The Position of Hippopotamidae Within Cetartiodactyla
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South Dakota to Nebraska
Geological Society of America Special Paper 325 1998 Lithostratigraphic revision and correlation of the lower part of the White River Group: South Dakota to Nebraska Dennis O. Terry, Jr. Department of Geology, University of Nebraska—Lincoln, Lincoln, Nebraska 68588-0340 ABSTRACT Lithologic correlations between type areas of the White River Group in Nebraska and South Dakota have resulted in a revised lithostratigraphy for the lower part of the White River Group. The following pedostratigraphic and lithostratigraphic units, from oldest to youngest, are newly recognized in northwestern Nebraska and can be correlated with units in the Big Badlands of South Dakota: the Yellow Mounds Pale- osol Equivalent, Interior and Weta Paleosol Equivalents, Chamberlain Pass Forma- tion, and Peanut Peak Member of the Chadron Formation. The term “Interior Paleosol Complex,” used for the brightly colored zone at the base of the White River Group in northwestern Nebraska, is abandoned in favor of a two-part division. The lower part is related to the Yellow Mounds Paleosol Series of South Dakota and rep- resents the pedogenically modified Cretaceous Pierre Shale. The upper part is com- posed of the unconformably overlying, pedogenically modified overbank mudstone facies of the Chamberlain Pass Formation (which contains the Interior and Weta Paleosol Series in South Dakota). Greenish-white channel sandstones at the base of the Chadron Formation in Nebraska (previously correlated to the Ahearn Member of the Chadron Formation in South Dakota) herein are correlated to the channel sand- stone facies of the Chamberlain Pass Formation in South Dakota. The Chamberlain Pass Formation is unconformably overlain by the Chadron Formation in South Dakota and Nebraska. -
About Pigs [PDF]
May 2015 About Pigs Pigs are highly intelligent, social animals, displaying elaborate maternal, communicative, and affiliative behavior. Wild and feral pigs inhabit wide tracts of the southern and mid-western United States, where they thrive in a variety of habitats. They form matriarchal social groups, sleep in communal nests, and maintain close family bonds into adulthood. Science has helped shed light on the depths of the remarkable cognitive abilities of pigs, and fosters a greater appreciation for these often maligned and misunderstood animals. Background Pigs—also called swine or hogs—belong to the Suidae family1 and along with cattle, sheep, goats, camels, deer, giraffes, and hippopotamuses, are part of the order Artiodactyla, or even-toed ungulates.2 Domesticated pigs are descendants of the wild boar (Sus scrofa),3,4 which originally ranged through North Africa, Asia and Europe.5 Pigs were first domesticated approximately 9,000 years ago.6 The wild boar became extinct in Britain in the 17th century as a result of hunting and habitat destruction, but they have since been reintroduced.7,8 Feral pigs (domesticated animals who have returned to a wild state) are now found worldwide in temperate and tropical regions such as Australia, New Zealand, and Indonesia and on island nations, 9 such as Hawaii.10 True wild pigs are not native to the New World.11 When Christopher Columbus landed in Cuba in 1493, he brought the first domestic pigs—pigs who subsequently spread throughout the Spanish West Indies (Caribbean).12 In 1539, Spanish explorers brought pigs to the mainland when they settled in Florida. -
New Postcranial Specimens of the Anthracotheriidae (Mammalia; Artiodactyla) from the Paleogene of Fayum Depression, Egypt
International Journal of Scientific Engineering and Applied Science (IJSEAS) - Volume-1, Issue-8,November 2015 ISSN: 2395-3470 www.ijseas.com New postcranial specimens of the Anthracotheriidae (Mammalia; Artiodactyla) from the Paleogene of Fayum Depression, Egypt 1 2 Afifi H. Sileem , Abdel Galil A Hewaidy 1 Vertebrate paleontology section, Cairo Geological Museum, Cairo, Egypt, [email protected] 2Department of Geology, Faculty of Science, Al-Azhar University, Egypt, <[email protected]> Abstract: The fossiliferous deposits exposed north of Birket Qarun in the Fayum Depression, northeast Egypt, have produced a remarkable collection of fossil mammals from localities that range in age from earliest late Eocene (~37 Ma) to latest early Oligocene (~29 Ma). Anthracotheriidae are among the most common mammals that are preserved in these deposits. Here we describe a new fossil specimens of the Anthracotheriidae (Mammalia, Artiodactyla) discovered in the Jebel Qatrani Formation of Fayum. The specimens consist of a seven astragalus, which is referable to Bothriogenys sp. from the formation. The specimens Bothriogenys sp. show a higher degree of size variation and some feature suggest that the anthracothere are not closely related to Hippopotamus. Key word: anthracothere, Bothriogenys; astragalus; Fayum; Early Oligocene. 376 International Journal of Scientific Engineering and Applied Science (IJSEAS) - Volume-1, Issue-8,November 2015 ISSN: 2395-3470 www.ijseas.com Introduction: The fossiliferous sedimentary deposits exposed north of Birket (lake) Qarun in the Fayum Depression (Fig.1), northeast Egypt, have produced a remarkable collection of a wide variety of fish, amphibian, reptile, bird and mammal taxa (e.g. Andrews, 1906; Simons and Rasmussen, 1990; Murray et al. -
