A New Classification of Mammals George Gaylord Simpson
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New Materials of Chalicotherium Brevirostris (Perissodactyla, Chalicotheriidae)
Geobios 45 (2012) 369–376 Available online at www.sciencedirect.com Original article New materials of Chalicotherium brevirostris (Perissodactyla, Chalicotheriidae) § from the Tunggur Formation, Inner Mongolia Yan Liu *, Zhaoqun Zhang Laboratory of Evolutionary Systematics of Vertebrate, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, 142, Xizhimenwai Street, PO Box 643, Beijing 100044, PR China A R T I C L E I N F O A B S T R A C T Article history: Chalicotherium brevirostris was named by Colbert based on a skull lacking mandibles from the late Middle Received 23 March 2011 Miocene Tunggur Formation, Tunggur, Inner Mongolia, China. Here we describe new mandibular Accepted 6 October 2011 materials collected from the same area. In contrast to previous expectations, the new mandibular Available online 14 July 2012 materials show a long snout, long diastema, a three lower incisors and a canine. C. brevirostris shows some sexual dimorphism and intraspecific variation in morphologic characters. The new materials differ Keywords: from previously described C. cf. brevirostris from Cixian County (Hebei Province) and the Tsaidam Basin, Tunggur which may represent a different, new species close to C. brevirostris. The diagnosis of C. brevirostris is Middle Miocene revised. Chalicotheriinae Chalicotherium ß 2012 Elsevier Masson SAS. All rights reserved. 1. Abbreviations progress in understanding the Tunggur geology and paleontology (Qiu et al., 1988). The most important result of this expedition so far is -
Chronostratigraphy of the Mammal-Bearing Paleocene of South America 51
Thierry SEMPERE biblioteca Y. Joirriiol ofSoiiih Ainorirari Euirli Sciriin~r.Hit. 111. No. 1, pp. 49-70, 1997 Pergamon Q 1‘197 PublisIlcd hy Elscvicr Scicncc Ltd All rights rescrvcd. Printed in Grcnt nrilsin PII: S0895-9811(97)00005-9 0895-9X 11/97 t I7.ol) t o.(x) -. ‘Inshute qfI Human Origins, 1288 9th Street, Berkeley, California 94710, USA ’Orstom, 13 rue Geoffroy l’Angevin, 75004 Paris, France 3Department of Geosciences, The University of Arizona, Tucson, Arizona 85721, USA Absfract - Land mammal faunas of Paleocene age in the southern Andean basin of Bolivia and NW Argentina are calibrated by regional sequence stratigraphy and rnagnetostratigraphy. The local fauna from Tiupampa in Bolivia is -59.0 Ma, and is thus early Late Paleocene in age. Taxa from the lower part of the Lumbrera Formation in NW Argentina (long regarded as Early Eocene) are between -58.0-55.5 Ma, and thus Late Paleocene in age. A reassessment of the ages of local faunas from lhe Rfo Chico Formation in the San Jorge basin, Patagonia, southern Argentina, shows that lhe local fauna from the Banco Negro Infeiior is -60.0 Ma, mak- ing this the most ancient Cenozoic mammal fauna in South,America. Critical reevaluation the ltaboraí fauna and associated or All geology in SE Brazil favors lhe interpretation that it accumulated during a sea-level lowsland between -$8.2-56.5 Ma. known South American Paleocene land inammal faunas are thus between 60.0 and 55.5 Ma (i.e. Late Paleocene) and are here assigned to the Riochican Land Maminal Age, with four subages (from oldest to youngest: Peligrian, Tiupampian, Ilaboraian, Riochican S.S.). -
Classification of Mammals 61
© Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FORCHAPTER SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION Classification © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC 4 NOT FORof SALE MammalsOR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC © Jones & Bartlett Learning, LLC NOT FOR SALE OR DISTRIBUTION NOT FOR SALE OR DISTRIBUTION © Jones & Bartlett Learning, LLC. NOT FOR SALE OR DISTRIBUTION. 2ND PAGES 9781284032093_CH04_0060.indd 60 8/28/13 12:08 PM CHAPTER 4: Classification of Mammals 61 © Jones Despite& Bartlett their Learning,remarkable success, LLC mammals are much less© Jones stress & onBartlett the taxonomic Learning, aspect LLCof mammalogy, but rather as diverse than are most invertebrate groups. This is probably an attempt to provide students with sufficient information NOT FOR SALE OR DISTRIBUTION NOT FORattributable SALE OR to theirDISTRIBUTION far greater individual size, to the high on the various kinds of mammals to make the subsequent energy requirements of endothermy, and thus to the inabil- discussions of mammalian biology meaningful. -
