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First Record of Non-Mineralized Cephalopod Jaws and Arm Hooks
Klug et al. Swiss J Palaeontol (2020) 139:9 https://doi.org/10.1186/s13358-020-00210-y Swiss Journal of Palaeontology RESEARCH ARTICLE Open Access First record of non-mineralized cephalopod jaws and arm hooks from the latest Cretaceous of Eurytania, Greece Christian Klug1* , Donald Davesne2,3, Dirk Fuchs4 and Thodoris Argyriou5 Abstract Due to the lower fossilization potential of chitin, non-mineralized cephalopod jaws and arm hooks are much more rarely preserved as fossils than the calcitic lower jaws of ammonites or the calcitized jaw apparatuses of nautilids. Here, we report such non-mineralized fossil jaws and arm hooks from pelagic marly limestones of continental Greece. Two of the specimens lie on the same slab and are assigned to the Ammonitina; they represent upper jaws of the aptychus type, which is corroborated by fnds of aptychi. Additionally, one intermediate type and one anaptychus type are documented here. The morphology of all ammonite jaws suggest a desmoceratoid afnity. The other jaws are identifed as coleoid jaws. They share the overall U-shape and proportions of the outer and inner lamellae with Jurassic lower jaws of Trachyteuthis (Teudopseina). We also document the frst belemnoid arm hooks from the Tethyan Maastrichtian. The fossils described here document the presence of a typical Mesozoic cephalopod assemblage until the end of the Cretaceous in the eastern Tethys. Keywords: Cephalopoda, Ammonoidea, Desmoceratoidea, Coleoidea, Maastrichtian, Taphonomy Introduction as jaws, arm hooks, and radulae are occasionally found Fossil cephalopods are mainly known from preserved (Matern 1931; Mapes 1987; Fuchs 2006a; Landman et al. mineralized parts such as aragonitic phragmocones 2010; Kruta et al. -
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 ------ - --- - - - - - --- --- - -- --- - -- - - --- -
Paléontologie Au Luxembourg (2) A
Paléontologie au Luxembourg (2) A. Di Cencio, D. Sadki, R. Weis (eds.) R. Weis D. Sadki, A. Di Cencio, Les ammonites de la Minette Andrea Di Cencio, Driss Sadki, Paléontologie au Luxembourg (2) Luxembourg au Paléontologie Robert Weis (eds.) Ferrantia Travaux scientifiques du Musée national d'histoire naturelle Luxembourg www.mnhn.lu 83 2020 Ferrantia 83 2020 2020 83 Ferrantia est une revue publiée à intervalles non réguliers par le Musée national d’histoire naturelle à Luxembourg. Elle fait suite, avec la même tomaison, aux T M ’ L parus entre 1981 et 1999. Comité de rédaction: Eric Buttini Guy Colling Alain Frantz Thierry Helminger Ben Thuy Mise en page: Romain Bei Design: Thierry Helminger Prix du volume: 20 € Rédaction: Échange: Musée national d’histoire naturelle Exchange MnhnL Rédaction Ferrantia c/o Musée national d’histoire naturelle 25, rue Münster 25, rue Münster L-2160 Luxembourg L-2160 Luxembourg Tél +352 46 22 33 - 1 Tél +352 46 22 33 - 1 Fax +352 46 38 48 Fax +352 46 38 48 Internet: http://www.mnhn.lu/ferrantia/ Internet: http://www.mnhnl.lu/biblio/exchange email: [email protected] email: [email protected] Page de couverture: Bredyia subinsignis (Oppel, 1856), DOU833. Natural History Museum of Luxembourg. Citation: Di Cencio A., Sadki D., Weis R. (eds.) 2020. - Paléontologie au Luxembourg (2) - Les ammonites de la Minette. Ferrantia 83, Musée national d’histoire naturelle, Luxembourg, 129 p. Date de publication: 15 décembre 2020 (réception du manuscrit: 19 mai 2020) Impression: Imprimerie Centrale climatiquement neutre Impression | LU-319-JR8FDJV | www.natureOffice.com Ferrantia est publiée sous la licence Creative Commons BY-NC-ND 3.0 LU. -
Early Bajocian Type Sonniniids and Hammatoceratids SW Germany
