Overdone Overkill E the Archaeological Perspective on Tasmanian Megafaunal Extinctions
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THYLACOLEO CARNIFEX and the NARACOORTE CAVES Michael Curry, Liz Reed1,2 and Steve Bourne3
RESEARCH CATCHING the MARSUPIAL ‘LION’ by the TAIL: THYLACOLEO CARNIFEX and the NARACOORTE CAVES Michael Curry, Liz Reed1,2 and Steve Bourne3 1School of Physical Sciences, The University of Adelaide, Adelaide, SA, Australia; 2School of Biological Sciences, Flinders University, Bedford Park, SA, Australia; 3Naracoorte Lucindale Council, Naracoorte, SA, Australia. “Thylacoleo exemplifies the simplest and most effective dental machinery for predatory life and carnivorous diet known in the Mammalian class. It is the extreme modification, to this end, of the Diprotodont type of Marsupialia.” Owen (1866) Introduction defending Thylacoleo as “A very gentle beast, and of good conscience” (Macleay 1859). Macleay based his Of all the extinct Australian Pleistocene megafauna argument on Thylacoleo’s relationship with other species, Thylacoleo carnifex (the marsupial ‘lion’) has Diprotodont marsupials, most of which are herbivores. captured the imagination and interest of people more Gerard Krefft, Curator of the Australian Museum, was than any other. Perhaps it is the allure of its predatory almost equally as unimpressed with Thylacoleo’s habits, (Australia’s Pleistocene answer to T. rex); or the carnivory, opining that it “…was not much more intriguing notion that it used caves as dens (Lundelius, carnivorous than the Phalangers (possums) of present 1966 ). It is certainly an enigma and, as Owen (1866) time.” (Krefft, 1866). Owen, meanwhile, had received an suggested, an extreme and meat-eating version of the almost complete skull from the Darling Downs, in otherwise herbivorous diprotodont marsupials. Queensland and published a more detailed paper, Spectacular fossil finds over the past few decades have further describing the skull and teeth of Thylacoleo, put to rest much of the speculation regarding its habits acknowledging its diprotodont affiliation but more and morphology. -
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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. -
Marsupial Fossils from Wellington Caves, New South Wales; the Historic and Scientific Significance of the Collections in the Australian Museum, Sydney
AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS Dawson, Lyndall, 1985. Marsupial fossils from Wellington Caves, New South Wales; the historic and scientific significance of the collections in the Australian Museum, Sydney. Records of the Australian Museum 37(2): 55–69. [1 August 1985]. doi:10.3853/j.0067-1975.37.1985.335 ISSN 0067-1975 Published by the Australian Museum, Sydney naturenature cultureculture discover discover AustralianAustralian Museum Museum science science is is freely freely accessible accessible online online at at www.australianmuseum.net.au/publications/www.australianmuseum.net.au/publications/ 66 CollegeCollege Street,Street, SydneySydney NSWNSW 2010,2010, AustraliaAustralia Records of the Australian Museum (1985) Vo!. 37(2): 55-69. ISSN·1975·0067. 55 Marsupial Fossils from Wellington Caves, New South Wales; the Historic and Scientific Significance of the Collections in the Australian Museum, Sydney LYNDALL DAWSON School of Zoology, University of New South Wales, Kensington, N.S.W., 2033 ABSTRACT. Since 1830, fossil vertebrates, particularly marsupials, have been collected from Wellington Caves, New South Wales. The history of these collections, and particularly of the collection housed in the Australian Museum, Sydney, is reviewed in this paper. A revised faunal list of marsupials from Wellington Caves is included, based on specimens in mUSeum collections. The provenance of these specimens is discussed. The list comprises 58 species, of which 30 are extinct throughout Australia, and a further 12 no longer inhabit the Wellington region. The deposit also contains bones of reptiles, birds, bats, rodents and monotremeS. On the basis of faunal correlation and some consideration of taphonomy in the deposits, the age range of the fossils represented in the mUSeum collections is suggested to be from the late Pliocene to late Pleistocene (with a possible minimum age of 40,000 years BP). -
