Mammalia, Proboscidea, Gomphotheriidae): Taxonomy, Phylogeny, and Biogeography
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1.1 První Chobotnatci 5 1.2 Plesielephantiformes 5 1.3 Elephantiformes 6 1.3.1 Mammutida 6 1.3.2 Elephantida 7 1.3.3 Elephantoidea 7 2
MASARYKOVA UNIVERZITA PŘÍRODOVĚDECKÁ FAKULTA ÚSTAV GEOLOGICKÝCH VĚD Jakub Březina Rešerše k bakalářské práci Využití mikrostruktur klů neogenních chobotnatců na příkladu rodu Zygolophodon Vedoucí práce: doc. Mgr. Martin Ivanov, Dr. Brno 2012 OBSAH 1. Současný pohled na evoluci chobotnatců 3 1.1 První chobotnatci 5 1.2 Plesielephantiformes 5 1.3 Elephantiformes 6 1.3.1 Mammutida 6 1.3.2 Elephantida 7 1.3.3 Elephantoidea 7 2. Kly chobotnatců a jejich mikrostruktura 9 2.1 Přírůstky v klech chobotnatců 11 2.1.1 Využití přírůstků v klech chobotnatců 11 2.2 Schregerův vzor 12 2.2.1 Stavba Schregerova vzoru 12 2.2.2 Využití Schregerova vzoru 12 2.3 Dentinové kanálky 15 3 Sedimenty s nálezy savců v okolí Mikulova 16 3.1 Baden 17 3.2 Pannon a Pont 18 1. Současný pohled na evoluci chobotnatců Současná systematika chobotnatců není kompletně odvozena od jejich fylogeneze, rekonstruované pomocí kladistických metod. Diskutované skupiny tak mnohdy nepředstavují monofyletické skupiny. Přestože jsou taxonomické kategorie matoucí (např. Laurin 2005), jsem do jisté míry nucen je používat. Některým skupinám úrovně stále přiřazeny nebyly a zde této skutečnosti není přisuzován žádný význam. V této rešerši jsem se zaměřil hlavně na poznatky, které následovaly po vydání knihy; The Proboscidea: Evolution and Paleoecology of Elephants and Their Relatives, od Shoshaniho a Tassyho (1996). Chobotnatci jsou součástí skupiny Tethytheria společně s anthracobunidy, sirénami a desmostylidy (Shoshani 1998; Shoshani & Tassy 1996; 2005; Gheerbrant & Tassy 2009). Základní klasifikace sestává ze dvou skupin. Ze skupiny Plesielephantiformes, do které patří čeledě Numidotheriidae, Barytheriidae a Deinotheridae a ze skupiny Elephantiformes, do které patří čeledě Palaeomastodontidae, Phiomiidae, Mammutida, Gomphotheriidae, tetralofodontní gomfotéria, Stegodontidae a Elephantidae (Shoshani & Marchant 2001; Shoshani & Tassy 2005; Gheerbrant & Tassy 2009). -
Matheus Souza Lima Ribeiro
Palaeogeography, Palaeoclimatology, Palaeoecology 392 (2013) 546–556 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Climate and humans set the place and time of Proboscidean extinction in late Quaternary of South America Matheus Souza Lima-Ribeiro a,b,⁎, David Nogués-Bravo c,LeviCarinaTerribilea, Persaram Batra d, José Alexandre Felizola Diniz-Filho e a Departamento de Ciências Biológicas, Universidade Federal de Goiás, Campus Jataí, Cx. Postal 03, 75804-020 Jataí, GO, Brazil b Programa de Pós-graduação em Ecologia e Evolução, Universidade Federal de Goiás, Cx. Postal 131, 74001-970 Goiânia, GO, Brazil c Centre for Macroecology, Evolution and Climate, University of Copenhagen, Universitetsparken 15, 2100, Denmark d Department of Geology, Greenfield Community College, Greenfield, MA 01301, USA e Departamento de Ecologia, ICB, Universidade Federal de Goiás, Cx. Postal 131, 74001-970 Goiânia, GO, Brazil article info abstract Article history: The late Quaternary extinctions have been widely debated for a long time, but the varying magnitude of Received 18 April 2013 human vs. climate change impacts across time and space is still an unresolved question. Here we assess Received in revised form 7 October 2013 the geographic range shifts in response to climate change based on Ecological Niche Models (ENMs) and Accepted 21 October 2013 modeled the timing for extinction under human hunting scenario, and both variables were used to explain Available online 30 October 2013 the extinction dynamics of Proboscideans during a full interglacial/glacial cycle (from 126 ka to 6 ka) in South America. We found a large contraction in the geographic range size of two Proboscidean species stud- Keywords: Late Quaternary extinctions ied (Cuvieronius hyodon and Notiomastodon platensis) across time. -
