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University of Michigan University Library
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY UNIVERSITY OF MICHIGAN VOL. XI NO.6, pp. 101-157 (12 pk., 1 map) MARCH25, 1953 TRILOBITES OF THE DEVONIAN TRAVERSE GROUP OF MICHIGAN BY ERWIN C. STUMM UNIVERSITY OF MICHIGAN PRESS ANN ARBOR CONTMBUTIONS FROM THE MUSEUM OF PALEONTOLOGY UNIVERSITY OF MICHIGAN MUSEUM OF PALEONTOLOGY Director: LEWIS B. KELLUM The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collections in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and also to individuals upon request. Correspondence should be directed to the University of Michigan Press. A list of the separate papers in Volumes II-IX will be sent upon request. VOL. I. The Stratigraphy and Fauna of the Hackberry Stage of the Upper Devonian, by C. L. Fenton and M. A. Fenton. Pages xi+260. Cloth. $2.75. VOL. 11. Fourteen papers. Pages ix+240. Cloth. $3.00. Parts sold separately in paper covers. VOL. 111. Thirteen papers. Pages viii+275. Cloth. $3.50. Parts sold separately in paper covers. VOL. IV. Eighteen papers. Pages viiif295. Cloth. $3.50. Parts sold separately in paper covers, VOL. V. Twelve papers. Pages viii+318. Cloth. $3.50. Parts sold separately in paper covers. VOL. VI. Ten papers. Pages vii+336. Paper covers. $3.00. Parts sold separately. VOLS. VII-IX. Ten numbers each, sold separately. (Continued on inside back cover) VOL. -
Joachim 8Arrande (1819) 1799-1883 Pierre Pavot (44) Et Jean-Maurice Poutiers, Attaché Au Muséum National D'histoire Naturelle De Paris
LIBRES PROPOS • Bicentenaire d'un ancien plus célèbre à Prague qu'à Paris, Joachim 8arrande (1819) 1799-1883 Pierre Pavot (44) et Jean-Maurice Poutiers, attaché au Muséum national d'histoire naturelle de Paris Prague honorera cet été le bicentenaire de la naissance de ce savant géologue par une exposition et un symposium international. E Il AOÛT 1799 naissait dans la région de Saugues CHaute-Loire) L un garçon qui s'intéressera très tôt à la nature, à la technique et aux machines. Grâce à la solide aisance de ses parents, le jeune Joachim peut poursuivre ses études dans un éta blissement renommé de Paris, le col lège Stanislas. Entré à l'École poly technique en 1819, il en sort major en 1821 puis termine sa formation aux Ponts et Chaussées en 1824. Son intérêt personnel pour les sciences naturelles le conduit à suivre des cours et conférences des plus grands naturalistes de l'époque comme Georges Cuvier, Alexandre Brongniart, Alcide d'Orbigny .. Évoluant dans la société parisienne et aussi à la cour royale, il est remar qué par le dauphin, le duc d'An goulême, pour son intelligence excep tionnelle, son ardeur au travail et sa probité. À la fin des années 1820, Charles X l'appelle à être le précep- m )UIN1UILLET 1999 LA JAUNE ET LA ROUG E TRILOBITES Depuis cette époque, la Bohême est devenue un terrain classique d'études de l'ère primaire, connu de tous les géologues et naturalistes érudits. Par ses études et ses recherches, Barrande a débordé le domaine étroit de la Bohême en établissant des cor rélations avec les autres régions du monde grâce à une documentation considérable. -
Trilobites of the Hagastrand Member (Tøyen Formation, Lowermost Arenig) from the Oslo Region, Norway. Part Il: Remaining Non-Asaphid Groups
Trilobites of the Hagastrand Member (Tøyen Formation, lowermost Arenig) from the Oslo Region, Norway. Part Il: Remaining non-asaphid groups OLE A. HOEL Hoel, O. A.: Trilobites of the Hagastrand Member (Tøyen Formation, lowermost Arenig) from the Oslo Region, Norway. Part Il: remaining non-asaphid groups. Norsk Geologisk Tidsskrift, Vol. 79, pp. 259-280. Oslo 1999. ISSN 0029-196X. This is Part Il of a two-part description of the trilobite fauna of the Hagastrand Member (Tøyen Formation) in the Oslo, Eiker Sandsvær, Modum and Mjøsa areas. In this part, the non-asaphid trilobites are described, while the asaphid species have been described previously. The history and status of the Tremadoc-Arenig Boundary problem is also reviewed, and I have found no reason to insert a Hunnebergian Series between the Tremadoc and the Arenig series, as has been suggested by some workers. Descriptions of the localities yielding this special trilobite