Complex Rostral Neurovascular System in a Giant Pliosaur
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Cranial Anatomy, Taxonomic Implications
[Palaeontology, Vol. 55, Part 4, 2012, pp. 743–773] CRANIAL ANATOMY, TAXONOMIC IMPLICATIONS AND PALAEOPATHOLOGY OF AN UPPER JURASSIC PLIOSAUR (REPTILIA: SAUROPTERYGIA) FROM WESTBURY, WILTSHIRE, UK by JUDYTH SASSOON1, LESLIE F. NOE` 2 and MICHAEL J. BENTON1* 1School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, UK; e-mails: [email protected], [email protected] 2Geociencias, departamento de Fisica, Universidad de los Andes, Bogota´ DC, Colombia; e-mail: [email protected] *Corresponding author. Typescript received 5 December 2010; accepted in revised form 6 April 2011 Abstract: Complete skulls of giant marine reptiles of the genera. The two Westbury Pliosaurus specimens share many Late Jurassic are rare, and so the discovery of the 1.8-m- features, including the form of the teeth, but marked differ- long skull of a pliosaur from the Kimmeridge Clay Forma- ences in the snout and parietal crest suggest sexual dimor- tion (Kimmeridgian) of Westbury, Wiltshire, UK, is an phism; the present specimen is probably female. The large important find. The specimen shows most of the cranial size of the animal, the extent of sutural fusion and the and mandibular anatomy, as well as a series of pathological pathologies suggest this is an ageing individual. An erosive conditions. It was previously referred to Pliosaurus brachy- arthrotic condition of the articular glenoids led to pro- spondylus, but it can be referred reliably only to the genus longed jaw misalignment, generating a suite of associated Pliosaurus, because species within the genus are currently in bone and dental pathologies. -
A New Species of the Sauropsid Reptile Nothosaurus from the Lower Muschelkalk of the Western Germanic Basin, Winterswijk, the Netherlands
A new species of the sauropsid reptile Nothosaurus from the Lower Muschelkalk of the western Germanic Basin, Winterswijk, The Netherlands NICOLE KLEIN and PAUL C.H. ALBERS Klein, N. and Albers, P.C.H. 2009. A new species of the sauropsid reptile Nothosaurus from the Lower Muschelkalk of the western Germanic Basin, Winterswijk, The Netherlands. Acta Palaeontologica Polonica 54 (4): 589–598. doi:10.4202/ app.2008.0083 A nothosaur skull recently discovered from the Lower Muschelkalk (early Anisian) locality of Winterswijk, The Nether− lands, represents at only 46 mm in length the smallest nothosaur skull known today. It resembles largely the skull mor− phology of Nothosaurus marchicus. Differences concern beside the size, the straight rectangular and relative broad parietals, the short posterior extent of the maxilla, the skull proportions, and the overall low number of maxillary teeth. In spite of its small size, the skull can not unequivocally be interpreted as juvenile. It shows fused premaxillae, nasals, frontals, and parietals, a nearly co−ossified jugal, and fully developed braincase elements, such as a basisphenoid and mas− sive epipterygoids. Adding the specimen to an existing phylogenetic analysis shows that it should be assigned to a new species, Nothosaurus winkelhorsti sp. nov., at least until its juvenile status can be unequivocally verified. Nothosaurus winkelhorsti sp. nov. represents, together with Nothosaurus juvenilis, the most basal nothosaur, so far. Key words: Sauropterygia, Nothosaurus, ontogeny, Anisian, The Netherlands. Nicole Klein [nklein@uni−bonn.de], Steinmann−Institut für Geologie, Mineralogie und Paläontologie, Universtät Bonn, Nußallee 8, 53115 Bonn, Germany; Paul C.H. Albers [[email protected]], Naturalis, Nationaal Natuurhistorisch Museum, Darwinweg 2, 2333 CR Leiden, The Netherlands. -
Decapod Crustaceans from the Middle Jurassic Opalinus Clay of Northern Switzerland, with Comments on Crustacean Taphonomy
