Plio-Pleistocene Large Carnivores from the Italian Peninsula: Functional Morphology and Macroecology
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Aspects of the Functional Morphology in the Cranial and Cervical Skeleton of the Sabre-Toothed Cat Paramachairodus Ogygia (Kaup, 1832) (Felidae
Blackwell Science, LtdOxford, UKZOJZoological Journal of the Linnean Society0024-4082The Lin- nean Society of London, 2005? 2005 1443 363377 Original Article FUNCTIONAL MORPHOLOGY OF P. OGYGIAM. J. SALESA ET AL. Zoological Journal of the Linnean Society, 2005, 144, 363–377. With 11 figures Aspects of the functional morphology in the cranial and cervical skeleton of the sabre-toothed cat Paramachairodus ogygia (Kaup, 1832) (Felidae, Machairodontinae) from the Late Miocene of Spain: Downloaded from https://academic.oup.com/zoolinnean/article-abstract/144/3/363/2627519 by guest on 18 May 2020 implications for the origins of the machairodont killing bite MANUEL J. SALESA1*, MAURICIO ANTÓN2, ALAN TURNER1 and JORGE MORALES2 1School of Biological & Earth Sciences, Byrom Street, Liverpool John Moores University, Liverpool, L3 3AF, UK 2Departamento de Palaeobiología, Museo Nacional de Ciencias Naturales-CSIC, José Gutiérrez Abascal, 2. 28006 Madrid, Spain Received January 2004; accepted for publication March 2005 The skull and cervical anatomy of the sabre-toothed felid Paramachairodus ogygia (Kaup, 1832) is described in this paper, with special attention paid to its functional morphology. Because of the scarcity of fossil remains, the anatomy of this felid has been very poorly known. However, the recently discovered Miocene carnivore trap of Batallones-1, near Madrid, Spain, has yielded almost complete skeletons of this animal, which is now one of the best known machairodontines. Consequently, the machairodont adaptations of this primitive sabre-toothed felid can be assessed for the first time. Some characters, such as the morphology of the mastoid area, reveal an intermediate state between that of felines and machairodontines, while others, such as the flattened upper canines and verticalized mandibular symphysis, show clear machairodont affinities. -
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. -
University of Florida Thesis Or Dissertation Formatting
UNDERSTANDING CARNIVORAN ECOMORPHOLOGY THROUGH DEEP TIME, WITH A CASE STUDY DURING THE CAT-GAP OF FLORIDA By SHARON ELIZABETH HOLTE 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 2018 © 2018 Sharon Elizabeth Holte To Dr. Larry, thank you ACKNOWLEDGMENTS I would like to thank my family for encouraging me to pursue my interests. They have always believed in me and never doubted that I would reach my goals. I am eternally grateful to my mentors, Dr. Jim Mead and the late Dr. Larry Agenbroad, who have shaped me as a paleontologist and have provided me to the strength and knowledge to continue to grow as a scientist. I would like to thank my colleagues from the Florida Museum of Natural History who provided insight and open discussion on my research. In particular, I would like to thank Dr. Aldo Rincon for his help in researching procyonids. I am so grateful to Dr. Anne-Claire Fabre; without her understanding of R and knowledge of 3D morphometrics this project would have been an immense struggle. I would also to thank Rachel Short for the late-night work sessions and discussions. I am extremely grateful to my advisor Dr. David Steadman for his comments, feedback, and guidance through my time here at the University of Florida. I also thank my committee, Dr. Bruce MacFadden, Dr. Jon Bloch, Dr. Elizabeth Screaton, for their feedback and encouragement. I am grateful to the geosciences department at East Tennessee State University, the American Museum of Natural History, and the Museum of Comparative Zoology at Harvard for the loans of specimens. -
Raymond M. Alf Museum of Paleontology EDUCATOR's GUIDE
