New Clade of Enigmatic Early Archosaurs Yields Insights
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(Reptilia: Archosauria) from the Late Triassic of North America
Journal of Vertebrate Paleontology 20(4):633±636, December 2000 q 2000 by the Society of Vertebrate Paleontology RAPID COMMUNICATION FIRST RECORD OF ERPETOSUCHUS (REPTILIA: ARCHOSAURIA) FROM THE LATE TRIASSIC OF NORTH AMERICA PAUL E. OLSEN1, HANS-DIETER SUES2, and MARK A. NORELL3 1Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964; 2Department of Palaeobiology, Royal Ontario Museum, 100 Queen's Park, Toronto, Ontario, Canada M5S 2C6 and Department of Zoology, University of Toronto, Toronto, Ontario, Canada M5S 3G5; 3Division of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, New York 10024 INTRODUCTION time-scales (Gradstein et al., 1995; Kent and Olsen, 1999). Third, Lucas et al. (1998) synonymized Stegomus with Aeto- To date, few skeletal remains of tetrapods have been recov- saurus and considered the latter taxon an index fossil for con- ered from the Norian- to Rhaetian-age continental strata of the tinental strata of early to middle Norian age. As discussed else- Newark Supergroup in eastern North America. It has always where, we regard this as the weakest line of evidence (Sues et been assumed that these red clastic deposits are largely devoid al., 1999). of vertebrate fossils, and thus they have almost never been sys- tematically prospected for such remains. During a geological DESCRIPTION ®eld-trip in March 1995, P.E.O. discovered the partial skull of a small archosaurian reptile in the lower part of the New Haven The fossil from Cheshire is now housed in the collections of Formation (Norian) of the Hartford basin (Newark Supergroup; the American Museum of Natural History, where it is cata- Fig. -
8. Archosaur Phylogeny and the Relationships of the Crocodylia
8. Archosaur phylogeny and the relationships of the Crocodylia MICHAEL J. BENTON Department of Geology, The Queen's University of Belfast, Belfast, UK JAMES M. CLARK* Department of Anatomy, University of Chicago, Chicago, Illinois, USA Abstract The Archosauria include the living crocodilians and birds, as well as the fossil dinosaurs, pterosaurs, and basal 'thecodontians'. Cladograms of the basal archosaurs and of the crocodylomorphs are given in this paper. There are three primitive archosaur groups, the Proterosuchidae, the Erythrosuchidae, and the Proterochampsidae, which fall outside the crown-group (crocodilian line plus bird line), and these have been defined as plesions to a restricted Archosauria by Gauthier. The Early Triassic Euparkeria may also fall outside this crown-group, or it may lie on the bird line. The crown-group of archosaurs divides into the Ornithosuchia (the 'bird line': Orn- ithosuchidae, Lagosuchidae, Pterosauria, Dinosauria) and the Croco- dylotarsi nov. (the 'crocodilian line': Phytosauridae, Crocodylo- morpha, Stagonolepididae, Rauisuchidae, and Poposauridae). The latter three families may form a clade (Pseudosuchia s.str.), or the Poposauridae may pair off with Crocodylomorpha. The Crocodylomorpha includes all crocodilians, as well as crocodi- lian-like Triassic and Jurassic terrestrial forms. The Crocodyliformes include the traditional 'Protosuchia', 'Mesosuchia', and Eusuchia, and they are defined by a large number of synapomorphies, particularly of the braincase and occipital regions. The 'protosuchians' (mainly Early *Present address: Department of Zoology, Storer Hall, University of California, Davis, Cali- fornia, USA. The Phylogeny and Classification of the Tetrapods, Volume 1: Amphibians, Reptiles, Birds (ed. M.J. Benton), Systematics Association Special Volume 35A . pp. 295-338. Clarendon Press, Oxford, 1988. -
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. -
On the Presence of the Subnarial Foramen in Prestosuchus Chiniquensis (Pseudosuchia: Loricata) with Remarks on Its Phylogenetic Distribution
