DOCSLIB.ORG

Nautiloid Cephalopods from the Julfa Beds, Upper Permian, Northwest Iran

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Nautiloid Cephalopods from the Julfa Beds, Upper Permian, Northwest Iran NAUTILOID CEPHALOPODS FROM THE JULFA BEDS, UPPER PERMIAN, NORTHWEST IRAN CURT TEICHERT' AND BERNHARD KUMMEL" Aii.sTRACT. Sexenteen species of niiutiloid ceph- Abich (1878), who described the following alopods, from the Upper Permian Julfa Beds of the Araks Araxes west species from ( ) Gorge northwestern Iran are descrihed and discnssed. of Soviet Dzhulfa (the modern generic as- Tlie\ belong to t\\el\e genera. Eight of the species is in : are assigned to, or compared with, pre\iously de- signment placed parentheses ) scrihed species; the remainder is left nnnamed. This Nautilus excentricus Eichwald appears to be one of the richest nantiloid faunas known from beds of very Late Permian age. {Permonautilus) Nautilus propiiKjuus Abich INTRODUCTION (Liroceras) Nautiloicls of Late Permian age are ex- Nautilus parallelus Abich tremely imeommon. In coimeetion with our {Doniatoccras) study of tlie Ali Bashi Formation'' at Kuli-e- Nautilus convergens Abich Ali Ha.slii near Julfa, northwestern Iran (Stenopoceras) (Teichert, Kimimel, and Sweet, in press; Nautilus concavus Sowerby Kummel and in Teichert, 1971, and press), (Liroceras) we were al^le to collect a fairK' large fauna Nautilus clolerus Abich of nautiloids from the underhing Julfa (Doniatoceras) Beds. This is report a description and dis- Nautilus dorsoannatus Abich cussion of this fauna. (Metacoceras) We wish to acknowledge assistance re- Nautilus picJileri v. Hauer ceived from Victoria Kohler, at Harvard (Pleuronautilus) University, and William L. Fisher, at the Nautilus incertus Abich University of Kansas. The material \\'as (Pleuronautilus) collected in 1968, during field work sup- Nautilus tubercularis Abich ported bv National Science Foundation Grant GA-996. (Pleuronautilus) Nautilus (lorsoplicatus Abich PREVIOUS WORK ( Tainoceras) The first record of nautiloids from the Nautilus armeniacus Abich Late Permian of the Transcaucasus was by ( Pseudotitanoceras) Nautilus cornutus Golovinski ^ University of Kansas. (Permonautilus) " Harvard University'. Oiihoceras annulatum ^ Sowerby This formation is being described by Teichert, ( ?Neocycloccras) Kummel, and Sweet (in press). It conesponds Orthoceras cribrosum Geinitz essentially to the "Transition beds" plus "Paiatiro- lites beds" et al. of Stepanov ( 1969 ) (?) Bull. Mus. Comp. ZooL, 144(6): 409-434, March, 1973 409 410 BiiUetin Museum of Comparative Zoology, Vol. 144, No. 6 Orthoceras transversum Abich '"Domatoceras atypicum Shimanskiy (?) ^•'^Domatoceras hunicum (Diener) Orthoceras hicinctum Abich "Domatoceras gracile Shimanskiy k-t:- (") Domatoceras parallehim (Abich) Orthoceras margaritatum Abich Domatoceras cf. gracile Shimanskiy 1 ( ?Neocyc!oceras ) ^^Domatoceras sp. Orthoceras turriteUum Abich ^Pseudotitanoceras arrneniacum (Abich) (?) Permonautihis abichi (Kruglov) Permonautilus sp. Regardless of whether or not the species *'^-?Stearoceras sp. are narrowly defined, for a late Paleozoic ^^Paranautilus pcrcgrimis (Waagen) fauna this an impressively diverse list. In a "Styrioiiaufilus sp. rcstudy of the Soviet Dzhulfian fauna Art- '^*Neocycloceras obUqueannulatum haber (in Freeh and Arthaber, 1900) intro- ( Waagen ) duced only one new species, namely, Pleuro- cf. nautihts verae Arthaber. Even the review of *^?NeocycIoceras cyclophorum ( Waagen ) the stratigraph}' and of these paleontolog)- Abich beds 1910 resulted in **?NeocycIoceras marg(iritatu)n ( ) by Stoyanow ( ) only ?Neocycloceras cf. margaritatum two new species of nautiloids—Orthoceras (Abich) lopingense Stoyanow and Nautihis himiciis lopingense (Stoyanow) Diener. In fact these are the only nautiloids "^Lopingoceras Lopingoceras cf. lopingense (Stoya- described by Stoyanow in that report. In the comprehensive monograph on now) hicinctum the Permo-Triassic formations of So\det ^^'Cycloceras (Abich) Dzhulfa, edited V. E. Ruzhentsev and by Only six of these species were com- T. G. 1965 , the nautiloids were Sarycheva ( ) pletely described and illustrated in the text. studied Shimanski\', who the by recognized These are indicated by a single asterisk in from the Araxoceras and following species the above list. A number of species were Vedioceras beds: illustrated on plates but were not described "^Tainoceras in the text, and these are indicated in the dorsopUcatum ( Abich ) above list a double asterisk. A few '^^Metacoceras dorsoarmatum (Abich) by gen- eral comments on this impressive list of Metacoceras sp. 1 (ex. gr. dorsoarma- are in order. Pseudotemnocheilus tum Abich) species we regard as a synonym of Temnocheilus. ^^Pseudotemm:>cJ}eihis sp. The illustration by Shimanskiy (in Ruz- '^'^Foordiceras sp. 1 hentsev and 1965, ]}\. 14, fig. 7) ^^Foordiceras cf. grypoceroides (Reed) Sar)'cheva, of a specimen of Pseudotemnocheilus is very "'^Foordiceras cf. flemingiamim (Kon- poor, but it seems to be possibly conspecific inck ) with what we describe here as Temno- ""^Tirolonautihis sp. " * cheilus sp. indet. The illustrations of the ?Hexago) i ites sp . various of Foordiceras to be ^"Pleuronaiitihis incertus (Abich) species appear similar to we to Pleuro- Pleuronautihis ci. incertus (Abich) specimens assign Pleuronaiitilus verae (Arthaber) nautilus sp. indet. 2. Tirolonautilus sp. and '^^Pleuronautilus tuhercularis (Abich) Hexagonites sp. were both based on single, "Pleuronautihis dzJndfensis Shimanskiy \'ery fragmentary specimens. On the basis "Pleuroiiautihis costalis Shimanskiy of the illustrations of these specimens, we Pleuronautilus sp. do not believe that they are generically ^"?Phaedrysmocheilus sp. identifiable. The generic identification of ^-^Domatoceras convergens (Abich) Phaedrysmocheilus and Stearoceras were Upper Permian Nautiloids, Iran • Tcidieii and Kummcl 411 (juestioned by Shimanskiy, and. on the basis does not include Pernwnautilus. Faranau- of the ilkistrations he presented, we agree tiJii.s, and Styriotwutihi.s. that these identifications are doubtful. Ex- In an analysis of the nautiloid fauna of the ckiding the orthoccrids it appears that this Julfa Beds it is important to consider the nautiloid fauna of Soviet Dzhulfa includes fauna of the overlying Ali Bashi Fonnation. nine genera, which, as late Paleozoic nau- It is these strata that are of prime impor- tiloid faunas go, is a large number. tance in consideration of the Permian- Triassic boundary of this region. Shimanski}' PRESENT INVESTIGATIONS (in Ruzhentse\- and Sarycheva. 1965: 41) listed the from the The specimens described in the present following species equiv- alents of the Ali Bashi Formation at So\'iet paper were collected by us from that part Dzhulfa beds beds 1-4 of of the section which Stepano\- et ul. (1969) {Phisonitc.s plus the "Induan called Julfa Beds. These correspond to the stage"): Dzhulfian of Stage ( Dzhulfinskiy Yarns) Tainuceras sp. 1 (ex. gr. cluingliiigpiiciise Grunt, and Ru- Arakclyan, Shevyrev {in Chao) zhentsev and 1965: 23). .