Wetlands of the Great Artesian Basin Water Control District (Northern Territory)
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Lake Pinaroo Ramsar Site
Ecological character description: Lake Pinaroo Ramsar site Ecological character description: Lake Pinaroo Ramsar site Disclaimer The Department of Environment and Climate Change NSW (DECC) has compiled the Ecological character description: Lake Pinaroo Ramsar site in good faith, exercising all due care and attention. DECC does not accept responsibility for any inaccurate or incomplete information supplied by third parties. No representation is made about the accuracy, completeness or suitability of the information in this publication for any particular purpose. Readers should seek appropriate advice about the suitability of the information to their needs. © State of New South Wales and Department of Environment and Climate Change DECC is pleased to allow the reproduction of material from this publication on the condition that the source, publisher and authorship are appropriately acknowledged. Published by: Department of Environment and Climate Change NSW 59–61 Goulburn Street, Sydney PO Box A290, Sydney South 1232 Phone: 131555 (NSW only – publications and information requests) (02) 9995 5000 (switchboard) Fax: (02) 9995 5999 TTY: (02) 9211 4723 Email: [email protected] Website: www.environment.nsw.gov.au DECC 2008/275 ISBN 978 1 74122 839 7 June 2008 Printed on environmentally sustainable paper Cover photos Inset upper: Lake Pinaroo in flood, 1976 (DECC) Aerial: Lake Pinaroo in flood, March 1976 (DECC) Inset lower left: Blue-billed duck (R. Kingsford) Inset lower middle: Red-necked avocet (C. Herbert) Inset lower right: Red-capped plover (C. Herbert) Summary An ecological character description has been defined as ‘the combination of the ecosystem components, processes, benefits and services that characterise a wetland at a given point in time’. -
Following the Finke: a Modern Expedition Down the River of Time
FOLLOWING THE FINKE FOLLOWING THE FINKE: A MODERN EXPEDITION DOWN THE RIVER OF TIME PART I: TRAVERSING AN ANCIENT LAND DR KATE LEEMING HOPS ON HER CUSTOM-MADE BIKE TO TAKE ON THE AUSTRALIAN INTERIOR. WORDS AND PICS: KATE LEEMING Back in 2004, during my 25,000km Great for the local Aboriginal people and wildlife, unpredictable surfaces requires a similar skill Australian Cycle Expedition (GRACE), in the present day and for eons past. If Uluru set to pedalling over snow. My ‘Following the cycling companion Greg Yeoman and symbolises the nation’s heart, then the Finke Finke River’ expedition therefore would double I camped beside the Finke River near to River, or Larapinta as it is known to the local as a credible expedition in its own right and where it intersects with the Stuart Highway. Arrernte, must surely be its ancient artery. as excellent physical and mental training for We were on our way to Uluru and beyond This is where the germ of my idea to travel cycling across Antarctica. and the Finke River crossing was at the end the course of the Finke River evolved, however The Finke originates about 130km west of of our first day’s ride south of Alice Springs. the concept of biking along the sandy and Alice Springs in the West MacDonnell Ranges, I’d aimed to reach this point because I stony bed of the ephemeral river at that time the remnants of an ancient system of fold wanted to experience camping beside was an impossibility. A decade later, the mountains that was once on the scale of the what is commonly referred to as the world’s development of fatbike technology began Himalayas, but has now diminished to be a oldest river. -
ACT Flood Watch Areas
! ! ! ! Barkly Warrego Flood Watch Area No. ! Homestead Ayr ! ! Tennant Roadhouse Angas and Brem!er Rivers 28 Flood Watch Areas ! Home Balgo Creek Camooweal Charters ! Broughton RivHeirll 19 ! Hill !Towers South Australia ! Cooper Creek Bowen 7 ! Mount Julia Danggali Rivers and CCreolelinkssville Prose1rp7ine Creek ! NT Isa Cloncurry ! ! ! Diamantina River 3 !Hughenden Eastern Eyre Peninsula 18 Stamford MACKAY " Telfer ! Eastern Great Victoria Desert 9 ! Sarina ! Finke River and Stephenson Creek 5 Fleurieu Peninsula 29 !Moranbah Flinders Ranges Rivers Cotton Yuendumu 1 ! Winton 15 Creek ! and Creeks ! Dysart Gawler River ! 24 Clermont Boulia ! ! Georgina River and Eyre Creek 1 Papunya ! Kangaroo Island 30 !Longreach Alice Lake Eyre !Emerald 10 Springs !Alpha WA ! 2 Lake Frome 11 Hermannsburg ! Santa 3 Lake Gairdner Springsure 12 !Teresa ! Light and Wakefield Rivers 21 Docker River QLD Limestone and (Kaltukatjara) 31 ! M!iTllaicmebnot Coast Rivers and Creeks Erldunda Lower Eyre Peninsula 22 ! ! Yulara Tourist Village 4 Windorah ! North West Lake Torrens 14 ! Carnegie NullarbAougr aDthiesltlarict Rivers 13 ! Birdsville ! ! Onkaparinga River 27 Warburton! ! River Murray Murraylands 26 Amata 5 Charleville ! Mitchell River Murray Riverlands! Rom20a !Quilpie ! Simpson Desert 4 Tjukayirla 6 Roadhouse Torrens and metropolitan rivers Surat ! 2!5 and creeks ! 7 Warburton District Rivers 6 Innamincka Oodnadatta 8 ! Warburton River 8 !Thargomindah St George West Coast Rivers and Creeks ! 16 Ilkurlka ! 9 Western Desert 2 Dirranbandi !Laverton ! Coober -