fauna are provided. Most of the 22 trilobite species found in the Hagastrand Member also occur in Sweden. The 12 non-asaphid trilobites described herein belong to the families Metagnostidae, Shumardiidae, Remopleurididae, Nileidae, Cyclopygidae, Raphiophoridae, Alsataspididae and Pliomeridae. One new species is described; Robergiella tjemviki n. sp. Ole A. Hoel, Paleontologisk Museum, Sars gate l, N-0562 Oslo, Norway. Introduction contemporaneous platform deposits in Sweden are domi nated by a condensed limestone succession. In Norway, the The Tremadoc-Arenig Boundary interval is a crucial point Tøyen Formation is divided into two members: the lower in the evolution of several invertebrate groups, especially among the graptolites and the trilobites. In the graptolites, this change consisted most significantly in the loss of bithekae and a strong increase in diversity. -
Instituto De Geociências Revisão Sistemática E
UNIVERSIDADE DE SÃO PAULO INSTITUTO DE GEOCIÊNCIAS REVISÃO SISTEMÁTICA E PALEOBIOGEOGRÁFICA DE TRILOBITAS PHACOPIDA (HOMALONOTIDAE E CALMONIIDAE) DO DEVONIANO DAS BACIAS DO PARNAÍBA E AMAZONAS, BRASIL Felipe van Enck Meira Tese apresentada ao Programa de Pós- Graduação em Geoquímica e Geotectônica do Instituto de Geociências da Universidade de São Paulo, como parte dos requisitos para a obtenção do título de doutor. Orientadora: Prof. Dra. Juliana de Moraes Leme TESE DE DOUTORAMENTO Programa de Pós-graduação em Geoquímica e Geotectônica São Paulo 2016 “Kites rise highest against the wind - not with it.” - Winston Churchill Agradecimentos Agradeço a Deus, por sempre iluminar o caminho durante esses anos de altos e baixos do Doutorado. Agradeço a Ele também por enviar dois verdadeiros anjos da guarda à minha vida – minha esposa Angela Faleiros van Enck Meira e meu filho, Thomas Faleiros van Enck Meira. Agradeço a meus pais, José Carlos e Sylvia, e à minha irmã, Patrícia, pelo apoio durante a jornada, ainda que à distância, por vezes. Sou grato aos meus sogros, Jair e Lucia, que sempre foram como verdadeiros pais e conselheiros. À FAPESP (Processo n° 2012/07075-3), pelo suporte financeiro, sem o qual o Doutorado não seria viável. À minha orientadora, Drª. Juliana de Moraes Leme, pela orientação, discussões e esclarecimentos pertinentes ao projeto. Ao Doutorando Fabio Carbonaro e ao Dr. Renato Ghilardi (UNESP-Bauru), pela parceria e por discussões importantes na realização do trabalho. À Drª. Niède Guidon (FUMDHAM), pelo empréstimo de fósseis da região de São João Vermelho (Piauí), estudados aqui. Sou grato às seguintes pessoas, por permitirem meu acesso às instituições para visita de acervos, e por sua disponibilidade, atenção e ajuda durante minha permanência: Bushra Hussaini (AMNH), Flávia Alessandra Figueiredo, Mônica de Medina Coeli, Dr. -
W 1. Introductory. W 2. Establishment of the S~Wcession
Downloaded from http://jgslegacy.lyellcollection.org/ at University of California-San Diego on January 17, 2016 476 J o E. MA.RR AND T. ROBERTS ON THE 35. The Lowsa PAT.~OZ0IC ROCXS of the NzIs~vowaoov of ttAWR- ~ORDW~.ST. By J. E. 3~Aaa, Esq., M.A., F.G.S., Fellow of St. John's College, Cambridge, and T. ROBERTS, Esq., B.A., F.G.S., St. John's College, Cambridge. (Read June 10, 1885.) [PLATs XV.] w 1. Introductory. T~x~. country around Haverfordwest is of great interest to geologists, first, on account of the evidence fur~tished therein of the relations of the graptolite-bearing beds to the strata which are characterized by the presence of higher organisms, and secondly, from the nature of the foldings which the rocks of the district have undergone. We propose, in this communication, to devote our attention to the former of these subjects. Our work is based upon that which has been done by the Geo- logical Survey, and published in Sheet 40, ]~orizontal Sections, Nos. 1 & 2, and Mem. Geol. Survey, vol. ii. part i. Whilst fully acknowledging the great value of these publications, we think it desirable, now that our knowledge of the forms of life occurring in these rocks has been so much increased by the labours of many geologists in recent years, to attempt a more minute classifi- cation of the rocks of this district than that adopted by the Govern- ment Surveyors. In our opinion, this further description of the beds will throw considerable fight upon the character of the movements which the district has undergone. -