Anais da Academia Brasileira de Ciências (2016) (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 http://dx.doi.org/10.1590/0001-3765201620150456 www.scielo.br/aabc On the presence of the subnarial foramen in Prestosuchus chiniquensis (Pseudosuchia: Loricata) with remarks on its phylogenetic distribution LÚCIO ROBERTO-DA-SILVA1,2, MARCO A.G. FRANÇA3, SÉRGIO F. CABREIRA3, RODRIGO T. MÜLLER1 and SÉRGIO DIAS-DA-SILVA4 ¹Programa de Pós-Graduação em Biodiversidade Animal, Universidade Federal de Santa Maria, Av. Roraima, 1000, Bairro Camobi, 97105-900 Santa Maria, RS, Brasil ²Laboratório de Paleontologia, Universidade Luterana do Brasil, Av. Farroupilha, 8001, Bairro São José, 92425-900 Canoas, RS, Brasil ³Laboratório de Paleontologia e Evolução de Petrolina, Campus de Ciências Agrárias, Universidade Federal do Vale do São Francisco, Rodovia BR 407, Km12, Lote 543, 56300-000 Petrolina, PE, Brasil 4Centro de Apoio à Pesquisa da Quarta Colônia, Universidade Federal de Santa Maria, Rua Maximiliano Vizzotto, 598, 97230-000 São João do Polêsine, RS, Brasil Manuscript received on July 1, 2015; accepted for publication on April 15, 2016 ABSTRACT Many authors have discussed the subnarial foramen in Archosauriformes. Here presence among Archosauriformes, shape, and position of this structure is reported and its phylogenetic importance is investigated. Based on distribution and the phylogenetic tree, it probably arose independently in Erythrosuchus, Herrerasaurus, and Paracrocodylomorpha. In Paracrocodylomorpha the subnarial foramen is oval-shaped, placed in the middle height of the main body of the maxilla, and does not reach the height of ascending process. In basal loricatans from South America (Prestosuchus chiniquensis and Saurosuchus galilei) the subnarial foramen is ‘drop-like’ shaped, the subnarial foramen is located above the middle height of the main body of the maxilla, reaching the height of ascending process, a condition also present in Herrerasaurus ischigualastensis. -
New Insights on Prestosuchus Chiniquensis Huene
New insights on Prestosuchus chiniquensis Huene, 1942 (Pseudosuchia, Loricata) based on new specimens from the “Tree Sanga” Outcrop, Chiniqua´ Region, Rio Grande do Sul, Brazil Marcel B. Lacerda1, Bianca M. Mastrantonio1, Daniel C. Fortier2 and Cesar L. Schultz1 1 Instituto de Geocieˆncias, Laborato´rio de Paleovertebrados, Universidade Federal do Rio Grande do Sul–UFRGS, Porto Alegre, Rio Grande do Sul, Brazil 2 CHNUFPI, Campus Amı´lcar Ferreira Sobral, Universidade Federal do Piauı´, Floriano, Piauı´, Brazil ABSTRACT The ‘rauisuchians’ are a group of Triassic pseudosuchian archosaurs that displayed a near global distribution. Their problematic taxonomic resolution comes from the fact that most taxa are represented only by a few and/or mostly incomplete specimens. In the last few decades, renewed interest in early archosaur evolution has helped to clarify some of these problems, but further studies on the taxonomic and paleobiological aspects are still needed. In the present work, we describe new material attributed to the ‘rauisuchian’ taxon Prestosuchus chiniquensis, of the Dinodontosaurus Assemblage Zone, Middle Triassic (Ladinian) of the Santa Maria Supersequence of southern Brazil, based on a comparative osteologic analysis. Additionally, we present well supported evidence that these represent juvenile forms, due to differences in osteological features (i.e., a subnarial fenestra) that when compared to previously described specimens can be attributed to ontogeny and indicate variation within a single taxon of a problematic but important -
Heptasuchus Clarki, from the ?Mid-Upper Triassic, Southeastern Big Horn Mountains, Central Wyoming (USA)