Final Report Template
Native Legumes as a Grain Crop for Diversification in Australia RIRDC Publication No. 10/223 RIRDCInnovation for rural Australia Native Legumes as a Grain Crop for Diversification in Australia by Megan Ryan, Lindsay Bell, Richard Bennett, Margaret Collins and Heather Clarke October 2011 RIRDC Publication No. 10/223 RIRDC Project No. PRJ-000356 © 2011 Rural Industries Research and Development Corporation. All rights reserved. ISBN 978-1-74254-188-4 ISSN 1440-6845 Native Legumes as a Grain Crop for Diversification in Australia Publication No. 10/223 Project No. PRJ-000356 The information contained in this publication is intended for general use to assist public knowledge and discussion and to help improve the development of sustainable regions. You must not rely on any information contained in this publication without taking specialist advice relevant to your particular circumstances. While reasonable care has been taken in preparing this publication to ensure that information is true and correct, the Commonwealth of Australia gives no assurance as to the accuracy of any information in this publication. The Commonwealth of Australia, the Rural Industries Research and Development Corporation (RIRDC), the authors or contributors expressly disclaim, to the maximum extent permitted by law, all responsibility and liability to any person, arising directly or indirectly from any act or omission, or for any consequences of any such act or omission, made in reliance on the contents of this publication, whether or not caused by any negligence on the part of the Commonwealth of Australia, RIRDC, the authors or contributors. The Commonwealth of Australia does not necessarily endorse the views in this publication. -
Munga-Thirri–Simpson Desert Conservation Park and Regional Reserve
<iframe src="https://www.googletagmanager.com/ns.html?id=GTM-5L9VKK" height="0" width="0" style="display:none;visibility:hidden"></iframe> Munga-Thirri–Simpson Desert Conservation Park and Regional Reserve About Check the latest Desert Parks Bulletin (https://cdn.environment.sa.gov.au/parks/docs/desert-parks-bulletin- 30092021.pdf) before visiting this park. Located within the driest region of the Australian continent, the Munga-Thirri–Simpson Desert Conservation Park is in the centre of the Simpson Desert, one of the world's best examples of parallel dunal desert. The Simpson Desert's sand dunes stretch over hundreds of kilometres and lie across the corners of three states - South Australia, Queensland and the Northern Territory. The Munga-Thirri–Simpson Desert Regional Reserve, just outside the Conservation Park, features a wide variety of desert wildlife preserved in a landscape of varied dune systems, extensive playa lakes, spinifex grasslands and acacia woodlands. The reserve links the Munga-Thirri–Simpson Desert Conservation Park to Witjira National Park. Simpson Desert parks in South Australia and Queensland are closed in summer from 1 December to 15 March. Vehicles are required to have high visibility safety flags (#safety) attached to the front of the vehicle. Opening hours Open daily. Munga-Thirri–Simpson Desert Conservation Park and Regional Reserve are closed from 1 December to 15 March each year. Access may be restricted due to local road conditions. Please refer to the latest Desert Parks Bulletin (https://cdn.environment.sa.gov.au/parks/docs/desert-parks-bulletin-30092021.pdf) for current access and road condition information. Closures and safety This park is closed on days of Catastrophic Fire Danger and may also be closed on days of Extreme Fire Danger. -
Dusky Hopping Mouse
Threatened Species of the Northern Territory DUSKY HOPPING-MOUSE Notomys fuscus Conservation status Australia: Vulnerable Northern Territory: Endangered Photo: P. Canty Description as Ooldea in South Australia and east to the Victoria/New South Wales borders. The dusky hopping-mouse is characterized by its strong incisor teeth, long tail, large ears, The species has not been recorded in the dark eyes, and extremely lengthened and Northern Territory since 1939 when it was narrow hind feet, which have only four pads collected in sand dunes on Maryvale Station on the sole. The head-body length is 91-177 and on Andado Station. An earlier record is mm, tail length is 125-225 mm, and body from Charlotte Waters. weight is about 20-50 g. Coloration of the Conservation reserves where reported: upper parts varies from pale sandy brown to