International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution"

Total Page:16

File Type:pdf, Size:1020Kb

International Geological Correlation Programme. Project 591 International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution". Proceedings of the 3rd IGCP 591 Annual Meeting : Lund, Sweden, 9–19 June 2013 Lindskog, Anders; Mehlqvist, Kristina 2013 Link to publication Citation for published version (APA): Lindskog, A., & Mehlqvist, K. (Eds.) (2013). International Geological Correlation Programme. Project 591 "The Early to Middle Paleozoic Revolution". Proceedings of the 3rd IGCP 591 Annual Meeting : Lund, Sweden, 9–19 June 2013. (International Geological Correlation Programme, UNESCO; Vol. 3). Department of Geology, Lund University. Total number of authors: 2 General rights Unless other specific re-use rights are stated the following general rights apply: Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal Read more about Creative commons licenses: https://creativecommons.org/licenses/ Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. LUND UNIVERSITY PO Box 117 221 00 Lund +46 46-222 00 00 ANDERS LINDSKOG | KRISTINA MEHLQVIST Printed by Media-Tryck, Lund 2013 Proceedings of the 3rd IGCP 591 Annual Meeting Proceedings of the 3 Lund, Sweden, 9–19 June 2013 EDITED BY ANDERS LINDSKOG | KRISTINA MEHLQVIST DEPARTMENT OF GEOLOGY | LUND UNIVERSITY The abstracts within this volume were presented at the 3rd IGCP 591 Annual rd Meeting, which was held in Lund, Sweden, in June 2013. This meeting was Annual IGCP 591 Meeting co-arranged with the International Subcommission on Cambrian Stratigraphy (ISCS), the International Subcommission on Ordovician Stratigraphy (ISOS) and the International Subcommission on Silurian Stratigraphy (ISSS). The formal theme of the meeting was ‘Early Palaeozoic Global Change’. ‒ Lund, Sweden, 9–19 June 2013 Lund, Sweden, June 9–19 2013 ISBN 978-91-86746-87-2 9 789186 746872 LUND UNIVERSITY Department of Geology Sölvegatan 12 SE-223 62 Lund, Sweden ISBN: 978-91-86746-87-2 Proceedings of the 3rd IGCP 591 Annual Meeting Lund, Sweden, 9–19 June 2013 Edited by Anders Lindskog and Kristina Mehlqvist 1 Suggested reference format Lindskog, A. & Mehlqvist, K., 2013: Proceedings of the 3rd IGCP 591 Annual Meeting – Lund, Sweden, 9–19 June 2013. Lund University. 368 pp. Hinnov, L.A., 2013: Prospects for a Paleozoic Astronomical Time Scale. In A. Lind- skog & K. Mehlqvist (eds.): Proceedings of the 3rd IGCP 591 Annual Meeting – Lund, Sweden, 9–19 June 2013, 19–20. Lund University. Department of Geology Lund University Sölvegatan 12 SE-223 62 Lund Sweden http://www.geol.lu.se http://www.igcp591.org ISBN: 978-91-86746-87-2 En del av Förpacknings- och Tidningsinsamlingen (FTI) 2 Foreword and acknowledgements This abstract volume has been prepared for the 3rd annual meeting of the IUGS/UNESCO International Geoscience Programme Project 591 The Early to Middle Palaeozoic Revolution. The meeting was hosted by the Department of Geology, Lund University, in June 9–19 2013 and followed the successful annual meetings held in Madrid/Ludlow (2011) and Cincinnati (2012). The Lund conference was arranged jointly with the annual meetings of the Cambrian, Ordovician and Silurian subcommissions on stratigraphy, and included a post-conference excursion to key geological localities in Skåne, Västergötland and the Oslo Region. The conference was a focus for cutting-edge research in Lower and Middle Palaeozoic geology and palaeontology, and the presentations covered a wide range of topics from morphology and taxonomy of various fossil groups through advances in geochemistry and stratigraphy to biogeography, palaeoecology and