2008-11 R&C Newsletter
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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 -
Paleoecological Comparison Between Late Miocene Localities of China and Greece Based on Hipparion Faunas
Paleoecological comparison between late Miocene localities of China and Greece based on Hipparion faunas Tao DENG Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044 (China) [email protected] Deng T. 2006. — Paleoecological comparison between late Miocene localities of China and Greece based on Hipparion faunas. Geodiversitas 28 (3) : 499-516. ABSTRACT Both China and Greece have abundant fossils of the late Miocene Hipparion fauna. Th e habitat of the Hipparion fauna in Greece was a sclerophyllous ever- green woodland. Th e Chinese late Miocene Hipparion fauna is represented respectively in the Guonigou fauna (MN 9), the Dashengou fauna (MN 10), and the Yangjiashan fauna (MN 11) from Linxia, Gansu, and the Baode fauna (MN 12) from Baode, Shanxi. According to the evidence from lithology, carbon isotopes, paleobotany, taxonomic framework, mammalian diversity and faunal similarity, the paleoenvironment of the Hipparion fauna in China was a subarid open steppe, which is diff erent from that of Greece. Th e red clay bearing the Hipparion fauna in China is windblown in origin, i.e. eolian deposits. Stable carbon isotopes from tooth enamel and paleosols indicate that C3 plants domi- nated the vegetation during the late Miocene in China. Pollens of xerophilous and sub-xerophilous grasses show a signal of steppe or dry grassland. Forest mammals, such as primates and chalicotheres, are absent or scarce, but grass- land mammals, such as horses and rhinoceroses, are abundant in the Chinese Hipparion fauna. Th e species richness of China and Greece exhibits a similar KEY WORDS trend with a clear increase from MN 9 to MN 12, but the two regions have Hipparion fauna, low similarities at the species level. -
LATE MIOCENE FISHES of the CACHE VALLEY MEMBER, SALT LAKE FORMATION, UTAH and IDAHO By
LATE MIOCENE FISHES OF THE CACHE VALLEY MEMBER, SALT LAKE FORMATION, UTAH AND IDAHO by PATRICK H. MCCLELLAN AND GERALD R. SMITH MISCELLANEOUS PUBLICATIONS MUSEUM OF ZOOLOGY, UNIVERSITY OF MICHIGAN, 208 Ann Arbor, December 17, 2020 ISSN 0076-8405 P U B L I C A T I O N S O F T H E MUSEUM OF ZOOLOGY, UNIVERSITY OF MICHIGAN NO. 208 GERALD SMITH, Editor The publications of the Museum of Zoology, The University of Michigan, consist primarily of two series—the Miscellaneous Publications and the Occasional Papers. Both series were founded by Dr. Bryant Walker, Mr. Bradshaw H. Swales, and Dr. W. W. Newcomb. Occasionally the Museum publishes contributions outside of these series. Beginning in 1990 these are titled Special Publications and Circulars and each is sequentially numbered. All submitted manuscripts to any of the Museum’s publications receive external peer review. The Occasional Papers, begun in 1913, serve as a medium for original studies based principally upon the collections in the Museum. They are issued separately. When a sufficient number of pages has been printed to make a volume, a title page, table of contents, and an index are supplied to libraries and individuals on the mailing list for the series. The Miscellaneous Publications, initiated in 1916, include monographic studies, papers on field and museum techniques, and other contributions not within the scope of the Occasional Papers, and are published separately. Each number has a title page and, when necessary, a table of contents. A complete list of publications on Mammals, Birds, Reptiles and Amphibians, Fishes, I nsects, Mollusks, and other topics is available. -
An Early Miocene Dome-Skulled Chalicothere
PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, NY 10024 Number 3486, 45 pp., 26 ®gures, 8 tables October 27, 2005 An Early Miocene Dome-Skulled Chalicothere from the ``Arikaree'' Conglomerates of Darton: Calibrating the Ages of High Plains Paleovalleys Against Rocky Mountain Tectonism ROBERT M. HUNT, JR.1 CONTENTS Abstract ....................................................................... 2 Introduction .................................................................... 2 Geologic Setting ................................................................ 3 Systematic Paleontology ........................................................ 12 Age of the Dome-Skulled Chalicothere ........................................... 28 The ``Arikaree'' Conglomerates of N.H. Darton ................................... 32 Post-Laramide Evolution of the Rocky Mountains ................................. 39 Acknowledgments ............................................................. 42 References .................................................................... 42 1 Department of Geosciences, W436 Nebraska Hall, University of Nebraska, Lincoln, NE 68588-0549 ([email protected]). Copyright q American Museum of Natural History 2005 ISSN 0003-0082 2 AMERICAN MUSEUM NOVITATES NO. 3486 ABSTRACT Fragmentary skeletal remains discovered in 1979 in southeastern Wyoming, associated with a mammalian fauna of early Hemingfordian age (;18.2 to 18.8 Ma), represent the oldest known occurrence of dome-skulled chalicotheres -