\11 col- Sarycheva. Tainocero.s sp. 2 (ex. gr. changlingpuense lections were obtained in a small side valley, Chao) to the main access \'alle\' to Kuh- parallel Tainoccra.s sp. 3 8 of and c-Ali Bashi, about km west Julfa Metacoceras sp. 2 (ex. gr. dorsoainuitinn about 200-300 m upstream from our .\li Abich) Bashi locality 4 (Teichert, Kummel, and PFoordice ras s p . 2 Fleuronautilus dieneri v. Sweet, in press). Our collections contain sp. (ex. gr. the following genera and species: Krafft) PFIeuronautilus sp. Lopiuiioccras Iopingen.se (Stoyanow) Tainionautilus sp. cf. L. Lopingoceras sp. lopingense (Stoy- Domatoceras sp. 2 anow ) PSyringomiutihis vagus Shimanskiy Ne cloce ras cf. N. ocy sp. ohJiqueannulatum ?Faranautilus sp. (\\'aagen) PNeocycloceras sp. Tainoceras sp. indet. Onl\- Metacoceras- (lorasluimeme Shimanskiy PSyringonautilus vagus Shimanski)' was described and illustrated in Ruzhen- Metacoceras dorsoarnuitum (Abich) ( tsev and 1965: 163, 16, PlcuroiuiutiJiis sp. indet. 1 Sarycheva, pi. fig. Most of the were Fleuronautilus sp. indet. 2 9). remaining species illustrated b\' Tainiondutihis sp. indet. photographs, unaccompanied The to TeninoclicUus sp. indet. by descriptions. specimen assigned Doiiuitoccra.s Jninicmn (Diener) PSyringonautilus. to judge from the illustra- Domatoceras paralleJuni (Abich) tion, appears to be more likeK' to represent Donmtoceras sp. indet. a species of Stearoceras. Stenopoceras sp. indet. Teichert, Kummel, and Sweet (in press) Titanoccros indet. sp. describe the following species of nautiloids Pscudotitanoccra.s armeniacum (Abich) from the Ali Bashi Formation at Kuh-e-Ali Lirocera.s indet. sp. Bashi: This fauna is essentialh" the same as that PDoIorthoceras sp. from the beds at Soviet corresponding Neocycloceras sp. Dzhulfa for the of Teni- except presence Lopingoceras sp. nocheihis, Tainionautilu.s, and Titonoceras. Tainoceras sp. indet. .\t the same time the Kuh-e-Ali Bashi fauna Metacoceras sp. indet. 412 Bulletin Museum of Comparative Zoology, Vol. 144, No. 6 Table I DlSTRIBUTIOX OF NaUTILOID GeNERA IX JuLFA Beds axd Ali Bashi Formatiox Upper Permian Nautiloids, Iran • Teichert and Kummel 413 Figure 1. Diagram showing inferred phylogeny and geologic distribution of late Paleozoic and Triassic coiled nautiloids. (Adapted from Kummel, 1953.) Vol. No. 6 414 Bulletin Museum of Comparative Zoology, 144, estab- MCZ 9776 4, unfigured speci- placed Lopingoceras in his newly (PI. fig. 11), with- men KU 34435. lished family, Pseudocycloceratidae, out stating reasons. Lop/ngoceras sp. cf. L. lopingense Lopingoceras lopingense (Stoyanow) (Stoyanow) Plate 4, figures 13, 14 Plate 4, figures 9, 1 1 Our collections
Load more

Recommended publications
  • Cephalopods) from the Carboniferous of the Donets Basin (Eastern Ukraine
    Дослідницькі та огляДоВІ статті Research AND Review Papers https://doi.org/10.30836/igs.1025-6814.2021.2.227012 UDC 564.53:551.735.2(477.61) V.S. DERNOV Institute of Geological Sciences of the NAS of Ukraine, Kyiv, Ukraine е-mail: [email protected] * Corresponding author THREE NEW SPECIES OF NAUTILIDS (CEPHALOPODS) FROM THE CARBONIFEROUS OF THE DONETS BASIN (EASTERN UKRAINE) Three new species of nautilids (Gzheloceras aisenvergi sp. nov., Knightoceras extorris sp. nov. and Planetoceras yefimenkoi sp. nov.) have been described from the Carboniferous of the Donets Basin (Ukraine). Gzheloceras aisenvergi sp. nov. is mor- phologically close to the “Gzheloceras” orthocostatum (Kruglov, 1939) and Gzheloceras memorandum Shimansky, 1967. Knightoceras oxylobatum Miller et Downs, 1948 and K. patulum (Unklesbay, 1962) are the most morphologically related species to the K. extorris sp. nov. The form of the conch and the surface ornamentation of Planetoceras yefimenkoi sp. nov. are most similar to the type of genus (Planetoceras retardum Hyatt, 1893). The new data are expanding the taxonomic composition of the genera Gzheloceras, Knightoceras, and Planetoceras and also clarify their geographical distribution. Keywords: Cephalopoda; Nautilida; Carboniferous; Donets Basin; Ukraine. Introduction sippian and the Pennsylvanian of the Donets Basin (Eastern Ukraine) in result of studying the collec- Sediments of the Carboniferous system are in- tion of cephalopod remains. These species are de- volved in the geological structure of a significant scribed below. part of the territory of Ukraine. Unfortunately, the level of study of Carboniferous in different parts of Ukraine is not the same. Remains of nautiloids are History of research found in the Carboniferous deposits of the Don- Dnieper Downwarp (Dernov, 2018; Librovitch, Mississippian cephalopods of the Donets Basin are 1939) and the Lviv Paleozoic Downwarp (Shulga, very poorly studied.
    [Show full text]
  • 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 ------ - --- - - - - - --- --- - -- --- - -- - - ---
    [Show full text]
  • Non-Equilibrium Evolution of Volatility in Origination and Extinction Explains Fat-Tailed Fluctuations in Phanerozoic Biodiversi
    Non-equilibrium evolution of volatility in origination and extinction explains fat-tailed fluctuations in Phanerozoic biodiversity One sentence summary: Phanerozoic marine invertebrate richness fluctuates out of equilibrium due to pulsed adaptive evolution. Andrew J. Rominger1, *, Miguel A. Fuentes1, 2, 3, and Pablo A. Marquet1, 4, 5, 6, 7, 8 1Santa Fe Institute, 1399 Hyde Park Road, Santa Fe, New Mexico 87501, US 2Instituto de Investigaciones Filos´oficas,SADAF, CONICET, Bulnes 642, 1428 Buenos Aires, Argentina 3Facultad de Ingenier´ıay Tecnolog´ıa,Universidad San Sebasti´an,Lota 2465, Santiago 7510157, Chile 4Departamento de Ecolog´ıa,Facultad de Ciencias Biol´ogicas,Pontificia Universidad de Chile, Alameda 340, Santiago, Chile 5Instituto de Ecolog´ıay Biodiversidad (IEB), Casilla 653, Santiago, Chile 6Laboratorio Internacional de Cambio Global (LINCGlobal), and Centro de Cambio Global UC, Pontificia Universidad Catolica de Chile, Santiago, Chile. 7Instituto de Sistemas Complejos de Vlapara´ıso(ISCV), Artiller´ıa470, Cerro Artiller´ıa, Valpara´ıso,Chile 8Centro de Ciencias de la Complejidad (C3), Universidad Nacional Aut´onomade M´exico. *To whom correspondence should be addressed, e-mail: [email protected] arXiv:1707.09268v3 [q-bio.PE] 10 May 2019 1 Fluctuations in biodiversity, both large and small, are pervasive through the fossil record, yet we do not understand the processes generating them. Here we extend theory from non-equilibrium statistical physics to describe the previously unaccounted for fat-tailed form of fluctuations in marine inver- tebrate richness through the Phanerozoic. Using this theory, known as super- statistics, we show that the simple fact of heterogeneous rates of origination and extinction between clades and conserved rates within clades is sufficient to account for this fat-tailed form.
