Approved Conservation Advice for Phascogale Calura (Red-Tailed Phascogale)
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Broken Hill Complex
Broken Hill Complex Bioregion resources Photo Mulyangarie, DEH Broken Hill Complex The Broken Hill Complex bioregion is located in western New South Wales and eastern South Australia, spanning the NSW-SA border. It includes all of the Barrier Ranges and covers a huge area of nearly 5.7 million hectares with approximately 33% falling in South Australia! It has an arid climate with dry hot summers and mild winters. The average rainfall is 222mm per year, with slightly more rainfall occurring in summer. The bioregion is rich with Aboriginal cultural history, with numerous archaeological sites of significance. Biodiversity and habitat The bioregion consists of low ranges, and gently rounded hills and depressions. The main vegetation types are chenopod and samphire shrublands; casuarina forests and woodlands and acacia shrublands. Threatened animal species include the Yellow-footed Rock- wallaby and Australian Bustard. Grazing, mining and wood collection for over 100 years has led to a decline in understory plant species and cover, affecting ground nesting birds and ground feeding insectivores. 2 | Broken Hill Complex Photo by Francisco Facelli Broken Hill Complex Threats Threats to the Broken Hill Complex bioregion and its dependent species include: For Further information • erosion and degradation caused by overgrazing by sheep, To get involved or for more information please cattle, goats, rabbits and macropods phone your nearest Natural Resources Centre or • competition and predation by feral animals such as rabbits, visit www.naturalresources.sa.gov.au -
Tanami Desert 1
Tanami Desert 1 Tanami Desert 1 (TAN1 – Tanami 1 subregion) GORDON GRAHAM SEPTEMBER 2001 Subregional description and The Continental Stress Class for TAN1 is 5. biodiversity values Known special values in relation to landscape, ecosystem, species and genetic values Description and area There are no known special values within TAN1. Mainly red Quaternary sandplains overlying Permian and Proterozoic strata that are exposed locally as hills and Existing subregional or bioregional plans and/or ranges. The sandplains support mixed shrub steppes of systematic reviews of biodiversity and threats Hakea spp., desert bloodwoods, Acacia spp. and Grevillea spp. over soft spinifex (Triodia pungens) hummock The CTRC report in 1974 (System 7) formed the basis grasslands. Wattle scrub over soft spinifex (T. pungens) of the Department’s publication “Nature Conservation hummock grass communities occur on the ranges. Reserves in the Kimberley” (Burbidge et al. 1991) which Alluvial and lacustrine calcareous deposits occur has itself been incorporated in a Departmental Draft throughout. In the north they are associated with Sturt Regional Management Plan (Portlock et al. 2001). These Creek drainage, and support ribbon grass (Chrysopogon reports were focused on non-production lands and those spp.) and Flinders grass (Iseilema spp.) short-grasslands areas not likely to be prospective for minerals. Action often as savannas with river red gum. The climate is arid statements and strategies in the draft regional tropical with summer rain. Subregional area is 3, 214, management plan do not go to the scale of subregion or 599ha. even bioregion. Dominant land use Apart from specific survey work there has been no systematic review of biodiversity but it is apparent that The dominant land use is (xi) UCL and Crown reserves there are on-going changes to the status of fauna (see Appendix B, key b). -
PRINCESS PARROT Polytelis Alexandrae
Threatened Species of the Northern Territory PRINCESS PARROT Polytelis alexandrae Conservation status Australia: Vulnerable Northern Territory: Vulnerable Princess parrot. ( Kay Kes Description Conservation reserves where reported: The princess parrot is a very distinctive bird The princess parrot is not resident in any which is slim in build, beautifully plumaged conservation reserve in the Northern and has a very long, tapering tail. It is a Territory but it has been observed regularly in medium-sized parrot with total length of 40- and adjacent to Uluru Kata Tjuta National 45 cm and body mass of 90-120 g. The basic Park, and there is at least one record from colour is dull olive-green; paler on the West MacDonnell National