Systematics in Palaeontology
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The Lithostratigraphy and Biostratigraphy of the Chalk Group (Upper Coniacian 1 to Upper Campanian) at Scratchell’S Bay and Alum Bay, Isle of Wight, UK
Manuscript Click here to view linked References The lithostratigraphy and biostratigraphy of the Chalk Group (Upper Coniacian 1 to Upper Campanian) at Scratchell’s Bay and Alum Bay, Isle of Wight, UK. 2 3 Peter Hopson1*, Andrew Farrant1, Ian Wilkinson1, Mark Woods1 , Sev Kender1 4 2 5 and Sofie Jehle , 6 7 1 British Geological Survey, Sir Kingsley Dunham Centre, Nottingham, NG12 8 5GG. 9 2 10 University of Tübingen, Sigwartstraße 10, 72074 Tübingen, Germany 11 12 * corresponding author [email protected] 13 14 Keywords: Cretaceous, Isle of Wight, Chalk, lithostratigraphy, biostratigraphy, 15 16 17 Abstract 18 19 The Scratchell‟s Bay and southern Alum Bay sections, in the extreme west of the Isle 20 21 of Wight on the Needles promontory, cover the stratigraphically highest Chalk Group 22 formations available in southern England. They are relatively inaccessible, other than 23 by boat, and despite being a virtually unbroken succession they have not received the 24 attention afforded to the Whitecliff GCR (Geological Conservation Review series) 25 site at the eastern extremity of the island. A detailed account of the lithostratigraphy 26 27 of the strata in Scratchell‟s Bay is presented and integrated with macro and micro 28 biostratigraphical results for each formation present. Comparisons are made with 29 earlier work to provide a comprehensive description of the Seaford Chalk, Newhaven 30 Chalk, Culver Chalk and Portsdown Chalk formations for the Needles promontory. 31 32 33 The strata described are correlated with those seen in the Culver Down Cliffs – 34 Whitecliff Bay at the eastern end of the island that form the Whitecliff GCR site. -
From the Ordovician (Darriwillian) of Morocco
Palaeogeographic implications of a new iocrinid crinoid (Disparida) from the Ordovician (Darriwillian) of Morocco Samuel Zamora1, Imran A. Rahman2 and William I. Ausich3 1 Instituto Geologico´ y Minero de Espana,˜ Zaragoza, Spain 2 School of Earth Sciences, University of Bristol, Bristol, United Kingdom 3 School of Earth Sciences, Ohio State University, Columbus, OH, United States ABSTRACT Complete, articulated crinoids from the Ordovician peri-Gondwanan margin are rare. Here, we describe a new species, Iocrinus africanus sp. nov., from the Darriwilian-age Taddrist Formation of Morocco. The anatomy of this species was studied using a combination of traditional palaeontological methods and non-destructive X-ray micro-tomography (micro-CT). This revealed critical features of the column, distal arms, and aboral cup, which were hidden in the surrounding rock and would have been inaccessible without the application of micro-CT. Iocrinus africanus sp. nov. is characterized by the presence of seven to thirteen tertibrachials, three in-line bifurcations per ray, and an anal sac that is predominantly unplated or very lightly plated. Iocrinus is a common genus in North America (Laurentia) and has also been reported from the United Kingdom (Avalonia) and Oman (middle east Gondwana). Together with Merocrinus, it represents one of the few geographically widespread crinoids during the Ordovician and serves to demonstrate that faunal exchanges between Laurentia and Gondwana occurred at this time. This study highlights the advantages of using both conventional -
The Alan-Kyr Coniacian–Campanian Section (Crimean Mountains): Biostratigraphy and Paleobiogeography Aspects V