The osteology and phylogenetic position of the loricatan (Archosauria: Pseudosuchia) Heptasuchus clarki, from the ?Mid-Upper Triassic, southeastern Big Horn Mountains, Central Wyoming (USA) † Sterling J. Nesbitt1, John M. Zawiskie2,3, Robert M. Dawley4 1 Department of Geosciences, Virginia Tech, Blacksburg, VA, USA 2 Cranbrook Institute of Science, Bloomfield Hills, MI, USA 3 Department of Geology, Wayne State University, Detroit, MI, USA 4 Department of Biology, Ursinus College, Collegeville, PA, USA † Deceased author. ABSTRACT Loricatan pseudosuchians (known as “rauisuchians”) typically consist of poorly understood fragmentary remains known worldwide from the Middle Triassic to the end of the Triassic Period. Renewed interest and the discovery of more complete specimens recently revolutionized our understanding of the relationships of archosaurs, the origin of Crocodylomorpha, and the paleobiology of these animals. However, there are still few loricatans known from the Middle to early portion of the Late Triassic and the forms that occur during this time are largely known from southern Pangea or Europe. Heptasuchus clarki was the first formally recognized North American “rauisuchian” and was collected from a poorly sampled and disparately fossiliferous sequence of Triassic strata in North America. Exposed along the trend of the Casper Arch flanking the southeastern Big Horn Mountains, the type locality of Heptasuchus clarki occurs within a sequence of red beds above the Alcova Limestone and Crow Mountain formations within the Chugwater Group. The age of the type locality is poorly constrained to the Middle—early Late Triassic and is Submitted 17 June 2020 Accepted 14 September 2020 likely similar to or just older than that of the Popo Agie Formation assemblage from Published 27 October 2020 the western portion of Wyoming. -
Macroevolutionary Patterns in the Evolutionary Radiation of Archosaurs (Tetrapoda: Diapsida) Stephen L
Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 101, 367–382, 2011 (for 2010) Macroevolutionary patterns in the evolutionary radiation of archosaurs (Tetrapoda: Diapsida) Stephen L. Brusatte1,2, Michael J. Benton3, Graeme T. Lloyd4, Marcello Ruta3 and Steve C. Wang5 1 Division of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, NY 10024, USA Email: [email protected] 2 Department of Earth and Environmental Sciences, Columbia University, New York, NY, USA 3 School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol, BS8 1RJ, UK 4 Department of Palaeontology, Natural History Museum, Cromwell Road, London SW7 5BD, UK 5 Department of Mathematics and Statistics, Swarthmore College, Swarthmore, PA 19081, USA ABSTRACT: The rise of archosaurs during the Triassic and Early Jurassic has been treated as a classic example of an evolutionary radiation in the fossil record. This paper reviews published studies and provides new data on archosaur lineage origination, diversity and lineage evolution, morpho- logical disparity, rates of morphological character change, and faunal abundance during the Triassic–Early Jurassic. The fundamental archosaur lineages originated early in the Triassic, in concert with the highest rates of character change. Disparity and diversity peaked later, during the Norian, but the most significant increase in disparity occurred before maximum diversity. Archo- saurs were rare components of Early–Middle Triassic faunas, but were more abundant in the Late Triassic and pre-eminent globally by the Early Jurassic. The archosaur radiation was a drawn-out event and major components such as diversity and abundance were discordant from each other. -
Table of Contents
Downloaded from http://sp.lyellcollection.org/ by guest on October 1, 2021 Contents Participants from the First Symposium of Early Archosaur Evolution vii NESBITT, S. J., DESOJO,J.B.&IRMIS, R. B. Anatomy, phylogeny and palaeobiology of early 1 archosaurs and their kin EZCURRA, M. D., BUTLER,R.J.&GOWER, D. J. ‘Proterosuchia’: the origin and early history of 9 Archosauriformes SOOKIAS,R.B.&BUTLER, R. J. Euparkeriidae 35 SUES, H.-D., DESOJO,J.B.&EZCURRA, M. D. Doswelliidae: a clade of unusual armoured 49 archosauriforms from the Middle and Late Triassic TROTTEYN, M. J., ARCUCCI,A.B.&RAUGUST, T. Proterochampsia: an endemic archosauriform 59 clade from South America STOCKER,M.R.&BUTLER, R. J. Phytosauria 91 DALLA VECCHIA, F. M. Triassic pterosaurs 119 LANGER, M. C., NESBITT, S. J., BITTENCOURT,J.S.&IRMIS, R. B. Non-dinosaurian 157 Dinosauromorpha VON BACZKO,M.B.