palaeoclimatology. We would like to express our sincere gratitude to Anders Lindskog and Kristina Mehlqvist for their meticulous editing of the meeting proceedings. We are also grateful for valuable input from the organization and scientific committee associated with the meeting. We acknowledge financial support from the Swedish Research Council (grant D0013001 to MC), the Geological Survey of Sweden, the Geological Society of Sweden, the Department of Geology at Lund University, and the municipality of Lund. Lund on 8 May 2013 Mikael Calner (meeting chair) Oliver Lehnert (vice chair) Per Ahlberg 3 4 Contents Keynote: Prospects for a Paleozoic Astronomical Time Scale 19 LINDA A. HINNOV Keynote: Marine biodiversity dynamics and reef evolution in the Early Paleozoic 21 WOLFGANG KIESSLING The risk of misleading eustatic and ‘epeirogenic’ processes in the correlation of the Cambrian Series 2–3 boundary interval in rift and drift (passive margin) basins 23 J. JAVIER ÁLVARO The nature of Ordovician limestone–mudstone alternations in the Oslo-Asker area (Norway): Primary or diagenetic rhythms? 25 CHLOÉ AMBERG, TIM COLLART, WOUT SALENBIEN, THIJS R. A. VANDENBROUCKE, LISA M. EGGER3, AXEL MUNNECKE, ARNE T. NIELSEN, ØYVIND HAMMER AND JACQUES VERNIERS Wenlock on the northeastern margin of the European platform 27 ANNA I. ANTOSHKINA Placing Upper Ordovician “butter shale” Lagerstätten within a sequence stratigraphic framework 29 CHRISTOPHER D. AUCOIN, CARLTON BRETT, THOMAS MALGIERI AND JAMES THOMKA 13 The Ccarb curve from the Green Point succession in western Newfoundland, Canada and correlation of the GSSP section of the Cambrian–Ordovician boundary 31 KAREM AZMY, SVEND STOUGE, GABRIELLA BAGNOLI AND UWE BRAND The early Rhuddanian survival interval of the Ordovician/Silurian extinction in the Central Oslo Region 34 B. GUDVEIG BAARLI “Cedaria” woosteri and the Cedaria Zone (Cambrian: Guzhangian) of Laurentia 37 LOREN E. BABCOCK AND MARK T. BARANOSKI Palynology and sedimentology of the Upper Ordovician–lowermost Llandovery in the Röstånga-1 core, southern Sweden 39 AHMED S. BADAWY, PER AHLBERG, MIKAEL CALNER, KRISTINA MEHLQVIST AND VIVI VAJDA New mid-Cambrian palaeoscolecid sclerites of Hadimopanella oezgueli from the Cantabrian Mountains, northern Spain 42 TANIA BARRAGÁN, JORGE ESTEVE, DIEGO C. GARCÍA-BELLIDO, SAMUEL ZAMORA AND J. JAVIER ÁLVARO1 5 Chitinozoan biostratigraphy in the Haljala Regional Stage, Upper Ordovician: A new high-resolution approach from NE Estonia 45 GARMEN BAUERT, JAAK NÕLVAK AND HEIKKI BAUERT Depositional environments of Ordovician and Silurian sediments of the Siljan impact structure (Sweden) – insights from organic geochemistry 47 ULRICH BERNER, OLIVER LEHNERT AND GUIDO MEINHOLD Middle Ordovician cephalopods from the Abarsaj area, northern Iran 50 OLGA K. BOGOLEPOVA, BJÖRN KRÖGER, MOSTAFA FALAHATGAR AND MOJABA JAVIDAN The first Silurian chitinozoans from Severnaya Zemlya, Arctic Russia 51 OLGA K. BOGOLEPOVA, FLORENTIN PARIS AND ALEXANDER P. GUBANOV A reexamination of the contributions of biotope and geographic range to extinction risk in Ordovician graptolites 52 JAMES T. BOYLE, H. DAVID SHEETS, SHUANG-YE WU, DANIEL GOLDMAN, MICHAEL J. MELCHIN, ROGER A. COOPER, PETER M. SADLER AND CHARLES E. MITCHELL Comparative facies and carbon isotope analysis of the Sheinwoodian succession in the western Baltic and eastern North America: Evidence for a composite Ireviken Event 54 CARLTON BRETT, PATRICK MCLAUGHLIN AND POUL EMSBO A 13C composite standard for the Ordovician of Sweden based on the Tingskullen (Öland) and Borenshult (Östergötland) cores 56 MIKAEL CALNER, OLIVER LEHNERT AND MICHAEL M. JOACHIMSKI First evidence of unmineralized and non-cuticular