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Lower Cretaceous Terebratulidae of the Jura Region. Part 3, Terebratula Salevensis De Loriol and the Genera Praelongithyris and Tropeothyris
Lower Cretaceous terebratulidae of the Jura region. Part 3, Terebratula salevensis de Loriol and the genera praelongithyris and tropeothyris Autor(en): Middlemiss, Frank A. Objekttyp: Article Zeitschrift: Eclogae Geologicae Helvetiae Band (Jahr): 77 (1984) Heft 3 PDF erstellt am: 24.09.2021 Persistenter Link: http://doi.org/10.5169/seals-165523 Nutzungsbedingungen Die ETH-Bibliothek ist Anbieterin der digitalisierten Zeitschriften. Sie besitzt keine Urheberrechte an den Inhalten der Zeitschriften. Die Rechte liegen in der Regel bei den Herausgebern. Die auf der Plattform e-periodica veröffentlichten Dokumente stehen für nicht-kommerzielle Zwecke in Lehre und Forschung sowie für die private Nutzung frei zur Verfügung. Einzelne Dateien oder Ausdrucke aus diesem Angebot können zusammen mit diesen Nutzungsbedingungen und den korrekten Herkunftsbezeichnungen weitergegeben werden. Das Veröffentlichen von Bildern in Print- und Online-Publikationen ist nur mit vorheriger Genehmigung der Rechteinhaber erlaubt. Die systematische Speicherung von Teilen des elektronischen Angebots auf anderen Servern bedarf ebenfalls des schriftlichen Einverständnisses der Rechteinhaber. Haftungsausschluss Alle Angaben erfolgen ohne Gewähr für Vollständigkeit oder Richtigkeit. Es wird keine Haftung übernommen für Schäden durch die Verwendung von Informationen aus diesem Online-Angebot oder durch das Fehlen von Informationen. Dies gilt auch für Inhalte Dritter, die über dieses Angebot zugänglich sind. Ein Dienst der ETH-Bibliothek ETH Zürich, Rämistrasse 101, 8092 Zürich, Schweiz, www.library.ethz.ch http://www.e-periodica.ch Eclogae geol. Helv. Vol. 77 Nr. 3 Pages 583 617 Basel, December 1984 Lower Cretaceous Terebratulidae of the Jura region 3. TEREBRATULA SALEVENSIS DE LORIOL AND THE GENERA PRAELONGITHYRIS AND TROPEOTHYRIS By Frank A. Middlemiss') ABSTRACT Terebratula salvensis de Loriol is referred to the genus Praelongithyris. -
From the Western of the United
from the Western of the United GEOLOGICAL SURVEY P R® BES&lON AL PAPER 1057 Early Triassic Terebratulid Brachiopods from the Western Interior of the United States By PETER R. HOOVER GEOLOGICAL SURVEY PROFESSIONAL PAPER 1057 Description and illustration offive species of terebratulid brachiopods, and discussion of their distribution and developmental and evolutionary history UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1979 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Hoover, Peter R. Early Triassic Terebratulid Brachiopods from the Western Interior of the United States (Geological Survey Professional Paper 1057) Bibliography: p. 19 Includes index Supt. of Docs. No.: I 19:16:1057 1. Terebratulida, Fossil. 2. Paleontology Triassic. 3. Paleontology The West. I. Title. II. Series: United States Geological Survey Professional Paper 1057 QE797.T29H66 564'.8 77-608314 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03182-5 CONTENTS Page Page Systematic paleontology Continued Abstract ....................... 1 Family Dielasmatidae Continued Introduction .................... 1 Subfamily Dielasmatinae. Previous work................ 1 Rhaetina Waagen ..... Present study ................ 3 Family Terebratulidae ......... 9 Acknowledgments ............ 3 Subfamily Plectoconchiinae. 9 Fossil localities cited in this report. .... 3 Vex, n. gen. ......... 9 Stratigraphic setting of the brachiopods 4 Family Cryptonellidae ......... 11 Faunal relationships. .............. 6 Subfamily Cryptacanthiinae . 11 Biostratigraphic implications........ 6 Obnixia, n. gen. ...... 11 Systematic paleontology............ 7 Family Zeilleriidae ............ 17 Family Dielasmatidae.......... 7 Periallus, n. gen. ......... 17 Subfamily Zugmayeriinae . 7 References cited. ................. 19 Portneufia, n. gen. .... 7 Index ......................... 21 ILLUSTRATIONS [Plates follow index] PLATE 1. -
