Ediacara Conservation Park
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GREAT ARTESIAN BASIN Responsibility to Any Person Using the Information Or Advice Contained Herein
S O U T H A U S T R A L I A A N D N O R T H E R N T E R R I T O R Y G R E A T A R T E S I A N B A S I N ( E RNturiyNaturiyaO M A N G A B A S I N ) Pmara JutPumntaara Jutunta YuenduYmuuendumuYuelamu " " Y"uelamu Hydrogeological Map (Part " 2) Nyirri"pi " " Papunya Papunya ! Mount Liebig " Mount Liebig " " " Haasts Bluff Haasts Bluff ! " Ground Elevation & Aquifer Conditions " Groundwater Salinity & Management Zones ! ! !! GAB Wells and Springs Amoonguna ! Amoonguna " GAB Spring " ! ! ! Salinity (μ S/cm) Hermannsburg Hermannsburg ! " " ! Areyonga GAB Spring Exclusion Zone Areyonga ! Well D Spring " Wallace Rockhole Santa Teresa " Wallace Rockhole Santa Teresa " " " " Extent of Saturated Aquifer ! D 1 - 500 ! D 5001 - 7000 Extent of Confined Aquifer ! D 501 - 1000 ! D 7001 - 10000 Titjikala Titjikala " " NT GAB Management Zone ! D ! Extent of Artesian Water 1001 - 1500 D 10001 - 25000 ! D ! Land Surface Elevation (m AHD) 1501 - 2000 D 25001 - 50000 Imanpa Imanpa ! " " ! ! D 2001 - 3000 ! ! 50001 - 100000 High : 1515 ! Mutitjulu Mutitjulu ! ! D " " ! 3001 - 5000 ! ! ! Finke Finke ! ! ! " !"!!! ! Northern Territory GAB Water Control District ! ! ! Low : -15 ! ! ! ! ! ! ! FNWAP Management Zone NORTHERN TERRITORY Birdsville NORTHERN TERRITORY ! ! ! Birdsville " ! ! ! " ! ! SOUTH AUSTRALIA SOUTH AUSTRALIA ! ! ! ! ! ! !!!!!!! !!!! D !! D !!! DD ! DD ! !D ! ! DD !! D !! !D !! D !! D ! D ! D ! D ! D ! !! D ! D ! D ! D ! DDDD ! Western D !! ! ! ! ! Recharge Zone ! ! ! ! ! ! D D ! ! ! ! ! ! N N ! ! A A ! L L ! ! ! ! S S ! ! N N ! ! Western Zone E -
Lake Torrens SA 2016, a Bush Blitz Survey Report
Lake Torrens South Australia 28 August–9 September 2016 Bush Blitz Species Discovery Program Lake Torrens, South Australia 28 August–9 September 2016 What is Bush Blitz? Bush Blitz is a multi-million dollar partnership between the Australian Government, BHP Billiton Sustainable Communities and Earthwatch Australia to document plants and animals in selected properties across Australia. This innovative partnership harnesses the expertise of many of Australia’s top scientists from museums, herbaria, universities, and other institutions and organisations across the country. Abbreviations ABRS Australian Biological Resources Study AD State Herbarium of South Australia ANIC Australian National Insect Collection CSIRO Commonwealth Scientific and Industrial Research Organisation DEWNR Department of Environment, Water and Natural Resources (South Australia) DSITI Department of Science, Information Technology and Innovation (Queensland) EPBC Act Environment Protection and Biodiversity Conservation Act 1999 (Commonwealth) MEL National Herbarium of Victoria NPW Act National Parks and Wildlife Act 1972 (South Australia) RBGV Royal Botanic Gardens Victoria SAM South Australian Museum Page 2 of 36 Lake Torrens, South Australia 28 August–9 September 2016 Summary In late August and early September 2016, a Bush Blitz survey was conducted in central South Australia at Lake Torrens National Park (managed by SA Department of Environment, Water and Natural Resources) and five adjoining pastoral stations to the west (Andamooka, Bosworth, Pernatty, Purple Downs and Roxby Downs). The traditional owners of this country are the Kokatha people and they were involved with planning and preparation of the survey and accompanied survey teams during the expedition itself. Lake Torrens National Park and surrounding areas have an arid climate and are dominated by three land systems: Torrens (bed of Lake Torrens), Roxby (dunefields) and Arcoona (gibber plains). -
Back Matter (PDF)