Park. underparts. It has a red bill, blue-grey crown, pink chin, throat and foreneck, prominent yellow-green shoulder patches, bluish rump and back, and blue-green uppertail. Distribution This species has a patchy and irregular distribution in arid Australia. In the Northern Territory, it occurs in the southern section of the Tanami Desert south to Angas Downs and Yulara and east to Alice Springs. The exact distribution within this range is not well understood and it is unclear whether the species is resident in the Northern Territory. Few locations exist in the Northern Territory where the species is regularly seen, and even Known locations of the princess parrot. then there may be long intervals (up to 20 years) between records. Most records from = pre 1970; • = post 1970. the MacDonnell Ranges bioregion are during dry periods. For more information visit www.denr.nt.gov.au Ecology • extreme fluctuations in number of mature individuals. -
Aborigines and the Administration of Social Welfate in Central Australia
j8 BURNJNG MT. KETLY: ABORIGTNËS AND']]IIII AD}IINISTRATÏON OF SOCTAL b]ETù-ARE TN CET'ITRAI, AUST'R.ALTA JEFFREY REf D COLLMANN, B '4. M"A. (ECON" ) Department of AnthropologY The UniversitY of Adelaide 23rd I'lay, L979 J- TABLB OF CONTENTS Tit1e page Tabl-e of Contents t Brief Summary l-t Disclaimer ].V Acknov¡Led.gements V Introduction I Chapter I The Policy of "Self-d.etermination" ancl the Fraqmentation of Aboriginal A<lministratjon i,n Cent-ral Austral-ia L4 Chapter 2 Racial Tensic¡n ancl the Politics of Detriba lization 46 Chapter 3 Frirrge-camps and the Development of Abori.ginaI Adrnj-njstr:ation in Central Aust-ralia oa Chapter 4 lr]c¡men, Childrett, and the Siqni.ficance of the Domestic Group to Ur:l¡arr Aborigines in Central Australi a 127 Chap-Ler 5 Men, Vüork, and the Significance of the Cattle Industry to Urban Fr-inge-Cwel-lers in Central Australia l5:6 Chapter 6 Food, Liquor, and Domestic Credit: A Theory of Drinking among Fringe-dwellers i.n Central Austra l.ia I86 Chapter 7 Violenc,e, Debt and the Negotiat-íon cf Exchatrge 21.r Chapter 8 Conclusirln 256 Appendix J. The Strr¡et-,ure alrd Development of the Centl:a1 Ar:stral-ian Cattle Industry 286 Apper-iCix IT l'lork Careers of Mt" Kelly Aclul.ts 307 Bibliography 308 t1 BRIEF SUMMARY This thesis i.s a general analysis of the structure of social relatícnships between Aborigines and whites in Central Australia. Of particular importance .t. tfr. -
Phylogenetic Structure of Vertebrate Communities Across the Australian
Journal of Biogeography (J. Biogeogr.) (2013) 40, 1059–1070 ORIGINAL Phylogenetic structure of vertebrate ARTICLE communities across the Australian arid zone Hayley C. Lanier*, Danielle L. Edwards and L. Lacey Knowles Department of Ecology and Evolutionary ABSTRACT Biology, Museum of Zoology, University of Aim To understand the relative importance of ecological and historical factors Michigan, Ann Arbor, MI 48109-1079, USA in structuring terrestrial vertebrate assemblages across the Australian arid zone, and to contrast patterns of community phylogenetic structure at a continental scale. Location Australia. Methods We present evidence from six lineages of terrestrial vertebrates (five lizard clades and one clade of marsupial mice) that have diversified in arid and semi-arid Australia across 37 biogeographical regions. Measures of within-line- age community phylogenetic structure and species turnover were computed to examine how patterns differ across the continent and between taxonomic groups. These results were examined in relation to climatic and historical fac- tors, which are thought to play a role in community phylogenetic structure. Analyses using a novel sliding-window approach confirm the generality of pro- cesses structuring the assemblages of the Australian arid zone at different spa- tial scales. Results Phylogenetic structure differed greatly across taxonomic groups. Although these lineages have radiated within the same biome – the Australian arid zone – they exhibit markedly different community structure at the regio- nal and local levels. Neither current climatic factors nor historical habitat sta- bility resulted in a uniform response across communities. Rather, historical and biogeographical aspects of community composition (i.e. local lineage per- sistence and diversification histories) appeared to be more important in explaining the variation in phylogenetic structure. -