The Present-Day Mediterranean Brachiopod Fauna: Diversity, Life Habits, Biogeography and Paleobiogeography*
SCI. MAR., 68 (Suppl. 1): 163-170 SCIENTIA MARINA 2004 BIOLOGICAL OCEANOGRAPHY AT THE TURN OF THE MILLENIUM. J.D. ROS, T.T. PACKARD, J.M. GILI, J.L. PRETUS and D. BLASCO (eds.) The present-day Mediterranean brachiopod fauna: diversity, life habits, biogeography and paleobiogeography* A. LOGAN1, C.N. BIANCHI2, C. MORRI2 and H. ZIBROWIUS3 1 Centre for Coastal Studies and Aquaculture, University of New Brunswick, Saint John, N.B. E2L 4L5, Canada. E-mail: [email protected] 2 DipTeRis (Dipartimento Territorio e Risorse), Università di Genova, Corso Europa 26, I-16132 Genoa, Italy. 3 Centre d’Océanologie de Marseille, Station Marine d’Endoume, Rue Batterie des Lions, 13007 Marseilles, France. SUMMARY: The present-day brachiopods from the Mediterranean Sea were thoroughly described by nineteenth-century workers, to the extent that Logan’s revision in 1979 listed the same 11 species as Davidson, almost 100 years earlier. Since then recent discoveries, mainly from cave habitats inaccessible to early workers, have increased the number of species to 14. The validity of additional forms, which are either contentious or based on scanty evidence, is evaluated here. Preferred substrates and approximate bio-depth zones of all species are given and their usefulness for paleoecological reconstruction is discussed. A previous dearth of material from the eastern Mediterranean has now been at least partially remedied by new records from the coasts of Cyprus, Israel, Egypt, and, in particular, Lebanon and the southern Aegean Sea. While 11 species (79 % of the whole fauna) have now been recorded from the eastern basin, Terebratulina retusa, Argyrotheca cistellula, Megathiris detruncata and Platidia spp. -
A Note on Dallina Septigera (Loven), (Brachiopoda, Dallinidae)
J. mar. bioi. Ass. U.K. (1960) 39, 91-99 91 Printed in Great Britain A NOTE ON DALLINA SEPTIGERA (LOVEN), (BRACHIOPODA, DALLINIDAE) By D. ATKINS,D.Sc. From the Plymouth Laboratory (Plate I and Text-figs. 1-5) The discovery of a homoeomorph, Pallax dalliniformis, of Dallina septigera (Loven) dredged with that species (Atkins, 1960) and, it is believed, some• times confused with it, certainly by Fischer & Oehlert (1891), has made a brief redescription desirable. During the present work more than a hundred D. septigera of shell length 5-31 mm have been obtained, and most of them examined internally. The original description in Latin-without figures-of Dallina septigera (= Terebratula septigera) was by Loven in 1846 (p. 183). Unfortunately his description does not now clearly separate his species from Pallax dallini• formis, except perhaps his failure to mention the presence of dental plates, pedicle collar and spiculation. It is doubtful how much weight can be attached to this, for on the same page he failed to mention the presence of dental plates in Macandrevia cranium. He gave the length as 28 mm, width as 21·5 mm and depth as 17 mm. The Stockholm Natural History Museum, the most likely Museum to possess Loven's type specimen, unfortunately does not have it, and it is probable that he did not designate one. The Museum, however, does possess old collections of dried shells of this species from Norway and the ~orth Sea, which Loven probably studied. Through the kindness of Dr H.Mutvei a large specimen from these was loaned to me: he stated that it is not known with certainty whether it was collected before or after 1846-the date of publication of Loven's paper. -