&EZCURRA, M. D. Ornithosuchidae: a group of Triassic archosaurs with a 187 unique ankle joint DESOJO, J. B., HECKERT, A. B., MARTZ, J. W., PARKER, W. G., SCHOCH, R. R., 203 SMALL,B.J.&SULEJ, T. Aetosauria: a clade of armoured pseudosuchians from the Upper Triassic continental beds NESBITT, S. J., BRUSATTE, S. L., DESOJO, J. B., LIPARINI, A., DE FRANc¸a, M. A. G., 241 WEINBAUM,J.C.&GOWER, D. J. Rauisuchia IRMIS, R. B., NESBITT,S.J.&SUES, H.-D. Early Crocodylomorpha 275 RAUGUST, T., LACERDA,M.&SCHULTZ, C. L. The first occurrence of Chanaresuchus bonapartei 303 Romer 1971 (Archosauriformes, Proterochampsia) of the Middle Triassic of Brazil from the Santacruzodon Assemblage Zone, Santa Maria Formation (Parana´ Basin) NIEDZ´ WIEDZKI, G., BRUSATTE,S.L.&BUTLER,R.J.Prorotodactylus and Rotodactylus tracks: an 319 ichnological record of dinosauromorphs from the Early–Middle Triassic of Poland LANGER,M.C.&FERIGOLO, J. -
(Diapsida, Archosauriformes) from the Late Triassic of the Iberian Peninsula
Journal of Vertebrate Paleontology ISSN: 0272-4634 (Print) 1937-2809 (Online) Journal homepage: https://www.tandfonline.com/loi/ujvp20 The first phytosaur (Diapsida, Archosauriformes) from the Late Triassic of the Iberian Peninsula Octávio Mateus, Richard J. Butler, Stephen L. Brusatte, Jessica H. Whiteside & J. Sébastien Steyer To cite this article: Octávio Mateus, Richard J. Butler, Stephen L. Brusatte, Jessica H. Whiteside & J. Sébastien Steyer (2014) The first phytosaur (Diapsida, Archosauriformes) from the Late Triassic of the Iberian Peninsula, Journal of Vertebrate Paleontology, 34:4, 970-975, DOI: 10.1080/02724634.2014.840310 To link to this article: https://doi.org/10.1080/02724634.2014.840310 Published online: 08 Jul 2014. Submit your article to this journal Article views: 229 View related articles View Crossmark data Citing articles: 7 View citing articles Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=ujvp20 Journal of Vertebrate Paleontology 34(4):970–975, July 2014 © 2014 by the Society of Vertebrate Paleontology SHORT COMMUNICATION THE FIRST PHYTOSAUR (DIAPSIDA, ARCHOSAURIFORMES) FROM THE LATE TRIASSIC OF THE IBERIAN PENINSULA OCTAVIO´ MATEUS,*,1,2 RICHARD J. BUTLER,3,4 STEPHEN L. BRUSATTE,5 JESSICA H. WHITESIDE,6 and J. SEBASTIEN´ STEYER7; 1GeoBioTec, DCT, Faculdade de Cienciasˆ e Tecnologia, Universidade Nova de Lisboa, 2829-516 Caparica, Portugal, [email protected]; 2Museu da Lourinha,˜ 2530-157 Lourinha,˜ Portugal; 3GeoBio-Center, Ludwig-Maximilians-Universitat¨ -
Proceedings of the United States National Museum
A NEW LABYRINTHODONT FROM THE I^NSAS COAL ]\IEASURES. By Roy L. Moodie, Of the University of Kansas. The remains of labyriuthodoiits in the coal measures of North America are very scanty. The specimens described from this horizon can be counted ahnost on the fingers of one hand. The earliest discovery of labyrinthodont-hke remains was made by Dawson, in 1850, in the coal measures of Nova Scotia. He secured from the coal mines near Albion an incomplete skull, wliich he sent to London, where it was described in 1854 by Sir Richard Owen as Baphetes planiceps. Its relations with the typical labyrinthodonts are somewhat uncertain, but it is more closely related to that group than to any other, so far as we may judge from the material presei-ved. Hay^ places this form in his new suborder, Apoecospondyli and in the family Dendrepetontidae. Hay includes also in this new sub- order the Sauropleuridse, Archegosauridse, Cricotidse, Anthracosau- ridje, Eryopidse, and Mastodonsauridse, which is a very heterogeneous assemblage. Baphetes and Dendrerpeton may possibly belong in the same family, but they are still too imperfectly known to be sure of their relations. The Sauropleuridag are typical microsaurians. Two ordere and three suborders are represented by the other families included by Hay in his Apoecospondyli. The discovery of Baphetes was followed in 1863 by the finding of typical labyrinthodont vertebrae in the coal measures of Nova Scotia, unless it be that the species of Dendrerpeton prove to be labyrintho- dont, in which case their discovery would precede that just mentioned. The two vertebrae were described and named by Prof. -