ISSN 0145-8752, Moscow University Geology Bulletin, 2016, Vol. 71, No. 3, pp. 217–233. © Allerton Press, Inc., 2016. Original Russian Text © V.N. Benyamovskiy, L.F. Kopaevich, 2016, published in Vestnik Moskovskogo Universiteta, Seriya 4: Geologiya, 2016, No. 00000, pp. 00000–00000. The Alan-Kyr Coniacian–Campanian Section (Crimean Mountains): Biostratigraphy and Paleobiogeography Aspects V. N. Benyamovskiya and L. F. Kopaevichb aGeological Institute, Russian Academy of Sciences, Pyzhevsky per. 7, Moscow, 119017 Russia bDepartment of Geology, Moscow State University, Moscow, 119991 Russia e-mail: [email protected] Received December 8, 2015 Abstract⎯This investigation continues the study of the Alan-Kyr reference section (Central Crimea, Belogorsk Region). The zoned age difference in the stratigraphic scheme of the Upper Cretaceous in the Eastern European Platform is considered according to benthic and planktonic foraminifers, as well as radio- larians in the Alan-Kyr section. This fact can be explained based on the suggestion that stratigraphically important taxa could have appeared in Crimea several million years earlier than on the platform, where they could migrate under the great global eustatic transgression in the Early Campanian. We also considered the influence of paleobiogeographic conditions on the taxonomic composition of the zoned foraminifer com- plexes, both benthic and planktonic. Keywords: benthic and planktonic foraminifers, radiolarians, biostratigraphy, paleobiogeography, Alan-Kyr section, Crimea Mountain center, and Coniacian–Campanian DOI: 10.3103/S0145875216030042 INTRODUCTION material makes it possible to consider the important stratigraphy issues related to these two genera. This investigation continues the study of the Alan- Despite the high interest in Bolivinoides and Sten- Kyr Coniacian–Campanian section, which is located sioeina in the biostratigraphy of the Upper Santonian– near the Lechebnoe Settlement in the Belogorsk Maastrichtian, the thorough paleontological mono- Region of the Crimean Mountains (Fig. -
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https://doi.org/10.24199/j.mmv.1939.11.02 November 1939 MEM. NAT. Mus. VrcT., XI, 193Q. GRAPTOLITES OF AUSTRALIA: BIBLIOGRAPHY AND HISTORY OF RESEARCH By R. A. Keble, F.G.S. ( Palaeontologist, National 1J1usem·n, JJ:[elboiirne) and Professor TV. N. Benson, B.A., D.Sc. (University of Otago, Dunedin, New Zealcind.) The Australian graptolite fauna is probably the most complete in the world, certainly in regard to its Ordovician components, a fact clearly appreciated by McCoy. He had ready for the press descriptions and figures of most of the species afterwards described in J amcs Hall's J\fonograph published iu 1865, which may be regarded as the basis of systematic graptolite research, when he received from Hall a proof of his fignres. McCoy immediately conceded him priority and adopted his specific names. Had Hall delayed sending his proof, McCoy wonld certainly have pnblisl1ed his figures and descriptions and his name would have been just as pl'ominent in the literature of graptoliies as Hall's. Com menting on "Graptolitcs (Didymograpsus) frutieosus (Hall sp.)," l\IcCoy snys, "this is the first Victorian gmptolitc I ever smv, and, as it was then a new species, I had named it in my .MSS. after J\fr. J. A. Panton, who found it iu the soft shalcs of Bcn(Ugo, of ·which goldficld he was then "\Varden, nncl in ·whose hospitable camp I was then able to recognize the true g-cological age of the gold-bearing Rlates of the colony for the first time. �rhe same species was subsequently dis covered by Professor Hall in Canada; aud ns he kindly sent me an early proof of his illustration before publication, I of course adopted his name as above" (Prod. -
Nautiloid Shell Morphology
MEMOIR 13 Nautiloid Shell Morphology By ROUSSEAU H. FLOWER STATEBUREAUOFMINESANDMINERALRESOURCES NEWMEXICOINSTITUTEOFMININGANDTECHNOLOGY CAMPUSSTATION SOCORRO, NEWMEXICO MEMOIR 13 Nautiloid Shell Morphology By ROUSSEAU H. FLOIVER 1964 STATEBUREAUOFMINESANDMINERALRESOURCES NEWMEXICOINSTITUTEOFMININGANDTECHNOLOGY CAMPUSSTATION SOCORRO, NEWMEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS EXOFFICIO THEHONORABLEJACKM.CAMPBELL ................................ Governor of New Mexico LEONARDDELAY() ................................................... Superintendent of Public Instruction APPOINTEDMEMBERS WILLIAM G. ABBOTT ................................ ................................ ............................... Hobbs EUGENE L. COULSON, M.D ................................................................. Socorro THOMASM.CRAMER ................................ ................................ ................... Carlsbad EVA M. LARRAZOLO (Mrs. Paul F.) ................................................. Albuquerque RICHARDM.ZIMMERLY ................................ ................................ ....... Socorro Published February 1 o, 1964 For Sale by the New Mexico Bureau of Mines & Mineral Resources Campus Station, Socorro, N. Mex.—Price $2.50 Contents Page ABSTRACT ....................................................................................................................................................... 1 INTRODUCTION -
