Papers and Proceedings of the Royal Society of Tasmania
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SUPPLEMENTARY INFORMATION for a New Family of Diprotodontian Marsupials from the Latest Oligocene of Australia and the Evolution
Title A new family of diprotodontian marsupials from the latest Oligocene of Australia and the evolution of wombats, koalas, and their relatives (Vombatiformes) Authors Beck, RMD; Louys, J; Brewer, Philippa; Archer, M; Black, KH; Tedford, RH Date Submitted 2020-10-13 SUPPLEMENTARY INFORMATION FOR A new family of diprotodontian marsupials from the latest Oligocene of Australia and the evolution of wombats, koalas, and their relatives (Vombatiformes) Robin M. D. Beck1,2*, Julien Louys3, Philippa Brewer4, Michael Archer2, Karen H. Black2, Richard H. Tedford5 (deceased) 1Ecosystems and Environment Research Centre, School of Science, Engineering and Environment, University of Salford, Manchester, UK 2PANGEA Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, New South Wales, Australia 3Australian Research Centre for Human Evolution, Environmental Futures Research Institute, Griffith University, Queensland, Australia 4Department of Earth Sciences, Natural History Museum, London, United Kingdom 5Division of Paleontology, American Museum of Natural History, New York, USA Correspondence and requests for materials should be addressed to R.M.D.B (email: [email protected]) This pdf includes: Supplementary figures Supplementary tables Comparative material Full description Relevance of Marada arcanum List of morphological characters Morphological matrix in NEXUS format Justification for body mass estimates References Figure S1. Rostrum of holotype and only known specimen of Mukupirna nambensis gen. et. sp. nov. (AMNH FM 102646) in ventromedial (a) and anteroventral (b) views. Abbreviations: C1a, upper canine alveolus; I1a, first upper incisor alveolus; I2a, second upper incisor alveolus; I1a, third upper incisor alveolus; P3, third upper premolar. Scale bar = 1 cm. -
Australian Journal of Earth Sciences Paleosol Record of Neogene Climate
This article was downloaded by: [Retallack, Gregory J.][University of Oregon] On: 28 September 2010 Access details: Access Details: [subscription number 917394740] Publisher Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37- 41 Mortimer Street, London W1T 3JH, UK Australian Journal of Earth Sciences Publication details, including instructions for authors and subscription information: http://www.informaworld.com/smpp/title~content=t716100753 Paleosol record of Neogene climate change in the Australian outback C. A. Metzgera; G. J. Retallacka a Department of Geological Sciences, University of Oregon, Eugene, OR, USA Online publication date: 24 September 2010 To cite this Article Metzger, C. A. and Retallack, G. J.(2010) 'Paleosol record of Neogene climate change in the Australian outback', Australian Journal of Earth Sciences, 57: 7, 871 — 885 To link to this Article: DOI: 10.1080/08120099.2010.510578 URL: http://dx.doi.org/10.1080/08120099.2010.510578 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.informaworld.com/terms-and-conditions-of-access.pdf This article may be used for research, teaching and private study purposes. Any substantial or systematic reproduction, re-distribution, re-selling, loan or sub-licensing, systematic supply or distribution in any form to anyone is expressly forbidden. The publisher does not give any warranty express or implied or make any representation that the contents will be complete or accurate or up to date. The accuracy of any instructions, formulae and drug doses should be independently verified with primary sources. The publisher shall not be liable for any loss, actions, claims, proceedings, demand or costs or damages whatsoever or howsoever caused arising directly or indirectly in connection with or arising out of the use of this material. -
Megafauna Extinction
