Maragheh Ungulate Mesowear: Interpreting Paleodiet and Paleoecology from a Diverse Fauna with Restricted Sample Sizes
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Unit-V Evolution of Horse
UNIT-V EVOLUTION OF HORSE Horses (Equus) are odd-toed hooped mammals belong- ing to the order Perissodactyla. Horse evolution is a straight line evolution and is a suitable example for orthogenesis. It started from Eocene period. The entire evolutionary sequence of horse history is recorded in North America. " Place of Origin The place of origin of horse is North America. From here, horses migrated to Europe and Asia. By the end of Pleis- tocene period, horses became extinct in the motherland (N. America). The horses now living in N. America are the de- scendants of migrants from other continents. Time of Origin The horse evolution started some 58 million years ago, m the beginning of Eocene period of Coenozoic era. The modem horse Equus originated in Pleistocene period about 2 million years ago. Evolutionary Trends The fossils of horses that lived in different periods, show that the body parts exhibited progressive changes towards a particular direction. These directional changes are called evo- lutionary trends. The evolutionary trends of horse evolution are summarized below: 1. Increase in size. 2. Increase in the length of limbs. 3. Increase in the length of the neck. 4. Increase in the length of preorbital region (face). 5. Increase in the length and size of III digit. 6. Increase in the size and complexity of brain. 7. Molarization of premolars. Olfactory bulb Hyracotherium Mesohippus Equus Fig.: Evolution of brain in horse. 8. Development of high crowns in premolars and molars. 9. Change of plantigrade gait to unguligrade gait. 10. Formation of diastema. 11. Disappearance of lateral digits. -
Barren Ridge FEIS-Volume IV Paleo Tech Rpt Final March
March 2011 BARREN RIDGE RENEWABLE TRANSMISSION PROJECT Paleontological Resources Assessment Report PROJECT NUMBER: 115244 PROJECT CONTACT: MIKE STRAND EMAIL: [email protected] PHONE: 714-507-2710 POWER ENGINEERS, INC. PALEONTOLOGICAL RESOURCES ASSESSMENT REPORT Paleontological Resources Assessment Report PREPARED FOR: LOS ANGELES DEPARTMENT OF WATER AND POWER 111 NORTH HOPE STREET LOS ANGELES, CA 90012 PREPARED BY: POWER ENGINEERS, INC. 731 EAST BALL ROAD, SUITE 100 ANAHEIM, CA 92805 DEPARTMENT OF PALEOSERVICES SAN DIEGO NATURAL HISTORY MUSEUM PO BOX 121390 SAN DIEGO, CA 92112 ANA 032-030 (PER-02) LADWP (MARCH 2011) SB 115244 POWER ENGINEERS, INC. PALEONTOLOGICAL RESOURCES ASSESSMENT REPORT TABLE OF CONTENTS 1.0 INTRODUCTION ........................................................................................................................... 1 1.1 STUDY PERSONNEL ....................................................................................................................... 2 1.2 PROJECT DESCRIPTION .................................................................................................................. 2 1.2.1 Construction of New 230 kV Double-Circuit Transmission Line ........................................ 4 1.2.2 Addition of New 230 kV Circuit ......................................................................................... 14 1.2.3 Reconductoring of Existing Transmission Line .................................................................. 14 1.2.4 Construction of New Switching Station ............................................................................. -
Copyright by Robert Smith Scott 2004
Copyright by Robert Smith Scott 2004 The Dissertation Committee for Robert Smith Scott certifies that this is the approved version of the following dissertation: The Comparative Paleoecology of Late Miocene Eurasian Hominoids Committee: John Kappelman, Supervisor Claud Bramblett Deborah Overdorff Raymond L. Bernor Liza Shapiro The Comparative Paleoecology of Late Miocene Eurasian Hominoids by Robert Smith Scott, B.A., M.A. Dissertation Presented to the Faculty of the Graduate School of The University of Texas at Austin in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy The University of Texas at Austin August, 2004 Dedication This dissertation is dedicated to my grandmother Alma Dinehart Smith who dedicated her working years