Paleocene Mammalian Faunas of the Bison Basin in South-Central Wyoming
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 131, NUMBER 6 Cftarlesi ©, anb JHarp ^aux SKHalcott 3Res!earcf) Jf unb PALEOCENE MAMMALIAN FAUNAS OF THE BISON BASIN IN SOUTH-CENTRAL WYOMING (With 16 Plates) By C. LEWIS GAZIN Curator, Division of Vertebrate Paleontology United States National Museum Smithsonian Institution (Publication 4229) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION FEBRUARY 28, 1956 THE LORD BALTIMORE PRESS, INC. BALTIMORE, MD., U. S. A. CONTENTS Page Introduction i Acknowledgments 2 History of investigation 2 Occurrence and preservation of material 3 The Bison basin faunas 4 Environment and relationships between the Bison basin faunas 7 Age and correlation of the faunas lo Systematic description of vertebrate remains I2 Reptilia 12 Sauria 12 Anguidae 12 Mammalia 12 Multitubcrculata 12 Ptilodontidae 12 Marsupialia 14 Didelphidae 14 Insectivora 15 Leptictidae 15 Pantolestidae 17 Primates 19 Plesiadapidae 19 Carnivora 25 Arctocyonidae 25 Mesonychidae 35 Miacidae 35 Condylarthra 36 Hyopsodontidae 36 Phenacodontidae 42 Pantodonta 47 Coryphodontidae 47 References 51 Explanation of plates 54 ILLUSTRATIONS Plates (All plates following page 58.) 1. Mullituberculates and insectivores from the Bison basin Paleocene. 2. Primates and marsupials from the Bison basin Paleocene. 3. Pronothodcctes from the Bison basin Paleocene. 4. Plcsiadapis from the Bison basin Paleocene. 5. Triccntcs and Chriacus from the Bison basin Paleocene. 6. Thryptacodon from the Bison basin Paleocene. 7. Clacnodon from the Bison basin Paleocene. 8. Litomylus and Protoselcnc? from the Bison basin Paleocene. 9. Haplaletes and Gidleyina from the Bison basin Paleocene. 10. Phcnacodusl from the Bison basin Paleocene. 11. Condylarths and Titanoidcs from the Bison basin Paleocene. 12. Caenolambda from the Bison basin Paleocene. -
Perissodactyla: Tapirus) Hints at Subtle Variations in Locomotor Ecology
JOURNAL OF MORPHOLOGY 277:1469–1485 (2016) A Three-Dimensional Morphometric Analysis of Upper Forelimb Morphology in the Enigmatic Tapir (Perissodactyla: Tapirus) Hints at Subtle Variations in Locomotor Ecology Jamie A. MacLaren1* and Sandra Nauwelaerts1,2 1Department of Biology, Universiteit Antwerpen, Building D, Campus Drie Eiken, Universiteitsplein, Wilrijk, Antwerp 2610, Belgium 2Centre for Research and Conservation, Koninklijke Maatschappij Voor Dierkunde (KMDA), Koningin Astridplein 26, Antwerp 2018, Belgium ABSTRACT Forelimb morphology is an indicator for order Perissodactyla (odd-toed ungulates). Modern terrestrial locomotor ecology. The limb morphology of the tapirs are widely accepted to belong to a single enigmatic tapir (Perissodactyla: Tapirus) has often been genus (Tapirus), containing four extant species compared to that of basal perissodactyls, despite the lack (Hulbert, 1973; Ruiz-Garcıa et al., 1985) and sev- of quantitative studies comparing forelimb variation in eral regional subspecies (Padilla and Dowler, 1965; modern tapirs. Here, we present a quantitative assess- ment of tapir upper forelimb osteology using three- Wilson and Reeder, 2005): the Baird’s tapir (T. dimensional geometric morphometrics to test whether bairdii), lowland tapir (T. terrestris), mountain the four modern tapir species are monomorphic in their tapir (T. pinchaque), and the Malayan tapir (T. forelimb skeleton. The shape of the upper forelimb bones indicus). Extant tapirs primarily inhabit tropical across four species (T. indicus; T. bairdii; T. terrestris; T. rainforest, with some populations also occupying pinchaque) was investigated. Bones were laser scanned wet grassland and chaparral biomes (Padilla and to capture surface morphology and 3D landmark analysis Dowler, 1965; Padilla et al., 1996). was used to quantify shape. -
Revised Stratigraphy of Neogene Strata in the Cocinetas Basin, La Guajira, Colombia
