Techniques for Virtual Palaeontology

Total Page:16

File Type:pdf, Size:1020Kb

Techniques for Virtual Palaeontology Sutton New Analytical Methods Rahman TECHNIQUES FOR Garwood in Earth and VIRTUAL PALAEONTOLOGY Environmental Science Virtual palaeontology, the use of interactive three-dimensional digital models as a supplement or alternative to physical specimens for scientific study and communication, is rapidly becoming important to advanced students and researchers. Using non-invasive techniques, the method allows the capture of large quantities of useful data without damaging the fossils being studied. Techniques for Virtual Palaeontology guides palaeontologists through the decisions involved in TECHNIQUES FOR designing a virtual palaeontology workflow and gives a comprehensive overview, providing discussions of underlying theory, applications, historical development, details of practical methodologies, and case studies. Techniques covered include physical-optical tomography (serial sectioning), focused ion beam tomography, all forms of X-ray CT, neutron tomography, magnetic resonance imaging, optical tomography, laser scanning, and photogrammetry. Visualization techniques and data/file formats are also discussed in detail. TECHNIQUES FOR Readership: All palaeontologists and students interested in three-dimensional visualization and analysis. VIRTUAL Mark Sutton is a Senior Lecturer at Imperial College, London, UK specializing in Palaeozoic invertebrate palaeobiology and in three- PALAEONTOLOGY dimensional visualization techniques. He is the primary author of the SPIERS software suite for palaeontological 3D reconstruction. VIRTUAL Imran Rahman is a Research Fellow at The University of Bristol, UK. He specializes in the origin and early evolution of echinoderms, and uses virtual palaeontology to study the form and function of fossil taxa. Russell Garwood is an 1851 Royal Commission Research Fellow based at The University of Manchester, UK. He uses X-ray techniques Mark Sutton to study fossils, primarily early terrestrial arthropods. He is the secondary author of the SPIERS software suite. PALAEONTOLOGY Imran Rahman Russell Garwood New Analytical Methods in Earth and Environmental Science Because of the plethora of analytical techniques now available, and the acceleration of technological advance, many earth scientists find it difficult to know where to turn for reliable information on the latest tools at their disposal, and may lack the expertise to assess the relative strengths or limitations of a particular technique. This new series will address these difficulties by providing accessible introductions to important new techniques, lab and field protocols, suggestions for data handling and interpretation, and useful case studies. The series represents an invaluable and trusted source of information for researchers, advanced students and applied earth scientists wishing to familiarise themselves with emerging techniques in their field. All titles in this series are available in a variety of full-colour, searchable e-book formats. Titles are also available in an enhanced e-book edition which may include additional features such as DOI linking, high resolution graphics and video. ISBN 978-1-118-59113-0 Visit www.wiley.com/wiley-blackwell e-book Chapter No.: 1 Title Name: Lebohec Comp. by: AMagimaidass Date: 08 Oct 2013 Time: 06:42:18 AM Stage: Proof Page Number: i TECHNIQUES FOR VIRTUAL PALAEONTOLOGY Chapter No.: 1 Title Name: Lebohec Comp. by: AMagimaidass Date: 22 Nov 2013 Time: 10:13:51 AM Stage: Proof Page Number: i New Analytical Methods in Earth and Environmental Science A new e-book series from Wiley-Blackwell Because of the plethora of analytical techniques now available, and the acceleration of technological advance, many earth scientists find it difficult to know where to turn for reliable information on the latest tools at their disposal, and may lack the expertise to assess the relative strengths or potential limita- tions of a particular technique. This new series addresses these difficulties, and by virtue of its comprehensive and up-to-date coverage, provides a trusted resource for researchers, advanced students and applied earth scientists w ishing to familiarise themselves with emerging techniques in their field. Authors will be encouraged to reach out beyond their immediate speci- ality to the wider earth