Terry Harrison 1997.Pdf

Total Page:16

File Type:pdf, Size:1020Kb

Terry Harrison 1997.Pdf Neogene Paleontology of the Manonga Valley, Tanzania A Window into the Evolutionary History of East Africa TOPICS IN GEOBIOLOGY Series Editors: Neil H. Landman, American Museum of Natural History, New York, New York Douglas S. Jones, University of Florida, Gainesville, Florida Current volumes in this series: Volume 2 ANIMAL-SEDIMENT RELATIONS The Biogenic Alteration of Sediments Edited by Peter L. McCall and Michael J. S. Tevesz Volume 3 BIOTIC INTERACTIONS IN RECENT AND FOSSIL BENTHIC COMMUNITIES Edited by Michael J. S. Tevesz and Peter L. McCall Volume 4 THE GREAT AMERICAN BIOTIC INTERCHANGE Edited by Francis G. Stehli and S. David Webb Volume 5 MAGNETITE BIOMINERALIZATION AND MAGNETORECEPTION IN ORGANISMS A New Biomagnetism Edited by Joseph L. Kirschvink, Douglas S. Jones and Bruce J. MacFadden Volume 6 NAUTILUS The Biology and Paleobiology of a Living Fossil Edited by W. Bruce Saunders and Neil H. Landman Volume 7 HETEROCHRONY IN EVOLUTION A Multidisciplinary Approach Edited by Michael L. McKinney Volume 8 GALApAGOS MARINE INVERTEBRATES Taxonomy, Biogeography, and Evolution in Darwin's Islands Edited by Matthew J. James Volume 9 TAPHONOMY Releasing the Data Locked in the Fossil Record Edited by Peter A. Allison and Derek E. G. Briggs Volume 10 ORIGIN AND EARLY EVOLUTION OF THE METAZOA Edited by Jere H. Lipps and Philip W. Signor Volume 11 ORGANIC GEOCHEMISTRY Principles and Applications Edited by Michael H. Engel and Stephen A. Macko Volume 12 THE TERTIARY RECORD OF RODENTS IN NORTH AMERICA William Korth Volume 13 AMMONOID PALEOBIOLOGY Edited by Neil H. Landman, Kazushige Tanabe, and Richard Arnold Davis Volume 14 NEOGENE PALEONTOLOGY OF THE MANONGA VALLEY, TANZANIA A Window into the Evolutionary History of East Africa Edited by Terry Harrison A Continuation Order Plan is available for this series. A continuation order will bring delivery of each new volume immediately upon publication. Volumes are billed only upon actual shipment. For further information please contact the publisher. Neogene Paleontology of the Manonga Valley, Tanzania A Window into the Evolutionary History of East Africa Edited by Terry Harrison New York University New York, New York Springer Science+Business Media, LLC Library of Congress Cataloging-in-Publication Data Neogene paleontology of the Manonga Valley. Tanzania a window into the evolutionary history of East Africa I edited by Terry Harrison. p. cm. -- (Topics in geobiology ; v. 14) Includes bibliographical references and index. 1. Paleontology--Neogene. 2. Animals. Fossil--Tanzania--Manonga Valley. 3. Geology. Stratigraphic--Neogene. 4. Geology--Tanzania- -Manonga Valley. I. Harrison. Terry. II. Series. QE738.5.N46 1997 560' . 1786'0967827--dc21 97-14542 CIP ISBN 978-1-4419-3265-5 ISBN 978-1-4757-2683-1 (eBook) DOI 10.1007/978-1-4757-2683-1 © 1997 Springer Science+Business Media New York Originally published by Plenum Press, New York in 1997. Softcover reprint ofthe hardcover 1st edition 1997 http://www.plenum.com All rights reserved 10 9 8 7 6 5 4 3 2 1 No part of this book may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, microfilming, recording, or otherwise, without written permission from the Publisher To the people of Tanzania who welcomed me into their country and shared their knowledge and wisdom Contributors Miranda Armour-Chelu Department of Anatomy, College of Medicine, Howard University, Washington, D.C. 20059 Eric Baker Department of Anthropology, Paleoanthropology Laboratory, New York University, New York, New York 10003 Raymond L. Bernor College of Medicine, Department of Anatomy, Howard University, Washington, D.C. 20059 Laura C. Bishop Department of Human Anatomy and Cell Biology, University of Liverpool, Liverpool L69 3GE, United Kingdom Achilles Gautier Universiteit Gent, Vakgroep Geologie en Bodemkunde, Labo­ ratorium voor Paleontologie, B-9000 Gent, Belgium Alan W. Gentry c/o Department of Palaeontology, Natural History Museum, London