Boletín del Instituto de Fisiografía y Geología 91, 2021 1 New information on the Early Bajocian types of sonniniids and hammatoceratids (Ammonitina) described by W. Waagen (1867) from Gingen/Fils (SW Germany) Driss Sadki & Volker Dietze Sadki D. & Dietze V., 2021. New information on the Early Bajocian types of sonniniids and hammatoceratids (Ammonitina) described by W. Waagen (1867) from Gingen/Fils (SW Germany). Boletín del Instituto de Fisiografía y Geología 91: 1-16. Rosario, 08/05/2021. ISSN 1666-115X. Abstract. The type specimens of the species of sonniniids and hammatoceratids (Ammonitina) from the Lower Bajocian of Gingen/Fils (SW Germany) described by Waagen in 1867, and deposited in the Bavarian State Collection for Palaeontology and Geology in Munich, are revised. They are referred to the morphogenera Euhoploceras, Shirbuirnia, Papilliceras, Sonninia, Witchellia, and Fissilobiceras: E. adicrum (Waagen, 1867), E. polyacanthum (Waagen, 1867), E. mayeri (Waagen, 1867), S. gingensis (Waagen, 1867), P. mesacanthum (Waagen, 1867), S. patella (Waagen, 1867), W. jugifera (Waagen, 1867), and F. fissilobatum (Waagen, 1867). A lectotype is designated for E. Recibido 17/09/2020 Aceptado 29/10/2020 mayeri (Waagen, 1867). Keywords: Sonniniidae ▪ Hammatoceratidae ▪ Ammonitina ▪ Middle Jurassic ▪ Lower Bajocian ▪ W. Waagen ▪ Disponible vía Internet Southwest Germany. & versión impresa 08/05/2021 Resumen. Nueva información sobre los tipos de sonníniidos y hammatocerátidos (Ammonitina, Cephalopoda) del Editor: H. Parent Bajociano Inferior de Gingen/Fils (SO de Alemania) descriptos por W. Waagen (1867). Los especímenes tipo de sonníniidos y hammatocerátidos (Ammonitina) del Bajociano Inferior de Gingen/Fils (SO de Alemania) descriptos por Waagen en 1867, actualmente depositados en el Bayerischen Staatssammlung für Paläontologie und Geologie in München, son revisados y referidos a los morfogéneros Euhoploceras, Shirbuirnia, Papilliceras, Sonninia, Witchellia, y Fissilobiceras: E. -
TRIASSIC AMMONOID RECOVERIES and Extincfions. E.T.Tozer
39g TRIASSIC AMMONOID RECOVERIES AND EXTINCfIONS. E.T.Tozer, Geological Survey of Canada, 100 West Pender Street, Vancouver, British Columbia, V6B IR8, Canada. Triassic ammonoids provide an excellent glimpse of faunal recovery after the extinctions at the P-T boundary. No other animals, with the possible exception of those represented by conodonts, provide so nearly a continuous faunal record with more than 40 different successive faunas easily distinguished. The problems introduced by Lazarus taxa are reduced although there are still gaps that make positive elucidation of some phylogenies difficult or impossible. The Triassic chronology used here is that of most DNAG volumes, except that Scythian, the only Triassic stage in the Lower Triassic in the Introductory volume is divided into four, as in volumes for Western and Arctic Canada. Succession of Triassic series and st(\ges is thus: Lower Triassic - Griesbachian, Dienerian, Smithian, Spathian; Middle Triassic - Anisian, Ladinian; Upper Triassic Carnian, Norian. Rhaetian of some authors is part or parts of this Upper Norian. How much of the Upper Norian has not been settled. In a 1980 census Triassic Ammonoidea were assigned to 3 Orders, Prolecanitida (3 genera); Ceratitida (427); Phylloceratida (15). In the Ceratitida virtually every kind of morphological character is represented. Shells range in shape from serpenticone to globose and oxycone, or heteromorph; in sculpture from smooth to ribbed and/or tuberculate. All kinds of sutures are developed. The large number of taxa are necessary to express the variation. The Permian-Triassic boundary was not a disaster for the ammonoids. Three groups cross the boundary, one of Prolecanitida (Episageceratidae), two of Ceratitida (Otocerataceae and Xenodiscaceae). -
Main Morphological Events in the Evolution of Paleozoic Cephalopods I