Index Acraman impact ejecta layer 53–4, 117, 123, 126–9, Aspidella 130–2, 425–7 controversy 300, 301–3, 305 acritarchs ecology 303 Amadeus and Officer Basins 119 synonyms 302 biostratigraphy 115–25, 130–2 Australia Australian correlations 130–2 Acraman impact ejecta layer 53–4, 117, 123, 126–9, composite zonation scheme 119, 131, 132 130–2, 425–7 India 318–20 carbon isotope chemostratigraphy 126–9 Ireland 289 correlations of Ediacaran System and Period 18, Spain 232 115–35 sphaeromorphid 324 Marinoan glaciation 53–4, 126 Adelaide, Hallett Cove 68 Australia, Ediacaran System and Period Adelaide Rift Complex 115–22, 425 Bunyeroo–Wonoka Formation transition correlations with Officer Basin 127 137–9, 426 dating (Sr–Rb) 140 Centralian Superbasin 118, 125 generalized time–space diagram, correlations composite zonation scheme 131 between tectonic units 120 correlation methods and results 125–32 location maps 116, 118 time–space diagram 120 SE sector cumulative strata thickness 139 Vendian climatic indicators 17 stratigraphic correlation with Officer Basin 127 See also Adelaide Rift Complex; Flinders Ranges Stuart Shelf drill holes, correlations 117 Avalonian assemblages, Newfoundland 237–57, Sturtian (Umberatana) Group 116, 138 303–7, 427 Umberatana Group 116, 138 Africa backarc spreading, Altenfeld Formation 44–5, 47–8 Vendian climatic indicators 17 Baliana–Krol Group, NW Himalaya 319 see also Namibia Barut Formation, Iran 434 Aldanellidae 418 Bayesian analysis algal metaphyta, White Sea Region 271–4 eumetazoans 357–9 algal microfossils, White -
Northern Flinders Ranges Fire Management Plan 2016
Northern Flinders Ranges Fire Management Plan 2016 Incorporating: Ikara-Flinders Ranges National Park, Vulkathunha-Gammon Ranges National Park, Ediacara Conservation Park, Bunkers Conservation Reserve and included Crown lands and participating Heritage Agreements Ikara-Flinders Ranges National Park Co-Management Board Vulkathunha-Gammon Ranges National Park Co-Management Board For further information please contact: Department of Environment, Water and Natural Resources Phone Information Line (08) 8204 1910, or see SA White Pages for your local Department of Environment, Water and Natural Resources office. This Fire Management Plan is also available from: www.environment.sa.gov.au/fire/ Front Cover: Ikara (Wilpena Pound) by DEWNR Permissive Licence © State of South Australia through the Department of Environment, Water and Natural Resources. Apart from fair dealings and other uses permitted by the Copyright Act 1968 (Cth), no part of this publication may be reproduced, published, communicated, transmitted, modified or commercialised without the prior written approval of the Department of Environment, Water and Natural Resources. Written requests for permission should be addressed to: Communications Manager Communications and Community Engagement Branch Department of Environment, Water and Natural Resources GPO Box 1047 Adelaide SA 5001 Disclaimer While reasonable efforts have been made to ensure the contents of this publication are factually correct , the Department of Environment, Water and Natural Resources makes no representations and accepts no responsibility for the accuracy, completeness or fitness for any particular purpose of the contents, and shall not be liable for any loss or damage that may be occasioned directly or indirectly through the use of or reliance on the contents of this publication. -
Natural Resources Management District Groups
South Australian Arid Lands NRM Region NNAATTUURRAALL RREESSOOUURRCCEESS MMAANNAAGGEEMMEENNTT DDIISSTTRRIICCTT GGRROOUUPPSS NORTHERN TERRITORY QUEENSLAND Mount Dare H.S. CROWN POINT Pandie Pandie HS AYERS SIMPSON DESERT RANGE SOUTH Tieyon H.S. CONSERVATION PARK ALTON DOWNS TIEYON WITJIRA NATIONAL PARK PANDIE PANDIE CORDILLO DOWNS HAMILTON DEROSE HILL Hamilton H.S. SIMPSON DESERT KENMORE REGIONAL RESERVE Cordillo Downs HS PARK Lambina H.S. Mount Sarah H.S. MOUNT Granite Downs H.S. SARAH Indulkana LAMBINA Todmorden H.S. MACUMBA CLIFTON HILLS GRANITE DOWNS TODMORDEN COONGIE LAKES Marla NATIONAL PARK Mintabie EVERARD PARK Welbourn Hill H.S. WELBOURN HILL Marla - Oodnadatta INNAMINCKA ANANGU COWARIE REGIONAL PITJANTJATJARAKU Oodnadatta RESERVE ABORIGINAL LAND ALLANDALE Marree - Innamincka Wintinna HS WINTINNA KALAMURINA Innamincka ARCKARINGA Algebuckinna Arckaringa HS MUNGERANIE EVELYN Mungeranie HS DOWNS GIDGEALPA THE PEAKE Moomba Evelyn Downs HS Mount Barry HS MOUNT BARRY Mulka HS NILPINNA MULKA LAKE EYRE NATIONAL MOUNT WILLOUGHBY Nilpinna HS PARK MERTY MERTY Etadunna HS STRZELECKI ELLIOT PRICE REGIONAL CONSERVATION ETADUNNA TALLARINGA PARK RESERVE CONSERVATION Mount Clarence HS PARK COOBER PEDY COMMONAGE William Creek BOLLARDS LAGOON Coober Pedy ANNA CREEK Dulkaninna HS MABEL CREEK DULKANINNA MOUNT CLARENCE Lindon HS Muloorina HS LINDON MULOORINA CLAYTON Curdimurka MURNPEOWIE INGOMAR FINNISS STUARTS CREEK SPRINGS MARREE ABORIGINAL Ingomar HS LAND CALLANNA Marree MUNDOWDNA LAKE CALLABONNA COMMONWEALTH HILL FOSSIL MCDOUAL RESERVE PEAK Mobella -
