Hippotherium Primigenium 10.3 Ma

Total Page:16

File Type:pdf, Size:1020Kb

Hippotherium Primigenium 10.3 Ma the natural history of HOEWENEGG A SKELETON, BERNOR ET AL. 1997 HORSES RAY BERNOR,COLLEGE OF MEDICINE, DEPARTMENT OF ANATOMY, HOWARD UNIVERSITY, WASHINGTON D.C. the natural history of HORSES •BRIEF HISTORY OF EQUID RESEARCH •FIELD-BASED RESEARCH BEARING ON EVOLUTIONARY HISTORY OF O.W. HIPPARIONS •BIOGEOGRAPHIC PROVINCIALITY AND ITS BEARING ON EQUID EVOLUTION •RECONSTRUCTING PALEODIET •EVOLUTIONARY STUDIES OF THE GENUS EQUUS •ANATOMICAL AND BIOLOGICAL BASES OF RACE HORSE FOOT INJURIES • MOLECULAR AND PALEONTOLOGICAL ON EQUUS CONTRARY TO MIVART, Darwin DID not BELIEVE THAT THE EXTINCT THREE-TOED HORSE Hipparion evolved suddenly (DARWIN, 1872: 201) Gaudry 1866 T.H. Huxley 1876 VISITS YALE PEABODY MUSEUM TO DISCUSS HORSE EVOLUTION WITH O.C. MARSH, 1876 GAUDRY EARLY STUDENTS OF EQUID EVOLUTION MATTHEW MARSH OSBORN STIRTON Orthogenetic Evolution MATTHEW, 1903, 1926 STIRTON, 1940 George G. Simpson MacFadden, 2005 Science Vol. 307. no. 5716, pp. 1728 - 1730 Maragheh, N.W. Iran, 1974 Maragheh Field Team, 1976 Maragheh Geochronology 1980-1996 7.4 7.67.8 8.2 8.28.6 9.0 Maragheh Hipparion Evolution Cr. matthewi 7.9 aff. H. brachypus Cr. moldavicum 8.2 8.6 Taxa in red after Bernor et al. 2016 9.0 Old World Later Neogene Provinciality: Cluster Analyses on Genus Faunal Resemblances BERNOR, BERNOR AND PAVLAKIS, 1978 1987 BERNOR, 1983 EASTERN AFRICA PROVINCIALITY AND ZOOGEOGRAPHIC EVOLUTION OF THE OLD WORLD LATER NEOGENE BIOME 16-5.2 MA The Late Miocene Pikermian Chronofauna: The Samos family portrait Nikos 1993 Samos Horse Lineages: 10 taxa 8-6.7 Ma 6.7 Ma Cr. mediterraneum Hippotherium sp. Cr. matthewi H. dietrichi By: G. Koufos and D. Vlachou 8.2 Ma Cr. proboscideum Raup-Crick Genus Faunal Resemblance Index Values as Compared to Pikermi (MN 11, ca. 8.0 Ma) MN 7+8 MN 9 MN 12 MIO-PLIOCENE BOUNDARY = MN13/14 MN 14 (5.3-4.2) MN 13 (6.6-5.3) MN 12 (8.0-6.6) MN 11 (8.7-8.0) MN 10 (9.7-8.7) MN 9 (11.1-9.7) MN 13 MN 14 MN 7+8 (13.5-11.1) ERONEN, MIRZAIE, KARME, MICHEELS, BERNOR AND FORTELIUS,2009, PNAS Hegau District, S.W. Germany HEGAU DISTRICT, SOUTHERN GERMANY GRABUNG HOEWENEGG Hoewenegg Excavations in the 1950s and 60s Ho E Skeleton With Fetus in Situs Utero RENEWED RESEARCH 1986 1991 1992 2001-2016 TOBIEN REVISIT IN 1986 1986 TRENCH 1991 DISCOVERY OF MIOTRAGOCERUS SKULL Section Skeletons Reopened in 2003 Hoewenegg 2003 Miotragocerus with 2 fetuses in situs utero 2004 Extension of the Site to the NW 2005 - Extending the Excavation to the West Hoewenegg West Quarry Biotic Elements Collected 2004-2006 Field Seasons Exclusive of Gastropods 38 4 21 Plants 18 Crustacea 2 Vertebrata indet. Pices Amphibia 81 Reptilia 266 Aves Mammalia 2 Figure 11 - Proportions of Biotic Contents by Stratigraphic Level 100% Mammalia 80% Aves Reptilia 60% Amphibia Pices Vert. indet. 