A New Genus of Scolopendrid Centipede (Chilopoda: Scolopendromorpha: Scolopendrini) from the Central Australian Deserts
Zootaxa 3321: 22–36 (2012) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2012 · Magnolia Press ISSN 1175-5334 (online edition) A new genus of scolopendrid centipede (Chilopoda: Scolopendromorpha: Scolopendrini) from the central Australian deserts JULIANNE WALDOCK1 & GREGORY D. EDGECOMBE2 1Department of Terrestrial Zoology, Western Australian Museum, Locked Bag 49, Welshpool, WA 6986, Australia. E-mail: [email protected] 2The Natural History Museum, Department of Palaeontology, Cromwell Road, London SW7 5BD, United Kingdom. E-mail: [email protected] Abstract The first new species of Scolopendridae discovered in Australia since L.E. Koch’s comprehensive revision in the 1980s is named as a new monotypic genus of the Tribe Scolopendrini, Kanparka leki n. gen. n. sp. Its distribution includes the Gibson and Little Sandy Deserts in Western Australia and the western part of the Tanami Desert in the Northern Territory. The new genus is especially distinguished from other scolopendrines by the spinulation of its robust ultimate legs, partic- ular the presence of spines on the femur and tibia in addition to the predominantly irregularly scattered spines on the prefe- mur. Cladistic analysis based on morphological characters resolves Kanparka in a clade with Scolopendra, Arthrorhabdus, Akymnopellis and Hemiscolopendra, within which Scolopendra is non-monophyletic. Key words: Centipedes, Scolopendridae, Western Australia, Northern Territory, taxonomy, phylogeny Introduction The scolopendrid centipedes of Australia were revised in a series of studies by L.E. Koch that drew upon Austra- lian museum collections amassed during survey programs in the 1960s through early 1980s, as well as historical material. -
GREAT DESERT SKINK TJAKURA Egernia Kintorei
Threatened Species of the Northern Territory GREAT DESERT SKINK TJAKURA Egernia kintorei Conservation status Australia: Vulnerable Northern Territory: Vulnerable Photo: Steve McAlpin Description southern sections of the Great Sandy Desert of Western The great desert skink is a large, smooth bodied lizard with an average snout-vent length of 200 mm (maximum of 440 mm) and a body mass of up to 350 g. Males are heavier and have broader heads than females. The tail is slightly longer than the snout-vent length. The upperbody varies in colour between individuals and can be bright orange- brown or dull brown or light grey. The underbody colour ranges from bright lemon- yellow to cream or grey. Adult males often have blue-grey flanks, whereas those of females and juveniles are either plain brown or vertically barred with orange and cream. Known locations of great desert skink. Distribution The great desert skink is endemic to the Australia. Its former range included the Great Australian arid zone. In the Northern Territory Victoria Desert, as far west as Wiluna, and the (NT), most recent records (post 1980) come Northern Great Sandy Desert. from the western deserts region from Uluru- Conservation reserves where reported: Kata Tjuta National Park north to Rabbit Flat in the Tanami Desert. The Tanami Desert and Uluru-Kata Tjuta National Park, Watarrka Uluru populations are both global strongholds National Park and Newhaven Reserve for the species. (managed for conservation by the Australian Wildlife Conservancy). Outside the NT it occurs in North West South Australia and in the Gibson Desert and For more information visit www.denr.nt.gov.au Ecology qualifies as Vulnerable (under criteria C2a(i)) due to: The great desert skink occupies a range of • population <10,000 mature individuals; vegetation types with the major habitat being • continuing decline, observed, projected or sandplain and adjacent swales that support inferred, in numbers; and hummock grassland and scattered shrubs. -
Evidence of Altered Fire Regimes in the Western Desert Region of Australia