SW7 5BD, United Kingdom Terry Harrison Department of Anthropology, Paleoanthropology Laboratory, New York University, New York, New York 10003 Michael 1. Mbago Director General, National Museums of Tanzania, Dar es Salaam, Tanzania Medard Mutakyahwa Department of Geology, University of Dar es Salaam, Dar es Salaam, Tanzania William J. Sanders Museum of Paleontology, University of Michigan, Ann Arbor, Michigan 48109 Kathlyn M. Stewart Paleobiology Section, Canadian Museum of Nature, Ottawa, Ontario K1P 6P4, Canada Dirk Van Damme Universiteit Gent, Vakgroep Geologie en Bodemkunde, Labo­ ratorium voor Paleontologie, B-9000, Gent, Belgium Jacques Verniers Universiteit Gent, Vakgroep Geologie en Bodemkunde, Labo­ ratorium voor Paleontologie, B-9000, Gent, Belgium Alisa J. Winkler Shuler Museum of Paleontology, Southern Methodist Univer­ sity, Dallas, Texas 75275 vii Preface In spite of the dedication and resourcefulness shown by paleontologists and paleoanthropologists over the past seventy years in their quest to find new fossil hominids, it is clear that, in the enterprise of reconstructing the evolutionary history of humans (and other mammals), we still have much to accomplish. It is true that we have made significant advances, with the help of some remarkable fossil discoveries, in documenting the main phylogenetic strands, but we know very little about the detailed anatomy or paleobiology of these lineages, or about the critical events that led to their divergence and subsequent evolutionary changes. Our image of the early evolutionary history of our own species is based on a montage of snapshots obtained from fleeting glimpses of the phylogenetic tree as seen through a few narrow temporal and spatial windows provided us by the fossil record. If our objective is not simply to fill in the missing gaps, and thereby document the configuration of the major branches of the human evolu­ tionary tree, but rather to gain some real insight into early hominid diversity in space and time, and to explain this diversity in terms of the complexity of ecological, geographic, and evolutionary factors that produced it, then we need a broader perspective. We should strive to improve the quality (not just the quantity) of the hominid fossil record, so that it includes a wider geographic coverage and a finer temporal resolution. In order to achieve this objective, the search for new paleontological sites in Africa, and elsewhere, must be considered as a high priority. Paleontology is inherently a risky business, with no guarantee of returns on one's investment, but given the right balance of effort, perseverance, funding, and good fortune, significant advances in our knowledge of human evolution can be made. Exciting new finds of Plio-Pleistocene hominids from Ethiopia, Eritrea, Kenya, Malawi, and Chad provide tangible evidence of such successes. The people of Tanzania are justifiably proud of the fact that some of the most important fossil and archaeological finds pertaining to the earliest stages of human evolution have been discovered in their country. Olduvai Gorge and Laetoli are famous throughout the world, and fossil discoveries at these sites have made a significant contribution toward helping to piece together the evolutionary history of humankind over the past four million years. Today, Tanzania is celebrated internationally as a leading center for paleoanthropologi­ cal studies. Even so, only three sites in Tanzania have yielded the remains of early fossil hominids, Olduvai Gorge, Laetoli, and Peninj, all located in the Serengeti Plains in the northeastern part of the country. This limited distribution is primarily a consequence of geological factors. The sites cluster at the southern ix x Preface extremity of the Gregory Rift. where the eastern branch of the East African Rift valley splays out around the margin of the resistant Tanganyika shield. The rift valley. and its associated volcanism. provides an ideal geological setting for the preservation and recovery of fossils. Indeed. almost