Quantitative Analysis of Suture Lines in Carboniferous Ammonoids
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VOLUME 33 December 2017
VOLUME 33 December 2017 Volume 33 Table of Contents EXECUTIVE’S COLUMN…………………………………………………………………..…….. 2 OBITUARY……………………………………………………………………………………..…5 SCCS REPORTS………………………………………………………………………………….7 ANNUAL REPORT TO ICS FOR 2016-2017…………………………………………………..….7 TASK GROUP REPORTS FOR 2016-2017 AND WORK PLANS FOR 2017 FISCAL YEAR………….11 Report of the task group to establish a GSSP close to the existing Viséan-Serpukhovian boundary…………11 Report of the task group to establish a GSSP close to the existing Bashkirian-Moscovian boundary………16 Report of the task group to establish the Moscovian-Kasimovian and Kasimovian-Gzhelian boundaries…....18 SCCS DOCUMENTS (CONTRIBUTIONS BY MEMBERS)…………………………………...……21 SHALLOW-WATER SIPHONODELLIDS AND DEFINITION OF THE DEVONIAN-CARBONIFEROUS BOUNDARY…………………………………………………………………………………….21 REPORT FOR PROGRESS FOR 2017 ACTIVITIES IN THE CANTABRIAN MOUNTAINS, SPAIN AND THE AMAZONAS BASIN, BRAZIL……………………………………………...………………26 TAXONOMIC AND STRATIGRAPHIC PROBLEMS CONCERNING THE CONODONTS LOCHRIEA SENCKENBERGICA NEMIROVSKAYA, PERRET & MEISCHNER, 1994 AND LOCHRIEA ZIEGLERI NEMIROVSKAYA, PERRET & MEISHCNER, 1994-CONSEQUENCES FOR DEFINING THE VISÉAN- SERPUKHOVIAN BOUNDARY………………………………………………………………………………...28 PROGRESS ON THE VISÉAN-SERPUKHOVIAN BOUNDARY IN SOUTH CHINA AND GERMANY……………………………………………………………………………………..35 POTENTIAL FOR A MORE PRECISE CORRELATION OF THE BASHKIRIAN AMMONOID AND FORAMINIFERAL ZONES IN THE SOUTH URALS…………………………………………..……42 CHEMOMETRICS AND CARBONIFEROUS MEDULLOSALEAN FRONDS: IMPLICATIONS FOR CARBONIFEROUS PHYTOSTRATIGRAPHY…………………………………………………...…45 -
Significance for International Correlation of the Perapertú Formation in Northern Palencia, Cantabrian Mountains
PERAPERTÚ FM, CANTABRIAN MTS. GONIATITES 127 SIGNIFICANCE FOR INTERNATIONAL CORRELATION OF THE PERAPERTÚ FORMATION IN NORTHERN PALENCIA, CANTABRIAN MOUNTAINS. TECTONIC/STRATIGRAPHIC CONTEXT AND DESCRIPTION OF MISSISSIPPIAN AND UPPER BASHKIRIAN GONIATITES Jürgen KULLMANN1, Robert H. WAGNER2 and Cornelis F. WINKLER PRINS3 1 Institut für Geowissenschaften der Universität Tübingen, Sigwartstraβe 10, D 72076 Tübingen, Germany; e-mail: [email protected] 2 Corresponding author: Centro Paleobotánico, Jardín Botánico de Córdoba, Avda. de Linneo, s/n, E 1�00������������ Córdoba �Spain����������; e-mail: [email protected] 3 Nationaal Natuurhistorisch Museum, Postbus 9517, NL 2300 RA Leiden, The Netherlands; e-mail: [email protected] Kullmann, J., Wagner R. H. & Winkler Prins, C.F. 2007. Significance for international correlation of the Pera- pertú Formation in northern Palencia, Cantabrian Mountains. Tectonic/stratigraphic context and description of Mississippian and Upper Bashkirian goniatites. �������������������������������������������������������������El significado de la Formación Perapertú para la correlación internacional, norte de Palencia, Cordillera Cantábrica. Contexto tectónico/estratigráfico y descripción de go- niatítidos misisípicos y del Bashkiriense Superior.] Revista Española de Paleontología, 22 �2�, 127-1�5. ISSN 0213-6937. ABSTRACT Small ammonoid assemblages are recorded from the Perapertú Formation in northern Palencia. This is a mud- stone unit with local platform limestones characterised by carbonate debris flows -
United States National Museum Bulletin 262
SMITHSONIAN INSTITUTION MUSEUM O F NATURAL HISTORY For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C., 20402 - Price 70 cents UNITED STATES NATIONAL MUSEUM BULLETIN 262 Catalog of the Type Specimens of Invertebrate Fossils LOUIS R. PURNELL Part I: Paleozoic Cephalopoda SMITHSONIAN INSTITUTION PRESS WASHINGTON, D.C. 1968 Publications of the United States National Museum The scientific publications of the United States National Museum in- clude two series, Proceedings of the United States National Museum and United States National Museum Bulletin. In these series are published original articles and monographs dealing with the collections and work of the Museum and setting forth newly ac- quired facts in the field of anthropology, biology, geology, history, and technology. Copies of each publication are