to science as a scientific illustrator of considerable skill and who has always been an inspiration to her whole family. Acknowledgements This work was supported by NSF grant BCS-0112659 to J. Kappelman (PI) and R.S. Scott (Co-PI) and a Homer Lindsey Bruce Fellowship from the University of Texas at Austin to R.S. Scott. Thanks to Ray Bernor for the contribution of measurements from his extensive hipparion database funded by NSF grant EAR-0125009. Thanks to Adam Gordon and Dave Raichlen for their many commentaries on and off topic. Additional thanks to my committee John Kappelman, Ray Bernor, Claud Bramblett, Deborah Overdorff, and Liza Shapiro. Much gratitude is due my many hospitable European colleagues who have helped make this work possible. And finally, thanks to my wife Shannon for her patience and support throughout this process. v The Comparative Paleoecology of Late Miocene Eurasian Hominoids Publication No._____________ Robert Smith Scott, Ph.D The University of Texas at Austin, 2004 Supervisor: John Kappelman Abstract: Remains of late Miocene hominoids increasingly indicate both taxonomic and adaptive diversity. -
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. -
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. -
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). -
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. -
Actual Problems of Protection and Sustainable Use of the Animal World Diversity
ACADEMY OF SCIENCES OF MOLDOVA DEPARTMENT OF NATURE AND LIFE SCIENCES INSTITUTE OF ZOOLOGY Actual problems of protection and sustainable use of ThE animal world diversity International Conference of Zoologists dedicated to the 50th anniversary from the foundation of Institute of Zoology of ASM Chisinau – 2011 ACTUAL PRObLEMS OF PROTECTION AND SUSTAINAbLE USE OF ThE ANIMAL wORLD DIVERSITY Content CZU 59/599:502.74 (082) D 53 Dumitru Murariu. READING ABOUT SPECIES CONCEPT IN BIOLOGY.......................................................................10 Dan Munteanu. AChievements Of Romania in ThE field Of nature The materials of International Conference of Zoologists „Actual problems of protection and protection and implementation Of European Union’S rules concerning ThE biodiversity conservation (1990-2010)...............................................................................11 sustainable use of animal world diversity” organized by the Institute of Zoology of the Aca- demy of Sciences of Moldova in celebration of the 50th anniversary of its foundation are a gene- Laszlo Varadi. ThE protection and sustainable use Of Aquatic resources.....................................13 ralization of the latest scientific researches in the country and abroad concerning the diversity of aquatic and terrestrial animal communities, molecular-genetic methods in systematics, phylo- Terrestrial Vertebrates.................................................................................................................................................15 -
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. -
Hipparion Zandaense (Figs
Supporting Information Deng et al. 10.1073/pnas.1201052109 SI Text Overall, the fossiliferous middle Zanda sequence yields char- Geologic Setting of Zanda Basin. Zanda Basin is a late Cenozoic acteristic Pliocene faunas (Table S1), although the upper alluvial basin (Fig. S1A) located just north of the high Himalayan conglomerates and lower fluvial sandstones, from which few ridgecrest in the west-central part of the orogen (∼32° N, 80° E; vertebrate fossils are found thus far, range into the Pleistocene elevation 3,700–4,500 m). The basin fill consists of ∼800 m of and Miocene, respectively. Based on our paleontologic con- fluvial, lacustrine, eolian, and alluvial fan deposits (1). straints, we reinterpreted previously published paleomagnetic Since the initial establishment of the Zanda Formation as a columns from various parts of the basin, and our new age esti- lithological unit (2), additional formation (such as the Tuolin and mates (Fig. S1C) of the Zanda section spans ∼400 ka to 6.1 Ma Xiangze formations) or even group names (Zanda Group) were in GPTS of ATNTS2004 (8). Our alternative interpretation is proposed (3), often based on a perceived depositional hiatus that closest (but not identical) to those proposed by Qian (5) and later proved to be false (1, 4). Here we use a single unit name, takes into account the fast deposition in the upper conglom- fl Zanda Formation, for the entire basin sequence. erates and lower uvial sandstones. The fossils were collected from the eastern bank of the main ZD0918 is approximately at 267 m level of leg 6 in the South wash of Daba Canyon in the Zanda Basin (ZD0918. -
