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041-2011-Abstracts-BOE-III-Crete.Pdf
Boreskov Institute of Catalysis of the Siberian Branch of Russian Academy of Sciences, Novosibirsk, Russia Institute of Cytology and Genetics of the Siberian Branch of Russian Academy of Sciences, Novosibirsk, Russia Borissiak Paleontological Institute of Russian Academy of Sciences, Moscow, Russia III International Conference “Biosphere Origin and Evolution” RETHYMNO, CRETE, GREECE OCTOBER 16-20, 2011 ABSTRACTS Novosibirsk, 2011 © Boreskov Institute of Catalysis, 2011 INTERNATIONAL SCIENTIFIC COMMITTEE Alexei Rozanov, Borissiak Paleontological Institute RAS, Moscow, Russia Co‐Chairman Georgii Zavarzin, Institute of Microbiology RAS, Moscow, Russia Co‐Chairman Vadim Agol Moscow State University, Russia Yury Chernov Severtsov Institute of Ecology and Evolution, Moscow, Russia Institute of Protein Research RAS, Pushchino, Moscow region, Alexander Chetverin Russia David Deamer Biomolecular Engineering, School of Engineering, Santa Cruz, USA V.S. Sobolev Institute of Geology and Mineralogy SB RAS, Nikolay Dobretsov Novosibirsk, Russia Mikhail Fedonkin Geological Institute RAS, Moscow, Russia Siegfried Franck Potsdam Institute for Climate Impact Research, Germany V.I. Vernadskii Institute of Geochemistry and Analytical Chemistry Eric Galimov RAS, Moscow, Russia Mikhail Grachev Limnological Institute SB RAS, Irkutsk, Russia Richard Hoover Nasa Marshall Space Flight Ctr., Huntsville, USA North‐Western Scientific Center RAS, St. Petersburg State Sergey Inge‐Vechtomov University, Russia Trofimuk Institute of Petroleum‐Gas Geology and Geophysics Alexander Kanygin SB RAS, Novosibirsk, Russia Astrospace Centre of Lebedev Physical Institute RAS, Moscow, Nikolay Kardashev Russia Józef Kaźmierczak Institute of Paleobiology PAN, Warsaw, Poland Nikolay Kolchanov Institute of Cytology and Genetics SB RAS, Novosibirsk, Russia Trofimuk Institute of Petroleum‐Gas Geology and Geophysics Alexei Kontorovich SB RAS, Novosibirsk, Russia National Center for Biotechnology Information, National Library Eugene V. -
Ascocerid Cephalopods from the Hirnantian?–Llandovery Stages of the Southern Paraná Basin (Paraguay, South America): first Record from High Paleolatitudes
Journal of Paleontology, page 1 of 11 Copyright © 2018, The Paleontological Society 0022-3360/18/0088-0906 doi: 10.1017/jpa.2018.59 Ascocerid cephalopods from the Hirnantian?–Llandovery stages of the southern Paraná Basin (Paraguay, South America): first record from high paleolatitudes M. Cichowolski,1,2 N.J. Uriz,3 M.B. Alfaro,3 and J.C. Galeano Inchausti4 1Universidad de Buenos Aires, Facultad de Ciencias Exactas y Naturales, Departamento de Ciencias Geológicas, Área de Paleontología, Ciudad Universitaria, Pab. 2, C1428EGA, Buenos Aires, Argentina 〈[email protected]〉 2CONICET-Universidad de Buenos Aires, Instituto de Estudios Andinos “Don Pablo Groeber” (IDEAN), Buenos Aires, Argentina 3División Geología del Museo de La Plata, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, La Plata, Argentina. 〈[email protected]〉, 〈[email protected]〉 4Ministerio de Obras Públicas y Comunicaciones de Paraguay, Asunción, Paraguay 〈[email protected]〉 Abstract.—Ascocerid cephalopods are described for the first time from high paleolatitudes of Gondwana. Studied material was collected from the Hirnantian?–Llandovery strata of the Eusebio Ayala and Vargas Peña formations, Paraná Basin, southeastern Paraguay. The specimens are poorly preserved and were questionably assigned to the sub- family Probillingsitinae Flower, 1941, being undetermined at genus and species rank because diagnostic characters are not visible. A particular feature seen in our material is the presence of both parts of the ascocerid conch (the juve- nile or cyrtocone and the mature or brevicone) joined together, which is a very rare condition in the known paleonto- logical record. The specimens are interpreted as at a subadult stage of development because fully grown ascocerids would have lost the juvenile shell. -
Cephalopod Reproductive Strategies Derived from Embryonic Shell Size
