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11 Sualdea Et Al.Indd
SPANISH J OURNAL OF P ALAEONTOLOGY 20 years at campus: heritage assessment update for Somosaguas fossil geosite (Pozuelo de Alarcón, Madrid) Lucía R. SUALDEA 1* , Adriana OLIVER 2, Fernando BLANCO 3, Iris MENÉNDEZ 1,4 , Manuel HERNÁNDEZ FERNÁNDEZ1,4, Laura DOMINGO 1,5 & Ana Rosa GÓMEZ CANO 6,7 1 Departamento de Geodinámica, Estratigrafía y Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, C/ José Antonio Novais 12, 28040, Madrid; [email protected], [email protected], [email protected], [email protected]. 2 Geosfera, C/ Madres de la Plaza de Mayo, 2, 28523, Rivas-Vaciamadrid, Madrid; [email protected] 3 Museum für Naturkunde, Leibniz-Institut für Evolutions und Biodiversitätsforschung, Invalidenstraße 43, 10115, Berlin, Germany; [email protected] 4 Departamento de Geología Sedimentaria y Cambio Medioambiental, Instituto de Geociencias IGEO (CSIC, UCM), C/ Dr. Severo Ochoa, 7, 28040, Madrid 5 Earth and Planetary Sciences Department. University of California Santa Cruz, 1156 High Street, 95064, Santa Cruz, USA 6 Transmitting Science, C/ Gardenia 2, Piera, 08784, Barcelona. 7 Institut Català de Paleontologia Miquel Crusafont, Edifi ci ICP, Campus de la UAB s/n, 08193, Cerdanyola del Vallès; [email protected] * Corresponding author Sualdea, L.R., Oliver, A., Blanco, F., Menéndez, I., Hernández Fernández, M., Domingo, L. & Gómez Cano, A.R. 2019. 20 years at campus: heritage assessment update for Somosaguas fossil geosite (Pozuelo de Alarcón, Madrid). [20 años en el campus: actualización de la valoración -
The Bioinformaticist's Toolbox in The
THE BIOINFORMATICIST’S TOOLBOX IN THE POST-GENOMIC AGE: APPLICATIONS AND DEVELOPMENTS By DAVID R. SCHREIBER A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2007 1 Copyright 2007 By David R. Schreiber 2 ACKNOWLEDGMENTS Tremendous thanks go to James Deyrup—for the opportunity, the faith, understanding, generosity, goodwill, humanity and love. Thanks also go to Steve Benner—for the freedom, the enthusiasm, the privilege, and for an absurd portion of patience. And thanks go to my family— for being there, wherever “there” chose to be. 3 TABLE OF CONTENTS page ACKNOWLEDGMENTS ...............................................................................................................3 LIST OF TABLES...........................................................................................................................6 LIST OF FIGURES .........................................................................................................................7 LIST OF ABBREVIATIONS..........................................................................................................8 ABSTRACT...................................................................................................................................10 EXOBIOLOGY AND POST-GENOMIC SCIENCE ...................................................................12 Introduction.............................................................................................................................12 -
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. -
(Suidae, Artiodactyla) from the Upper Miocene of Hayranlı-Haliminhanı, Turkey
Turkish Journal of Zoology Turk J Zool (2013) 37: 106-122 http://journals.tubitak.gov.tr/zoology/ © TÜBİTAK Research Article doi:10.3906/zoo-1202-4 Microstonyx (Suidae, Artiodactyla) from the Upper Miocene of Hayranlı-Haliminhanı, Turkey 1 2 3, Jan VAN DER MADE , Erksin GÜLEÇ , Ahmet Cem ERKMAN * 1 Spanish National Research Council, National Museum of Natural Sciences, Madrid, Spain 2 Department of Anthropology, Faculty of Languages, History, and Geography, Ankara University, Ankara, Turkey 3 Department of Anthropology, Faculty of Science and Literature, Ahi Evran University, Kırşehir, Turkey Received: 05.02.2012 Accepted: 11.07.2012 Published Online: 24.12.2012 Printed: 21.01.2013 Abstract: The suid remains from localities 58-HAY-2 and 58-HAY-19 in the Late Miocene Derindere Member of the İncesu Formation in the Hayranlı-Haliminhanı area (Sivas, Turkey) are described and referred to as Microstonyx major (Gervais, 1848–1852). Microstonyx shows