0012-9402/04/030381-12 Eclogae geol. Helv. 97 (2004) 381–392 DOI 10.1007/s00015-004-1137-2 Birkhäuser Verlag, Basel, 2004 Decapod crustaceans from the Middle Jurassic Opalinus Clay of northern Switzerland, with comments on crustacean taphonomy WALTER ETTER Key words: Decapoda, Peracarida, Jurassic, Switzerland, ecology, crustacean taphonomy ABSTRACT ZUSAMMENFASSUNG Four species of decapod crustaceans from the Middle Jurassic Opalinus Clay Aus dem Opalinuston (Mittlerer Jura, Aalenian) der Nordschweiz werden vier (Aalenian) of Northern Switzerland are described. Of these, Mecochirus cf. Arten von decapoden Krebsen beschrieben. Von Aeger sp., Eryma cf. bedelta eckerti is the most common one, while Eryma cf. bedelta, Glyphea sp. and und Glyphaea sp. wurden nur ganz wenige Exemplaren gefunden, während Aeger sp. were present as individuals, or only a few specimens. The preserva- Mecochirus cf. eckerti etwas häufiger ist. Die Erhaltungsbedingungen waren tion of these crustaceans ranges from moderate to excellent, reflecting the während der Ablagerung des Opalinustones günstig, was sich in einer geringen favourable taphonomic conditions of the depositional environment. An inter- Disartikulations- und Fragmentationsrate der Krebse widerspiegelt. Ein in- esting aspect of the taphocoenosis in the Opalinus Clay is that the decapod teressanter Aspekt der Taphocoenose ist die deutliche Dominanz der Klein- crustaceans are by far outnumbered by small peracarid crustaceans (isopods krebse (Peracarida: Isopoden und Tanaidaceen). Dies dürfte die Zahlenver- and tanaids). This is interpreted as reflecting the original differences in abun- hältnisse der ehemaligen Lebensgemeinschaft widerspiegeln. In den meisten dance. Yet this distribution is not frequently encountered in sedimentary se- Ablagerungen dominieren jedoch die decapoden Krebse, wogegen Peracarida quences where decapods (although rare) are far more common than isopods äusserst selten sind. -
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. -
The Importance of Winterswijk for Under- Standing Placodontiform Evolution U Vindt Een Samenvatting Aan Het Eind Van De Tekst
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2019 The importance of Winterswijk for understanding placodontiform evolution Neenan, James M ; During, Melanie A D ; Scheyer, Torsten M Abstract: Placodontiformes are basal, semi-aquatic sauropterygians that mostly preyed upon hard-shelled organisms and often had substantial dermal armour. While their fossil remains are rare, they can be found in Triassic sediments throughout Europe, the Middle East and southern China, often in the form of their unusually large, tablet-shaped teeth. Winterswijk, however, boasts one of the most important fossil records for placodontiforms in the world, with two unique genera that are not currently known from anywhere else: Palatodonta bleekeri and Pararcus diepenbroeki. Other than these, more widespread genera are probably also represented in the form of Placodus sp. and Cyamodus sp. Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-181650 Journal Article Published Version Originally published at: Neenan, James M; During, Melanie A D; Scheyer, Torsten M (2019). The importance of Winterswijk for understanding placodontiform evolution. Staringia, 73(5/6):222-225. A B C FIGURE 1. | Placodontiform morphotypes that have been found in Winterswijk. Palatodonta bleekeri (A) is the closest relative of the placodonts, and had small sharp teeth for eating soft prey. The placodonts Placodus gigas (B) and Cyamodus hildegardis (C) had large crushing teeth for eating hard-shelled prey. Note the heavy armour in Cyamodus. Reconstructions by Jaime Chirinos. The importance of Winterswijk for under- standing placodontiform evolution U vindt een samenvatting aan het eind van de tekst. -
(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. -
Mesozoic Marine Reptile Palaeobiogeography in Response to Drifting Plates
ÔØ ÅÒÙ×Ö ÔØ Mesozoic marine reptile palaeobiogeography in response to drifting plates N. Bardet, J. Falconnet, V. Fischer, A. Houssaye, S. Jouve, X. Pereda Suberbiola, A. P´erez-Garc´ıa, J.-C. Rage, P. Vincent PII: S1342-937X(14)00183-X DOI: doi: 10.1016/j.gr.2014.05.005 Reference: GR 1267 To appear in: Gondwana Research Received date: 19 November 2013 Revised date: 6 May 2014 Accepted date: 14 May 2014 Please cite this article as: Bardet, N., Falconnet, J., Fischer, V., Houssaye, A., Jouve, S., Pereda Suberbiola, X., P´erez-Garc´ıa, A., Rage, J.-C., Vincent, P., Mesozoic marine reptile palaeobiogeography in response to drifting plates, Gondwana Research (2014), doi: 10.1016/j.gr.2014.05.005 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Mesozoic marine reptile palaeobiogeography in response to drifting plates To Alfred Wegener (1880-1930) Bardet N.a*, Falconnet J. a, Fischer V.b, Houssaye A.c, Jouve S.d, Pereda Suberbiola X.e, Pérez-García A.f, Rage J.-C.a and Vincent P.a,g a Sorbonne Universités CR2P, CNRS-MNHN-UPMC, Département Histoire de la Terre, Muséum National d’Histoire Naturelle, CP 38, 57 rue Cuvier, -