Biol. Rev. (2017), pp. 000–000. 1 doi: 10.1111/brv.12341 Cephalopod embryonic shells as a tool to reconstruct reproductive strategies in extinct taxa Vladimir Laptikhovsky1,∗, Svetlana Nikolaeva2,3,4 and Mikhail Rogov5 1Fisheries Division, Cefas, Lowestoft, NR33 0HT, U.K. 2Department of Earth Sciences Natural History Museum, London, SW7 5BD, U.K. 3Laboratory of Molluscs Borissiak Paleontological Institute, Russian Academy of Sciences, Moscow, 117997, Russia 4Laboratory of Stratigraphy of Oil and Gas Bearing Reservoirs Kazan Federal University, Kazan, 420000, Russia 5Department of Stratigraphy Geological Institute, Russian Academy of Sciences, Moscow, 119017, Russia ABSTRACT An exhaustive study of existing data on the relationship between egg size and maximum size of embryonic shells in 42 species of extant cephalopods demonstrated that these values are approximately equal regardless of taxonomy and shell morphology. Egg size is also approximately equal to mantle length of hatchlings in 45 cephalopod species with rudimentary shells. Paired data on the size of the initial chamber versus embryonic shell in 235 species of Ammonoidea, 46 Bactritida, 13 Nautilida, 22 Orthocerida, 8 Tarphycerida, 4 Oncocerida, 1 Belemnoidea, 4 Sepiida and 1 Spirulida demonstrated that, although there is a positive relationship between these parameters in some taxa, initial chamber size cannot be used to predict egg size in extinct cephalopods; the size of the embryonic shell may be more appropriate for this task. The evolution of reproductive strategies in cephalopods in the geological past was marked by an increasing significance of small-egged taxa, as is also seen in simultaneously evolving fish taxa. Key words: embryonic shell, initial chamber, hatchling, egg size, Cephalopoda, Ammonoidea, reproductive strategy, Nautilida, Coleoidea. -
Nautiloidea, Oncocerida) from the Prague Basin
Revision of the Pragian Rutoceratoidea Hyatt, 1884 (Nautiloidea, Oncocerida) from the Prague Basin TÌPÁN MANDA & VOJTÌCH TUREK Superfamily Rutoceratoidea Hyatt, 1884 (Pragian to Frasnian, Devonian) includes nautiloid cephalopods having exogastric cyrtoceracone or coiled shells with periodic walls or raised growth lines (megastriae) forming ridges, some- times modified in various ways into collars, frills, or different outgrowths. High disparity and intraspecific variability of the shell form and sculpture of the rutoceratoids are conspicuous among Early Palaeozoic nautiloids. Consequently, rutoceratoids are divided according to different patterns of growth structures into three families. Parauloceratidae fam. nov. (Pragian to Emsian) contains taxa with cyrtoceracone shells and simple recurrent ribs with ventral sinus. Family Hercoceratidae Hyatt, 1884 (Pragian to Givetian) comprises forms with periodically raised ridges with three lobes form- ing ventrolateral outgrowths during shell growth such as wings, nodes or spines. Family Rutoceratidae Hyatt, 1884 (Pragian to Frasnian) encompases taxa having growth ridges with ventral lobe transforming into undulated frills or dis- tinct periodic collars (megastriae). All of these families had already appeared during early radiation of rutoceratoids in the Pragian. The early radiation of rutoceratoids is, however, adequately recorded only from the Prague Basin. Rutoceratoids become widespread within faunas of Old World and Eastern American realms later during the Emsian and especially Middle Devonian. Three new genera are erected: Parauloceras gen. nov., Otomaroceras gen. nov. and Pseudorutoceras gen. nov. The Pragian Gyroceras annulatum Barrande, 1865 is assigned to the genus Aphyctoceras Zhuravleva, 1974. Rutoceratoids are thus represented by seven genera and eight species in the Pragian Stage of the Prague Basin. In addition, variability of shell coiling among rutoceratoids and its significance for their systematics are discussed. -
Sepkoski, J.J. 1992. Compendium of Fossil Marine Animal Families
MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. Department of the Geophysical Sciences University of Chicago Chicago, Illinois 60637 Milwaukee Public Museum Contributions in Biology and Geology Rodney Watkins, Editor (Reviewer for this paper was P.M. Sheehan) This publication is priced at $25.00 and may be obtained by writing to the Museum Gift Shop, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Orders must also include $3.00 for shipping and handling ($4.00 for foreign destinations) and must be accompanied by money order or check drawn on U.S. bank. Money orders or checks should be made payable to the Milwaukee Public Museum. Wisconsin residents please add 5% sales tax. In addition, a diskette in ASCII format (DOS) containing the data in this publication is priced at $25.00. Diskettes should be ordered from the Geology Section, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Specify 3Y. inch or 5Y. inch diskette size when ordering. Checks or money orders for diskettes should be made payable to "GeologySection, Milwaukee Public Museum," and fees for shipping and handling included as stated above. Profits support the research effort of the GeologySection. ISBN 0-89326-168-8 ©1992Milwaukee Public Museum Sponsored by Milwaukee County Contents Abstract ....... 1 Introduction.. ... 2 Stratigraphic codes. 8 The Compendium 14 Actinopoda. -
