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Revision Des Faunes De Vertebres Du Site De Proven Cheres-Sur-Meuse (Trias Terminal, Nord-Est De La France)
REVISION DES FAUNES DE VERTEBRES DU SITE DE PROVEN CHERES-SUR-MEUSE (TRIAS TERMINAL, NORD-EST DE LA FRANCE) par Gilles CUNY * SOMMAIRE Page Résumé, Abstract ..................... : . .. 103 Introduction ..................................................................... 103 Historique. 103 Révision des anciennes collections ................................................... 105 Muséum National d'Histoire Naturelle ................... 105 Université Pierre et Marie Curie. .. .. .. 106 Besançon . 120 Dijon. .. .. .. .. 121 Langres - Saint-Dizier. 121 Lyon ....................................................................... 123 Etude du matériel récent. 126 Discussion ...................................................................... 127 Conclusion ................................................................. :. 129 Remerciements. .. 130 Bibliographie . .. 130 Légendes des planches. 134 * Laboratoire de Paléontologie des Vertébrés, Université Pierre et Marie Curie - Boîte 106, 4 place Jussieu, 75252 PARIS cédex OS, France. Mots-clés: Trias, Rhétien, Poissons, Amphibiens, Reptiles Key-words: Triassic, Rhetian, Fishes, Amphibians, Reptiles PalaeoveT/ebra/a. Montpellier, 24 (1-2): 10H34. 6 fig .• 3 pl. (Reçu le 23 Février 1994. accepté le 15 Mai 1994. publié le 14 Juin 1995) -~----------------- - --.------- --------------- 500MHRES -- ------ - ------ -- --- ---- -------- ---.- A--- ..L -L ~ ~ 1.10 1.00 1 <6~::<:<=.: :~:~:::,'EE: J '_ 0.50 =...- ~ ::_-_____ -___ ---___ ~~:: ~-- __ .- _______ ~:: ----___ ~: ~-____ : ~ ~-. ~ ~ '_____ -
The Early Triassic Jurong Fish Fauna, South China Age, Anatomy, Taphonomy, and Global Correlation
Global and Planetary Change 180 (2019) 33–50 Contents lists available at ScienceDirect Global and Planetary Change journal homepage: www.elsevier.com/locate/gloplacha Research article The Early Triassic Jurong fish fauna, South China: Age, anatomy, T taphonomy, and global correlation ⁎ Xincheng Qiua, Yaling Xua, Zhong-Qiang Chena, , Michael J. Bentonb, Wen Wenc, Yuangeng Huanga, Siqi Wua a State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan 430074, China b School of Earth Sciences, University of Bristol, BS8 1QU, UK c Chengdu Center of China Geological Survey, Chengdu 610081, China ARTICLE INFO ABSTRACT Keywords: As the higher trophic guilds in marine food chains, top predators such as larger fishes and reptiles are important Lower Triassic indicators that a marine ecosystem has recovered following a crisis. Early Triassic marine fishes and reptiles Fish nodule therefore are key proxies in reconstructing the ecosystem recovery process after the end-Permian mass extinc- Redox condition tion. In South China, the Early Triassic Jurong fish fauna is the earliest marine vertebrate assemblage inthe Ecosystem recovery period. It is constrained as mid-late Smithian in age based on both conodont biostratigraphy and carbon Taphonomy isotopic correlations. The Jurong fishes are all preserved in calcareous nodules embedded in black shaleofthe Lower Triassic Lower Qinglong Formation, and the fauna comprises at least three genera of Paraseminotidae and Perleididae. The phosphatic fish bodies often show exceptionally preserved interior structures, including net- work structures of possible organ walls and cartilages. Microanalysis reveals the well-preserved micro-structures (i.e. collagen layers) of teleost scales and fish fins. -
American Museum Published by the American Museum of Natural History Central Park West at 79Th Street New York, N.Y