all of the spectacular early hominid fossil finds in East Africa are from sites located within the Eastern Rift. However. another significant factor is that the sites in northern Tanzania are easily accessible. especially from Kenya. The full paleontological potential of Olduvai Gorge was not realized until the 1950s. when Louis and Mary Leakey were able to intensify their explorations from their base in Nairobi. Today it is relatively easy for expeditions and tourist buses to reach Olduvai Gorge. but when Louis Leakey began his pioneering work there in the early 1930s. it was a major logistical problem. Louis Leakey's initial paleontological experiences in the southern part of Tanzania give some indication of the past difficulties and dangers involved in mounting major expeditions to the more remote regions of the country. In 1924. Louis Leakey took part in an ill-fated expedition to the Jurassic site of Tendaguru. where W. E. Cutler. the leader of the expedition. succumbed to blackwater fever. Our knowledge of the paleontology and archae­ ology of most of Tanzania is quite limited. especially when compared with that of neighboring Kenya. which has been much more extensively explored. Geolo­ gists interested in locating economically important minerals and deposits have surveyed much ofTanzania. and in the process they have reported finding further sites with fossils. but very few paleontologists or archaeologists have ever visited these sites. As a consequence, a large number
Recommended publications
  • Browsing and Non-Browsing Extant and Extinct Giraffids Evidence From
    Browsing and non-browsing extant and extinct giraffids Evidence from dental microwear textural analysis Gildas Merceron, Marc Colyn, Denis Geraads To cite this version: Gildas Merceron, Marc Colyn, Denis Geraads. Browsing and non-browsing extant and extinct giraffids Evidence from dental microwear textural analysis. Palaeogeography, Palaeoclimatology, Palaeoecol- ogy, Elsevier, 2018, 505, pp.128-139. 10.1016/j.palaeo.2018.05.036. hal-01834854v2 HAL Id: hal-01834854 https://hal-univ-rennes1.archives-ouvertes.fr/hal-01834854v2 Submitted on 6 Sep 2018 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. 1 Browsing and non-browsing extant and extinct giraffids: evidence from dental microwear 2 textural analysis. 3 4 Gildas MERCERON1, Marc COLYN2, Denis GERAADS3 5 6 1 Palevoprim (UMR 7262, CNRS & Université de Poitiers, France) 7 2 ECOBIO (UMR 6553, CNRS & Université de Rennes 1, Station Biologique de Paimpont, 8 France) 9 3 CR2P (UMR 7207, Sorbonne Universités, MNHN, CNRS, UPMC, France) 10 11 1Corresponding author: [email protected] 12 13 Abstract: 14 15 Today, the family Giraffidae is restricted to two genera endemic to the African 16 continent, Okapia and Giraffa, but, with over ten genera and dozens of species, it was far 17 more diverse in the Old World during the late Miocene.
    [Show full text]
  • Astragalar Morphology of Selected Giraffidae
    RESEARCH ARTICLE Astragalar Morphology of Selected Giraffidae Nikos Solounias1,2☯*, Melinda Danowitz1☯ 1 Department of Anatomy, New York Institute of Technology College of Osteopathic Medicine, Old Westbury, NY, United States of America, 2 Department of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, NY, United States of America ☯ These authors contributed equally to this work. * [email protected] Abstract The artiodactyl astragalus has been modified to exhibit two trochleae, creating a double pullied structure allowing for significant dorso-plantar motion, and limited mediolateral motion. The astragalus structure is partly influenced by environmental substrates, and cor- respondingly, morphometric studies can yield paleohabitat information. The present study establishes terminology and describes detailed morphological features on giraffid astragali. Each giraffid astragalus exhibits a unique combination of anatomical characteristics. The giraffid astragalar morphologies reinforce previously established phylogenetic relationships. We find that the enlargement of the navicular head is a feature shared by all giraffids, and that the primitive giraffids possess exceptionally tall astragalar heads in relation to the total astragalar height. The sivatheres and the okapi share a reduced notch on the lateral edge OPEN ACCESS of the astragalus. We find that Samotherium is more primitive in astragalar morphologies Citation: Solounias N, Danowitz M (2016) Astragalar than Palaeotragus, which is reinforced