changes in incisor morphology, which are interpreted as a further adaptation to rooting. This occurred probably in a short period between 8.7 and 8.121 Ma ago and possibly is a reaction to environmental change. The incisor morphology in locality 58-HAY-2 suggests that it is temporally close to this change, which would imply that this locality and the lithostratigraphically lower 58-HAY-19 belong to the lower part of MN11 and not to MN12. The findings are discussed in the regional context and contribute to the knowledge of the Anatolian fossil mammals. Key words: Suidae, Microstonyx, rooting, ecology, Late Miocene 1. Introduction 1.1. Location and stratigraphy The first of the Hayranlı-Haliminhanı fossil localities was Anatolia lies at the intersection of Asia, Europe, and Afro- discovered in 1993 by members of the Vertebrate Fossils Arabia, and its geology has been subject to the plate tectonic Research Project, a collaborative survey effort. -
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. -
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. -
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. -
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. -
GC University Lahore
GC University Lahore PALAEOENVIRONMENTAL STUDY OF PAKISTAN SIWALIKS Name: MUHAMMAD TARIQ Session: 2007-2010 Roll No: 05-GCU-PHD-Z-07 Supervisor: Prof. Dr. Nusrat Jahan Department: Zoology PALAEOENVIRONMENTAL STUDY OF PAKISTAN SIWALIKS Submitted to GC University Lahore in fulfillment of the requirements for the award of Degree of Doctor of Philosophy in Zoology by Name: MUHAMMAD TARIQ Session: 2007-2010 Roll No: 05-GCU-PHD-Z-07 Department of Zoology GC University Lahore DEDICATION This work is dedicated to MY LOVING PARENTS (Gulzar Ahmad and Sugran Abdullah) through whom I acquired indefatigable temperament, morality, and determination for achieving objectives in every walk of life MY YOUNGER BROTHERS (Muhammad Yasin and Muhammad Noor-ul-Amin) who gave hope and strength to meet with the challenges of life MY YOUNGER SISTERS Zainab Gulzar, Shahida Gulzar and Shakeela Gulzar for their care, affection and cooperation MY DEAREST DAUGHTER (Kashaf Tariq) who proved great blessing for achieving goals of my life ALL GREAT SOULS who pursue their dreams with persistent efforts to make this world a better place to live in DECLARATION I, Mr. Muhammad Tariq Roll No. 05-GCU-PHD-Z-07 student of PhD in the subject of Zoology session: 2007-2010, hereby declare that the matter printed in the thesis titled “Palaeoenvironmental Study of Pakistan Siwaliks” is my own work and has not been printed, published and submitted as research work, thesis or publication in any form in any University, Research Institution etc in Pakistan or abroad. ________________ _____________________ Dated Signatures of Deponent RESEARCH COMPLETION CERTIFICATE Certified that the research work contained in this thesis titled “Palaeoenvironmental Study of Pakistan Siwaliks” has been carried out and completed by Mr. -
Suidae, Mammalia) from the Late Middle Miocene of Gratkorn (Austria, Styria
Palaeobio Palaeoenv (2014) 94:595–617 DOI 10.1007/s12549-014-0152-1 ORIGINAL PAPER Taxonomic study of the pigs (Suidae, Mammalia) from the late Middle Miocene of Gratkorn (Austria, Styria) Jan van der Made & Jérôme Prieto & Manuela Aiglstorfer & Madelaine Böhme & Martin Gross Received: 21 November 2013 /Revised: 26 January 2014 /Accepted: 4 February 2014 /Published online: 23 April 2014 # Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2014 Abstract The locality of Gratkorn of early late Sarmatian age European Tetraconodontinae. The morphometric changes that (Styria, Austria, Middle Miocene) has yielded an abundant occurred in a series of fossil samples covering the known and diverse fauna, including invertebrates, micro-vertebrates temporal ranges of the species Pa. steinheimensis are docu- and large mammals, as well as plants. As part of the taxonom- mented. It is concluded that Parachleuastochoerus includes ical study of the mammals, two species of suids, are described three species, namely Pa. steinheimensis, Pa. huenermanni here and assigned to Listriodon splendens Vo n M ey er, 1 84 6 and Pa. crusafonti. Evolutionary changes are recognised and Parachleuastochoerus steinheimensis (Fraas, 1870). As among the Pa. steinheimensis fossil samples. In addition, it the generic affinities of the latter species were subject to is proposed that the subspecies Pa. steinheimensis olujici was debate, we present a detailed study of the evolution of the present in Croatia long before the genus dispersed further into Europe. This article is an additional contribution to the special issue "The Sarmatian vertebrate locality Gratkorn, Styrian Basin". Keywords Listriodontinae . Tetraconodontinae . Middle J. van der Made (*) Miocene . -