High-Level Classification of the Nautiloid Cephalopods: a Proposal for the Revision of the Treatise Part K
Swiss Journal of Palaeontology (2019) 138:65–85 https://doi.org/10.1007/s13358-019-00186-4 (0123456789().,-volV)(0123456789().,- volV) REGULAR RESEARCH ARTICLE High-level classification of the nautiloid cephalopods: a proposal for the revision of the Treatise Part K 1 2 Andy H. King • David H. Evans Received: 4 November 2018 / Accepted: 13 February 2019 / Published online: 14 March 2019 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2019 Abstract High-level classification of the nautiloid cephalopods has been largely neglected since the publication of the Russian and American treatises in the early 1960s. Although there is broad general agreement amongst specialists regarding the status of nautiloid orders, there is no real consensus or consistent approach regarding higher ranks and an array of superorders utilising various morphological features has been proposed. With work now commencing on the revision of the Treatise Part K, there is an urgent need for a methodical and standardised approach to the high-level classification of the nautiloids. The scheme proposed here utilizes the form of muscle attachment scars as a diagnostic feature at subclass level; other features (including siphuncular structures and cameral deposits) are employed at ordinal level. We recognise five sub- classes of nautiloid cephalopods (Plectronoceratia, Multiceratia, Tarphyceratia nov., Orthoceratia, Nautilia) and 18 orders including the Order Rioceratida nov. which contains the new family Bactroceratidae. This scheme has the advantage of relative simplicity (it avoids the use of superorders) and presents a balanced approach which reflects the considerable morphological diversity and phylogenetic longevity of the nautiloids in comparison with the ammonoid and coleoid cephalopods. -
The Pennsylvanian
Official Publication of Volume 35 No. 2 Mid-America Paleontology Society Date: Mar-April, 2012 THE PENNSYLVANIAN A LOVE OF FOSSILS BRINGS US TOGETHER M.A.P.S. Digest--EXPO XXXIV Edition M.A.P.S. Board Members President: Marvin Houg 1st Vice President: Dale Stout 2nd Vice President: Tom Williams Secretary: Tiffany Adrain Treasurer: Jim Preslicka Digest Editors: John Catalani Chris Cozart Membership: Dale Stout Immediate Past President: Gilbert Norris Directors: Charles Newsom Doug DeRosear Karl Stuekerjuergen EXPO Show Chair: Tom Williams EXPO Table Chair: Steve Holley Preface The editors wish to thank the contributors for responding to the Call for Papers in such a timely manner. The papers represent a wide range of Pennsylvanian related topics contributed by our members and others. We would also like to thank Scott D. Elrick for delivering the keynote address. About the Cover The cover image illustrates the Mazon Creek Biota from the Mazon Creek Coal Forest diorama exhibit that debuted at the Field Museum, Chicago, in 1931. See Figure 5 of Shabica and Baird this volume for a complete description. (© The Field Museum, #GEO85637c) Western Illinois University Western Hall Macomb, Illinois March 30, 31 and April 1, 2012 1 John Catalani and Chris Cozart, Editors Table of Contents Page Introduction to the Pennsylvanian of North America – Chris Cozart 3 Paleontology of a Late Pennsylvanian Quarry: Part 1 – Stratigraphy – David Carlson 8 Paleontology of a Late Pennsylvanian Quarry: Part 2 – Gastropods – David Carlson 11 Pennsylvanian Nautiloids of the Midcontinent – John A. Catalani 23 Pennsylvanian Crinoids of Illinois – Thomas Williams 33 Notable Pennsylvanian Localities and Paleobiotas in Knox and Peoria Counties, Illinois – Merrill W. -
Annual Meeting 2007