Raymond M. Alf Museum of Paleontology EDUCATOR’S GUIDE Dear Educator: This guide is recommended for educators of grades K-4 and is designed to help you prepare students for their Alf Museum visit, as well as to provide resources to enhance your classroom curriculum. This packet includes background information about the Alf Museum and the science of paleontology, a summary of our museum guidelines and what to expect, a pre-visit checklist, a series of content standard-aligned activities/exercises for classroom use before and/or after your visit, and a list of relevant terms and additional resources. Please complete and return the enclosed evaluation form to help us improve this guide to better serve your needs. Thank you! Paleontology: The Study of Ancient Life Paleontology is the study of ancient life. The history of past life on Earth is interpreted by scientists through the examination of fossils, the preserved remains of organisms which lived in the geologic past (more than 10,000 years ago). There are two main types of fossils: body fossils, the preserved remains of actual organisms (e.g. shells/hard parts, teeth, bones, leaves, etc.) and trace fossils, the preserved evidence of activity by organisms (e.g. footprints, burrows, fossil dung). Chances for fossil preservation are enhanced by (1) the presence of hard parts (since soft parts generally rot or are eaten, preventing preservation) and (2) rapid burial (preventing disturbance by bio- logical or physical actions). Many body fossils are skeletal remains (e.g. bones, teeth, shells, exoskel- etons). Most form when an animal or plant dies and then is buried by sediment (e.g. -
Phylogenetic and Phylogeographic Analysis of Iberian Lynx Populations
Journal of Heredity 2004:95(1):19–28 ª 2004 The American Genetic Association DOI: 10.1093/jhered/esh006 Phylogenetic and Phylogeographic Analysis of Iberian Lynx Populations W. E. JOHNSON,J.A.GODOY,F.PALOMARES,M.DELIBES,M.FERNANDES,E.REVILLA, AND S. J. O’BRIEN From the Laboratory of Genomic Diversity, National Cancer Institute-FCRDC, Frederick, MD 21702-1201 (Johnson and O’Brien), Department of Applied Biology, Estacio´ n Biolo´ gica de Don˜ana, CSIC, Avda. Marı´a Luisa s/n, 41013, Sevilla, Spain (Godoy, Palomares, Delibes, and Revilla), and Instituto da Conservac¸a˜o da Natureza, Rua Filipe Folque, 46, 28, 1050-114 Lisboa, Portugal (Fernandes). E. Revilla is currently at the Department of Ecological Modeling, UFZ-Center for Environmental Research, PF 2, D-04301 Leipzig, Germany. The research was supported by DGICYT and DGES (projects PB90-1018, PB94-0480, and PB97-1163), Consejerı´a de Medio Ambiente de la Junta de Andalucı´a, Instituto Nacional para la Conservacion de la Naturaleza, and US-Spain Joint Commission for Scientific and Technological Cooperation. We thank A. E. Pires, A. Piriz, S. Cevario, V. David, M. Menotti-Raymond, E. Eizirik, J. Martenson, J. H. Kim, A. Garfinkel, J. Page, C. Ferris, and E. Carney for advice and support in the laboratory and J. Calzada, J. M. Fedriani, P. Ferreras, and J. C. Rivilla for assistance in the capture of lynx. Museo Nacional de Ciencias Naturales, Don˜ana Biological Station scientific collection, Don˜ana National Park, and Instituto da Conservac¸a˜o da Natureza of Portugal provided samples of museum specimens. -
Working with the Public: How an Unusual Museum Enquiry Turned Into Travels Through Time and Space