    [Show full text]
  • Geology of the Nairobi Region, Kenya
    % % % % % % % % %% %% %% %% %% %% %% % GEOLOGIC HISTORY % %% %% % % Legend %% %% %% %% %% %% %% % % % % % % HOLOCENE: %% % Pl-mv Pka %%% Sediments Mt Margaret U. Kerichwa Tuffs % % % % %% %% % Longonot (0.2 - 400 ka): trachyte stratovolcano and associated deposits. Materials exposed in this map % %% %% %% %% %% %% % section are comprised of the Longonot Ash Member (3.3 ka) and Lower Trachyte (5.6-3.3 ka). The % Pka' % % % % % % L. Kerichwa Tuff % % % % % % Alluvial fan Pleistocene: Calabrian % % % % % % % Geo% lo% gy of the Nairobi Region, Kenya % trachyte lavas were related to cone building, and the airfall tuffs were produced by summit crater formation % % % % % % % % % % % % % % % % % Pna % % % % %% % (Clarke et al. 1990). % % % % % % Pl-tb % % Narok Agglomerate % % % % % Kedong Lake Sediments Tepesi Basalt % % % % % % % % % % % % % % % % %% % % % 37.0 °E % % % % 36.5 °E % % % % For area to North see: Geology of the Kijabe Area, KGS Report 67 %% % % % Pnt %% % PLEISTOCENE: % % %% % % % Pl-kl %% % % Nairobi Trachyte % %% % -1.0 ° % % % % -1.0 ° Lacustrine Sediments % % % % % % % % Pleistocene: Gelasian % % % % % Kedong Valley Tuff (20-40 ka): trachytic ignimbrites and associated fall deposits created by caldera % 0 % 1800 % % ? % % % 0 0 % % % 0 % % % % % 0 % 0 8 % % % % % 4 % 4 Pkt % formation at Longonot. There are at least 5 ignimbrite units, each with a red-brown weathered top. In 1 % % % % 2 % 2 % % Kiambu Trachyte % Pl-lv % % % % % % % % % % %% % % Limuru Pantellerite % % % % some regions the pyroclastic glass and pumice has been
    [Show full text]
  • PALEONTOLOGICAL (PLANKTIC FORAMINIFER-OSTRACOD) INVESTIGATION of EOCENE SEQUENCE of KARAMAN REGION Ümit ŞAFAK* ABSTRACT
    PALEONTOLOGICAL (PLANKTIC FORAMINIFER-OSTRACOD) INVESTIGATION OF EOCENE SEQUENCE OF KARAMAN REGION Ümit ŞAFAK* ABSTRACT.- The microfauna of Eocene sequence outcropping around Karaman have been investigated. These planktic foraminifers and ostracods were systematically described; also Acarinina bullbrooki planktic foraminifer zone belonging to Lutetian has been determined and this zone was compared with other Eocene planktic foraminifer zones over the world indicat- ing same level. In addition, ostracod species described were stratigraphically and paleogeographically compared with those of other basins. OSTRACOD AND FORAMINIFER ASSEMBLAGES OF TERTIARY SEDIMENTS AT W. BAKIRKÖY (ISTANBUL) Ümit ŞAFAK*. Niyazi AVŞAR* and Engin MERİÇ** ABSTRACT.- The drilling samples taken from the western part of the Bakırköy Basin were investigated, and the microplaeonto- logical data were evaluated. Pliocene, Late Miocene and Late Eocene aged sediments have been observed from top to bottom of drilling, at the results of the laboratory investigation. 14 genera and 25 species from the ostracods and 10 genera and 8 species of benthic foraminifera from the Pliocene sediments: 6 genera and 11 species of ostracods, 9 genera 9 species of ben- thic foraminifera from the Late Miocene deposits and 11 genera and 11 sepices of ostracods and 20 genera and 6 species of benthic foraminifera from the Late Eocene sediments were described. The microfauna of Pliocene sediments consists of Cyprideis seminulum (Reuss), C. pannonica (Mehes), C.anatolica Bassiouni, C. torosa (Jones). C. tuberculata(Mehes). C. tritu- berculata Kristic. C. pontica Kristic are rare, and characteristic for Pontic Basin. In addition, Loxoconcha sp., Semicytherura sp.. Xestoleberis margaritae Mauller, X. ventricosa Mueller. X, reymenti Ruggieri, X. communis Mueller.
