Origin and Beyond
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Microchiroptera: Mystacinidae) from Australia, with a Revised Diagnosis of the Genus
New Miocene Icarops material (Microchiroptera: Mystacinidae) from Australia, with a revised diagnosis of the genus SUZANNE HAND, MICHAEL ARCHER & HENK GODTHELP HAND, S.l., ARCHER, M. & GODTHELP, H., 2001:12:20. New Miocene lcarops material (Microchiroptera: Mystacinidae) from Australia, with a revised diagnosis of the genus. Memoirs of the Association of Australasian Palaeontologists 25,139-146. ISSN 0810-8889 New fossil material referable to Icarops paradox Hand et al., 1998 is described from the early Miocene Judith's Horizontalis Site in the Riversleigh World Heritage Property of northwestern Queensland. Fused dentaries contain the partial lower dentition of I. paradox. The diagnosis of the genus Icarops is revised. The new material confirms the identity of Icarops species as mystacinids and enablesre-examination of interrelationships between extinct and extant members of this Gondwanan bat family. S.J: Hand, M. Archer* & H. Godthelp, School of Biological Science, University of New South Wales,New South Wales, 2052; * also Australian Museum, 6-8 College St, Sydney, New South Wales,2000. Received ]4 December 2000 Keywords: Mystacinidae, Icarops, Mystacina, bat, lower dentition, Miocene, Riversleigh THE FIRST pre-Pleistocene record for the QMF refers to specimens held in the fossil Mystacinidae and first record of this bat family collections of the QueenslandMuseum, Brisbane. from outside New Zealand were reported by Hand et al. ( 1998) from Miocene sedimentsin Australia. SYSTEMAllC PALAEONTOLOGY Three species of the new mystacinid genus Icarops were described: Icarops breviceps from OrderCIllROPTERAB1wnenbach, 1779 the middle Miocene Bullock Creek deposit of the SuborderMICROCIllROPTERA Dobson, 1875 Northern Territory; I. aenae from the early SuperfamilyNocmIoNoIDEA Van Va1en, Miocene Wayne's Wok deposit, D Site Plateau, 1979 Riversleigh, northwestern Queensland; and I. -
The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
Artiodactyla and Perissodactyla (Mammalia) from the Early-Middle Eocene Kuldana Formation of Kohat (Pakistan)
CO"uTK1BL 11015 FKOLI IHt \lC5tLL1 OF I' ALEO\ IOLOG1 THE UNIVERSITY OF IVICHIGAN VOI 77 Lo 10 p 717-37.1 October 33 1987 ARTIODACTYLA AND PERISSODACTYLA (MAMMALIA) FROM THE EARLY-MIDDLE EOCENE KULDANA FORMATION OF KOHAT (PAKISTAN) BY J. G. M. THEWISSEN. P. D. GINGERICH and D. E. RUSSELL MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Charles B. Beck, Director Jennifer A. Kitchell, Editor This series of contributions from the Museum of Paleontology is a medium for publication of papers based chiefly on collections in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate issues may also be obtained by request. Correspond- ence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48109. VOLS. II-XXVII. Parts of volumes may be obtained if available. Price lists are available upon inquiry. I ARTIODACTI L .-I A\D PERISSODACTYL4 (kl.iihlhlAL1A) FROM THE EARLY-h1IDDLE EOCEUE KCLD..I\4 FORMATIO\ OF KOHAT (PAKISTAY) J. G. M. THEWISSEN. P. D. GINGERICH AND D. E. RUSSELL Ah.strcict.-Chorlakki. yielding approximately 400 specimens (mostly isolated teeth and bone fragments). is one of four major early-to-middle Eocene niammal localities on the Indo-Pakistan subcontinent. On the basis of ung~~latesclescribed in this paper we consider the Chorlakki fauna to be younger than that from Barbora Banda. -
Inferring Echolocation in Ancient Bats Arising From: N