Episode 15 Teacher Resource 2nd June 2020 Megafauna Extinction 1. Before watching the BTN story, record what you know about Students will learn more about Australian megafauna and megafauna. investigate why they became 2. What is megafauna? extinct. 3. About how many years ago did megafauna exist in Australia? a. 4,000 b. 40,000 c. 400,000 Science – Year 6 The growth and survival of living 4. Complete the following sentence. A Diprotodon was a giant things are affected by physical _________________. conditions of their environment. 5. What did palaeontologist Dr Scott Hocknull and his team discover? Science – Year 7 6. Where did they make the discovery? Scientific knowledge has changed peoples’ understanding of the 7. What did they use to create images of what the megafauna might world and is refined as new have looked like? evidence becomes available. 8. Give some examples of the megafauna species they discovered. Interactions between organisms, 9. What might have caused megafauna to become extinct? including the effects of human 10. What did you learn watching the BTN story? activities can be represented by food chains and food webs. What do you know about megafauna? As a class discuss the BTN Megafauna Extinction story and ask students to record what they learnt watching the story. Record any questions they have. Here are some questions they can use to help guide their discussion. • What does the term megafauna mean? • When did megafauna exist? • How do we know they existed? • Why did megafauna grow so big? • What might have caused Australia’s megafauna to die out? Glossary Students will brainstorm a list of key words and terms that relate to the BTN Megafauna Extinction story. -
Relative Demographic Susceptibility Does Not Explain the Extinction Chronology of Sahul's Megafauna
bioRxiv preprint doi: https://doi.org/10.1101/2020.10.16.342303; this version posted October 19, 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 Full title: Relative demographic susceptibility does not explain the 2 extinction chronology of Sahul’s megafauna 3 Short title: Demographic susceptibility of Sahul’s megafauna 4 5 Corey J. A. Bradshaw1,2,*, Christopher N. Johnson3,2, John Llewelyn1,2, Vera 6 Weisbecker4,2, Giovanni Strona5, and Frédérik Saltré1,2 7 1 Global Ecology, College of Science and Engineering, Flinders University, GPO Box 2100, Adelaide, 8 South Australia 5001, Australia, 2 ARC Centre of Excellence for Australian Biodiversity and Heritage, 9 EpicAustralia.org, 3 Dynamics of Eco-Evolutionary Pattern, University of Tasmania, Hobart, Tasmania 10 7001, Australia, 4 College of Science and Engineering, Flinders University, GPO Box 2100, Adelaide, 11 South Australia 5001, Australia, 5 Research Centre for Ecological Change, University of Helsinki, 12 Viikinkaari 1, Biocentre 3, 00790, Helsinki, Finland 13 14 * [email protected] (CJAB) 15 ORCIDs: C.J.A. Bradshaw: 0000-0002-5328-7741; C.N. Johnson: 0000-0002-9719-3771; J. 16 Llewelyn: 0000-0002-5379-5631; V. WeisbecKer: 0000-0003-2370-4046; F. Saltré: 0000- 17 0002-5040-3911 18 19 Keywords: vombatiformes, macropodiformes, flightless birds, carnivores, extinction 20 Author Contributions: C.J.A.B and F.S. conceptualized the paper, and C.J.A.B. -
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13 STUDIES IN TASMANIAN MAMMALS, LIVING AND EXTINCT. Number I. Nototherium mitchelli. (A Marsupial Rhinoceros.) lierium. mitchelli, Owen, British Association for Advancement of Science, Report 1844, p. ?Zygomaturus trilobus, De Vis, Proceedings Royal S of Queensland. 1888, Vol. V., pt. .1 p. 111. By I!. 11. Scott (Curator, Launceston Museum); and Clive E. Lord (Curator, Tasmanian Museum). (Received 3rd May, L920. Read 10th May, 1920.) The discovery at Smithton, during the present year, <• of a nearly complete i Nototherium mitchelli forms the occasion for a revision of many of our ideas - - markable marsupial animals, since 1 1 * I ntarv remains hitherto available for study have 1 to yield the sequence of evidence we now possess, be only— inf nded to place upon record the hat. Nototherium mitchelli was an extinct marsupial rhino< I that the four genera, Nototherium, Zygo- maturus, Euowenia, and Sthenomerus, with their - species, are accordingly under revision— and will later on be dealt with in detail. ma > Material 1 in ibids anything like speculation ; . hut it is within the mark to observe thai two groups of these animals have be instinctively felt (by all workers) to have existed, quite irrespective of sex ques- tion- —one a platyrhine and the other a latifrons type, and that it now appears that they were also a horned, and a hornless group, and that Nototherium mitchelli belonged to the former, or cerathine group, and that some other species constituted the acerathine group, in which the 14 STUDIES IN TASMANIAN MAMMALS, LIVING AND EXTINCT, weapons were reduced to very small things, or actually missing. -