    [Show full text]
  • Original Giraffokeryx Punjabiensis (Artiodactyla, Ruminantia, Giraffidae) from Lower Siwaliks (Chinji Formation) of Dhok Bun
    Original Giraffokeryx punjabiensis (Artiodactyla, Ruminantia, Giraffidae) from Lower Siwaliks (Chinji Formation) of Dhok Bun Ameer Khatoon, Pakistan Khizar Samiullah1*, Muhammad Akhtar2, Abdul Ghaffar3, Muhammad Akbar Khan4 Received : 28 January 2011 ; Accepted : 13 September 2011 Abstract Fossil remains of Giraffokeryx punjabiensis (premolar and molar teeth belonging to the upper and lower jaws) have been collected and discussed from Chinji Formation of Dhok Bun Ameer Khatoon (32o 47’ 26.4” N, 72° 55’ 35.7” E). All these (twenty one) specimens are isolated teeth, which provide new data and give valuable information on the biostratigrphy and paleoecology of Giraffokeryx punjabiensis as well as the stratigraphy and paleoclimates of these Miocene rocks of the Chakwal district, Pakistan. Keywords: Giraffokeryx punjabiensis, isolated teeth, Chinji Formation, biostratigraphy Miocene rocks, Chakwal district. Introduction Dhok Bun Ameer Khatoon (DBAK) is poorly known fossil ramii and a number of isolated teeth. Mathew4 studied site of the Siwaliks. Previous pioneer workers 1,2,3,4,5 did the material of this species at the Indian Museum, not visit this site nor mentioned it in their faunal list. Kolkata (Calcutta), and recognized a larger and a During the last decade, this site had got attraction of smaller form. However, Colbert5 suggested there was researchers when few fossils were unearthed during a continuous size gradation of the dental material of the mechanical work for construction of dam for water the species through the Chinji to the Nagri Formation storage purposes. Girafids, bovids, tragulids, suids, and therefore that no such size division exists in the hominids, rhinos, chilothers anthracothers and carnivors material of the genus Giraffokeryx.
    [Show full text]
  • Chapter 1 - Introduction
    EURASIAN MIDDLE AND LATE MIOCENE HOMINOID PALEOBIOGEOGRAPHY AND THE GEOGRAPHIC ORIGINS OF THE HOMININAE by Mariam C. Nargolwalla A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Graduate Department of Anthropology University of Toronto © Copyright by M. Nargolwalla (2009) Eurasian Middle and Late Miocene Hominoid Paleobiogeography and the Geographic Origins of the Homininae Mariam C. Nargolwalla Doctor of Philosophy Department of Anthropology University of Toronto 2009 Abstract The origin and diversification of great apes and humans is among the most researched and debated series of events in the evolutionary history of the Primates. A fundamental part of understanding these events involves reconstructing paleoenvironmental and paleogeographic patterns in the Eurasian Miocene; a time period and geographic expanse rich in evidence of lineage origins and dispersals of numerous mammalian lineages, including apes. Traditionally, the geographic origin of the African ape and human lineage is considered to have occurred in Africa, however, an alternative hypothesis favouring a Eurasian origin has been proposed. This hypothesis suggests that that after an initial dispersal from Africa to Eurasia at ~17Ma and subsequent radiation from Spain to China, fossil apes disperse back to Africa at least once and found the African ape and human lineage in the late Miocene. The purpose of this study is to test the Eurasian origin hypothesis through the analysis of spatial and temporal patterns of distribution, in situ evolution, interprovincial and intercontinental dispersals of Eurasian terrestrial mammals in response to environmental factors. Using the NOW and Paleobiology databases, together with data collected through survey and excavation of middle and late Miocene vertebrate localities in Hungary and Romania, taphonomic bias and sampling completeness of Eurasian faunas are assessed.
    [Show full text]
  • 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.