Stratigraphy and Geological Correlation, Vol. 2, No. 1, 1994, pp. 49 - 55. Translated from Stratigrafiya. Geologicheskaya Korrelyatsiya, Vol. 2, No. 1,1994, pp. 55 - 61. Original Russian Text Copyright © 1994 by Barskov, Bogoslovskaya, Zhuravleva, Kiselev, Kuzina, Leonova, Shimanskii, Yatskov. English Translation Copyright © 1994 by Interperiodica Publishing (Russia). Main Morphological Events in the Evolution of Paleozoic Cephalopods I. S. Barskov*, M. F. Bogoslovskaya*, F. A. Zhuravleva*, G. N. Kiselev**, L. F. Kuzina*, T. B. Leonova*, V. N. Shimanskii*, and S. V. Yatskov* institute of Paleontology, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117647 Russia **Department of Paleontology, St. Petersburg State University, 16-ya Liniya 29, St. Petersburg, 199178 Russia Received January 26,1993 Abstract - New morphological features in shell structure, which were the starting points of cephalopod diver sification into taxa of high ranks (subclasses, orders, superfamilies), are considered as phylogenetic events. Main morphological innovations in the evolution of nautiloid cephalopods; the formation of endosiphuncular and cameral deposits, shell coiling, truncation of the phragmocone’s apical end, and contracted aperture, which originated to make the relative shell positioning in the water more efficient. Changes in the lobe line structure and various types of complications in the primary lobes (ventral, umbonal, and lateral) were the most important morphological innovations in convolute ammonoids. The functional significance of these changes remains unclear, but recognition of equally significant changes in primary lobes requires a review of the Paleozoic Ammonoidea taxonomy at the suborder level. This paper is a continuation of a study whose first lation of the buoyancy process and to support in various results have been published (Barskov et al., 1993). -
Cephalopod Reproductive Strategies Derived from Embryonic Shell Size
Biol. Rev. (2017), pp. 000–000. 1 doi: 10.1111/brv.12341 Cephalopod embryonic shells as a tool to reconstruct reproductive strategies in extinct taxa Vladimir Laptikhovsky1,∗, Svetlana Nikolaeva2,3,4 and Mikhail Rogov5 1Fisheries Division, Cefas, Lowestoft, NR33 0HT, U.K. 2Department of Earth Sciences Natural History Museum, London, SW7 5BD, U.K. 3Laboratory of Molluscs Borissiak Paleontological Institute, Russian Academy of Sciences, Moscow, 117997, Russia 4Laboratory of Stratigraphy of Oil and Gas Bearing Reservoirs Kazan Federal University, Kazan, 420000, Russia 5Department of Stratigraphy Geological Institute, Russian Academy of Sciences, Moscow, 119017, Russia ABSTRACT An exhaustive study of existing data on the relationship between egg size and maximum size of embryonic shells in 42 species of extant cephalopods demonstrated that these values are approximately equal regardless of taxonomy and shell morphology. Egg size is also approximately equal to mantle length of hatchlings in 45 cephalopod species with rudimentary shells. Paired data on the size of the initial chamber versus embryonic shell in 235 species of Ammonoidea, 46 Bactritida, 13 Nautilida, 22 Orthocerida, 8 Tarphycerida, 4 Oncocerida, 1 Belemnoidea, 4 Sepiida and 1 Spirulida demonstrated that, although there is a positive relationship between these parameters in some taxa, initial chamber size cannot be used to predict egg size in extinct cephalopods; the size of the embryonic shell may be more appropriate for this task. The evolution of reproductive strategies in cephalopods in the geological past was marked by an increasing significance of small-egged taxa, as is also seen in simultaneously evolving fish taxa. Key words: embryonic shell, initial chamber, hatchling, egg size, Cephalopoda, Ammonoidea, reproductive strategy, Nautilida, Coleoidea. -
Smithian (Early Triassic) Ammonoids from Tulong, South Tibet§