    [Show full text]
  • Pre-Tertiary Stratigraphy and Upper Triassic Paleontology of the Union District Shoshone Mountains Nevada
    Pre-Tertiary Stratigraphy and Upper Triassic Paleontology of the Union District Shoshone Mountains Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 322 Pre-Tertiary Stratigraphy and Upper Triassic Paleontology of the Union District Shoshone Mountains Nevada By N. J. SILBERLING GEOLOGICAL SURVEY PROFESSIONAL PAPER 322 A study of upper Paleozoic and lower Mesozoic marine sedimentary and volcanic rocks, with descriptions of Upper Triassic cephalopods and pelecypods UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Page Abstract_ ________________________________________ 1 Paleontology Continued Introduction _______________________________________ 1 Systematic descriptions-------------------------- 38 Class Cephalopoda___--_----_---_-_-_-_-_--_ 38 Location and description of the area ______________ 2 Order Ammonoidea__-__-_______________ 38 Previous work__________________________________ 2 Genus Klamathites Smith, 1927_ __ 38 Fieldwork and acknowledgments________________ 4 Genus Mojsisovicsites Gemmellaro, 1904 _ 39 Stratigraphy _______________________________________ 4 Genus Tropites Mojsisovics, 1875_____ 42 Genus Tropiceltites Mojsisovics, 1893_ 51 Cambrian (?) dolomite and quartzite units__ ______ 4 Genus Guembelites Mojsisovics, 1896__ 52 Pablo formation (Permian?)____________________ 6 Genus Discophyllites Hyatt,
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Abrek Bay Area, South Primorye, Russia
    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)
    [Show full text]
  • Aui Geologie
    Available online at http://geology.uaic.ro/auig/ AUI Analele Stiintifice ale Universitatii “Al. I. Cuza” din Iasi GEOLOGIE Seria Geologie 59 (1) (2013) 73–87 New records of Norian coiled nautiloids from the Timon Klippe (Rarău Syncline, Eastern Carpathians, Romania) Paul Ţibuleac1 1 “Al. I. Cuza” University of Iaşi, Faculty of Geography and Geology, Department of Geology, 20A Carol I Blv., 700505 Iaşi, Romania Abstract Nautiloids were cosmopolitan species during the Mesozoic, being well-known from the worldwide realms. They could often be found togheter with the ammonites in the same beds, but the nautiloid fauna is much scarcer in the taxonomic diversification and frequency of records than the ammonites have been documented. Given this general background, on the one hand, and its diversity and particular records, on the other, the Timon Klippe could be regarded as important instance of Late Triassic nautiloids in the Eastern Carpathians. The present paper adds new coiled nautiloid records (Grypoceras sp. ?G. mesodicum HYATT, 1883), Syriongonautilus sp. (one of the latest occurrences of this genus), Syringoceras sp., Paranautilus simonyi (HAUER, 1849), and Proclydonautilus sp. (specimen with intermediate features between several Proclydonautilus species) to the previously-known fauna. Keywords: Late Triassic, coiled nautiloids, previous and new records. Introduction pending the collection of more specimens. The dynamics of genera development in The Triassic nautiloid fauna is mostly a the Boreal Realm suggested two major phases continuation
    [Show full text]
  • Zoologischer Jahresbericht