Freedman, J and Evans, J 2015 Working with the Public: How an Unusual Museum Enquiry Turned into Travels Through Time and Space. Open Quaternary, 1: 8, pp. 1–14, DOI: http://dx.doi.org/10.5334/oq.ah ENGAGEMENT PAPER Working with the Public: How an Unusual Museum Enquiry Turned into Travels Through Time and Space Jan Freedman* and Jane Evans† This article has been corrected here: Museum enquiries offer a unique opportunity to engage on a one-to-one level with members of the pub- lic. This paper covers an unusual enquiry from 2013 of an unknown tooth that was brought into Plym- outh City Museum and Art Gallery for identification. We highlight how museum enquiries can engage with members of the public by involving them directly with original scientific research. The tooth was found in a garden in Plymouth with no associated data of about where it originated. We identified the tooth, and the enquirer researched the history of the house. The tooth gave the appearance of a sub-fossil so with the large number of Quaternary sites in Plymouth, together with the identifica- tion of the previous owner on the site, there were valid reasons to undertake testing of the tooth to determine its origin. Strontium (Sr) isotope analysis of the tooth was carried out to determine if the tooth was British and radiocarbon dating was undertaken to work out the age of the tooth. The 87Sr /86Sr of the leopard tooth gave a value of 0.716131, with Sr concentrations at 568ppm. This is a high concentration of Sr ppm relative to other British data, suggesting a non-British origin. -
New Data on the Early Villafranchian Fauna from Vialette (Haute-Loire, France) Based on the Collection of the Crozatier Museum (Le Puy-En-Velay, Haute-Loire, France)
ARTICLE IN PRESS Quaternary International 179 (2008) 64–71 New data on the Early Villafranchian fauna from Vialette (Haute-Loire, France) based on the collection of the Crozatier Museum (Le Puy-en-Velay, Haute-Loire, France) Fre´de´ric Lacombata,Ã, Laura Abbazzib, Marco P. Ferrettib, Bienvenido Martı´nez-Navarroc, Pierre-Elie Moulle´d, Maria-Rita Palomboe, Lorenzo Rookb, Alan Turnerf, Andrea M.-F. Vallig aForschungsstation fu¨r Quata¨rpala¨ontologie Senckenberg, Weimar, Am Jakobskirchhof 4, D-99423 Weimar, Germany bDipartimento di Scienze della Terra, Universita` di Firenze, Via G. La Pira 4, 50121 Firenze, Italy cICREA, A`rea de Prehisto`ria, Universitat Rovira i Virgili-IPHES, Plac-a Imperial Tarraco 1, 43005 Tarragona, Spain dMuse´e de Pre´histoire Re´gionale de Menton, Rue Lore´dan Larchey, 06500 Menton, France eDipartimento di Scienze della Terra, Universita` degli Studi di Roma ‘‘La Sapienza’’, CNR, Ple. Aldo Moro, 500185 Roma, Italy fSchool of Biological and Earth Sciences, Liverpool John Moore University, Liverpool L3 3AF, UK g78 rue du pont Guinguet, 03000 Moulins, France Available online 7 September 2007 Abstract Vialette (3.14 Ma), like Sene` ze, Chilhac, Sainzelles, Ceyssaguet or Soleilhac, is one of the historical sites located in Haute-Loire (France). The lacustrine sediments of Vialette are the result of a dammed lake formed by a basalt flow above Oligocene layers, and show a geological setting typical for this area, where many localities are connected with maar structures that have allowed intra-crateric lacustrine deposits to accumulate. Based on previous studies and this work, a faunal list of 17 species of large mammals has been established. -
Human Origin Sites and the World Heritage Convention in Eurasia
World Heritage papers41 HEADWORLD HERITAGES 4 Human Origin Sites and the World Heritage Convention in Eurasia VOLUME I In support of UNESCO’s 70th Anniversary Celebrations United Nations [ Cultural Organization Human Origin Sites and the World Heritage Convention in Eurasia Nuria Sanz, Editor General Coordinator of HEADS Programme on Human Evolution HEADS 4 VOLUME I Published in 2015 by the United Nations Educational, Scientific and Cultural Organization, 7, place de Fontenoy, 75352 Paris 07 SP, France and the UNESCO Office in Mexico, Presidente Masaryk 526, Polanco, Miguel Hidalgo, 11550 Ciudad de Mexico, D.F., Mexico. © UNESCO 2015 ISBN 978-92-3-100107-9 This publication is available in Open Access under the Attribution-ShareAlike 3.0 IGO (CC-BY-SA 3.0 IGO) license (http://creativecommons.org/licenses/by-sa/3.0/igo/). By using the content of this publication, the users accept to be bound by the terms of use of the UNESCO Open Access Repository (http://www.unesco.org/open-access/terms-use-ccbysa-en). The designations employed and the presentation of material throughout this publication do not imply the expression of any opinion whatsoever on the part of UNESCO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The ideas and opinions expressed in this publication are those of the authors; they are not necessarily those of UNESCO and do not commit the Organization. Cover Photos: Top: Hohle Fels excavation. © Harry Vetter bottom (from left to right): Petroglyphs from Sikachi-Alyan rock art site. -