On the Evolution of Kangaroos and Their Kin (Family Macropodidae) Using Retrotransposons, Nuclear Genes and Whole Mitochondrial Genomes
ON THE EVOLUTION OF KANGAROOS AND THEIR KIN (FAMILY MACROPODIDAE) USING RETROTRANSPOSONS, NUCLEAR GENES AND WHOLE MITOCHONDRIAL GENOMES William George Dodt B.Sc. (Biochemistry), B.Sc. Hons (Molecular Biology) Principal Supervisor: Dr Matthew J Phillips (EEBS, QUT) Associate Supervisor: Dr Peter Prentis (EEBS, QUT) External Supervisor: Dr Maria Nilsson-Janke (Senckenberg Biodiversity and Research Centre, Frankfurt am Main) Submitted in fulfilment of the requirements for the degree of Doctor of Philosophy Science and Engineering Faculty Queensland University of Technology 2018 1 Keywords Adaptive radiation, ancestral state reconstruction, Australasia, Bayesian inference, endogenous retrovirus, evolution, hybridization, incomplete lineage sorting, incongruence, introgression, kangaroo, Macropodidae, Macropus, mammal, marsupial, maximum likelihood, maximum parsimony, molecular dating, phylogenetics, retrotransposon, speciation, systematics, transposable element 2 Abstract The family Macropodidae contains the kangaroos, wallaroos, wallabies and several closely related taxa that occupy a wide variety of habitats in Australia, New Guinea and surrounding islands. This group of marsupials is the most species rich family within the marsupial order Diprotodontia. Despite significant investigation from previous studies, much of the evolutionary history of macropodids (including their origin within Diprotodontia) has remained unclear, in part due to an incomplete early fossil record. I have utilized several forms of molecular sequence data to shed -
Of the Early Pleistocene Nelson Bay Local Fauna, Victoria, Australia
Memoirs of Museum Victoria 74: 233–253 (2016) Published 2016 ISSN 1447-2546 (Print) 1447-2554 (On-line) http://museumvictoria.com.au/about/books-and-journals/journals/memoirs-of-museum-victoria/ The Macropodidae (Marsupialia) of the early Pleistocene Nelson Bay Local Fauna, Victoria, Australia KATARZYNA J. PIPER School of Geosciences, Monash University, Clayton, Vic 3800, Australia ([email protected]) Abstract Piper, K.J. 2016. The Macropodidae (Marsupialia) of the early Pleistocene Nelson Bay Local Fauna, Victoria, Australia. Memoirs of Museum Victoria 74: 233–253. The Nelson Bay Local Fauna, near Portland, Victoria, is the most diverse early Pleistocene assemblage yet described in Australia. It is composed of a mix of typical Pleistocene taxa and relict forms from the wet forests of the Pliocene. The assemblage preserves a diverse macropodid fauna consisting of at least six genera and 11 species. A potentially new species of Protemnodon is also possibly shared with the early Pliocene Hamilton Local Fauna and late Pliocene Dog Rocks Local Fauna. Together, the types of species and the high macropodid diversity suggests a mosaic environment of wet and dry sclerophyll forest with some open grassy areas was present in the Nelson Bay area during the early Pleistocene. Keywords Early Pleistocene marsupials, Macropodinae, Nelson Bay Local Fauna, Australia, Protemnodon, Hamilton Local Fauna. Introduction Luckett (1993) and Luckett and Woolley (1996). All specimens are registered in the Museum Victoria palaeontology collection The Macropodoidea (kangaroos and relatives) are one of the (prefix NMV P). All measurements are in millimetres. most conspicuous elements of the Australian fauna and are often also common in fossil faunas. -
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. -
FIELDIANA Geology
