Structures for Survival Rakali, the Australian Water Rat (Hydromys Chryogaster)
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Australia: State of the Environment 1996: Chapter 4
Chapter 4 . Biodiversity ‘Still Flying’ from the painting of a Wandering Albatross by Richard Prepared by Weatherly. Denis Saunders (Chair), CSIRO Division of Wildlife and Ecology Andrew Beattie, Centre for Biodiversity and Bioresources, School of Biological Sciences, Macquarie University Susannah Eliott (Research Assistant/Science Writer), Centre for Science Communication, University of Technology, Sydney Marilyn Fox, School of Geography, University of New South Wales Burke Hill, CSIRO Division of Fisheries Bob Pressey, New South Wales National Parks and Wildlife Service Duncan Veal, Centre for Biodiversity and Bioresources, School of Biological Sciences, Macquarie University Jackie Venning, State of Environment Reporting, South Australian Department of Environment and Natural Resources Mathew Maliel (State of the Environment Reporting Unit member), Department of the Environment, Sport and Territories (Facilitator) Charlie Zammit (former State of the Environment Reporting Unit member), Department of the Environment, Sport and Territories (former Facilitator) 4-1 . Australia: State of the Environment 1996 . Contents Introduction. 4-4 Pressure . 4-7 Human populations . 4-9 Urban development . 4-9 Tourism and recreation . 4-9 Harvesting resources and land use. 4-10 Fisheries . 4-10 Forestry . 4-11 Pastoralism. 4-12 Agriculture . 4-12 Introduced species . 4-16 Vertebrates . 4-16 Invertebrates. 4-17 Plants. 4-18 Micro-organisms. 4-20 Native species out of place . 4-20 Pollution . 4-21 Mining . 4-22 Climate change . 4-22 State . 4-23 The state of ecosystem diversity . 4-23 Biogeographic regionalisations for Australia . 4-23 Ecosystem diversity. 4-26 The state of species diversity. 4-30 Number and distribution of species . 4-31 Status of species . -
Bindaring Park Bassendean - Fauna Assessment
Bindaring Park Bassendean - Fauna Assessment Wetland habitat within Bindaring Park study area (Rob Browne-Cooper) Prepared for: Coterra Environment Level 3, 25 Prowse Street, WEST PERTH, WA 6005 Prepared by: Robert Browne-Cooper and Mike Bamford M.J. & A.R. Bamford Consulting Ecologists 23 Plover Way KINGSLEY WA 6026 6th April 2017 Bindaring Park - Fauna Assessment Summary Bamford Consulting Ecologists was commissioned by Coterra Environment to conduct a Level 1 fauna assessment (desktop review and site inspection) of Bindaring Park in Bassendean (the study area). The fauna survey is required to provide information on the ecological values for the Town of Bassendean’s Stage 2 Bindaring Wetland Concept Plan Development. This plan include developing design options (within wetland area) to enhance ecological values and habitat. The purpose of this report is to provide information on the fauna values of the habitat, particularly for significant species, and an overview of the ecological function of the site within the local and regional context. This assessment focuses on vertebrate fauna associated with the wetland and surrounding parkland vegetation within the study area, with consideration for connectivity with the Swan River. An emphasis is placed on locally-occurring conservation significant species and their habitat. Relevant species include Carnaby’s Black-Cockatoo, Forest Red-tailed Black-Cockatoo, and other local native species such as the Water Rat or Rakali. The fauna investigations were based on a desktop assessment and a field survey conducted in February 2017. The desktop study identified 180 vertebrate fauna species as potentially occurring in the Bindaring Park study area (see Table 3 and Appendix 5): five fish, 6 frogs, 20 reptiles, 134 birds, 8 native and 7 introduced mammals. -
Survey of the Underground Signs of Marsupial Moles in the WA Great Victoria Desert
