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The Lower Triassic System in the Abrek Bay area, South Primorye, Russia Edited by Yasunari Shigeta Yuri D. Zakharov Haruyoshi Maeda Alexander M. Popov National Museum of Nature and Science Tokyo, March 2009 v Contents Contributors .................................................................vi Abstract ....................................................................vii Introduction (Y. Shigeta, Y. D. Zakharov, H. Maeda, A. M. Popov, K. Yokoyama and H. Igo) ...1 Paleogeographical and geological setting (Y. Shigeta, H. Maeda, K. Yokoyama and Y. D. Zakharov) ....................3 Stratigraphy (H. Maeda, Y. Shigeta, Y. Tsujino and T. Kumagae) .........................4 Biostratigraphy Ammonoid succession (Y. Shigeta, H. Maeda and Y. D. Zakharov) ..................24 Conodont succession (H. Igo) ...............................................27 Correlation (Y. Shigeta and H. Igo) ...........................................29 Age distribution of detrital monazites in the sandstone (K. Yokoyama, Y. Shigeta and Y. Tsutsumi) ..............................30 Discussion Age data of monazites (K. Yokoyama, Y. Shigeta and Y. Tsutsumi) ..................34 The position of the Abrek Bay section in the “Ussuri Basin” (Y. Shigeta and H. Maeda) ...36 Ammonoid mode of occurrence (H. Maeda and Y. Shigeta) ........................36 Aspects of ammonoid faunas (Y. Shigeta) ......................................38 Holocrinus species from the early Smithian (T. Oji) ..............................39 Recovery of nautiloids in the Early Triassic (Y. Shigeta) -
Contributions in BIOLOGY and GEOLOGY
MILWAUKEE PUBLIC MUSEUM Contributions In BIOLOGY and GEOLOGY Number 51 November 29, 1982 A Compendium of Fossil Marine Families J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions in BIOLOGY and GEOLOGY Number 51 November 29, 1982 A COMPENDIUM OF FOSSIL MARINE FAMILIES J. JOHN SEPKOSKI, JR. Department of the Geophysical Sciences University of Chicago REVIEWERS FOR THIS PUBLICATION: Robert Gernant, University of Wisconsin-Milwaukee David M. Raup, Field Museum of Natural History Frederick R. Schram, San Diego Natural History Museum Peter M. Sheehan, Milwaukee Public Museum ISBN 0-893260-081-9 Milwaukee Public Museum Press Published by the Order of the Board of Trustees CONTENTS Abstract ---- ---------- -- - ----------------------- 2 Introduction -- --- -- ------ - - - ------- - ----------- - - - 2 Compendium ----------------------------- -- ------ 6 Protozoa ----- - ------- - - - -- -- - -------- - ------ - 6 Porifera------------- --- ---------------------- 9 Archaeocyatha -- - ------ - ------ - - -- ---------- - - - - 14 Coelenterata -- - -- --- -- - - -- - - - - -- - -- - -- - - -- -- - -- 17 Platyhelminthes - - -- - - - -- - - -- - -- - -- - -- -- --- - - - - - - 24 Rhynchocoela - ---- - - - - ---- --- ---- - - ----------- - 24 Priapulida ------ ---- - - - - -- - - -- - ------ - -- ------ 24 Nematoda - -- - --- --- -- - -- --- - -- --- ---- -- - - -- -- 24 Mollusca ------------- --- --------------- ------ 24 Sipunculida ---------- --- ------------ ---- -- --- - 46 Echiurida ------ - --- - - - - - --- --- - -- --- - -- - - --- -
Memorial to Brian Frederick Glenister
Memorial to Brian Frederick Glenister (1928–2012) DESMOND COLLINS 501-437 Roncesvalles Avenue, Toronto, Ontario M6R 3B9, Canada GILBERT KLAPPER Department of Earth and Planetary Sciences, Northwestern University, Evanston, Illinois 60208, USA W.W. NASSICHUK Geological Survey of Canada, 3303 33rd Street NW, Calgary, Alberta, T2L 2A7, Canada HOLMES SEMKEN Department of Geoscience, University of Iowa, Iowa City, Iowa 52242, USA CLAUDE SPINOSA Department of Geosciences, Boise State University, Boise, Idaho 83725 Brian F. Glenister, 83, a leading researcher on Paleozoic ammonoids, passed away on 7 June 2012 in Phoenix, Arizona. He was an influential member of the International Stratigraphic Commission and several of its subcommissions, led many seminars on Holocene lithofacies and molluscan biofacies in Florida Bay, and was an inspiring teacher for almost forty years at The University of Iowa in Iowa City. Brian was born in Albany, Western Australia on 28 September 1928 into a large family whose father died four years later. He was then raised by his eldest sister but also encouraged greatly in his studies by his mother. He attended the University of Western Australia in Perth, where he received a B.Sc., majoring in physics in 1948. Brian had taken an introductory geology course in order to fulfill requirements for the degree, and decided that he Brian Glenister at the Conklin Quarry in the liked it enough to switch to geology at the first opportunity, Middle Devonian Cedar Valley Limestone near so he took a postgraduate year of geology courses in Perth Iowa City, 1964, courtesy Desmond Collins. in 1949. In 1950, he enrolled in the M.Sc. -