NATURE | Vol 466 | 19 August 2010 BRIEF COMMUNICATIONS ARISING Inferring echolocation in ancient bats Arising from: N. Veselka et al. Nature 463, 939–942 (2010) Laryngeal echolocation, used by most living bats to form images of O. finneyi falls outside the size range seen in living echolocating bats their surroundings and to detect and capture flying prey1,2, is con- and is similar to the proportionally smaller cochleae of bats that lack sidered to be a key innovation for the evolutionary success of bats2,3, laryngeal echolocation4,8, suggesting that it did not echolocate. and palaeontologists have long sought osteological correlates of echolocation that can be used to infer the behaviour of fossil bats4–7. Veselka et al.8 argued that the most reliable trait indicating echoloca- tion capabilities in bats is an articulation between the stylohyal bone (part of the hyoid apparatus that supports the throat and larynx) and a the tympanic bone, which forms the floor of the middle ear. They examined the oldest and most primitive known bat, Onychonycteris finneyi (early Eocene, USA4), and argued that it showed evidence of this stylohyal–tympanic articulation, from which they concluded that O. finneyi may have been capable of echolocation. We disagree with their interpretation of key fossil data and instead argue that O. finneyi was probably not an echolocating bat. The holotype of O. finneyi shows the cranial end of the left stylohyal resting on the tympanic bone (Fig. 1c–e). However, the stylohyal on the right side is in a different position, the tip of the stylohyal extends beyond the tympanic on both sides of the skull, and both tympanics are crushed. -
NM IF C3 4 16 Fossil Imprint
FOSSIL IMPRINT • vol. 72 • 2016 • no. 3-4 • pp. 183–201 (formerly ACTA MUSEI NATIONALIS PRAGAE, Series B – Historia Naturalis) HIPPOPOTAMODON ERYMANTHIUS (SUIDAE, MAMMALIA) FROM MAHMUTGAZI, DENIZLI-ÇAL BASIN, TURKEY MARTIN PICKFORD Sorbonne Universités – CR2P, MNHN, CNRS, UPMC – Paris VI, 8, rue Buffon, 75005, Paris, France; e-mail: [email protected]. Pickford, M. (2016): Hippopotamodon erymanthius (Suidae, Mammalia) from Mahmutgazi, Denizli-Çal Basin, Turkey. – Fossil Imprint, 72(3-4): 183–201, Praha. ISSN 2533-4050 (print), ISSN 2533-4069 (on-line). Abstract: The Staatliches Museum für Naturkunde in Karlsruhe houses an interesting collection of Turolian mammals from Mahmutgazi, Turkey, among which is a comprehensive sample of the large suid, Hippopotamodon erymanthius. The fossils plot out within the range of metric variation of H. erymanthius from Pikermi and Samos, Greece, but lie at the lower end of the range. Like the suids from these sites, the Mahmutgazi specimens lack the first premolar. Overall, the Mahmutgazi sample is metrically and morphologically close to the material from Akkaşdağı, Turkey. The upper and lower third molars and fourth premolars are, on average, smaller than those of Hippopotamodon major from Luberon, France (MN 13). Two undescribed fossils of H. ery- manthius from Pikermi are housed at the SMNK, and are included in this paper in order to fill out the data base for the species at this locality. The chronological position, palaeoecology and sexual dimorphism of the Mahmutgazi suids are discussed. Key words: Suidae, Late Miocene, Turkey, Hippopotamodon, biochronology, palaeoecology, sexual dimorphism Received: October 10, 2016 | Accepted: November 28, 2016 | Issued: December 30, 2016 Introduction (2010) mentions suids at the site, and correlated it to MN 11–12 (Early to Middle Turolian). -
Chapter 1 - Introduction
EURASIAN MIDDLE AND LATE MIOCENE HOMINOID PALEOBIOGEOGRAPHY AND THE GEOGRAPHIC ORIGINS OF THE HOMININAE by Mariam C. Nargolwalla A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Graduate Department of Anthropology University of Toronto © Copyright by M. Nargolwalla (2009) Eurasian Middle and Late Miocene Hominoid Paleobiogeography and the Geographic Origins of the Homininae Mariam C. Nargolwalla Doctor of Philosophy Department of Anthropology University of Toronto 2009 Abstract The origin and diversification of great apes and humans is among the most researched and debated series of events in the evolutionary history of the Primates. A fundamental part of understanding these events involves reconstructing paleoenvironmental and paleogeographic patterns in the Eurasian Miocene; a time period and geographic expanse rich in evidence of lineage origins and dispersals of numerous mammalian lineages, including apes. Traditionally, the geographic origin of the African ape and human lineage is