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Studies on Continental Late Triassic Tetrapod Biochronology. I. the Type Locality of Saturnalia Tupiniquim and the Faunal Succession in South Brazil
Journal of South American Earth Sciences 19 (2005) 205–218 www.elsevier.com/locate/jsames Studies on continental Late Triassic tetrapod biochronology. I. The type locality of Saturnalia tupiniquim and the faunal succession in south Brazil Max Cardoso Langer* Departamento de Biologia, FFCLRP, Universidade de Sa˜o Paulo (USP), Av. Bandeirantes 3900, 14040-901 Ribeira˜o Preto, SP, Brazil Received 1 November 2003; accepted 1 January 2005 Abstract Late Triassic deposits of the Parana´ Basin, Rio Grande do Sul, Brazil, encompass a single third-order, tetrapod-bearing sedimentary sequence that includes parts of the Alemoa Member (Santa Maria Formation) and the Caturrita Formation. A rich, diverse succession of terrestrial tetrapod communities is recorded in these sediments, which can be divided into at least three faunal associations. The stem- sauropodomorph Saturnalia tupiniquim was collected in the locality known as ‘Waldsanga’ near the city of Santa Maria. In that area, the deposits of the Alemoa Member yield the ‘Alemoa local fauna,’ which typifies the first association; includes the rhynchosaur Hyperodapedon, aetosaurs, and basal dinosaurs; and is coeval with the lower fauna of the Ischigualasto Formation, Bermejo Basin, NW Argentina. The second association is recorded in deposits of both the Alemoa Member and the Caturrita Formation, characterized by the rhynchosaur ‘Scaphonyx’ sulcognathus and the cynodont Exaeretodon, and correlated with the upper fauna of the Ischigualasto Formation. Various isolated outcrops of the Caturrita Formation yield tetrapod fossils that correspond to post-Ischigualastian faunas but might not belong to a single faunal association. The record of the dicynodont Jachaleria suggests correlations with the lower part of the Los Colorados Formation, NW Argentina, whereas remains of derived tritheledontid cynodonts indicate younger ages. -
A Revision of the Classification of the Plesiosauria with a Synopsis of the Stratigraphical and Geographical Distribution Of
LUNDS UNIVERSITETS ARSSKRIFT. N. F. Avd. 2. Bd 59. Nr l. KUNGL. FYSIOGRAFISKA SÅLLSKAPETS HANDLINGAR, N. F. Bd 74. Nr 1. A REVISION OF THE CLASSIFICATION OF THE PLESIOSAURIA WITH A SYNOPSIS OF THE STRATIGRAPHICAL AND GEOGRAPHICAL DISTRIBUTION OF THE GROUP BY PER OVE PERSSON LUND C. W. K. GLEER UP Read before the Royal Physiographic Society, February 13, 1963. LUND HÅKAN OHLSSONS BOKTRYCKERI l 9 6 3 l. Introduction The sub-order Plesiosauria is one of the best known of the Mesozoic Reptile groups, but, as emphasized by KuHN (1961, p. 75) and other authors, its classification is still not satisfactory, and needs a thorough revision. The present paper is an attempt at such a revision, and includes also a tabular synopsis of the stratigraphical and geo graphical distribution of the group. Some of the species are discussed in the text (pp. 17-22). The synopsis is completed with seven maps (figs. 2-8, pp. 10-16), a selective synonym list (pp. 41-42), and a list of rejected species (pp. 42-43). Some forms which have been erroneously referred to the Plesiosauria are also briefly mentioned ("Non-Plesiosaurians", p. 43). - The numerals in braekets after the generic and specific names in the text refer to the tabular synopsis, in which the different forms are numbered in successional order. The author has exaroined all material available from Sweden, Australia and Spitzbergen (PERSSON 1954, 1959, 1960, 1962, 1962a); the major part of the material from the British Isles, France, Belgium and Luxembourg; some of the German spec imens; certain specimens from New Zealand, now in the British Museum (see LYDEK KER 1889, pp. -
Tetrapod Biostratigraphy and Biochronology of the Triassic–Jurassic Transition on the Southern Colorado Plateau, USA
Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 242–256 www.elsevier.com/locate/palaeo Tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau, USA Spencer G. Lucas a,⁎, Lawrence H. Tanner b a New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104-1375, USA b Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA Received 15 March 2006; accepted 20 June 2006 Abstract Nonmarine fluvial, eolian and lacustrine strata of the Chinle and Glen Canyon groups on the southern Colorado Plateau preserve tetrapod body fossils and footprints that are one of the world's most extensive tetrapod fossil records across the Triassic– Jurassic boundary. We organize these tetrapod fossils into five, time-successive biostratigraphic assemblages (in ascending order, Owl Rock, Rock Point, Dinosaur Canyon, Whitmore Point and Kayenta) that we assign to the (ascending order) Revueltian, Apachean, Wassonian and Dawan land-vertebrate faunachrons (LVF). In doing so, we redefine the Wassonian and the Dawan LVFs. The Apachean–Wassonian boundary approximates the Triassic–Jurassic boundary. This tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau confirms that crurotarsan extinction closely corresponds to the end of the Triassic, and that a dramatic increase in dinosaur diversity, abundance and body size preceded the end of the Triassic. © 2006 Elsevier B.V. All rights reserved. Keywords: Triassic–Jurassic boundary; Colorado Plateau; Chinle Group; Glen Canyon Group; Tetrapod 1. Introduction 190 Ma. On the southern Colorado Plateau, the Triassic– Jurassic transition was a time of significant changes in the The Four Corners (common boundary of Utah, composition of the terrestrial vertebrate (tetrapod) fauna. -
Evaluating the Ecology of Spinosaurus: Shoreline Generalist Or Aquatic Pursuit Specialist?