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. -
A Giant's Comeback
W INT E R 2 0 1 0 n o s d o D y l l i B Home to elephants, rhinos and more, African Heartlands are conservation landscapes large enough to sustain a diversity of species for centuries to come. In these landscapes— places like Kilimanjaro and Samburu—AWF and its partners are pioneering lasting conservation strate- gies that benefit wildlife and people alike. Inside TH I S ISSUE n e s r u a L a n a h S page 4 These giraffes are members of the only viable population of West African giraffe remaining in the wild. A few herds live in a small AWF Goes to West Africa area in Niger outside Regional Parc W. AWF launches the Regional Parc W Heartland. A Giant’s Comeback t looks like a giraffe, walks like a giraffe, eats totaling a scant 190-200 individuals. All live in like a giraffe and is indeed a giraffe. But a small area—dubbed “the Giraffe Zone”— IGiraffa camelopardalis peralta (the scientific outside the W National Parc in Niger, one of name for the West African giraffe) is a distinct the three national parks that lie in AWF’s new page 6 subspecies of mother nature’s tallest mammal, transboundary Heartland in West Africa (see A Quality Brew having split from a common ancestral popula- pp. 4-5). Conserving the slopes of Mt. Kilimanjaro tion some 35,000 years ago. This genetic Entering the Zone with good coffee. distinction is apparent in its large orange- Located southeast of Niamey, Niger’s brown skin pattern, which is more lightly- capital, the Giraffe Zone spans just a few hun- colored than that of other giraffes. -
Quaternary International 603 (2021) 40–63
Quaternary International 603 (2021) 40–63 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Taxonomy, taphonomy and chronology of the Pleistocene faunal assemblage at Ngalau Gupin cave, Sumatra Holly E. Smith a,*, Gilbert J. Price b, Mathieu Duval c,a, Kira Westaway d, Jahdi Zaim e, Yan Rizal e, Aswan e, Mika Rizki Puspaningrum e, Agus Trihascaryo e, Mathew Stewart f, Julien Louys a a Australian Research Centre for Human Evolution, Environmental Futures Research Institute, Griffith University, Nathan, Queensland, 4111, Australia b School of Earth and Environmental Sciences, The University of Queensland, St Lucia, Queensland, 4072, Australia c Centro Nacional de Investigacion´ Sobre la Evolucion´ Humana (CENIEH), Burgos, 09002, Spain d Department of Earth and Environmental Sciences, Macquarie University, Sydney, New South Wales, Australia e Geology Study Program, Institut Teknologi Bandung, Jawa Barat, 40132, Indonesia f Extreme Events Research Group, Max Planck Institutes for Chemical Ecology, the Science of Human History, and Biogeochemistry, Jena, Germany ARTICLE INFO ABSTRACT Keywords: Ngalau Gupin is a broad karstic cave system in the Padang Highlands of western Sumatra, Indonesia. Abundant Taxonomy fossils, consisting of mostly isolated teeth from small-to large-sized animals, were recovered from breccias Taphonomy cemented on the cave walls and unconsolidated sediments on the cave floor.Two loci on the walls and floorsof Cave Ngalau Gupin, named NG-A and NG-B respectively, are studied. We determine that NG-B most likely formed as a Pleistocene result of the erosion and redeposition of material from NG-A. The collection reveals a rich, diverse Pleistocene Southeast Asia Hexaprotodon faunal assemblage (Proboscidea, Primates, Rodentia, Artiodactyla, Perissodactyla, Carnivora) largely analogous ESR and U-series dating to extant fauna in the modern rainforests of Sumatra. -
Endangered Species (Protection, Conser Va Tion and Regulation of Trade)