Belemnites of the Bohemian Cretaceous Basin in a Global Context
Acta Geologica Polonica, Vol. 54 (2004), No.4, pp. 511-533 Belemnites of the Bohemian Cretaceous Basin in a global context MARTIN KOStAKl, STANISLAV CECH2, BORIS EKRT3, MARTIN MAZUCHl, FRANK WIESE4, SILKE VOIGTs, CHRISTOPHER J. WOOD6 lInstitute of Geology and Palaeontology, Charles University, Albertov 6, Prague 2, 12843, Czech Republic, E-mail: kostak@natw:[email protected] 2Czech Geological Swvey, Kldrov 3, 11821, Czech Republic, E-mail: [email protected] 3National Museum, Vdclavske namest! 68, Prague 1,11579, Czech Republic, E-mail: [email protected] 4Fachlichtung Palaontologie, FU Berlin, Malteserstl: 74-100, D-12249 Berlin, GClmany, E-mail: [email protected] 5 Geological Institute, University of Cologne, Zulpicher StI: 49a, D-50764 Cologne, Gelmany, E-mail: [email protected] 631 Periton Lane, Minehead, Somerset, TA24 SAQ, UK, [email protected] ABSTRACT: KostAK, M., QCH, S., EKRT, E., MAzUCH, M., WIESE, F., VOIGT, S. & WOOD, C.l 2004. Belemnites of the Bohemian Cretaceous Basin in a global context. Acta Geologica Polonica, 54 (4), 511-533. Warszawa. Belemnites occur infrequently from the Upper Cenomanian through the Middle/Upper Coniacian in the Bohemian Cretaceous. Four species of the family Belemnitellidae PAVLOW, 1914 have been described so far. A typical boreal fau nal incursion, represented by belemnites, happened five to six times in the Bohemian Cretaceous Basin (BCB). Praeactinocamax plenus immigrated during the Late Cenomanian Metoicoceras geslinianum ammonite Zone (plenus Event); there were two short-term incursions of P. bohemicus in the Late Turonian (Subplionocyclus neptuni to Plionocyclus gelmali ammonite zones) and an incursion of Goniocamax lundgreni in the late Early Coniacian (below and intra-Cremnoceramus crassus inoceramid Zone). -
Geology and Paleontology of the Southwest Quarter of the Big Bend Quadrangle Shasta County, California
GEOLOGY AND PALEONTOLOGY OF THE SOUTHWEST QUARTER OF THE BIG BEND QUADRANGLE SHASTA COUNTY, CALIFORNIA By ALBERT F. SANBORN Geologist, Standard Oil Company of California Salt Lake City, Utah Special Report 63 CALIFORNIA DIVISION OF MINES FERRY BUILDING, SAN FRANCISCO, 1960 STATE OF CALIFORNIA EDMUND G. BROWN, Governor DEPARTMENT OF NATURAL RESOURCES eWITT NELSON, Director DIVISION OF MINES IAN CAMPBELL, Chief Special Report 63 Price 75$ , GEOLOGY AND PALEONTOLOGY OF THE SOUTHWEST QUARTER OF THE BIG BEND QUADRANGLE SHASTA COUNTY, CALIFORNIA By Albert F. Sandorn * OUTLINE OF REPORT ABSTRACT Abstract 3 The area covered by this report is the southwest quarter of the Big Bend quadrangle in the vicinity of lntroductu.il 3 the town of Big Bendj Shasta County) California. General stratigraphy 5 This region, which has been geologically unknown, contains sedimentary volcanic strata of Triassic system _ 5 and Mesozoic an( Pit formation (Middle and Upper Triassic) 5 * Cenozoic ages. Hosselkus limestone (Upper Triassic) 7 The Mesozoic deposits are composed of pyroclastic Brock shale (Upper Triassic) 7 rocks, lava flows, tuffaceous sandstone, argillite, and Modin formation (Upper Triassic) 8 limestone. The Mesozoic formations, from the oldest Hawkins Creek member T0 the youngest, are the Pit formation of Middle and I Devils Canyon member 10 jate Triassic age ; the Hosselkus limestone, the Brock Kosk member ll shale, and the Modin formation of Late Triassic age; . the Arvison formation of Early Jurassic age ; and the s sy em -—- -- - --- Bagley andesite and Potem formation of Early and Arvison formation (Lower Jurassic) 11 „•,,, T . ,-.., ., e ,. , ' „ , . .. .. __ . , T 1( Middle Jurassic age. Or the seven formations mapped,rr Nature of the contact of the Triassic and Jurassic svstems 14 ,. -
