The Early Evolution of Rhynchosaurs Butler, Richard; Montefeltro, Felipe; Ezcurra, Martin

Total Page:16

File Type:pdf, Size:1020Kb

The Early Evolution of Rhynchosaurs Butler, Richard; Montefeltro, Felipe; Ezcurra, Martin University of Birmingham The early evolution of Rhynchosaurs Butler, Richard; Montefeltro, Felipe; Ezcurra, Martin DOI: 10.3389/fevo.2015.00142 License: Creative Commons: Attribution (CC BY) Document Version Publisher's PDF, also known as Version of record Citation for published version (Harvard): Butler, R, Montefeltro, F & Ezcurra, M 2016, 'The early evolution of Rhynchosaurs', Frontiers in Ecology and Evolution. https://doi.org/10.3389/fevo.2015.00142 Link to publication on Research at Birmingham portal Publisher Rights Statement: Frontiers is fully compliant with open access mandates, by publishing its articles under the Creative Commons Attribution licence (CC-BY). Funder mandates such as those by the Wellcome Trust (UK), National Institutes of Health (USA) and the Australian Research Council (Australia) are fully compatible with publishing in Frontiers. Authors retain copyright of their work and can deposit their publication in any repository. The work can be freely shared and adapted provided that appropriate credit is given and any changes specified. 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. When citing, please reference the published version. Take down policy While the University of Birmingham exercises care and attention in making items available there are rare occasions when an item has been uploaded in error or has been deemed to be commercially or otherwise sensitive. If you believe that this is the case for this document, please contact [email protected] providing details and we will remove access to the work immediately and investigate. Download date: 04. Oct. 2021 ORIGINAL RESEARCH published: 11 January 2016 doi: 10.3389/fevo.2015.00142 The Early Evolution of Rhynchosaurs Martín D. Ezcurra 1, 2*, Felipe Montefeltro 2, 3 and Richard J. Butler 2 1 Sección Paleontología de Vertebrados, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia,” Buenos Aires, Argentina, 2 School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, UK, 3 Departamento de Biologia e Zootecnia, FEIS, Universidade Estadual Paulista, Ilha Solteira, Brazil The rhynchosaurian archosauromorphs are an important and diverse group of fossil tetrapods that first appeared during the Early Triassic and probably became extinct during the early Late Triassic (early Norian). Here, the early evolution of rhynchosaurs during the Early and early Middle Triassic (Induan-Anisian: 252.2-242 Mya) is reviewed based on new anatomical observations and their implications for the taxonomy, phylogenetic relationships and macroevolutionary history of the group. A quantitative phylogenetic analysis recovered a paraphyletic genus Rhynchosaurus, with “Rhynchosaurus” brodiei more closely related to hyperodapedontines than to Rhynchosaurus articeps. Therefore, a new genus is erected, resulting in the new combination Langeronyx brodiei. A body size analysis found two independent increases in size in the evolutionary history of rhynchosaurs, one among stenaulorhynchines and the other in the hyperodapedontine lineage. Maximum likelihood fitting of phenotypic evolution models to body size data Edited by: Michel Laurin, found ambiguous results, with body size evolution potentially interpreted as fitting either Muséum National d’Histoire Naturelle, a non-directional Brownian motion model or a stasis model. A Dispersal-Extinction- France Cladogenesis analysis reconstructed the areas that are now South Africa and Europe Reviewed by: Sean P. Modesto, as the ancestral areas of Rhynchosauria and Rhynchosauridae, respectively. The Cape Breton University, Canada reconstruction of dispersal events between geographic areas that are broadly separated Fernando Abdala, paleolatitudinally implies that barriers to the dispersal of rhynchosaurs from either side of University of the Witwatersrand, Johannesburg, South Africa the paleo-Equator during the Middle Triassic were either absent or permeable. Juan Carlos Cisneros, Universidade Federal do Piauí, Brazil Keywords: Permo-Triassic, Diapsida, Archosauromorpha, body size, phylogeny, paleobiogeography *Correspondence: Martín D. Ezcurra [email protected] INTRODUCTION ∼ Specialty section: The Permo-Triassic mass extinction occurred 252 million years ago, and produced a dramatic This article was submitted to change in the composition of floral and faunal communities (Raup and Sepkoski, 1982; Erwin, Paleontology, 1994; Looy et al., 