Palaeontologia Electronica palaeo-electronica.org Evaluating the ecology of Spinosaurus: Shoreline generalist or aquatic pursuit specialist? David W.E. Hone and Thomas R. Holtz, Jr. ABSTRACT The giant theropod Spinosaurus was an unusual animal and highly derived in many ways, and interpretations of its ecology remain controversial. Recent papers have added considerable knowledge of the anatomy of the genus with the discovery of a new and much more complete specimen, but this has also brought new and dramatic interpretations of its ecology as a highly specialised semi-aquatic animal that actively pursued aquatic prey. Here we assess the arguments about the functional morphology of this animal and the available data on its ecology and possible habits in the light of these new finds. We conclude that based on the available data, the degree of adapta- tions for aquatic life are questionable, other interpretations for the tail fin and other fea- tures are supported (e.g., socio-sexual signalling), and the pursuit predation hypothesis for Spinosaurus as a “highly specialized aquatic predator” is not supported. In contrast, a ‘wading’ model for an animal that predominantly fished from shorelines or within shallow waters is not contradicted by any line of evidence and is well supported. Spinosaurus almost certainly fed primarily from the water and may have swum, but there is no evidence that it was a specialised aquatic pursuit predator. David W.E. Hone. Queen Mary University of London, Mile End Road, London, E1 4NS, UK. [email protected] Thomas R. Holtz, Jr. Department of Geology, University of Maryland, College Park, Maryland 20742 USA and Department of Paleobiology, National Museum of Natural History, Washington, DC 20560 USA. -
(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. -
University of Birmingham the Earliest Bird-Line Archosaurs and The
University of Birmingham The earliest bird-line archosaurs and the assembly of the dinosaur body plan Nesbitt, Sterling; Butler, Richard; Ezcurra, Martin; Barrett, Paul; Stocker, Michelle; Angielczyk, Kenneth; Smith, Roger; Sidor, Christian; Niedzwiedzki, Grzegorz; Sennikov, Andrey; Charig, Alan DOI: 10.1038/nature22037 License: None: All rights reserved Document Version Peer reviewed version Citation for published version (Harvard): Nesbitt, S, Butler, R, Ezcurra, M, Barrett, P, Stocker, M, Angielczyk, K, Smith, R, Sidor, C, Niedzwiedzki, G, Sennikov, A & Charig, A 2017, 'The earliest bird-line archosaurs and the assembly of the dinosaur body plan', Nature, vol. 544, no. 7651, pp. 484-487. https://doi.org/10.1038/nature22037 Link to publication on Research at Birmingham portal Publisher Rights Statement: Checked for eligibility: 03/03/2017. General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. Where a licence is displayed above, please note the terms and conditions of the licence govern your use of this document. -
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, -
A Ne\T Prolacertiform Reptile from the Late Triassic of Northern Italy
Riv. It. Paleont. Strat. v. 100 n.2 pp. 285-306 tav. 1-3 Ottobre 1994 A NE\T PROLACERTIFORM REPTILE FROM THE LATE TRIASSIC OF NORTHERN ITALY SLVIO RENESTO Key-uords: Langobardisaurus pandolfii, New Genus, Reptilia, Diapsida, Late Triassic, Description, Palaeoecology. Riassunto. Vengono descritti due esemplari di Renili fossili raccolti a Cene (Val Seriana, Bergamo), nel Calcare di Zorzino (Norico Medio, Triassico Superiore). I due esemplari provengono dal medesimo strato e presentano caratteri scheletrici pressochè identici, per cui possono essere considerati conspecifici con ragione- vole cerf.ezza. Possono inohre essere classificati come appartenenti all' ordine dei Prolacertiformi. I confronti con i taxa già noti, consentono di ritenerli come appartenenti ad un genere ed una specie nuovi per la scienza: Langobardisaurus pand.olfii. Le caratteristiche dello scheletro