distributed to libraries and scientific organizations and to specialists and others interested in the various subjects. The Proceedings, begun in 1878, are intended for the publication, in separate form, of shorter papers. These are gathered in volumes, octavo in size, with the publication date of each paper recorded in the table of contents of the volume. In the Bulletin series, the first of which was issued in 1875, appear longer, separate publications consisting of monographs (occasionally in several parts) and volumes in which are collected works on related sub- jects. Bulletins are either octavo or quarto in size, depending on the the needs of the presentation. Since 1902, papers relating to the botanical collections of the Museum have been published in the Bulletin series under the heading Contributions from the United States National Herbarium. -
The Coarse Wrinkle Layer of Palaeozoic Ammonoids: New Evidence from the Early Carboniferous of Morocco
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2014 The coarse wrinkle layer of Palaeozoic ammonoids: new evidence from the Early Carboniferous of Morocco Korn, Dieter ; Klug, Christian ; Mapes, Royal H DOI: https://doi.org/10.1111/pala.12087 Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-85343 Journal Article Originally published at: Korn, Dieter; Klug, Christian; Mapes, Royal H (2014). The coarse wrinkle layer of Palaeozoic ammonoids: new evidence from the Early Carboniferous of Morocco. Palaeontology, 57(4):771-781. DOI: https://doi.org/10.1111/pala.12087 [Palaeontology, Vol. 57, Part 4, 2014, pp. 771–781] THE COARSE WRINKLE LAYER OF PALAEOZOIC AMMONOIDS: NEW EVIDENCE FROM THE EARLY CARBONIFEROUS OF MOROCCO by DIETER KORN1*, CHRISTIAN KLUG2 and ROYAL H. MAPES3 1Museum fur€ Naturkunde, Leibniz-Institut fur€ Evolutions- und Biodiversit€atsforschung, Invalidenstraße 43, Berlin, D-10115, Germany; e-mail: [email protected] 2Pal€aontologisches Institut und Museum, Karl Schmid-Strasse 4, Zurich,€ CH-8006, Switzerland; e-mail: [email protected] 3Department of Geological Sciences, Ohio University, Athens, OH 45701, USA; e-mail: [email protected] *Corresponding author Typescript received 29 May 2013; accepted in revised form 9 October 2013 Abstract: The wrinkle layer is a dorsal shell structure tres into the lumen of the body chamber. Possible func- occurring in a number of ammonoids, but its function is tions are discussed and the most likely interpretation for still debated. Here, we describe, from Moroccan material of the structure is ‘fabricational noise’, which is related to the the Early Carboniferous species Maxigoniatites saourensis coarsening of the shell ornament of the terminal body (Pareyn, 1961), the most conspicuous wrinkle layer known chamber. -
Evolution of the Goniatitaceae and Vis6an-Namurian Biogeography
Evolution of the Goniatitaceae and Vis6an-Namurian biogeography DIETERKORN Korn, D. 1997. Evolution of the Goniatitaceaeand Vis6an-Namurian biogeography.- Acta Pal eontologica P olonica 42, 2, 177 -199. Evolutionary lineages within the Carboniferous ammonoid superfamily Goniatitaceae can be recognized using cladistic and stratopheneticanalyses, showing that both ap- proaches lead to coinciding results. In the late Vis6an and Namurian A, ammonoid provinces can be defined by the distribution of lineages within the goniatite superfamily Goniatitaceae. The first province corresponds to the Subvariscan Realm (where the superfamily became extinct near the Vis6an-Namurian boundary), and the second em- braces the majority of the occurrences,e.g. the south urals, central Asia, and North America (where the superfamily with different independent lieages continued up into the late Namurian A). In the Vis6an, the superfamily was, in two short epochs, globally distributed with major transgressions,which probably led to migration events. The first is at the end of the late Vis6an A(G. fi.mbrians and G. spirifer Zones, when the genus Goniatites had a world-wide distribution with various species),and the second at the beginning of the late Vis6an C (L. poststriatumZone, when Lusitanoceras is globally distributed). K e y w o r d s : Ammonoidea, Goniatitaceae, Early Carboniferous, phylogeny, palaeo- biogeography. Dieter Korn [dieter.korn@uni+uebingen.de], Institut und Museum fiir Geologie und Palciontologieder Eberhard-Karls-(Jniversitrit, SigwartstraJJe10, 72076 Tiibingen, Ger- many. Introduction Late Vis6an and early Namurian goniatite faunashave been reported fiom numerous localities in the northernhemisphere, from Alaska andCanada, the Westernand Central United States,various regions in Europeand North Africa, Novaya Zemlya and the South Urals, Central Asia, as well as from China. -