NovitatesAMERICAN MUSEUM PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET NEW YORK, N.Y. 10024 U.S.A. NUMBER 2718 NOVEMBER 19, 1981 JOHN G. MAISEY Studies on the Paleozoic Selachian Genus Ctenacanthus Agassiz No. 1. Historical Review and Revised Diagnosis of Ctenacanthus, With a List of Referred Taxa AMERICAN MUSEUM Novitates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 2718, pp. 1-22, figs. 1-21 November 19, 1981 Studies on the Paleozoic Selachian Genus Ctenacanthus Agassiz No. 1. Historical Review and Revised Diagnosis of Ctenacanthus, With a List of Referred Taxa JOHN G. MAISEY1 ABSTRACT Ctenacanthus Agassiz is a genus of elasmo- elasmobranch finspines, whereas others resemble branch, originally recognized by its dorsal fin- hybodontid finspines. The fish described by Dean spines but now known from more complete re- as Ctenacanthus clarkii should be referred to C. mains. However, many other fossils, including compressus. Both C. clarkii and C. compressus isolated spines and complete fish, have been in- finspines are sufficiently like those of C. major cluded in Ctenacanthus, although the spines dif- for these species to remain within the genus. fer from those of the type species, C. major, and Ctenacanthus compressus is the only articulated from other presumably related species. Earlier Paleozoic shark so far described which can be diagnoses of Ctenacanthus are critically reviewed assigned to Ctenacanthus. Ctenacanthus costel- and the significance of previous diagnostic latus finspines are not like those of C. major, but changes is discussed. -
Introduction
BELGIAN GEOLOGICAL SURVEY. Professional Paper, 278: Elasmobranches et Stratigraphie (1994), 11-21,1995. Chondrichthyens mésozoïques du Grand Duché de Luxembourg par Dominique DELSATE (*) Résumé: Rappel des faunes de Chondrichthyens du Grand Duché de Luxembourg précédemment décrites. Des spécimens nouveaux sont signalés. Description d'une dent d 'Acrodus de l'Hettangien de Burmerange, et d'une dent â'Hybodus grossiconus du Toarcien inférieur de Soleuvre. Deux aiguillons de nageoire dorsale d'Hybodontoidea, de l'Hettangien (Brouch) et du Toarcien (Soleuvre), sont présentés. Identification formelle du genre Sphenodus parmi les dents du Bajocien luxembourgeois. Mots-clés: Chondrichthyes, Mésozoïque, Luxembourg. Abstract: Previously described Chondrichthyes teeth from the Grand Duchy of Luxembourg are reminded. New specimens are reported. A tooth of Acrodus from the Hettangian of Burmerange and a tooth of Hybodus grossiconus from the lower Toarcian of Soleuvre are described. A very large fin spine from the Lower Toarcian of Soleuvre and a small one from the Hettangian of Brouch are introduced. Some Bajocian teeth are assigned to the genus Sphenodus. Key words: Chondrichthyes, Mesozoic, Luxembourg Kurzfassung: Ein Zahn von Acrodus aus dem Hettangium von Biirmeningen wird beschrieben; ein Zahn aus dem Unter-Toarcium von Zolver wird Hybodus grossiconus zugeordnet. Zwei fossile Stacheln von Rückenflossen, einer aus dem Hettangium (Brouch) und einer aus dem Toarcium (Soleuvre) stammen von Hybodontoidea. Einige Zähne des Toarciums und Bajociums werden der Gattung Sphenodus zugewiesen. Schlüsselwörter: Chondrichthyes, Mesozoicum, Luxemburg * Dominique DELSATE: Centre de Recherches Lorraines (B-6760 Ethe) ou 5 Rue du Quartier (B-6792 Battincourt), Belgique. Introduction Le Centre de Recherches Lorraines, le Service Géologique de Belgique et l'Institut Royal des Sciences Naturelles de Belgique ont entrepris conjointement l'exploration systématique des différents niveaux du Mésozoïque grand- ducal ainsi que l'examen des collections nationales ou privées existantes. -
Copyrighted Material
06_250317 part1-3.qxd 12/13/05 7:32 PM Page 15 Phylum Chordata Chordates are placed in the superphylum Deuterostomia. The possible rela- tionships of the chordates and deuterostomes to other metazoans are dis- cussed in Halanych (2004). He restricts the taxon of deuterostomes to the chordates and their proposed immediate sister group, a taxon comprising the hemichordates, echinoderms, and the wormlike Xenoturbella. The phylum Chordata has been used by most recent workers to encompass members of the subphyla Urochordata (tunicates or sea-squirts), Cephalochordata (lancelets), and Craniata (fishes, amphibians, reptiles, birds, and mammals). The Cephalochordata and Craniata form a mono- phyletic group (e.g., Cameron et al., 2000; Halanych, 2004). Much disagree- ment exists concerning the interrelationships and classification of the Chordata, and the inclusion of the urochordates as sister to the cephalochor- dates and craniates is not as broadly held as the sister-group relationship of cephalochordates and craniates (Halanych, 2004). Many excitingCOPYRIGHTED fossil finds in recent years MATERIAL reveal what the first fishes may have looked like, and these finds push the fossil record of fishes back into the early Cambrian, far further back than previously known. There is still much difference of opinion on the phylogenetic position of these new Cambrian species, and many new discoveries and changes in early fish systematics may be expected over the next decade. As noted by Halanych (2004), D.