Apostles Vs Fossils
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Life History, Mating Behavior, and Multiple Paternity in Octopus
LIFE HISTORY, MATING BEHAVIOR, AND MULTIPLE PATERNITY IN OCTOPUS OLIVERI (BERRY, 1914) (CEPHALOPODA: OCTOPODIDAE) A DISSERTATION SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAI´I AT MĀNOA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN ZOOLOGY DECEMBER 2014 By Heather Anne Ylitalo-Ward Dissertation Committee: Les Watling, Chairperson Rob Toonen James Wood Tom Oliver Jeff Drazen Chuck Birkeland Keywords: Cephalopod, Octopus, Sexual Selection, Multiple Paternity, Mating DEDICATION To my family, I would not have been able to do this without your unending support and love. Thank you for always believing in me. ii ACKNOWLEDGMENTS I would like to thank all of the people who helped me collect the specimens for this study, braving the rocks and the waves in the middle of the night: Leigh Ann Boswell, Shannon Evers, and Steffiny Nelson, you were the hard core tako hunters. I am eternally grateful that you sacrificed your evenings to the octopus gods. Also, thank you to David Harrington (best bucket boy), Bert Tanigutchi, Melanie Hutchinson, Christine Ambrosino, Mark Royer, Chelsea Szydlowski, Ily Iglesias, Katherine Livins, James Wood, Seth Ylitalo-Ward, Jessica Watts, and Steven Zubler. This dissertation would not have happened without the support of my wonderful advisor, Dr. Les Watling. Even though I know he wanted me to study a different kind of “octo” (octocoral), I am so thankful he let me follow my foolish passion for cephalopod sexual selection. Also, he provided me with the opportunity to ride in a submersible, which was one of the most magical moments of my graduate career. -
Husbandry Manual for BLUE-RINGED OCTOPUS Hapalochlaena Lunulata (Mollusca: Octopodidae)
Husbandry Manual for BLUE-RINGED OCTOPUS Hapalochlaena lunulata (Mollusca: Octopodidae) Date By From Version 2005 Leanne Hayter Ultimo TAFE v 1 T A B L E O F C O N T E N T S 1 PREFACE ................................................................................................................................ 5 2 INTRODUCTION ...................................................................................................................... 6 2.1 CLASSIFICATION .............................................................................................................................. 8 2.2 GENERAL FEATURES ....................................................................................................................... 8 2.3 HISTORY IN CAPTIVITY ..................................................................................................................... 9 2.4 EDUCATION ..................................................................................................................................... 9 2.5 CONSERVATION & RESEARCH ........................................................................................................ 10 3 TAXONOMY ............................................................................................................................12 3.1 NOMENCLATURE ........................................................................................................................... 12 3.2 OTHER SPECIES ........................................................................................................................... -
The University of Sydney
THE UNIVERSITY OF SYDNEY 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 Copyright Service. sydney.edu.au/copyright A STRUCTURAL ANALYSIS OF THE SOUTHERN HORNSBY PLATEAU, SYDNEY BASIN, NEW SOUTH WALES by Anthony Richard Norman, B.Sc. (Hons) A thesis submitted in fulfilment of the requirements for the degree of Master of Science DEPARTMENT OF GEOLOGY AND GEOPHYSICS UNIVERSITY OF SYDNEY September, 1986 ABSTRACT The Hornsby Plateau rises north of Sydney. Aerial photo interpretation of an area north of Hornsby and south of the Hawkesbury River revealed two well defined extensive traces. -
Background Paper on New South Wales Geology with a Focus on Basins Containing Coal Seam Gas Resources
Background Paper on New South Wales Geology With a Focus on Basins Containing Coal Seam Gas Resources for Office of the NSW Chief Scientist and Engineer by Colin R. Ward and Bryce F.J. Kelly School of Biological, Earth and Environmental Sciences University of New South Wales Date of Issue: 28 August 2013 Our Reference: J083550 CONTENTS Page 1. AIMS OF THE BACKGROUND PAPER .............................................................. 1 1.1. SIGNIFICANCE OF AUSTRALIAN CSG RESOURCES AND PRODUCTION ................... 1 1.2. DISCLOSURE .................................................................................................... 2 2. GEOLOGY AND EVALUATION OF COAL AND COAL SEAM GAS RESOURCES ............................................................................................................. 3 2.1. NATURE AND ORIGIN OF COAL ........................................................................... 3 2.2. CHEMICAL AND PHYSICAL PROPERTIES OF COAL ................................................ 4 2.3. PETROGRAPHIC PROPERTIES OF COAL ............................................................... 4 2.4. GEOLOGICAL FEATURES OF COAL SEAMS .......................................................... 6 2.5. NATURE AND ORIGIN OF GAS IN COAL SEAMS .................................................... 8 2.6. GAS CONTENT DETERMINATION ........................................................................10 2.7. SORPTION ISOTHERMS AND GAS HOLDING CAPACITY .........................................11 2.8. METHANE SATURATION ....................................................................................12 -