INTERNATIONAL CONFERENCE “UPPERMOST DEVONIAN and CARBONIFEROUS CARBONATE BUILDUPS and BOUNDARY STRATOTYPES” Abstracts and P
Қ.И.СӘТБАЕВ АТЫНДАҒЫ ГЕОЛОГИЯЛЫҚ ҒЫЛЫМДАР ИНСТИТУТЫ ИНСТИТУТ ГЕОЛОГИЧЕСКИХ НАУК ИМ. К.И. САТПАЕВА K.I. SATPAYEV INSTITUTE OF GEOLOGICAL SCIENCES INTERNATIONAL CONFERENCE “UPPERMOST DEVONIAN AND CARBONIFEROUS CARBONATE BUILDUPS AND BOUNDARY STRATOTYPES” Abstracts and papers of International Field Meeting of the I.U.G.S. Subkomission on Carboniferous Stratigraphy Almaty-Turkestan, August 15-22, 2017 МЕЖДУНАРОДНОЕ СОВЕЩАНИЕ «ВЕРХНЕДЕВОНСКИЕ И КАМЕННОУГОЛЬНЫЕ КАРБОНАТНЫЕ ПОСТРОЙКИ И СТРАТОТИПЫ ГРАНИЦ» Сборник статей Международного совещания Алматы – Туркестан, 15 – 22 августа, 2017 Под эгидой I.U.G.S. Международной подкомиссии по стратиграфии карбона SCCS Almaty, 2017 1 УДК 551.1/.4 (063) ББК 26.3 В 36 Board of Editors: Prof. Zholtaev G.Zh., Zhaimina V.Ya., Fazylov E.M., Nikolaeva S.V., Musina E.S. 36 UPPERMOST DEVONIAN AND CARBONIFEROUS CARBONATE BUILDUPS AND BOUNDARY STRATOTYPES Almaty: LLP «378», 2017- 73 p. ISBN 978-601-323-051-1 Articles of the compilation contain materials provided by participans of International Field Meeting “Upper Devonian – Carboniferous Reef buildups and stratotype boundary” - experts on stratigraphy and paleontology from the Canada, United Kingdom, France, Germany, Denmark, Repablic of China, Russia and Kazakhsnan. They cover the issues of development of the International Chronostratigraphic Chart of Carboniferous System, guestions and objectives related to selection and approval of the Global Boundary Stratotipe Section and Points (GSSP) for Visean- Serpukhovian boundary based on reliable biostratigraphic markers, being the First Appearance Data (FAD) of the global index taxa. The results of recently studies on biostratigraphy, bio-facies bioherms, reefs and mounds, conodonts, bryozoans, stromatolites and other groups of fossils. УДК 551.1/.4 (063) ББК 26.3 ISBN 978-601-323-051-1 © K.I. -
Sccs Voting & Corresponding Membership 2009
Volume 30 Table of Contents EXCECUTIVE’S COLUMN..................................................................................................................................................................... 2 MEMBERSHIP ...................................................................................................................................................................................... 3 REPORT FROM THE BUSINESS MEETING OF SUBCOMMISSION ON CARBONIFEROUS STRATIGRAPHY AT THE 34TH IGC IN BRISBANE, AUSTRALIA ...................................................................................................................................................................... 7 ANNUAL REPORT FOR NOVEMBER 1ST, 2010 TO OCTOBER 31ST, 2011 ............................................................................ 13 TASK-GROUP REPORTS FOR THE NOV. 1ST, 2011 TO OCT. 31ST, 2012 FISCAL YEAR ......................................................... 31 REPORT OF THE JOINT DEVONIAN–CARBONIFEROUS BOUNDARY GSSP REAPPRAISAL TASK GROUP.......................................... 31 REPORT OF THE TASK GROUP TO ESTABLISH A GSSP CLOSE TO THE EXISTING VISÉAN–SERPUKHOVIAN BOUNDARY ...................... 35 REPORT OF THE TASK GROUP TO ESTABLISH A GSSP CLOSE TO THE EXISTING BASHKIRIAN–MOSCOVIAN BOUNDARY ................... 39 REPORT OF THE TASK GROUP TO ESTABLISH THE MOSCOVIAN–KASIMOVIAN AND KASIMOVIAN–GZHELIAN BOUNDARIES ............. 42 CONTRIBUTIONS BY MEMBERS .................................................................................................................................................... -
Ammonoids of the Antler Foreland Basin (Nevada, Utah)