Title Stegodon Miensis Matsumoto (Proboscidea) from the Pliocene Yaoroshi Formation, Akiruno City, Tokyo, Japan( Fulltext ) Auth
Stegodon miensis Matsumoto (Proboscidea) from the Pliocene Title Yaoroshi Formation, Akiruno City, Tokyo, Japan( fulltext ) Author(s) AIBA, Hiroaki; BABA, Katsuyoshi; MATSUKAWA, Masaki Citation 東京学芸大学紀要. 自然科学系, 58: 203-206 Issue Date 2006-09-00 URL http://hdl.handle.net/2309/63450 Committee of Publication of Bulletin of Tokyo Gakugei Publisher University Rights Bulletin of Tokyo Gakugei University, Natural Sciences, 58, pp.203 ~ 206 , 2006 Stegodon miensis Matsumoto (Proboscidea) from the Pliocene Yaoroshi Formation, Akiruno City, Tokyo, Japan Hiroaki AIBA *, Katsuyoshi BABA *, Masaki MATSUKAWA ** Environmental Sciences (Received for Publication ; May 26, 2006) AIBA, H., BABA, K. and MATSUKAWA, M.: Stegodon miensis Matsumoto (Proboscidea) from the Pliocene Yaoroshi Formation, Akiruno City, Tokyo, Japan. Bull. Tokyo Gakugei Univ. Natur. Sci., 58: 203 – 206 (2006) ISSN 1880–4330 Abstract The molar of Stegodon from the Pliocene Yaoroshi Formation in Akiruno City, Tokyo, is described as S. miensis Matsumoto, based on morphological characteristics and dimensional characters of the specimen. The present specimen of S. miensis from the Yaoroshi Formation is shown to represent the uppermost-known horizon of the species. Key words : Stegodon miensis, Yaoroshi Formation, Late Pliocene, molar, paleontological description * Keio Gijyuku Yochisha, Shibuya, Tokyo 150-0013, Japan. ** Department of Environmental Sciences, Tokyo Gakugei University, Koganei, Tokyo 184-8501, Japan. Corresponding author : Masaki Matsukawa ([email protected]) Introduction ulna. The materials were initially identified as Stegodon bombifrons (Itsukaichi Stegodon Research Group, 1980) and Stegodon miensis Matsumoto (Proboscidea) is the oldest- subsequently distinguished as S. shinshuensis (Taruno, known species of the genus Stegodon in Japan. The species 1991a). Taru and Kohno (2002) considered S. -
The Mastodonts of Brazil': the State of the Art of South American
Quaternary International 443 (2017) 52e64 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Sixty years after ‘The mastodonts of Brazil’: The state of the art of South American proboscideans (Proboscidea, Gomphotheriidae) * Dimila Mothe a, b, , Leonardo dos Santos Avilla a, c, Lidiane Asevedo a, d, Leon Borges-Silva a, Mariane Rosas e, Rafael Labarca-Encina f, Ricardo Souberlich g, Esteban Soibelzon h, i, Jose Luis Roman-Carrion j, Sergio D. Ríos k, Ascanio D. Rincon l, Gina Cardoso de Oliveira b, Renato Pereira Lopes m a Laboratorio de Mastozoologia, Departamento de Zoologia, Instituto de Bioci^encias, Universidade Federal do Estado do Rio de Janeiro, Av. Pasteur, 458, 501, Urca, CEP 22290-240, Rio de Janeiro, Brazil b Programa de Pos-graduaç ao~ em Geoci^encias, Centro de Tecnologia e Geoci^encias, Universidade Federal de Pernambuco, Rua Acad^emico Helio Ramos, s/n, Cidade Universitaria, CEP 50740-467, Recife, Brazil c Programa de Pos-graduaç ao~ em Biodiversidade Neotropical, Instituto de Bioci^encias, Universidade Federal do Estado do Rio de Janeiro, Av. Pasteur, 458, 501, Urca, CEP 22290-240, Rio de Janeiro, Brazil d Faculdade de Geoci^encias (Fageo), Campus Cuiaba, Universidade Federal de Mato Grosso, Av. Fernando Correa da Costa, 2367, Jardim Petropolis, CEP 78070-000, Cuiaba, Mato Grosso, Brazil e Laboratorio de Paleontologia, Centro de Ci^encias Agrarias, Ambientais e Biologicas, Universidade Federal do Reconcavo^ da Bahia, Cruz das Almas, Bahia, Brazil f Laboratorio de Paleoecología, Instituto de Ciencias Ambientales y Evolutivas, Universidad Austral de Chile, Casilla 567, Valdivia, Chile g Laboratorio de Paleontología, Departamento de Geología, Facultad de Ciencias Exactas y Naturales, Acceso Av. -