Of Time and Taphonomy: Preservation in the Ediacaran
See discussions, stats, and author profiles for this publication at: http://www.researchgate.net/publication/273127997 Of time and taphonomy: preservation in the Ediacaran CHAPTER · JANUARY 2014 READS 36 2 AUTHORS, INCLUDING: Charlotte Kenchington University of Cambridge 5 PUBLICATIONS 2 CITATIONS SEE PROFILE Available from: Charlotte Kenchington Retrieved on: 02 October 2015 ! OF TIME AND TAPHONOMY: PRESERVATION IN THE EDIACARAN CHARLOTTE G. KENCHINGTON! 1,2 AND PHILIP R. WILBY2 1Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK <[email protected]! > 2British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK ABSTRACT.—The late Neoproterozoic witnessed a revolution in the history of life: the transition from a microbial world to the one known today. The enigmatic organisms of the Ediacaran hold the key to understanding the early evolution of metazoans and their ecology, and thus the basis of Phanerozoic life. Crucial to interpreting the information they divulge is a thorough understanding of their taphonomy: what is preserved, how it is preserved, and also what is not preserved. Fortunately, this Period is also recognized for its abundance of soft-tissue preservation, which is viewed through a wide variety of taphonomic windows. Some of these, such as pyritization and carbonaceous compression, are also present throughout the Phanerozoic, but the abundance and variety of moldic preservation of body fossils in siliciclastic settings is unique to the Ediacaran. In rare cases, one organism is preserved in several preservational styles which, in conjunction with an increased understanding of the taphonomic processes involved in each style, allow confident interpretations of aspects of the biology and ecology of the organisms preserved. -
Ediacara Biota’
Accepted Manuscript There is no such thing as the ‘Ediacara Biota’ Breandán Anraoi MacGabhann PII: S1674-9871(13)00109-6 DOI: 10.1016/j.gsf.2013.08.001 Reference: GSF 237 To appear in: Geoscience Frontiers Received Date: 26 June 2013 Revised Date: 8 August 2013 Accepted Date: 14 August 2013 Please cite this article as: MacGabhann, B.A., There is no such thing as the ‘Ediacara Biota’, Geoscience Frontiers (2013), doi: 10.1016/j.gsf.2013.08.001. This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT MANUSCRIPT Sandstone mould + casts ACCEPTED Burgess Shale-style ACCEPTED MANUSCRIPT Research Highlights • The term ‘Ediacara Biota’ is commonly used to refer to early megascopic fossils • This term is inconsistent, arbitrarily excludes certain fossils, and cannot be defined • Studies of early metazoan evolution must consider all fossils of Ediacaran age MANUSCRIPT ACCEPTED ACCEPTED MANUSCRIPT 1 There is no such thing as the ‘Ediacara Biota’ 2 Breandán Anraoi MacGabhann 3 School of GeoSciences, University of Edinburgh, King's Buildings, West Mains Road, 4 Edinburgh EH9 3JW, UK. Tel: +44 131 6 508543 5 Email address: [email protected] 6 7 Abstract: The term ‘Ediacara Biota’ (or many variants thereof) is commonly used to refer to 8 certain megascopic fossils of Precambrian and early Palaeozoic age – but what does the term 9 actually mean? What differentiates a non-Ediacaran ‘Ediacaran’ and an Ediacaran 10 ‘Ediacaran’ from an Ediacaran non-‘Ediacaran’? Historically, the term has been used in 11 either a geographic, stratigraphic, taphonomic, or biologic sense. -
Ediacaria and Hiemalora - Disc-Like Attachments