Exceptional Fossil Preservation During CO2 Greenhouse Crises? Gregory J
Palaeogeography, Palaeoclimatology, Palaeoecology 307 (2011) 59–74 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Exceptional fossil preservation during CO2 greenhouse crises? Gregory J. Retallack Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403, USA article info abstract Article history: Exceptional fossil preservation may require not only exceptional places, but exceptional times, as demonstrated Received 27 October 2010 here by two distinct types of analysis. First, irregular stratigraphic spacing of horizons yielding articulated Triassic Received in revised form 19 April 2011 fishes and Cambrian trilobites is highly correlated in sequences in different parts of the world, as if there were Accepted 21 April 2011 short temporal intervals of exceptional preservation globally. Second, compilations of ages of well-dated fossil Available online 30 April 2011 localities show spikes of abundance which coincide with stage boundaries, mass extinctions, oceanic anoxic events, carbon isotope anomalies, spikes of high atmospheric carbon dioxide, and transient warm-wet Keywords: Lagerstatten paleoclimates. Exceptional fossil preservation may have been promoted during unusual times, comparable with fi Fossil preservation the present: CO2 greenhouse crises of expanding marine dead zones, oceanic acidi cation, coral bleaching, Trilobite wetland eutrophication, sea level rise, ice-cap melting, and biotic invasions. Fish © 2011 Elsevier B.V. All rights reserved. Carbon dioxide Greenhouse 1. Introduction Zeigler, 1992), sperm (Nishida et al., 2003), nuclei (Gould, 1971)and starch granules (Baxter, 1964). Taphonomic studies of such fossils have Commercial fossil collectors continue to produce beautifully pre- emphasized special places where fossils are exceptionally preserved pared, fully articulated, complex fossils of scientific(Simmons et al., (Martin, 1999; Bottjer et al., 2002). -
Recognizing Cephalopod Boreholes in Shells and the Northward Spread of Octopus Vulgaris Cuvier, 1797 (Cephalopoda, Octopodoidea)
Vita Malacologica 13: 53-56 20 December 2015 Recognizing cephalopod boreholes in shells and the northward spread of Octopus vulgaris Cuvier, 1797 (Cephalopoda, Octopodoidea) Auke-Florian HIEMSTRA Middelstegracht 20B, 2312 TW Leiden, The Netherlands email: [email protected] Key words: Cephalopods, Octopus , predation, hole-boring, The Netherlands ABSTRACT & Arnold, 1969; Wodinsky, 1969; Hartwick et al., 1978; Boyle & Knobloch, 1981; Cortez et al., 1998; Steer & Octopuses prey on molluscs by boring through their shell. Semmens, 2003; Anderson et al., 2008; for taxonomical Among the regular naticid borings, traces of cephalopod pre - updates see Norman & Hochberg, 2005). However, the habit dation should be found soon on Dutch beaches. Bottom trawl - of drilling may prove to be more widespread within octopods ing has declined, and by the effects of global warming since only few species have actually been investigated Octopus will find its way back to the North Sea where it lived (Bromley, 1993). Drilled holes were found in polypla - before. I describe the distinguishing characters for Octopus cophoran, gastropod and bivalve mollusc shells, Nautilus and bore holes, give an introduction into this type of behaviour, crustacean carapaces (Tucker & Mapes, 1978; Saunders et al., present a short history of Dutch octopuses and a prediction of 1991; Nixon & Boyle, 1982; Guerra & Nixon, 1987; Nixon et their future. al., 1988; Mather & Nixon, 1990; Nixon, 1987). Arnold & Arnold (1969) and Wodinsky (1969) both describe the act of drilling in detail. This behaviour consists INTRODUCTION of the following steps (Wodinsky, 1969): recognizing and selecting the prey, drilling a hole in the shell, ejecting a secre - Aristotle was the first to observe octopuses feed on mol - tory substance into the drilled hole, and removing the mollusc luscs (see D’Arcy Thompson, 1910), but it was Fujita who from its shell and eating it. -
Timing and Dynamics of Late Pleistocene Mammal Extinctions in Southwestern Australia