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. -
Early Changhsingian (Late Permian) Ammonoids from NW Iran
N. Jb. Geol. Paläont. Abh. 293/1 (2019), 37–56 Article E Stuttgart, July 2019 Early Changhsingian (Late Permian) ammonoids from NW Iran Dieter Korn, Abbas Ghaderi, and Nahideh Ghanizadeh Tabrizi With 25 figures Abstract: Early Changhsingian ammonoids from the Transcaucasus-NW Iranian region are poorly known. Here we revise the ammonoids of this interval based on new findings in sections of the Aras Valley and Ali Bashi Mountains of the Julfa region, NW Iran. We revise the ceratitid genera Phisonites, Iranites, Shevyrevites and Dzhulfites. We introduce the new genus Araxoceltites with the three new species A. sanestapanus, A. laterocostatus and A. cristatus. Key words: Late Permian, Ammonoidea, Iran, stratigraphy, diversity. 1. Introduction a high species richness, those from the Transcaucasus are comparatively poor. In their monograph describing Late Permian (Lopingian) ammonoids are remarkable the sections in Armenia and Azerbaijan, for instance, for their high overturn rates, which stand in contrast to Ruzhencev & Shevyrev (1965) listed only eight the Early and Middle Permian, during which the group xenodiscid species from this interval. This is in strik- evolved considerably slowly on the substage and stage ing contrast to the late Changhsingian, from where levels (e.g., Miller & Furnish 1940; Ruzhencev alone nearly 30 species are known from the Paratiro- 1952; Ruzhencev 1956; Leonova 2002). The Late lites Limestone of NW Iran (Korn et al. 2016). A Permian is, after the end-Guadalupian extinction event diversity analysis showed that the ammonoid diver- that caused a significant extinction of the goniati- sity is increasing towards the top of the formation tid ammonoids, characterized by the presence of am- (Kiessling et al. -
Paleontological Contributions
THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS May 15, 1970 Paper 47 SIGNIFICANCE OF SUTURES IN PHYLOGENY OF AMMONOIDEA JURGEN KULLMANN AND JOST WIEDMANN Universinit Tubingen, Germany ABSTRACT Because of their complex structure ammonoid sutures offer best possibilities for the recognition of homologies. Sutures comprise a set of individual elements, which may be changed during the course of ontogeny and phylogeny as a result of heterotopy, hetero- morphy, and heterochrony. By means of a morphogenetic symbol terminology, sutural formulas may be established which show the composition of adult sutures as well as their ontogenetic development. WEDEKIND ' S terminology system is preferred because it is the oldest and morphogenetically the most consequent, whereas RUZHENTSEV ' S system seems to be inadequate because of its usage of different symbols for homologous elements. WEDEKIND ' S system includes only five symbols: E (for external lobe), L (for lateral lobe), I (for internal lobe), A (for adventitious lobe), U (for umbilical lobe). Investigations on ontogenetic development show that all taxonomic groups of the entire superorder Ammonoidea can be compared one with another by means of their sutural development, expressed by their sutural formulas. Most of the higher and many of the lower taxa can be solely characterized and arranged in phylogenetic relationship by use of their sutural formulas. INTRODUCTION Today very few ammonoid workers doubt the (e.g., conch shape, sculpture, growth lines) rep- importance of sutures as indication of ammonoid resent less complicated structures; therefore, phylogeny. The considerable advances in our numerous homeomorphs restrict the usefulness of knowledge of ammonoid evolution during recent these features for phylogenetic investigations. -
Early Permian Ammonoids from the Takakurayama Area, Abukuma Mountains, Northeast Japan Masayuki FUJIKAWA* and Chisato SUZUKI**