Agate Fossil Beds
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln U.S. National Park Service Publications and Papers National Park Service 1980 Agate Fossil Beds Follow this and additional works at: http://digitalcommons.unl.edu/natlpark "Agate Fossil Beds" (1980). U.S. National Park Service Publications and Papers. 160. http://digitalcommons.unl.edu/natlpark/160 This Article is brought to you for free and open access by the National Park Service at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in U.S. National Park Service Publications and Papers by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Agate Fossil Beds cap. tfs*Af Clemson Universit A *?* jfcti *JpRPP* - - - . Agate Fossil Beds Agate Fossil Beds National Monument Nebraska Produced by the Division of Publications National Park Service U.S. Department of the Interior Washington, D.C. 1980 — — The National Park Handbook Series National Park Handbooks, compact introductions to the great natural and historic places adminis- tered by the National Park Service, are designed to promote understanding and enjoyment of the parks. Each is intended to be informative reading and a useful guide before, during, and after a park visit. More than 100 titles are in print. This is Handbook 107. You may purchase the handbooks through the mail by writing to Superintendent of Documents, U.S. Government Printing Office, Washington DC 20402. About This Book What was life like in North America 21 million years ago? Agate Fossil Beds provides a glimpse of that time, long before the arrival of man, when now-extinct creatures roamed the land which we know today as Nebraska. -
Chapter 26 Cenozoic Life
236 Chapter 26 Cenozoic Life GUIDED STUDY The text chapter should be studied one section at a time. Life on Land (pp. 552-560) Before you read, preview each section by skimming it, noting headings and boldface items. Then read the 5. Describe the adaptations of grasses and herbaceous appropriate section objectives from the following plants that caused their spectacular radiation in the outline. Keep these objectives in mind and, as you read Cenozoic. the chapter section, search for the information that will enable you to meet each objective. Once you have finished a section, write out answers for its objectives. Cenozoic Marine Life (pp. 550-552) 1. List examples of major invertebrate groups that were missing from Cenozoic seas. 6. Discuss the diversification of birds in the Cenozoic, and the dominant roles they played. 2. Describe the diversification of foraminifera during the early Cenozoic. 7. Marsupial mammals developed in both South America and Australia. Why did those in South America suffer greatly from extinction in the Pliocene Epoch, but those in Australia have survived untouched until modern times? 3. Which marine invertebrates seemed little affected by the Cretaceous-Tertiary extinction event? 8. Describe the different stages in the development of the modern horse. What features underwent the most change, and why? 4. Describe the various forms that led to the evolution of whales from original land-based predators. Copyright © Houghton Mifflin Company. All rights reserved. 237 Quaternary Extinctions (pp. 560-562) CHAPTER REVIEW 9. Describe the kinds of animals, both mammal and When you have finished reading the chapter, work bird, that were lost in the late Quaternary extinction through the material that follows to review it. -
Endemism and Migration in the Kochkor Basin? Identification and Description of Adcrocuta Eximia (Mammalia: Carnivora: Hyaenidae) and C.F
Palaeontologia Electronica palaeo-electronica.org Endemism and migration in the Kochkor Basin? Identification and description of Adcrocuta eximia (Mammalia: Carnivora: Hyaenidae) and c.f. Paramachaerodus (Mammalia: Carnivora: Felidae) fossils at the Miocene locality of Ortok, Kyrgyzstan Sophie A. Miller, Paul Z. Barrett, Win N.F. McLaughlin, and Samantha S.B. Hopkins ABSTRACT Dentition from a Miocene hyaenid and a saber-toothed felid are described from the Chu Formation of Kyrgyzstan. Identified as Adcrocuta eximia (UOMNH F-70508) and c.f. Paramachaerodus (UOMNH F-70509), these represent one of the only formal- ized descriptions of fossil taxa from the Miocene in Kyrgyzstan. These specimens were recovered from the Ortok