Timing and dynamics of Late Pleistocene mammal extinctions in southwestern Australia Gavin J. Prideauxa,1, Grant A. Gullya, Aidan M. C. Couzensb, Linda K. Ayliffec, Nathan R. Jankowskid, Zenobia Jacobsd, Richard G. Robertsd, John C. Hellstrome, Michael K. Gaganc, and Lindsay M. Hatcherf aSchool of Biological Sciences, Flinders University, Bedford Park, South Australia 5042, Australia; bSchool of Earth and Environment, University of Western Australia, Crawley, Western Australia 6009, Australia; cResearch School of Earth Sciences, Australian National University, Canberra, Australian Capital Territory 0200, Australia; dCentre for Archaeological Science, School of Earth and Environmental Sciences, University of Wollongong, Wollongong, New South Wales 2522, Australia; eSchool of Earth Sciences, University of Melbourne, Melbourne, Victoria 3010, Australia; and fAugusta–Margaret River Tourism Association, Margaret River, Western Australia 6285, Australia Edited by Paul L. Koch, University of California, Santa Cruz, CA, and accepted by the Editorial Board November 1, 2010 (received for review July 27, 2010) Explaining the Late Pleistocene demise of many of the world’s larger tims, falling in alongside sediments and charcoal that were washed terrestrial vertebrates is arguably the most enduring and debated in via now-blocked solution pipes, although tooth marks on some topic in Quaternary science. Australia lost >90% of its larger species bones suggest that the carnivores Sarcophilus and Thylacoleo by around 40 thousand years (ka) ago, but the relative importance played a minor accumulating role. of human impacts and increased aridity remains unclear. Resolving To establish an environmental background against which TEC the debate has been hampered by a lack of sites spanning the last faunal changes could be analyzed, we investigated stratigraphic glacial cycle. -
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. -
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. -
Coal Resource Recovery Plan
Tahmoor Coal Pty Ltd COAL RESOURCE RECOVERY PLAN Tahmoor North Western Domain Longwalls West 1 and West 2 July 2019 simecgfg.com This page has been left blank intentionally. 2 | Tahmoor North Western Domain LW W1-W2 – Coal Resource Recovery Plan TAH-HSEC-243 (July 2019 Ver1) This page has been left blank intentionally. 4 | Tahmoor North Western Domain LW W1-W2 – Coal Resource Recovery Plan TAH-HSEC-243 (July 2019 Ver1) Table of Contents Table of Contents ....................................................................................................................... 5 List of Figures ............................................................................................................................. 7 List of Tables .............................................................................................................................. 7 1 Introduction ........................................................................................................................ 9 Background ............................................................................................................................... 9 Purpose ..................................................................................................................................... 9 Scope ......................................................................................................................................... 9 2 Regulatory Requirements ................................................................................................. -
Strategic Assessment Report, Heathcote Ridge, West Menai
STRATEGIC ASSESSMENT REPORT HEATHCOTE RIDGE, WEST MENAI November 2012 Prepared for Gandangara Local Aboriginal Land Council By Cumberland Ecology with input from BBC Consulting Planners and 1. PURPOSE AND DESCRIPTION .......................................................................... 3 1.1 Introduction ........................................................................................................ 3 1.1.1 Background........................................................................................................... 3 1.2 The Program ..................................................................................................... 4 1.2.1 Background........................................................................................................... 4 1.2.2 Proposed Development Concept ..................................................................... 5 1.3 Regional Context ............................................................................................. 12 1.4 Land Use Planning .......................................................................................... 13 1.4.1 Land to Which the SEPP Amendment will Apply ............................................ 13 1.4.2 Proposed Land Use Zones ................................................................................. 13 1.4.3 Principal Development Standards ................................................................... 14 1.4.4 Consent Authority ..............................................................................................