Copyrighted Material
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Geckos from the Middle Miocene of Devı´Nska Nova´ Ves (Slovakia): New Material and a Review of the Previous Record
Swiss Journal of Geosciences (2018) 111:183–190 https://doi.org/10.1007/s00015-017-0292-1 (0123456789().,-volV)(0123456789().,-volV) Geckos from the middle Miocene of Devı´nska Nova´ Ves (Slovakia): new material and a review of the previous record 1 2 3 Andrej Cˇ ernˇ ansky´ • Juan D. Daza • Aaron M. Bauer Received: 16 May 2017 / Accepted: 17 July 2017 / Published online: 16 January 2018 Ó Swiss Geological Society 2017 Abstract New species of a gecko of the genus Euleptes is described here—E. klembarai. The material comes from the middle Miocene (Astaracian, MN 6) of Slovakia, more precisely from the well-known locality called Zapfe‘s fissure fillings (Devı´nska Nova´ Ves, Bratislava). The fossil material consists of isolated left maxilla, right dentary, right pterygoid and cervical and dorsal vertebrae. The currently known fossil record suggests that isolation of environment of the Zapfe‘s fissure site, created a refugium for the genus Euleptes in Central Europe (today, this taxon still inhabits southern part of Europe and North Africa—E. europea), probably resulting from the island geography of this area during the middle Miocene. The isolation of this territory might have facilitated allopatric speciation. Keywords Gekkota Á Euleptes Á Neogene Á Zapfe’s fissure 1 Introduction superb preservation of skeletal and soft tissue (Bo¨hme 1984; Daza and Bauer 2012; Daza et al. 2013b, 2016). Gekkota (geckos and pygopods) is a speciose clade of Very important and superbly preserved find in Baltic amber lepidosaurs, comprising more than 1600 extant species is represented by Yantarogecko balticus from the Early (Bauer 2013; Uetz and Freed 2017). -
The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
The Taxonomy of Primates in the Laboratory Context
P0800261_01 7/14/05 8:00 AM Page 3 C HAPTER 1 The Taxonomy of Primates T HE T in the Laboratory Context AXONOMY OF P Colin Groves RIMATES School of Archaeology and Anthropology, Australian National University, Canberra, ACT 0200, Australia 3 What are species? D Taxonomy: EFINITION OF THE The biological Organizing nature species concept Taxonomy means classifying organisms. It is nowadays commonly used as a synonym for systematics, though Disagreement as to what precisely constitutes a species P strictly speaking systematics is a much broader sphere is to be expected, given that the concept serves so many RIMATE of interest – interrelationships, and biodiversity. At the functions (Vane-Wright, 1992). We may be interested basis of taxonomy lies that much-debated concept, the in classification as such, or in the evolutionary implica- species. tions of species; in the theory of species, or in simply M ODEL Because there is so much misunderstanding about how to recognize them; or in their reproductive, phys- what a species is, it is necessary to give some space to iological, or husbandry status. discussion of the concept. The importance of what we Most non-specialists probably have some vague mean by the word “species” goes way beyond taxonomy idea that species are defined by not interbreeding with as such: it affects such diverse fields as genetics, biogeog- each other; usually, that hybrids between different species raphy, population biology, ecology, ethology, and bio- are sterile, or that they are incapable of hybridizing at diversity; in an era in which threats to the natural all. Such an impression ultimately derives from the def- world and its biodiversity are accelerating, it affects inition by Mayr (1940), whereby species are “groups of conservation strategies (Rojas, 1992). -
Human Evolution: a Paleoanthropological Perspective - F.H