Variable Impact of Late-Quaternary Megafaunal Extinction in Causing
Variable impact of late-Quaternary megafaunal SPECIAL FEATURE extinction in causing ecological state shifts in North and South America Anthony D. Barnoskya,b,c,1, Emily L. Lindseya,b, Natalia A. Villavicencioa,b, Enrique Bostelmannd,2, Elizabeth A. Hadlye, James Wanketf, and Charles R. Marshalla,b aDepartment of Integrative Biology, University of California, Berkeley, CA 94720; bMuseum of Paleontology, University of California, Berkeley, CA 94720; cMuseum of Vertebrate Zoology, University of California, Berkeley, CA 94720; dRed Paleontológica U-Chile, Laboratoria de Ontogenia, Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Chile; eDepartment of Biology, Stanford University, Stanford, CA 94305; and fDepartment of Geography, California State University, Sacramento, CA 95819 Edited by John W. Terborgh, Duke University, Durham, NC, and approved August 5, 2015 (received for review March 16, 2015) Loss of megafauna, an aspect of defaunation, can precipitate many megafauna loss, and if so, what does this loss imply for the future ecological changes over short time scales. We examine whether of ecosystems at risk for losing their megafauna today? megafauna loss can also explain features of lasting ecological state shifts that occurred as the Pleistocene gave way to the Holocene. We Approach compare ecological impacts of late-Quaternary megafauna extinction The late-Quaternary impact of losing 70–80% of the megafauna in five American regions: southwestern Patagonia, the Pampas, genera in the Americas (19) would be expected to trigger biotic northeastern United States, northwestern United States, and Berin- transitions that would be recognizable in the fossil record in at gia. We find that major ecological state shifts were consistent with least two respects. -
La Brea and Beyond: the Paleontology of Asphalt-Preserved Biotas
La Brea and Beyond: The Paleontology of Asphalt-Preserved Biotas Edited by John M. Harris Natural History Museum of Los Angeles County Science Series 42 September 15, 2015 Cover Illustration: Pit 91 in 1915 An asphaltic bone mass in Pit 91 was discovered and exposed by the Los Angeles County Museum of History, Science and Art in the summer of 1915. The Los Angeles County Museum of Natural History resumed excavation at this site in 1969. Retrieval of the “microfossils” from the asphaltic matrix has yielded a wealth of insect, mollusk, and plant remains, more than doubling the number of species recovered by earlier excavations. Today, the current excavation site is 900 square feet in extent, yielding fossils that range in age from about 15,000 to about 42,000 radiocarbon years. Natural History Museum of Los Angeles County Archives, RLB 347. LA BREA AND BEYOND: THE PALEONTOLOGY OF ASPHALT-PRESERVED BIOTAS Edited By John M. Harris NO. 42 SCIENCE SERIES NATURAL HISTORY MUSEUM OF LOS ANGELES COUNTY SCIENTIFIC PUBLICATIONS COMMITTEE Luis M. Chiappe, Vice President for Research and Collections John M. Harris, Committee Chairman Joel W. Martin Gregory Pauly Christine Thacker Xiaoming Wang K. Victoria Brown, Managing Editor Go Online to www.nhm.org/scholarlypublications for open access to volumes of Science Series and Contributions in Science. Natural History Museum of Los Angeles County Los Angeles, California 90007 ISSN 1-891276-27-1 Published on September 15, 2015 Printed at Allen Press, Inc., Lawrence, Kansas PREFACE Rancho La Brea was a Mexican land grant Basin during the Late Pleistocene—sagebrush located to the west of El Pueblo de Nuestra scrub dotted with groves of oak and juniper with Sen˜ora la Reina de los A´ ngeles del Rı´ode riparian woodland along the major stream courses Porciu´ncula, now better known as downtown and with chaparral vegetation on the surrounding Los Angeles. -
