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European Journal of Taxonomy 753: 1–80 ISSN 2118-9773 https://doi.org/10.5852/ejt.2021.753.1389 www.europeanjournaloftaxonomy.eu 2021 · Tissier J. et al. This work is licensed under a Creative Commons Attribution License (CC BY 4.0). Monograph urn:lsid:zoobank.org:pub:8009DD3B-53B0-45C9-921E-58D04C9C0B48 New species, revision, and phylogeny of Ronzotherium Aymard, 1854 (Perissodactyla, Rhinocerotidae) Jérémy TISSIER 1,*, Pierre-Olivier ANTOINE 2 & Damien BECKER 3 1,3 Route de Fontenais 21, JURASSICA Museum, 2900 Porrentruy, Switzerland & Chemin du musée 4, Université de Fribourg, Department of Geosciences, 1700 Fribourg, Switzerland. 2 Place Eugène Bataillon, Institut des sciences de l’évolution de Montpellier-CNRS-IRD-RPHE, Université de Montpellier, 34095 Montpellier, France. * Corresponding author: [email protected] 2 Email: [email protected] 3 Email: [email protected] 1 urn:lsid:zoobank.org:author:7418361D-FAA0-4D7D-AE4A-80B5C9288B31 2 urn:lsid:zoobank.org:author:61FBD377-963B-4530-A4BC-0AB4CBCAD967 3 urn:lsid:zoobank.org:author:E1D8E6B2-6F92-4B0B-A772-4F5C561851DB Abstract. Ronzotherium is one of the earliest Rhinocerotidae in Europe, which fi rst appeared just after the Eocene/Oligocene transition (Grande Coupure), and became extinct at the end of the Oligocene. It is a large-sized rhinocerotid, with a special position in the phylogeny of this group, as being one of the earliest-branching true Rhinocerotidae. However, its intra-generic systematics has never been tested through computational phylogenetic methods and it is basically unknown. Its taxonomical history has gone through numerous complications, and thus we aim to provide here a complete revision of this genus, through phylogenetic methods. -
From the Late–Middle Eocene of Eastern Thrace
G Model PALEVO-993; No. of Pages 15 ARTICLE IN PRESS C. R. Palevol xxx (2017) xxx–xxx Contents lists available at ScienceDirect Comptes Rendus Palevol www.sci encedirect.com General Palaeontology, Systematics and Evolution (Vertebrate Palaeontology) First occurrence of Palaeotheriidae (Perissodactyla) from the late–middle Eocene of eastern Thrace (Greece) Première occurrence de Palaeotheriidae (Perissodactyla) du Miocène moyen–tardif de Thrace orientale (Grèce) a,b,∗ a Grégoire Métais , Sevket Sen a CR2P, Paléobiodiversité et Paléoenvironnements, UMR 7207 (CNRS, MNHN, UPMC), Sorbonne Université, Muséum national d’histoire naturelle, 8, rue Buffon, 75005 Paris, France b Department of Ecology and Evolutionary Biology, University of Kansas, 66045 Lawrence, Kansas, USA a b s t r a c t a r t i c l e i n f o Article history: A detailed assessment of postcranial fossils collected at Balouk Keui (Thrace, Greece) in the Received 11 July 2016 mid-19th Century by the naturalist Auguste Viquesnel enabled us to identify the material Accepted after revision 10 January 2017 as pertaining to Palaeotherium sp., cf. P. magnum, which constitutes the easternmost occur- Available online xxx rence of the genus during the Eocene. We have constrained the geographic and stratigraphic provenance of the fossil by reassessing information about Viquesnel’s itinerary and observa- Handled by Lars vanden Hoek Ostende tions. Although the exact age of the fossil remains uncertain, the occurrence of a palaeothere in the Thrace Basin during the Eocene indicates a wider geographic distribution for the Keywords: genus, which had previously been restricted to western and central Europe. The palaeothere Palaeotherium of Balouk Keui confirms that the palaeogeographic range of this group included the Balkans Thrace during the middle–late Eocene. -
Mammal Collections Accredited by the American Society of Mammalogists, Systematics Collections Committee
