The Nothosaurs of the Southern German Lettenkeuper (Triassic

Total Page:16

File Type:pdf, Size:1020Kb

The Nothosaurs of the Southern German Lettenkeuper (Triassic The Nothosaurs of the Southern German Lettenkeuper (Triassic, Late Ladinian) Dissertation der Mathematisch-Naturwissenschaftlichen Fakultät der Eberhard Karls Universität Tübingen zur Erlangung des Grades eines Doktors der Naturwissenschaften (Dr. rer. nat.) vorgelegt von Dipl.- Geol. Juliane Katharina Mittag geb. Hinz aus Reutlingen Tübingen 2020 Gedruckt mit Genehmigung der Mathematisch-Naturwissenschaftlichen Fakultät der Eberhard Karls Universität Tübingen. Tag der mündlichen Qualifikation: 24.11.2020 Stellvertretender Dekan: Prof. Dr. József Fortágh 1. Berichterstatter: Prof. Dr. James Nebelsick 2. Berichterstatter: PD Dr. Ingmar Werneburg Ich erkläre hiermit, dass ich die zur Promotion eingereichte Arbeit mit dem Titel: The Nothosaurs of the Southern German Lettenkeuper (Triassic, Late Ladinian) selbständig verfasst, nur die angegebenen Quellen und Hilfsmittel benutzt und wörtlich oder inhaltlich übernommene Stellen (alternativ: Zitate) als solche gekennzeichnet habe. Ich erkläre, dass die Richtlinien zur Sicherung guter wissenschaftlicher Praxis der Universität Tübingen (Beschluss des Senats vom 25.5.2000) beachtet wurden. Ich versichere an Eides statt, dass diese Angaben wahr sind und dass ich nichts verschwiegen habe. Mir ist bekannt, dass die falsche Abgabe einer Versicherung an Eides statt mit Freiheitsstrafe bis zu drei Jahren oder mit Geldstrafe bestraft wird. "If I have seen further, it is by standing upon the shoulders of giants" Isaac Newton, 1675 I dedicate this work to Prof. Dr. Hans-Ulrich Pfretzschner, who was always there for me. He was my supervisor, my mentor, and he will always be my inspiration for scientific curiosity, pursuit of knowledge, and beyond. Table of contents 1. Summary .................................................................................................................... 3 1.1. Zusammenfassung .................................................................................................. 3 1.2. Summary in English ................................................................................................ 4 2. List of publications ...................................................................................................... 5 3. Own contribution ......................................................................................................... 6 4. Introduction ................................................................................................................. 7 5. Aim of this study ........................................................................................................12 6. A potential geographical origin of the Sauropterygia ..................................................14 6.1. Existing theories .....................................................................................................14 6.2. “Out of Russia” .......................................................................................................15 6.3. Materials and methods ...........................................................................................15 6.4. Results, discussion, and conclusions .....................................................................16 7. A new nothosaur (Sauropterygia) from the Ladinian of Vellberg-Eschenau, southern Germany ..............................................................................................................................20 7.1. The history of Vellberg-Eschenau ...........................................................................20 7.2. Stratigraphy ............................................................................................................21 7.3. Paleoecology ..........................................................................................................23 7.4. Materials and methods after HINZ ET AL. (2019) ......................................................24 7.5. Description .............................................................................................................25 7.6. Comparison ............................................................................................................29 7.6.1. General shape of the skull ...............................................................................30 7.6.2. Tooth counts ...................................................................................................31 7.6.3. The orbitonasal region .....................................................................................31 7.6.4. The postorbital bridge ......................................................................................31 7.6.5. The sagittal crest and the location of the parietal foramen ...............................32 7.6.6. The vomer .......................................................................................................33 7.6.7. The ectopterygoid and hyoid ...........................................................................33 7.7. Phylogeny ..............................................................................................................33 1 7.8. Discussion and conclusions ...................................................................................34 8. A Nothosaurus (Sauropterygia) skull from Kupferzell (Triassic, late Ladinian; SW Germany) .............................................................................................................................38 8.1. The history of Kupferzell .........................................................................................38 8.2. Stratigraphy ............................................................................................................38 8.3. Paleoecology ..........................................................................................................40 8.4. Materials and methods after (HINZ ET AL. 2020) ......................................................41 8.5. Description and comparison ...................................................................................41 8.5.1. Comparison with Nothosaurus edingerae ........................................................45 8.5.2. Comparison with Nothosaurus jagisteus..........................................................47 8.5.3. Comparison with Nothosaurus cristatus ..........................................................47 8.5.4. Comparison with Nothosaurus mirabilis...........................................................49 8.5.5. Comparison with Nothosaurus giganteus ........................................................53 8.6. Discussion and conclusion .....................................................................................57 9. Acknowledgments ......................................................................................................60 10. List of abbreviations ...................................................................................................61 11. List of figures and tables ............................................................................................63 12. References ................................................................................................................68 13. Appendix 1 – Published manuscript " A new nothosaur (Sauropterygia) from the Ladinian of Vellberg-Eschenau, southern Germany” ............................................................80 14. Appendix 2 Supplement of the published manuscript " A new nothosaur (Sauropterygia) from the Ladinian of Vellberg-Eschenau, southern Germany” .............................................111 14.1. Supplement 1. Measurements (in mm) of N. cristatus n. sp. ................................. 111 14.2. Supplement 2. Changes of the character codings with explanations. ................... 113 15. Appendix 3 – Codings for the phylogeny described in chapter 13 ............................ 122 16. Appendix 4 – A Nothosaurus (Sauropterygia) skull from Kupferzell (Triassic, late Ladinian; SW Germany) .....................................................................................................123 2 1. Summary 1.1. Zusammenfassung Die zu den heute ausgestorbenen Sauroptergygiern gehörende Ordnung der Nothosaurier bildete zusammen mit den Ichthyosauriern die Spitze der Nahrungskette triassischer mariner Ökosysteme. Mit Ausnahme zweier in Nordamerika gefundener Sauropterygier beschränkte sich die Verbreitung der Sauropterygier und der dazu gehörigen Ordnung der Nothosaurier im Speziellen auf den Tethysrand und das Germanische Becken, das während der Trias einen der Hauptlebensräume der Nothosaurier darstellte. Bisher wurde angenommen, dass die hauptsächliche Verbreitung von Nothosauriern im voll marinen Muschelkalk erfolgte und die Diversität dieser Tiergruppe im Lettenkeuper mit der zunehmenden Verlandung des Germanischen Beckens von Norden her nach und nach geringer wurde. Im Rahmen dieser Arbeit werden neue Nothosaurierfunde aus dem Lettenkeuper des Germanischen Beckens vorgestellt, die ein neues Licht auf die Diversität und zeitliche Verteilung der Nothosaurier in Süddeutschland werfen. Bei eigenen Grabungen im Lettenkeuper von Vellberg-Eschenau bei Schwäbisch Hall wurde im Jahr 2017 ein vollständig erhaltener Schädel einer neuen Nothosaurierart entdeckt. Im Zuge einer ausführlichen Publikation wurde der Fund als Nothosaurus cristatus neu beschrieben, gezeichnet und in einer eigenen phylogenetischen Analyse in den Stammbaum der Nothosaurier eingegliedert. Dieser Fund ist von großer Relevanz, da er zeigen konnte, dass die Diversität von Nothosauriern im Lettenkeuper
Recommended publications
  • Foramina in Plesiosaur Cervical Centra Indicate a Specialized Vascular System
    Foss. Rec., 20, 279–290, 2017 https://doi.org/10.5194/fr-20-279-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 4.0 License. Foramina in plesiosaur cervical centra indicate a specialized vascular system Tanja Wintrich1, Martin Scaal2, and P. Martin Sander1 1Bereich Paläontologie, Steinmann-Institut für Geologie, Mineralogie und Paläontologie, Universität Bonn, 53115 Bonn, Germany 2Institut für Anatomie II, Universität zu Köln, Joseph-Stelzmann-Str. 9, 50937 Cologne, Germany Correspondence: Tanja Wintrich ([email protected]) Received: 16 August 2017 – Revised: 13 November 2017 – Accepted: 14 November 2017 – Published: 19 December 2017 Abstract. The sauropterygian clade Plesiosauria arose in the 1 Introduction Late Triassic and survived to the very end of the Cretaceous. A long, flexible neck with over 35 cervicals (the highest 1.1 Sauropterygian evolution and plesiosaur origins number of cervicals in any tetrapod clade) is a synapomor- phy of Pistosauroidea, the clade that contains Plesiosauria. Plesiosauria are Mesozoic marine reptiles that had a global Basal plesiosaurians retain this very long neck but greatly distribution almost from their origin in the Late Triassic reduce neck flexibility. In addition, plesiosaurian cervicals (Benson et al., 2012) to their extinction at the end of the have large, paired, and highly symmetrical foramina on the Cretaceous (Ketchum and Benson, 2010; Fischer et al., ventral side of the centrum, traditionally termed “subcentral 2017). Plesiosauria belong to the clade Sauropterygia and foramina”, and on the floor of the neural canal. We found are its most derived and only post-Triassic representatives, that these dorsal and the ventral foramina are connected by being among the most taxonomically diverse of all Meso- a canal that extends across the center of ossification of the zoic marine reptiles (Motani, 2009).