Paleobiogeography of Trilophodont Gomphotheres (Mammalia: Proboscidea)
Revista Mexicana deTrilophodont Ciencias Geológicas, gomphotheres. v. 28, Anúm. reconstruction 2, 2011, p. applying235-244 DIVA (Dispersion-Vicariance Analysis) 235 Paleobiogeography of trilophodont gomphotheres (Mammalia: Proboscidea). A reconstruction applying DIVA (Dispersion-Vicariance Analysis) María Teresa Alberdi1,*, José Luis Prado2, Edgardo Ortiz-Jaureguizar3, Paula Posadas3, and Mariano Donato1 1 Departamento de Paleobiología, Museo Nacional de Ciencias Naturales, CSIC, José Gutiérrez Abascal 2, 28006, Madrid, España. 2 INCUAPA, Departamento de Arqueología, Universidad Nacional del Centro, Del Valle 5737, B7400JWI Olavarría, Argentina. 3 LASBE, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Paseo del Bosque S/Nº, B1900FWA La Plata, Argentina. * [email protected] ABSTRACT The objective of our paper was to analyze the distributional patterns of trilophodont gomphotheres, applying an event-based biogeographic method. We have attempted to interpret the biogeographical history of trilophodont gomphotheres in the context of the geological evolution of the continents they inhabited during the Cenozoic. To reconstruct this biogeographic history we used DIVA 1.1. This application resulted in an exact solution requiring three vicariant events, and 15 dispersal events, most of them (i.e., 14) occurring at terminal taxa. The single dispersal event at an internal node affected the common ancestor to Sinomastodon plus the clade Cuvieronius – Stegomastodon. A vicariant event took place which resulted in two isolated groups: (1) Amebelodontinae (Africa – Europe – Asia) and (2) Gomphotheriinae (North America). The Amebelodontinae clade was split by a second vicariant event into Archaeobelodon (Africa and Europe), and the ancestors of the remaining genera of the clade (Asia). In contrast, the Gomphotheriinae clade evolved mainly in North America. -
Mammals and Stratigraphy : Geochronology of the Continental Mammal·Bearing Quaternary of South America
MAMMALS AND STRATIGRAPHY : GEOCHRONOLOGY OF THE CONTINENTAL MAMMAL·BEARING QUATERNARY OF SOUTH AMERICA by Larry G. MARSHALLI, Annallsa BERTA'; Robert HOFFSTETTER', Rosendo PASCUAL', Osvaldo A. REIG', Miguel BOMBIN', Alvaro MONES' CONTENTS p.go Abstract, Resume, Resumen ................................................... 2, 3 Introduction .................................................................. 4 Acknowledgments ............................................................. 6 South American Pleistocene Land Mammal Ages ....... .. 6 Time, rock, and faunal units ...................... .. 6 Faunas....................................................................... 9 Zoological character and history ................... .. 9 Pliocene-Pleistocene boundary ................................................ 12 Argentina .................................................................... 13 Pampean .................................................................. 13 Uquian (Uquiense and Puelchense) .......................................... 23 Ensenadan (Ensenadense or Pampeano Inferior) ............................... 28 Lujanian (LuJanense or Pampeano lacus/re) .................................. 29 Post Pampean (Holocene) ........... :....................................... 30 Bolivia ................ '...................................................... ~. 31 Brazil ........................................................................ 37 Chile ........................................................................ 44 Colombia -