PHYSICAL (BIOLOGICAL) ANTHROPOLOGY - Human Evolution: A Paleoanthropological Perspective - F.H. Smith HUMAN EVOLUTION: A PALEOANTHROPOLOGICAL PERSPECTIVE F.H. Smith Department of Anthropology, Loyola University Chicago, USA Keywords: Human evolution, Miocene apes, Sahelanthropus, australopithecines, Australopithecus afarensis, cladogenesis, robust australopithecines, early Homo, Homo erectus, Homo heidelbergensis, Australopithecus africanus/Australopithecus garhi, mitochondrial DNA, homology, Neandertals, modern human origins, African Transitional Group. Contents 1. Introduction 2. Reconstructing Biological History: The Relationship of Humans and Apes 3. The Human Fossil Record: Basal Hominins 4. The Earliest Definite Hominins: The Australopithecines 5. Early Australopithecines as Primitive Humans 6. The Australopithecine Radiation 7. Origin and Evolution of the Genus Homo 8. Explaining Early Hominin Evolution: Controversy and the Documentation- Explanation Controversy 9. Early Homo erectus in East Africa and the Initial Radiation of Homo 10. After Homo erectus: The Middle Range of the Evolution of the Genus Homo 11. Neandertals and Late Archaics from Africa and Asia: The Hominin World before Modernity 12. The Origin of Modern Humans 13. Closing Perspective Glossary Bibliography Biographical Sketch Summary UNESCO – EOLSS The basic course of human biological history is well represented by the existing fossil record, although there is considerable debate on the details of that history. This review details both what is firmly understood (first echelon issues) and what is contentious concerning humanSAMPLE evolution. Most of the coCHAPTERSntention actually concerns the details (second echelon issues) of human evolution rather than the fundamental issues. For example, both anatomical and molecular evidence on living (extant) hominoids (apes and humans) suggests the close relationship of African great apes and humans (hominins). That relationship is demonstrated by the existing hominoid fossil record, including that of early hominins. -
Unravelling the Positional Behaviour of Fossil Hominoids: Morphofunctional and Structural Analysis of the Primate Hindlimb
ADVERTIMENT. Lʼaccés als continguts dʼaquesta tesi queda condicionat a lʼacceptació de les condicions dʼús establertes per la següent llicència Creative Commons: http://cat.creativecommons.org/?page_id=184 ADVERTENCIA. El acceso a los contenidos de esta tesis queda condicionado a la aceptación de las condiciones de uso establecidas por la siguiente licencia Creative Commons: http://es.creativecommons.org/blog/licencias/ WARNING. The access to the contents of this doctoral thesis it is limited to the acceptance of the use conditions set by the following Creative Commons license: https://creativecommons.org/licenses/?lang=en Doctorado en Biodiversitat Facultad de Ciènces Tesis doctoral Unravelling the positional behaviour of fossil hominoids: Morphofunctional and structural analysis of the primate hindlimb Marta Pina Miguel 2016 Memoria presentada por Marta Pina Miguel para optar al grado de Doctor por la Universitat Autònoma de Barcelona, programa de doctorado en Biodiversitat del Departamento de Biologia Animal, de Biologia Vegetal i d’Ecologia (Facultad de Ciències). Este trabajo ha sido dirigido por el Dr. Salvador Moyà Solà (Institut Català de Paleontologia Miquel Crusafont) y el Dr. Sergio Almécija Martínez (The George Washington Univertisy). Director Co-director Dr. Salvador Moyà Solà Dr. Sergio Almécija Martínez A mis padres y hermana. Y a todas aquelas personas que un día decidieron perseguir un sueño Contents Acknowledgments [in Spanish] 13 Abstract 19 Resumen 21 Section I. Introduction 23 Hominoid positional behaviour The great apes of the Vallès-Penedès Basin: State-of-the-art Section II. Objectives 55 Section III. Material and Methods 59 Hindlimb fossil remains of the Vallès-Penedès hominoids Comparative sample Area of study: The Vallès-Penedès Basin Methodology: Generalities and principles Section IV. -