    [Show full text]
  • A New Archosauriform Reptile with Distinctive Teeth from the Middle Triassic (Ladinian) of Germany
    Journal of Vertebrate Paleontology ISSN: (Print) (Online) Journal homepage: https://www.tandfonline.com/loi/ujvp20 A new archosauriform reptile with distinctive teeth from the Middle Triassic (Ladinian) of Germany Hans-Dieter Sues , Rainer R. Schoch , Gabriela Sobral & Randall B. Irmis To cite this article: Hans-Dieter Sues , Rainer R. Schoch , Gabriela Sobral & Randall B. Irmis (2020) A new archosauriform reptile with distinctive teeth from the Middle Triassic (Ladinian) of Germany, Journal of Vertebrate Paleontology, 40:1, e1764968, DOI: 10.1080/02724634.2020.1764968 To link to this article: https://doi.org/10.1080/02724634.2020.1764968 View supplementary material Published online: 23 Jun 2020. Submit your article to this journal Article views: 200 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=ujvp20 Journal of Vertebrate Paleontology e1764968 (14 pages) The work of Hans–Dieter Sues was authored as part of his official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 USC. 105, no copyright protection is available for such works under US Law. Rainer R. Schoch, Gabriela Sobral and Randall B. Irmis hereby waive their right to assert copyright, but not their right to be named as co–authors in the article. DOI: 10.1080/02724634.2020.1764968 ARTICLE A NEW ARCHOSAURIFORM REPTILE WITH DISTINCTIVE TEETH FROM THE MIDDLE TRIASSIC (LADINIAN) OF GERMANY HANS-DIETER SUES, *,1 RAINER R. SCHOCH, 2 GABRIELA SOBRAL, 2 and RANDALL B. IRMIS3 1Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, MRC 121, P.O.
    [Show full text]
  • Estimating the Evolutionary Rates in Mosasauroids and Plesiosaurs: Discussion of Niche Occupation in Late Cretaceous Seas
    Estimating the evolutionary rates in mosasauroids and plesiosaurs: discussion of niche occupation in Late Cretaceous seas Daniel Madzia1 and Andrea Cau2 1 Department of Evolutionary Paleobiology, Institute of Paleobiology, Polish Academy of Sciences, Warsaw, Poland 2 Independent, Parma, Italy ABSTRACT Observations of temporal overlap of niche occupation among Late Cretaceous marine amniotes suggest that the rise and diversification of mosasauroid squamates might have been influenced by competition with or disappearance of some plesiosaur taxa. We discuss that hypothesis through comparisons of the rates of morphological evolution of mosasauroids throughout their evolutionary history with those inferred for contemporary plesiosaur clades. We used expanded versions of two species- level phylogenetic datasets of both these groups, updated them with stratigraphic information, and analyzed using the Bayesian inference to estimate the rates of divergence for each clade. The oscillations in evolutionary rates of the mosasauroid and plesiosaur lineages that overlapped in time and space were then used as a baseline for discussion and comparisons of traits that can affect the shape of the niche structures of aquatic amniotes, such as tooth morphologies, body size, swimming abilities, metabolism, and reproduction. Only two groups of plesiosaurs are considered to be possible niche competitors of mosasauroids: the brachauchenine pliosaurids and the polycotylid leptocleidians. However, direct evidence for interactions between mosasauroids and plesiosaurs is scarce and limited only to large mosasauroids as the Submitted 31 July 2019 predators/scavengers and polycotylids as their prey. The first mosasauroids differed Accepted 18 March 2020 from contemporary plesiosaurs in certain aspects of all discussed traits and no evidence Published 13 April 2020 suggests that early representatives of Mosasauroidea diversified after competitions with Corresponding author plesiosaurs.