Enamel Prism Patterns in Proboscidean Molar Teeth F
Elephant Volume 2 | Issue 2 Article 11 9-6-1986 Enamel Prism Patterns in Proboscidean Molar Teeth F. Daniel Cring Department of Anthropology, University of Florida Follow this and additional works at: https://digitalcommons.wayne.edu/elephant Recommended Citation Cring, F. D. (1986). Enamel Prism Patterns in Proboscidean Molar Teeth. Elephant, 2(2), 72-79. Doi: 10.22237/elephant/ 1521732011 This Article is brought to you for free and open access by the Open Access Journals at DigitalCommons@WayneState. It has been accepted for inclusion in Elephant by an authorized editor of DigitalCommons@WayneState. Enamel Prism Patterns in Proboscidean Molar Teeth Cover Page Footnote This study was made possible by a research grant from Sigma Xi, the Scientific Research Society, and by the help of two friends, J. Shoshani and C. T. Madden. This article is available in Elephant: https://digitalcommons.wayne.edu/elephant/vol2/iss2/11 72 ELEPHANT Vol. 2, No. 2 ENAMEL PRISM PATTERNS IN PROBOSCIDEAN MOLAR TEETH by F. Daniel Cring Department of Anthropology, University of Florida Gainesville, Florida 32611 USA ABSTRACT: Molar fragments of five proboscidean taxa, representing three families, were examined under the scanning electron microscope for their enamel prism patterns. (Three of the five examined are extinct.) Results show that enamel prisms of Deinotherium are the least dense, whereas the prisms of the Elephantidae genera (Loxodonta, Elephas and Mammuthus) are the most dense, with the enamel prisms of Gomphotherium being intermediate in their density. No significant variations were found among Elephantidae genera. These observations correlate with those of earlier workers (e.g., Osborn, 1942) in that many of the morphological changes used to separate elephants (sensu stricto) from other proboscideans are the result of an evolutionary trend in diet, from the predominately browsing animals (having brachyodont thick-enamel molar teeth) to the predominately grazing animals (having hypsodont thin-enamel molar teeth). -
Retour Sur La Série Type De Gomphotherium Angustidens
e390-11 Tassy.qxd 30/1/12 14:24 Página 321 Estudios Geológicos, 67(2) julio-diciembre 2011, 321-332 ISSN: 0367-0449 doi:10.3989/egeol.40539.191 Retour sur la série type de Gomphotherium angustidens (Proboscidea, Mammalia): de Daubenton à Cuvier, et après Focus on the type series of Gomphotherium angustidens (Proboscidea, Mammalia): from Daubenton to Cuvier, and further P.Tassy1, U.B. Göhlich2 RESUME Les spécimens qui ont permis à Cuvier de décrire le «mastodonte à dents étroites» en 1806, dénom- mé par lui Mastodon angustidens en 1817, sont révisés. Certains d’entre eux (molaires et fragments de molaires), provenant de Simorre (Gers), avaient déjà été mentionnés par Réaumur et par Daubenton au 18e siècle. La série type de Gomphotherium angustidens (CUVIER, 1817) est présentée, discutée et réin- terprétée. Mots clés: Gomphotherium angustidens, proboscidiens, nomenclature, Miocène, Simorre, Daubenton, Cuvier. ABSTRACT We analyze the specimens used by Cuvier to describe in 1806 his «mastodonte à dents étroites», named by him Mastodon angustidens later in 1817. Some of them – molars and partial molars from Simorre (Gers) – were already mentioned by Réaumur and Daubenton during the 18th century. What is considered as the original type series of Gomphotherium angustidens (CUVIER, 1817) is presented and newly interpreted. Key words: Gomphotherium angustidens, proboscideans, nomenclature, Miocene, Simorre, Daubenton, Cuvier. Introduction supérieure restent conjecturales, même si l’espèce est reconnue depuis la Zone MN5 (peut-être même [L]es méthodes de travail et de raisonnement scien- MN4) jusqu’à la Zone MN9 (Göhlich, 1999, pp.162, tifique ont considérablement évolué au cours des 166). -