2001; Benton and Twitchett, 2003; Fröbisch, 2013; Benton and Newell, 2014; a section of the journal Smith and Botha-Brink, 2014). In the case of vertebrates, numerous new lineages first appeared or Frontiers in Ecology and Evolution Received: 20 August 2015 Institutional Abbreviations: AM, Albany Museum, Grahamstown, South Africa; BRSUG, University of Bristol, School of Accepted: 30 November 2015 Earth Sciences, Bristol, UK; EXEMS, Royal Albert Memorial Museum, Exeter, UK; FZB, Fundação Zoobotânica do Rio Published: 11 January 2016 Grande do Sul, Porto Alegre, Brazil; GPIT, Paläontologische Sammlung der Universität Tübingen, Tübingen, Germany; ISI, Indian Statistical Institute, Kolkata, India; MACN-Pv, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia,” Citation: Paleontología de Vertebrados, Buenos Aires, Argentina; NHMUK PV, Natural History Museum, Palaeontology Vertebrates, Ezcurra MD, Montefeltro F and London, UK; PIMUZ, Paläontologisches Institut und Museum der Universität Zürich, Zurich, Switzerland; PVSJ, Museo Butler RJ (2016) The Early Evolution of de Ciencias Naturales, Universidad de San Juan, San Juan, Argentina; SAM-PK, Iziko South African Museum, Cape Rhynchosaurs. Town, South Africa; SIDMM, Sidmouth Museum, Sidmouth, UK; SHYMS, Shropshire Museums, Ludlow, UK; UFRGS, Front. Ecol. Evol. 3:142. Instituto de Geociências, Universidade Federal do Rio Grande do Sul, Porto Alegre, Brazil; WARMS, Warwickshire Museum, doi: 10.3389/fevo.2015.00142 Warwick, UK. Frontiers in Ecology and Evolution | www.frontiersin.org 1 January 2016 | Volume 3 | Article 142 Ezcurra et al. Early Rhynchosaurs diversified in the aftermath of this extinction. Many of these Fodonyx spenceri based on new, first-hand observations of lineages replaced clades that flourished during the Paleozoic but specimens. We added three characters from previously published vanished or were decimated at the end-Permian mass extinction phylogenetic analyses relevant to the basal relationships of event (e.g., pareiasaurs, non-mammalian synapsids, such as Rhynchosauria (Dilkes, 1998; Ezcurra et al., 2014, 2015) and gorgonopsians and anomodonts). Among the new Triassic we modified the formulation of two characters from the clades are the first representatives of several modern vertebrate original character list of Butler et al. (2015: characters 63 groups, including teleosts, lissamphibians, eucynodonts, stem- and 84; see Supplementary Material). We also expanded the testudinatans, lepidosauromorphs, crocodylomorphs, and stem- taxonomic sampling of the analysis by adding the oldest known avialans, including the first non-avian dinosaurs (Bonaparte, rhynchosaur, Noteosuchus colletti (Watson, 1912; Carroll, 1976; 1982; Benton, 1983a; Colbert, 1984; Gaffney, 1986; Arratia, 2001; Dilkes, 1998; Ezcurra et al., 2014). Scoring of taxa was based Bonaparte et al., 2003; Evans, 2003; Marjanovic and Laurin, 2008; primarily on first-hand examination of specimens, with the Nesbitt, 2011; Jones et al., 2013; Ezcurra et al., 2014; Schoch and exception of Isalorhynchus genovefae, which was scored using Sues, 2015). Langer et al. (2000a) and Whatley (2005). The Triassic also witnessed the evolution of numerous The final matrix (15 taxa and 96 characters) was analyzed amniote groups that occur only within this time interval using TNT version 1.1 (Goloboff et al., 2008) using the implicit and which became extinct at or before the end-Triassic enumeration algorithm. Multistate characters 63, 70, 73, and mass extinction event (e.g., traversodontids, doswelliids, 75 were treated as additive because they represent nested tanystropheids, aetosaurs, phytosaurs; Abdala and Ribeiro, 2010; sets of homologies. Zero branch length nodes were collapsed Liu and Olsen, 2010; Desojo et al., 2013; Stocker and Butler, following the search (Coddington and Scharff, 1994). Absolute 2013; Sues et al., 2013; Pritchard et al., 2015). Although restricted and GC bootstrap frequencies were calculated after 10,000 to the Triassic, these groups achieved high morphological pseudoreplicates. GC bootstrap frequencies are the difference diversity and taxonomic richness, and some of them become key between the frequencies with which the original group and ecological components of their communities
Recommended publications
  • A Building Stone Atlas of Warwickshire