Eomoropus, an American Eocene Chali- Cothere. by Henry Fairfield Osborn
56.9,725E (1181 :7) Article XIV.- EOMOROPUS, AN AMERICAN EOCENE CHALI- COTHERE. BY HENRY FAIRFIELD OSBORN. With Eleven Text Figures. 1. Triplopus amarorum Cope, a new chalicothere type. 2. Resemblances to Moropus. 3. Early European chalicotheres. 4. Description of Eomoropus, type skull and skeleton. 5. Relations to the Perissodactyla. 1. Triplopus amarorum COPE, A NEW CHALICOTHERE TYPE. The recognition of an upper Middle Eocene ancylopod or chalicothere in the type of Triplopus amarorum Cope is a matter of great interest: first, because it shows that a supposedly European family was established as early in America as in Europe and may have been of American origin; second, because geologically the family is carried back from the American Lower Miocene into the close of Middle Eocene times, the Washakie or Bartonian stage; third, the knowledge of considerable portions of the skeleton of this most primitive known chalicothere strengthens the relations of the Chalicotheres to the Perissodactyla. The species T. amarorum has always appeared to the present writer quite distinct from the genus Triplopu, the type species of which is T. cubitalis Cope. Dep4ret was the last author to examine the type of T. amarorum and he pointed out the resemblance of its superior molar teeth, with their interrupted anterior crests, to those of his genus Lophiaspis. But Lophi- aspis is a true lophiodont in the structure of the ectoloph of its superior molar teeth, which exhibits no mesostyle and a concave metacone. The type specimen of T. amarorum, as described by Cope in 1884 in the 'Tertiary Vertebrata', was not thoroughly worked out from the matrix so that his description included chiefly the skull and the pes. -
Eastern Georgia and Western Azerbaijan, South Caucasus)
Synopsis of the terrestrial vertebrate faunas from the Middle Kura Basin (Eastern Georgia and Western Azerbaijan, South Caucasus) MAIA BUKHSIANIDZE and KAKHABER KOIAVA Bukhsianidze, M. and Koiava, K. 2018. Synopsis of the terrestrial vertebrate faunas from the Middle Kura Basin (Eastern Georgia and Western Azerbaijan, South Caucasus). Acta Palaeontologica Polonica 63 (3): 441–461. This paper summarizes knowledge on the Neogene–Quaternary terrestrial fossil record from the Middle Kura Basin accumulated over a century and aims to its integration into the current research. This fossil evidence is essential in understanding the evolution of the Eurasian biome, since this territory is located at the border of Eastern Mediterranean and Central Asian regions. The general biostratigraphic framework suggests existence of two major intervals of the terrestrial fossil record in the area, spanning ca. 10–7 Ma and ca. 3–1 Ma, and points to an important hiatus between the late Miocene and late Pliocene. General aspects of the paleogeographic history and fossil record suggest that the biogeographic role of the Middle Kura Basin has been changing over geological time from a refugium (Khersonian) to a full-fledged part of the Greco-Iranian province (Meotian–Pontian). The dynamic environmental changes during the Quaternary do not depict this territory as a refugium in its general sense. The greatest value of this fossil record is the potential to understand a detailed history of terrestrial life during demise of late Miocene Hominoidea in Eurasia and early Homo dispersal out of Africa. Late Miocene record of the Middle Kura Basin captures the latest stage of the Eastern Paratethys regression, and among other fossils counts the latest and the easternmost occurence of dryopithecine, Udabnopithecus garedziensis, while the almost uninterrupted fossil record of the late Pliocene–Early Pleistocene covers the time interval of the early human occupation of Caucasus and Eurasia.