science community, and to regularly update their contributions in the light of new developments. Written by leading international figures, the volumes in the series will typically be 75–200 pages (30,000 to 60,000 words) in length – longer than a typical review article, but shorter than a normal book. Volumes in the series will deal with: ● the elucidation and evaluation of new analytical, numerical modelling, imaging or measurement tools/techniques that are expected to have, or are already having, a major impact on the subject; ● new applications of established techniques; ● interdisciplinary applications using novel combinations of techniques. All titles in this series are available in a variety of full-colour, searchable e-book formats. Titles are also available in an enhanced e-book edition which may include additional features such as DOI linking, high resolution graphics and video. Series Editors Kurt Konhauser, University of Alberta (biogeosciences) Simon Turner, Macquarie University (magmatic geochemistry) Arjun Heimsath, Arizona State University (earth-surface processes) Peter Ryan, Middlebury College (environmental/low T geochemistry) Mark Everett, Texas A&M (applied geophysics) Chapter No.: 1 Title Name: Lebohec Comp. by: AMagimaidass Date: 22 Nov 2013 Time: 10:13:51 AM Stage: Proof Page Number: ii TECHNIQUES FOR VIRTUAL PALAEONTOLOGY MARK D. SUTTON Department of Earth Science and Engineering, Imperial College London, London, UK I mran A. RAHMAN School of Earth Sciences, University of Bristol, Wills Memorial Building, Bristol, UK R USSELL J. Garwood School of Materials/School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Manchester, UK Chapter No.: 1 Title Name: Lebohec Comp. by: AMagimaidass Date: 22 Nov 2013 Time: 11:50:40 AM Stage: Proof Page Number: iii This edition first published 2014 © 2014 by John Wiley & Sons, Ltd Registered Office John Wiley & Sons, Ltd, The Atrium, Southern Gate, Chichester, West Sussex, PO19 8SQ, UK Editorial Offices 9600 Garsington Road, Oxford, OX4 2DQ, UK The Atrium, Southern Gate, Chichester, West Sussex, PO19 8SQ, UK 111 River Street, Hoboken, NJ 07030–5774, USA For details of our global editorial offices, for customer services and for information about how to apply for permission to reuse the copyright material in this book please see our website at www.wiley.com/wiley-blackwell. The right of the author to be identified as the author of this work has been asserted in accordance with the UK Copyright, Designs and Patents Act 1988. All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, except as permitted by the UK Copyright, Designs and Patents Act 1988, without the prior permission of the publisher. Designations used by companies to distinguish their products are often claimed as trademarks. All brand names and product names used in this book are trade names, service marks, trademarks or registered trademarks of their respective owners. The publisher is not associated with any product or vendor mentioned in this book. Limit of Liability/Disclaimer of Warranty: While the publisher and author(s) have used their best efforts in preparing this book, they make no representations or warranties with respect to the accuracy or completeness of the contents of this book and specifically disclaim any implied warranties of merchantability or fitness for a particular purpose. It is sold on the understanding that the publisher is not engaged in rendering professional services and neither the publisher nor the author shall be liable for damages arising herefrom. If professional advice or other expert assistance is required, the services of a competent professional should be sought. Library of Congress Cataloging-in-Publication Data Sutton, M. D. (Mark D.), author. Techniques for virtual palaeontology / Mark D. Sutton, Imran A. Rahman, Russell J. Garwood. pages cm Includes bibliographical references and index. ISBN 978-1-118-59113-0 (cloth) 1. Paleontological modeling. 2. Virtual reality in paleontology. 