40% Insecta Crustacea 20% Gastropoda Plants 0% 5 7 9 Sol 11 13 15 17 19 Proportion of Hoewenegg Mammal Species Skeletons 5% 2% 2% Hippotherium 7% Miotragocerus 37% Rhinos Deinotherium Dorcatherium Muntiak 47% Stratigraphic Provenance of the Höwenegg Skeletons – The Jorg and Tobien Stratigraphic Numbering System HORIZO Hippotherium Miotragocerus Rhinos Deinotherium Dorcatherium Muntjak N 18 1 20 6 (2) 9 (6, f) 1 1 (1) 1 22a 25 4 (f) 2 1 1 27 1 3 32 3 2 34 2 42 1 Hoewenegg Lageplan 2012 Central European Vallesian Habitats 11-9.7 Ma BERNOR ET AL., 1988 VEGETATION RECONSTRUCTION BY JOHANNA EDER GYRAULUS KLEINI ULMUS Populus TROPIDOMPHALUS (P.) ZELLI HOEWENEGG FLORA & INVERTEBRATES Hoewenegg Hippotherium primigenium 10.3 Ma. POF-LACRIMAL SPINOUS PROCESSES SACRUM TEETH LIMBS COMPOSITE CHRONOLOGY OF THE SINAP FORMATION FOSSIL LOCALITIES, TURKEY 11-9 MA DETAIL OF SINAP TEPE "Hipparion" uzunagizli 9.97 Cormohipparion "Hipparion" sp. sinapensis cursorial form 10.692 10.08 "Hipparion" kecigibi "Hipparion" Old World 9.92 sp. large Hipparions 9.59 Cormohipparion sp.(Woodburne, 2007&2009) 11 Ma 40 11.2-6MA 11.2 10.08-9.59 11.2 10.7 10.5 10.7 10.5 A Systematic, Biostratigraphic, and Paleogeographic Reevaluation of the Siwalik Hipparion Horse Assemblage from the Potwar Plateau, Northern Pakistan - an application of paleontological and paleoecological methodology to the assessment of a regional population of hipparionine horses Wolf, 2012. Siwalik Taxonomy – Sivalhippus perimense Wolf, Bernor and Hussain, 2013) Sivalhippus theobaldi Bernor et al. (2010) AMNH 98728 GSI C153; holotype MacFadden and Woodburne (1982) Stratigraphic Distribution of Siwalik Hipparionines Wolf, Bernor and Hussain, 2013 MAJOR OLD WORLD LATE MIOCENE CLADES 1996 Plio-Pleistocene Lineages: Eurygnathohippus, Plesiohipparion, Proboscidipparion DIACHRONEITY OF CROWN HEIGHT SPIKES IN OLD WORLD HIPPARIONS 2013 11.4 Ma = 50 MM 2 MA > 90 MM 6.7 MA = 10.5 = 85 MM 60 MM 8.5 MA = 70 MM 1.2 MA = 90 MM 5 MA = 80 MM Horses Eat Grass MESOWEAR ANALYSIS Fortelius and Solounias, 2000, Mihlbachler et al., 2011, Wolf et al., 2012 0 0 Sharp CUSPS & HIGH RELIEF 0.51 2 1 Rounded CUSPS & HIGH RELIEF 1.53 2 4 Rounded CUPS & LOW RELIEF 2.55 Blunt CUSPS & LOW 6 RELIEF 3 VARIABLES: RELIEF RELIEF AND SHAPE Old World Hipparionine Diets EURYGNATHOHIPPUS CORNELIANUS DINOTHERIENSANDE 1.4 MA 10 MA CLUSTER ANALYSIS OF MESOWEAR PARAMETER FREQUENCIES IN 27 EXTANT UNGULATE SPECIES AND 10 HIPPARIONINE POPULATIONS (Methodology Following Fortelius & Solounias, 2000; Bernor & Kaiser 2006 a & b; Bernor et al., 2004) Bison bison CERATOTHERIUM SIMUM EQUUS BURCHELLI EQUUS GREVYI DAMALISCUS LUNATUS GRAZER Eurygnathohippus (LANGEBAANWEG & SAHABI) CONNOCHAETES TAURINUS Alcelaphus buselaphus HIPPOTRAGUS NIGER Redunca redunca HIPPOTRAGUS EQUINUS KOBUS ELLIPSIPRYMNUS Cormohipparion goorisi Cormohipparion quinni Merychippus insignis (BALTAVAR) AEPYCEROS MELAMPUS CAPRICORNIS SUMATRAENSIS CERVUS CANADENSIS Cormohipparion sp. (CHORORA) MIXED TAUROTRAGUS ORYX TRAGELAPHUS SCRIPTUS FEEDER Hippotherium prim/intrans (DD & RUD) GAZELLA GRANTI GAZELLA THOMSONI OVIBOS MOSCHATUS GIRAFFA CAMELOPARDALIS ODOCOILEUS HEMIONUS Hippotherium primigenium (HOEWENEGG) DICERORHINUS SUMATRENSIS OKAPIA JOHNSTONI ODOCOILEUS VIRGINIANUS DICEROS BICORNIS BROWSER ALCES ALCES RHINOCEROS SONDAICUS NED 0 10 20 30 40 50 60 70 80 90 100 SCRATCHES PITS LIGHT MICROSCOPE MICROWEAR Courtesy of Gina Semprebon (SCALE BAR = 0.4 MM) Phylogeny of Equus Azzaroli, 2003 