    [Show full text]
  • A New Plesiosaur from the Lower Jurassic of Portugal and the Early Radiation of Plesiosauroidea
    A new plesiosaur from the Lower Jurassic of Portugal and the early radiation of Plesiosauroidea EDUARDO PUÉRTOLAS-PASCUAL, MIGUEL MARX, OCTÁVIO MATEUS, ANDRÉ SALEIRO, ALEXANDRA E. FERNANDES, JOÃO MARINHEIRO, CARLA TOMÁS, and SIMÃO MATEUS Puértolas-Pascual, E., Marx, M., Mateus, O., Saleiro, A., Fernandes, A.E., Marinheiro, J., Tomás, C. and Mateus, S. 2021. A new plesiosaur from the Lower Jurassic of Portugal and the early radiation of Plesiosauroidea. Acta Palaeontologica Polonica 66 (2): 369–388. A new plesiosaur partial skeleton, comprising most of the trunk and including axial, limb, and girdle bones, was collected in the lower Sinemurian (Coimbra Formation) of Praia da Concha, near São Pedro de Moel in central west Portugal. The specimen represents a new genus and species, Plesiopharos moelensis gen. et sp. nov. Phylogenetic analysis places this taxon at the base of Plesiosauroidea. Its position is based on this exclusive combination of characters: presence of a straight preaxial margin of the radius; transverse processes of mid-dorsal vertebrae horizontally oriented; ilium with sub-circular cross section of the shaft and subequal anteroposterior expansion of the dorsal blade; straight proximal end of the humerus; and ventral surface of the humerus with an anteroposteriorly long shallow groove between the epipodial facets. In addition, the new taxon has the following autapomorphies: iliac blade with less expanded, rounded and convex anterior flank; highly developed ischial facet of the ilium; apex of the neural spine of the first pectoral vertebra inclined posterodorsally with a small rounded tip. This taxon represents the most complete and the oldest plesiosaur species in the Iberian Peninsula.
    [Show full text]
  • (Diapsida: Saurosphargidae), with Implications for the Morphological Diversity and Phylogeny of the Group
    Geol. Mag.: page 1 of 21. c Cambridge University Press 2013 1 doi:10.1017/S001675681300023X A new species of Largocephalosaurus (Diapsida: Saurosphargidae), with implications for the morphological diversity and phylogeny of the group ∗ CHUN LI †, DA-YONG JIANG‡, LONG CHENG§, XIAO-CHUN WU†¶ & OLIVIER RIEPPEL ∗ Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, PO Box 643, Beijing 100044, China ‡Department of Geology and Geological Museum, Peking University, Beijing 100871, PR China §Wuhan Institute of Geology and Mineral Resources, Wuhan, 430223, PR China ¶Canadian Museum of Nature, PO Box 3443, STN ‘D’, Ottawa, ON K1P 6P4, Canada Department of Geology, The Field Museum, 1400 S. Lake Shore Drive, Chicago, IL 60605-2496, USA (Received 31 July 2012; accepted 25 February 2013) Abstract – Largocephalosaurus polycarpon Cheng et al. 2012a was erected after the study of the skull and some parts of a skeleton and considered to be an eosauropterygian. Here we describe a new species of the genus, Largocephalosaurus qianensis, based on three specimens. The new species provides many anatomical details which were described only briefly or not at all in the type species, and clearly indicates that Largocephalosaurus is a saurosphargid. It differs from the type species mainly in having three premaxillary teeth, a very short retroarticular process, a large pineal foramen, two sacral vertebrae, and elongated small granular osteoderms mixed with some large ones along the lateral most side of the body. With additional information from the new species, we revise the diagnosis and the phylogenetic relationships of Largocephalosaurus and clarify a set of diagnostic features for the Saurosphargidae Li et al.