organisms in the Cambrian ‘Orsten’ assemblages of the Alum Shale Formation of Sweden 58 CHRISTOPHER CASTELLANI, ANDREAS MAAS, JOACHIM T. HAUG, CAROLIN HAUG AND DIETER WALOSZEK Re-appraisal of the faunal diversity of the ‘Orsten’ assemblages of Sweden – new insight into the late Cambrian Alum Shale ecosystem 60 CHRISTOPHER CASTELLANI, ANDREAS MAAS, JOACHIM T. HAUG AND DIETER WALOSZEK Temporal and spatial distribution of the Wufeng black shales (Upper Ordovician) in South China 62 QING CHEN, JUNXUAN FAN, MICHAEL J. MELCHIN AND LINNA ZHANG The Lower Palaeozoic palaeogeography of Gondwana 63 L. ROBIN M. COCKS AND TROND H. TORSVIK A draboviid association from Portugal: Palaeoecological and palaeogeographical significance 65 JORGE COLMENAR, ARTUR A. SÁ AND NUNO VAZ Muscles versus environment: Morphofunctional analysis of the brachiopod genus Svobodaina 67 JORGE COLMENAR, DAVID A. T. HARPER AND ENRIQUE VILLAS Revised conodont biostratigraphy of the Silurian of Cellon, Carnic Alps 69 CARLO CORRADINI, MARIA G. CORRIGA AND PEEP MÄNNIK 6 Upper Silurian and Lower Devonian conodonts and crinoids from the scyphocrinoid beds of southeastern Morocco 71 MARIA G. CORRIGA, CARLO CORRADINI, REIMUND HAUDE AND OTTO H. WALLISER(†) Rapid geochemical change in Silurian oceans: Implications for global 13C and 87Sr/86Sr systematics 73 BRADLEY D. CRAMER, MARK D. SCHMITZ, WARREN D. HUFF, STIG M. BERGSTRÖM AND DENNIS R. KOLATA A complete record of the ‘Lower’ Cambrian–Middle Ordovician succession of Öland, southern Sweden, based on the Tingskullen core 74 PETER DAHLQVIST, MIKAEL CALNER, OLIVER LEHNERT AND PER AHLBERG Latitudinal
Recommended publications
  • A Probable Case of Heterochrony in the Solutan
    A probable case of heterochrony in the solutan Dendrocystites Barrande, 1887 (Echinodermata: Blastozoa) from the Upper Ordovician of the Prague Basin (Czech Republic) and a revision of the family Dendrocystitidae Bassler, 1938 FLEUR NOAILLES, BERTRAND LEFEBVRE & LIBOR KAIÈKA The morphology of the Late Ordovician solutan Dendrocystites is reevaluated based on more than 300 specimens from the Letná and Zahořany formations (Prague Basin, Czech Republic). This genus is reported for the first time from the Bohdalec Formation, and its presence is confirmed in the Vinice Formation. The morphology of all specimens of the stratigraphically older species D. barrandei (Sandbian) is identical to that of small to medium-size individuals of D. sedgwicki (Katian). Distinctive characters of D. sedgwicki occur only in the largest specimens, and are all size-related (more asymmetrical thecal outlines, stronger ornamentation, rosetting pattern of thecal plates, proliferation of platelets in the proxistele). Consequently, the transition from D. barrandei to D. sedgwicki is interpreted as the result of heterochronic processes, with the largest individuals of D. sedgwicki displaying hyperadult morphologies (hyper- morphosis). Dendrocystites is locally abundant in both the Letná and Zahořany formations, but extremely rare in the deeper deposits of the Vinice and Bohdalec formations. This pattern coincides closely with first order fluctuations of the sea-level in the Prague Basin. The life orientation and implied feeding strategy of Dendrocystites and other solutans are both critically discussed. Several independent lines of evidence suggest that solutans were more likely detritus-feeders. Finally, it is proposed that two morphologically distinct patterns of dististele organization were elaborated independently from the polyplated, undifferentiated stalk-like appendage of Coleicarpus (plesiomorphic condition).
    [Show full text]
  • 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.