The Palaeontological Association 51st Annual Meeting 16th–19th December 2007 Uppsala University, Sweden __________________________________________________________________ PROGRAMME WITH ABSTRACTS _________________________________________________ edited by Graham E. Budd, Michael Streng, Allison C. Daley and Sebastian Willman Uppsala, 2007 51st Palaeontological Association Annual Meeting Uppsala 2007 CONTENTS SUMMARY INFORMATION.................................................................... 3 CONFERENCE SCHEDULE OVERVIEW ............................................. 5 SUNDAY 16TH DECEMBER ...................................................................... 8 MONDAY 17TH DECEMBER .................................................................... 8 TUESDAY 18TH DECEMBER.................................................................. 10 WEDNESDAY 19TH DECEMBER........................................................... 12 ABSTRACT OF ANNUAL ADDRESS.................................................... 13 ABSTRACTS OF SEMINAR PRESENTATIONS ................................ 14 ABSTRACTS OF ORAL PRESENTATIONS........................................ 18 ABSTRACTS OF POSTER PRESENTATIONS ................................... 57 SUBJECT AND TAXONOMIC INDEX ................................................. 99 AUTHOR INDEX .................................................................................... 104 2 51st Palaeontological Association Annual Meeting Uppsala 2007 The Palaeontological Association 51st Annual Meeting 16th–19th December -
Cephalopods of the Early Permian Shakh-Tau Reef
©Filodiritto Editore – Proceedings Cephalopods of the Early Permian Shakh-Tau reef LEONOVA Tatiana1, SHCHEDUKHIN Alexander2 1 Borissiak Paleontological Institute of RAS, Moscow, (RUSSIA) 2 Moscow State University, Moscow, (RUSSIA) Emails: [email protected], [email protected] DOI: 10.26352/D924F5026 Abstract This paper presents the first results of the study of the cephalopod collection from the Early Permian Shakh-Tau Reef. This Late Asselian-Early Sakmarian ammonoid assemblage contains nine species of nine genera, some of which are identified in open nomenclature. In the Early Permian (Asselian-Sakmarian and Late Artinskian) assemblages of non-ammonoid cephalopods, about 30 species of coiled nautilids, four species of straight nautiloids (Orthocerida and Pseudorthocerida), and two species of Bactritida have been identified. In addition, two species belonging to the order Oncocerida were found in the Asselian-Sakmarian assemblage. The Asselian-Sakmarian reef community of non-ammonoid cephalopods differs significantly from the Sakmarian communities known from the basinal sediments of the South Urals, both taxonomically and in prevailing morphotypes. The Late Artinskian post-reef assemblage is closer in all respects to the Artinskian South Uralian assemblages, but also has its own characteristics. Keywords: Ammonoids, bactritids, nautiloids, oncocerids, Early Permian, Urals, Shakh-Tau reef Introduction The Early Permian Shakh-Tau reef, one of the four Sterlitamak reef mounds (“shikhans”), has now been almost completely excavated by a limestone quarry and has ceased to exist. The history of the study, geological structure, and components of the bioherm facies have been the subject of a number of works, and were studied in particular detail by Korolyuk [1]. During the quarrying of the limestone, layers containing the richest invertebrate fauna, including cephalopods, were opened. -
Nautiloid Cephalopods – a Review of Their Use and Potential in Biostratigraphy
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Denisia Jahr/Year: 2014 Band/Volume: 0032 Autor(en)/Author(s): Evans David H., King Andy H., Histon Kathleen, Cichowolski Marcela Artikel/Article: Nautiloid cephalopods - a review of their use and potential in biostratigraphy 7-22 © Biologiezentrum Linz/Austria; download unter www.biologiezentrum.at Nautiloid cephalopods – a review of their use and potential in biostratigraphy D.H. EVANS, A.H. KING, K. HISTON & M. CICHOWOLSKI Abstract: In terms of their use as biostratigraphical tools, nautiloid cephalopods are the poor relations of ammonoids. Neverthe- less, in certain situations, they may provide useful biostratigraphical data, particularly where other biostratigraphically valuable taxa are not present; or in certain situations demonstrate a resolution as great as, or greater than ammonoids, trilobites, grapto- lites or conodonts. Nautiloid cephalopods are of especial value in palaeobiogeographical studies, but their use for this purpose may be hampered by the poor understanding of the stratigraphical ranges of individual taxa. The biostratigraphical value of nautiloid cephalopods is demonstrated here through a number of case studies of Ordovician taxa, combined with a review of their biostrati- graphical use in Palaeozoic and Mesozoic successions. These both demonstrate the potential of this group and indicate great scope for further research. Keywords: Nautiloids, cephalopods, biostratigraphy, Palaeozoic, Mesozoic Introduction taxonomically without investigation of the internal morphology of the phragmocone due to the similarities The widespread stratigraphical and geographical of the external features, thus entailing the preparation occurrence of nautiloid cephalopods, particularly, but of polished or thin sections for study, requiring more ef- not exclusively during the Lower Palaeozoic is docu- fort, and possibly resulting in more equivocal data than mented in many substantial monographic works (e.g. -
