009, AUSTRALIA 4Corresponding author. E-mail: [email protected] Table of contents Abstract . 1 Introduction . 2 Results . 6 Molecular analyses . 6 Morphology. 10 Advertisement calls . 12 Taxonomy . 14 Uperoleia Gray, 1841 . 15 Uperoleia glandulosa Davies, Mahony, and Roberts, 1985 . 15 Uperoleia micromeles Tyler, Davies and Martin, 1981 . 17 Uperoleia russelli (Loveridge, 1933) . 19 Uperoleia talpa Tyler, Davies, and Martin, 1981 . 21 Uperoleia saxatilis sp. nov. 23 Discussion . 25 Acknowledgements . 27 References . 27 Appendix . 29 Abstract We generated a multi-locus phylogeny to test monophyly and distributional limits in Australian toadlets of the genus Up- eroleia from the western arid zone of Australia. The molecular data were used in combination with a detailed assessment of morphological variation and some data on call structure to complete a taxonomic revision of the species that occur in this region. Our work reveals the existence of not two but five species in the region. Uperoleia russelli is restricted to the Carnarvon and Gascoyne Regions south of the Pilbara.
    [Show full text]
  • Kimberley Science and Conservation Strategy Kimberley Science and Conservation Strategy
    Kimberley Science and Conservation Strategy Kimberley Science and Conservation Strategy © Government of Western Australia May 2011 Foreword Western Australia’s vast Kimberley region is renowned international profile and increasing visitor numbers as well for its natural beauty and enormous cultural significance. as a growing population. A strategy that recognises this Awareness of its economic, cultural and biological values growth, and sets a path to conserve the region’s natural and is rapidly increasing across Australia and around the world. cultural values, is vital. It is a region filled with beauty and mystique, containing unique terrestrial and marine ecosystems, set in wild, The State Government has met this challenge by rugged and remote landscapes. developing a comprehensive Kimberley Science and Conservation Strategy and committing an initial $63 million Central to the Kimberley’s past, present and future is a over the five years to 2015 to implement it. Ongoing rich and living Aboriginal culture. Aboriginal people retain funding will be provided for key initiatives, including marine strong links to and responsibility for country, and they have park management and landscape-scale fire, feral animal and a key role in protecting the Kimberley’s cultural and natural weed control. This is a major investment in conserving the heritage. Archaeological sites in the Kimberley are amongst region’s unique values and providing new opportunities for the oldest in Australia and offer unparalleled opportunities Aboriginal employment and for nature-based tourism. This to contribute to the history of Australia and to world funding is also expected to create significant opportunities human history. The region has the greatest diversity of rock to leverage cash and in-kind funding from a wide array of art in Australia.
    [Show full text]
  • Interim Biogeographic Regionalisation for Australia, Version 7 Data Used Are Assumed to Be Correct As Received from the Data Suppliers
    ARC Arnhem Coast ARP Arnhem Plateau TIW AUA Australian Alps AVW Avon Wheatbelt DARWIN BBN Brigalow Belt North ARC BBS Brigalow Belt South BEL Ben Lomond ITI DAC PCK ARP BHC Broken Hill Complex CEA BRT Burt Plain CAR Carnarvon ARC CEA Central Arnhem DAB CYP CEK Central Kimberley CER Central Ranges NOK VIB CHC Channel Country CMC Central Mackay Coast GUC COO Coolgardie GFU STU COP Cobar Peneplain COS Coral Sea CEK CYP Cape York Peninsula OVP DAB Daly Basin DAC Darwin Coastal DAL WET GUP EIU DAL Dampierland DEU Desert Uplands DMR Davenport Murchison Ranges COS DRP Darling Riverine Plains DMR TAN EIU Einasleigh Uplands MII ESP Esperance Plains GSD EYB Eyre Yorke Block FIN Finke FLB Flinders Lofty Block CMC FUR Furneaux BRT GAS Gascoyne PIL DEU GAW Gawler MGD BBN GES Geraldton Sandplains GFU Gulf Fall and Uplands MAC GID Gibson Desert LSD GID GSD Great Sandy Desert GUC Gulf Coastal GUP Gulf Plains CAR GAS CER FIN CHC GVD Great Victoria Desert HAM Hampton ITI Indian Tropical Islands SSD JAF Jarrah Forest KAN Kanmantoo KIN King GVD LSD Little Sandy Desert STP BBS MUR SEQ MAC MacDonnell Ranges MUL BRISBANE MAL Mallee MDD Murray Darling Depression YAL MGD GES Mitchell Grass Downs STP MII Mount Isa Inlier MUL Mulga Lands NUL MUR Murchison NAN Nandewar GAW NET NCP Naracoorte Coastal Plain SWA COO NAN NET New England Tablelands AVW HAM BHC DRP NNC NSW North Coast FLB NOK Northern Kimberley PERTH COP NSS NSW South Western Slopes MDD NNC NUL Nullarbor MAL EYB OVP Ord Victoria Plain PCK Pine Creek JAF ESP SYB PIL Pilbara ADELAIDE SYDNEY PSI PSI Pacific
    [Show full text]