272 Conservation Science W. Aust. 5 (3)N.D. : 272–284 Burrows (2006) et al. Evidence of altered fire regimes in the Western Desert region of Australia N.D. BURROWS1, A.A. BURBIDGE2, P.J. FULLER3 AND G. BEHN1 1Department of Conservation and Land Management, Locked Bag 104, Bentley Delivery Centre, Bentley, Western Australia, 6983. 2Department of Conservation and Land Management, Western Australian Wildlife Research Centre, P.O. Box 51, Wanneroo, Western Australia, 6946. 33 Willow Rd, Warwick, Western Australia, 6024. SUMMARY and senescing vegetation or vast tracts of vegetation burnt by lightning-caused wildfires. The relatively recent exodus of Aboriginal people from parts of the Western Desert region of Australia has coincided with an alarming decline in native mammals INTRODUCTION and a contraction of some fire sensitive plant communities. Proposed causes of these changes, in what The Great Victoria, Gibson, Great Sandy and Little Sandy is an otherwise pristine environment, include an altered Deserts (the Western Desert) occupy some 1.6 million fire regime resulting from the departure of traditional km2 of Western Australia, of which more than 100 000 Aboriginal burning, predation by introduced carnivores km2 is managed for nature conservation. The and competition with feral herbivores. conservation reserves in the Western Desert are large, Under traditional law and custom, Aboriginal people remote and relatively undisturbed. A management option inherit, exercise and bequeath customary responsibilities for such reserves is not to intervene -
Verifying Bilby Presence and the Systematic
CSIRO PUBLISHING Australian Mammalogy Review https://doi.org/10.1071/AM17028 Verifying bilby presence and the systematic sampling of wild populations using sign-based protocols – with notes on aerial and ground survey techniques and asserting absence Richard Southgate A, Martin A. Dziminski B,E, Rachel Paltridge C, Andrew Schubert C and Glen Gaikhorst D AEnvisage Environmental Services, PO Box 305, Kingscote, SA 5223, Australia. BDepartment of Biodiversity, Conservation and Attractions, Western Australia, Woodvale Wildlife Research Centre, Locked Bag 104, Bentley Delivery Centre, WA 6983, Australia. CDesert Wildlife Services, PO Box 4002, Alice Springs, NT 0871, Australia. DGHD Pty Ltd, 999 Hay Street, Perth, WA 6004, Australia. ECorresponding author. Email: [email protected] Abstract. The recognition of sign such as tracks, scats, diggings or burrows is widely used to detect rare or elusive species. We describe the type of sign that can be used to confirm the presence of the greater bilby (Macrotis lagotis)in comparison with sign that should be used only to flag potential presence. Clear track imprints of the front and hind feet, diggings at the base of plants to extract root-dwelling larvae, and scats commonly found at diggings can be used individually, or in combination, to verify presence, whereas track gait pattern, diggings in the open, and burrows should be used to flag potential bilby activity but not to verify presence. A protocol to assess potential activity and verify bilby presence is provided. We provide advice on the application of a plot-based technique to systematically search for sign and produce data for the estimation of regional occupancy. -
Supplementary
Step 4: Interpretation We hope this approach has shorty Jangala robertson, Warlpiri, they unleashed a great thunderstorm enhanced your exploration and born about 1935, Yuendumu, Western that ultimately created the large un- Interpretation involves bringing enjoyment of this painting. If you desert, Northern territory derground wells that are represented your close observation, analysis, by the repeated concentric circles. A Closer Look like, you can try this method and any additional information Ngapa Jukurrpa—Puyurru with other works of art. simply these “water holes” provide both you have gathered about a work (Water Dreaming at Puyurru) physical and spiritual sustenance to ask yourself with each work: of art together to try to under- 2007 the region’s Warlpiri people. the long stand what it means. curving yellow lines in the painting What do I see? Acrylic on canvas Promised gift of Will owen and harvey represent the fast-flowing rivers that (Close observation) there can be multiple interpreta- Wagner; eL.2011.60.45 form after a heavy rain. the lines that tions of a work of art. the best- cross between the curving lines suggest What do I think? informed ones are based on visual the lightning and rain-making clouds. (Analysis) Aboriginal Australian painting is often the fields of colored dots allude to the evidence and accurate research. inspired by a particular place, but it flowering of the desert after the rain, How can I learn more? also represents, through a sophisticated but the energy that they create on the some interpretive questions to (research) visual language, ancient stories about surface of the canvas also suggests the consider for this painting might the ancestors who visited and shaped continual spiritual presence of the include the following: What might it mean? that place, information about how to Ancestors. -