A New Family of Diprotodontian Marsupials from the Latest Oligocene of Australia and the Evolution of Wombats, Koalas, and Their Relatives (Vombatiformes) Robin M
www.nature.com/scientificreports OPEN A new family of diprotodontian marsupials from the latest Oligocene of Australia and the evolution of wombats, koalas, and their relatives (Vombatiformes) Robin M. D. Beck1,2 ✉ , Julien Louys3, Philippa Brewer4, Michael Archer2, Karen H. Black2 & Richard H. Tedford5,6 We describe the partial cranium and skeleton of a new diprotodontian marsupial from the late Oligocene (~26–25 Ma) Namba Formation of South Australia. This is one of the oldest Australian marsupial fossils known from an associated skeleton and it reveals previously unsuspected morphological diversity within Vombatiformes, the clade that includes wombats (Vombatidae), koalas (Phascolarctidae) and several extinct families. Several aspects of the skull and teeth of the new taxon, which we refer to a new family, are intermediate between members of the fossil family Wynyardiidae and wombats. Its postcranial skeleton exhibits features associated with scratch-digging, but it is unlikely to have been a true burrower. Body mass estimates based on postcranial dimensions range between 143 and 171 kg, suggesting that it was ~5 times larger than living wombats. Phylogenetic analysis based on 79 craniodental and 20 postcranial characters places the new taxon as sister to vombatids, with which it forms the superfamily Vombatoidea as defned here. It suggests that the highly derived vombatids evolved from wynyardiid-like ancestors, and that scratch-digging adaptations evolved in vombatoids prior to the appearance of the ever-growing (hypselodont) molars that are a characteristic feature of all post-Miocene vombatids. Ancestral state reconstructions on our preferred phylogeny suggest that bunolophodont molars are plesiomorphic for vombatiforms, with full lophodonty (characteristic of diprotodontoids) evolving from a selenodont morphology that was retained by phascolarctids and ilariids, and wynyardiids and vombatoids retaining an intermediate selenolophodont condition. -
1 TABLE S1 Global List of Extinct and Extant Megafaunal Genera By
Supplemental Material: Annu. Rev. Ecol. Syst.. 2006. 37:215-50 doi: 10.1146/annurev.ecolsys.34.011802.132415 Late Quaternary Extinctions: State of the Debate Koch and Barnosky TABLE S1 Global list of extinct and extant megafaunal genera by continent. STATUS TAXON TIME AFRICA Mammalia Carnivora Felidae Acinonyx Panthera Hyaenidae Crocuta Hyaena Ursidae Ursusa Primates Gorilla Proboscidea Elephantidae C Elephas <100 Loxodonta Perissodactyla Equidae S Equus <100 E Hipparion <100 Rhinocerotidae Ceratotherium Diceros E Stephanorhinus <100 Artiodactyla Bovidae Addax Ammotragus Antidorcas Alcelaphus Aepyceros C Bos 11.5-0 Capra Cephalopus Connochaetes Damaliscus Gazella S Hippotragus <100 Kobus E Rhynotragus/Megalotragus 11.5-0 Oryx E Pelorovis 11.5-0 E Parmulariusa <100 Redunca Sigmoceros Syncerus Taurotragus Tragelaphus Camelidae C Camelus <100 1 Supplemental Material: Annu. Rev. Ecol. Syst.. 2006. 37:215-50 doi: 10.1146/annurev.ecolsys.34.011802.132415 Late Quaternary Extinctions: State of the Debate Koch and Barnosky Cervidae E Megaceroides <100 Giraffidae S Giraffa <100 Okapia Hippopotamidae Hexaprotodon Hippopotamus Suidae Hylochoerus Phacochoerus Potamochoerus Susa Tubulidenta Orycteropus AUSTRALIA Reptilia Varanidae E Megalania 50-15.5 Meiolanidae E Meiolania 50-15.5 E Ninjemys <100 Crocodylidae E Palimnarchus 50-15.5 E Quinkana 50-15.5 Boiidae? E Wonambi 100-50 Aves E Genyornis 50-15.5 Mammalia Marsupialia Diprotodontidae E Diprotodon 50-15.5 E Euowenia <100 E Euryzygoma <100 E Nototherium <100 E Zygomaturus 100-50 Macropodidae S Macropus 100-50 E Procoptodon <100 E Protemnodon 50-15.5 E Simosthenurus 50-15.5 E Sthenurus 100-50 Palorchestidae E Palorchestes 50-15.5 Thylacoleonidae E Thylacoleo 50-15.5 Vombatidae S Lasiorhinus <100 E Phascolomys <100 E Phascolonus 50-15.5 E Ramsayia <100 2 Supplemental Material: Annu. -
The Chinchilla Local Fauna: an Exceptionally Rich and Well-Preserved Pliocene Vertebrate Assemblage from Fluviatile Deposits of South-Eastern Queensland, Australia