    [Show full text]
  • The Magnetobiostratigraphy of the Middle Triassic and the Latest Early Triassic from Spitsbergen, Arctic Norway Mark W
    Intercalibration of Boreal and Tethyan time scales: the magnetobiostratigraphy of the Middle Triassic and the latest Early Triassic from Spitsbergen, Arctic Norway Mark W. Hounslow,1 Mengyu Hu,1 Atle Mørk,2,6 Wolfgang Weitschat,3 Jorunn Os Vigran,2 Vassil Karloukovski1 & Michael J. Orchard5 1 Centre for Environmental Magnetism and Palaeomagnetism, Geography, Lancaster Environment Centre, Lancaster University, Bailrigg, Lancaster, LA1 4YQ, UK 2 SINTEF Petroleum Research, NO-7465 Trondheim, Norway 3 Geological-Palaeontological Institute and Museum, University of Hamburg, Bundesstrasse 55, DE-20146 Hamburg, Germany 5 Geological Survey of Canada, 101-605 Robson Street, Vancouver, BC, V6B 5J3, Canada 6 Department of Geology and Mineral Resources Engineering, Norwegian University of Sciences and Technology, NO-7491 Trondheim, Norway Keywords Abstract Ammonoid biostratigraphy; Boreal; conodonts; magnetostratigraphy; Middle An integrated biomagnetostratigraphic study of the latest Early Triassic to Triassic. the upper parts of the Middle Triassic, at Milne Edwardsfjellet in central Spitsbergen, Svalbard, allows a detailed correlation of Boreal and Tethyan Correspondence biostratigraphies. The biostratigraphy consists of ammonoid and palynomorph Mark W. Hounslow, Centre for Environmental zonations, supported by conodonts, through some 234 m of succession in two Magnetism and Palaeomagnetism, adjacent sections. The magnetostratigraphy consists of 10 substantive normal— Geography, Lancaster Environment Centre, Lancaster University, Bailrigg, Lancaster, LA1 reverse polarity chrons, defined by sampling at 150 stratigraphic levels. The 4YQ, UK. E-mail: [email protected] magnetization is carried by magnetite and an unidentified magnetic sulphide, and is difficult to fully separate from a strong present-day-like magnetization. doi:10.1111/j.1751-8369.2008.00074.x The biomagnetostratigraphy from the late Olenekian (Vendomdalen Member) is supplemented by data from nearby Vikinghøgda.
    [Show full text]
  • Exceptional Vertebrate Biotas from the Triassic of China, and the Expansion of Marine Ecosystems After the Permo-Triassic Mass Extinction
    Earth-Science Reviews 125 (2013) 199–243 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Exceptional vertebrate biotas from the Triassic of China, and the expansion of marine ecosystems after the Permo-Triassic mass extinction Michael J. Benton a,⁎, Qiyue Zhang b, Shixue Hu b, Zhong-Qiang Chen c, Wen Wen b, Jun Liu b, Jinyuan Huang b, Changyong Zhou b, Tao Xie b, Jinnan Tong c, Brian Choo d a School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK b Chengdu Center of China Geological Survey, Chengdu 610081, China c State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (Wuhan), Wuhan 430074, China d Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China article info abstract Article history: The Triassic was a time of turmoil, as life recovered from the most devastating of all mass extinctions, the Received 11 February 2013 Permo-Triassic event 252 million years ago. The Triassic marine rock succession of southwest China provides Accepted 31 May 2013 unique documentation of the recovery of marine life through a series of well dated, exceptionally preserved Available online 20 June 2013 fossil assemblages in the Daye, Guanling, Zhuganpo, and Xiaowa formations. New work shows the richness of the faunas of fishes and reptiles, and that recovery of vertebrate faunas was delayed by harsh environmental Keywords: conditions and then occurred rapidly in the Anisian. The key faunas of fishes and reptiles come from a limited Triassic Recovery area in eastern Yunnan and western Guizhou provinces, and these may be dated relative to shared strati- Reptile graphic units, and their palaeoenvironments reconstructed.
    [Show full text]
  • What Really Happened in the Late Triassic?
    Historical Biology, 1991, Vol. 5, pp. 263-278 © 1991 Harwood Academic Publishers, GmbH Reprints available directly from the publisher Printed in the United Kingdom Photocopying permitted by license only WHAT REALLY HAPPENED IN THE LATE TRIASSIC? MICHAEL J. BENTON Department of Geology, University of Bristol, Bristol, BS8 1RJ, U.K. (Received January 7, 1991) Major extinctions occurred both in the sea and on land during the Late Triassic in two major phases, in the middle to late Carnian and, 12-17 Myr later, at the Triassic-Jurassic boundary. Many recent reports have discounted the role of the earlier event, suggesting that it is (1) an artefact of a subsequent gap in the record, (2) a complex turnover phenomenon, or (3) local to Europe. These three views are disputed, with evidence from both the marine and terrestrial realms. New data on terrestrial tetrapods suggests that the late Carnian event was more important than the end-Triassic event. For tetrapods, the end-Triassic extinction was a whimper that was followed by the radiation of five families of dinosaurs and mammal- like reptiles, while the late Carnian event saw the disappearance of nine diverse families, and subsequent radiation of 13 families of turtles, crocodilomorphs, pterosaurs, dinosaurs, lepidosaurs and mammals. Also, for many groups of marine animals, the Carnian event marked a more significant turning point in diversification than did the end-Triassic event. KEY WORDS: Triassic, mass extinction, tetrapod, dinosaur, macroevolution, fauna. INTRODUCTION Most studies of mass extinction identify a major event in the Late Triassic, usually placed at the Triassic-Jurassic boundary.