    [Show full text]
  • Proceedings of the Indiana Academy of Science 1919, 35:261-340
    Notes on the History of the Paleontological Collection, Department of Geology, Indiana University Alan Stanley Horowitz Department of Geology, Indiana University Bloomington, Indiana 47405 Introduction In the past, paleontologic papers, especially those printed prior to 1930, com- monly did not indicate the repository of the collections on which the published record was based. Workers generally assume the collections reside at the institution to which the author was associated as either student or faculty. Some early workers were not associated with any academic institution, and early collections have been scattered or destroyed. Because inquiries are made frequently to Indiana University concerning both the University and Indiana State Geological Survey collections, this paper provides some general information on earlier collections insofar as is presently known. According to Wylie (36), the records of Indiana University prior to 1883 were largely destroyed by fire. Wylie (36:31) quoted statements concerning geological col- lections from as early as 1852 in legislative acts affecting the University, e.g., "The Lecturers were also to make geological examinations, and collect mineralogical specimens for the cabinet by volunteer donations." No attempt has been made to reconstruct possible paleontological collections, other than the Owen collection, based on any ex- tant University catalogues or Reports of the President of Indiana University published prior to 1883, and I assume that any geological collections or catalogues prior to this date were lost in the 1883 fire reported by Wylie (36:83). The Owen Collection Our knowledge of the Indiana University Department of Geology (IUB) paleon- tological collections begins with the collection of David Dale Owen.
    [Show full text]
  • Reinterpretation of the Enigmatic Ordovician Genus Bolboporites (Echinodermata)
    Reinterpretation of the enigmatic Ordovician genus Bolboporites (Echinodermata). Emeric Gillet, Bertrand Lefebvre, Véronique Gardien, Emilie Steimetz, Christophe Durlet, Frédéric Marin To cite this version: Emeric Gillet, Bertrand Lefebvre, Véronique Gardien, Emilie Steimetz, Christophe Durlet, et al.. Reinterpretation of the enigmatic Ordovician genus Bolboporites (Echinodermata).. Zoosymposia, Magnolia Press, 2019, 15 (1), pp.44-70. 10.11646/zoosymposia.15.1.7. hal-02333918 HAL Id: hal-02333918 https://hal.archives-ouvertes.fr/hal-02333918 Submitted on 13 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Reinterpretation of the Enigmatic Ordovician Genus Bolboporites 2 (Echinodermata) 3 4 EMERIC GILLET1, BERTRAND LEFEBVRE1,3, VERONIQUE GARDIEN1, EMILIE 5 STEIMETZ2, CHRISTOPHE DURLET2 & FREDERIC MARIN2 6 7 1 Université de Lyon, UCBL, ENSL, CNRS, UMR 5276 LGL-TPE, 2 rue Raphaël Dubois, F- 8 69622 Villeurbanne, France 9 2 Université de Bourgogne - Franche Comté, CNRS, UMR 6282 Biogéosciences, 6 boulevard 10 Gabriel, F-2100 Dijon, France 11 3 Corresponding author, E-mail: [email protected] 12 13 Abstract 14 Bolboporites is an enigmatic Ordovician cone-shaped fossil, the precise nature and systematic affinities of 15 which have been controversial over almost two centuries.
    [Show full text]
  • The Cambrian Substrate Revolution and the Early Evolution of Attachment in MARK Suspension-Feeding Echinoderms
    Earth-Science Reviews 171 (2017) 478–491 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev The Cambrian Substrate Revolution and the early evolution of attachment in MARK suspension-feeding echinoderms ⁎ Samuel Zamoraa,b, , Bradley Delinec, J. Javier Álvarod, Imran A. Rahmane a Instituto Geológico y Minero de España, C/Manuel Lasala, 44, 9B, Zaragoza 50006, Spain b Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington DC 20013-7012, USA c University of West Georgia, Carrollton, GA, USA d Instituto de Geociencias (CSIC-UCM), c/José Antonio Novais 12, 28040 Madrid, Spain e Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PW, UK ARTICLE INFO ABSTRACT Keywords: The Cambrian, characterized by the global appearance of diverse biomineralized metazoans in the fossil record Palaeoecology for the first time, represents a pivotal point in the history of life. This period also documents a major change in Evolution the nature of the sea floor: Neoproterozoic-type substrates stabilized by microbial mats were replaced by un- fl Sea oor consolidated soft substrates with a well-developed mixed layer. The effect of this transition on the ecology and Attachment evolution of benthic metazoans is termed the Cambrian Substrate Revolution (CSR), and this is thought to have impacted greatly on early suspension-feeding echinoderms in particular. According to this paradigm, most echinoderms rested directly on non-bioturbated soft substrates as sediment attachers and stickers during the Cambrian Epoch 2. As the substrates became increasingly disturbed by burrowing, forming a progressively thickening mixed layer, echinoderms developed new strategies for attaching to firm and hard substrates.