FIELDIANA Geology Publistied by Field Museum of Natural History New Series, No. 8 THE FAMILIES AND GENERA OF MARSUPIALIA LARRY G.MARSHALL •.981 UBRARY FIELD m^cim July 20, 1981 Publication 1320 THE FAMILIES AND GENERA OF MARSUPIALIA FIELDIANA Geology Published by Field Museum of Natural History New Series, No. 8 THE FAMILIES AND GENERA OF MARSUPIALIA LARRY G.MARSHALL Assistant Curator of Fossil Mammals DqMirtment of Geology Field Museum of Natural History Accepted for publication August 6, 1979 July 20, 1981 Publication 1320 Library of Congress Catalog No.: 81-65225 ISSN 0096-2651 PRINTED IN THE UNITED STATES OF AMERICA CONTENTS Part A 1 i^4troduc^on 1 Review of History and Development of Marsupial Systematics 1 Part B 19 Detailed Classification of Families and Genera of Marsupialia 19 I. New World and European Marsupialia 19 Fam. Didelphidae 19 Subfam. Dideiphinae 19 Subfam. Caluromyinae 21 *Subfam. Glasbiinae 21 *Subfam. Caroloameghiniinae 21 •Fam. Sparassocynidae 21 •Fam. Pediomyidae 21 Fam. Microbiotheriidae 21 •Fam. Stagodonddae 22 •Fam. Borhyaenidae 22 •Subfam. Hathlyacyninae 22 •Subfam. Borhyaeninae 23 •Subfam. Prothylacyninae 23 •Subfam. Proborhyaeninae 23 •Fam. Thylacosmilidae 23 •Fam. Argyrolagidae 24 Fam. Caenolesddae 24 Subfam. Caenolestinae 24 Tribe Caenolestini 24 •Tribe Pichipilini 24 •Subfam. Palaeothentinae 24 •Subfam. Abderitinae 25 •Tribe Parabderitini 25 •Tribe Abderitini 25 •Fam. Polydolopidae 25 •Fam. Groeberiidae 25 Marsupialia incertae sedis 25 Marsupialia(?) 25 II. Australasian Marsupialia 26 Fam. Dasyuridae 26 Subfam. Dasyurinae 26 Tribe Dasyurini 26 Tribe Sarcophilini 26 Fam. Myrmecobiidae 27 •Fam. Thylacinidae 27 Fam. Peramelidae 27 Fam. Thylacomyidae 27 Fam. Notoryctidae 27 Fam. Phalangeridae 27 Subfam. Phalangerinae 27 Subfam. Trichosurinae 28 •Fam. -
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. -
Prevalence of Macropod Progressive Periodontal Disease (“Lumpy Jaw”) in Wild Western Grey Kangaroos (Macropus Fuliginosus)
Prevalence of Macropod Progressive Periodontal Disease (“lumpy jaw”) in wild western grey kangaroos (Macropus fuliginosus) Authors: Rendle, Jessica, Yeap, Lian, Jackson, Bethany, Warren, Kristin, Ward, Samantha J., et al. Source: Journal of Vertebrate Biology, 69(4) Published By: Institute of Vertebrate Biology, Czech Academy of Sciences URL: https://doi.org/10.25225/jvb.20030 BioOne Complete (complete.BioOne.org) is a full-text database of 200 subscribed and open-access titles in the biological, ecological, and environmental sciences published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Complete website, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/terms-of-use. Usage of BioOne Complete content is strictly limited to personal, educational, and non - commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. Downloaded From: https://bioone.org/journals/Journal-of-Vertebrate-Biology on 07 Dec 2020 Terms of Use: https://bioone.org/terms-of-use Journal of Open Access Vertebrate Biology J. Vertebr. Biol. 2020, 69(4): 20030 DOI: 10.25225/jvb.20030 Prevalence of Macropod Progressive -
Extinctions, Modern Examples Of
EXTINCTIONS, MODERN EXAMPLES OF Ga´bor. L. Lo¨ vei University of Aarhus I. Species Life Spans can trigger a chain of extinctions, the ‘‘B.’’ For ex- II. Examples, Postglacial ample, when the passenger pigeon died out, at least III. Examples, First-Contact Extinctions two feather lice parasites followed it into extinc- IV. Examples, Historical Extinctions (1600–) tion. ‘‘Coextinction’’ occurs when more than one V. Examples, Extinction Cascades species dies out at the same time (this by definition VI. Problems in our Understanding of must happen when the host of an obligate parasite Extinctions dies out). VII. Theoretical Aspects of Extinction first-contact extinctions A wave of extinction of spe- VIII. The Present: A Full-Fledged Mass cies native to a continent or island, following the Extinction first arrival of humans to that area. living dead A term coined by the American tropical biologist, Daniel Janzen, denoting the last living individuals of a species destined to extinction. By GLOSSARY definition, extinction happens when the last individual of a species dies. In reality, however, ex- extinction Disappearance of the last living individual tinction of a species can be certain even earlier. of a species. Extinction can be ‘‘local B,’’ if it con- Most species need both males and females to re- cerns a definite population or location; we speak of produce. If there are no fertile individuals of one ‘‘B in the wild’’ when the only individuals alive of a sex, the species is doomed to extinction even if species are in captivity; and of ‘‘global B’’ when no several individuals are still alive.