Taylorsville Region, California
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR 353 GEOLOGY OF THE TAYLORSVILLE REGION, CALIFORNIA BY J. S. DILLER WASHINGTON GOVERNMENT PRINTING OFFICE 1908 t f CONTENTS. Page Introduction.............................................................. 7 Location and extent................................................... 7 Outline of geography and geology of region.............................. 7 Topography............................................................... 9 Relief. ............................................................... 9 Diamond Mountain block.......................................... 9 The escarpment. .............................................. 10 The plateau slope.............................................. 10 Valleys on southwest border.................................... 10 Genesee Valley............................................. 10 Indian Valley............................................. 10 Mountain Meadows........................................ 11 Jura Valley................................................ 11 Grizzly Mountain block........................................... 11 Crest line and escarpment..................................... 11 Southwest slope............................................... .12 Drainage.............................................................. 12 Descriptive geology........................................................ 13 General statement........'............................................... 13 Sedimentary rocks.................................................... -
Fossil Brachiopods from the Pleistocene of the Antilles
Fossil brachiopods from the Pleistocene of the Antilles David A.T. Harper & Stephen K. Donovan Harper, D.A.T. & Donovan, S.K. Fossil brachiopods from the Pleistocene of the Antilles. Scripta Geologica, 135: 213-239, 3 fi gs., 3 pls, 1 table. Leiden, November 2007. David A.T. Harper, Geological Museum, University of Copenhagen, Øster Voldgade 5-7, DK-1350 Copen- hagen K, Denmark ([email protected]); Stephen K. Donovan, Department of Geology, Nationaal Natuurhistorisch Museum, Postbus 9517, NL-2300 RA Leiden, The Netherlands (donovan@naturalis. nnm.nl). Key words – Brachiopoda, Pleistocene, systematics, Jamaica, Barbados, Antilles. Pleistocene brachiopods are poorly known from the Antillean region, but are locally common in fore- reef deposits of Jamaica (lower Pleistocene Manchioneal Formation) and Barbados (Coral Rock). Of the four species known, two are new. Lacazella sp. cf. L. caribbeanensis Cooper, an encrusting thecideidean, is known from only three valves. Other species are terebratulides. Tichosina inconstanta sp. nov. is a large, ventribiconvex Tichosina species of elongate oval to tear-drop shaped outline, variably uniplicate with a pedicle foramen of moderate diameter. It differs from the similar Tichosina? bartletti (Dall) in having a larger pedicle foramen and a less-marked plication. Argyrotheca barrettiana (Davidson) is a medium to large, usually transverse Argyrotheca species, multicostellate with usually eight costae and costellae, in- creasing by intercalation up to 21 on the largest shell. The species was originally described from the Recent of the Caribbean. Terebratulina manchionealensis sp. nov. is a small, elongately oval to subtriangu- lar Terebratulina species with a ventral sulcus and subcarinate dorsal valve. -