Platycrinites and Associated Crinoids from Pennsylvanian Rocks of the Sacramento Mountains, New Mexico
Platycrinites and associated crinoids from Pennsylvanian rocks of the Sacramento Mountains, New Mexico by Arthur L. Bowsher and Harrell L. Strimple CIRCULAR 197 New Mexico Bureau of Mines & Mineral Resources 1986 A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY COVER—Platycrinites nactus n.sp., see Fig. 48f for further explanation. Circular 197 New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Platycrinites and associated crinoids from Pennsylvanian rocks of the Sacramento Mountains, New Mexico by Arthur L. Bowsher1 and Harrell L. Strimplet+ 'Yates Petroleum Corporation, Artesia, New Mexico 88201 SOCORRO 1986 iii Contents ABSTRACT 5 PARULOCRINUS Moore and Plummer 15 Parulocrinus globatus n.sp. 15 INTRODUCTION 5 ERISOCRINUS Meek and Worthen 16 GENERAL 5 Erisocrinus typus Meek and Worthen 16 LOCALITIES AND STRATIGRAPHY 6 Erisocrinus aff. erectus Moore and Plummer 17 PLATYCRINITIDS AND INCOMPLETENESS OF THE Erisocrinus sp. 17 GEOLOGIC RECORD 7 ENDELOCRINUS Moore and Plummer 17 SYSTEMATIC DESCRIPTIONS 10 Endelocrinus bifidus Moore and Plummer 17 PLATYCRINITES Miller 10 Endelocrinus perasper n.sp. 17 Platycrinites nactus n.sp. 10 SCIADIOCRINUS Moore and Plummer 18 EXSULACRINUS n.gen. 12 Sciadiocrinus aff. harrisae Moore and Plummer 18 Exsulacrinus alleni n.sp. 12 STENOPECRINUS Strimple 18 LECYTHIOCRINUS White 13 Stenopecrinus glaber n.sp. 18 Lecythiocrinus sacculus n.sp. 13 PERIMESTOCRINUS Moore and Plummer 19 LAUDONOCRINUS Moore and Plummer 14 Perimestocrinus sp. indet. 19 Laudonocrinus -
A Late Oligocene Or Earliest Miocene Molluscan Fauna from Sitkinak Island, Alaska
A Late Oligocene or Earliest Miocene Molluscan Fauna From Sitkinak Island, Alaska By RICHARD C. ALLISON and LOUIE MARINCOVICH, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1233 Describes the late Oligocene or earliest Miocene molluscan fauna from the Narrow Cape Formation on Sitkinak Island, noting the mixture of Asiatic, North American, and endemic high-latitude North Pacific taxa. UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1981 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, &cretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Catal ogi ng in Pub1 ication Data A1 1i son, Richard C., 1935- A late Oligocene or earliest Miocene molluscan fauna from Sitki nak Is1and, A1 aska. ( Geological Survey Professional Paper ; 1233) Bibl iography: p. 9-10. Supt. of Doc. no.: I 19.16:1233 1. Moll usks, Fossil --A1 aska--Si tkinak I sl and. 2. Pal eontol ogy--01 igocene . 3. Pal eontol ogy--Mi ocene . I. Marincovich, Louie. 11. Title. 111. Series. QE801. A44 564' .09798' 4 81-607925 AACR2 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Introduction Faunal composition Age and correlation .................................................................................................................................. Relation to the type Narrow Cape Formation of Kodiak Island Paleoecology ................................................................................................................................................ Water depth Water temperature -
Zwei Miocaene Arten Von Aturia (Nautilaceae)