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. -
Abstracts Volume
SVPCA 58, Cambridge 2010, Preface Welcome to the 58th Symposium of Vertebrate Palaeontology and Comparative Anatomy, hosted by the University Museum of Zoology, Cambridge. We very much hope you find the meeting rewarding, and that you have time to enjoy the other attractions of the university, colleges, and city centre. The meeting logo was designed by Julia Molnar1 and depicts the finback whale (Balaenoptera physalus) on display above the Museum of Zoology. Enjoy your time in Cambridge! 1JuliaMolnar,RoyalVeterinaryCollege,jmolnar-at-rvc.ac.uk 1 SPPC/SVPCA 2010 Programme Overview Tuesday 14th September: SPPC Session 1, Chair: Matt Lowe 15.30-15.50 Christian Baars Infacol – if it’s good enough for babies, it’s good enough for ammonites. 15.50-15.10 Nigel R Larkin The joy of steel: How to master your awkward fossil in the field. 16.10-16.30 Frank Osbaeck Mechanical and chemical preparation methods used on the lower Eocene cementstone concretions from the Mo-Clay of northern Denmark 19.00 onwards EVENING RECEPTION, ZOOLOGY MUSEUM Wednesday 15th September 9.10-9.20 Welcome, notices for the day Session 1, Chair: Paul Barret 9.20-9.40 Eric Buffetaut et al. The Early Cretaceous vertebrate assemblage from the Napai Formation of Guangxi, southern China: a comparison with Thai assemblages 9.40-10.00 Michael J Benton et al. Recovery and expansion of marine vertebrate faunas in the Triassic of South China 10.00-10.20 Susan E Evans and Magdalend Borsuk-Bialynicka The Early Triassic faunal assemblage of Czatkowice, Poland 10.20-10.40 Sweetman, Steven C The first records of amphibians, lizards and maniraptoran dinosaurs from the Lower Cretaceous Hastings Group of south-east England 10.40-11.10 COFFEE BREAK Session 2, Chair: Jenny Clack 11.10-11.30 Tim Smithson and Stan Wood Eliminating Romer’s Gap: new tetrapods from the basal Carboniferous of the Scottish Borders 2 11.30-11.50 Per E Ahlberg et al. -
Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming
Distribution and Stratigraphip Correlation of Upper:UB_ • Ju Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming U,S. GEOLOGICAL SURVEY PROFESS IONAL PAPER 1540 Cover. A member of the American Museum of Natural History 1896 expedition enter ing the badlands of the Willwood Formation on Dorsey Creek, Wyoming, near what is now U.S. Geological Survey fossil vertebrate locality D1691 (Wardel Reservoir quadran gle). View to the southwest. Photograph by Walter Granger, courtesy of the Department of Library Services, American Museum of Natural History, New York, negative no. 35957. DISTRIBUTION AND STRATIGRAPHIC CORRELATION OF UPPER PALEOCENE AND LOWER EOCENE FOSSIL MAMMAL AND PLANT LOCALITIES OF THE FORT UNION, WILLWOOD, AND TATMAN FORMATIONS, SOUTHERN BIGHORN BASIN, WYOMING Upper part of the Will wood Formation on East Ridge, Middle Fork of Fifteenmile Creek, southern Bighorn Basin, Wyoming. The Kirwin intrusive complex of the Absaroka Range is in the background. View to the west. Distribution and Stratigraphic Correlation of Upper Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Tatman Formations, Southern Bighorn Basin, Wyoming By Thomas M. Down, Kenneth D. Rose, Elwyn L. Simons, and Scott L. Wing U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1540 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director For sale by U.S. Geological Survey, Map Distribution Box 25286, MS 306, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. -
From the Gulf Coastal Plain
Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 355-361 355 EKGMOWECHASHALA (MAMMALIA, ?PRIMATES) FROM THE GULF COASTAL PLAIN L. Barry Albright III1 A single, small, water-worn tooth from the “middle” Arikareean Toledo Bend Local Fauna of the Gulf Coastal Plain closely resembles the lower fourth premolar of the questionable primate Ekgmowechashala. The only known species of the genus, Ekgmowechashala philotau Macdonald (1963), was originally recovered from the early Arikareean Sharps Formation of South Dakota, but is also known from similar aged strata of the John Day Formation, Oregon. Although the Toledo Bend specimen differs somewhat in morphology from the p4 of E. philotau, a new species is not named in this report because of such limited material and because the specimen is incomplete. Unfortunately, the specimen does not provide information that helps clarify current arguments regarding the affinities of Ekgmowechashala with primates or plagiomenids. It does, however, provide (1) a temporal range extension for the genus to the early late Arikareean, or about four million years younger than previously known, and (2) a geographic extension east and considerably south of its prior distribution. If Ekgmowechashala is ultimately deter- mined to belong to the Primates, then the Toledo Bend species would become the last known North American representative of the order. Key Words: Ekgmowechashala; Primates; Plagiomenidae; Texas Gulf Coastal Plain; Arikareean INTRODUCTION brate paleontology collections of the Louisiana State Uni- In 1990, while screen-washing matrix from the “middle” versity Museum of Geoscience (LSUMG V). Arikareean Toledo Bend site in the Fleming Formation of easternmost Texas (Albright 1994, 1996, 1998a, 1998b, BACKGROUND 1999), a small, unusual, water-worn tooth was recov- Ekgmowechashala philotau is a small “enigmatic late ered that differed considerably from the site’s more com- Oligocene mammal” (McKenna, 1990:226) heretofore mon and readily identifiable rodent teeth. -
Juvenile Hominoid Cranium from the Terminal Miocene of Yunnan, China
Article Geology November 2013 Vol.58 No.31: 37713779 doi: 10.1007/s11434-013-6021-x Juvenile hominoid cranium from the terminal Miocene of Yunnan, China JI XuePing1,2, JABLONSKI Nina G3, SU Denise F4, DENG ChengLong5, FLYNN Lawrence J6, YOU YouShan7 & KELLEY Jay8* 1 Department of Paleoanthropology, Yunnan Institute of Cultural Relics and Archaeology, Kunming 650118, China; 2 Yunnan Key Laboratory for Paleobiology, Yunnan University, Kunming 650091, China; 3 Department of Anthropology, The Pennsylvania State University, University Park, PA 16802, USA; 4 Department of Paleobotany and Paleoecology, Cleveland Museum of Natural History, Cleveland, OH 44106, USA; 5 State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 6 Peabody Museum of Archaeology and Ethnology, Harvard University, Cambridge, MA 02138, USA; 7 Zhaotong Institute of Cultural Relics, Zhaotong 657000, China; 8 Institute of Human Origins and School of Human Evolution and Social Change, Arizona State University, Tempe, AZ 85287, USA Received May 28, 2013; accepted July 8, 2013; published online August 7, 2013 Fossil apes are known from several late Miocene localities in Yunnan Province, southwestern China, principally from Shihuiba (Lufeng) and the Yuanmou Basin, and represent three species of Lufengpithecus. They mostly comprise large samples of isolated teeth, but there are also several partial or complete adult crania from Shihuiba and a single juvenile cranium from Yuanmou. Here we describe a new, relatively complete and largely undistorted juvenile cranium from the terminal Miocene locality of Shuitangba, also in Yunnan. It is only the second ape juvenile cranium recovered from the Miocene of Eurasia and it is provisionally assigned to the species present at Shihuiba, Lufengpithecus lufengensis. -
69Th Annual Meeting Society of Vertebrate Paleontology