Ediacaria and Hiemalora - Disc-like Attachments of Benthic Organisms from the White Sea and Arctic Siberia (Russia) E. A. Serezhnikova Paleontological Institute, Russian Academy of Sciences, 123 Profsoyuznaya, Moscow, 117868, Russia Localities of Vendian soft-bodied metazoans from Arctic Siberia and Zimnii Bereg along the White Sea coast are well known, just as they are in the classic Australian sequences. Fossils occur on the Olenek Uplift in dark gray, thin-bedded limestones of the Khatyspyt Formation in the Khorbusuonka Group, which crops out in the Olenek River Basin, along the Horbusuonka and Anabyl rivers. The Khorbusuonka Group can be correlated with Yudomian sediments using stromatolites, microphytolites and is dated radiometrically (Sokolov and Fedonkin, 1985). Fossils in the White Sea section are found primarily in fine-grained sandstones, siltstones and greenish clays that interfinger with cross-bedded siltstones and lenticular, cross-bedded sandstones. These strata have been dated as 553.3 +/- 0.3 Ma (Martin, et al., 2000), and they represent the Redkino Stage of the Vendian. Material from recently discovered new localities and well-preserved new specimens are significantly increasing the understanding of some Ediacaran taxa and changing views on their reconstructions. The best revisions of older reconstructions are made when the sample size for any one taxon is large and especially when that taxon is from one fossiliferous bed. T. M. Harris (1932) pioneered the use of this method of analysis based on his paleobotanic studies. This paper discusses new data on a number of taxa. Genus Hiemalora Fedonkin, 1982. Material of this genus consists of low-relief imprints of an organism with a rounded central disc and straight or smoothly curved, rod-like radial elements. -
Introduction and Background
Environment Assessment Chapter 8 Physical Environment Chapter 8 Physical Environment This chapter describes the existing physical environment of the proposed sites and the potential impacts of the proposal on the physical environment. The physical environment includes: geology geomorphology soils surface hydrology hydrogeology climate air quality noise fire. 8.1 Geology 8.1.1 Regional Geology The three proposed sites for the national radioactive waste repository are located in the Stuart Shelf geological province, to the west of Lake Torrens in South Australia. This province comprises incomplete sequences of flat-lying, undeformed Proterozoic (Precambrian) and early Palaeozoic (Cambrian) marine sediments of the Adelaide Geosyncline, overlying the northeastern part of the Archean Gawler Craton. The schematic geology of the area is shown in Figures 8.1 and 8.2. The Stuart Shelf is bounded to the east and northeast by the Torrens Hinge Zone, a major northerly trending structural feature running beneath Lake Torrens and forming the boundary between the Stuart Shelf and the Adelaide Geosyncline. The northern extension of the shelf is overlain by sediments of the Jurassic/Cretaceous Eromanga Basin. A thin veneer of younger Cainozoic (Tertiary and Quaternary) sediments or in situ deposits (e.g. silcrete or calcrete) is commonly encountered at the landscape surface. To the north of the Stuart Shelf the Eromanga Basin is the largest and most central of the three depressions that together make up the Great Artesian Basin (the other two are the Carpentaria Basin in northern Queensland and the Surat Basin in southeast Queensland and northeast New South Wales). Although the term ‘Great Artesian Basin’ has obvious hydrological connotations, it is entrenched in geological literature and has been used as a geological term even though the artesian and sedimentary limits are not the same. -
Ediacara Biota'
Edinburgh Research Explorer There is no such thing as the 'Ediacara Biota' Citation for published version: MacGabhann, BA 2014, 'There is no such thing as the 'Ediacara Biota'', Geoscience Frontiers, vol. 5, no. 1, pp. 53-62. https://doi.org/10.1016/j.gsf.2013.08.001 Digital Object Identifier (DOI): 10.1016/j.gsf.2013.08.001 Link: Link to publication record in Edinburgh Research Explorer Document Version: Publisher's PDF, also known as Version of record Published In: Geoscience Frontiers Publisher Rights Statement: Open Access General rights Copyright for the publications made accessible via the Edinburgh Research Explorer is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The University of Edinburgh has made every reasonable effort to ensure that Edinburgh Research Explorer content complies with UK legislation. If you believe that the public display of this file breaches copyright please contact [email protected] providing details, and we will remove access to the work immediately and investigate your claim. Download date: 08. Oct. 2021 Geoscience Frontiers 5 (2014) 53e62 Contents lists available at ScienceDirect China University of Geosciences (Beijing) Geoscience Frontiers journal homepage: www.elsevier.com/locate/gsf Focus paper There is no such thing as the ‘Ediacara Biota’ Breandán Anraoi MacGabhann* School of GeoSciences, University of Edinburgh, King’s Buildings, -