Geobios 43 (2010) 403–431 Original article Smithian (Early Triassic) ammonoids from Tulong, South Tibet§ Ammonoïdes du Smithien (Trias inférieur) de Tulong, Tibet du Sud Thomas Brühwiler a,*, Hugo Bucher a,b, Nicolas Goudemand a a Paläontologisches Institut und Museum der Universität Zürich, Karl Schmid-Strasse 4, 8006 Zürich, Switzerland b Department of Earth Sciences, ETH, Universitätsstrasse 16, 8092 Zürich, Switzerland Received 6 August 2009; accepted 8 December 2009 Available online 26 May 2010 Abstract Intensive sampling of the Tulong Formation in South Tibet has facilitated the construction of a highly-resolved middle and late Smithian ammonoid succession. The new biostratigraphical sequence comprises the middle Smithian Brayardites compressus beds, Nammalites pilatoides beds, and the Nyalamites angustecostatus beds followed by the late Smithian Wasatchites distractus beds and Glyptophiceras sinuatum beds. This faunal succession correlates very well with that of other Tethyan sequences such as the Salt Range (Pakistan), Spiti (India), Oman and South China. The Smithian faunal sequence from Tulong contains several taxa with broad geographic distribution (e.g., Owenites, Paranannites spathi, Shigetaceras, Wasatchites), thus enabling correlation with faunal successions from areas outside the Tethys (e.g., USA, British Columbia, Arctic Canada, South Primorye, Siberia). Early Smithian ammonoid faunas are almost absent in Tulong because of a preservation bias (absence of carbonate rocks). Five new ammonoid genera (Brayardites, Nammalites, Nyalamites, Shigetaceras, Tulongites) and six new species (Brayardites crassus, Brayardites compressus, Prionites involutus,?Subflemingites compressus, Tulongites xiaoqiaoi, Urdyceras tulongensis) are described. # 2010 Elsevier Masson SAS. All rights reserved. Keywords: Ammonoidea; Early Triassic; South Tibet; Smithian; Biostratigraphy Résumé Un échantillonnage intensif de la Formation Tulong du sud-Tibet permet l’établissement d’une séquence très détaillée des faunes d’ammonites du Smithien moyen et supérieur. -
Evolution of Habitat Depth in the Jurassic– Cretaceous Ammonoids
COMMENTARY COMMENTARY Evolution of habitat depth in the Jurassic– Cretaceous ammonoids Kazuyoshi Moriya1 oxygen isotopic analyses of shell materials of Department of Earth Sciences, Faculty of Education and Integrated Arts and Sciences, ammonoids reveal the temperature at which Waseda University, Shinjuku-ku, Tokyo 169-8050, Japan the shell was secreted. This technique, called oxygen isotopic thermometry, has been widely Ammonoids, a group of cephalopods with body fossils and close modern relatives. For used in paleoclimatological and paleobiologi- external chambered shells, arose in the early example, although one may usually imagine that cal research. It was also applied to ammonoid Devonian and went extinct at the Cretaceous/ ammonoids were planktic or nektic organisms fossils more than 40 y ago (2, 3). Many scien- Paleogene (K/Pg) boundary. During their 340- within a water column, like the Nautilus,which tists, however, assumed that ammonoids were planktic or nektic organisms, so their discus- million-y history, ammonoids suffered three is the sole surviving cephalopod bearing an sion focused mainly on growth rates inferred major diversity crises at the end of the Devonian, external chambered shell, there is very little by identifying sinusoidal patterns, hence sea- Permian, and Triassic Periods, and the terminal direct evidence showing the habitat depth of sonality, in the temperature data. Among extinction event at the K/Pg boundary. Because ammonoids within an ancient water column. those previous workers, Anderson et al. (4) of their rapid morphological evolution and rich Sessa et al. (1) shed new light on the habitat analyzed oxygen isotopic composition of the fossil record, ammonoids have been used to depth of the Cretaceous ammonoids using geo- middle Jurassic ammonoids and compared determine the relative age of marine strata and chemical proxy records. -
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. -
Abstracts and Program. – 9Th International Symposium Cephalopods ‒ Present and Past in Combination with the 5Th