ISSN 0272-4634 September 2009 Society of Vertebrate Paleontology Society of Vertebrate Volume 29, Supplement to Number 3 Volume 69th Annual Meeting Paleontology Society of Vertebrate and Palaeontology of Vertebrate and the 57th Symposium Comparative Anatomy (SVPCA) University of Bristol Bristol, United Kingdom September 23-26, 2009 Program and Abstracts Vol. 29, Supplement to No. 3 September 2009 Wills Memorial 2 1/8” = 1/4 Mile Bristol/Precinct Map Building A4018, M5 junction 17 Badock Hall, Churchill Hall, Durdham Hall, Hiatt Baker Hall, KEY University Hall, Wills Hall Main Entrance to Sites Car Parks Traffic Flow Railway Station Victoria Rooms Burwalls via the Suspension Bridge A369, M5 junction 19 Bristol Marriott B3129 City Centre Hotel Avon Gorge Hotel to M32, M4 junction 19 (A38, A420, A421) Temple Meads Chemistry Building Broadmead Shopping Centre The Grand by Thistle Clifton Hill House Goldney Hall & Clifton Village DETAIL MAP Hotel Novotel Bristol Centre Bristol Temple Meads Railway Station Bristol Marriott A4 Royal Hotel A38, A420, M5 Bristol Airport Taunton, The South West Travelodge Bristol { Central Hotel SEE Bristol Hotel DETAIL MAP Hotel Ibis At-Bristol Bristol Centre Museum University of Bristol Vol. 29, Supplement to No. 3, September 2009 Vol. Technical Session IV, Wednesday 3:30 from the road, is very accessible. All these factors – together with its status as part of the PALEOECOLOGY OF SOUTH ASIAN PRIMATES: PALEOENVIRONMENTAL Ichnite Route of Soria, an open-air museographical area with 15 sites that can be visited IMPLICATIONS and a visitors’ centre – underlay the interest of the local authorities in converting it into a RAMDARSHAN, Anusha, Institut des Sciences de l’Evolution de Montpellier (UMR-CNRS point of tourist and cultural interest that is also accessible to the physically and visually 5554), Montpellier, France; MARIVAUX, Laurent, Institut des Sciences de l’Evolution de handicapped. -
Mammals from the Earliest Uintan (Middle Eocene) Turtle Bluff Member, Bridger Formation, Southwestern Wyoming, USA, Part 1: Primates and Rodentia
Palaeontologia Electronica palaeo-electronica.org Mammals from the earliest Uintan (middle Eocene) Turtle Bluff Member, Bridger Formation, southwestern Wyoming, USA, Part 1: Primates and Rodentia Thomas S. Kelly and Paul C. Murphey ABSTRACT The Turtle Bluff Member (TBM) is the stratotype section for the earliest Uintan bio- chron, Ui1a, of the middle Eocene Uintan North American Land Mammal age. For more than a century, the TBM had yielded only a few fragmentary specimens. As the result of many years of field work, numerous mammal fossils have now been recov- ered and provide an unprecedented opportunity to better define this poorly known interval. This is the first in a series of papers that provide detailed descriptions and tax- onomic revisions of the fauna of the TBM. Here we document the occurrence of the fol- lowing taxa in the TBM: Uintasorex parvulus; Microsyops annectans; Notharctus robustior; Omomys carteri; Trogolemur myodes; Washakius insignis; Thisbemys corru- gatus; Microparamys minutus; Microparamys sp.; Sciuravus nitidus; Tillomys senex; Tillomys? parvidens; Taxymys lucaris; Pauromys sp., cf. P. perdit us ; three informal sci- uravid species (sp. A, B and C); cf. Pareumys sp.; Metanoiamys sp.; and Elymys? emryi new species. Except for the previously described Hemiacodon engardae, all of the primates from the TBM are holdover taxa from the earlier Bridgerian Land Mammal age, whereas the rodents exhibit a modest diversification during the earliest Uintan. Elymys? emryi and four additional informal rodent species (Microparamys sp., sci- uravid sp. A, cf. Pareumys sp., and Metanoiamys sp.) make their appearances in the TBM and, as such, can be added to the list of index species characterizing biochron Ui1a.