Zwei miocaene Arten von Aturia (Nautilaceae) Autor(en): Jung, Peter Objekttyp: Article Zeitschrift: Eclogae Geologicae Helvetiae Band (Jahr): 59 (1966) Heft 1 PDF erstellt am: 29.09.2021 Persistenter Link: http://doi.org/10.5169/seals-163385 Nutzungsbedingungen Die ETH-Bibliothek ist Anbieterin der digitalisierten Zeitschriften. Sie besitzt keine Urheberrechte an den Inhalten der Zeitschriften. Die Rechte liegen in der Regel bei den Herausgebern. Die auf der Plattform e-periodica veröffentlichten Dokumente stehen für nicht-kommerzielle Zwecke in Lehre und Forschung sowie für die private Nutzung frei zur Verfügung. Einzelne Dateien oder Ausdrucke aus diesem Angebot können zusammen mit diesen Nutzungsbedingungen und den korrekten Herkunftsbezeichnungen weitergegeben werden. Das Veröffentlichen von Bildern in Print- und Online-Publikationen ist nur mit vorheriger Genehmigung der Rechteinhaber erlaubt. Die systematische Speicherung von Teilen des elektronischen Angebots auf anderen Servern bedarf ebenfalls des schriftlichen Einverständnisses der Rechteinhaber. Haftungsausschluss Alle Angaben erfolgen ohne Gewähr für Vollständigkeit oder Richtigkeit. Es wird keine Haftung übernommen für Schäden durch die Verwendung von Informationen aus diesem Online-Angebot oder durch das Fehlen von Informationen. Dies gilt auch für Inhalte Dritter, die über dieses Angebot zugänglich sind. Ein Dienst der ETH-Bibliothek ETH Zürich, Rämistrasse 101, 8092 Zürich, Schweiz, www.library.ethz.ch http://www.e-periodica.ch Zwei miocaene Arten von Atavia (Nautilaceae) von Peter Jung (Basel)1) Mit 1 Textfigur und 2 Tafeln ABSTRACT .A neotype of Aturia aturi (Basterot) is designated and figured. Several Miocene species of Aturia from Northern South America, Japan and Australia are believed to be synonyms either of the European A. aturi or the Middle .American A. -
Shorter Contributions to the Stratigraphy and Geochronology of Upper Cretaceous Rocks in the 2 > C F Western Interior of the United States
/foe. Depositor. u > APR 06 1995 n A il LIBRARIES. Shorter Contributions to the Stratigraphy and Geochronology of Upper Cretaceous Rocks in the 2 > C f Western Interior of the United States o I U.S. GEOLOGICAL SURVEY BULLETIN 2113 1-4 OHIO STATE UNIVERSITY LIBRARIES Shorter Contributions to the Stratigraphy and Geochronology of Upper Cretaceous Rocks in the Western Interior of the United States A. Conglomerate Facies and Contact Relationships of the Upper Cretaceous Upper Part of the Frontier Formation and Lower Part of the Beaverhead Group, Lima Peaks Area, Southwestern Montana and Southeastern Idaho By T.S. Dyman, J.C. Haley, and W.J. Perry, Jr. B. U-Pb Ages of Volcanogenic Zircon from Porcellanite Beds in the Vaughn Member of the Mid-Cretaceous Blackleaf Formation, Southwestern Montana By R.E. Zartman, T.S. Dyman, R.G. Tysdal, and R.C. Pearson C. Occurrences of the Free-Swimming Upper Cretaceous Crinoids Uintacrinus and Marsupites in the Western Interior of the United States By William A. Cobban , . - U.S. GEOLOGICAL SURVEY BULLETIN 2113 This volume is published as chapters A-C. These chapters are not available separately UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1995 8 /MO C.2- U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director Published in the Central Region, Denver, Colorado Manuscript approved for publication August 9, 1994 Edited by Judith Stoeser Graphics by Wayne Hawkins Type composed by Wayne Hawkins For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, GO 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. -
What Is a Species, and What Is Not? Ernst Mayr Philosophy of Science
What Is a Species, and What Is Not? Ernst Mayr Philosophy of Science, Vol. 63, No. 2. (Jun., 1996), pp. 262-277. Stable URL: http://links.jstor.org/sici?sici=0031-8248%28199606%2963%3A2%3C262%3AWIASAW%3E2.0.CO%3B2-H Philosophy of Science is currently published by The University of Chicago Press. Your use of the JSTOR archive indicates your acceptance of JSTOR's Terms and Conditions of Use, available at http://www.jstor.org/about/terms.html. JSTOR's Terms and Conditions of Use provides, in part, that unless you have obtained prior permission, you may not download an entire issue of a journal or multiple copies of articles, and you may use content in the JSTOR archive only for your personal, non-commercial use. Please contact the publisher regarding any further use of this work. Publisher contact information may be obtained at http://www.jstor.org/journals/ucpress.html. Each copy of any part of a JSTOR transmission must contain the same copyright notice that appears on the screen or printed page of such transmission. The JSTOR