locality at the northwestern corner of the Kochkor Basin, the youngest of the known bone-bed localities in the Chu Formation. Using bio- and mag- netostratigraphy, the Chu Formation is attributed to the late Miocene to Pliocene, deposited approximately at 8 to 4 Ma. The Adcrocuta specimen consists of a partial dentary with condylar and angular processes, one upper, five lower teeth, and the par- tial root and alveoli of a fifth mandibular tooth. The c.f. Paramachaerodus specimen includes a partial M1, P4, and C1, and exhibits the features of the “scimitar-toothed” machairodontines. Preserved diagnostic characters place the Kyrgyz specimen closest to P. ogygia, although with certain features similar to that of P. transasiaticus, such as incipient crenulations on the canine. However, the age of the Kyrgyz specimen, approximately 6 Ma, is substantially younger than what is known for either of these taxa. We therefore hypothesize this Paramachaerodus specimen could be evidence of an endemic taxon in Kyrgyzstan from earlier migrating Asian species, potentially due to geological uplift with the Tien Shan Mountains. -
From the Late Miocene of Thermopigi (Serres, N.Greece), and the Relationships of the Genus Denis Geraads, Nikolaï Spassov, Evangelia Tsoukala
A skull of Ancylotherium (Chalicotheriidae, Mammalia) from the Late Miocene of Thermopigi (Serres, N.Greece), and the relationships of the genus Denis Geraads, Nikolaï Spassov, Evangelia Tsoukala To cite this version: Denis Geraads, Nikolaï Spassov, Evangelia Tsoukala. A skull of Ancylotherium (Chalicotheriidae, Mammalia) from the Late Miocene of Thermopigi (Serres, N.Greece), and the relationships of the genus. Journal of Vertebrate Palaeontology, 2007, 27 (2), pp.461-466. halshs-00158253 HAL Id: halshs-00158253 https://halshs.archives-ouvertes.fr/halshs-00158253 Submitted on 28 Jun 2007 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. A SKULL OF ANCYLOTHERIUM (CHALICOTHERIIDAE, MAMMALIA) FROM THE LATE MIOCENE OF THERMOPIGI (SERRES, N.GREECE), AND THE RELATIONSHIPS OF THE GENUS DENIS GERAADS 1, EVANGELIA TSOUKALA 2 and NIKOLAÏ SPASSOV 3 1 UPR 2147 CNRS, 44 rue de l'Amiral Mouchez, 75014 Paris, France, [email protected] (corresponding author) 2 School of Geology, Aristotle University, 54124 Thessaloniki, Greece, [email protected] 3 National Museum of Natural History, Tsar Osvoboditel Blvd 1, 1000 Sofia, Bulgaria, [email protected] RH: relationships of Ancylotherium 1 ABSTRACT The locality of Thermopigi in northern Greece has yielded a well- preserved skull of Ancylotherium pentelicum, among a rich collection of late Miocene mammals. -
Hyaenodonts and Carnivorans from the Early Oligocene to Early Miocene of Xianshuihe Formation, Lanzhou Basin, Gansu Province, China
Palaeontologia Electronica http://palaeo-electronica.org HYAENODONTS AND CARNIVORANS FROM THE EARLY OLIGOCENE TO EARLY MIOCENE OF XIANSHUIHE FORMATION, LANZHOU BASIN, GANSU PROVINCE, CHINA Xiaoming Wang, Zhanxiang Qiu, and Banyue Wang ABSTRACT Fieldwork in the 1990s produced a few records of carnivorous mammals (cre- odonts and carnivorans) in the early Oligocene through early Miocene of Lanzhou Basin, Gansu Province, China. Although only five taxa are known so far, most repre- sented by fragmentary material, the new carnivore assemblage is unique and shows little resemblance to faunas elsewhere in eastern Asia. The early Oligocene record is represented by a single premolar of a Hyaenodon, referable to H. pervagus. In the early Miocene, a new species of Hyaenodon, H. weilini sp. nov., represented by sev- eral cheek teeth, is the last record of this genus in east Asia. A horizontal ramus of an amphicyonid, here identified as Ictiocyon cf. I. socialis, is the first record of this taxon in Asia, and a very small musteloid lower carnassial, although difficult to identify to genus, is clearly a new record because nothing of this small size has been known in Asia. The overall faunal composition seems to suggest affinity with northern Eurasia rather than southern Asia. Xiaoming Wang. Department of Vertebrate Paleontology, Natural History Museum of Los Angeles County, 900 Exposition Blvd., Los Angeles, California 90007, United States [email protected] Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, P.O. Box 643, Beijing 100044, China. Zhanxiang Qiu. Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, P.O. Box 643, Beijing 100044, China. -
First North American Fossil Monkey and Early Miocene Tropical Biotic Interchange Jonathan I