considered to have occurred in Africa, however, an alternative hypothesis favouring a Eurasian origin has been proposed. This hypothesis suggests that that after an initial dispersal from Africa to Eurasia at ~17Ma and subsequent radiation from Spain to China, fossil apes disperse back to Africa at least once and found the African ape and human lineage in the late Miocene. The purpose of this study is to test the Eurasian origin hypothesis through the analysis of spatial and temporal patterns of distribution, in situ evolution, interprovincial and intercontinental dispersals of Eurasian terrestrial mammals in response to environmental factors. Using the NOW and Paleobiology databases, together with data collected through survey and excavation of middle and late Miocene vertebrate localities in Hungary and Romania, taphonomic bias and sampling completeness of Eurasian faunas are assessed. -
(Suidae, Artiodactyla) from the Upper Miocene of Hayranlı-Haliminhanı, Turkey
Turkish Journal of Zoology Turk J Zool (2013) 37: 106-122 http://journals.tubitak.gov.tr/zoology/ © TÜBİTAK Research Article doi:10.3906/zoo-1202-4 Microstonyx (Suidae, Artiodactyla) from the Upper Miocene of Hayranlı-Haliminhanı, Turkey 1 2 3, Jan VAN DER MADE , Erksin GÜLEÇ , Ahmet Cem ERKMAN * 1 Spanish National Research Council, National Museum of Natural Sciences, Madrid, Spain 2 Department of Anthropology, Faculty of Languages, History, and Geography, Ankara University, Ankara, Turkey 3 Department of Anthropology, Faculty of Science and Literature, Ahi Evran University, Kırşehir, Turkey Received: 05.02.2012 Accepted: 11.07.2012 Published Online: 24.12.2012 Printed: 21.01.2013 Abstract: The suid remains from localities 58-HAY-2 and 58-HAY-19 in the Late Miocene Derindere Member of the İncesu Formation in the Hayranlı-Haliminhanı area (Sivas, Turkey) are described and referred to as Microstonyx major (Gervais, 1848–1852). Microstonyx shows changes in incisor morphology, which are interpreted as a further adaptation to rooting. This occurred probably in a short period between 8.7 and 8.121 Ma ago and possibly is a reaction to environmental change. The incisor morphology in locality 58-HAY-2 suggests that it is temporally close to this change, which would imply that this locality and the lithostratigraphically lower 58-HAY-19 belong to the lower part of MN11 and not to MN12. The findings are discussed in the regional context and contribute to the knowledge of the Anatolian fossil mammals. Key words: Suidae, Microstonyx, rooting, ecology, Late Miocene 1. Introduction 1.1. Location and stratigraphy The first of the Hayranlı-Haliminhanı fossil localities was Anatolia lies at the intersection of Asia, Europe, and Afro- discovered in 1993 by members of the Vertebrate Fossils Arabia, and its geology has been subject to the plate tectonic Research Project, a collaborative survey effort. -
BIO 313 ANIMAL ECOLOGY Corrected
NATIONAL OPEN UNIVERSITY OF NIGERIA SCHOOL OF SCIENCE AND TECHNOLOGY COURSE CODE: BIO 314 COURSE TITLE: ANIMAL ECOLOGY 1 BIO 314: ANIMAL ECOLOGY Team Writers: Dr O.A. Olajuyigbe Department of Biology Adeyemi Colledge of Education, P.M.B. 520, Ondo, Ondo State Nigeria. Miss F.C. Olakolu Nigerian Institute for Oceanography and Marine Research, No 3 Wilmot Point Road, Bar-beach Bus-stop, Victoria Island, Lagos, Nigeria. Mrs H.O. Omogoriola Nigerian Institute for Oceanography and Marine Research, No 3 Wilmot Point Road, Bar-beach Bus-stop, Victoria Island, Lagos, Nigeria. EDITOR: Mrs Ajetomobi School of Agricultural Sciences Lagos State Polytechnic Ikorodu, Lagos 2 BIO 313 COURSE GUIDE Introduction Animal Ecology (313) is a first semester course. It is a two credit unit elective course which all students offering Bachelor of Science (BSc) in Biology can take. Animal ecology is an important area of study for scientists. It is the study of animals and how they related to each other as well as their environment. It can also be defined as the scientific study of interactions that determine the distribution and abundance of organisms. Since this is a course