Title Notes on Carnivore Fossils from the Pliocene Udunga Fauna
Notes on carnivore fossils from the Pliocene Udunga fauna, Title Transbaikal area, Russia Ogino, Shintaro; Nakaya, Hideo; Takai, Masanaru; Fukuchi, Author(s) Akira Citation Asian paleoprimatology (2009), 5: 45-60 Issue Date 2009 URL http://hdl.handle.net/2433/199776 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University Asian Paleoprimatology, vol. 5: 45-60 (2008) Kyoto University Primate Research Institute Notes on carnivore fossils from the Pliocene Udunga fauna, Transbaikal area, Russia Shintaro Ogino1*, Hideo Nakaya2, Masanaru Takai1, Akira Fukuchi2, 3 1Primate Research Institute, Kyoto University. Inuyama 484-8506, Japan 2Graduate School of Science and Engineering, Kagoshima University, Kagoshima 890-0065, Japan 3Graduate School of Natural Science and Technology, Okayama University, Okayama 700-8530, Japan *Corresponding author. e-mail: [email protected] Abstract We provide notes of carnivore fossils from the middle Pliocene Udunga fauna, Transbaikal area, Russia. The fossil carnivore assemblage consists of more than 200 specimens including eleven genera. Ursus, Parailurus, Parameles, and Ferinestrix are representative of the animals of thermophilic forest biotopes. On the other hand, Chasmaporthetes and Pliocrocuta are probably specialized in open environment. The prosperity both in foresal and semiarid carnivores indicate that the Udunga fauna is comprised of mosaic elements. Introduction The fauna dating back to the Pliocene in Udunga, Transbaikalia, Russia, comprises eleven species of mammals, such as rodents, lagomorphs, carnivores, perissodactyls, artiodactyls, and elephants (Kalmykov, 1989, 1992, 2003; Kalmykov and Maschenko, 1992, 1995 Vislobokova et al., 1993, 1995;; Erbajeva et al., 2003). The Udunga site is located on the left bank of the Temnik River, the tributary of the Selenga River in the vicinity of Udunga village (Figure 1). -
A Mammalian Lost World in Southwest Europe During the Late Pliocene
A Mammalian Lost World in Southwest Europe during the Late Pliocene Alfonso Arribas1*, Guiomar Garrido1,Ce´sar Viseras2, Jesu´ s M. Soria3, Sila Pla2, Jose´ G. Solano1, Miguel Garce´s4, Elisabet Beamud5, Jose´ S. Carrio´ n6 1 Departamento de Investigacio´n en Recursos Geolo´gicos, Instituto Geolo´gico y Minero de Espan˜a, Madrid, Spain, 2 Departamento de Estratigrafı´a y Paleontologı´a, Facultad de Ciencias, Universidad de Granada, Granada, Spain, 3 Departamento de Ciencias de la Tierra y del Medio Ambiente, Facultad de Ciencias, Universidad de Alicante, Alicante, Spain, 4 Departamento de Estratigrafı´a, Paleontologı´a y Geociencias Marinas, Facultad de Geologı´a, Universidad de Barcelona, Barcelona, Spain, 5 Paleomagnetic Laboratory (UB-CSIC) Institute of Earth Sciences, Jaume Almera, Barcelona, Spain, 6 Departamento de Biologı´a Vegetal, Facultad de Biologı´a, Universidad de Murcia, Murcia, Spain Abstract Background: Over the last decades, there has been an increasing interest on the chronology, distribution and mammal taxonomy (including hominins) related with the faunal turnovers that took place around the Pliocene-Pleistocene transition [ca. 1.8 mega-annum (Ma)] in Europe. However, these turnovers are not fully understood due to: the precarious nature of the period’s fossil record; the ‘‘non-coexistence’’ in this record of many of the species involved; and the enormous geographical area encompassed. This palaeontological information gap can now be in part bridged with data from the Fonelas P-1 site (Granada, Spain), whose faunal composition and late Upper Pliocene date shed light on some of the problems concerning the timing and geography of the dispersals. Methodology/Principal Findings: This rich fossil site yielded 32 species of mammals, among which autochthonous species of the European Upper Villafranchian coexist with canids (Canis), ovibovines (Praeovibos)andgiraffids(Mitilanotherium) from Asia. -