ENDANGERED SPECIES (PROTECTION, CONSER VA TION AND REGULATION OF TRADE) THE ENDANGERED SPECIES (PROTECTION, CONSERVATION AND REGULATION OF TRADE) ACT ARRANGEMENT OF SECTIONS Preliminary Short title. Interpretation. Objects of Act. Saving of other laws. Exemptions, etc., relating to trade. Amendment of Schedules. Approved management programmes. Approval of scientific institution. Inter-scientific institution transfer. Breeding in captivity. Artificial propagation. Export of personal or household effects. PART I. Administration Designahem of Mana~mentand establishment of Scientific Authority. Policy directions. Functions of Management Authority. Functions of Scientific Authority. Scientific reports. PART II. Restriction on wade in endangered species 18. Restriction on trade in endangered species. 2 ENDANGERED SPECIES (PROTECTION, CONSERVATION AND REGULA TION OF TRADE) Regulation of trade in species spec fled in the First, Second, Third and Fourth Schedules Application to trade in endangered specimen of species specified in First, Second, Third and Fourth Schedule. Export of specimens of species specified in First Schedule. Importation of specimens of species specified in First Schedule. Re-export of specimens of species specified in First Schedule. Introduction from the sea certificate for specimens of species specified in First Schedule. Export of specimens of species specified in Second Schedule. Import of specimens of species specified in Second Schedule. Re-export of specimens of species specified in Second Schedule. Introduction from the sea of specimens of species specified in Second Schedule. Export of specimens of species specified in Third Schedule. Import of specimens of species specified in Third Schedule. Re-export of specimens of species specified in Third Schedule. Export of specimens specified in Fourth Schedule. PART 111. -
Last Interglacial (MIS 5) Ungulate Assemblage from the Central Iberian Peninsula: the Camino Cave (Pinilla Del Valle, Madrid, Spain)
Palaeogeography, Palaeoclimatology, Palaeoecology 374 (2013) 327–337 Contents lists available at SciVerse ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Last Interglacial (MIS 5) ungulate assemblage from the Central Iberian Peninsula: The Camino Cave (Pinilla del Valle, Madrid, Spain) Diego J. Álvarez-Lao a,⁎, Juan L. Arsuaga b,c, Enrique Baquedano d, Alfredo Pérez-González e a Área de Paleontología, Departamento de Geología, Universidad de Oviedo, C/Jesús Arias de Velasco, s/n, 33005 Oviedo, Spain b Centro Mixto UCM-ISCIII de Evolución y Comportamiento Humanos, C/Sinesio Delgado, 4, 28029 Madrid, Spain c Departamento de Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, Ciudad Universitaria, 28040 Madrid, Spain d Museo Arqueológico Regional de la Comunidad de Madrid, Plaza de las Bernardas, s/n, 28801-Alcalá de Henares, Madrid, Spain e Centro Nacional de Investigación sobre la Evolución Humana (CENIEH), Paseo Sierra de Atapuerca, s/n, 09002 Burgos, Spain article info abstract Article history: The fossil assemblage from the Camino Cave, corresponding to the late MIS 5, constitutes a key record to un- Received 2 November 2012 derstand the faunal composition of Central Iberia during the last Interglacial. Moreover, the largest Iberian Received in revised form 21 January 2013 fallow deer fossil population was recovered here. Other ungulate species present at this assemblage include Accepted 31 January 2013 red deer, roe deer, aurochs, chamois, wild boar, horse and steppe rhinoceros; carnivores and Neanderthals Available online 13 February 2013 are also present. The origin of the accumulation has been interpreted as a hyena den. Abundant fallow deer skeletal elements allowed to statistically compare the Camino Cave fossils with other Keywords: Early Late Pleistocene Pleistocene and Holocene European populations. -
Hoganson, J.W., 2009. Corridor of Time Prehistoric Life of North
Corridor of Time Prehistoric Life of North Dakota Exhibit at the North Dakota Heritage Center Completed by John W. Hoganson Introduction In 1989, legislation was passed that directed the North Dakota and a laboratory specialist, a laboratory for preparation of Geological Survey to establish a public repository for North fossils, and a fossil storage area. The NDGS paleontology staff, Dakota fossils. Shortly thereafter, the Geological Survey signed now housed at the Heritage Center, consists of John Hoganson, a Memorandum of Agreement with the State Historical Society State Paleontologist, and paleontologists Jeff Person and Becky of North Dakota which provided space in the North Dakota Gould. This arrangement has allowed the Geological Survey, in Heritage Center for development of this North Dakota State collaboration with the State Historical Society of North Dakota, Fossil Collection, including offices for the curator of the collection to create prehistoric life of North Dakota exhibits at the Heritage Center and displays of North Dakota fossils at over 20 other museums and interpretive centers around the state. The first of the Heritage Center prehistoric life exhibits was the restoration of the Highgate Mastodon skeleton in the First People exhibit area (fig. 1). Mastodons were huge, elephant- like mammals that roamed North America at the end of the last Ice Age about 11,000 years ago. This exhibit was completed in 1992 and was the first restored skeleton of a prehistoric animal ever displayed in North Dakota. The mastodon exhibit was, and still is, a major attraction in the Heritage Center. Because of its popularity, it was decided that additional prehistoric life displays should be included in the Heritage Center exhibit plans. -