    [Show full text]
  • Late Cretaceous) of Morocco : Palaeobiological and Behavioral Implications Remi Allemand
    Endocranial microtomographic study of marine reptiles (Plesiosauria and Mosasauroidea) from the Turonian (Late Cretaceous) of Morocco : palaeobiological and behavioral implications Remi Allemand To cite this version: Remi Allemand. Endocranial microtomographic study of marine reptiles (Plesiosauria and Mosasauroidea) from the Turonian (Late Cretaceous) of Morocco : palaeobiological and behavioral implications. Paleontology. Museum national d’histoire naturelle - MNHN PARIS, 2017. English. NNT : 2017MNHN0015. tel-02375321 HAL Id: tel-02375321 https://tel.archives-ouvertes.fr/tel-02375321 Submitted on 22 Nov 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. MUSEUM NATIONAL D’HISTOIRE NATURELLE Ecole Doctorale Sciences de la Nature et de l’Homme – ED 227 Année 2017 N° attribué par la bibliothèque |_|_|_|_|_|_|_|_|_|_|_|_| THESE Pour obtenir le grade de DOCTEUR DU MUSEUM NATIONAL D’HISTOIRE NATURELLE Spécialité : Paléontologie Présentée et soutenue publiquement par Rémi ALLEMAND Le 21 novembre 2017 Etude microtomographique de l’endocrâne de reptiles marins (Plesiosauria et Mosasauroidea) du Turonien (Crétacé supérieur) du Maroc : implications paléobiologiques et comportementales Sous la direction de : Mme BARDET Nathalie, Directrice de Recherche CNRS et les co-directions de : Mme VINCENT Peggy, Chargée de Recherche CNRS et Mme HOUSSAYE Alexandra, Chargée de Recherche CNRS Composition du jury : M.
    [Show full text]
  • Triassic Isopoda – Three New Species from Central Europe Shed Light On
    University of Groningen Triassic Isopoda – three new species from Central Europe shed light on the early diversity of the group Schädel, Mario; van Eldijk, Timo; Winkelhorst, Herman; Reumer, Jelle W.F.; Haug, Joachim T. Published in: Bulletin of Geosciences DOI: 10.3140/bull.geosci.1773 IMPORTANT NOTE: You are advised to consult the publisher's version (publisher's PDF) if you wish to cite from it. Please check the document version below. Document Version Publisher's PDF, also known as Version of record Publication date: 2020 Link to publication in University of Groningen/UMCG research database Citation for published version (APA): Schädel, M., van Eldijk, T., Winkelhorst, H., Reumer, J. W. F., & Haug, J. T. (2020). Triassic Isopoda – three new species from Central Europe shed light on the early diversity of the group. Bulletin of Geosciences, 95(2), 145-166. https://doi.org/10.3140/bull.geosci.1773 Copyright Other than for strictly personal use, it is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license (like Creative Commons). Take-down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. Downloaded from the University of Groningen/UMCG research database (Pure): http://www.rug.nl/research/portal. For technical reasons the number of authors shown on this cover page is limited to 10 maximum. Download date: 24-09-2021 Triassic Isopoda – three new species from Central Europe shed light on the early diversity of the group Mario Schädel, TiMo van eldijk, herMan WinkelhorST, jelle W.F.