3. Paleontology–Data processing. I. Rahman, Imran A., author. II. Garwood, Russell J., author. III. Title. QE721.2.M63S88 2014 560.285–dc23 2013024697 A catalogue record for this book is available from the British Library. Wiley also publishes its books in a variety of electronic formats. Some content that appears in print may not be available in electronic books. Cover image: “Ventral view of the horseshoe crab Dibasterium durgae Briggs et al. 2012, from the Silurian-aged Herefordshire Lagerstätte, England. Model reconstructed through physical-optical tomography, manual registration, virtual preparation, isosurfacing and ray-tracing, using software packages SPIERS and Blender.” Briggs, D.E.G., Siveter, Derek J., Siveter, David J., Sutton, M.D., Garwood, R.J, & Legg, D. 2012. Silurian horseshoe crab illuminates the evolution of arthropod limbs. P.N.A.S. 109, 15702–15705. Set in 10/12.5pt Minion by SPi Publisher Services, Pondicherry, India 1 2014 Chapter No.: 1 Title Name: Lebohec Comp. by: AMagimaidass Date: 22 Nov 2013 Time: 10:13:51 AM Stage: Proof Page Number: iv Contents Acknowledgements viii 1 Introduction
Recommended publications
  • Symmoriiform Sharks from the Pennsylvanian of Nebraska
    Acta Geologica Polonica, Vol. 68 (2018), No. 3, pp. 391–401 DOI: 10.1515/agp-2018-0009 Symmoriiform sharks from the Pennsylvanian of Nebraska MICHAŁ GINTER University of Warsaw, Faculty of Geology, Żwirki i Wigury 93, PL-02-089 Warsaw, Poland. E-mail: [email protected] ABSTRACT: Ginter, M. 2018. Symmoriiform sharks from the Pennsylvanian of Nebraska. Acta Geologica Polonica, 68 (3), 391–401. Warszawa. The Indian Cave Sandstone (Upper Pennsylvanian, Gzhelian) from the area of Peru, Nebraska, USA, has yielded numerous isolated chondrichthyan remains and among them teeth and dermal denticles of the Symmoriiformes Zangerl, 1981. Two tooth-based taxa were identified: a falcatid Denaea saltsmani Ginter and Hansen, 2010, and a new species of Stethacanthus Newberry, 1889, S. concavus sp. nov. In addition, there occur a few long, monocuspid tooth-like denticles, similar to those observed in Cobelodus Zangerl, 1973, probably represent- ing the head cover or the spine-brush complex. A review of the available information on the fossil record of Symmoriiformes has revealed that the group existed from the Late Devonian (Famennian) till the end of the Middle Permian (Capitanian). Key words: Symmoriiformes; Microfossils; Carboniferous; Indian Cave Sandstone; USA Midcontinent. INTRODUCTION size and shape is concerned [compare the thick me- dian cusp, almost a centimetre long, in Stethacanthus The Symmoriiformes (Symmoriida sensu Zan- neilsoni (Traquair, 1898), and the minute, 0.5 mm gerl 1981) are a group of Palaeozoic cladodont sharks wide, multicuspid, comb-like tooth of Denaea wangi sharing several common characters: relatively short Wang, Jin and Wang, 2004; Ginter et al. 2010, figs skulls, large eyes, terminal mouth, epicercal but ex- 58A–C and 61, respectively].
    [Show full text]
  • Sharks from the Middle-Late Devonian Aztec Siltstone, Southern Victoria Land, Antarctica
    Records of the Western Australian Museum 17: 287-308 (1995). Sharks from the Middle-Late Devonian Aztec Siltstone, southern Victoria Land, Antarctica John A. Longl and Gavin C. Young2 I Western Australian Museum, Francis Street, Perth, Western Australia 6000 2 Australian Geological Survey Organisation, p.a. Box 378, Canberra, A.C.T. 2601 Abstract Shark teeth representing three new taxa are described from the Middle-Late Devonian Aztec Siltstone of southern Victoria Land, Antarctica. Portalodus bradshawae gen. et sp. novo is represented by large diplodont teeth which have a base with a well-produced labial platform. It occurs in the middle to upper sections of the Aztec Siltstone. Aztecodus harmsenae gen. et sp. novo is represented by broad bicuspid teeth, wider than high, with numerous medial crenulations and twin nutritive foramina penetrating the rectangular base. It occurs in the middle sections of the Aztec Siltstone. The teeth of Anareodus statei gen. et sp. novo are characterised by having a main cusp which is more than twice as high as the second cusp, a small cusplet developed on the outer cutting edge of the main cusp, sometimes with few crenulations developed in the middle of the two cusps, and the base is strongly concave. Antarctilanma cf. prisca Young, 1982 is also recorded from the middle and upper sections of the Aztec Siltstone above the thelodont horizons and occurring with phyllolepids and Pambulaspis in the Cook Mountains section south of Mt Hughes. The chondrichthyan fauna from the Aztec Siltstone now contains at least 5 species, being the most diverse assemblage of Middle Devonian chondrichthyans (based on teeth) from one stratigraphic unit.