Spatial Distribution of Oncocerid Cephalopods on a Middle Devonian Bedding Plane Suggests Semelparous Life Cycle
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2020 Spatial distribution of oncocerid cephalopods on a Middle Devonian bedding plane suggests semelparous life cycle Pohle, Alexander ; Fuchs, Dirk ; Korn, Dieter ; Klug, Christian Abstract: Reproductive strategies of extinct organisms can only be recognised indirectly and hence, they are exceedingly rarely reported and tend to be speculative. Here, we present a mass-occurrence with common preservation of pairs of late Givetian (Middle Devonian) oncocerid cephalopods from Hamar Laghdad in the Tafilalt (eastern Anti-Atlas, Morocco). We analysed their spatial occurrences with spatial point pattern analysis techniques and Monte Carlo simulations; our results shows that the pairwise clustering is significant, while ammonoids on the same bedding plane reveal a more random distribution. It is possible that processes such as catastrophic mass mortality or post-mortem transport could have produced the pattern. However, we suggest that it is more likely that the oncocerids were semelparous and died shortly after mating. These findings shed new light on the variation and evolution of reproductive strategies in fossil cephalopods and emphasise that they cannot be based on comparisons with extant taxa without question. DOI: https://doi.org/10.1038/s41598-020-59507-0 Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-186136 Journal Article Published Version The following work is licensed under a Creative Commons: Attribution 4.0 International (CC BY 4.0) License. Originally published at: Pohle, Alexander; Fuchs, Dirk; Korn, Dieter; Klug, Christian (2020). -
Nautiloid and Bactritoid Cephalopods from the Carboniferous of the Jebel Qamar South Area, United Arab Emirates
Paleontological Research, vol. 1, no. 3, pp. 157-165,5 Figs., September 30, 1997 © by the Palaeontological Society of Japan Nautiloid and bactritoid cephalopods from the Carboniferous of the Jebel Qamar South area, United Arab Emirates SHWI NIK01, ALAIN PILLEVUIT2 and GERARD STAMPFLP IDepartment of Environmental Studies, Faculty of Integrated Arts and Sciences, Hiroshima University, Higashihiroshima, 739 Japan 21nstitute of Geophysics, University of Paris VII, 75251 Paris Cedex 05, France 31nstitute of Geology and Paleontology, University of Lausanne, BFSH 2, 1015 Lausanne-Dorigny, Switzerland Received 1 November 1996; Revised manuscript accepted 5 August 1997 Abstract. Nine species of cephalopods from the Ayim Formation of the Jebel Qamar South area, United Arab Emirates are described. They include orthoceratids: Michelinoceras sp. 1, Michelinoceras? sp. 2, Temperoceras ayimense sp. nov., Mooreoceras? sp. 1, Mooreoceras? sp. 2, Mitorthoceras? sp., Spyroceratinae, genus and species indeterminate; oncocerid: Poterioceratidae, genus and species in determinate; and bactritid: Bactrites cf. quadrilineatus Girty. Based on the fauna, the Early Carbonifer ous age of the formation is first established herein. Key words: Ayim Formation, Bactritida, Early Carboniferous, Oncocerida, Orthocerida, United Arab Emirates Introduction shale located in the lower part of the Ayim Formation (Figure 2). Besides cephalopods, the fossils include serpulids (Spir The cephalopods described herein were collected from orbis sp.), bryozoans, ostracodes, echinoderms, fish remains the Ayim Formation of previously uncertain age, during field (Robertson et al., 1990), and trace fossils (Pillevuit, 1993). An work in the Jebel Qamar South area, United Arab Emirates age between Ordovician and Early Permian for the Ayim (Figure 1). Although preservation of the material is poor, we Formation is not questionable because of its stratigraphic can provide new knowledge concerning age determination setting, viz.