    [Show full text]
  • BIASES in INTERPRETATION of the FOSSIL RECORD of CONODONTS by MARK A
    [Special Papers in Palaeontology, 73, 2005, pp. 7–25] BETWEEN DEATH AND DATA: BIASES IN INTERPRETATION OF THE FOSSIL RECORD OF CONODONTS by MARK A. PURNELL* and PHILIP C. J. DONOGHUE *Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK; e-mail: [email protected] Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK; e-mail: [email protected] Abstract: The fossil record of conodonts may be among and standing generic diversity. Analysis of epoch ⁄ stage-level the best of any group of organisms, but it is biased nonethe- data for the Ordovician–Devonian interval suggests that less. Pre- and syndepositional biases, including predation there is generally no correspondence between research effort and scavenging of carcasses, current activity, reworking and and generic diversity, and more research is required to bioturbation, cause loss, redistribution and breakage of ele- determine whether this indicates that sampling of the cono- ments. These biases may be exacerbated by the way in which dont record has reached a level of maturity where few genera rocks are collected and treated in the laboratory to extract remain to be discovered. One area of long-standing interest elements. As is the case for all fossils, intervals for which in potential biases and the conodont record concerns the there is no rock record cause inevitable gaps in the strati- pattern of recovery of different components of the skeleton graphic distribution of conodonts, and unpreserved environ- through time. We have found no evidence that the increas- ments lead to further impoverishment of the recorded ing abundance of P elements relative to S and M elements spatial and temporal distributions of taxa.
    [Show full text]
  • Guidebook for Field Trip to Precambrian-Cam8ri An
    GUIDEBOOK FOR FIELD TRIP TO PRECAMBRIAN-CAM8RI AN SUCCESSION WHITE-INYO MOUNTAINS, CALIFORNIA By C. A. Nelson and J. Wyatt Durham Thursday-Sunday, November 17-20, 1966 CONTENTS .°age General Introduction 1 Road log and trip guide . 1 Figure 1. - Columnar section, following page, .... 1 Figure 2. - Reed Flat map, following page ...... 5 Figure 3. - Cedar Flat map, following page 12 Fossil Plates, following page ... 15 General Index map - "The Bristlecone Pine Recreation Area," USFS unbound Geologic Map of the Blanco Mountain Quadrangle, Inyo and Mono Counties, California, USGS GQ-529 unbound GENERAL INTRODUCTION In addition to the Precambrian and Cambrian strata to be seen, the White-Inyo region and its environs affords a wide variety of geo- logic features. Although we will concentrate on the principal objectives of the trip, we will have the opportunity to observe many features of the structure, geomorpnology, and Cenozoic history of the region as well. Travel will be by bus from San Francisco to Bishop, California on Thursday, November 17. For this segment of the trip, and the re- turn to San Francisco from Bishop, no guidebook has been prepared. We are fortunate, however, to have Mr. Bennie Troxel of the Cali- fornia Division of Mines and Geology with us.. Together we will try to provide you with some of the highlights of the trans-Sierran route. Field gear, including sturdy shoes and warm clothing is essential. Stops at the higher elevations are likely to be cold ones. As is true of all too many field trips, especially those using bus transportation, many of the best localities for collecting Cambrian fossils and for viewing features of the Precambrian and Cambrian succession are in areas too remote or too inaccessible to be visited.