Equus asinus OLD WORLD GEOGRAPHY OF LIVING EQUUS SPECIES Mitochondrial Research 2005 Leonard, Rohland, Glaberman, Fleischer, Caccone and Hofreiter Barbaro and 8 Bells BARBARO AT THE DERBY 8 BELLS AT THE DERBY Jockey Gabriel Saez "heard the worst sound possible - a pop” [the Huffington Post, October 6, 2008 BARBARO BREAK AND THERAPY ! DR. CHRIS KAWCAK DVM, COLORADO STATE VETERINARY SCHOOL ANATOMY OF RACE HORSE FOOT FRACTURE DR. KAWCAK’S FACT-LIST • 97 % OF ALL FRACTURES ARE TO THE LATERAL CONDYLE OF MPIII [MORE FORELIMB THAN HINDLIMB] FOLLOWED BY FRACTURES OF THE SESAMOID AND THE PASTERN [1ST + 2ND PHALANGES] • FRACTURES ARE FOUND IN HORSES WITH LONG MPIII’S THERE IS REDUCED VOLUME [=SIZE] OF LATERAL CONDYLES THAT BREAK • A “GOOD HORSE” HAS SHORT METAPODIALS Do Race Horses Need 3 Toes? A. The Horse has MPII & IV splints with fibrous connection to MPIII B. Hipparions have fully functional MPIII/MPII & IV joints and complete digits II and IV C. MP IV is more stoutly developed than MPII giving greater support laterally than medially Diagrammatic expression maps for 50 genes of the Hox A (top) and Hox D (bottom) clusters during early, middle and late stages of forelimb outgrowth. Reno et al., 2007 Fig. 2 Anatomical Maps of the Autopod (wrist and hand) Reno et al., 2007 Fig. 3 CONSERVE THE SOMALIAN ASS THANK YOU PSW, 02-15-2017 END.
Recommended publications
  • The Baltavar Hippotherium: a Mixed Feeding Upper Miocene Hipparion (Equidae, Perissodactyla) from Hungary (East- Central Europe)
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Beiträge zur Paläontologie Jahr/Year: 2006 Band/Volume: 30 Autor(en)/Author(s): Kaiser Thomas M., Bernor Raymond L. Artikel/Article: The Baltavar Hippotherium: A mixed feeding Upper Miocene hipparion (Equidae, Perissodactyla) from Hungary (East-Central Europe) 241-267 ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont., 30:241-267, Wien 2006 The Baltavar Hippotherium: A mixed feeding Upper Miocene hipparion (Equidae, Perissodactyla) from Hungary (East- Central Europe) by Thomas M. Kaiser 1} & Raymond L. Bernor * 2) Kaiser , Th.M. & B ernor , R.L., 2006. The Baltavar Hippotherium. A mixed feeding Upper Miocene hipparion (Equidae, Perissodactyla) from Hungary (East-Central Europe). — Beitr. Palaont., 30:241-267, Wien. Abstract browse ratio of 50/50% in its diet. The impala lives in tropi­ cal east Africa in grass dominated open environments like The genus Hippotherium evolved in Central and Western bushland and Acacia savannahs but also in Acacia forests Europe following the “Hipparion Datum” and is particu­ and other deciduous woodlands. It further has one of the larly remarkable for its complexly ornamented enamel pli­ most abrasive diets among extant mixed feeders and is con­ cations on the maxillary and mandibular cheek teeth. The sistently classified next to the grazers in mesowear evalu­ Baltavar hipparion assemblage is of importance because it ation. The comparatively abrasive diet of H. “microdon” represents one of the latest known populations of Central suggests the presence of grass or other abrasive vegetation European Hippotherium. The Baltavar fauna accumulated in the Baltavar paleohabitat.