    [Show full text]
  • Carboniferous Formations and Faunas of Central Montana
    Carboniferous Formations and Faunas of Central Montana GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 Carboniferous Formations and Faunas of Central Montana By W. H. EASTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 A study of the stratigraphic and ecologic associa­ tions and significance offossils from the Big Snowy group of Mississippian and Pennsylvanian rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows : Eastern, William Heyden, 1916- Carboniferous formations and faunas of central Montana. Washington, U.S. Govt. Print. Off., 1961. iv, 126 p. illus., diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 348) Part of illustrative matter folded in pocket. Bibliography: p. 101-108. 1. Paleontology Montana. 2. Paleontology Carboniferous. 3. Geology, Stratigraphic Carboniferous. I. Title. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, B.C. CONTENTS Page Page Abstract-__________________________________________ 1 Faunal analysis Continued Introduction _______________________________________ 1 Faunal relations ______________________________ 22 Purposes of the study_ __________________________ 1 Long-ranging elements...__________________ 22 Organization of present work___ __________________ 3 Elements of Mississippian affinity.._________ 22 Acknowledgments--.-------.- ___________________
    [Show full text]
  • Chondrichthyan Fauna of the Frasnian–Famennian Boundary Beds in Poland
    Chondrichthyan fauna of the Frasnian–Famennian boundary beds in Poland MICHAŁ GINTER Michał Ginter. 2002. Chondrichthyan fauna of the Frasnian–Famennian boundary beds in Poland. Acta Palaeontologica Polonica 47 (2): 329–338. New chondrichthyan microremains from several Frasnian–Famennian sections in the Holy Cross Mountains and Dębnik area (Southern Poland) are investigated and compared to previous data. The reaction of different groups of chondrichthyans to environmental changes during the Kellwasser Event is analysed. Following the extinction of phoebodont sharks of Phoebodus bifurcatus group before the end of the Frasnian, only two chondrichthyan species, viz. Protacrodus vetustus Jaekel, 1921 and Stethacanthus resistens sp. nov. (possibly closely related to “Cladodus” wildungensis Jaekel, 1921), occur in the upper part of Frasnian Palmatolepis linguiformis conodont Zone and persist into the Famennian. Global cooling is considered a possible cause of the extinction of Frasnian subtropical phoe− bodonts on Laurussian margins. Key words: Chondrichthyes, Kellwasser Event, Devonian, Poland. Michał Ginter [[email protected]], Instytut Geologii Podstawowej, Uniwersytet Warszawski, Żwirki i Wigury 93, PL−02−089 Warszawa, Poland. Introduction Characteristics of the localities Chondrichthyan faunas of the late Palmatolepis linguiformis Three sections spanning the Frasnian–Famennian boundary and the Palmatolepis triangularis conodont zones on south− were sampled bed by bed (for location of most samples, see ern Laurussian margins substantially differ from those of the Racka 2000): the middle wall of the Kowala–Wola Quarry in rest of the Frasnian and Famennian. The main difference is the south−western Holy Cross Mts, south of Kielce; an artficial the absence of Phoebodus, a typical Mid− to Late Devonian trench on the eastern bank of Łagowica River, between the vil− pelagic, shelf dwelling shark (Ginter and Ivanov 1992).