    [Show full text]
  • New Hominoid Mandible from the Early Late Miocene Irrawaddy Formation in Tebingan Area, Central Myanmar Masanaru Takai1*, Khin Nyo2, Reiko T
    Anthropological Science Advance Publication New hominoid mandible from the early Late Miocene Irrawaddy Formation in Tebingan area, central Myanmar Masanaru Takai1*, Khin Nyo2, Reiko T. Kono3, Thaung Htike4, Nao Kusuhashi5, Zin Maung Maung Thein6 1Primate Research Institute, Kyoto University, 41 Kanrin, Inuyama, Aichi 484-8506, Japan 2Zaykabar Museum, No. 1, Mingaradon Garden City, Highway No. 3, Mingaradon Township, Yangon, Myanmar 3Keio University, 4-1-1 Hiyoshi, Kouhoku-Ku, Yokohama, Kanagawa 223-8521, Japan 4University of Yangon, Hlaing Campus, Block (12), Hlaing Township, Yangon, Myanmar 5Ehime University, 2-5 Bunkyo-cho, Matsuyama, Ehime 790-8577, Japan 6University of Mandalay, Mandalay, Myanmar Received 14 August 2020; accepted 13 December 2020 Abstract A new medium-sized hominoid mandibular fossil was discovered at an early Late Miocene site, Tebingan area, south of Magway city, central Myanmar. The specimen is a left adult mandibular corpus preserving strongly worn M2 and M3, fragmentary roots of P4 and M1, alveoli of canine and P3, and the lower half of the mandibular symphysis. In Southeast Asia, two Late Miocene medium-sized hominoids have been discovered so far: Lufengpithecus from the Yunnan Province, southern China, and Khoratpithecus from northern Thailand and central Myanmar. In particular, the mandibular specimen of Khoratpithecus was discovered from the neighboring village of Tebingan. However, the new mandible shows apparent differences from both genera in the shape of the outline of the mandibular symphyseal section. The new Tebingan mandible has a well-developed superior transverse torus, a deep intertoral sulcus (= genioglossal fossa), and a thin, shelf-like inferior transverse torus. In contrast, Lufengpithecus and Khoratpithecus each have very shallow intertoral sulcus and a thick, rounded inferior transverse torus.
    [Show full text]
  • AMERICAN MUSEUM NOVITATES Published by Tnui Amermican MUSZUM W Number 632 Near York Cityratt1ral Historay June 9, 1933
    AMERICAN MUSEUM NOVITATES Published by Tnui AmERMICAN MUSZUM W Number 632 Near York CityRATt1RAL HisToRay June 9, 1933 56.9, 735 G: 14.71, 4 A SKULL AND MANDIBLE OF GIRAFFOKERYX PUNJABIENSIS PILGRIM By EDWIN H. COLBERT The genus Giraffokeryx was founded by Dr. G. E. Pilgrim to desig- nate a primitive Miocene giraffe from the lower Siwalik beds of northern India. Doctor Pilgrim, in a series of papers,' described Giraffokeryx on the basis of fragmental and scattered dentitions.. Naturally, Pilgrim's knowledge of the genus was rather incomplete, and he was unable tQ formulate any opinions as to the structure.of the skull or mandible. An almost complete skull, found in the northern Punjab in 1922 by Mr. Barnum Brown of the American Museum, proves to be that of Giraffokeryx, and it exhibits such striking and unusual characters that a separate description of it has seemed necessary. This skull, together with numerous teeth and a lower. jaw, gives us. a very good comprehen- sion of the genus which forms the subject.of this paper. The drawings of the skull were made by John. C. Germann, and the remaining ones were done by Margaret Matthew. MATERIAL DESCRIBED Only the material referred to in this description will here be listed. There' are a great many specimens of Gir'affokeryx in the American'Mu- seum collection, but since 'most of them are'teeth, they will not be considered at this time. A subsequent paper, dealing with the American Museum Siwalik collection in detail, wtyill contain a complete list of the Giraffokeryx material.
    [Show full text]
  • ABSTRACTS BOOK Proof 03
    1st – 15th December ! 1st International Meeting of Early-stage Researchers in Paleontology / XIV Encuentro de Jóvenes Investigadores en Paleontología st (1December IMERP 1-stXIV-15th EJIP), 2018 BOOK OF ABSTRACTS Palaeontology in the virtual era 4 1st – 15th December ! Ist Palaeontological Virtual Congress. Book of abstracts. Palaeontology in a virtual era. From an original idea of Vicente D. Crespo. Published by Vicente D. Crespo, Esther Manzanares, Rafael Marquina-Blasco, Maite Suñer, José Luis Herráiz, Arturo Gamonal, Fernando Antonio M. Arnal, Humberto G. Ferrón, Francesc Gascó and Carlos Martínez-Pérez. Layout: Maite Suñer. Conference logo: Hugo Salais. ISBN: 978-84-09-07386-3 5 1st – 15th December ! Palaeontology in the virtual era BOOK OF ABSTRACTS 6 4 PRESENTATION The 1st Palaeontological Virtual Congress (1st PVC) is just the natural consequence of the evolution of our surrounding world, with the emergence of new technologies that allow a wide range of communication possibilities. Within this context, the 1st PVC represents the frst attempt in palaeontology to take advantage of these new possibilites being the frst international palaeontology congress developed in a virtual environment. This online congress is pioneer in palaeontology, offering an exclusively virtual-developed environment to researchers all around the globe. The simplicity of this new format, giving international projection to the palaeontological research carried out by groups with limited economic resources (expensive registration fees, travel, accomodation and maintenance expenses), is one of our main achievements. This new format combines the benefts of traditional meetings (i.e., providing a forum for discussion, including guest lectures, feld trips or the production of an abstract book) with the advantages of the online platforms, which allow to reach a high number of researchers along the world, promoting the participation of palaeontologists from developing countries.