suggeriscono infine che Langobardisaurus fosse un rettile terrestre e si nutrisse prevalentemente di insetti. Absúact. A new diapsid reptile is described from the locality of Cene (Seriana Valley, near Bergamo, Lombardy, Northern ltaly) from an outcrop of the Calcare di Zorzino (Zorzino Limestone) Formation (Middle Norian, Late Triassic). It is based on virtually identical specimens, differing only in size. Analysis of available diagnostic characters allows it to be included in the Prolacertiformes, represenring a new genus and species, Langobardisaurus pandolfi probably related to Macrocnemus, possibly to Cosesaums, and to the Tany- stropheìdae. It is assumed here that Langobardisaurus pandolfii was adapted to a terrestrial mode of life and probably to an insectivorous diet. Introduction. The Norian (Late Triassic) vertebrate localities from the Bergamo Prealps (Lom- bardy, Northern Italy) are of worldwide interest for the diversity and importance of their faunas. -
University of Birmingham Description and Phylogenetic Placement of A
University of Birmingham Description and phylogenetic placement of a new marine species of phytosaur (Archosauriformes: Phytosauria) from the Late Triassic of Austria Butler, Richard; Jones, Andrew; Buffetaut, Eric; Mandl, Gerhard; Scheyer, Torsten; Schultz, Ortwin DOI: 10.1093/zoolinnean/zlz014 License: Other (please specify with Rights Statement) Document Version Peer reviewed version Citation for published version (Harvard): Butler, R, Jones, A, Buffetaut, E, Mandl, G, Scheyer, T & Schultz, O 2019, 'Description and phylogenetic placement of a new marine species of phytosaur (Archosauriformes: Phytosauria) from the Late Triassic of Austria', Zoological Journal of the Linnean Society, vol. 187, no. 1, pp. 198-228. https://doi.org/10.1093/zoolinnean/zlz014 Link to publication on Research at Birmingham portal Publisher Rights Statement: Checked for eligibility 04/02/2019 This is a pre-copyedited, author-produced version of an article accepted for publication in Zoological Journal of the Linnean Society following peer review. The version of record Richard J Butler, Andrew S Jones, Eric Buffetaut, Gerhard W Mandl, Torsten M Scheyer, Ortwin Schultz, Description and phylogenetic placement of a new marine species of phytosaur (Archosauriformes: Phytosauria) from the Late Triassic of Austria, Zoological Journal of the Linnean Society, Volume 187, Issue 1, September 2019, Pages 198–228, is available online at: https://doi.org/10.1093/zoolinnean/zlz014. General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. -
Live Birth in an Archosauromorph Reptile
ARTICLE Received 8 Sep 2016 | Accepted 30 Dec 2016 | Published 14 Feb 2017 DOI: 10.1038/ncomms14445 OPEN Live birth in an archosauromorph reptile Jun Liu1,2,3, Chris L. Organ4, Michael J. Benton5, Matthew C. Brandley6 & Jonathan C. Aitchison7 Live birth has evolved many times independently in vertebrates, such as mammals and diverse groups of lizards and snakes. However, live birth is unknown in the major clade Archosauromorpha, a group that first evolved some 260 million years ago and is represented today by birds and crocodilians. Here we report the discovery of a pregnant long-necked marine reptile (Dinocephalosaurus) from the Middle Triassic (B245 million years ago) of southwest China showing live birth in archosauromorphs. Our discovery pushes back evidence of reproductive biology in the clade by roughly 50 million years, and shows that there is no fundamental reason that archosauromorphs could not achieve live birth. Our phylogenetic models indicate that Dinocephalosaurus determined the sex of their offspring by sex chromosomes rather than by environmental temperature like crocodilians. Our results provide crucial evidence for genotypic sex determination facilitating land-water transitions in amniotes. 1 School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China. 2 Chengdu Center, China Geological Survey, Chengdu 610081, China. 3 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, CAS, Nanjing 210008, China. 4 Department of Earth Sciences, Montana State University, Bozeman, Montana 59717, USA. 5 School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK. 6 School of Life and Environmental Sciences, The University of Sydney, Sydney, New South Wales 2006, Australia. -