    [Show full text]
  • I Vertebrati Fossili Della Cava Del Monticino Di Brisighella: Una Finestra Sui Popolamenti Continentali Del Mediterraneo Nel Miocene Superiore
    I GESSI DI BRISIGHELLA E RONTANA Memorie dell’Istituto Italiano di Speleologia s. II, 28, 2015, pp. 79-100 I VERTEBRATI FOSSILI DELLA CAVA DEL MONTICINO DI BRISIGHELLA: UNA FINESTRA SUI POPOLAMENTI CONTINENTALI DEL MEDITERRANEO NEL MIOCENE SUPERIORE LORENZO ROOK1, MASSIMO DELFINO2, MARCO SAMI3 Riassunto Situata all’estremità orientale della Vena del Gesso romagnola presso l’abitato di Brisighella (RA), la cava di gesso del Monticino, ora riconvertita a geoparco, rappresenta uno dei giacimenti paleon- tologici a vertebrati continentali tardo-miocenici più importanti d’Italia. I resti fossili, più o meno frammentari, sono preservati entro i sedimenti della Formazione a Colombacci che ricolmavano numerose fessure paleocarsiche caratterizzanti la sottostante F.ne Gessoso-solfifera, il tutto sigil- lato da peliti marine della F.ne Argille Azzurre; un assetto geologico di questo tipo ha permesso di vincolare cronologicamente la paleofauna alla parte terminale del Messiniano, circa 5,4 milioni di anni fa. L’associazione fossile del Monticino è rappresentata da 58 diverse specie di vertebrati ter- restri e cioè 19 taxa tra anfibi e rettili (ad esempio coccodrillo, varano, boa delle sabbie, ecc.) e 39 taxa di mammiferi (ad esempio scimmia, oritteropo, rinoceronte, ecc.): tra questi ultimi si segnala- no ben 5 specie nuove per la Scienza, quali lo ienide Plioviverrops faventinus, il canide Eucyon mon- ticinensis, il bovide Samotragus occidentalis nonché i roditori Stephanomys debruijni e Centralomys benericettii. L’analisi ecologica della paleofauna ha permesso di ipotizzare un antico ambiente con clima di tipo temperato-caldo o sub-tropicale. Parole chiave: Fossili, Vertebrati continentali, Formazione a Colombacci, Messiniano terminale, Italia. Abstract The Monticino gypsum quarry (now converted into a geo-park), located near the town of Brisighella (Ravenna, Northern Italy), at the Eastern margin of the Vena del Gesso romagnola, is one of the most important paleontological sites with continental vertebrates in the Late Miocene of Italy.