MAMMAL COLLECTIONS ACCREDITED BY THE AMERICAN SOCIETY OF MAMMALOGISTS The collections on this list meet or exceed the basic curatorial standards established by the ASM Systematic Collections Committee (Appendix V). Collections are listed alphabetically by country, then province or state. Date of accreditation (and reaccreditation) are indicated. Year of Province Collection name and acronym accreditation or state ARGENTINA Universidad Nacional de Tucumán, Colección de Mamíferos Lillo (CML) 1999 Tucumán CANADA Provincial Museum of Alberta (PMA) 1985 Alberta University of Alberta, Museum of Zoology (UAMZ) 1985 Alberta Royal British Columbia Museum (RBCM) 1976 British Columbia University of British Columbia, Cowan Vertebrate Museum (UBC) 1975 British Columbia Canadian Museum of Nature (CMN) 1975, 1987 Ontario Royal Ontario Museum (ROM) 1975, 1995 Ontario MEXICO Colección Nacional de Mamíferos, Instituto de Biología, Universidad Nacional Autónoma de México (CNMA) 1975, 1983 Distrito Federal Centro de Investigaciones Biologicas del Noroeste (CIBNOR) 1999 Baja California Sur UNITED STATES University of Alaska Museum (UAM) 1975, 1983 Alaska University of Arizona, Collection of Mammals (UA) 1975, 1982 Arizona Arkansas State University, Collection of Recent Mammals (ASUMZ) 1976 Arkansas University of Arkansas at Little Rock (UALRVC) 1977 Arkansas California Academy of Sciences (CAS) 1975 California California State University, Long Beach (CSULB) 1979, 1980 California Humboldt State University (HSU) 1984 California Natural History Museum of Los -
1 VERTEBRATE ZOOLOGY (BIO 353) Spring 2019 MW 8:45-10:00 AM, 207 Payson Smith Lab: M 11:45-3:35 PM, 160 Science INSTRUCTOR
VERTEBRATE ZOOLOGY (BIO 353) Spring 2019 MW 8:45-10:00 AM, 207 Payson Smith Lab: M 11:45-3:35 PM, 160 Science INSTRUCTOR: Dr. Chris Maher EMAIL: [email protected] OFFICE LOCATION: 201 Science (A Wing) or 178 Science (CSTH Dean’s office, C Wing) OFFICE PHONE: 207.780.4612; 207.780.4377 OFFICE HOURS: T 12:00 – 1:00 PM, W 10:00 AM – 12:00 PM, or by appointment I usually hold office hours in 201 Science; however, if plans change, I leave a note on the door, and you probably can find me in 178 Science. Office hours are subject to change due to my meeting schedule, and I try to notify you in advance. COURSE DESCRIPTION: Vertebrate Zoology is an upper division biology elective in Area 1 (Organismal Biology) that surveys major groups of vertebrates. We examine many aspects of vertebrate biology, including physiology, anatomy, morphology, ecology, behavior, evolution, and conservation. This course also includes a laboratory component, the primary focus of which will be a survey of vertebrates at a local natural area. As much as possible, we will spend time in the field, learning survey techniques and identifying vertebrates. This syllabus is intended as a guide for the semester; however, I reserve the right to make changes in topics or schedules as necessary. COURSE PREREQUISITES: You must have successfully completed (i.e., grade of C- or higher) Biological Principles III (BIO 109). Although not required, courses in evolution (BIO 217), ecology (e.g., BIO 203), and animal physiology (e.g., BIO 401) should prove helpful. -
Zoology Courses 1
Zoology Courses 1 Zoology Courses Courses ZOOL 2406. Vertebrate Zoology. Vertebrate Zoology: A survey of basic classification, functional systems, and biology of vertebrates. MATH 1508 may be taken concurrently with ZOOL 2406. Course fee required. [Common Course Number BIOL 1313] Department: Zoology 4 Credit Hours 6 Total Contact Hours 3 Lab Hours 3 Lecture Hours 0 Other Hours Prerequisite(s): (BIOL 1107 w/D or better AND BIOL 1305 w/D or better ) AND (BIOL 1108 w/D or better AND BIOL 1306 w/D or better) ZOOL 2466. Invertebrate Zoology. Invertebrate Zoology: Survey and laboratory exercises concerning the invertebrates with emphasis on phylogeny. Course fee required. [Common Course Number BIOL 1413] Department: Zoology 4 Credit Hours 6 Total Contact Hours 3 Lab Hours 3 Lecture Hours 0 Other Hours Prerequisite(s): (BIOL 1107 w/D or better AND BIOL 1305 w/D or better ) AND (BIOL 1108 w/D or better AND BIOL 1306 w/D or better) ZOOL 3464. Medical Parasitology. Medical Parasitology (3-3) A survey of medically important parasites. Prerequisite: ZOOL 2406, or BIOL 1306 and BIOL 1108. Lab fee required. Replaced ZOOL 3364 and ZOOL 1365. Department: Zoology 4 Credit Hours 6 Total Contact Hours 3 Lab Hours 3 Lecture Hours 0 Other Hours Prerequisite(s): (ZOOL 2406 w/D or better ) OR (BIOL 1108 w/D or better AND BIOL 1306 w/D or better) ZOOL 4181. Vertebrate Physiology Methods. Vertebrate Physiology Methods (0-3) Techniques and instrumentation used in the study of vertebrate function. Prerequisites: CHEM 1306-1106 or CHEM 1408 and (1) BIOL 1306-1108, (2) BIOL 2313-2113, (3) BIOL 3414, or (4) ZOOL 2406. -