    MARINE BIOLOGIGAL LABORATORY. ZOOLOGISCHER JAHRESBERICHT FÜR 1884. HERAUSGEGEBEN VON DER ZOOLOGISCHEN STATION ZU NEAPEL III. ABTHEILUNG: MOLLUSCA, BRACHIOPODA. MIT REGISTER. REDIGIRT D". PAUL MAYER IN NEAPEL. BERLIN VERLAG VON R. FRIEDLÄNDER & SOHN 1885. Jö' I (. Alle Rechte vorhehalten. ; Inhalts-Übersicht. Mollusca. Seite A. Anatomie, Ontogenie u. s. w. (Ref.: Dr. J. W. /Spende? in Bremen) 93 B. Geographische Verbreitung. Systematik u. s.w. (Ref. ; Dr. W. Kohelt in Schwanheim 1 I. Lebende Mollusken 1 1. Geographische Verbreitung 12 2. Systematik 21 a. Allgemeines 21 b. Cephalopoda 21 c. Pteropoda 24 d. Gastropoda 24 e. Solenoconchae 47 f. Lamellibranchiata 47 3. Biologie, Verwendung, Nutzen etc 50 II. Fossile Mollusken 53 1 Übersicht der Schichtenfolgen 59 2. Systematik 66 a. Cephalopoda 66 b. Pteropoda 72 c. Gastropoda 73 d. Solenoconchae 85 e. Lamellibranchiata 85 Brachiopoda 123 A. Anatomie, Ontogenie etc. (Ref.: Dr./. W. f%e^«!/s im Haag; ... 124 B. Systematik, Faunistik etc. (Ref.: Dr. W. Kohelt] 126 Resister 131 Die Referate über Polnische Literatur rühren zum Theil von Herrn Prof. A. Wrzesnioicshi [A. AV.] in Warschau her. Ein * vor einem Titel bedeutet, daß die Arbeit dem Referenten nicht zu- gänglich gewesen ist. Die fetten Zahlen hinter den Titeln verweisen auf die Seiten, wo sich das Referat befindet. Zusätze des Referenten stehen in f 1. Aufp 53, 59 und 66 sind die Überschriften gemäss obiger Übersicht abzuändern aufp 46 mnss es heissen : C. Basommatophora. — Mollusca. A. Anatomie, Ontogenie u. s. w. (Für dieses Jahr an zweiter Stelle.) B. Geographische Verbreitung, Systematik, Biologie, Fossilia. (Referent: Dr. W. Kobelt in Schwanheim a/M.) I.
    [Show full text]
  • University of Michigan University Library
    CONTRIBUTIONS FROM TRE MUSEUM OF PALEONTOLOGY UNIVERSITY OF MICHIGAN VOL XI, No. 6, pp. 111-151 (4 pls, 9 k.) NO~E~~BEB30, 1953 LOWER MISSISSIPPZAN CEPHALOPODS OF MICHIGAN PART 11. COILED NAUTILOIDS BY A. K. MILLER and H. F. GARNER UNIVERSITY OF MICHIGAN PRESS ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Director: LEWIS B. KELLUM The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collections in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and also to individuals upon request. Correspondence should be directed to the University of Michigan Press. A list of the separate papers will be sent upon request. VOL. I. The Stratigraphy and Fauna of the Hackberry Stage of the Upper Devonian, by C. L. Fenton and M. A. Fenton. Pages xi+260. Cloth. $2.75. VOLS. II-V. Available in cloth. Parts sold separately in paper covers. VOLS. VI-X. Ten numbers each, sold separately. (See also inside back cover) VOL. XI. NO. 6. pp . 111-151 (4 pls.. 9 figs.) NOVE~ER30. 1953 LOWER R/IISSISSIPPIAN CEPHALOPODS OF MICHIGAN . PART I1. COILED NAUTILOIDS BY A . K . MILLER and H . F. GARNER CONTENTS Introduction .............................................................. Systematic descriptions .................................................... Family Rineceratidae Hyatt ............................................ Chouteauoceras Miller and Garner. gen . nov ......................... Chouteauoceras? ingenitor (Winchell) .......................... Chouteauoceras? sp . aff . C.? tessellatum (de Koninck) ............ Chouteauoceras? spp.......................................... Genus Rineceras Hyatt ............................................ Rineceras meekianunz (Winchell) ..............................