Available Generic Names for Trilobites
AVAILABLE GENERIC NAMES FOR TRILOBITES P.A. JELL AND J.M. ADRAIN Jell, P.A. & Adrain, J.M. 30 8 2002: Available generic names for trilobites. Memoirs of the Queensland Museum 48(2): 331-553. Brisbane. ISSN0079-8835. Aconsolidated list of available generic names introduced since the beginning of the binomial nomenclature system for trilobites is presented for the first time. Each entry is accompanied by the author and date of availability, by the name of the type species, by a lithostratigraphic or biostratigraphic and geographic reference for the type species, by a family assignment and by an age indication of the type species at the Period level (e.g. MCAM, LDEV). A second listing of these names is taxonomically arranged in families with the families listed alphabetically, higher level classification being outside the scope of this work. We also provide a list of names that have apparently been applied to trilobites but which remain nomina nuda within the ICZN definition. Peter A. Jell, Queensland Museum, PO Box 3300, South Brisbane, Queensland 4101, Australia; Jonathan M. Adrain, Department of Geoscience, 121 Trowbridge Hall, Univ- ersity of Iowa, Iowa City, Iowa 52242, USA; 1 August 2002. p Trilobites, generic names, checklist. Trilobite fossils attracted the attention of could find. This list was copied on an early spirit humans in different parts of the world from the stencil machine to some 20 or more trilobite very beginning, probably even prehistoric times. workers around the world, principally those who In the 1700s various European natural historians would author the 1959 Treatise edition. Weller began systematic study of living and fossil also drew on this compilation for his Presidential organisms including trilobites. -
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Upper Cambrian – Arenig stratigraphy and biostratigraphy in the Purmamarca area, Jujuy Province, NW Argentina Guillermo F. Aceñolaza1 and Sergio M. Nieva1 1 INSUGEO – Conicet/Facultad de Ciencias Naturales e I.M.L. Universidad Nacional de Tucumán, Miguel Lillo 205, 4000 Tucumán. E-mail: [email protected] Palabras clave: Estratigrafía. Bioestratigrafía. Ordovícico. Purmamarca. Jujuy. Argentina. Key words: Stratigraphy. Biostratigraphy. Ordovician. Purmamarca. Jujuy. Argentina. Introduction The region of Purmamarca is a classical locality for geological studies in the argentine literature. Many authors have recognized and analyzed the Ordovician strata and its paleontological heritage (eg. Keidel, 1917; Kobayashi,1936, 1937; Harrington, 1938; De Ferraris, 1940; Harrington and Leanza, 1957; Ramos et al., 1967 and Tortello, 1990). However, strata are several times sliced by longitudinal faults of submeridional trend, cropping out in narrow belts alternating with Precambrian/Cambrian, Cambrian and Mesozoic units. As long ago stated by Harrington (1957), no continuous section is displayed, recording isolated Ordovician blocks of different stratigraphic position. Several Lower Ordovician units crop out in the Purmamarca area. The Casa Colorada Formation (Uppermost Cambrian – Lower Tremadocian) is widely represented by the eastern flank of the Quebrada de Humahuaca when meeting the Quebrada de Purmamarca. The Coquena and Cieneguillas shales (Upper Tremadocian), and the Sepulturas Formation (Arenig) are nicely displayed in the tributaries of the Quebrada de Purmamarca. Finally, it is worthwhile to mention that a paleontological collection from this South American locality was given to the renowned Japanese paleontologist Teiichi Kobayashi in the first decades of the XX century (Kobayashi, 1936). Within the material was a new trilobite genus, defined by him as Jujuyaspis(after Jujuy province). -
1416 Esteve.Vp