Early Eocene Fossils Suggest That the Mammalian Order Perissodactyla Originated in India
ARTICLE Received 7 Jul 2014 | Accepted 15 Oct 2014 | Published 20 Nov 2014 DOI: 10.1038/ncomms6570 Early Eocene fossils suggest that the mammalian order Perissodactyla originated in India Kenneth D. Rose1, Luke T. Holbrook2, Rajendra S. Rana3, Kishor Kumar4, Katrina E. Jones1, Heather E. Ahrens1, Pieter Missiaen5, Ashok Sahni6 & Thierry Smith7 Cambaytheres (Cambaytherium, Nakusia and Kalitherium) are recently discovered early Eocene placental mammals from the Indo–Pakistan region. They have been assigned to either Perissodactyla (the clade including horses, tapirs and rhinos, which is a member of the superorder Laurasiatheria) or Anthracobunidae, an obscure family that has been variously considered artiodactyls or perissodactyls, but most recently placed at the base of Proboscidea or of Tethytheria (Proboscidea þ Sirenia, superorder Afrotheria). Here we report new dental, cranial and postcranial fossils of Cambaytherium, from the Cambay Shale Formation, Gujarat, India (B54.5 Myr). These fossils demonstrate that cambaytheres occupy a pivotal position as the sister taxon of Perissodactyla, thereby providing insight on the phylogenetic and biogeographic origin of Perissodactyla. The presence of the sister group of perissodactyls in western India near or before the time of collision suggests that Perissodactyla may have originated on the Indian Plate during its final drift toward Asia. 1 Center for Functional Anatomy & Evolution, Johns Hopkins University School of Medicine, 1830 E. Monument Street, Baltimore, Maryland 21205, USA. 2 Department of Biological Sciences, Rowan University, Glassboro, New Jersey 08028, USA. 3 Department of Geology, H.N.B. Garhwal University, Srinagar 246175, Uttarakhand, India. 4 Wadia Institute of Himalayan Geology, Dehradun 248001, Uttarakhand, India. 5 Research Unit Palaeontology, Ghent University, Krijgslaan 281-S8, B-9000 Ghent, Belgium. -
Biblioqraphy & Natural History
BIBLIOQRAPHY & NATURAL HISTORY Essays presented at a Conference convened in June 1964 by Thomas R. Buckman Lawrence, Kansas 1966 University of Kansas Libraries University of Kansas Publications Library Series, 27 Copyright 1966 by the University of Kansas Libraries Library of Congress Catalog Card number: 66-64215 Printed in Lawrence, Kansas, U.S.A., by the University of Kansas Printing Service. Introduction The purpose of this group of essays and formal papers is to focus attention on some aspects of bibliography in the service of natural history, and possibly to stimulate further studies which may be of mutual usefulness to biologists and historians of science, and also to librarians and museum curators. Bibli• ography is interpreted rather broadly to include botanical illustration. Further, the intent and style of the contributions reflects the occasion—a meeting of bookmen, scientists and scholars assembled not only to discuss specific examples of the uses of books and manuscripts in the natural sciences, but also to consider some other related matters in a spirit of wit and congeniality. Thus we hope in this volume, as in the conference itself, both to inform and to please. When Edwin Wolf, 2nd, Librarian of the Library Company of Phila• delphia, and then Chairman of the Rare Books Section of the Association of College and Research Libraries, asked me to plan the Section's program for its session in Lawrence, June 25-27, 1964, we agreed immediately on a theme. With few exceptions, we noted, the bibliography of natural history has received little attention in this country, and yet it is indispensable to many biologists and to historians of the natural sciences. -
The Linnaean Collections