    [Show full text]
  • Late Devonian and Early Carboniferous Chondrichthyans from the Fairfield Group, Canning Basin, Western Australia
    Palaeontologia Electronica palaeo-electronica.org Late Devonian and Early Carboniferous chondrichthyans from the Fairfield Group, Canning Basin, Western Australia Brett Roelofs, Milo Barham, Arthur J. Mory, and Kate Trinajstic ABSTRACT Teeth from 18 shark taxa are described from Upper Devonian to Lower Carbonif- erous strata of the Lennard Shelf, Canning Basin, Western Australia. Spot samples from shoal facies in the upper Famennian Gumhole Formation and shallow water car- bonate platform facies in the Tournaisian Laurel Formation yielded a chondrichthyan fauna including several known species, in particular Thrinacodus ferox, Cladodus thomasi, Protacrodus aequalis and Deihim mansureae. In addition, protacrodont teeth were recovered that resemble formally described, yet unnamed, teeth from Tournaisian deposits in North Gondwanan terranes. The close faunal relationships previously seen for Late Devonian chondrichthyan taxa in the Canning Basin and the margins of north- ern Gondwana are shown here to continue into the Carboniferous. However, a reduc- tion in species overlap for Tournaisian shallow water microvertebrate faunas between the Canning Basin and South China is evident, which supports previous studies docu- menting a separation of faunal and terrestrial plant communities between these regions by this time. The chondrichthyan fauna described herein is dominated by crushing type teeth similar to the shallow water chondrichthyan biofacies established for the Famennian and suggests some of these biofacies also extended into the Early Carboniferous. Brett Roelofs. Department of Applied Geology, Curtin University, GPO Box U1987 Perth, WA 6845, Australia. [email protected] Milo Barham. Department of Applied Geology, Curtin University, GPO Box U1987 Perth, WA 6845, Australia. [email protected] Arthur J.
    [Show full text]
  • American Museum Novitates
    AMERICAN MUSEUM NOVITATES Number 3954, 29 pp. June 16, 2020 A new genus of Late Cretaceous angel shark (Elasmobranchii; Squatinidae), with comments on squatinid phylogeny JOHN G. MAISEY,1 DANA J. EHRET,2 AND JOHN S.S. DENTON3 ABSTRACT Three-dimensional Late Cretaceous elasmobranch endoskeletal elements (including palato- quadrates, ceratohyals, braincase fragments, and a series of anterior vertebrae) are described from the Late Cretaceous University of Alabama Harrell Station Paleontological Site (HSPS), Dallas County, Alabama. The material is referred to the extant elasmobranch Family Squatinidae on the basis of several distinctive morphological features. It also exhibits features not shared by any modern or fossil Squatina species or the extinct Late Jurassic squatinid Pseudorhina. A new genus and species is erected, despite there being some uncertainty regarding potential synonymy with existing nominal species previously founded on isolated fossil teeth (curiously, no squatinid teeth have been docu- mented from the HSPS). A preliminary phylogenetic analysis suggests that the new genus falls on the squatinid stem, phylogenetically closer to Squatina than Pseudorhina. The craniovertebral articu- lation in the new genus exhibits features considered convergent with modern batomorphs (skates and rays), including absence of contact between the posterior basicranium and first vertebral cen- trum, and a notochordal canal which fails to reach the parachordal basicranium. Supporting evi- dence that similarities in the craniovertebral articulation of squatinoids and batomorphs are convergent rather than synapomorphic (as “hypnosqualeans”) is presented by an undescribed Early Jurassic batomorph, in which an occipital hemicentrum articulates with the first vertebral centrum as in all modern sharklike (selachimorph) elasmobranchs. The fossil suggests instead that the bato- 1 Department of Vertebrate Paleontology, American Museum of Natural History, NY.