LETTER doi:10.1038/nature17415 First North American fossil monkey and early Miocene tropical biotic interchange Jonathan I. Bloch1, Emily D. Woodruff1,2, Aaron R. Wood1,3, Aldo F. Rincon1,4, Arianna R. Harrington1,2,5, Gary S. Morgan6, David A. Foster4, Camilo Montes7, Carlos A. Jaramillo8, Nathan A. Jud1, Douglas S. Jones1 & Bruce J. MacFadden1 New World monkeys (platyrrhines) are a diverse part of modern Primates Linnaeus, 1758 tropical ecosystems in North and South America, yet their early Anthropoidea Mivart, 1864 evolutionary history in the tropics is largely unknown. Molecular Platyrrhini Geoffroy, 1812 divergence estimates suggest that primates arrived in tropical Cebidae Bonaparte, 1831 Central America, the southern-most extent of the North American Panamacebus transitus gen. et sp. nov. landmass, with several dispersals from South America starting with the emergence of the Isthmus of Panama 3–4 million years Etymology. Generic name combines ‘Panama’ with ‘Cebus’, root taxon ago (Ma)1. The complete absence of primate fossils from Central for Cebidae. Specific name ‘transit’ (Latin, crossing) refers to its implied America has, however, limited our understanding of their history early Miocene dispersal between South and North America. in the New World. Here we present the first description of a fossil Holotype. UF 280128, left upper first molar (M1; Fig. 2a, b). monkey recovered from the North American landmass, the oldest Referred material. Left upper second molar (M2; UF 281001; Fig. 2a, b), known crown platyrrhine, from a precisely dated 20.9-Ma layer in partial left lower first incisor (I1; UF 280130), right lower second the Las Cascadas Formation in the Panama Canal Basin, Panama. -
The Late Miocene Percrocutas (Carnivora, Mammalia) of Macedonia, Greece
THE LATE MIOCENE PERCROCUTAS (CARNIVORA, MAMMALIA) OF MACEDONIA, GREECE by George D. KOUFOS' CONTENTS Page Abstract, Resume . 68 Introduction ..................................................................... 68 Palaeontology. 70 Dinocrocuta gigantea (SCHLOSSER, 1903) . 70 Discussion. 71 The problem of "Hyaena" salonicae ANDREWS, 1918 ..................................... 76 Biochronology of the percrocutas. .. .. .. 79 Acknowledgements ............... 82 References ...................................................................... 82 Legends of plates ..... 84 * Aristotle University of Thessaloniki, Department of Geology and Physical Geography, Laboratory of Geology and Palaeontology, 54006 Thessaloniki,, Greece. Key-words: Mammalia, Carnivora, Dinocrocuta, late Miocene, Greece, Description, Comparisons, Biocbronology. Mots-cles: Mammiteres, Carnivores, Dinocrocuta, Miocene superieur, Grece, Description, Comparaisons, Biocbronologie. Palaeovertebrala. Montpellier. 24 (1-2): 67-84. 6 fig" 2 pI. (Re~u le 2 Avri11993. ac«pte le 29 Avri11993. publie le 14 Juin 1995) ABSTRACf Some new material of percracutas from the late Miocene of Axios valley (Macedonia, Greece) is studied. They have been found in the locality of "Pentalophos I" (PNT). The material has been described and compared with the known late Miocene percrocutas of Eurasia. This comparison indicates that it can be identified as Dil/ocrocula gigalllea (SCHLOSSER, 1903). A maxilla of a percrocuta, named "Hyaena" salonicae, was found in the same area (Andrews, 1918). "Hyaena" -
Newsletter Number 52
The Palaeontology Newsletter Contents 52 Association Business 2 AGM 14 News 16 Association Meetings 20 From our own correspondents Conceptual fossils 24 Sutures joining Ontogeny and Fossils 29 Correspondence 33 Big Gamble for a Big Dead Fish 40 The Mystery Fossil 43 Obituary: Frank Hodson 46 Future meetings of other bodies 48 Meeting Reports 56 Book Reviews 68 Palaeontology vol 46 parts 1, 2, 3 99–101 Special Papers in Palaeontology no. 68 102 Reminder: The deadline for copy for Issue no 53 is 27th June 2003 On the Web: http://www.palass.org/ Newsletter 52 2 Newsletter 52 3 Meetings. Four meetings were held in 2002, and the Association extends its thanks to the Association Business organisers and host institutions of these meetings. a. Lyell Meeting. “Approaches to Reconstructing Phylogeny”, was convened on behalf of the Annual Report for 2002 Association by Prof. Gale (University of Greenwich) and Dr P.C.J. Donoghue (Lapworth Museum, University of Birmingham). Nature of the Association. The Palaeontological Association is a Charity registered in England, b. Forty-fifth Annual General Meeting and Address. 8th May. The address, entitled “Life and Charity Number 276369. Its Governing Instrument is the Constitution adopted on 27 February work of S.S. Buckmann (1860-1929) Geobiochronologist and the problems of assessing the work of 1957, amended on subsequent occasions as recorded in the Council Minutes. Trustees (Council past palaeontologists,” was given by Prof. Hugh Torrens and attended by 40 people. The meeting Members) are elected by vote of the Membership at the Annual General Meeting. The contact was held at the University of Birmingham and organised by Dr M.P.