THE LINNEAN SPECIAL ISSUE No. 7 The Linnaean Collections edited by B. Gardiner and M. Morris WILEY-BLACKWELL 9600 Garsington Road, Oxford OX4 2DQ © 2007 The Linnean Society of London All rights reserved. No part of this book may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage or retrieval system, without permission in writing from the publisher. The designations of geographic entities in this book, and the presentation of the material, do not imply the expression of any opinion whatsoever on the part of the publishers, the Linnean Society, the editors or any other participating organisations concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The Linnaean Collections Introduction In its creation the Linnaean methodology owes as much to Artedi as to Linneaus himself. So how did this come about? It was in the spring of 1729 when Linnaeus first met Artedi in Uppsala and they remained together for just over seven years. It was during this period that they not only became the closest of friends but also developed what was to become their modus operandi. Artedi was especially interested in natural history, mineralogy and chemistry; Linnaeus on the other hand was far more interested in botany. Thus it was at this point that they decided to split up the natural world between them. Artedi took the fishes, amphibia and reptiles, Linnaeus the plants, insects and birds and, while both agreed to work on the mammals, Linneaus obligingly gave over one plant family – the Umbelliforae – to Artedi “as he wanted to work out a new method of classifying them”. -
2014BOYDANDWELSH.Pdf
Proceedings of the 10th Conference on Fossil Resources Rapid City, SD May 2014 Dakoterra Vol. 6:124–147 ARTICLE DESCRIPTION OF AN EARLIEST ORELLAN FAUNA FROM BADLANDS NATIONAL PARK, INTERIOR, SOUTH DAKOTA AND IMPLICATIONS FOR THE STRATIGRAPHIC POSITION OF THE BLOOM BASIN LIMESTONE BED CLINT A. BOYD1 AND ED WELSH2 1Department of Geology and Geologic Engineering, South Dakota School of Mines and Technology, Rapid City, South Dakota 57701 U.S.A., [email protected]; 2Division of Resource Management, Badlands National Park, Interior, South Dakota 57750 U.S.A., [email protected] ABSTRACT—Three new vertebrate localities are reported from within the Bloom Basin of the North Unit of Badlands National Park, Interior, South Dakota. These sites were discovered during paleontological surveys and monitoring of the park’s boundary fence construction activities. This report focuses on a new fauna recovered from one of these localities (BADL-LOC-0293) that is designated the Bloom Basin local fauna. This locality is situated approximately three meters below the Bloom Basin limestone bed, a geographically restricted strati- graphic unit only present within the Bloom Basin. Previous researchers have placed the Bloom Basin limestone bed at the contact between the Chadron and Brule formations. Given the unconformity known to occur between these formations in South Dakota, the recovery of a Chadronian (Late Eocene) fauna was expected from this locality. However, detailed collection and examination of fossils from BADL-LOC-0293 reveals an abundance of specimens referable to the characteristic Orellan taxa Hypertragulus calcaratus and Leptomeryx evansi. This fauna also includes new records for the taxa Adjidaumo lophatus and Brachygaulus, a biostratigraphic verifica- tion for the biochronologically ambiguous taxon Megaleptictis, and the possible presence of new leporid and hypertragulid taxa. -
Chapter 1 Paleontology As a Science
Chapter 1 Paleontology as a science Key points • The key value of paleontology has been to show us the history of life through deep time – without fossils this would be largely hidden from us. • Paleontology has strong relevance today in understanding our origins, other distant worlds, climate and biodiversity change, the shape and tempo of evolution, and dating rocks. • Paleontology is a part of the natural sciences, and a key aim is to reconstruct ancient life. • Reconstructions of ancient life have been rejected as pure speculation by some, but careful consideration shows that they too are testable hypotheses and can be as scientifi c as any other attempt to understand the world. • Science consists of testing hypotheses, not in general by limiting itself to absolute cer- tainties like mathematics. • Classical and