None. yellowish brown to ashy brown or greyish. The underparts of dusky hopping-mice are white. The fur is fine, close and soft. Long hairs near the tip of the tail give the effect of a brush. The dusky hopping-mouse has a well- developed glandular area on the underside of its neck or chest. Females have four nipples. Distribution The current distribution of the dusky hopping-mouse appears to be restricted to the eastern Lake Eyre Basin within the Known locations of the dusky hopping-mouse Simpson-Strzelecki Dunefields bioregion in (ο = pre 1970). South Australia and Queensland. An intensive survey in the 1990s located populations at Ecology eight locations in the Strzelecki Desert and adjacent Cobbler Sandhills (South Australia) The dusky hopping-mouse occupies a variety and in south-west Queensland (Moseby et al. -
Arabunna Minerals Exploration ILUA Description of External Boundary
SI2003/008 - Arabunna Minerals Exploration ILUA Description of External Boundary Area of ILUA (geographic extent) = 34,460 sq km The Agreement Area commences on the northeastern corner of Coorikiana Pastoral Lease, then extends easterly, northerly, again easterly and again northerly along the boundaries of Todmorden Pastoral Lease, being also the boundaries of native title determination application SG6025/98 – “The Arabunna People’s Native Title Claim” (SC98/2), to Latitude 27.370907° South; then, along the boundaries of that claim, north easterly through coordinate point Longitude 135.685875° East, Latitude 27.216449° South, to the centreline of Macumba River (approximated by Longitude 135.717429° East, Latitude 27.205415° South), being also the boundary of native title determination application SG6016/98 – “The Wangkangurru/Yarluyandi Native Title Claim” (SC97/3). Then generally easterly and southeasterly along the centrelines of the Macumba and Warburton Rivers, being also the common boundaries of SC98/2 and SC97/3, to Longitude 137.265386° East; then southeasterly through the following coordinate points Longitude East Latitude South (Decimal Degrees) (Decimal Degrees) 137.384790 27.906602 137.415622 27.928522 137.462797 27.967863 137.513903 28.012450 137.557166 28.056982 being the boundaries of SC98/2. Then westerly, generally northwesterly and generally southerly along the northern and western boundaries of Lake Eyre National Park, to intersect the northern boundary of native title determination application SG6004/98 – “Kujani” (SC00/3) at Longitude 136.960827° East; then generally southwesterly through the following coordinates Longitude East Latitude South (Decimal Degrees) (Decimal Degrees) 136.866269 28.975909 136.695200 28.933393 136.579436 28.914085 136.481035 28.914085 136.423153 28.925669 136.376847 28.935324 136.274588 28.977801 136.191623 29.022209 136.126022 29.066618 136.044987 29.116819 135.950445 29.190189 Prepared by the Geospatial Analysis & Mapping Branch, National Native Title Tribunal, 11 November 2003. -
Arid and Semi-Arid Lakes
WETLAND MANAGEMENT PROFILE ARID AND SEMI-ARID LAKES Arid and semi-arid lakes are key inland This profi le covers the habitat types of ecosystems, forming part of an important wetlands termed arid and semi-arid network of feeding and breeding habitats for fl oodplain lakes, arid and semi-arid non- migratory and non-migratory waterbirds. The fl oodplain lakes, arid and semi-arid lakes support a range of other species, some permanent lakes, and arid and semi-arid of which are specifi cally adapted to survive in saline lakes. variable fresh to saline water regimes and This typology, developed by the Queensland through times when the lakes dry out. Arid Wetlands Program, also forms the basis for a set and semi-arid lakes typically have highly of conceptual models that are linked to variable annual surface water infl ows and vary dynamic wetlands mapping, both of which can in size, depth, salinity and turbidity as they be accessed through the WetlandInfo website cycle through periods of wet and dry. The <www.derm/qld.gov.au/wetlandinfo>. main management issues affecting arid and semi-arid lakes are: water regulation or Description extraction affecting local and/or regional This wetland management profi le focuses on the arid hydrology, grazing pressure from domestic and semi-arid zone lakes found within Queensland’s and feral animals, weeds and tourism impacts. inland-draining catchments in the Channel Country, Desert Uplands, Einasleigh Uplands and Mulga Lands bioregions. There are two broad types of river catchments in Australia: exhoreic, where most rainwater eventually drains to the sea; and endorheic, with internal drainage, where surface run-off never reaches the sea but replenishes inland wetland systems. -
Lake Eyre Basin (South Australia): Mapping and Conceptual Models of Shallow Groundwater Dependent Ecosystems