Sci. Rep., Niigata Univ. (Geology), No. 26, 61-72, 2011 61 Early Permian ammonoids from the Takakurayama area, Abukuma Mountains, northeast Japan Masayuki FUJIKAWA* and Chisato SUZUKI** Abstract Four ammonoid species, Thalassoceras? sp., Artinskia sp., Agathiceras sp., and Paragastrioceras? sp., are described from the lower part of the Takakurayama Formation in the Takakurayama area, Abukuma Mountains, northeast Japan. This fauna indicates an Early Permian (Sakmarian-Artinskian) age. Three of these species except for Agathiceras sp. are described from the Takakurayama Formation for the first time. Key words: Abukuma Mountains, ammonoid, Early Permian, Takakurayama. Introduction The Permian Takakurayama Formation (Onuki, 1966) is widely distributed in the Takakurayama area, Abukuma Mountains, South Kitakami Belt, northeast Japan (Fig. 1). The formation is exposed on the northeastern slope of Mt. Takakurayama, where it generally strikes NNE-SSW and dips at 30-45º to the west. It consists mainly of black shale with subordinate sandstone and conglomerate, and is more than 805 m in total thickness (Fig. 2). The formation is subdivided into three members: the Iriishikura, Motomura, and Kashiwadaira members, in ascending order (Onuki, 1966). These members are equivalent to the Iriishikura, Motomura, and Kashiwadaira formations proposed by Yanagisawa and Nemoto (1961). Here, we adopt Onuki’s scheme, and refer to the lower part of the Takakurayama beds as the Iriishikura Member. This paper describes ammonoid specimens * Akiyoshi-dai Museum of Natural History, Mine, Yamaguchi 754-0511, Japan ** Yotsukura-machi, Aza Nishi 2-6-3, Iwaki, Fukushima 979-0201, Japan (Manuscript received 13 December, 2010; accepted 22 February, 2011) 62 M. Fujikawa and C. -
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. -
Back Matter (PDF)
Index Page numbers in italics refer to Figures. Page numbers in bold refer to Tables. Abadeh Section (Iran) 74, 81, 83, 112 Annweiler Formation 397 Abadehceras 198 Anomalonema reumauxi–Peudestheria simoni assemblage Abichites 199 zone 370, 372–373 Abo Formation 73, 408, 409, 412, 425 Antarctica, palynostratigraphy 337 Abrahamskraal Formation 64, 78, 80, 418, 428 Anthracolithic System 25 radiometric dating 86 Anuites 193 Abrek Formation 295 Apache Dam Formation 409 acritarchs 322–323 Aquaw Creek (Colorado), magnetic polarity data 66 Admiral Formation 410 Arabia, palynostratigraphy 333, 333 Adrianites 194 Arabia Plate, fusuline biostratigraphy 255 A. elegans 195 Araksian Stage 40 Afghanistan Arasella 199 fusuline biostratigraphy 255, 260–261 Araxoceras spp. 196, 198 Agathiceras 187, 189 A. latissimum 198 Aidaralash CreekGSSP (Kazakstan)3, 28,29, 32, 53,67, 88,187,321,325 A. ventrosulcatum 198 Akiyoshi Terrane, fusuline biostratigraphy 270–271, 271 Archer City Formation 410, 411 Akmilleria 189 archosaurs 51 Aktastinian Substage 2, 33, 189 Argentina ammonoid assemblages 185 magnetic polarity data 64, 69, 72 Aktasty River Section 33 palynostratigraphy 330, 331, 331 Aktastynian Stage, ammonoid assemblages 185 tetrapods 387 Aktubinskia 189 Aricoceras 192 Aktyubinsk section 33 Aristoceras 187 Al Khlata Formation 336 Aristoceratoides 194 Alaska Region, fusuline biostratigraphy 255 Arizona, tetrapods 412–413 Albaillella cavitata interval zone 154, 157 Arnhardtia 39 Albaillella excelsa interval zone 155 Arrayo de Alamillo Formation 395, 409 Albaillella levis interval zone 155 Arroya del Agua Formation 408, 409, 425 Albaillella sinuata abindance zone 148–149 Arroya Formation 410 Albaillella triangularis interval zone 155, 157 Arroyo Vale Formation 411 Albaillella xiaodongensis assemblage zone 148 Artinskia spp. -
End-Permian Mass Extinctions: a Review
Geological Society of America Special Paper 356 2002 End-Permian mass extinctions: A review Douglas H. Erwin* Department of Paleobiology, MRC-121, National Museum of Natural History, Washington, D.C. 20560, USA Samuel A. Bowring Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, 77 Massachusetts Avenue, Cambridge, Massachusetts 02130, USA Jin Yugan Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China ABSTRACT Two mass extinctions brought the Paleozoic to a close: one at the end of the Guadalupian, or middle Permian (ca. 260 Ma), and a more severe, second event at the close of the Changhsingian Stage (ca. 251.6 Ma). Here we review work over the past decade that defines the probable causes