in animal ecology, we will focus on animals, which we will define fairly generally as organisms that can move around during some stages of their life and that must feed on other organisms or their products. There are various forms of animal ecology. This includes: • Behavioral ecology, the study of the behavior of the animals with relation to their environment and others • Population ecology, the study of the effects on the population of these animals • Marine ecology is the scientific study of marine-life habitat, populations, and interactions among organisms and the surrounding environment including their abiotic (non-living physical and chemical factors that affect the ability of organisms to survive and reproduce) and biotic factors (living things or the materials that directly or indirectly affect an organism in its environment). -
HOVASAURUS BOULEI, an AQUATIC EOSUCHIAN from the UPPER PERMIAN of MADAGASCAR by P.J
99 Palaeont. afr., 24 (1981) HOVASAURUS BOULEI, AN AQUATIC EOSUCHIAN FROM THE UPPER PERMIAN OF MADAGASCAR by P.J. Currie Provincial Museum ofAlberta, Edmonton, Alberta, T5N OM6, Canada ABSTRACT HovasauTUs is the most specialized of four known genera of tangasaurid eosuchians, and is the most common vertebrate recovered from the Lower Sakamena Formation (Upper Per mian, Dzulfia n Standard Stage) of Madagascar. The tail is more than double the snout-vent length, and would have been used as a powerful swimming appendage. Ribs are pachyostotic in large animals. The pectoral girdle is low, but massively developed ventrally. The front limb would have been used for swimming and for direction control when swimming. Copious amounts of pebbles were swallowed for ballast. The hind limbs would have been efficient for terrestrial locomotion at maturity. The presence of long growth series for Ho vasaurus and the more terrestrial tan~saurid ThadeosauTUs presents a unique opportunity to study differences in growth strategies in two closely related Permian genera. At birth, the limbs were relatively much shorter in Ho vasaurus, but because of differences in growth rates, the limbs of Thadeosau rus are relatively shorter at maturity. It is suggested that immature specimens of Ho vasauTUs spent most of their time in the water, whereas adults spent more time on land for mating, lay ing eggs and/or range dispersal. Specilizations in the vertebrae and carpus indicate close re lationship between Youngina and the tangasaurids, but eliminate tangasaurids from consider ation as ancestors of other aquatic eosuchians, archosaurs or sauropterygians. CONTENTS Page ABREVIATIONS . ..... ... ......... .......... ... ......... ..... ... ..... .. .... 101 INTRODUCTION . -
Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology
Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology by Paul David Polly B.A. (University of Texas at Austin) 1987 A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Paleontology in the GRADUATE DIVISION of the UNIVERSITY of CALIFORNIA at BERKELEY Committee in charge: Professor William A. Clemens, Chair Professor Kevin Padian Professor James L. Patton Professor F. Clark Howell 1993 Hyaenodontidae (Creodonta, Mammalia) and the Position of Systematics in Evolutionary Biology © 1993 by Paul David Polly To P. Reid Hamilton, in memory. iii TABLE OF CONTENTS Introduction ix Acknowledgments xi Chapter One--Revolution and Evolution in Taxonomy: Mammalian Classification Before and After Darwin 1 Introduction 2 The Beginning of Modern Taxonomy: Linnaeus and his Predecessors 5 Cuvier's Classification 10 Owen's Classification 18 Post-Darwinian Taxonomy: Revolution and Evolution in Classification 24 Kovalevskii's Classification 25 Huxley's Classification 28 Cope's Classification 33 Early 20th Century Taxonomy 42 Simpson and the Evolutionary Synthesis 46 A Box Model of Classification 48 The Content of Simpson's 1945 Classification 50 Conclusion 52 Acknowledgments 56 Bibliography 56 Figures 69 Chapter Two: Hyaenodontidae (Creodonta, Mammalia) from the Early Eocene Four Mile Fauna and Their Biostratigraphic Implications 