Marine Gastropods from the Pogibshi Formation (Alaska) and Their Paleobiogeographical Significance
Andean Geology 47 (3): 559-576. September, 2020 Andean Geology doi: 10.5027/andgeoV47n3-3278 www.andeangeology.cl Early Jurassic (middle Hettangian) marine gastropods from the Pogibshi Formation (Alaska) and their paleobiogeographical significance *Mariel Ferrari1, Robert B. Blodgett2, Montana S. Hodges3, Christopher L. Hodges3 1 Instituto Patagónico de Geología y Paleontología, IPGP (CCT CONICET-CENPAT), Boulevard Alte. Brown 2915, (9120) Puerto Madryn, Provincia de Chubut, Argentina. [email protected] 2 Blodgett and Associates, LLC, 2821 Kingfisher Drive, Anchorage, Alaska 99502, USA. [email protected] 3 California State University Sacramento, 6000 J Street, Sacramento, California 95819, USA. [email protected]; [email protected] * Corresponding author: [email protected] ABSTRACT. A middle Hettangian marine gastropod assemblage is reported from the Kenai Peninsula of south-central Alaska supplying new paleontological evidence of this group in Lower Jurassic rocks of North America. Pleurotomaria pogibshiensis sp. nov. is described from the middle Hettangian marine succession informally known as Pogibshi formation, being the first occurrence of the genus in the Kenai Peninsula and the oldest occurrence of the genus in present-day Alaska and North America. One species of the genus Lithotrochus, namely Lithotrochus humboldtii (von Buch), is also reported for the first time from the Kenai Peninsula. Lithotrochus has been considered as endemic to South America for a time range from the early Sinemurian -
Permophiles International Commission on Stratigraphy
Permophiles International Commission on Stratigraphy Newsletter of the Subcommission on Permian Stratigraphy Number 66 Supplement 1 ISSN 1684 – 5927 August 2018 Permophiles Issue #66 Supplement 1 8th INTERNATIONAL BRACHIOPOD CONGRESS Brachiopods in a changing planet: from the past to the future Milano 11-14 September 2018 GENERAL CHAIRS Lucia Angiolini, Università di Milano, Italy Renato Posenato, Università di Ferrara, Italy ORGANIZING COMMITTEE Chair: Gaia Crippa, Università di Milano, Italy Valentina Brandolese, Università di Ferrara, Italy Claudio Garbelli, Nanjing Institute of Geology and Palaeontology, China Daniela Henkel, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany Marco Romanin, Polish Academy of Science, Warsaw, Poland Facheng Ye, Università di Milano, Italy SCIENTIFIC COMMITTEE Fernando Álvarez Martínez, Universidad de Oviedo, Spain Lucia Angiolini, Università di Milano, Italy Uwe Brand, Brock University, Canada Sandra J. Carlson, University of California, Davis, United States Maggie Cusack, University of Stirling, United Kingdom Anton Eisenhauer, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany David A.T. Harper, Durham University, United Kingdom Lars Holmer, Uppsala University, Sweden Fernando Garcia Joral, Complutense University of Madrid, Spain Carsten Lüter, Museum für Naturkunde, Berlin, Germany Alberto Pérez-Huerta, University of Alabama, United States Renato Posenato, Università di Ferrara, Italy Shuzhong Shen, Nanjing Institute of Geology and Palaeontology, China 1 Permophiles Issue #66 Supplement -
Applied Stratigraphy Topics in Geobiology