    [Show full text]
  • Field Trip: Palaeozoic Echinoderms from Northern Spain
    FIELD TRIP: PALAEOZOIC ECHINODERMS FROM NORTHERN SPAIN S. Zamora & I. Rábano (eds.), Progress in Echinoderm Palaeobiology. Cuadernos del Museo Geominero, 19. Instituto Geológico y Minero de España, Madrid. ISBN: 978-84-7840-961-7 © Instituto Geológico y Minero de España 2015 FIELD TRIP: PALAEOZOIC ECHINODERMS FROM NORTHERN SPAIN Samuel Zamora 1 (coord.) José Javier Álvaro 2, Miguel Arbizu 3, Jorge Colmenar 4, Jorge Esteve 2, Esperanza Fernández-Martínez 5, Luis Pedro Fernández 3, Juan Carlos Gutiérrez-Marco 2, Juan Luis Suárez Andrés 6, Enrique Villas 4 and Johnny Waters 7 1 Instituto Geológico y Minero de España, Manuel Lasala 44 9ºB, 50006 Zaragoza, Spain. [email protected] 2 Instituto de Geociencias (CSIC-UCM), José Antonio Novais 12, 28040 Madrid, Spain. [email protected], jcgrapto@ ucm.es, [email protected] 3 Departamento de Geología, Universidad de Oviedo, Jesús Arias de Velasco s/n, 33005 Oviedo, Spain. [email protected], [email protected] 4Área de Paleontología, Departamento de Ciencias de la Tierra, Universidad de Zaragoza, Pedro Cerbuna 12, 50009 Zaragoza, Spain. [email protected], [email protected] 5 Facultad de Biología y Ciencias Ambientales, Universidad de León, Campus of Vegazana, 24071 León, Spain. [email protected] 6 Soningeo, S.L. PCTCAN, Isabel Torres, 9 P20. 39011 Santander, Cantabria, Spain. [email protected] 7 Department of Geology, Appalachian State University, ASU Box 32067, Boone, NC 28608-2067, USA. [email protected] Keywords: Cambrian, Ordovician, Silurian, Devonian, echinoderms, environments, evolution. INTRODUCTION Samuel Zamora Spain contains some of the most extensive and fossiliferous Palaeozoic outcrops in Europe , including echinoderm faunas that are internationally significant in terms of systematics, palaeoecology and palaeobiogeography.
    [Show full text]
  • (Silurian) Conodont Biostratigraphy of Saaremaa, Estonia, and a Correlation with Britain
    Journal of’ Micropalaeontology, 17: 33-50. 0262-821)</98 $10.00 0 1998 British Micropalaeontological Society. Upper Wenlock to Lower Piidoli (Silurian) conodont biostratigraphy of Saaremaa, Estonia, and a correlation with Britain VIIVE VIIRA’ & RICHARD J. ALDRIDGE’ ’ Institute of Geology, Estonia Avenue 7, EE0105 Tallinn, Estonia. Department of Geology, University of Leicester, Leicester LEI 7RH, UK ABSTRACT - The closely related conodonts Ozarkodina bohemica, 0. snajdri and 0. crispa form a clade that provides useful biostratigraphical indices through the upper Silurian. Collections from boreholes and surface outcrops on Saaremaa and from a borehole at Kolka, Latvia, contain new morphotypes of 0. bohemica and 0.crispa. A new subspecies, 0. snajdriparasnajdri, is also distinguished, occurring above 0. crispa in the Kuressaare and lowermost Kaugatuma stages. Evidence from conodonts and other fossils; primarily chitinozoans, ostracods and ichthyoliths, can be used to correlate the upper Silurian succession of Saaremaa with those of the Welsh Borderland and Gotland, although some problems remain to be solved. The microfossil distribution suggests that there may be a major break at the base of the Ludlow Bone Bed Member at Ludlow, equivalent to the Kuressaare Formation on Saaremaa. J. Micropalaeontul. 17(1): 33-50, April 1998. INTRODUCTION display frequent discontinuity surfaces, mud cracks, ripple The study of the Silurian rocks of Estonia dates back to the last marks and trace fossils. Abundant stromatolites and oncolites century, with the establishment of a Lower Palaeozoic occur, but the Fauna is restricted to eurypterids, thelodonts and stratigraphical scheme by Schmidt (1858). Details were added conodonts. The Paadla Formation is 26-32 m thick and consists in the earlier part of this century, and more recently scientific of detrital biomorphous and biohermal stromatoporoid-coral investigations have been considerably advanced by a group of limestones, dolomites and mark.