A Short-Snouted, Middle Triassic Phytosaur and Its Implications For
www.nature.com/scientificreports OPEN A Short-Snouted, Middle Triassic Phytosaur and its Implications for the Morphological Evolution and Received: 28 September 2016 Accepted: 08 March 2017 Biogeography of Phytosauria Published: 10 April 2017 Michelle R. Stocker1, Li-Jun Zhao2, Sterling J. Nesbitt1, Xiao-Chun Wu3 & Chun Li4 Following the end-Permian extinction, terrestrial vertebrate diversity recovered by the Middle Triassic, and that diversity was now dominated by reptiles. However, those reptilian clades, including archosaurs and their closest relatives, are not commonly found until ~30 million years post-extinction in Late Triassic deposits despite time-calibrated phylogenetic analyses predicting an Early Triassic divergence for those clades. One of these groups from the Late Triassic, Phytosauria, is well known from a near-Pangean distribution, and this easily recognized clade bears an elongated rostrum with posteriorly retracted nares and numerous postcranial synapomorphies that are unique compared with all other contemporary reptiles. Here, we recognize the exquisitely preserved, nearly complete skeleton of Diandongosuchus fuyuanensis from the Middle Triassic of China as the oldest and basalmost phytosaur. The Middle Triassic age and lack of the characteristically-elongated rostrum fill a critical morphological and temporal gap in phytosaur evolution, indicating that the characteristic elongated rostrum of phytosaurs appeared subsequent to cranial and postcranial modifications associated with enhanced prey capture, predating that general trend of morphological evolution observed within Crocodyliformes. Additionally, Diandongosuchus supports that the clade was present across Pangea, suggesting early ecosystem exploration for Archosauriformes through nearshore environments and leading to ease of dispersal across the Tethys. The Permian-Triassic mass extinction resulted in a colossal change in global vertebrate community structure1,2. -
Diversificação De Archosauromorpha Após a Extinção Permo-Triássica Survivors: Diversification of Archosauromorpha After Permo-Triassic Extinction
Terræ REVISÃO 10.20396/td.v16i0.8656060 Didatica Sobreviventes: Diversificação de Archosauromorpha após a Extinção Permo-Triássica SURVIVORS: DIVERSIFICATION OF ARCHOSAUROMORPHA AFTER PERMO-TRIASSIC EXTINCTION TIANE MACEDO DE-OLIVEIRA¹, FELIPE LIMA PINHEIRO², LEONARDO KERBER³ 1 - PROGR. PÓS-GRAD. BIODIVERSIDADE ANIMAL, UNIVERSIDADE FEDERAL DE SANTA MARIA (UFSM). SANTA MARIA, RS, BRASIL. 2 - LABORATÓRIO DE PALEOBIOLOGIA, UNIPAMPA, SÃO GABRIEL, RS, BRASIL. 3 - CENTRO DE APOIO À PESQUISA PALEONTOLÓGICA DA QUARTA COLÔNIA (CAPPA-UFSM), SÃO JOÃO DO POLÊSINE, RS, BRASIL. E-MAIL: [email protected], [email protected], [email protected] Abstract: The Archosauromorpha is defined as the clade that comprises all diapsids more closely related Citation/Citação: De-Oliveira, T. M., to the lineage of birds (Ornithodira or Avemetatarsalia) and crocodylians (Pseudosuchia or Crurotarsi) than Pinheiro, F. L., & Kerber, L. (2020). to Lepidosauria. In addition to their ‘basal’ taxa (e.g., Tanystropheidae, Rhynchosauria, and Allokotosau- Sobreviventes: Diversificação de Ar- ria), Archosauromorpha includes the clade Archosauriformes, which, by its turn, includes Archosauria. chosauromorpha após a Extinção During the Triassic, the archosauromorphs became the main group of diapsids to diversify in body size Permo-Triássica. Terræ Didatica, and morphological disparity. The Permo-Triassic mass extinction occurred 252 million years ago and 16, 1-23, e020009. doi: 10.20396/ produced a dramatic change in the composition of the floral and faunal communities at the beginning td.v16i0.8656060 of the Triassic period. The diversification of Archosauromorpha during the Triassic has been the focus of several recent studies, as this clade is a classic example of adaptive radiation. This paper synthesizes Keywords: Diapsida.