of the mass extinction, and evaluate several extinction hypotheses. The marine extinctions were selective; epifaunal sus- pension feeders were more affected than other clades, although significant variations occurred even among the filter feeders. In southern China, the Changhsingian marine extinction was nearly catastrophic, occurring in Ͻ0.5 m.y. On land, vertebrates, plants, and insects all underwent major extinctions. The event coincides with (1) a in both marine and terrestrial ‰2 to ‰2drop of d13C in carbonates, from ϳ sections; (2) the eruption of the massive Siberian continental flood basalts; and (3) evidence of shallow-water marine anoxia, and perhaps deep-water anoxia. Although the cause of the extinction remains unclear, a series of constraints on speculation have been established in the past few years. Leading contenders for the cause are the cli- matic effects, including acid rain and global warming, possibly induced by the erup- tion of the Siberian flood basalts; and marine anoxia. -
A New Griesbachian–Dienerian (Induan, Early Triassic) Ammonoid Fauna from Gujiao, South China
Journal of Paleontology, 93(1), 2019, p. 48–71 Copyright © 2018, The Paleontological Society 0022-3360/15/0088-0906 doi: 10.1017/jpa.2018.46 A new Griesbachian–Dienerian (Induan, Early Triassic) ammonoid fauna from Gujiao, South China Xu Dai,1 Haijun Song,1 Arnaud Brayard,2 and David Ware3 1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China 〈[email protected]〉, 〈[email protected]〉 2Biogéosciences, UMR 6282, CNRS, Université Bourgogne Franche-Comté, 6 Boulevard Gabriel, 21000 Dijon, France 〈[email protected]〉 3Museum für Naturkunde, Leibniz Institute for Evolution and Biodiversity Science, Invalidenstrasse 43, 10115 Berlin, Germany 〈[email protected]〉 Abstract.—Bed-by-bed sampling of the lower portion of the Daye Formation at Gujiao, Guizhou Province, South China, yielded new Griesbachian–Dienerian (Induan, Early Triassic) ammonoid faunas showing a new regional Induan ammonoid succession. This biostratigraphic scheme includes in chronological order the late Griesbachian Ophiceras medium and Jieshaniceras guizhouense beds, and the middle Dienerian Ambites radiatus bed. The latter is recognized for the first time as a separate biozone in South China. Eight genera and 13 species are identified, includ- ing one new species, Mullericeras gujiaoense n. sp. The new data show that a relatively high level of ammonoid taxonomic richness occurred rather rapidly after the Permian/Triassic mass extinction in the late Griesbachian, echo- ing similar observations in other basins, such as in the Northern Indian Margin. UUID: http://zoobank.org/a24a3387-f3dd-4da4-a134-84372352a63d Introduction Early Triassic (Brayard et al., 2006, 2009a; Brühwiler et al., 2010a; Ware et al., 2015). -
Paleontological Research
Paleontological Research ISSN 1342-8144 Formerly Transactions and Proceedings of the Palaeontological Society of Japan Vol. 5 No.3 September 2001 The Palaeontological Society of Japan Co-Editors Kazushige Tanabe and Tomoki Kase Language Editor Martin Janal (New Yorl<, USA) Associate Editors Alan G. Beu (Institute of Geological and Nuclear Sciences, Lower Hutt, New Zealand), Satoshi Chiba (Tohoku University, Sendai , Japan), Yoichi Ezaki (Osaka City University, Osaka, Japan), James C. lngle, Jr. (Stanford University, Stanford, USA), Kunio Kaiho (Tohoku University, Sendai, Japan), Susan M. Kidwell (University of Chicago, Chicago, USA), Hiroshi Kitazato (Shizuoka University, Shizuoka, Japan), Naoki Kohno (National Science Museum, Tokyo, Japan), Neil H. Landman (Amemican Museum of Natural History, New York, USA), Haruyoshi Maeda (Kyoto University, Kyoto, Japan), Atsushi Matsuoka (Niigata University, Niigata, Japan) , Rihito Morita (Natural History Museum and Institute, Chiba, Japan), Harufumi Nishida (Chuo University, Tokyo, Japan), Kenshiro Ogasawara (University of Tsukuba, Tsukuba, Japan), Tatsuo Oji (University of Tokyo, Tokyo, Japan), Andrew B. Smith (Natural History Museum, London, Great Britain), Roger D. K. Thomas (Franklin and Marshall College, Lancaster, USA), Katsumi Ueno (Fukuoka University, Fukuoka, Japan), Wang Hongzhen (China University of Geosciences, Beijing, China), Yang Seong Young (Kyungpook National University, Taegu, Korea) Officers for 2001 - 2002 President: Hiromichi Hirano Councillors: Shuko Adachi , Kazutaka Amano,