Goniatites Zone (middle Mississippian) ammonoids of the Antler Foreland Basin (Nevada, Utah) DIETER KORN & ALAN L. TITUS The ammonoid faunas from the Goniatites Zone (Late Viséan; Mississippian) of the Camp Canyon Member (Chainman Formation) are described for the first time. The assemblage shows close relationships to time equivalent occurrences in Alaska and the American Midcontinent, but differs markedly from occurrences in Europe, North Africa, and the South Urals. Seven successive ammonoid biozones are proposed for this interval in North America, in ascending or- der: (1) Calygirtyoceras confusionense Ammonoid Biozone, (2) Calygirtyoceras arcticum Ammonoid Biozone, (3) Girtyoceras primum Ammonoid Biozone, (4) Girtyoceras gordoni Ammonoid Biozone, (5) Goniatites deceptus Ammonoid Biozone, (6) Goniatites eganensis Ammonoid Biozone, and (7) Goniatites multiliratus Ammonoid Biozone. The following ammonoid species are revised or newly described: Bollandoceras occidentale sp. nov., Entogonites burbankensis sp. nov., Entogonites borealis (Gordon, 1957), Entogonites acus sp. nov., Calygirtyoceras confusionense sp. nov., Calygirtyoceras arcticum Gordon, 1957, Girtyoceras primum sp. nov., Girtyoceras gordoni sp. nov., Girtyoceras hamiltonense sp. nov., Dimorphoceras worki sp. nov., Dimorphoceras rileyi sp. nov., Metadimorphoceras mangeri sp. nov., Metadimorphoceras richardsi sp. nov., Kazakhoceras bylundi sp. nov., Goniatites americanus Gordon, 1971, Goniatites deceptus sp. nov., Goniatites eganensis sp. nov., Goniatites sowerbyi sp. nov., and -
Early Carboniferous Ammonoid Faunas and Stratigraphy of the Montagne Noire (France)
Fossil Record 10(2) (2007), 99–124 / DOI 10.1002/mmng.200700002 Early Carboniferous ammonoid faunas and stratigraphy of the Montagne Noire (France) Dieter Korn*,1 and Raimund Feist**,2 1 Museum fu¨ r Naturkunde der Humboldt-Universita¨t zu Berlin, Invalidenstraße 43, D-10115 Berlin, Germany 2 Institut des Sciences de l’Evolution, Universite´ Montpellier II, F-34095 Montpellier, France Received 20 November 2006, accepted 5 February 2007 Published 1 August 2007 With 20 figures Key words: Ammonoidea, Carboniferous, Montagne Noire, biostratigraphy, lithostratigraphy. Abstract The early Carboniferous (Mississippian) sedimentary succession of the Montagne Noire is subdivided into three major litho- stratigraphic units, in ascending order the Montagne Noire Griotte Group (Devonian to Early Tournaisian), the Tournaisian to Vise´an Saint-Nazaire Group (with the Lydiennes, Fauge`res, Colonnes, and Puech Capel Formations, the latter new), and the Laurens Flysch Group (late Vise´an). The ammonoid assemblages in these rock units are reviewed. A total of 29 Early Carbo- niferous ammonoid taxa at species level are determined. The new genus Nigrocyclus n. gen., and the new species Gattendorfia nazairensis n. sp., Globimitoceras albaillei n. sp., and Neogoniatites canovasi n. sp. are described. Schlu¨ sselwo¨ rter: Ammonoidea, Karbon, Montagne Noire, Biostratigraphie, Lithostratigraphie. Zusammenfassung Die unterkarbonische Abfolge von Sedimentgesteinen in der Montagne Noire wird in drei lithostratigraphische Einheiten un- tergliedert, von unten nach oben die Montagne Noire Griotte Gruppe (Oberdevon bis Untertournai), die Saint-Nazaire Gruppe des Tournaisium und Vise´um (mit den Lydiennes Fauge`res, Colonnes und Puech Capel Formationen, von denen die letzte neu ist), und der Laurens Flysch Gruppe (Obervise´um). -
ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh
ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh. Geol. B.-A. ISSN 0016–7800 ISBN 3-85316-02-6 Band 54 S. 345–375 Wien, ???????? 1999 North Gondwana: Mid-Paleozoic Terranes, Stratigraphy and Biota Editors: R. Feist, J.A. Talent & A. Daurer Viséan and Early Namurian Ammonoids from the Tafilalt (Eastern Anti-Atlas, Morocco) DIETER KORN, CHRISTIAN KLUG & ROYAL MAPES*) 11 Text-Figures, 5 Tables and 5 Plates Morocco Carboniferous Ammonoids Taxonomy Biostratigraphy Biogeography Contents Zusammenfassung ...................................................................................................... 345 Abstract ................................................................................................................. 345 1. Introduction ............................................................................................................. 