Survey of the underground signs of marsupial moles in the WA Great Victoria Desert Report to Tropicana Joint Venture and the Department of Natural Resources, Environment and the Arts, Northern Territory Government Joe Benshemesh Martin Schulz September 2008 Marsupial moles in the WA Great Victoria Desert Benshemesh & Schulz 2008 Contents Summary.......................................................................................................................3 Introduction..................................................................................................................5 Methods........................................................................................................................7 Methods........................................................................................................................8 Sites.........................................................................................................................8 Trenches.................................................................................................................9 Moleholes ..............................................................................................................9 Additional data ....................................................................................................9 Results..........................................................................................................................12 Characteristics attributes of backfilled tunnels in WA GVD.............................12 -
(A) Global Distribution of Hyperarid and Dryland Areas Figure 9.2
a Figure 9.2 (a) Global distribution of hyperarid and dryland areas Drylands Dry subhumid areas Dry subhumid areas DrylandsSemiarid areas AridSemiarid areas areas DrylandsDryDry subhumidsubhumid areasareas HyperaridArid areas areas SemiaridSemiaridDryDry subhumidsubhumid areasareas areasareas AridArid areasareasHyperarid areas SemiaridSemiarid areasareas HyperaridHyperarid areasareas Map produced by ZOÏ Environment Network, September 2010 Source: UNEAridAridP W orld areasareas Conservation Monitoring Centre DrylandsHyperaridHyperarid areasareas Map produced by ZOÏ Environment Network, September 2010 MapMap producedproduced byby ZOÏZOÏ EnvironmentEnvironment Network,Network, SeptemberSeptember 20102010 Source: UNEDryP subhumidWorld Conservation areas Monitoring Centre Source:Source:b UNEUNEPP WWorldorld ConservationConservation MonitoringMonitoring CentreCentre DrylandsSemiarid areas Arid areas Figure 9.2 DryDry subhumidsubhumid areasareas Hyperarid areas SemiaridSemiarid areasareas (b) Regions MapMap producedproduced byby ZOÏZOÏ EnvironmentEnvironment Network,Network, SeptemberSeptember 20102010 Source:Source: UNEUNEPPAridArid WW areasorldareasorld ConservationConservation MonitoringMonitoring CentreCentre vulnerable to HyperaridHyperarid areasareas Map produced by ZOÏ Environment Network, September 2010 Source: UNEP World Conservation Monitoring Centre desertification MapMap producedproduced byby ZOÏZOÏ EnvironmentEnvironment Network,Network, SeptemberSeptember 20102010 Source:Source: UNEUNEPP WWorldorld ConservationConservation MonitoringMonitoring -
Desert-2.Pdf
Desert Contens Top Ten Facts PG 1 front cover 1 All Deserts are all different but they all have low amounts of rain PG 2 contens 2 Deserts normally have less than 40 CM a year 3 The Sahara desert is in Northern Africa and is over 12 different countries PG 3 top ten facts 4 Sahara desert is the largest desert in the Earth PG 4 whether and climate 5 Only around 20% of the Deserts on Earth are covered in sand 6 Around one third of the Earth's surface is covered in Desert PG 5 desert map 7 The largest cold Desert on Earth is Antarctica PG 6 animals and people that live there 8 Located in South America, the Atacama Desert is the driest place in the world PG 7 what grows there 9 Lots of animals live in Deserts such as the wild dog 10 The Arabian Desert in the Middle East is the second largest hot desert on Earth but is substantially smaller than the Sahara. This is a list of the deserts in Wether And Climate the world Arabian Desert. ... Kalahari Desert. ... Wether Mojave Desert. ... Sonoran Desert. ... Chihuahuan Desert. ... This is a map showing Deserts are usually very, very dry. Even the wettest deserts get less than ten Thar Desert. ... the deserts in the world inches of precipitation a year. In most places, rain falls steadily throughout the Gibson Desert. year. But in the desert, there may be only a few periods of rains per year with a lot of time between rains. -
New England Peppermint (Eucalyptus Nova-Anglica) Grassy