Science Journals — AAAS
RESEARCH ARTICLE PALEONTOLOGY 2016 © The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. Distributed The earliest herbivorous marine reptile and its under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC). remarkable jaw apparatus 10.1126/sciadv.1501659 Li Chun,1* Olivier Rieppel,2 Cheng Long,3 Nicholas C. Fraser4* Newly discovered fossils of the Middle Triassic reptile Atopodentatus unicus call for a radical reassessment of its feeding behavior. The skull displays a pronounced hammerhead shape that was hitherto unknown. The long, straight anterior edges of both upper and lower jaws were lined with batteries of chisel-shaped teeth, whereas the remaining parts of the jaw rami supported densely packed needle-shaped teeth forming a mesh. The evidence indicates a novel feeding mechanism wherein the chisel-shaped teeth were used to scrape algae off the substrate, and the plant matter that was loosened was filtered from the water column through the more posteriorly positioned tooth mesh. This is the oldest record of herbivory within marine reptiles. Downloaded from INTRODUCTION The recovery of the trophic structure in both terrestrial and marine biota ventral margin of the otherwise closed cheek region. The slight varia- following the end-Permian mass extinction has recently been a topic of bility in the arrangement of the articulation of the frontal with the intense discussion (1–4). Here, we report the first herbivorous filter- parietal is readily attributable to individual -
Fossil Middle Triassic “Sea Cows” – Placodont Reptiles As Macroalgae Feeders Along the North-Western Tethys Coastline with Pangaea and in the Germanic Basin
Vol.3, No.1, 9-27 (2011) Natural Science http://dx.doi.org/10.4236/ns.2011.31002 Fossil middle triassic “sea cows” – placodont reptiles as macroalgae feeders along the north-western Tethys coastline with Pangaea and in the Germanic basin Cajus G. Diedrich Paleologic, Nansenstr, Germany; [email protected] Received 19 October 2010; revised 22 November 2010; accepted 27 November 2010. ABSTRACT this plant-feeding adaptation and may even ex- plain the origin or at least close relationship of The descriptions of fossil Triassic marine pla- the earliest Upper Triassic turtles as toothless codonts as durophagous reptiles are revised algae and jellyfish feeders, in terms of the through comparisons with the sirenia and basal long-term convergent development with the si- proboscidean mammal and palaeoenvironment rens. analyses. The jaws of placodonts are conver- gent with those of Halitherium/Dugong or Mo- Keywords: Placodont Reptiles; Triassic; eritherium in their general function. Whereas Convergent Evolutionary Ecological Adaptation; Halitherium possessed a horny oral pad and Sirenia; Macroalgae Feeders; NW Tethys Shelf; counterpart and a special rasp-like tongue to Palaeoecology grind seagrass, as does the modern Dugong, placodonts had large teeth that covered their 1. INTRODUCTION jaws to form a similar grinding pad. The sirenia also lost their anterior teeth during many Mil- The extinct reptile group of the placodonts found in lions of years and built a horny pad instead and Germany and other European sites (Figure 1), a group specialized tongue to fed mainly on seagrass, of diverse marine diving reptiles, had large teeth cover- whereas placodonts had only macroalgae availa- ing the lower and complete upper jaws (Figsure 2-5) ble. -
Sauropterygia I Placodontia, Pachypleurosauria, Nothosauroidea, Pistosauroidea
Teil 12A / Part 12A Sauropterygia I Placodontia, Pachypleurosauria, Nothosauroidea, Pistosauroidea by O. RlEPPEL With 80 Figures Verlag Dr. Friedrich Pfeil • Munchen 2000 ISBN 3-931516-78-4 Contents Foreword (P. WELLNHOFER) V Acknowledgements VI Institutional Acronyms VII Figure Abbreviations VIII Introduction: History of the Concept of Sauropterygia 1 Phylogenetic Relationships of Stem-Group Sauropterygia 4 Stratigraphic and Geographic Distribution of Stem-Group Sauropterygia 6 General Skeletal Anatomy of Stem-Group Sauropterygia 10 Systematic Review 16 Superorder Sauropterygia OWEN, 1860 16 Order Placodontia COPE, 1871 16 Suborder Placodontoidea COPE, 1871 16 Family Paraplacodontidae PEYER & KUHN-SCHNYDER, 1955 17 Anatomy of Paraplacodontidae 17 Genus Paraplacodus PEYER, 1931 18 Family Placodontidae COPE, 