-G. (D.) Shu and collaborators have discovered fossil ascidians (e.g., Cheungkongella), cephalochordate-like yunnanozoans (Haikouella and Yunnanozoon), and jaw- less craniates (Myllokunmingia, and its junior synonym Haikouichthys) over the 15 06_250317 part1-3.qxd 12/13/05 7:32 PM Page 16 16 Fishes of the World last few years that push the origins of these three major taxa at least into the Lower Cambrian (approximately 530–540 million years ago). -
The Early Triassic Jurong Fish Fauna, South China: Age, Anatomy, Taphonomy, and Global Correlation
Qiu, X., Xu, Y., Chen, Z. Q., Benton, M. J., Wen, W., Huang, Y., & Wu, S. (2019). The Early Triassic Jurong fish fauna, South China: Age, anatomy, taphonomy, and global correlation. Global and Planetary Change, 180, 33-50. https://doi.org/10.1016/j.gloplacha.2019.05.012 Peer reviewed version License (if available): CC BY-NC-ND Link to published version (if available): 10.1016/j.gloplacha.2019.05.012 Link to publication record in Explore Bristol Research PDF-document This is the accepted author manuscript (AAM). The final published version (version of record) is available online via Elsevier at https://doi.org/10.1016/j.gloplacha.2019.05.012 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Accepted Manuscript The Early Triassic Jurong fish fauna, South China: Age, anatomy, taphonomy, and global correlation Xincheng Qiu, Yaling Xu, Zhong-Qiang Chen, Michael J. Benton, Wen Wen, Yuangeng Huang PII: S0921-8181(18)30719-7 DOI: https://doi.org/10.1016/j.gloplacha.2019.05.012 Reference: GLOBAL 2972 To appear in: Global and Planetary Change Received date: 26 December 2018 Revised date: 20 May 2019 Accepted date: 29 May 2019 Please cite this article as: X. Qiu, Y. Xu, Z.-Q. Chen, et al., The Early Triassic Jurong fish fauna, South China: Age, anatomy, taphonomy, and global correlation, Global and Planetary Change, https://doi.org/10.1016/j.gloplacha.2019.05.012 This is a PDF file of an unedited manuscript that has been accepted for publication. -
Chondrichthyan Teeth from the Early Triassic Paris Biota (Bear Lake County, Idaho, USA)
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2019 Chondrichthyan teeth from the Early Triassic Paris Biota (Bear Lake County, Idaho, USA) Romano, Carlo ; Argyriou, Thodoris ; Krumenacker, L J Abstract: A new, diverse and complex Early Triassic assemblage was recently discovered west of the town of Paris, Idaho (Bear Lake County), USA. This assemblage has been coined the Paris Biota. Dated earliest Spathian (i.e., early late Olenekian), the Paris Biota provides further evidence that the biotic recovery from the end-Permian mass extinction was well underway ca. 1.3 million years after the event. This assemblage includes mainly invertebrates, but also vertebrate remains such as ichthyoliths (isolated skeletal remains of fishes). Here we describe first fossils of Chondrichthyes (cartilaginous fishes) from the Paris Biota. The material is composed of isolated teeth (mostly grinding teeth) preserved on two slabs and representing two distinct taxa. Due to incomplete preservation and morphological differences to known taxa, the chondrichthyans from the Paris Biota are provisionally kept in open nomenclature, as Hybodontiformes gen. et sp. indet. A and Hybodontiformes gen. et sp. indet. B, respectively. The present study adds a new occurrence to the chondrichthyan fossil record of the marine Early Triassic western USA Basin, from where other isolated teeth (Omanoselache, other Hybodontiformes) as well as fin spines of Nemacanthus (Neoselachii) and Pyknotylacanthus (Ctenachanthoidea) and denticles have been described previously. DOI: https://doi.org/10.1016/j.geobios.2019.04.001 Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-170655 Journal Article Accepted Version The following work is licensed under a Creative Commons: Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0) License. -
Callorhinchus Milii
Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1382 Development and three- dimensional histology of vertebrate dermal fin spines ANNA JERVE ACTA UNIVERSITATIS UPSALIENSIS ISSN 1651-6214 ISBN 978-91-554-9596-1 UPPSALA urn:nbn:se:uu:diva-286863 2016 Dissertation presented at Uppsala University to be publicly examined in Lindahlsalen, Evolutionary Biology Center, Norbyvägen 18A, Uppsala, Monday, 13 June 2016 at 09:00 for the degree of Doctor of Philosophy. The examination will be conducted in English. Faculty examiner: Philippe Janvier (Muséum National d'Histoire Naturelle, Paris, France). Abstract Jerve, A. 2016. Development and three-dimensional histology of vertebrate dermal fin spines. Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 1382. 53 pp. Uppsala: Acta Universitatis Upsaliensis. ISBN 978-91-554-9596-1. Jawed vertebrates (gnathostomes) consist of two clades with living representatives, the chondricthyans (cartilaginous fish including sharks, rays, and chimaeras) and the osteichthyans (bony fish and tetrapods), and two fossil groups, the "placoderms" and "acanthodians". These extinct forms were thought to be monophyletic, but are now considered to be paraphyletic partly due to the discovery of early chondrichthyans and osteichthyans with characters that had been previously used to define them. Among these are fin spines, large dermal structures that, when present, sit anterior to both median and/or paired fins in many extant and fossil jawed vertebrates. Making comparisons among early gnathostomes is difficult since the early chondrichthyans and "acanthodians", which have less mineralized skeleton, do not have large dermal bones on their skulls. As a result, fossil fin spines are potential sources for phylogenetic characters that could help in the study of the gnathostome evolutionary history. -
Progressive Palaeontology 2007
Progressive Palaeontology 2007 Thursday 12th – Saturday 14th April Department of Earth Sciences, University of Bristol 2 Welcome and acknowledgements We are pleased to welcome you to the Department of Earth Sciences at the University of Bristol for this year’s Progressive Palaeontology meeting. This appears to be the best attended and most presentation-packed Progressive Palaeontology on record – we are just shy of 60 delegates and there are 30 presentations in total (24 oral and 6 poster). As always Progressive Palaeontology’s aim is to provide a framework in which to present ideas and discuss work with those at a similar stage in their career. In order to achieve this the Friday presentation session is supplemented by two social events and a field trip. On Thursday evening there is a pre-conference gathering at the Berkeley pub (opposite the department on Queen’s Road) and following the presentation sessions on Friday there will also be an evening reception/dinner at Bristol Zoo. This year’s field trip will be to Aust Cliff (a site famous for its Late Triassic fish fossils – see the brief guide at the end of this booklet). We are lucky to have two experts on this site joining us on the day and we have scheduled a reasonably late start so please do come along if you have registered! We would also like to take this opportunity to thank the following individuals who have helped in supporting, preparing and running this year’s meeting: The Palaeontological Association and the University of Bristol Alumni Foundation for providing sponsorship. -
Morphology and Phylogeny of Synechodontiform Sharks (Chondrichthyes, Elasmobranchii) with Comments on the Origin and Early Evolution of Neoselachii
Morphology and Phylogeny of Synechodontiform Sharks (Chondrichthyes, Elasmobranchii) with Comments on the Origin and Early Evolution of Neoselachii Stefanie Klug Morphology and Phylogeny of Synechodontiform Sharks (Chondrichthyes, Elasmobranchii) with Comments on the Origin and Early Evolution of Neoselachii Dissertation zur Erlangung des akademischen Grades doctor rerum naturalium (Dr. rer. nat.) in der Wissenschaftsdisziplin Geologie / Paläontologie vorgelegt im Fachbereich Geowissenschaften der Freien Universität Berlin von Dipl.