    [Show full text]
  • Latest Hipparion Christol, 1832 in Europe. a Review of the Pliocene Hipparion Crassum Gervais Group and Other Finds (Mammalia, Equidae)
    Latest Hipparion Christol, 1832 in Europe. A review of the Pliocene Hipparion crassum Gervais Group and other finds (Mammalia, Equidae) † Ann FORSTEN Finnish Museum of Natural History, PB 17, FIN-00014 Helsinki (Finland) Forsten A. 2002. — Latest Hipparion Christol, 1832 in Europe. A review of the Pliocene Hipparion crassum Gervais Group and other finds (Mammalia, Equidae). Geodiversitas 24 (2) : 465-486. ABSTRACT The mainly late Miocene equid genus Hipparion Christol, 1832 still occurred in the early and middle Pliocene of Eurasia. Known European finds are here reviewed; most are referred to a “H. crassum Group”, chiefly because of their common dental morphology, but also on their limb bone proportions KEY WORDS when known. The group may comprise more than one species, as indicated Mammalia, by metapodial proportions, but new taxa are not formally described, because Equidae, of the paucity of the material mostly consisting of isolated teeth. Some other Hipparion crassum Group, Pliocene, finds from the same period, sometimes referred to H. crassum Gervais, 1859 Europe. but of uncertain relationship, are discussed. RÉSUMÉ Les derniers Hipparion Christol, 1832 en Europe. Examen du Groupe Hipparion crassum Gervais du Pliocène et autres découvertes (Mammalia, Equidae). Le genre Hipparion Christol, 1832, qui date principalement du Miocène supérieur, est encore présent dans le Pliocène de l’Eurasie. Les découvertes européennes connues sont examinées ici ; la plupart se réfèrent au « Groupe H. crassum », principalement en raison de leur morphologie dentaire, mais MOTS CLÉS aussi des proportions des os de leurs membres. Certaines autres découvertes Mammalia, de la même époque, parfois se référant à H. crassum Gervais, 1859 mais dont Equidae, les affinités sont incertaines, sont discutées.
    [Show full text]
  • 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.
    [Show full text]
  • Isotopic Dietary Reconstructions of Pliocene Herbivores at Laetoli: Implications for Early Hominin Paleoecology ⁎ John D
    Palaeogeography, Palaeoclimatology, Palaeoecology 243 (2007) 272–306 www.elsevier.com/locate/palaeo Isotopic dietary reconstructions of Pliocene herbivores at Laetoli: Implications for early hominin paleoecology ⁎ John D. Kingston a, , Terry Harrison b a Department of Anthropology, Emory University, 1557 Dickey Dr., Atlanta, GA 30322, United States b Center for the Study of Human Origins, Department of Anthropology, New York University, 25 Waverly Place, New York, NY 10003, United States Received 20 September 2005; received in revised form 1 August 2006; accepted 4 August 2006 Abstract Major morphological and behavioral innovations in early human evolution have traditionally been viewed as responses to conditions associated with increasing aridity and the development of extensive grassland-savanna biomes in Africa during the Plio- Pleistocene. Interpretations of paleoenvironments at the Pliocene locality of Laetoli in northern Tanzania have figured prominently in these discussions, primarily because early hominins recovered from Laetoli are generally inferred to be associated with grassland, savanna or open woodland habitats. As these reconstructions effectively extend the range of habitat preferences inferred for Pliocene hominins, and contrast with interpretations of predominantly woodland and forested ecosystems at other early hominin sites, it is worth reevaluating the paleoecology at Laetoli utilizing a new approach. Isotopic analyses were conducted on the teeth of twenty-one extinct mammalian herbivore species from the Laetolil Beds (∼4.3–3.5 Ma) and Upper Ndolanya Beds (∼2.7–2.6 Ma) to determine their diet, as well as to investigate aspects of plant physiognomy and climate. Enamel samples were obtained from multiple localities at different stratigraphic levels in order to develop a high-resolution spatio-temporal framework for identifying and characterizing dietary and ecological change and variability within the succession.
    [Show full text]
  • Issn: 2250-0588 Fossil Mammals
    IJREISS Volume 2, Issue 8 (August 2012) ISSN: 2250-0588 FOSSIL MAMMALS (RHINOCEROTIDS, GIRAFFIDS, BOVIDS) FROM THE MIOCENE ROCKS OF DHOK BUN AMEER KHATOON, DISTRICT CHAKWAL, PUNJAB, PAKISTAN 1Khizar Samiullah* 1Muhammad Akhtar, 2Muhammad A. Khan and 3Abdul Ghaffar 1Zoology department, Quaid-e-Azam campus, Punjab University, Lahore, Punjab, Pakistan 2Zoology Department, GC University, Faisalabad, Punjab, Pakistan 3Department of Meteorology, COMSATS Institute of Information Technology (CIIT), Islamabad ABSTRACT Fossil site Dhok Bun Ameer Khatoon (32o 47' 26.4" N, 72° 55' 35.7" E) yielded a significant amount of mammalian assemblage including two families of even-toed fossil mammal (Giraffidae, and Bovidae) and one family of odd-toed (Rhinocerotidae) of the Late Miocene (Samiullah, 2011). This newly discovered site has well exposed Chinji and Nagri formation and has dated approximately 14.2-9.5 Ma. This age agrees with the divergence of different mammalian genera. Sedimentological evidence of the site supports that this is deposited in locustrine or fluvial environment, as Chinji formation is composed primarily of mud-stone while the Nagri formation is sand dominated. Palaeoenvironmental data indicates that Miocene climate of Pakistan was probably be monsoonal as there is now a days. Mostly the genera recovered from this site resemble with the overlying younger Dhok Pathan formation of the Siwaliks while the size variation in dentition is taxonomically important for vertebrate evolutionary point of view and this is the main reason to conduct this study at this specific site to add additional information in the field of Palaeontology. A detailed study of fossils mammals found in Miocene rocks exposed at Dhok Bun Ameer Khatoon was carried out.