    [Show full text]
  • S Kaza Edimentary an Golovkin Y Earth Syst Sky Young Tems: Stratig
    Kazan Golovkinsky Young Scientists’ Stratigraphic Meeting, 2020 Sedimentary Earth Systems: Stratiggraphy, Geochronology, Petroleum Resources Kazan Golovkinsky Young Scientists’ Stratigraphic Meeting, 2020 Sedimentary Earth Systems: Stratiggraphy, Geochronology, Petroleum Resources Kazan Golovkinsky Young Scientists’ Strratigraphic Meeting, 2020 Sedimentary Earth Systems: Stratigraphy, Geocchronology, Petroleum Resources October 26–30, 2020, Kazan, Russia Abstract Volume Ediitor-in-Chief: Daniis K. Nurgaliev Scientific editor: Vladimir V. Silantiev; Milyausha N. Urazaeva Technical editor: Milyausha N. Urazaeva Kazan Golovkinsky Young Scientists’ Stratigraphic Meeting, 2020 Sedimentary Earth Systems: Stratiggraphy, Geochronology, Petroleum Resources Международная молодежная стратиграфическая конференция Головкинского, 2020 Осадочные планетарные системы: стратиграфия, геохронология, углеводородные ресурсы 26–30 октября 2020, Казань, Россия Сборник тезисов Ответственный редактор: Данис К. Нургалиев Научный редактор: Владиммир В. Силантьев; Миляуша Н. Уразаева Технический редактор: Миляуша Н. Уразаева УДК 55 ББК 26.3 М43 Ответственный редактор Данис К. Нургалиев Научный редактор Владимир В. Силантьев; Миляууша Н. Уразаева Техничческий редактор Миляуша Н. Уразаева М43 Международная молодежная стратиграфическая конференция Головкин- ского, 2020 «Осадочные планетарные системы: стратиграфия, геохронология, углеводородные ресурсы» (26–30 октября 2020 г.) [Электронный ресурс]: сборник тезисов. – Электрон. nекстовые дан. (1 файл: 4,06 Мб.). – Казань:
    [Show full text]
  • The Biogeography and Macroevolutionary Trends of Late
    The Biogeography and Macroevolutionary Trends of Late Paleozoic Cephalopods in the North American Midcontinent Sea: Understanding the response of pelagic organisms to changing climate during the Late Paleozoic Ice Age By: Kayla Kolis Submitted to the graduate degree program in Ecology and Evolutionary Biology and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Master of Science. Chair: Bruce S. Lieberman Member: Christopher K. Beard Member: Kirsten Jensen Date Defended: 02 June 2017 The dissertation committee for Kayla Kolis certifies that this is the approved version of the following dissertation: The Biogeography and Macroevolutionary Trends of Late Paleozoic Cephalopods in the North American Midcontinent Sea: Understanding the response of pelagic organisms to changing climate during the Late Paleozoic Ice Age Chair: Bruce S. Lieberman Member: Christopher K. Beard Date Approved: 02 June 2017 ii Abstract: Geographic range is an important macroevolutionary parameter that is frequently considered in paleontological studies. Species distribution and geographic range size are determined by a variety of biotic and abiotic factors that are well known to affect the differential birth and death of species. Thus, considering how species distributions and geographic range sizes fluctuate over time can provide important insight into evolutionary dynamics across the geologic time scale. In this study, I examine how geographic range size and rates of speciation and extinction changed throughout the Pennsylvanian and Early Permian in the North American Midcontinent Sea in an important pelagic clade, the Cephalopoda, using Geographic Information Systems (GIS). This period is particularly interesting for biogeographic and evolutionary analysis because it is characterized by repetitive glacial cycles, a global transition from an icehouse to greenhouse climate during the Late Paleozoic Ice Age and sluggish macroevolutionary dynamics, i.e.
    [Show full text]