A New Species of Chleuastochoerus (Artiodactyla: Suidae) from the Linxia Basin, Gansu Province, China
Zootaxa 3872 (5): 401–439 ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2014 Magnolia Press ISSN 1175-5334 (online edition) http://dx.doi.org/10.11646/zootaxa.3872.5.1 http://zoobank.org/urn:lsid:zoobank.org:pub:5DBE5727-CD34-4599-810B-C08DB71C8C7B A new species of Chleuastochoerus (Artiodactyla: Suidae) from the Linxia Basin, Gansu Province, China SUKUAN HOU1, 2, 3 & TAO DENG1 1Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044, China 2State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sci- ences Nanjing 210008, China 3Corresponding author. E-mail: [email protected] Abstract The Linxia Basin, Gansu Province, China, is known for its abundant and well-preserved fossils. Here a new species, Chleuastochoerus linxiaensis sp. nov., is described based on specimens collected from the upper Miocene deposits of the Linxia Basin, distinguishable from C. stehlini by the relatively long facial region, more anteromedial-posterolaterally compressed upper canine and more complicated cheek teeth. A cladistics analysis placed Chleuastochoerus in the sub- family Hyotheriinae, being one of the basal taxa of this subfamily. Chleuastochoerus linxiaensis and C. stehlini are con- sidered to have diverged before MN 10. C. tuvensis from Russia represents a separate lineage of Chleuastochoerus, which may have a closer relationship to C. stehlini but bears more progressive P4/p4 and M3. Key words: Linxia Basin, upper Miocene Liushu Formation, Hyotheriinae, Chleuastochoerus, phylogeny Introduction Chleuastochoerus Pearson 1928 is a small late Miocene-early Pliocene fossil pig (Suidae). -
Early Hominid Evolution and Ecological Change Through the African
Kaye E. Reed Early hominid evolution and ecological Institute of Human Origins, 1288 9th change through the African Street, Berkeley, California 94710, U.S.A. & Bernard Price Institute for Plio-Pleistocene Palaeontological Research, University of the Witwatersrand, Johannesburg, The habitats in which extinct hominids existed has been a key issue in 2050, South Africa addressing the origin and extinction of early hominids, as well as in under- standing various morphological and behavioral adaptations. Many researchers Received 15 January 1996 postulated that early hominids lived in an open savanna (Dart, 1925; Revision received 1 August Robinson, 1963; Howell, 1978). However, Vrba (1985, 1988) has noted that a 1996 and accepted 9 October major global climatic and environmental shift from mesic, closed to xeric, open 1996 habitats occurred in the late African Pliocene (approximately 2·5 m.y.a.), thus implying that the earliest hominids existed in these mesic, wooded environs. Keywords: Australopithecus, This climatic shift is also suggested to have contributed to a pulse in speciation Paranthropus, ecological diversity, events with turnovers of many bovid and possibly hominid species. Previous paleoecology. environmental reconstructions of hominid localities have concentrated on taxonomic identities and taxonomic uniformitarianism to provide habitat reconstructions (e.g., Vrba, 1975; Shipman & Harris, 1988). In addition, relative abundances of species are often used to reconstruct a particular environment, when in fact taphonomic factors could be affecting the propor- tions of taxa. This study uses the morphological adaptations of mammalian assemblages found with early hominids to reconstruct the habitat based on each species’ ecological adaptations, thus minimizing problems introduced by taxonomy and taphonomy.