APPLIED STRATIGRAPHY TOPICS IN GEOBIOLOGY http://www.springeronline.com/sgw/cda/frontpage/0,11855,4-40109-69-33109783-0,00.html Series Editors: Neil H. Landman, American Museum of Natural History, New York, New York Douglas S. Jones, University of Florida, Gainesville, Florida Current volumes in this series Volume 23: Applied Stratigraphy Eduardo A. M. Koutsoukos Hardbound, ISBN, 1-4020-2632-3, 2005 Volume 22: The Geobiology and Ecology of Metasequoia Ben A. LePage, Christopher J. Williams and Hong Yang Hardbound, ISBN, 1-4020-2631-5, 2004 Volume 21: High-Resolution Approaches in Stratigraphic Paleontology Peter J. Harries Hardbound, ISBN 1-4020-1443-0, September 2003 Volume 20: Predator-Prey Interactions in the Fossil Record Patricia H. Kelley, Michal Kowalewski, Thor A. Hansen Hardbound, ISBN 0-306-47489-1, January 2003 Volume 19: Fossils, Phylogeny, and Form Jonathan M. Adrain, Gregory D. Edgecombe, Bruce S. Lieberman Hardbound, ISBN 0-306-46721-6, January 2002 Volume 18: Eocene Biodiversity Gregg F. Gunnell Hardbound, ISBN 0-306-46528-0, September 2001 Volume 17: The History and Sedimentology of Ancient Reef Systems George D. Stanley Jr. Hardbound, ISBN 0-306-46467-5, November 2001 Volume 16: Paleobiogeography Bruce S. Lieberman Hardbound, ISBN 0-306-46277-X, May 2000 Volume 15: Environmental Micropaleontology Ronald E. Martin Hardbound, ISBN 0-306-46232-X, July 2000 Volume 14: Neogene, Paleontology of the Manonga Valley, Tanzania Terry Harrison Hardbound, ISBN 0-306-45471-8, May 1997 Volume 13: Ammonoid Paleobiology Neil H. Landman, Kazushige Tanabe, Richard Arnold Davis Hardbound, ISBN 0-306-45222-7, May 1996 A Continuation Order Plan is available for this series. -
THE Geologlcal SURVEY of INDIA Melvioirs
MEMOIRS OF THE GEOLOGlCAL SURVEY OF INDIA MElVIOIRS OF THE GEOLOGICAL SURVEY OF INDIA VOLUME XXXVI, PART 3 THE TRIAS OF THE HIMALAYAS. By C. DIENER, PH.0., Professor of Palceontology at the Universz'ty of Vienna Published by order of the Government of India __ ______ _ ____ __ ___ r§'~-CIL04l.~y_, ~ ,.. __ ..::-;:;_·.•,· ' .' ,~P-- - _. - •1~ r_. 1..1-l -. --~ ·~-'. .. ~--- .,,- .'~._. - CALCU'l"l'A: V:/f/ .. -:-~,_'."'' SOLD AT THE Ol<'FICE OF THE GEOLOGICAL SURVEY o'U-1kI>i'A,- 27, CHOWRINGHim ROAD LONDON: MESSRS. KEGAN PAUT,, TRENCH, TRUBNER & CO. BERLIN : MESSRS. FRIEDLANDEH UND SOHN 1912. CONTENTS. am I• PA.GE, 1.-INTBODUCTION l 11.-LJ'rERA.TURE • • 3· III.-GENERAL DE\'ELOPMEKT OF THE Hrn:ALAYA.K TRIAS 111 A. Himalayan Facies 15 1.-The Lower Trias 15 (a) Spiti . Ip (b) Painkhanda . ·20 (c) Eastern Johar 25 (d) Byans . 26 (e) Kashmir 27 (/) Interregional Correlation of fossiliferous horizons 30 (g) Correlation with the Ceratite beds of the Salt Range 33 (Ti) Correlation with the Lower Trias of Europe, Xorth America and Siberia . 36 (i) The Permo-Triassic boundary . 42 II.-The l\Iiddle Trias. (Muschelkalk and Ladinic stage) 55 (a) The Muschelkalk of Spiti and Painkhanda v5 (b) The Muschelkalk of Kashmir . 67 (c) The llluschelka)k of Eastern Johar 68 (d) The l\Iuschelkalk of Byans 68 (e) The Ladinic stage.of Spiti 71 (f) The Ladinic stage of Painkhanda, Johar and Byans 75 (g) Correl;i.tion "ith the Middle Triassic deposits of Europe and America . 77 III.-The Upper Trias (Carnie, Korie, and Rhretic stages) 85 (a) Classification of the Upper Trias in Spiti and Painkhanda 85 (b) The Carnie stage in Spiti and Painkhanda 86 (c) The Korie and Rhretic stages in Spiti and Painkhanda 94 (d) Interregional correlation and homotaxis of the Upper Triassic deposits of Spiti and Painkhanda with those of Europe and America 108 (e) The Upper Trias of Kashmir and the Pamir 114 A.-Kashmir .