Swiss J Palaeontol (2015) 134:5–43 DOI 10.1007/s13358-015-0071-4 Revised stratigraphy of Neogene strata in the Cocinetas Basin, La Guajira, Colombia F. Moreno • A. J. W. Hendy • L. Quiroz • N. Hoyos • D. S. Jones • V. Zapata • S. Zapata • G. A. Ballen • E. Cadena • A. L. Ca´rdenas • J. D. Carrillo-Bricen˜o • J. D. Carrillo • D. Delgado-Sierra • J. Escobar • J. I. Martı´nez • C. Martı´nez • C. Montes • J. Moreno • N. Pe´rez • R. Sa´nchez • C. Sua´rez • M. C. Vallejo-Pareja • C. Jaramillo Received: 25 September 2014 / Accepted: 2 February 2015 / Published online: 4 April 2015 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2015 Abstract The Cocinetas Basin of Colombia provides a made exhaustive paleontological collections, and per- valuable window into the geological and paleontological formed 87Sr/86Sr geochronology to document the transition history of northern South America during the Neogene. from the fully marine environment of the Jimol Formation Two major findings provide new insights into the Neogene (ca. 17.9–16.7 Ma) to the fluvio-deltaic environment of the history of this Cocinetas Basin: (1) a formal re-description Castilletes (ca. 16.7–14.2 Ma) and Ware (ca. 3.5–2.8 Ma) of the Jimol and Castilletes formations, including a revised formations. We also describe evidence for short-term pe- contact; and (2) the description of a new lithostratigraphic riodic changes in depositional environments in the Jimol unit, the Ware Formation (Late Pliocene). We conducted and Castilletes formations. The marine invertebrate fauna extensive fieldwork to develop a basin-scale stratigraphy, of the Jimol and Castilletes formations are among the richest yet recorded from Colombia during the Neogene. -
B.Sc. II YEAR CHORDATA
B.Sc. II YEAR CHORDATA CHORDATA 16SCCZO3 Dr. R. JENNI & Dr. R. DHANAPAL DEPARTMENT OF ZOOLOGY M. R. GOVT. ARTS COLLEGE MANNARGUDI CONTENTS CHORDATA COURSE CODE: 16SCCZO3 Block and Unit title Block I (Primitive chordates) 1 Origin of chordates: Introduction and charterers of chordates. Classification of chordates up to order level. 2 Hemichordates: General characters and classification up to order level. Study of Balanoglossus and its affinities. 3 Urochordata: General characters and classification up to order level. Study of Herdmania and its affinities. 4 Cephalochordates: General characters and classification up to order level. Study of Branchiostoma (Amphioxus) and its affinities. 5 Cyclostomata (Agnatha) General characters and classification up to order level. Study of Petromyzon and its affinities. Block II (Lower chordates) 6 Fishes: General characters and classification up to order level. Types of scales and fins of fishes, Scoliodon as type study, migration and parental care in fishes. 7 Amphibians: General characters and classification up to order level, Rana tigrina as type study, parental care, neoteny and paedogenesis. 8 Reptilia: General characters and classification up to order level, extinct reptiles. Uromastix as type study. Identification of poisonous and non-poisonous snakes and biting mechanism of snakes. 9 Aves: General characters and classification up to order level. Study of Columba (Pigeon) and Characters of Archaeopteryx. Flight adaptations & bird migration. 10 Mammalia: General characters and classification up -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
The Hypocone As a Key Innovation in Mammalian Evolution (Adaptive Zone/Convergent Evolution/Dentition/Diversity/Theria) JOHN P
Proc. Natl. Acad. Sci. USA Vol. 92, pp. 10718-10722, November 1995 Evolution The hypocone as a key innovation in mammalian evolution (adaptive zone/convergent evolution/dentition/diversity/Theria) JOHN P. HUNTER* AND JUKKA JERNVALLt *Department of Anatomical Sciences, State University of New York, Stony Brook, NY 11794-8081; and tDepartment of Ecology and Systematics and Institute of Biotechnology, University of Helsinki, P.O. Box 17, FIN-00014, Finland Communicated by Elwyn L. Simons, Duke University Primate Center, Durham, NC, June 19, 1995 ABSTRACT The hypocone, a cusp added to the primi- occlusal contact between metacrista and paracristid (16), tively triangular upper molar teeth of therian mammals, has crests that are well developed in carnivorous mammals. Thus, evolved convergently >20 times among mammals during the possession of a hypocone is generally thought to be associated Cenozoic. Acquisition of the hypocone itself involves little with herbivory. phenotypic change, but subsequent diversification of groups We investigated the evolutionary potential