Abhandlungen Der Geologischen Bundesanstalt in Wien
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Abhandlungen der Geologischen Bundesanstalt in Wien Jahr/Year: 1893 Band/Volume: 15 Autor(en)/Author(s): Skuphos Theodor Georg Artikel/Article: Ueber Partanosaurus Zitteli Skuphos und Microleptosaurus Schlosseri nov. gen., nov. spec. aus den Vorarlberger Partnachschichten 1-16 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Ausgegeben am 10. October 1893. Ueber Partanosaurus Zitteli Skuphos und Microleptosaurus Schlössen nov. gen., nov. spec. aus den Vorarlberger Partnachschichten. Von Dr. Theodor Georg Skuphos aus Paros. (Mit 3 lithographirten Tafeln und 1 Zinkotypie im Text.) ABHANDLUNGEN DER K. K. GEOLOGISCHEN REICHSANSTALT. BAND XV. HEFT 5. Preis: Oe. W. Ü 4 = R.-M. 8. WIEN, 1893. Verlag der k. k. geolog. Reichsanstalt III., Rasumoffskygasse 23. Gesellschafts-Buchdruckerei Brüder Hollinek, Wien,' III., Erdbergstrasse 3. ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at INHALTS -VERZEICHNIS. Seite Einleitung 1 I. Specielle Beschreibung: von Partanosaurus Zittell Skuphos 3 1. Die Wirbel Nr. 14— 12 3 2. Die Wirbel Nr. 11-8 4 3. Die Wirbel Nr. 7—1 5 Vereinzelte Wirbel 6 Brustgürtel 7 Rippen 8 II. Zusammenfassung und Beziehungen zu den nächstverwandten Nothosauriden 9 III. Das geologische Vorkommen von Partanosaurus Zittell 11 IV. Specielle Beschreibung von Microleptosaurus Schlossert, Skuphos 12 I. Rippen 12 a) Vordere Halsrippen 12 ß) Hinterste Halsrippen t 12 \\ Thorakalrippen 12 o) Bauchrippen 13 II. Wirbel 13 III. Beziehungen zu den nächstverwandten Nothosauriden 13 V. Anhang. Kolposaiirus nov, (je» 14 Kolposaurw vor. spec 14 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ©Geol. -
Ministerio De Cultura Y Educacion Fundacion Miguel Lillo
MINISTERIO DE CULTURA Y EDUCACION FUNDACION MIGUEL LILLO NEW MATERIALS OF LAGOSUCHUS TALAMPAYENSIS ROMER (THECODONTIA - PSEUDOSUCHIA) AND ITS SIGNIFICANCE ON THE ORIGIN J. F. BONAPARTE OF THE SAURISCHIA. LOWER CHANARIAN, MIDDLE TRIASSIC OF ARGENTINA ACTA GEOLOGICA LILLOANA 13, 1: 5-90, 10 figs., 4 pl. TUCUMÁN REPUBLICA ARGENTINA 1975 NEW MATERIALS OF LAGOSUCHUS TALAMPAYENSIS ROMER (THECODONTIA - PSEUDOSUCHIA) AND ITS SIGNIFICANCE ON THE ORIGIN OF THE SAURISCHIA LOWER CHANARIAN, MIDDLE TRIASSIC OF ARGENTINA* by JOSÉ F. BONAPARTE Fundación Miguel Lillo - Career Investigator Member of CONICET ABSTRACT On the basis of new remains of Lagosuchus that are thoroughly described, including most of the skeleton except the manus, it is assumed that Lagosuchus is a form intermediate between Pseudosuchia and Saurischia. The presacral vertebrae show three morphological zones that may be related to bipedality: 1) the anterior cervicals; 2) short cervico-dorsals; and 3) the posterior dorsals. The pelvis as a whole is advanced, in particular the pubis and acetabular area of the ischium, but the ilium is rather primitive. The hind limb has a longer tibia than femur, and the symmetrical foot is as long as the tibia. The tarsus is of the mesotarsal type. The morphology of the distal area of the tibia and fibula, and the proximal area of the tarsus, suggest a stage transitional between the crurotarsal and mesotarsal conditions. The forelimb is proportionally short, 48% of the hind limb. The humerus is slender, with advanced features in the position of the deltoid crest. The radius and ulna are also slender, the latter with a pronounced olecranon process. A new family of Pseudosuchia is proposed for this form: Lagosuchidae.