Archive is a trusted digital repository providing for long-term preservation and access to leading academic journals and scholarly literature from around the world. The Archive is supported by libraries, scholarly societies, publishers, and foundations. It is an initiative of JSTOR, a not-for-profit organization with a mission to help the scholarly community take advantage of advances in technology. For more information regarding JSTOR, please contact [email protected]. http://www.jstor.org Tue Aug 21 14:59:32 2007 WHAT IS A SPECIES, AND WHAT IS NOT?" ERNST MAYRT I analyze a number of widespread misconceptions concerning species. -
The Great Ordovician Radiation of Marine Life: Examples from South China
Available online at www.sciencedirect.com Progress in Natural Science 18 (2008) 1–12 Review The great Ordovician radiation of marine life: Examples from South China Renbin Zhan a,*, Jisuo Jin b, Yuandong Zhang a, Wenwei Yuan a a State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China b Department of Earth Sciences, University of Western Ontario, London Ont., Canada N6A 5B7 Received 14 March 2007; received in revised form 23 July 2007; accepted 27 July 2007 Abstract The Ordovician radiation is the earliest and most important biodiversification event in the evolution of the Paleozoic Evolutionary Fauna (PEF), when the basic framework of PEF was established. The radiation underwent a gradual, protracted process spanning more than 40 million years and was marked by several diversity maxima of the PEF. Case studies conducted on the Upper Yangtze Platform (South China Palaeoplate) showed that the Ordovician radiation was characterized by drastic increases in a- and b-diversity in various groups of organisms. During the radiation, brachiopods, trilobites, and graptolites of the PEF became more diverse to dominate over the Cambrian Evolutionary Fauna (CEF) in all marine environments. At either global or regional scales, however, the Ordovician radiation was highly heterogeneous in time and space, and the rate and pattern of radiation exhibited by different major fossil groups were also variable. Ó 2007 National Natural Science Foundation of China and Chinese Academy of Sciences. Published by Elsevier Limited and Science in China Press. All rights reserved. Keywords: Ordovician radiation; Paleozoic Evolutionary Fauna; a-diversity; b-diversity; Upper Yangtze Platform 1. -
Paleontology and Stratigraphy of Eocene Rocks at Pulali Point, Jefferson County, Eastern Olympic Peninsula, Washington
PALEONTOLOGY AND STRATIGRAPHY OF EOCENE ROCKS AT PULALI POINT, JEFFERSON COUNTY, EASTERN OLYMPIC PENINSULA, WASHINGTON by RICHARD L. SQUIRES, JAMES L. GOEDERT, and KEITH L. KALER WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES REPORT OF INVESTIGATIONS 31 1992 ., WASHINGTON STATE DEPARTMENT OF Natural Resources Brian Boyle • Commhstoner of Public Lands An Steo_r0$ - Superv1sor Division ol Geology and Earth Resources Raymond Lcmnanls. State Geologlsl PALEONTOLOGY AND STRATIGRAPHY OF EOCENE ROCKS AT PULALI POINT, JEFFERSON COUNTY, EASTERN OLYMPIC PENINSULA, WASHINGTON by RICHARD L. SQUIRES, JAMES L. GOEDERT, AND KEITH L. KALER WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES REPORT OF INVESTIGATIONS 31 1992 W>.SHING'TON STAT1r OEPARTMDIT or Natural Resources 8ncll) Bov,. · COmmmioner ot Pu!xk: tancb M $i.atni; S\lp$1'WOJ' DtY!llcn 01 Gtology ahCS £artti ~ Raymond l.mlMn.:I ~Geologist Cover: From left, ?Falsifusus marysvillensis; Pachycrommium clarki; large bivalve, Veneri cardia hornii s.s.; Delectopecten cf. D. vancouverensis sanjuanensis; Turritella uvasana hendoni. These specimens are shown at 150 percent of the dimensions on Plates 1 and 3. Use of trade, product, or firm names in this report is for descriptive purposes only and does not consitute endorsement by the Washington Division of Geology and Earth Resources. This report is available from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources P.O. Box 47007 Olympia, WA 98504-7007 Price $ 1.85 Tax (Stale residenl.t only) .15 Total $ 2.00 Mail orders must be prepaid; please add $1.00 to each order for postage and handling. Make checks payable to the Department of Natural Resources.