345 2. Systematic Palaeontology ............................................................................................... 346 3. Biogeographical Implications ............................................................................................ 359 3.1. Methods ........................................................................................................... 360 3.2. Palaeobiogeographical Units ........................................................................................ 362 3.2.1. Subvariscan ................................................................................................. 362 3.2.2. Kazakhian .................................................................................................. -
Carboniferous Geology and Biostratigraphy of the Appalachian Basin
Carboniferous Geology and Biostratigraphy of the Appalachian Basin Edited by Stephen F. Greb and Donald R. Chesnut Jr. Kentucky Geological Survey James C. Cobb, State Geologist and Director University of Kentucky, Lexington Carboniferous of the Appalachian and Black Warrior Basins Edited by Stephen F. Greb and Donald R. Chesnut Jr. Special Publication 10 Series XII, 2009 Our Mission Our mission is to increase knowledge and understanding of the mineral, energy, and water resources, geologic hazards, and geology of Kentucky for the benefit of the Commonwealth and Nation. Earth Resources—Our Common Wealth www.uky.edu/kgs Technical Level General Intermediate Technical © 2009 University of Kentucky For further information contact: Technology Transfer Officer Kentucky Geological Survey 228 Mining and Mineral Resources Building University of Kentucky Lexington, KY 40506-0107 ISSN 0075-5613 Contents Foreward ...................................................................................................................................................................1 1: Introduction Donald R. Chesnut Jr. and Stephen F. Greb ............................................................................................3 2: Carboniferous of the Black Warrior Basin Jack C. Pashin and Robert A. Gastaldo ..................................................................................................10 3: The Mississippian of the Appalachian Basin Frank R. Ettensohn ....................................................................................................................................22 -
Quantitative Analysis of Suture Lines in Carboniferous Ammonoids
Foss. Rec., 21, 223–236, 2018 https://doi.org/10.5194/fr-21-223-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Quantitative analysis of suture lines in Carboniferous ammonoids Michael Wegerer1, Kenneth De Baets2, and Dieter Korn1 1Museum für Naturkunde Berlin, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Invalidenstraße 43, 10115 Berlin, Germany 2GeoZentrum Nordbayern, Universität Erlangen-Nürnberg, Loewenichstraße 28, 91054 Erlangen, Germany Correspondence: Dieter Korn ([email protected]) Received: 5 May 2018 – Revised: 13 August 2018 – Accepted: 30 August 2018 – Published: 11 September 2018 Abstract. Two morphometric methods are applied and com- The classic investigations of shape variation in organ- pared for the analysis of suture lines in Early Carbonifer- isms were mainly based on metric parameters. Francis Gal- ous ammonoids of the superfamilies Pericycloidea, Girty- ton (Galton, 1883) proposed an approach towards a quan- oceratoidea and Goniatitoidea. We analysed (1) classic met- titative differentiation between human faces, later known ric data (proportions of the width and depths or heights of as two-point shape coordinates or Bookstein shape coor- lobes and saddles) using multivariate statistic methods and dinates (BCs). An approach towards the analysis of geo- (2) outline data of the external lobe and the ventrolateral sad- metric shape differences was developed by the mathemati- dle of the same ammonoid taxa using the elliptic Fourier cian D’Arcy W. Thompson (Thompson, 1917) in his seminal analysis. Both methods lead to similar results and simulta- book On Growth and Form. However, the methodology of neously demonstrate ontogenetic and phylogenetic trends of this time faced the problem that the morphological charac- these ammonoids.