    Strategic Stone Study A Building Stone Atlas of Warwickshire First published by English Heritage May 2011 Rebranded by Historic England December 2017 Introduction The landscape in the county is clearly dictated by the Cob was suitable for small houses but when more space was underlying geology which has also had a major influence on needed it became necessary to build a wooden frame and use the choice of building stones available for use in the past. The wattle fencing daubed with mud as the infilling or ‘nogging’ to geological map shows that much of this generally low-lying make the walls. In nearly all surviving examples the wooden county is underlain by the red mudstones of the Triassic Mercia frame was built on a low plinth wall of whatever stone was Mudstone Group. This surface cover is however, broken in the available locally. In many cases this is the only indication we Nuneaton-Coventry-Warwick area by a narrow strip of ancient have of the early use of local stones. Adding the stone wall rocks forming the Nuneaton inlier (Precambrian to early served to protect the wooden structure from rising damp. The Devonian) and the wider exposure of the unconformably infilling material has often been replaced later with more overlying beds of the Warwickshire Coalfield (Upper durable brickwork or stone. Sometimes, as fashion or necessity Carboniferous to early Permian). In the south and east of the dictated, the original timber framed walls were encased in county a series of low-lying ridges are developed marking the stone or brick cladding, especially at the front of the building outcrops of the Lower and Middle Jurassic limestone/ where it was presumably a feature to be admired.
    [Show full text]
  • The Origin and Early Evolution of Dinosaurs
    Biol. Rev. (2010), 85, pp. 55–110. 55 doi:10.1111/j.1469-185X.2009.00094.x The origin and early evolution of dinosaurs Max C. Langer1∗,MartinD.Ezcurra2, Jonathas S. Bittencourt1 and Fernando E. Novas2,3 1Departamento de Biologia, FFCLRP, Universidade de S˜ao Paulo; Av. Bandeirantes 3900, Ribeir˜ao Preto-SP, Brazil 2Laboratorio de Anatomia Comparada y Evoluci´on de los Vertebrados, Museo Argentino de Ciencias Naturales ‘‘Bernardino Rivadavia’’, Avda. Angel Gallardo 470, Cdad. de Buenos Aires, Argentina 3CONICET (Consejo Nacional de Investigaciones Cient´ıficas y T´ecnicas); Avda. Rivadavia 1917 - Cdad. de Buenos Aires, Argentina (Received 28 November 2008; revised 09 July 2009; accepted 14 July 2009) ABSTRACT The oldest unequivocal records of Dinosauria were unearthed from Late Triassic rocks (approximately 230 Ma) accumulated over extensional rift basins in southwestern Pangea. The better known of these are Herrerasaurus ischigualastensis, Pisanosaurus mertii, Eoraptor lunensis,andPanphagia protos from the Ischigualasto Formation, Argentina, and Staurikosaurus pricei and Saturnalia tupiniquim from the Santa Maria Formation, Brazil. No uncontroversial dinosaur body fossils are known from older strata, but the Middle Triassic origin of the lineage may be inferred from both the footprint record and its sister-group relation to Ladinian basal dinosauromorphs. These include the typical Marasuchus lilloensis, more basal forms such as Lagerpeton and Dromomeron, as well as silesaurids: a possibly monophyletic group composed of Mid-Late Triassic forms that may represent immediate sister taxa to dinosaurs. The first phylogenetic definition to fit the current understanding of Dinosauria as a node-based taxon solely composed of mutually exclusive Saurischia and Ornithischia was given as ‘‘all descendants of the most recent common ancestor of birds and Triceratops’’.
    [Show full text]
  • The Early Evolution of Rhynchosaurs Butler, Richard; Montefeltro, Felipe; Ezcurra, Martin
    University of Birmingham The early evolution of Rhynchosaurs Butler, Richard; Montefeltro, Felipe; Ezcurra, Martin DOI: 10.3389/fevo.2015.00142 License: Creative Commons: Attribution (CC BY) Document Version Publisher's PDF, also known as Version of record Citation for published version (Harvard): Butler, R, Montefeltro, F & Ezcurra, M 2016, 'The early evolution of Rhynchosaurs', Frontiers in Ecology and Evolution. https://doi.org/10.3389/fevo.2015.00142 Link to publication on Research at Birmingham portal Publisher Rights Statement: Frontiers is fully compliant with open access mandates, by publishing its articles under the Creative Commons Attribution licence (CC-BY). Funder mandates such as those by the Wellcome Trust (UK), National Institutes of Health (USA) and the Australian Research Council (Australia) are fully compatible with publishing in Frontiers. Authors retain copyright of their work and can deposit their publication in any repository. The work can be freely shared and adapted provided that appropriate credit is given and any changes specified. 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.