of the hypocone possessing the hypocone may be greatly enhanced. Our anal- in two ways. First, we compared taxonomic diversity of living, ysis of the Cenozoic mammalian radiations, including the terrestrial, nonvolant mammals with different molar types Recent fauna, shows that high species diversity of mammals across dietary groups to determine whether the hypocone is with hypocones and association of the hypocone with her- indeed associated with herbivorous habits and whether mam- bivory strongly support recognition of the hypocone as a key mals with hypocones are more diverse today than those lacking innovation that has allowed invasion of, and diversification hypocones. Second, we compared the taxonomic diversity of within, herbivorous adaptive zones. -
Mammalia, Notoungulata), from the Eocene of Patagonia, Argentina
Palaeontologia Electronica palaeo-electronica.org An exceptionally well-preserved skeleton of Thomashuxleya externa (Mammalia, Notoungulata), from the Eocene of Patagonia, Argentina Juan D. Carrillo and Robert J. Asher ABSTRACT We describe one of the oldest notoungulate skeletons with associated cranioden- tal and postcranial elements: Thomashuxleya externa (Isotemnidae) from Cañadón Vaca in Patagonia, Argentina (Vacan subage of the Casamayoran SALMA, middle Eocene). We provide body mass estimates given by different elements of the skeleton, describe the bone histology, and study its phylogenetic position. We note differences in the scapulae, humerii, ulnae, and radii of the new specimen in comparison with other specimens previously referred to this taxon. We estimate a body mass of 84 ± 24.2 kg, showing that notoungulates had acquired a large body mass by the middle Eocene. Bone histology shows that the new specimen was skeletally mature. The new material supports the placement of Thomashuxleya as an early, divergent member of Toxodon- tia. Among placentals, our phylogenetic analysis of a combined DNA, collagen, and morphology matrix favor only a limited number of possible phylogenetic relationships, but cannot yet arbitrate between potential affinities with Afrotheria or Laurasiatheria. With no constraint, maximum parsimony supports Thomashuxleya and Carodnia with Afrotheria. With Notoungulata and Litopterna constrained as monophyletic (including Macrauchenia and Toxodon known for collagens), these clades are reconstructed on the stem -
The Largest Fossil Rodent Andre´S Rinderknecht1 and R
Proc. R. Soc. B doi:10.1098/rspb.2007.1645 Published online The largest fossil rodent Andre´s Rinderknecht1 and R. Ernesto Blanco2,* 1Museo Nacional de Historia Natural y Antropologı´a, Montevideo 11300, Uruguay 2Facultad de Ingenierı´a, Instituto de Fı´sica, Julio Herrera y Reissig 565, Montevideo 11300, Uruguay The discovery of an exceptionally well-preserved skull permits the description of the new South American fossil species of the rodent, Josephoartigasia monesi sp. nov. (family: Dinomyidae; Rodentia: Hystricognathi: Caviomorpha). This species with estimated body mass of nearly 1000 kg is the largest yet recorded. The skull sheds new light on the anatomy of the extinct giant rodents of the Dinomyidae, which are known mostly from isolated teeth and incomplete mandible remains. The fossil derives from San Jose´ Formation, Uruguay, usually assigned to the Pliocene–Pleistocene (4–2 Myr ago), and the proposed palaeoenviron- ment where this rodent lived was characterized as an estuarine or deltaic system with forest communities. Keywords: giant rodents; Dinomyidae; megamammals 1. INTRODUCTION 3. HOLOTYPE The order Rodentia is the most abundant group of living MNHN 921 (figures 1 and 2; Museo Nacional de Historia mammals with nearly 40% of the total number of Natural y Antropologı´a, Montevideo, Uruguay): almost mammalian species recorded (McKenna & Bell 1997; complete skull without left zygomatic arch, right incisor, Wilson & Reeder 2005). In general, rodents have left M2 and right P4-M1. body masses smaller than 1 kg with few exceptions. The largest living rodent, the carpincho or capybara 4. AGE AND LOCALITY (Hydrochoerus hydrochaeris), which lives in the Neotro- Uruguay, Departament of San Jose´, coast of Rı´odeLa pical region of South America, has a body mass of Plata, ‘Kiyu´’ beach (348440 S–568500 W). -
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.