Enrolled agnostids from Cambrian of Spain provide new insights about the mode of life in these forms JORGE ESTEVE & SAMUEL ZAMORA Enrolled agnostids have been known since the beginning of the nineteenth century but assemblages with high number of enrolled specimens are rare. There are different hypotheses about the life habits of this arthropod group and why they en- rolled. These include: a planktic or epiplanktic habit, with the rolled-up posture resulting from clapping cephalon and pygidium together, ectoparasitic habit or a sessile lifestyle, either attached to seaweeds or on the sea floor. Herein we de- scribe two new assemblages from the middle Cambrian of Purujosa (Iberian Chains, North Spain) where agnostids are minor components of the fossil assemblages but occasionally appear enrolled. The taphonomic and sedimentological data suggest that these agnostids were suddenly buried and rolled up as a response to adverse palaeoenvironmental con- ditions. Their presence with typical benthic components supports a benthic mode of life for at least some species of agnostids. • Key words: middle Cambrian, Gondwana, arthropods, behavior, Spain. ESTEVE,J.&ZAMORA, S. 2014. Enrolled agnostids from Cambrian of Spain provide new insights about the mode of life in these forms. Bulletin of Geosciences 89(2), 283–291 (7 figures). Czech Geological Survey, Prague, ISSN 1214-1119. Manuscript received February 5, 2013; accepted in revised form August 6, 2013; published online March 11, 2014; is- sued May 19, 2014. Jorge Esteve, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, No. 39 East Beijing Road, Nanjing 210008, China and University of West Bohemia, Center of Biology, Geosciences and Environment, Klatovská 51, 306 14 Pilsen, Czech Republic; [email protected] • Samuel Zamora, Department of Paleobiology, National Mu- seum of Natural History, Smithsonian Institution, Washington DC, 20013-7012, USA Agnostids were lower Paleozoic (Cambrian–Ordovician) 2011). -
001-012 Primeras Páginas
PUBLICACIONES DEL INSTITUTO GEOLÓGICO Y MINERO DE ESPAÑA Serie: CUADERNOS DEL MUSEO GEOMINERO. Nº 9 ADVANCES IN TRILOBITE RESEARCH ADVANCES IN TRILOBITE RESEARCH IN ADVANCES ADVANCES IN TRILOBITE RESEARCH IN ADVANCES planeta tierra Editors: I. Rábano, R. Gozalo and Ciencias de la Tierra para la Sociedad D. García-Bellido 9 788478 407590 MINISTERIO MINISTERIO DE CIENCIA DE CIENCIA E INNOVACIÓN E INNOVACIÓN ADVANCES IN TRILOBITE RESEARCH Editors: I. Rábano, R. Gozalo and D. García-Bellido Instituto Geológico y Minero de España Madrid, 2008 Serie: CUADERNOS DEL MUSEO GEOMINERO, Nº 9 INTERNATIONAL TRILOBITE CONFERENCE (4. 2008. Toledo) Advances in trilobite research: Fourth International Trilobite Conference, Toledo, June,16-24, 2008 / I. Rábano, R. Gozalo and D. García-Bellido, eds.- Madrid: Instituto Geológico y Minero de España, 2008. 448 pgs; ils; 24 cm .- (Cuadernos del Museo Geominero; 9) ISBN 978-84-7840-759-0 1. Fauna trilobites. 2. Congreso. I. Instituto Geológico y Minero de España, ed. II. Rábano,I., ed. III Gozalo, R., ed. IV. García-Bellido, D., ed. 562 All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage and retrieval system now known or to be invented, without permission in writing from the publisher. References to this volume: It is suggested that either of the following alternatives should be used for future bibliographic references to the whole or part of this volume: Rábano, I., Gozalo, R. and García-Bellido, D. (eds.) 2008. Advances in trilobite research. Cuadernos del Museo Geominero, 9. -
Distribution of the Middle Ordovician Copenhagen Formation and Its Trilobites in Nevada
Distribution of the Middle Ordovician Copenhagen Formation and its Trilobites in Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 749 Distribution of the Middle Ordovician Copenhagen Formation and its Trilobites in Nevada By REUBEN JAMES ROSS, JR., and FREDERICK C. SHAW GEOLOGICAL SURVEY PROFESSIONAL PAPER 749 Descriptions of Middle Ordovician trilobites belonging to 21 genera contribute to correlations between similar strata in Nevada) California) and 0 klahoma UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. lVIOR TON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 78-190301 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 70 cents (paper cover) Stock Number 2401-2109 CONTENTS Page Page Abstract ______________________________ -------------------------------------------------- 1 Descriptions of trilobites __________________________________________________ _ 14 Introduction ________________________________________________________________________ _ 1 Genus T1·iarth1·us Green, 1832 .... ------------------------------ 14 Previous investigations _____________________________________________ _ 1 Genus Carrickia Tripp, 1965 ____________________________________ _ 14 Acknowledgments-------------------------------------------------------· 1 Genus Hypodicranotus Whittington, 1952 _____________ _ 15 Geographic occurrences of the Copenhagen Genus Robergia Wiman, 1905·---------------------------------- -