Appendix G Paleontological Resources Assessment
Appendix G Paleontological Resources Assessment Paleontological Resource Assessment for the California Flats Solar Project, Monterey and San Luis Obispo Counties, California Jessica L. DeBusk Prepared By Applied EarthWorks, Inc. 743 Pacific Street, Suite A San Luis Obispo, CA 93401 Prepared For Element Power US, LLC 421 SW Sixth Avenue, Suite 1000 Portland, OR 97204 April 2013 draft SUMMARY OF FINDINGS At the request of Element Power US, LLC, parent company of California Flats Solar, LLC (the Applicant), Applied EarthWorks Inc. (Æ) performed a paleontological resource assessment for the California Flats Solar Project (Project) located southeast of Parkfield in Monterey and San Luis Obispo counties, California. The study consisted of a museum records search, a comprehensive literature and geologic map review, and a field survey. This report summarizes the methods and results of the paleontological resource assessment and provides Project-specific management recommendations. This assessment included a comprehensive review of published and unpublished literature and museum collections records maintained by the Natural History Museum of Los Angeles County (LACM) and the University of California Museum of Paleontology (UCMP). The purpose of the literature review and museum records search was to identify the geologic units underlying the Project area and to determine whether or not previously recorded paleontological localities occur either within the Project boundaries or within the same geologic units elsewhere. The museum records search was followed by a field survey. The purpose of the field survey was to visually inspect the ground surface for exposed fossils and to evaluate geologic exposures for their potential to contain preserved fossil material at the subsurface. -
Prehistoric Panama 20 Million Years Ago: Evidence from the Fossil Record
Prehistoric Panama 20 Million Years Ago: Evidence from the Fossil Record Bruce J. MacFadden Florida Museum of Natural History Outline 1. Background & context: Panama as a gateway to the Americas 2. GABI (Great American Biotic Interchange) 3. Collecting Miocene fossils in Panama: A once-in-a- century opportunity 4. Panama 20 million years ago: • Cast of characters • Age and ancient ecology, etc. 5. Why should we care? Background: Panama as a Gateway to the Americas GABI (Great American Biotic Interchange) • Has fascinated paleontologists and biologists since the mid 18th century • Simple and classic story: during the Pleistocene (about 2 million years ago) the Isthmus formed, resulting in a land bridge • This profoundly impacted life – On land – In the oceans S. David Webb, FLMNH Simpson—1980, Splendid Isolation • Three faunal horizons “strata” in South America representing past 60 million years – First Phase: Old timers alone – Second Phase: Aliens appear – Third phase: Interchange (GABI) GABI—a more complex story that continues to evolve • In contrast to Simpson’s third phase (GABI), several distinct phases and pulses of land species dispersal before and after the formation of the Isthmus • In contrast to the classic story of the floodgates opening during the Pleistocene, GABI started about 8 million years ago with multiple dispersal events Late Miocene— 8 million years ago • Ground sloths in Florida • Racoons, coati, etc (procyonids) and mastodonts to S. America • With no Isthmus, Dispersal route problematical Pliocene: 4 to 5 million