    [Show full text]
  • LOWER TRIASSIC CONODONTS from NORTH VIETNAM This
    Acta Palaeontologica Polonica -- - - Vol. 34, No. 4 pp. 391416; pls. 29-34 Warszawa, 1989 BUI DUC THANG LOWER TRIASSIC CONODONTS FROM NORTH VIETNAM BUI DUC THANG: Lower Triassic conodonts from North Vietnam. Acta Palaeont. Polonica, 34, 4 391-416, 1989 (issued 1990). The paper concerns an assemblage of conodonts from the upper part of the Suoi Bang Formation (Olenekian), North Vietnam. 37 taxa, including 6 new ones: Neospathodus gondolellaefmmtr, N. regularis, Ozakodina gigantea, Pachycladina multispinosa, Neohidneodella uietnamica, Hindeodella langsonensis, have been described dating this part ot the formrrtion at the Smithian. The assemblage lacks the genus Gondolella. K e y w o r d s: Conodonts, Lower Triassic, stratigraphy, Nmth Vietnam. Bui Duc Thang, Department of Palaeontoogy, Institute of Geology and Mineral Resources Thanh Xuan, Hanot. Received: December, 1987. INTRODUCTION This paper is the first report on Triassic conodonts from Vietnam. The conodonts were found in a section exposed near the railway station Bac Thuy (fig. 1) in the province of Lang Son in the northeastern part of Vietnam. The rocks exposed there belong to the Suoi Bang Formation (fig. 2), the lower part of which consists of sandstones, mudstones, and clays, while intercalations of marine carbonate sediments (dolomitic sand- stones and limestones) appear towards the upper part (Vu Khuc 1980). Thirteen samples (about 1 kilogram each sample) have been collected in the section (fig. 3). Only five samples from the highest part of the section yielded conodonts (fig. 3, table I), on average 150-200 specimens per sample. Three hundred sixty specimens were suitablye for determina- tion. Samples with abundant conodonts included also fish scales and teeth, small ammonite shells, and foraminifera.
    [Show full text]
  • Athenacrinus N. Gen. and Other Early Echinoderm Taxa Inform Crinoid
    Athenacrinus n. gen. and other early echinoderm taxa inform crinoid origin and arm evolution Thomas Guensburg, James Sprinkle, Rich Mooi, Bertrand Lefebvre, Bruno David, Michel Roux, Kraig Derstler To cite this version: Thomas Guensburg, James Sprinkle, Rich Mooi, Bertrand Lefebvre, Bruno David, et al.. Athenacri- nus n. gen. and other early echinoderm taxa inform crinoid origin and arm evolution. Journal of Paleontology, Paleontological Society, 2020, 94 (2), pp.311-333. 10.1017/jpa.2019.87. hal-02405959 HAL Id: hal-02405959 https://hal.archives-ouvertes.fr/hal-02405959 Submitted on 13 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution| 4.0 International License Journal of Paleontology, 94(2), 2020, p. 311–333 Copyright © 2019, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/20/1937-2337 doi: 10.1017/jpa.2019.87 Athenacrinus n. gen. and other early echinoderm taxa inform crinoid origin and arm evolution Thomas E.
    [Show full text]
  • Middle Cambrian Gogiid Echinoderms from Northeast Spain: Taxonomy, Palaeoecology, and Palaeogeographic Implications
    Middle Cambrian gogiid echinoderms from Northeast Spain: Taxonomy, palaeoecology, and palaeogeographic implications SAMUEL ZAMORA, RODOLFO GOZALO, and ELADIO LIÑÁN Zamora, S., Gozalo, R., and Liñán, E. 2009. Middle Cambrian gogiid echinoderms from Northeast Spain: Taxonomy, palaeo− ecology, and palaeogeographic implications. Acta Palaeontologica Polonica 54 (2): 253–265. DOI: 10.4202/app.2008.0010 Gogia parsleyi Zamora sp. nov. and Gogia sp. are described from two different echinoderm assemblages, both from the middle Cambrian of the Murero Formation (Iberian Chains, NE Spain). Gogia parsleyi is reconstructed and described on the basis of fifteen complete or partial specimens and numerous isolated plates. It is characterised by spiralled brachioles, simple epispires, sometimes covered by stereomic domes or tiny cover plates, and by thecal plates arranged in subregular circlets. This gogiid population comprises juveniles, advanced juveniles and mature individuals. The material was found in the upper part of the Murero Formation (upper Caesaraugustian–lower Languedocian). Gogia sp. is represented by two almost complete specimens and several isolated plates from the lower part of the Murero Formation (lower Caesar− augustian). The genus Gogia was first described in Western Gondwana from the Languedocian (upper middle Cambrian) of France, but the material from Spain is older and represents the oldest record of this genus in Gondwana, suggesting an early migration from Laurentia. The gogiids are well preserved in two echinoderm Lagerstätten, which, together with other echinoderms, comprise the majority of the fossil fauna. Both levels are derived from obrution deposits produced in calm and open marine conditions, sometimes affected by sporadic storms. Their holdfast morphology suggests that these gogiids were low−tier suspension feeders, living attached to trilobite fragments in a soft, muddy environment.
    [Show full text]