L'odontologie De Gomphotherium Angustidens (Cuvier, 1817
L’odontologie de Gomphotherium angustidens (Cuvier, 1817) (Proboscidea, Mammalia) : données issues du gisement d’En Péjouan (Miocène moyen du Gers, France) Pascal Tassy To cite this version: Pascal Tassy. L’odontologie de Gomphotherium angustidens (Cuvier, 1817) (Proboscidea, Mam- malia) : données issues du gisement d’En Péjouan (Miocène moyen du Gers, France). Geodiversitas, Museum National d’Histoire Naturelle Paris, 2014, 36 (1), pp.35-115. 10.5252/g2014n1a2. hal- 01324877 HAL Id: hal-01324877 https://hal.sorbonne-universite.fr/hal-01324877 Submitted on 1 Jun 2016 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. L’odontologie de Gomphotherium angustidens (Cuvier, 1817) (Proboscidea, Mammalia) : données issues du gisement d’En Péjouan (Miocène moyen du Gers, France) Pascal TASSY Muséum national d’Histoire naturelle, Département Histoire de la Terre, UMR 7207 CNRS- MNHN-UPMC, Centre de Recherches sur la Paléobiodiversité et les Paléoenvironnements (CR2P), case postale 38, 57 rue Cuvier, 75231 Paris cedex 05 (France) [email protected] Tassy P. 2014. -
Notes from the ...Field the Landmark Is on Fire
The Newsletter of Lubbock Lake National Historic Landmark Winter 2013 Notes from the ...Field The Landmark is on Fire By Matthew McEwen, Heritage Maintenance Technician Heritage Maintenance Supervisor Scott Trevey directs fire fighters from Lubbock Fire Department At the Landmark, prescribed burning is a part of restoration efforts in order to manipulate the vegetation to what it looked like before European settlement. Fire plays an integral part for achieving many of the management objectives. These objectives include suppressing mesquite, increasing biodiversity, and improving habitat for the Texas horned lizard. Prescribed burning is the controlled application of fire to the landscape under specified environmental conditions. Weather in the for of wind speed, direction, temperature, humidity, and frontal systems are important factors when planning and implementing a prescribed burn. The trails, perimeter roads, and archaeology-friendly mineral lines are used where possible to confine where the fire should burn. The Landmark’s recent reintroduction of fire includes prescribed burning of several hundred brush piles since 2006, a prescribed burn around the Llano Estacado Wildflower Trail in 2009, and another in the northern 80 acres in 2010. These burns have been applied during the dormant season. The dormant season typically provides for higher humidity and lower temperatures, allowing the fire behavior to be relatively predictable. Continued on page 3 Inside this Issue….. The Landmark is on Fire 1 Bison antiquus Skeletal Remains found in Firstview 4 2B Sediments Root or Fence Post?: Excavations at a Historic Cowboy Camp 6 Ancient Deposits Reveal Extinct and Extant Animals of the 7 Southern High Plains Licking Horse Bones in Mustang Draw 9 Summer Fun at Lubbock Lake Landmark 10 Summer Youth make Quilts for Project Linus 11 Pleistocene Proboscidean Tusk Segments Discovered 12 The turtle appears to be a three-toed box turtle based on the Raised-arm human with horns and possible arrow clear depiction of three toes on one of the hind feet.