Lake Eyre Basin Springs Assessment Lake Eyre Basin (South Australia): mapping and conceptual models of shallow groundwater dependent ecosystems DEWNR Technical note 2015/22 Funding for these projects has been provided by the Australian Government through the Bioregional Assessment Programme. Lake Eyre Basin Springs Assessment Lake Eyre Basin (South Australia): mapping and conceptual models of shallow groundwater dependent ecosystems Catherine Miles1 and Justin F. Costelloe2 Department of Environment, Water and Natural Resources December, 2015 DEWNR Technical note 2015/22 1Miles Environmental Consulting 2Department of Infrastructure Engineering, University of Melbourne Department of Environment, Water and Natural Resources GPO Box 1047, Adelaide SA 5001 Telephone National (08) 8463 6946 International +61 8 8463 6946 Fax National (08) 8463 6999 International +61 8 8463 6999 Website www.environment.sa.gov.au Disclaimer The Department of Environment, Water and Natural Resources and its employees do not warrant or make any representation regarding the use, or results of the use, of the information contained herein as regards to its correctness, accuracy, reliability, currency or otherwise. The Department of Environment, Water and Natural Resources and its employees expressly disclaims all liability or responsibility to any person using the information or advice. Information contained in this document is correct at the time of writing. This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of -
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. -
Into Queensland, to Within 45 Km of the Georgina River Floodout Complex
into Queensland, to within 45 km of the Georgina River floodout complex. As a consequence, it is correctly included in the Georgina Basin. There is one river of moderate size in the Georgina basin that does not connect to any of the major rivers and that is Lucy Creek, which runs east from the Dulcie Ranges and may once have connected to the Georgina via Manners Creek. Table 7. Summary statistics of the major rivers and creeks in Lake Eyre Drainage Division Drainage Major Tributaries Initial Interim Highest Point Height of Lowest Straight System Bioregion & in Catchment highest Point Line Terminal (m asl) Major in NT Length Bioregions Channel (m asl) (km) (m asl) Finke River Basin: Finke R. Hugh R., Palmer R., MAC FIN, STP, 1,389 700 130 450† Karinga Ck., SSD Mt Giles Coglin Ck. Todd River Basin: Todd R. Ross R. BRT MAC, SSD 1,164 625 220 200 Mt Laughlin Hale R. Cleary Ck., Pulya Ck. MAC SSD 1,203 660 200 225 Mt Brassey Illogwa Ck. Albarta Ck. MAC BRT, SSD 853 500 230 140 Mt Ruby Hay River Basin: Plenty R. Huckitta Ck., Atula MAC BRT, SSD 1,203 600 130 270 Ck., Marshall R. Mt Brassey Corkwood (+ Hay R.) Bore Hay R. Marshall R., Arthur MAC, BRT, SSD 594 440 Marshal 70 355 Ck. (+ Plenty R.) CHC 340 Arthur Georgina River Basin: Georgina R. Ranken R., James R., MGD, CHC, SSD 220 215 190 >215 † (?Sandover R.) (?BRT) Sandover R. Mueller Ck., Waite MAC, BRT, BRT, 996 550 260 270 Ck., Bundey R., CHC, DAV CHC, Bold Hill Ooratippra Ck. -
Factsheet 27 – Why Is There a National Park in a Desert?
Factsheet 27 – Why is there a national park in a desert? Quirky fact : Canegrass thrives in arid environments Australian Curriculum Links because it is almost Year Subject Curriculum Links leafless, so water 5 Geography ACHGK027, ACHGK028 is not lost through evaporation. Science ACSSU043 When it rains, the 6 Science ACSSU094 green stems direct 7 Geography ACHGK037, ACHGK039, ACHGK041 moisture straight to Science ACSSU112 8 Geography ACHGK048, ACHGK049, ACHGK050, the roots through ACHGK052 photosynthesis. Science ACSHE136 Background Information At one million hectares, Munga-Thirri (Simpson Desert) the Channel Country occasionally sweep across the plains National Park is Queensland’s largest protected area. At quenching the dry rivers and creek beds that feed Lake Eyre. Poeppel Corner it meets South Australia’s Simpson Desert Bare, windswept crests stand atop slopes secured by spinifex Conservation Park and the Northern Territory’s Simpson and canegrass. Flat plains between dunes can be wind- Desert Regional Reserve. The entire Simpson Desert covers polished gibber pebbles or mineral-encrusted claypans but more than 17 million hectares of Central Australia. many, surprisingly, support open shrublands of acacias, Across the Simpson, parallel dunes run south-east to north- hakeas and grevilleas. Georgina gidgee, a rounded wattle tree, west, the dominant wind direction when they formed during is found extensively in dune swales and is well known for its the Pleistocene epoch about 80,000 years ago. Spaced about pungent odour after rain. 1 km apart, dunes can extend 200 kms. Far from deserted, Munga-Thirri (Simpson Desert) National Park is home to hardy mammals, many reptiles and over 180 The range in temperature can be extreme.