-Geol. Stefanie Klug Berlin, Dezember 2008 Tag der Disputation 20. April 2009 1. Gutachter Prof. Dr. Helmut Keupp Deparment of Earth Sciences, Geological Sciences, Palaeontology Free University Berlin Malteserstrasse 74-100, Haus D 12249 Berlin, Germany 2. Gutachter Prof. Dr. Bettina Reichenbacher Department of Geo- and Environmental Sciences, Palaeontology Ludwig-Maximilians-University Munich Richard-Wagner-Strasse 10 80333 Munich, Germany To my family for their permanent support, continuous encouragement and always believing in me Hiermit versichere ich, dass ich die vorliegende Arbeit ohne Hilfe Dritter und ohne Verwendung anderer als der angeführten Hilfsmittel und Quellen angefertigt habe, und dass die Arbeit in gleicher oder ähnlicher Form noch keiner anderen Prüfungs- behörde vorgelegen hat. Alle Ausführungen der Arbeit die wörtlich oder sinngemäß übernommen wurden, sind entsprechend gekennzeichnet. Berlin, Dezember 2008 Taxonomic Disclaimer This doctoral thesis is produced only for the purpose of a -
Oxygen Isotopes in Phosphates of Fossil Fish-Devonian to Recent
Stable Isotope Geochemistry: A Tribute to Samuel Epstein © The Geochemical Society, Special Publication No.3, 1991 Editors: H. P. Taylor, Jr., J. R. O'Neil and l. R. Kaplan Oxygen isotopes in phosphates of fossil fish-Devonian to Recent YEHOSHUAKOLODNYand BOAZLuz Department of Geology, The Institute of Earth Sciences, The Hebrew University of Jerusalem, Jerusalem, Israel 18 Abstract-The isotopic composition of oxygen in the phosphate of apatite (/) 0p) was determined in 159 fish bones and teeth from museum collections throughout the world. The fossils were both marine and fresh water, ranging in age from Devonian to the Recent. In 45 of those we also determined 18 the isotopic composition of oxygen and carbon of the lattice carbonate in apatite (/) 0c and /)13C). In most cases the isotopic results are compatible with previously available geological information: the difference between marine and fresh water, the indication of previously known warm and cold time periods, and the ranking of fishes from warm to cold according to their inferred life habitat. 18 18 The relationship between /) 0p and /) 0c suggests early diagenetic replacement of an originally phos- phatic phase by carbonate fluor apatite (CFA). The correlated latitudinal variation in /)180of meteoric 18 water and temperature should result in a small variation of /) 0p in fresh-water fish. The large range 18 in /) 0p of Recent fish is the outcome of the "altitude effect" (DANSGAARD, 1964), i.e. of the existence of post orogenic high altitudes. INTRODUCfION case of apatitic fossilsshould become lessacute than THE "ESTIMATIONOFthe paleotemperatures of an- it is with calcium carbonate. -
A New Neoselachian Shark from the Upper Triassic of Grozon (Jura, France)
Geol. Mag. 135 (5), 1998, pp. 657–668. Printed in the United Kingdom © 1998 Cambridge University Press 657 A new neoselachian shark from the Upper Triassic of Grozon (Jura, France) GILLES CUNY*, MICHEL MARTIN†, RAYMOND RAUSCHER‡ & JEAN-MICHEL MAZIN§ * Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, UK † Musée d’Histoire naturelle, 115, boulevard Eurvin, 62200 Boulogne-sur-Mer, France ‡ Centre de Géochimie de la Surface (C.N.R.S.), Institut de Géologie, 1, rue Blessig, 67084 Strasbourg cedex, France § Laboratoire de Géobiologie, Biochronologie et Paléontologie humaine, Université de Poitiers, 40, avenue du Recteur Pineau, 86022 Poitiers cedex, France (Received 11 December 1997; accepted 7 May 1998) Abstract – Two successive assemblages of vertebrate microremains have been found at Grozon (Jura, northeastern France). Palynological analysis confirms a Norian age for the first one and a Rhaetian age for the second. A new species of neoselachian shark, Grozonodon candaui, is erected from isolated teeth of Norian age, based on their enameloid ultrastructure. Distinctive parallel-fibred enameloid is recognized among teeth previously assigned to Hybodus minor, which therefore represents another early neoselachian shark. These structural characteristics confirm the close relationship of hybodont and neoselachian sharks. 1. Introduction The site of Grozon is located 3.5 km north of the town of Poligny (Jura, Fig. 1) and was visited briefly by two of us (GC and JMM) in 1992 and 1994. It is a small disused quarry, belonging to the society Platrières de Grozon. This locality was cited more than a century ago by Henry (1876, p.