Biodiversity, Distribution and Patterns of Extinction of the Last Odontopleuroid Trilobites During the Devonian (Givetian, Frasnian)
Geol. Mag. 144 (5), 2007, pp. 777–796. c 2007 Cambridge University Press 777 doi:10.1017/S0016756807003779 First published online 13 August 2007 Printed in the United Kingdom Biodiversity, distribution and patterns of extinction of the last odontopleuroid trilobites during the Devonian (Givetian, Frasnian) ∗ RAIMUND FEIST & KENNETH J. MCNAMARA† ∗Laboratoire de Paleontologie,´ Institut des Sciences de l’Evolution, Universite´ Montpellier II, Cc 062, Place E. Bataillon, 34095 Montpellier, France †Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK (Received 18 September 2006; accepted 22 February 2007) Abstract – Biostratigraphical ranges and palaeogeographical distribution of mid-Givetian to end- Frasnian odontopleurids are investigated. The discovery of Leonaspis rhenohercynica sp. nov. in mid-Givetian strata extends this genus unexpectedly up to the late Middle Devonian. New material of Radiaspis radiata (Goldfuss, 1843) and the first koneprusiine in Britain, Koneprusia? sp., are described from the famous Lummaton shell-bed, Torquay, Devon. New taxa of Koneprusia, K. serrensis, K. aboussalamae, K. brevispina,andK. sp. A and K. sp. B are defined. Ceratocephala (Leonaspis) harborti Richter & Richter, 1926, is revised and reassigned to Gondwanaspis Feist, 2002. Two new species of Gondwanaspis, G. dracula and G. spinosa, plus three others left in open nomenclature, are described from the late Frasnian of Western Australia. A further species of Gondwanaspis, G. prisca, is described from the early Frasnian of Montagne Noire. Species of Gondwanaspis are shown to possess a number of paedomorphic features. A functional analysis suggests that, unlike other odontopleurids, Gondwanaspis actively fed and rested with the same cephalic orientation. The sole odontopleurid survivors of the severe terminal mid-Givetian biocrisis (‘Taghanic Event’) belong to the koneprusiine Koneprusia in the late Givetian and Frasnian, and, of cryptogenic origin, the acidaspidine Gondwanaspis in the Frasnian. -
George P. Merrill Collection, Circa 1800-1930 and Undated
George P. Merrill Collection, circa 1800-1930 and undated Finding aid prepared by Smithsonian Institution Archives Smithsonian Institution Archives Washington, D.C. Contact us at [email protected] Table of Contents Collection Overview ........................................................................................................ 1 Administrative Information .............................................................................................. 1 Historical Note.................................................................................................................. 1 Descriptive Entry.............................................................................................................. 2 Names and Subjects ...................................................................................................... 3 Container Listing ............................................................................................................. 4 Series 1: PHOTOGRAPHS, CORRESPONDENCE AND RELATED MATERIAL CONCERNING INDIVIDUAL GEOLOGISTS AND SCIENTISTS, CIRCA 1800-1920................................................................................................................. 4 Series 2: PHOTOGRAPHS OF GROUPS OF GEOLOGISTS, SCIENTISTS AND SMITHSONIAN STAFF, CIRCA 1860-1930........................................................... 30 Series 3: PHOTOGRAPHS OF THE UNITED STATES GEOLOGICAL AND GEOGRAPHICAL SURVEY OF THE TERRITORIES (HAYDEN SURVEYS), CIRCA 1871-1877..............................................................................................................