78 Abstract 79 Introduction 79 Materials and Methods 80 iv Systematic Paleontology 80 The Four Mile Fauna and Wasatchian Biostratigraphic Zonation 84 Conclusion 86 Acknowledgments 86 Bibliography 86 Figures 87 Chapter Three: A New Genus Eurotherium (Creodonta, Mammalia) in Reference to Taxonomic Problems with Some Eocene Hyaenodontids from Eurasia (With B. Lange-Badré) 89 Résumé 90 Abstract 90 Version française abrégéé 90 Introduction 93 Acknowledgments 96 Bibliography 96 Table 3.1: Original and Current Usages of Genera and Species 99 Table 3.2: Species Currently Included in Genera Discussed in Text 101 Chapter Four: The skeleton of Gazinocyon vulpeculus n. -
Gorgonopsia: Rubidgeinae) with Implications for the Identity of This Species
Rediscovery of the holotype of Clelandina major Broom, 1948 (Gorgonopsia: Rubidgeinae) with implications for the identity of this species Christian F. Kammerer North Carolina Museum of Natural Sciences, 11 W. Jones Street, Raleigh, North Carolina 27604, U.S.A., and Evolutionary Studies Institute, University of the Witwatersrand, Private Bag 3, WITS, Johannesburg, 2050 South Africa E-mail: [email protected] Received 7 November 2017. Accepted 8 December 2017 No specimen number was given for the holotype of the rubidgeine gorgonopsian species Clelandina major Broom, 1948 in its original description. Historically, a specimen in the Rubidge Collection (RC 94) was considered to represent Broom’s type specimen for C. major. However, recent study has revealed that the holotype of C. major is in fact a different specimen in the McGregor Museum in Kimberley (MMK 5031). The morphology of this specimen is consistent with the genus Clelandina, contra work based on RC 94 that considered C. major referable to Aelurognathus. Clelandina major is here considered synonymous with the type species Clelandina rubidgei. MMK 5031 represents only the fifth known specimen of this rare and unusual gorgonopsian. Keywords: Synapsida, Therapsida, Gorgonopsia, Permian, holotype, taxonomy. Palaeontologia africana 2017. ©2017 Christian F.Kammerer. This is an open-access article published under the Creative Commons Attribution 4.0 Unported License (CC BY4.0). To view a copy of the license, please visit http://creativecommons.org/licenses/by/4.0/. This license permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. The article is permanently archived at: http://wiredspace.wits.ac.za/handle/10539/23480 INTRODUCTION provided no specimen numbers for the holotypes of Clelandina is one of the rarest and most unusual C. -
Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming
Distribution and Stratigraphip Correlation of Upper:UB_ • Ju Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming U,S. GEOLOGICAL SURVEY PROFESS IONAL PAPER 1540 Cover. A member of the American Museum of Natural History 1896 expedition enter ing the badlands of the Willwood Formation on Dorsey Creek, Wyoming, near what is now U.S. Geological Survey fossil vertebrate locality D1691 (Wardel Reservoir quadran gle). View to the southwest. Photograph by Walter Granger, courtesy of the Department of Library Services, American Museum of Natural History, New York, negative no. 35957. DISTRIBUTION AND STRATIGRAPHIC CORRELATION OF UPPER PALEOCENE AND LOWER EOCENE FOSSIL MAMMAL AND PLANT LOCALITIES OF THE FORT UNION, WILLWOOD, AND TATMAN FORMATIONS, SOUTHERN BIGHORN BASIN, WYOMING Upper part of the Will wood Formation on East Ridge, Middle Fork of Fifteenmile Creek, southern Bighorn Basin, Wyoming. The Kirwin intrusive complex of the Absaroka Range is in the background. View to the west. Distribution and Stratigraphic Correlation of Upper Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Tatman Formations, Southern Bighorn Basin, Wyoming By Thomas M. Down, Kenneth D. Rose, Elwyn L. Simons, and Scott L. Wing U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1540 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director For sale by U.S. Geological Survey, Map Distribution Box 25286, MS 306, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S.