A Unique View on the Evolution of Marine Life
EXCEPTIONAL FOSSIL PRESERVATION: A Unique View on the Evolution of Marine Life Edited by DAVID J. BOTTJER COLUMBIA UNIVERSITY PRESS Bottjer_00FM 5/16/02 1:23 PM Page i EXCEPTIONAL FOSSIL PRESERVATION Critical Moments and Perspectives in Earth History and Paleobiology DAVID J. BOTTJER RICHARD K. BAMBACH Editors Bottjer_00FM 5/16/02 1:23 PM Page ii Critical Moments and Perspectives in Earth History and Paleobiology David J. Bottjer and Richard K. Bambach, Editors The Emergence of Animals: The Cambrian Breakthrough Mark A. S. McMenamin and Dianna L. S. McMenamin Phanerozoic Sea-Level Changes Anthony Hallam The Great Paleozoic Crisis: Life and Death in the Permian Douglas H. Erwin Tracing the History of Eukaryotic Cells: The Enigmatic Smile Betsey Dexter Dyer and Robert Alan Obar The Eocene-Oligocene Transition: Paradise Lost Donald R. Prothero The Late Devonian Mass Extinction: The Frasnian/Famennian Crisis George R. McGhee Jr. Dinosaur Extinction and the End of an Era: What the Fossils Say J. David Archibald One Long Experiment: Scale and Process in Earth History Ronald E. Martin Interpreting Pre-Quaternary Climate from the Geologic Record Judith Totman Parrish Theoretical Morphology: The Concept and Its Applications George R. McGhee Jr. Principles of Paleoclimatology Thomas M. Cronin The Ecology of the Cambrian Radiation Andrey Yu. Zhuravlev and Robert Riding, Editors Plants Invade the Land: Evolutionary and Environmental Perspectives Patricia G. Gensel and Dianne Edwards, Editors Bottjer_00FM 5/16/02 1:23 PM Page iii EXCEPTIONAL FOSSIL PRESERVATION A Unique View on the Evolution of Marine Life Edited by DAVID J. BOTTJER, WALTER ETTER, JAMES W. -
Lake Torrens Murdie Exploration Program
CONSULTATION INFORMATION PACKAGE Application for authorisation under the Aboriginal Heritage Act 1988 (SA) Kelaray Pty Ltd – Lake Torrens Murdie Exploration Program Applicant: Kelaray Pty Ltd Application Type: Authorisation under section 23 of the Aboriginal Heritage Act 1988 (SA) Application Area: The area within Exploration Licences 5937 and 5945 bounded in blue on the map at Figure 1, which includes a portion of Lake Torrens and a portion of Andamooka Island. Proposed Activities: Gravity in-fill surveys; deep diamond exploration drilling; upgrading existing access tracks; creation of new access tracks; drilling for water bores; construction of a new exploration camp on Andamooka Island; vegetation clearing; and the construction of multiple lake access points. Helicopter-assisted ‘offshore’ exploration drilling (image courtesy of Applicant) 1 INTRODUCTION The Premier of South Australia, as Minister responsible for the Aboriginal Heritage Act 1988 (SA) (Act), has received an application for authorisation under section 23 of the Act from Kelaray Pty Ltd (Applicant). The Applicant has sought the authorisation to enable it to assess the potential for economic mineral deposits, primarily focused on iron oxide copper-gold mineralisation in the northern portion of Lake Torrens, as part of its Lake Torrens Murdie Exploration Program (Exploration Program). The authorisation is sought to cover the entirety of Exploration Licence (EL) 5945 (Murdie), as well as the part of EL 5937 (West Lake Torrens) that intersects the boundary of the Lake Torrens Aboriginal site (6436-7237) (together the Application Area). The Application Area includes part of the Lake Torrens lake surface, a southern portion of Andamooka Island and a 500-metre wide section of the Lake Torrens shoreline that forms part of the Lake Torrens Aboriginal site.