The Status and Distribution of Mediterranean Mammals
THE STATUS AND DISTRIBUTION OF MEDITERRANEAN MAMMALS Compiled by Helen J. Temple and Annabelle Cuttelod AN E AN R R E IT MED The IUCN Red List of Threatened Species™ – Regional Assessment THE STATUS AND DISTRIBUTION OF MEDITERRANEAN MAMMALS Compiled by Helen J. Temple and Annabelle Cuttelod The IUCN Red List of Threatened Species™ – Regional Assessment The designation of geographical entities in this book, and the presentation of material, do not imply the expression of any opinion whatsoever on the part of IUCN or other participating organizations, concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The views expressed in this publication do not necessarily reflect those of IUCN or other participating organizations. Published by: IUCN, Gland, Switzerland and Cambridge, UK Copyright: © 2009 International Union for Conservation of Nature and Natural Resources Reproduction of this publication for educational or other non-commercial purposes is authorized without prior written permission from the copyright holder provided the source is fully acknowledged. Reproduction of this publication for resale or other commercial purposes is prohibited without prior written permission of the copyright holder. Red List logo: © 2008 Citation: Temple, H.J. and Cuttelod, A. (Compilers). 2009. The Status and Distribution of Mediterranean Mammals. Gland, Switzerland and Cambridge, UK : IUCN. vii+32pp. ISBN: 978-2-8317-1163-8 Cover design: Cambridge Publishers Cover photo: Iberian lynx Lynx pardinus © Antonio Rivas/P. Ex-situ Lince Ibérico All photographs used in this publication remain the property of the original copyright holder (see individual captions for details). -
The Late Miocene Mammalian Fauna of Chorora, Awash Basin
The late Miocene mammalian fauna of Chorora, Awash basin, Ethiopia: systematics, biochronology and 40K-40Ar ages of the associated volcanics Denis Geraads, Zeresenay Alemseged, Hervé Bellon To cite this version: Denis Geraads, Zeresenay Alemseged, Hervé Bellon. The late Miocene mammalian fauna of Chorora, Awash basin, Ethiopia: systematics, biochronology and 40K-40Ar ages of the associated volcanics. Tertiary Research, 2002, 21 (1-4), pp.113-122. halshs-00009761 HAL Id: halshs-00009761 https://halshs.archives-ouvertes.fr/halshs-00009761 Submitted on 24 Mar 2006 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. The late Miocene mammalian fauna of Chorora, Awash basin, Ethiopia: systematics, biochronology and 40K-40Ar ages of the associated volcanics Denis GERAADS - EP 1781 CNRS, 44 rue de l'Amiral Mouchez, 75014 PARIS, France Zeresenay ALEMSEGED - National Museum, P.O.Box 76, Addis Ababa, Ethiopia Hervé BELLON - UMR 6538 CNRS, Université de Bretagne Occidentale, BP 809, 29285 BREST CEDEX, France ABSTRACT New whole-rock 40K-40Ar ages on lava flows bracketing the Chorora Fm, Ethiopia, confirm that its Hipparion-bearing sediments must be in the 10-11 Ma time-range. The large Mammal fauna includes 10 species. -
Investigating Sexual Dimorphism in Ceratopsid Horncores
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2013-01-25 Investigating Sexual Dimorphism in Ceratopsid Horncores Borkovic, Benjamin Borkovic, B. (2013). Investigating Sexual Dimorphism in Ceratopsid Horncores (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/26635 http://hdl.handle.net/11023/498 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Investigating Sexual Dimorphism in Ceratopsid Horncores by Benjamin Borkovic A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DEPARTMENT OF BIOLOGICAL SCIENCES CALGARY, ALBERTA JANUARY, 2013 © Benjamin Borkovic 2013 Abstract Evidence for sexual dimorphism was investigated in the horncores of two ceratopsid dinosaurs, Triceratops and Centrosaurus apertus. A review of studies of sexual dimorphism in the vertebrate fossil record revealed methods that were selected for use in ceratopsids. Mountain goats, bison, and pronghorn were selected as exemplar taxa for a proof of principle study that tested the selected methods, and informed and guided the investigation of sexual dimorphism in dinosaurs. Skulls of these exemplar taxa were measured in museum collections, and methods of analysing morphological variation were tested for their ability to demonstrate sexual dimorphism in their horns and horncores.