    [Show full text]
  • Xxvi Jornadas...Qxd
    AMEGHINIANA Revista de la Asociación Paleontológica Argentina RESÚMENES TOMO 46 Número 4 BUENOS AIRES REPÚBLICA ARGENTINA 2009 Se deja constancia que el presente suplemento se halla desprovisto de validez para propósitos nomenclaturales Disclaimer: this supplement is not deemed to be valid for nomenclatural purposes El Comité Editor de la Asociación Paleontológica Argentina deja constancia que solamente se incluyen en este Suplemento los resúmenes enviados por los organizadores de las diferentes reuniones. AMEGHINIANA 46 (4) Suplemento, 2009-RESÚMENES XXIV JORNADAS ARGENTINAS DE PALEONTOLOGÍA DE VERTEBRADOS RESÚMENES 4 al 7 de mayo de 2009 Museo de Historia Natural de San Rafael (MHNSR), San Rafael, Mendoza COMISIÓN ORGANIZADORA Presidente Marcelo S. de la Fuente (MHNSR) Secretarias Analía Forasiepi (MHNSR) Juliana Sterli (MHNSR) Vocales Miriam Ayala (MHNSR) René Biglione (DGE-Mendoza) Sergio Dieguez (CNEA) Gladys García (Universidad Champagnat) Miguel Giardina (MHNSR) Adolfo Gil (MHNSR) Gustavo Neme (MHNSR) Clara Otaola (MHNSR) Nuria Sugrañes (MHNSR) Financiado por ANPCyT, CONICET y Fondo Provincial de la Cultura de la Pcia. de Mendoza. Auspiciado por Asociación Paleontológica Argentina, Museo de Historia Natural de San Rafael y Municipalidad de San Rafael (Mendoza). AMEGHINIANA 46 (4) Sumplemento, 2009-RESÚMENES 4R CONFERENCIAS Origen de la ictiofauna marina y continental de América del Sur Austral A.L. CIONE1 La ictiofauna neotropical continental es la más rica en especies del mundo. Su mayor riqueza se localiza en las áreas intertropi- cales, un paralelo de lo que sucede con otros organismos. Se calcula que pueden existir 8.000 especies de peces continentales, un cuarto de la totalidad de los conocidos en todo el mundo en ambiente marino o continental.
    [Show full text]
  • Mississippian: Osagean)
    CHONDRICHTHYAN DIVERSITY WITHIN THE BURLINGTON- KEOKUK FISH BED OF SOUTHEAST IOWA AND NORTHWEST ILLINOIS (MISSISSIPPIAN: OSAGEAN) A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science By MATTHEW MICHAEL JAMES HOENIG B.S., Hillsdale College, 2017 2019 Wright State University WRIGHT STATE UNIVERSITY GRADUATE SCHOOL Thursday, September 5th, 2019 I HEREBY RECOMMEND THAT THE THESIS PREPARED UNDER MY SUPERVISION BY Matthew Michael James Hoenig ENTITLED Chondrichthyan diversity within the Burlington-Keokuk Fish Bed of Southeast Iowa and Northwest Illinois (Mississippian: Osagean) BE ACCEPTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF Master of Science Charles N. Ciampaglio, Ph.D. Thesis Director Doyle R. Watts, Ph.D. Chair, Department of Earth & Environmental Sciences Committee on Final Examination David A. Schmidt, Ph.D. Stephen J. Jacquemin, Ph.D. Barry Milligan, Ph.D. Professor and Interim Dean of the Graduate School ABSTRACT Hoenig, Matthew Michael James. M.S. Department of Earth & Environmental Sciences, Wright State University, 2019. Chondrichthyan diversity within the Burlington-Keokuk Fish Bed of Southeast Iowa and Northwest Illinois (Mississippian: Osagean) Chondrichthyan remains occur in abundance within a thin layer of limestone at the top of the Burlington Limestone at the point of the contact with the overlying Keokuk Limestone. This layer of rock, the “Burlington-Keokuk Fish Bed,”1 is stratigraphically consistent and laterally extensive in exposures of the Burlington Limestone near its type section along the Iowa-Illinois border. Deposition of the fish bed occurred on the Burlington Continental Shelf carbonate ramp off the subtropical western coast of Laurussia during the Lower Carboniferous (Late Tournaisian; Osagean) due to a drop in sea level, although the specific mechanism(s) that concentrated the vertebrate fossils remain(s) unknown.