Advice to the Minister for Sustainability, Environment, Water, Population and Communities from the Threatened Species Scientific Committee on an Amendment to the List of Threatened Ecological Communities under the Environment Protection and Biodiversity Conservation Act 1999 (EPBC Act) 1. Name of the ecological community New England Peppermint (Eucalyptus nova-anglica) Grassy Woodlands This advice follows the assessment of two public nominations to list the ‘New England Peppermint (Eucalyptus nova-anglica) Woodlands on Sediment on the Northern Tablelands’ and the ‘New England Peppermint (Eucalyptus nova-anglica) Woodlands on Basalt on the Northern Tablelands’ as threatened ecological communities under the EPBC Act. The Threatened Species Scientific Committee (the Committee) recommends that the national ecological community be renamed New England Peppermint (Eucalyptus nova-anglica) Grassy Woodlands. The name reflects the fact that the definition of the ecological community has been expanded to include all grassy woodlands dominated or co-dominated by Eucalyptus nova-anglica (New England Peppermint), in New South Wales and Queensland. Also the occurrence of the ecological community extends beyond the New England Tableland Bioregion, into adjacent areas of the New South Wales North Coast and the Nandewar bioregions. Part of the national ecological community is listed as endangered in New South Wales, as ‘New England Peppermint (Eucalyptus nova-anglica) Woodland on Basalts and Sediments in the New England Tableland Bioregion’ (NSW Scientific Committee, 2003); and, as an endangered Regional Ecosystem in Queensland ‘RE 13.3.2 Eucalyptus nova-anglica ± E. dalrympleana subsp. heptantha open-forest or woodland’ (Qld Herbarium, 2009). 2. Public Consultation A technical workshop with experts on the ecological community was held in 2005. -
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 -
Copyright and Use of This Thesis This Thesis Must Be Used in Accordance with the Provisions of the Copyright Act 1968
COPYRIGHT AND USE OF THIS THESIS This thesis must be used in accordance with the provisions of the Copyright Act 1968. Reproduction of material protected by copyright may be an infringement of copyright and copyright owners may be entitled to take legal action against persons who infringe their copyright. Section 51 (2) of the Copyright Act permits an authorized officer of a university library or archives to provide a copy (by communication or otherwise) of an unpublished thesis kept in the library or archives, to a person who satisfies the authorized officer that he or she requires the reproduction for the purposes of research or study. The Copyright Act grants the creator of a work a number of moral rights, specifically the right of attribution, the right against false attribution and the right of integrity. You may infringe the author’s moral rights if you: - fail to acknowledge the author of this thesis if you quote sections from the work - attribute this thesis to another author - subject this thesis to derogatory treatment which may prejudice the author’s reputation For further information contact the University’s Director of Copyright Services sydney.edu.au/copyright The role of ecological interactions: how intrinsic and extrinsic factors shape the spatio-temporal dynamics of populations Aaron C. Greenville A thesis submitted in fulfilment of the requirements for the degree of Doctor of Philosophy Faculty of Science The University of Sydney, Australia February 2015 Declaration of originality I hereby declare that the work contained in this thesis is my own and contains the results of an original investigation, except where otherwise referenced or acknowledged. -
(Hydromys Chrysogaster) in the Greater Perth Region, Western Australia
Journal of the Royal Society of Western Australia, 94: 533–539, 2011 Influence of habitat characteristics on the distribution of the water-rat (Hydromys chrysogaster) in the greater Perth region, Western Australia C Smart 1, P C Speldewinde 2 & H R Mills 1 1 School of Animal Biology, University of Western Australia, 35 Stirling Highway, Crawley, WA 6009 2 Centre of Excellence in Natural Resource Management, University of Western Australia, 35 Stirling Highway, Crawley, WA 6009 Manuscript received August 2010; accepted May 2011 Abstract This study investigated the distribution of the water-rat (Hydromys chrysogaster) in the greater Perth region, and proposes the potential of the species as a bioindicator of habitat quality. The degradation and loss of wetlands on the Swan Coastal Plain are associated with changes to habitat quality, including vegetation cover, stream cover, habitat diversity and bank stability. The occurrence of H. chrysogaster was analysed with respect to these factors at various water bodies around the greater Perth area. Sites positive for the presence of H. chrysogaster