    [Show full text]
  • Linnean 20-4 Web.P65
    THE LINNEAN Newsletter and Proceedings of THE LINNEAN SOCIETY OF LONDON Bur lington House , Piccadill y, London W1J 0BF VOLUME 20 • NUMBER 4 • OCTOBER 2004 THE LINNEAN SOCIETY OF LONDON Burlington House, Piccadilly, London W1J 0BF Tel. (+44) (0)20 7434 4479; Fax: (+44) (0)20 7287 9364 e-mail: [email protected]; internet: www.linnean.org President Secretaries Council Professor G McG Reid BOTANICAL The Officers and Dr J R Edmondson Dr L Allcock Vice-Presidents Prof J R Barnett Dr R M Bateman ZOOLOGICAL Prof S Blackmore Professor D F Cutler Dr V R Southgate Prof J Browne Dr J M Edmonds Dr J S Churchfield Dr V R Southgate EDITORIAL Dr J C David Professor D F Cutler Dr A Farjon Treasurer Dr M F Fay Professor G Ll Lucas OBE COLLECTIONS Dr P Kenrick Mrs S Gove Dr K N Maybury Executive Secretary Dr A D Rogers Mr Adrian Thomas OBE Librarian & Archivist Dr B R Rosen Miss Gina Douglas Dr D A Simpson Office/Facilities Manager Dr R A Sweeting Mr Dominic Clark Assistant Librarian Ms Cathy Broad Library Assistant Finance (on secondment to NHM) Mr Matthew Derrick Mr Priya Nithianandan Catalogue Coordinator Conservator Ms Lynn Crothall Ms Janet Ashdown THE LINNEAN Newsletter and Proceedings of the Linnean Society of London Edited by B. G. Gardiner Editorial .............................................................................................................. 1 Society News ............................................................................................................ 2 Library .............................................................................................................
    [Show full text]
  • Hipparion” Cf
    ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont., 30:15-24, Wien 2006 Hooijer’s Hypodigm for “ Hipparion” cf. ethiopicum (Equidae, Hipparioninae) from Olduvai, Tanzania and comparative Material from the East African Plio-Pleistocene by Miranda A rmour -Chelu 1}, Raymond L. Bernor 1} & Hans-Walter Mittmann * 2) A rmour -C helu , M., Bernor , R.L. & M ittmann , H.-W., 2006. Hooijer’s Hypodigm for “ Hipparion” cf. ethiopicum (Equidae, Hipparioninae) from Olduvai, Tanzania and comparative Material from the East African Plio-Pleistocene. — Beitr. Palaont., 30:15-24, Wien. Abstract cranialen Elemente die Hooijer zu diesem Taxon gestellt hat, auf die er sich bezogen hat oder die in irgendeiner We review here the problematic history of the nomen Beziehung dazu stehen, haben wir wiedergefunden. Selbst “Hipparion”cf. ethiopicum and Hooijer’s efforts to bring zusätzliche Fundstücke aus zeitgleichen Horizonten haben some taxonomic sense to the later Pliocene - Pleistocene wir miteinbezogen, in der Absicht, die Gültigkeit von Eu­ hipparion record. We review his reasoning, and the shifts rygnathohippus cf.“ethiopicum" und seines Verwandten in taxonomic allocation made by him and other equid Eurygnathohippus cornelianus und weiterer Formen, von researchers during the 1970’s. We have relocated many denen Hooijer geglaubt hat, dass sie in einem evolutionären of the postcranial specimens attributed by Hooijer to Zusammenhang mit „ Hipparion“ cf. ethiopicum stehen, “Hipparion” cf. ethiopicum, as well as other specimens zu testen. Wir machen statistische und vergleichende which he referred to, or related to this species. We have Analysen um dieses Hypodigma zu klären. also considered additional specimens from contempo­ raneous horizons, in order to reevaluate the efficacy of Eurygnathohippus cf “ethiopicum” and its apparent rela­ 1.