1871 19 Anatomy of Placodontidae 19 Genus Placodus AGASSIZ, 1933 21 Suborder Cyamodontoidea NOPCSA, 1923 23 Anatomy of Cyamodontoidea 23 Interrelationships of Cyamodontoidea 25 Superfamily Cyamodontida NOPCSA, 1923 25 Family Henodontidae F. v. HUENE, 1948 26 Genus Henodus F. v. HUENE, 1936 26 Family Cyamodontidae NOPCSA, 1923 27 Genus Cyamodus MEYER, 1863 27 Superfamily Placochelyida ROMER, 1956 32 Family Macroplacidae nov. fam 32 Genus Macroplacus SCHUBERT-KLEMPNAUER, 1975 32 Family Protenodontosauridae nov. fam 33 Genus Protenodontosaurus PINNA, 1990 33 Family Placochelyidae ROMER, 1956 34 Genus Placochelys JAEKEL, 1902 34 Genus Psephoderma MEYER, 1858 36 Genus Psephosaurus E. FRAAS, 1896 38 Cyamodontoidea indet 39 IX Order Eosauropterygia -
Marine Reptiles
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Institutional Research Information System University of Turin Geobios 39 (2006) 346–354 http://france.elsevier.com/direct/GEOBIO/ Marine reptiles (Thalattosuchia) from the Early Jurassic of Lombardy (northern Italy) Rettili marini (Thalattosuchia) del Giurassico inferiore della Lombardia (Italia settentrionale) Reptiles marins (Thalattosuchia) du Jurassique inférieur de la Lombardie (Italie du nord) Massimo Delfino a,*, Cristiano Dal Sasso b a Dipartimento di Scienze della Terra, Università di Firenze, Via G. La Pira 4, 50121 Firenze, Italy b Museo Civico di Storia Naturale, Corso Venezia 55, 20121 Milano, Italy Received 24 May 2004; accepted 3 January 2005 Available online 28 February 2006 Abstract The fossil remains of two small reptiles recently discovered in the Sogno Formation (Lower Toarcian) near Cesana Brianza (Lecco Province), represent the first mesoeucrocodylians reported for Lombardy and some of the few Jurassic reptiles from Italy. Due to the absence of diagnostic skeletal elements (the skulls are lacking), it is not possible to refer the new specimens at genus level with confidence. Although the well devel- oped dermal armour would characterise Toarcian thalattosuchians of the genera Steneosaurus (Teleosauridae) and Pelagosaurus (Metriorhynch- idae), the peculiar morphology of the osteoderms allow to tentatively refer the remains to the latter taxon (cf. Pelagosaurus sp.). The small size, along with the opening of the neurocentral vertebral sutures and, possibly, the non sutured caudal pleurapophyses, indicate that the specimens were morphologically immature at death. These “marine crocodiles” confirm the affinities between the fauna of the Calcare di Sogno Formation and coeval outcrops of central Europe that also share the presence of similar fishes and crustaceans. -
Geol. Quart. 49 (3)
Geological Quarterly, 2005, 49 (3): 317–330 The Ciechocinek Formation (Lower Jurassic) of SW Poland: petrology of green clastic rocks Paulina LEONOWICZ Leonowicz P. (2005) — The Ciechocinek Formation (Lower Jurassic) of SW Poland: petrology of green clastic rocks. Geol. Quart., 49 (3): 317–330. Warszawa. The Lower Jurassic Ciechocinek Formation from the Czêstochowa-Wieluñ region of SW Poland comprises greenish-grey muds and silts as well as poorly consolidated mudstones and siltstones with lenticular intercalations of fine-grained sands, sandstones and siderites. Analysis of a mineral composition indicates that the detrital material was derived mainly from the weathering of metamorphic and sedi- mentary rocks of the eastern Sudetes with their foreland and of the Upper Silesia area, and that this material underwent repeated redeposition. The Fe-rich chlorites which give the green colour to the mudstones of the Ciechocinek Formation are most probably early diagenetic minerals, genetically linked with the deposition in a brackish sedimentary basin. Paulina Leonowicz, Institute of Geology, University of Warsaw, ¯wirki i Wigury 93, PL-02-089 Warszawa, Poland, e-mail: [email protected] (received: June 8, 2004; accepted: March 3, 2005). Key words: Lower Jurassic, Cracow-Silesian Upland, provenance, petrology, sandstones, mudstones. INTRODUCTION and Wieluñ (Fig. 2). Its main purpose is recognition of the provenance of clastic material in these rocks, based on their mineral composition, and investigation of the origin of the The Ciechocinek Formation (Pieñkowski, 2004), earlier characteristic green colour of the mudstones, generally consid- known as the Lower £ysiec, Gryfice, Ciechocinek or Estheria ered as the characteristic feature of the Ciechocinek Formation.