correlated with high value habitat quality characteristics, including high bank stability, habitat diversity, stream cover and foreshore vegetation. The presence of H. chrysogaster was not correlated to the occurrence and abundance of other local mammal species, except for a positive relationship with the introduced black rat (Rattus rattus) in relation to abundance. Based on the habitat requirements of H. chrysogaster, the species has some potential as a bioindicator of wetland condition on the Swan Coastal Plain, Western Australia, although the viability of such a method is uncertain. Key words: wetland, habitat quality, bioindicator, rakali, Swan Coastal Plain Introduction Suitability of habitat is thought to be one of the factors influencing the distribution of mammals (Geier & Best Effective conservation of biodiversity in urbanised 1980). -
The Vegetation of the Western Australian Deserts
©Reinhold-Tüxen-Gesellschaft (http://www.reinhold-tuexen-gesellschaft.de/) Ber. d. Reinh.-Tüxen-Ges. 18, 219-228. Hannover 2006 The Vegetation of the Western Australian Deserts - Erika and Sandro Pignatti, Rom - Abstract The internal area of W. Australia has arid climate and conditions for plant growth are particularly difficult. The surface of this huge, almost uninhabited territory consists of four landscape systems: the Great Sandy Desert, the Little Sandy Desert, the Great Victoria Desert, the Gibson Desert. The four deserts extend between 21-26° of south- ern latitude, linking to the central Australian deserts and the Nullarbor Plain in the South. Meteorological stations are only in settlements of the surrounding semi-desert areas (Wiluna, Meekatharra, Cue, Warburton), and all show around 200-250 mm year- ly rainfall; in the centre of the deserts rainfall is still much lower, and indicated as “erratic and unreliable”; some areas may lack rain for several years. Despite of the par- ticularly severe ecological conditions, most of the surface is covered by vegetation (at least a discontinuous one) and during expeditions in 2001 and 2002 over 700 species were collected and more than 350 phytosociological relevés were carried out.Two main habitat types can be recognized: Mulga – scattered growth of treelets (Acacia aneura, generally about 3-4 m height), with open understorey (Senna, Eremophila, Solanum) and herbs usually covering less than 20 % of the surface; in the Gibson Desert mulga occurs mainly on hard rock sub- strate (granite, laterite). Because of the discontinuous plant cover, fire can spread only over limited areas. Spinifex – Quite a compact cover of perennial grasses (several species of Triodia, with sharply pointed leaves in dense tussocks 3-5 dm high, panicles up to 1 m and high- er) in monospecific populations covering 60-80 % of the surface; in the sandy deserts, on siliceous sand. -
Gibson Desert Bioregion
Gibson Desert bioregion Description Data sources available Area: 156 290 km2 There are no site-based monitoring data. The Gibson Desert bioregion has vast, undulating Other data sources include: sand plains, dunefields and lateritic gibber plains. The vegetation is mainly mulga and other mixed shrubs n fire extent, intensity and frequency, which over spinifex. The bioregion includes Aboriginal land, provides high reliability for reporting change unallocated crown land and conservation reserves. n dust Conservation and Aboriginal land are the main land n distribution and relative abundance of invasive uses. The bioregion has a very low population, with animals and weeds the major centres being the Kanpa, Patjarr and Tjirrkarli Aboriginal communities. n land use n conservation estate. Location The Gibson Desert bioregion is located in the Climate central east rangelands of Western Australia The Gibson Desert bioregion has an arid climate (see Figure 1). with variable and unpredictable rainfall. Spatially averaged median (1890–2005) rainfall is 163 mm Figure 1 Location of the Gibson Desert (April to March rainfall year; see Figure 2). bioregion Figure 2 Decile rainfall for the period 1991–1992 to 2004–2005 10 9 8 7 6 median 5 4 3 Rainfall decile 2 1 0 1991-92 1993-94 1995-96 1997-98 1999-00 2001-02 2003-04 Rainfall year Annual rainfall is for the 12‑month period 1 April to 31 March. Location of Gibson Desert bioregion Gibson Desert bioregion 1 Decile rainfall was generally well above average for Components of total grazing the 1992–2005 period after improving from a drier pressure year in 1991–1992.