    [Show full text]
  • A New Collection of Hipparionine from the Type Locality of the Dhok Pathan Formation of the Middle Siwaliks
    Khan et al. The Journal of Animal & Plant Sciences, 21(1): 2011, Page:J. Anim.83-89 Plant Sci. 21(1):2011 ISSN: 1018-7081 A NEW COLLECTION OF HIPPARIONINE FROM THE TYPE LOCALITY OF THE DHOK PATHAN FORMATION OF THE MIDDLE SIWALIKS M. A. Khan, F. Manzoor, M. Ali**, Z. H. Bhatti**, and M. Akhtar** Zoology Department, GC University, Faisalabad *Zoology Department, Government College Science, Wahdat Road, Lahore **Zoology Department, Quaid-e-Azam Campus, Punjab University, Lahore Corresponding author e-mail: ABSTRACT The new discovered material found from the Dhok Pathan type locality identifies two species of Hipparionine, Sivalhippus cf. theobaldi and Hipparion sp. The described material consists of the isolated upper cheek teeth and reflects all morphological features of Sivalhippus cf. theobaldi and Hipparion sp. Sivalhippus cf. theobaldi comprises two well preserved specimens and Hipparion sp. comprises four well preserved specimens. Sivalhippus cf. theobaldi is a large species with less complicated enamel plications whereas Hipparion sp. is moderate in size with more complicated enamel plications. Key words: Hipparion, Middle Siwaliks, Mammals, Dhok Pathan Formation. INTRODUCTION the late Miocene to Pliocene in age (Fig. 1). The Dhok Pathan Formation is composed of sand stones with In the Siwaliks, Hipparion first appeared by a alternate clay and minor layers of conglomerate in lower single migration, recorded in lithologic boundary of the part and more conglomerates with sandstone and clay in Nagri Formation (Pilbeam et al., 1997). Hipparion sp. upper part. The clays are orange brown in colour (Barry was found abundantly in the Middle Siwaliks and et al., 2002). considered to be as one of the faunal members of the Siwalik Late Miocene sediments (Hussain, 1971; Naseem MATERIALS AND METHODS et al., 2009).
    [Show full text]
  • The First Occurrence of Eurygnathohippus Van Hoepen, 1930 (Mammalia, Perissodactyla, Equidae) Outside Africa and Its Biogeograph
    TO L O N O G E I L C A A P I ' T A A T L E I I A Bollettino della Società Paleontologica Italiana, 58 (2), 2019, 171-179. Modena C N O A S S. P. I. The frst occurrence of Eurygnathohippus Van Hoepen, 1930 (Mammalia, Perissodactyla, Equidae) outside Africa and its biogeographic signifcance Advait Mahesh Jukar, Boyang Sun, Avinash C. Nanda & Raymond L. Bernor A.M. Jukar, Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington DC 20013, USA; [email protected] B. Sun, Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China; University of Chinese Academy of Sciences, Beijing 100039, China; College of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, Howard University, Washington D.C. 20059, USA; [email protected] A.C. Nanda, Wadia Institute of Himalayan Geology, Dehra Dun 248001, India; [email protected] R.L. Bernor, College of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, Howard University, Washington D.C. 20059, USA; [email protected] KEY WORDS - South Asia, Pliocene, Biogeography, Dispersal, Siwalik, Hipparionine horses. ABSTRACT - The Pliocene fossil record of hipparionine horses in the Indian Subcontinent is poorly known. Historically, only one species, “Hippotherium” antelopinum Falconer & Cautley, 1849, was described from the Upper Siwaliks. Here, we present the frst evidence of Eurygnathohippus Van Hoepen, 1930, a lineage hitherto only known from Africa, in the Upper Siwaliks during the late Pliocene. Morphologically, the South Asian Eurygnathohippus is most similar to Eurygnathohippus hasumense (Eisenmann, 1983) from Afar, Ethiopia, a species with a similar temporal range.