    [Show full text]
  • Download Curriculum Vitae
    JOHN G. MAISEY CURATOR AND PROFESSOR DIVISION OF PALEONTOLOGY HIGHEST DEGREE EARNED Ph.D. AREA OF SPECIALIZATION Morphology, phylogeny and evolution of sharks EDUCATIONAL EXPERIENCE Ph.D., University of London (University College), l974. D. Phil., University of London (University College), l970-l97l B.Sc. with Honors, University of Exeter, England, l967-l970 PREVIOUS EXPERIENCE IN DOCTORAL EDUCATION FACULTY APPOINTMENTS Adjunct Professor, Department of Biology and Doctoral faculty of the Graduate School and University Center, City University of New York, 1990 Adjunct Professor, Department of Ichthyology, University of Guelph, Ontario, 1990 Lecturer, Geology, St. Albans College, Hertfordshire, England, l976-l979 Demonstrator, Geology, University of Exeter, Devonshire, England, l973-l975 Demonstrator, Zoology Department, University College London, England, l970-l972 Lecturer, Geology, Polytechnic of North London, 1970-1972 COURSES TAUGHT Directed Reading (Jennifer Lane), City University of New York, 2004-2005 Comparative anatomy and evolution of fishes, City University of New York, 1994-1995 Lectures on the principles of cladistic analysis and biogeography, Federal University of Rio de Janeiro, 1992 Tutorial sessions in Paleoichthyology, City University of New York, 1990 Part of NYU course in Ichthyology, AMNH, Dept. of Ichthyology, 1987 Part of NYU course in Ichthyology, AMNH, Dept. of Ichthyology, 1981 Various courses in Geology, Geography, Vertebrate Zoology; St. Albans College, 1978- 1979 Geology, Paleontology; Open University tutorials, 1977-1978 Geology; Open University tutorials, 1976-1977 Vertebrate Paleontology; Dept. of Geology, University of Exeter, 1974-1975 General Paleontology; Dept. of Geology, University of Exeter, 1973-1974 Comparative Vertebrate Anatomy; Dept. Zoology & Comparative Anatomy, University College, London, 1971-1972 General Paleontology; Geology Dept., Polytechnic of North London, 1971-1972 General Paleontology; Geology Dept., Polytechnic of North London, 1970-1971 GRADUATE COMMITTEES Jennifer Lane, City University of New York, Ph.D.
    [Show full text]
  • (1929–2000) EV Popov
    Proceedings of the Zoological Institute RAS Vol. 320, No. 1, 2016, рр. 25–49 УДК 567.1/.5(01) + 597.2/.5(01) + 929Гликман AN ANNOTATED BIBLIOGRAPHY OF THE SOVIET PALAEOICHTHYOLOGIST LEONID GLICKMAN (1929–2000) E.V. Popov Saratov State University, Astrakhanskaya Str. 83, 410012 Saratov, Russia; e-mail: [email protected] ABSTRACT The paper presents a short biography and an annotated bibliography of the well-known Soviet palaeoichthyologist and evolutionary morphologist Leonid S. Glickman (1929–2000). His bibliography consists of 46 titles, including 2 monographs, 3 book chapters, 33 research papers, 4 popular papers, and 4 unpublished research reports and dissertations, devoted mainly to Cretaceous and Cenozoic elasmobranchs (principally Lamniformes). The publi- cations cover a period of time between the years 1952 and 1998. Key words: bibliography, biography, evolution, functional morphology, Glickman Leonid Sergeevich, sharks, skates, teeth АННОТИРОВАННАЯ БИБЛИОГРАФИЯ СОВЕТСКОГО ПАЛЕОИХТИОЛОГА ЛЕОНИДА СЕРГЕЕВИЧА ГЛИКМАНА (1929–2000) Е.В. Попов Саратовский государственный университет, ул. Астраханская 83, 410012 Саратов, Россия; e-mail: [email protected] РЕЗЮМЕ В статье приводится краткая биографическая справка и аннотированная библиография известного Со- ветского палеоихтиолога и эволюционного морфолога Леонида Сергеевича Гликмана (1929–2000). Библиография содержит 46 наименований, включая 2 монографии, 3 раздела в коллективных монографиях, 33 научных и 4 популярных статьи, а также 3 неопубликованных квалификационных работы и один отчет НИР, посвященные меловым и кайнозойским эласмобранхиям (в основном, ламнообразным акулам). Время издания публикаций охватывает период с 1952 по 1998 г. Ключевые слова: библиография, биография, эволюция, функциональная морфология, Гликман Леонид Сергеевич, акулы, скаты, зубы INTRODUCTION where he worked: Leningrad, Saratov and Vladivo- stok (Fig. 1). In 1939 the family left Leningrad for A short biography1.