The Chinchilla Local Fauna: An exceptionally rich and well-preserved Pliocene vertebrate assemblage from fluviatile deposits of south-eastern Queensland, Australia JULIEN LOUYS and GILBERT J. PRICE Louys, J. and Price, G.J. 2015. The Chinchilla Local Fauna: An exceptionally rich and well-preserved Pliocene verte- brate assemblage from fluviatile deposits of south-eastern Queensland, Australia. Acta Palaeontologica Polonica 60 (3): 551–572. The Chinchilla Sand is a formally defined stratigraphic sequence of Pliocene fluviatile deposits that comprise interbed- ded clay, sand, and conglomerate located in the western Darling Downs, south-east Queensland, Australia. Vertebrate fossils from the deposits are referred to as the Chinchilla Local Fauna. Despite over a century and a half of collection and study, uncertainties concerning the taxa in the Chinchilla Local Fauna continue, largely from the absence of stratigraph- ically controlled excavations, lost or destroyed specimens, and poorly documented provenance data. Here we present a detailed and updated study of the vertebrate fauna from this site. The Pliocene vertebrate assemblage is represented by at least 63 taxa in 31 families. The Chinchilla Local Fauna is Australia’s largest, richest and best preserved Pliocene ver- tebrate locality, and is eminently suited for palaeoecological and palaeoenvironmental investigations of the late Pliocene. Key words: Mammalia, Marsupialia, Pliocene, Australia, Queensland, Darling Downs. Julien Louys [[email protected]], Department of Archaeology and Natural History, School of Culture, History, and Languages, ANU College of Asia and the Pacific, The Australian National University, Canberra, 0200, Australia. Gilbert J. Price [[email protected]], School of Earth Sciences, The University of Queensland, Brisbane, Queensland, 4072, Australia. -
Climate Change Not to Blame for Late Quaternary Megafauna Extinctions in Australia
ARTICLE Received 25 Jun 2015 | Accepted 13 Dec 2015 | Published 29 Jan 2016 DOI: 10.1038/ncomms10511 OPEN Climate change not to blame for late Quaternary megafauna extinctions in Australia Fre´de´rik Saltre´1, Marta Rodrı´guez-Rey1, Barry W. Brook2, Christopher N. Johnson2, Chris S.M. Turney3, John Alroy4, Alan Cooper1,5, Nicholas Beeton2, Michael I. Bird6, Damien A. Fordham1, Richard Gillespie7,8, Salvador Herrando-Pe´rez1,9, Zenobia Jacobs7, Gifford H. Miller10,11, David Nogue´s-Bravo12, Gavin J. Prideaux13, Richard G. Roberts7 & Corey J.A. Bradshaw1 Late Quaternary megafauna extinctions impoverished mammalian diversity worldwide. The causes of these extinctions in Australia are most controversial but essential to resolve, because this continent-wide event presaged similar losses that occurred thousands of years later on other continents. Here we apply a rigorous metadata analysis and new ensemble- hindcasting approach to 659 Australian megafauna fossil ages. When coupled with analysis of several high-resolution climate records, we show that megafaunal extinctions were broadly synchronous among genera and independent of climate aridity and variability in Australia over the last 120,000 years. Our results reject climate change as the primary driver of megafauna extinctions in the world’s most controversial context, and instead estimate that the megafauna disappeared Australia-wide B13,500 years after human arrival, with shorter periods of coexistence in some regions. This is the first comprehensive approach to incorporate uncertainty in fossil ages, extinction timing and climatology, to quantify mechanisms of prehistorical extinctions. 1 The Environment Institute and School of Biological Sciences, The University of Adelaide, North Terrace, Adelaide, South Australia 5005, Australia. -
Systematic and Palaeobiological Implications of Postcranial Morphology in the Diprotodontidae (Marsupialia)
Systematic and palaeobiological implications of postcranial morphology in the Diprotodontidae (Marsupialia) Aaron B. Camens School of Earth and Environmental Sciences Discipline of Ecology and Evolutionary Biology The University of Adelaide South Australia A thesis submitted in partial fulfilment of the degree of Doctor of Philosophy at the University of Adelaide February 2010 II Declaration This work contains no material which has been accepted for the award of any other degree or diploma in any university or other tertiary institution to Aaron Camens and, to the best of my knowledge and belief, contains no material previously published or written by another person, except where due reference has been made in the text. I give consent to this copy of my thesis when deposited in the University Library, being made available for loan and photocopying, subject to the provisions of the Copyright Act 1968. The author