    [Show full text]
  • New Insights on the Early Pleistocene Equids from Roca-Neyra (France, Central Europe): Implications for the Hipparion LAD and the Equus FAD in Europe
    Journal of Paleontology, 95(2), 2021, p. 406–425 Copyright © The Author(s), 2020. Published by Cambridge University Press on behalf of The Paleontological Society 0022-3360/21/1937-2337 doi: 10.1017/jpa.2020.99 New insights on the Early Pleistocene equids from Roca-Neyra (France, central Europe): implications for the Hipparion LAD and the Equus FAD in Europe Omar Cirilli,1,2* Raymond L. Bernor,3,4 and Lorenzo Rook2 1Dottorato di Ricerca in Scienze della Terra, Università di Pisa, Via S. Maria 53, 56126 Pisa, Italy <[email protected]> 2Dipartimento di Scienze della Terra, Paleo[Fab]Lab, Università degli Studi di Firenze, Via G. La Pira 4, 50121 Firenze, Italy <lorenzo. rook@unifi.it> 3College of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, 520 W St. N.W., 20059, Washington D.C., USA <[email protected]> 4Human Origins Program, Department of Anthropology, Smithsonian Institution, 20560, Washington D.C., USA Abstract.—We undertake a redescription of the equid sample from the Early Pleistocene of Roca-Neyra, France. This locality has been recently calibrated at the Pliocene/Pleistocene boundary (2.6 ± 0.2 Ma) and therefore it is of interest for the first appearance of the genus Equus and last appearance of hipparionine horses. The Roca-Neyra equid sample, re- analyzed herein using morphological, morphometrical, and statistical analyses, has revealed the co-occurrence of Plesio- hipparion cf. ?P. rocinantis and Equus cf. E. livenzovensis. The analysis undertaken on several European, African, and Asian “Hipparion” sensu lato species from late Miocene to Early Pleistocene has revealed different remnant Hipparion lineages in the Plio-Pleistocene of Europe: Plesiohipparion, Proboscidippaion, and likely Cremohipparion.
    [Show full text]
  • The Evolution of Occlusal Enamel Complexity in Middle
    THE EVOLUTION OF OCCLUSAL ENAMEL COMPLEXITY IN MIDDLE MIOCENE TO RECENT EQUIDS (MAMMALIA: PERISSODACTYLA) OF NORTH AMERICA by NICHOLAS ANTHONY FAMOSO A THESIS Presented to the Department of Geological Sciences and the Graduate School of the University of Oregon in partial fulfillment of the requirements for the degree of Master of Science June 2013 THESIS APPROVAL PAGE Student: Nicholas Anthony Famoso Title: The Evolution of Occlusal Enamel Complexity in Middle Miocene to Recent Equids (Mammalia: Perissodactyla) of North America This thesis has been accepted and approved in partial fulfillment of the requirements for the Master of Science degree in the Department of Geological Sciences by: Dr. Edward Davis Chair Dr. Qusheng Jin Member Dr. Stephen Frost Outside Member and Kimberly Andrews Espy Vice President for Research & Innovation/Dean of the Graduate School Original approval signatures are on file with the University of Oregon Graduate School. Degree awarded June 2013 ii © 2013 Nicholas Anthony Famoso iii THESIS ABSTRACT Nicholas Anthony Famoso Master of Science Department of Geological Sciences June 2013 Title: The Evolution of Occlusal Enamel Complexity in Middle Miocene to Recent Equids (Mammalia: Perissodactyla) of North America Four groups of equids, “Anchitheriinae,” Merychippine-grade Equinae, Hipparionini, and Equini, coexisted in the middle Miocene, and only the Equini remains after 16 million years of evolution and extinction. Each group is distinct in its occlusal enamel pattern. These patterns have been compared qualitatively but rarely quantitatively. The processes controlling the evolution of these occlusal patterns have not been thoroughly investigated with respect to phylogeny, tooth position, and climate through geologic time. I investigated two methods of quantitative analysis, Occlusal Enamel Index for shape and fractal dimensionality for complexity.
    [Show full text]