    [Show full text]
  • 15. Fossile Lebensgemeinschaften Im Lettenkeuper 15 Hans Hagdorn, Klaus-Peter Kelber Und Rainer Schoch
    15. Fossile Lebensgemeinschaften im Lettenkeuper 15 Hans Hagdorn, Klaus-Peter Kelber und Rainer Schoch Abstract This chapter aims at reconstructing Lower Keuper palaeocommunities in their habitats and to elucidate interdependences of plants, invertebrates, and vertebrates. Four major groups of palaeocommunities are differentiated: (1) The terrestrial palaeocommunities are poorly known from transported fl oral and faunal elements into submersed depositional environments and rooted soil horizons. Clusters of insect eggs and nutritional traces on plants indicate animal-plant-interactions. Small pieces of charcoal give evidence of fi res. The terrestrial reptile record comprises small insectivores and larger carnivores with the rauisuchian Batrachotomus as the top predator, while herbivores are still unknown. The other groups of palaeocommunities depend on the salinity of the water bodies. (2) The fresh- water palaeocommunities are characterized by charophytes, by darwinulid ostracods, by bivalves (Unionites brevis/Unionites donaci- nus) and by amphibians. Here, a low diverse amphibian (Mastodonsaurus/Plagiosuchus/Gerrothorax) and a high diverse amphibian/ reptile palaeocommunity (Mastodonsaurus, Callistomordax, Kupferzellia, Trematolestes, choristoderes, and questionable juvenile tha- lattosaurs) can be discerned. (3) The three brackish water palaeocommunities are dominated by invertebrates: Myophoria/Bakevel- lia, Lingularia/Euestheria, “Anodonta” gregaria). (4) Among the nearly marine palaeocommunities are fi ve bivalve-dominated: Entolium
    [Show full text]
  • 2009 Geologic Time Scale Cenozoic Mesozoic Paleozoic Precambrian Magnetic Magnetic Bdy
    2009 GEOLOGIC TIME SCALE CENOZOIC MESOZOIC PALEOZOIC PRECAMBRIAN MAGNETIC MAGNETIC BDY. AGE POLARITY PICKS AGE POLARITY PICKS AGE PICKS AGE . N PERIOD EPOCH AGE PERIOD EPOCH AGE PERIOD EPOCH AGE EON ERA PERIOD AGES (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) HIST. HIST. ANOM. ANOM. (Ma) CHRON. CHRO HOLOCENE 65.5 1 C1 QUATER- 0.01 30 C30 542 CALABRIAN MAASTRICHTIAN NARY PLEISTOCENE 1.8 31 C31 251 2 C2 GELASIAN 70 CHANGHSINGIAN EDIACARAN 2.6 70.6 254 2A PIACENZIAN 32 C32 L 630 C2A 3.6 WUCHIAPINGIAN PLIOCENE 260 260 3 ZANCLEAN 33 CAMPANIAN CAPITANIAN 5 C3 5.3 266 750 NEOPRO- CRYOGENIAN 80 C33 M WORDIAN MESSINIAN LATE 268 TEROZOIC 3A C3A 83.5 ROADIAN 7.2 SANTONIAN 271 85.8 KUNGURIAN 850 4 276 C4 CONIACIAN 280 4A 89.3 ARTINSKIAN TONIAN C4A L TORTONIAN 90 284 TURONIAN PERMIAN 10 5 93.5 E 1000 1000 C5 SAKMARIAN 11.6 CENOMANIAN 297 99.6 ASSELIAN STENIAN SERRAVALLIAN 34 C34 299.0 5A 100 300 GZELIAN C5A 13.8 M KASIMOVIAN 304 1200 PENNSYL- 306 1250 15 5B LANGHIAN ALBIAN MOSCOVIAN MESOPRO- C5B VANIAN 312 ECTASIAN 5C 16.0 110 BASHKIRIAN TEROZOIC C5C 112 5D C5D MIOCENE 320 318 1400 5E C5E NEOGENE BURDIGALIAN SERPUKHOVIAN 326 6 C6 APTIAN 20 120 1500 CALYMMIAN E 20.4 6A C6A EARLY MISSIS- M0r 125 VISEAN 1600 6B C6B AQUITANIAN M1 340 SIPPIAN M3 BARREMIAN C6C 23.0 345 6C CRETACEOUS 130 M5 130 STATHERIAN CARBONIFEROUS TOURNAISIAN 7 C7 HAUTERIVIAN 1750 25 7A M10 C7A 136 359 8 C8 L CHATTIAN M12 VALANGINIAN 360 L 1800 140 M14 140 9 C9 M16 FAMENNIAN BERRIASIAN M18 PROTEROZOIC OROSIRIAN 10 C10 28.4 145.5 M20 2000 30 11 C11 TITHONIAN 374 PALEOPRO- 150 M22 2050 12 E RUPELIAN
    [Show full text]