Landscape Evolution in the Finke (Larapinta) River Transverse Drainage, Central Mountain Ranges, Australia
PL ISSN 0081-6434 studia geomorphologica carpatho-balcanica vol. lV, 2021 : 9– 44 VICTOR r. BAKer (tucson) LANDSCAPE EVOLUTION IN THE FINKE (LARAPINTA) RIVER TRANSVERSE DRAINAGE, CENTRAL MOUNTAIN RANGES, AUSTRALIA Abstract : the cross-axial pattern of the Finke (larapinta) river across the central ranges of- australia developed through a complex combination of processes including early planation;- deep weathering (late mesozoic/early cainozoic); long-term stream impression; etchplana- tion; progressive aridity, leading to late (pliocene and Quaternary) changes in fluvial flood reg imen; all associated with regressive river erosion, stream capture, and/or epeirogenic move ments. an early phase of etchplanation explains the development on easily weathered rocks of intramontane basins and strike valleys. combined with stream impression, this process led to the superposing of the Finke and the hugh rivers across resistant rock units. the most unusual aspect of the Finke is a palimpsest, developed in the Krichauff ranges, in which an ancient, relict gorge, is incised into a local planation surface (the shoulder surface), and preserved as- paleomeander segments, in which the original quartzite gravel fill has been cemented with iron oxides and silica. the shoulder surface was subsequently more deeply incised by a later mani festation of the river to produce the meandering contemporary gorge that is intertwined with the relict one. the incision of the contemporary gorge occurred in association with the change in flood regimen, and involved either (1) prior aggradation of the incised paleomeandering stream to permit alluvial meandering across the shoulder surface and subsequent incision into it, or (2) headward recession of a knick point created where the Finke flowed from resistant sandstones into what are now the strike valleys of the James ranges, from which weathered mantlesKeywords had been removed by etchplanation processes. -
Human Refugia in Australia During the Last Glacial Maximum and Terminal Pleistocene: a Geospatial Analysis of the 25E12 Ka Australian Archaeological Record
Journal of Archaeological Science 40 (2013) 4612e4625 Contents lists available at SciVerse ScienceDirect Journal of Archaeological Science journal homepage: http://www.elsevier.com/locate/jas Human refugia in Australia during the Last Glacial Maximum and Terminal Pleistocene: a geospatial analysis of the 25e12 ka Australian archaeological record Alan N. Williams a,*, Sean Ulm b, Andrew R. Cook c, Michelle C. Langley d, Mark Collard e a Fenner School of Environment and Society, The Australian National University, Building 48, Linnaeus Way, Canberra, ACT 0200, Australia b Department of Anthropology, Archaeology and Sociology, School of Arts and Social Sciences, James Cook University, PO Box 6811, Cairns, QLD 4870, Australia c School of Biological, Earth and Environmental Sciences, The University of New South Wales, NSW 2052, Australia d Institute of Archaeology, University of Oxford, Oxford OX1 2PG, United Kingdom e Human Evolutionary Studies Program and Department of Archaeology, Simon Fraser University, Burnaby, British Columbia, Canada article info abstract Article history: A number of models, developed primarily in the 1980s, propose that Aboriginal Australian populations Received 13 February 2013 contracted to refugia e well-watered ranges and major riverine systems e in response to climatic Received in revised form instability, most notably around the Last Glacial Maximum (LGM) (w23e18 ka). We evaluate these 3 June 2013 models using a comprehensive continent-wide dataset of archaeological radiocarbon ages and geospatial Accepted 17 June 2013 techniques. Calibrated median radiocarbon ages are allocated to over-lapping time slices, and then K-means cluster analysis and cluster centroid and point dispersal pattern analysis are used to define Keywords: Minimum Bounding Rectangles (MBR) representing human demographic patterns.