acknowledges that copyright of published works contained within this thesis (as listed below) resides with the copyright holder(s) of those works. I also give permission for the digital version of my thesis to be made available on the web, via the University’s digital research repository, the Library catalogue, the Australasian Digital Theses Program (ADTP) and also through web search engines, unless permission has been granted by the University to restrict access for a period of time. Publications in this thesis include: Camens, A. B. and Wells, R.T. 2009. Diprotodontid footprints from the Pliocene of Central Australia. Journal of Vertebrate Paleontology 29: 863-869. Copyright held by Taylor and Francis. Camens, A. B. and Wells, R.T. -
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https://doi.org/10.24199/j.mmv.1973.34.03 9 May 1973 FOSSIL VERTEBRATE FAUNAS FROM THE LAKE VICTORIA REGION, S.W. NEW SOUTH WALES, AUSTRALIA By Larry G. Marshall Zoology Department, Monash University, Victoria* Abstract Fossil vertebrate localities and faunas in the Lake Victoria region of S.W. New South Wales, Australia, are described. The oldest fossil bearing deposit, the late Pliocene or early Pleistocene Moorna Formation and associated Chowilla Sand have yielded specimens of Neoceratodus sp., Emydura macquarrii, several species of small dasyurid, specimens of Glaucodon cf. G. ballaratensis, a species of Protemnodon which compares closely with P. cf. P. otibandus from the late Pliocene or early Pleistocene Chinchilla Sand in SE. Queensland, specimens of Lagostrophus cf L. fasciatus, species of Petrogale, Macropus, Osphranter, Sthenurus, Bettongia, Diprotodon, Lasiorhinus, a peramelid, at least two species of pseudomyine rodents and a species of Rattus cf. R. lutreolus. It is shown that the holotype of Zygomaturus victoriae (Owen) 1872 may have been collected from these sediments. The late Pliocene or early Pleistocene Blanchetown Clay has yielded species of Neoceratodus, Thylacoleo, Phas- colonus, Bettongia, Sthenurus, a diprotodontid, and a rodent. The late Pleistocene Rufus Formation has yielded species of Dasycercus, Sarcophilus, Thylacinus, Phascolonus, Lasiorhinus, Bettongia, Procoptodon, Onychogalea, Macropus, and Leporillus. A large species of macropod and a species of Phascolonus were collected from the late Pleistocene Monoman Formation. The lunette on the E. side of Lake Victoria has yielded a large, diverse fauna of late Pleistocene —Holocene age, that includes such extinct species as Protemnodon anak, P. brehus, Procoptodon goliah, Sthenurus andersoni, S. -
Kenny TRAVOUILLON Phd Thesis Complete
PALAEOECOLOGICAL AND BIOCHRONOLOGICAL STUDIES OF RIVERSLEIGH, WORLD HERITAGE PROPERTY, OLIGO-MIOCENE FOSSIL LOCALITIES, NORTH-WESTERN QUEENSLAND, AUSTRALIA Kenny J mes TRAVOUILLON Thesis submitted for the degree of Doctor of Philoso.hy t the University of Ne0 South W les, Austr li August, 2008 i N1 d2ordre Ann3e 2008 THESE .r3sent3e devant l2UNIVERSITE CLAUDE BERNARD - LYON 1 .our l2obtention du DIPLOME DE DOCTORAT 8 rr9t3 du 7 o;t 2006 et rr9t3 du 6 j nvier 2005) Souten nce : Novembre 2008 . r M. Kenny J mes TRAVOUILLON TITRE : ETUDES PALEOECOLOGIQUES ET BIOCHRONOLOGIQUES DES GISEMENTS FOSSILIFERES DE L2OLIGO-MIOCENE DE RIVERSLEIGH, WORLD HERITAGE PROPERTY, NORD-OUEST DU QUEENSLAND, AUSTRALIE Directeur de thBse : Dr Serge Legendre Prof Mich el Archer Dr SuC nne H nd JURY : Dr. Serge Legendre Directeur de ThBse Pr. Mich el Archer Directeur de ThBse Pr. Christo.he Lecuyer ED min teur Dr. Gilles Esc rguel ED min teur Dr. So.hie Montuire R ..orteur Pr. Phili. Gingerich R ..orteur Dr. M nuel Hern ndeC Fern ndeC Ra..orteur ii THE UNIVERSITY OF NEW SOUTH WALES ThesisEDissert tion Sheet Surname or Family name: Tr vouillon First name: Kenny Other name/s: J mes Abbreviation for degree as given in the University calendar: PhD School: BEES Faculty: Science itle: PALAEOECOLOGICAL AND BIOCHRONOLOGICAL STUDIES OF RIVERSLEIGH, WORLD HERITAGE PROPERTY, OLIGO-MIOCENE FOSSIL LOCALITIES, NORTH-WESTERN QUEENSLAND, AUSTRALIA Abstr ct 350 0ords m Dimum: Riversleigh, World Heritage Property, located in North-western Queensland, Australia, contains over 200 fossil bearing localities from the Oligo-Miocene. The study presented here aims at finding new methods to improve the accuracy of palaeoecological and biochronological studies and describe the palaeoenvironmental and chronological settings of the Riversleigh fossil deposits.