    [Show full text]
  • Early and Middle Pleistocene Faunal and Hominins Dispersals Through Southwestern Asia
    Early and Middle Pleistocene Faunal and Hominins Dispersals through Southwestern Asia The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Bar-Yosef, Ofer and Miriam Belmaker. Forthcoming. Early and Middle Pleistocene faunal and hominins dispersals through Southwestern Asia. Quaternary Science Reviews 29. Published Version doi:10.1016/j.quascirev.2010.02.016 Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:4270472 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Open Access Policy Articles, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#OAP 1 Early and Middle Pleistocene Faunal and Hominins Dispersals through 2 Southwestern Asia 3 4 5 Ofer Bar-Yosef and Miriam Belmaker 6 Department of Anthropology 7 Harvard University 8 11 Divinity Avenue 9 Cambridge MA 02138 10 Phone ++ 1 617 495 1279 11 Fax ++ 1 617 496 8041 12 1 12 Abstract 13 This review summarizes the paleoecology of the Early and Middle Pleistocene of 14 southwestern Asia, based on both flora and fauna, retrieved from a series of ‘windows’ 15 provided by the excavated sites. The incomplete chrono-stratigraphy of this vast region 16 does not allow to accept the direct chronological correlation between the available sites 17 and events of faunal and hominin dispersals from Africa. It also demonstrates that 18 hominins survived in a mixed landscape of open parkland with forested surrounding hills. 19 In addition, the prevailing environmental conditions are not sufficient to explain the 20 differences between ‘core and flake’ and the Acheulian industries that probably reflect 21 the learned traditions of different groups of hominins successful adaptations to new 22 ecological niches away from the African savanna.
    [Show full text]
  • Aswa5-01-Belmaker-20
    ARCHAEOZOOLOGY OF THE NEAR EAST V Proceedings of the fifth international symposium on the archaeozoology of southwestern Asia and adjacent areas edited by H. Buitenhuis, A.M. Choyke, M. Mashkour and A.H. Al-Shiyab ARC-Publicaties 62 Groningen, The Netherlands, 2002 Cover illustrations: Logo of the Yarmouk University, Jordan This publication is sponsored by: ARCbv and Vledderhuizen Beheer bv Copyright: ARC-bv Printing: RCG-Groningen Parts of this publications can be used by third parties if source is clearly stated Information and sales: ARCbv, Kraneweg 13, Postbus 41018, 9701 CA, Groningen, The Netherlands Tel: +31 (0)50 3687100, fax: +31 (0)50 3687199, email: [email protected], internet: www.arcbv.nl ISBN 90 – 77170 – 01– 4 NUGI 680 -430 Preface When I participated in the IV th International Conference of ASWA, held in the summer of 1998 in Paris, I was gratified to learn that the Scientific committee had unanimously agreed to hold the next meeting in Jordan. Thus, on 2 April 2000, the V th International Conference of the Archaeozoology of Southwest Asia and Adjacent Areas was held for the first time within the region at Yarmouk University in Irbid, Jordan after being held on the past four occasions in Europe. The themes of this conference were divided into five areas including: • Paleo-environment and biogeography • Domestication and animal management • Ancient subsistence economies • Man/animal interactions in the past • Ongoing research projects in the field and related areas I wish to thank all those who helped make this conference such a success. In particular, I would like to express my appreciation to the Director of the Institute of Archaeology and anthropology at Yarmouk University Special thanks are due to his excellency, the President of Yarmouk University, Professor Khasawneh, who gave his full support and encouragement to the convening of this conference at Yarmouk University and to all those who contributed the working papers which made the conference possible.
    [Show full text]