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/265856753 Abstracts and program. – 9th International Symposium Cephalopods ‒ Present and Past in combination with the 5th... Conference Paper · September 2014 CITATIONS READS 0 319 2 authors: Christian Klug Dirk Fuchs University of Zurich 79 PUBLICATIONS 833 CITATIONS 186 PUBLICATIONS 2,148 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Exceptionally preserved fossil coleoids View project Paleontological and Ecological Changes during the Devonian and Carboniferous in the Anti-Atlas of Morocco View project All content following this page was uploaded by Christian Klug on 22 September 2014. The user has requested enhancement of the downloaded file. in combination with the 5th International Symposium Coleoid Cephalopods through Time Abstracts and program Edited by Christian Klug (Zürich) & Dirk Fuchs (Sapporo) Paläontologisches Institut und Museum, Universität Zürich Cephalopods ‒ Present and Past 9 & Coleoids through Time 5 Zürich 2014 ____________________________________________________________________________ 2 Cephalopods ‒ Present and Past 9 & Coleoids through Time 5 Zürich 2014 ____________________________________________________________________________ 9th International Symposium Cephalopods ‒ Present and Past in combination with the 5th International Symposium Coleoid Cephalopods through Time Edited by Christian Klug (Zürich) & Dirk Fuchs (Sapporo) Paläontologisches Institut und Museum Universität Zürich, September 2014 3 Cephalopods ‒ Present and Past 9 & Coleoids through Time 5 Zürich 2014 ____________________________________________________________________________ Scientific Committee Prof. Dr. Hugo Bucher (Zürich, Switzerland) Dr. Larisa Doguzhaeva (Moscow, Russia) Dr. Dirk Fuchs (Hokkaido University, Japan) Dr. Christian Klug (Zürich, Switzerland) Dr. Dieter Korn (Berlin, Germany) Dr. Neil Landman (New York, USA) Prof. Pascal Neige (Dijon, France) Dr. -
The Soft-Tissue Attachment Scars in Late Jurassic Ammonites from Central Russia
The soft-tissue attachment scars in Late Jurassic ammonites from Central Russia ALEKSANDR A. MIRONENKO Mironenko, A.A. 2015. The soft-tissue attachment scars in Late Jurassic ammonites from Central Russia. Acta Palaeonto- logica Polonica 60 (4): 981–1000. Soft-tissue attachment scars of two genera and four species of Late Jurassic craspeditid ammonites from the Russian Platform are described. A previously suggested relationship between lateral attachment scars and ammonoid hyponome is confirmed, however, a new interpretation is proposed for dorsal attachment scars: they could have been areas not only for attachment of the dorsal (nuchal) retractors, but also of the cephalic retractors. The new type of the soft-tissue attachment—anterior lateral sinuses, located between the lateral attachment scars and the aperture of the ammonite body chamber is described. Enclosed elliptical or subtriangular areas in apertural parts of the anterior lateral sinuses were found for the first time. Their presence and location suggest that this structure could have been used for attaching the funnel-locking apparatus, similar to those of coleoids. A transformation of shape and position of lateral attachment scars through the evolution of the Late Jurassic craspeditid lineage starting from platycones (Kachpurites fulgens) to keeled oxycones (Garniericeras catenulatum) is recognized. Key words: Ammonoidea, Craspeditidae, Kachpurites, Garniericeras, attachment scars, paleobiology, Jurassic, Russia. Aleksandr A. Mironenko [[email protected]], Kirovogradskaya st., 28-1-101, 117519 Moscow, Russia. Received 9 November 2013, accepted 24 May 2014, available online 16 June 2014. Copyright © 2015 A.A. Mironenko. This is an open-access article distributed under the terms of the Creative Commons Attribution License (for details please see http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.