    [Show full text]
  • Contributions to the Morphology of Cladoselache (Cladodus)
    CONTRIBUTIONS TO THE MORPHOLOGY OF CLAD0 SE LA C H E (CZadodzds) . BASHFORD DEAN, COLUMBIACOLLEGE, NEW YORK CITY. UNTILvery recent times the Morphology of Elasmobranchs has received few contributions from the study of the earlier fossil forms. It was, in fact, hardly to be expected that uncalcified shark structures should have preserved with any completeness the record of their ancient characters. Fragmentary remains on the other hand have, in many cases, led to confused and contradictory results. It was not until 1858 that accounts, in any way satisfactory, were given of the chief features of palaeozoic sharks, In this year there appeared almost simul- taneously, a description of the Carboniferous Pleuracanthus by Brongniart,' of the Lower Carboniferous Chondrenchelys and Cladodus (pectoral fin) by Traquair,Z, 147 of a Cladodont shark from the Ohio Waverly by Newberry,3 and of the pectoral fin of Xenacanthus by Fritsch.4 Subsequent papers of especial importance morphologically were contributed by Fritsch,$?6 Doderlein,'/ Smith Woodward,x, 9 Newberry,IO WiedersheimI 1 and Jaekel.Iz,I3 The sharks discussed at that time by Newberry were received from Rev. Dr. William Kepler of New London, Ohio. They had been collected at Linton, and represented the remains of about six individuals. The remarkable characters they exhibited proved in no small degree puzzling to their describer. The dentition was undoubtedly Cladodont and the name Cladodzu was retained, although it was clearly recognized that a number of genera and even families might be represented by this generalized type of dentition, and that a new genus might be assigned when more material of the type (Cladodus mirubiZis) should be found.
    [Show full text]
  • Chondrichthyans from the Devonian-Early Carboniferous of Belarus
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Kazan Federal University Digital Repository Estonian Journal of Earth Sciences 2018 vol.67 N1, pages 43-58 Chondrichthyans from the devonian-early carboniferous of belarus Kazan Federal University, 420008, Kremlevskaya 18, Kazan, Russia Abstract © 2018 Authors. Diverse remains of chondrichthyans were found in several stratigraphic levels in 18 cores of the Devonian and Lower Carboniferous of Belarus. Most of the taxa were first reported in that territory. A new species of ctenacanthiform shark, Tamiobatis elgae, is described. The internal structure of teeth of this species is reconstructed for the first time using microtomography. The distribution of chondrichthyan taxa is analysed. http://dx.doi.org/10.3176/earth.2018.03 Keywords Belarus, Chondrichthyes, Lower devonian-lower carboniferous References [1] Bonaparte, C. L. J. L. 1838. Selachorum tabula analytica. Nuovi Annali delle Scienze Naturali, 1, 195-214. [2] Cappetta, H., Duffin, C. & Zidek, J. 1993, Chondrichthyes. In The Fossil Record 2 (Benton, M. J., ed.), pp. 593- 609. [3] Chapman and Hall, London, Dean, B. 1909. Studies on fossil fishes (sharks, chimaeroids and arthrodires). Memoirs of the American Museum of Natural History, Part V, 9, 211-287. [4] Downs, J. P. & Daeschler, E. B. 2001. Variation within a large sample of Ageleodus pectinatus teeth (Chondrichthyes) from the Late Devonian of Pennsylvania, U.S.A. Journal of Vertebrate Paleontology, 21, 811- 814. [5] Eastman, C. R. 1897. Tamiobatis vetustus: a new form of fossil skate. American Journal of Science, 4, 85-90. [6] Esin, D., Ginter, M., Ivanov, A., Lebedev, O., Luksevics, E., Avkhimovich, V., Golubtsov, V.
    [Show full text]