medieval views about fossils were often magical and mystical. • Observations in the 16th and 17th centuries showed that fossils were the remains of ancient plants and animals. • By 1800, many scientists accepted the idea of extinction. • By 1830, most geologists accepted that the Earth was very old. • By 1840, the major divisions of deep time, the stratigraphic record, had been established by the use of fossils. • By 1840, it was seen that fossils showed direction in the history of life, and by 1860 this had been explained by evolution. • Research in paleontology has many facets, including fi nding new fossils and using quan- titative methods to answer questions about paleobiology, paleogeography, macroevolu- tion, the tree of life and COPYRIGHTEDdeep time. MATERIAL All science is either physics or stamp collecting. -
An Analysis of Anchitherine Equids Across the Eocene–Oligocene Boundary in the White River Group of the Western Great Plains
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Earth and Atmospheric Sciences, Department Atmospheric Sciences of 2010 An Analysis of Anchitherine Equids Across the Eocene–Oligocene Boundary in the White River Group of the Western Great Plains David M. Masciale University of Nebraska at Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons, Paleobiology Commons, and the Paleontology Commons Masciale, David M., "An Analysis of Anchitherine Equids Across the Eocene–Oligocene Boundary in the White River Group of the Western Great Plains" (2010). Dissertations & Theses in Earth and Atmospheric Sciences. 11. https://digitalcommons.unl.edu/geoscidiss/11 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. AN ANALYSIS OF ANCHITHERINE EQUIDS ACROSS THE EOCENE– OLIGOCENE BOUNDARY IN THE WHITE RIVER GROUP OF THE WESTERN GREAT PLAINS by David M. Masciale A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Major: Geosciences Under the Supervision of Professors Ross Secord and Robert M. Hunt, Jr. Lincoln, NE April, 2010 AN ANALYSIS OF ANCHITHERINE EQUIDS ACROSS THE EOCENE– OLIGOCENE BOUNDARY IN THE WHITE RIVER GROUP OF THE WESTERN GREAT PLAINS David M. Masciale, M.S. University of Nebraska, 2010 Advisers: Ross Secord and Robert M. -
Earliest Record of Rhinocerotoids (Mammalia: Perissodactyla) from Switzerland: Systematics and Biostratigraphy
1661-8726/09/030489-16 Swiss J. Geosci. 102 (2009) 489–504 DOI 10.1007/s00015-009-1330-4 Birkhäuser Verlag, Basel, 2009 Earliest record of rhinocerotoids (Mammalia: Perissodactyla) from Switzerland: systematics and biostratigraphy DAMIEN BECKER 1 Key words: Rhinocerotidae, Amynodontidae, Hyracodontidae, Early Oligocene, north-central Jura Molasse, Switzerland ABSTRACT Earliest rhinocerotoids from Switzerland are reviewed on the basis of dental Epiaceratherium magnum and E. aff. magnum could indicate a new speciation remains from the earliest Oligocene north-central Jura Molasse localities of within the Epiaceratherium lineage around the top of MP22. The rhinocer- Bressaucourt (MP21/22) and Kleinblauen (top MP22). The record in Bress- otoid associations of Bressaucourt with Ronzotherium – Cadurcotherium on aucourt is restricted to Ronzotherium and Cadurcotherium, representing the western side of the southernmost Rhine Graben area, and Kleinblauen Switzerland’s oldest, well-dated post-“Grande Coupure” large mammal as- with Epiaceratherium – Ronzotherium – Eggysodon on the eastern side, re- sociation, the only occurrence of Cadurcotherium, and the earliest occurrence spectively, reveal a possible environmental barrier constituted by the Early of rhinocerotoids in Switzerland. The correlation with high-resolution stra- Oligocene Rhenish sea and its eventual connection with the Perialpine sea. tigraphy of this locality permitted a dating of the fauna to ca. 32.6 Ma, less This one could have separated an arid area in central-eastern France from than a million years after the “Grande Coupure” event. The rhinocerotoids of a humid area in Switzerland and Germany. These results, combined with the Kleinblauen are represented by Epiaceratherium, Ronzotherium and Eggyso- repartition of similar rhinocerotoid associations in Western Europe, also give don.