    [Show full text]
  • 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.
    [Show full text]
  • Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships
    438 Article 438 by Saswati Bandyopadhyay1* and Sanghamitra Ray2 Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships 1Geological Studies Unit, Indian Statistical Institute, 203 B. T. Road, Kolkata 700108, India; email: [email protected] 2Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur 721302, India; email: [email protected] *Corresponding author (Received : 23/12/2018; Revised accepted : 11/09/2019) https://doi.org/10.18814/epiiugs/2020/020028 The twelve Gondwanan stratigraphic horizons of many extant lineages, producing highly diverse terrestrial vertebrates India have yielded varied vertebrate fossils. The oldest in the vacant niches created throughout the world due to the end- Permian extinction event. Diapsids diversified rapidly by the Middle fossil record is the Endothiodon-dominated multitaxic Triassic in to many communities of continental tetrapods, whereas Kundaram fauna, which correlates the Kundaram the non-mammalian synapsids became a minor components for the Formation with several other coeval Late Permian remainder of the Mesozoic Era. The Gondwana basins of peninsular horizons of South Africa, Zambia, Tanzania, India (Fig. 1A) aptly exemplify the diverse vertebrate faunas found Mozambique, Malawi, Madagascar and Brazil. The from the Late Palaeozoic and Mesozoic. During the last few decades much emphasis was given on explorations and excavations of Permian-Triassic transition in India is marked by vertebrate fossils in these basins which have yielded many new fossil distinct taxonomic shift and faunal characteristics and vertebrates, significant both in numbers and diversity of genera, and represented by small-sized holdover fauna of the providing information on their taphonomy, taxonomy, phylogeny, Early Triassic Panchet and Kamthi fauna.
    [Show full text]
  • A Taxonomic Note Concerning a Dicynodont (Synapsida: Anomodontia) from the Middle Triassic of East Africa
    Short Communication A taxonomic note concerning a dicynodont (Synapsida: Anomodontia) from the Middle Triassic of East Africa A.J. Renaut1*, R.J. Damiani1, A.M. Yates1 & P.J. Hancox2 1Bernard Price Institute for Palaeontological Research, School of Geosciences, University of the Witwatersrand, Private Bag 3, WITS, 2050 South Africa 2School of Geosciences, University of the Witwatersrand, Private Bag 3, WITS, 2050 South Africa Received 26 May 2003. Accepted 20 November 2003 The complicated histories of the Indian dicynodont Rechnisaurus and the East African dicynodont Kannemeyeria cristarhynchus has led to the incorrect use of the name ‘cristarhynchus’ for the latter taxon. This paper therefore proposes a new species name and diagnosis. Keywords: Triassic, therapsid, Kannemeyeria. INTRODUCTION previously been referred to Kannemeyeria simocephalus by Dicynodonts were a diverse clade of herbivorous, non- Keyser (1973). Keyser & Cruickshank (1979) recognized mammalian therapsids (‘mammal-like reptiles’), which that BP/1/3638 and R313 were in fact congeneric with flourished during the Permian and Triassic periods. Kannemeyeria, but a different species from Kannemeyeria Dicynodont fossils have been recorded from every simocephalus. Consequently, Keyser & Cruickshank (1979), continent and an enormous number of genera and species accepting that BP/1/3638 was conspecific with the Indian have been named, many of which are ill-diagnosed or Rechnisaurus cristarhynchus Roy-Chowdhury, argued that based on poorly preserved material (King 1988). Not Rechnisaurus was a junior synonym of Kannemeyeria. This surprisingly, the taxonomy and phylogenetic inter- recognized the new combination Kannemeyeria crista- relationships of dicynodonts remains contentious (e.g. rhynchus (Roy-Chowdhury) for the Indian and Zambian Angielczyk 2001; Hancox et al.
    [Show full text]
  • 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.
    [Show full text]
  • The Role of Fossils in Interpreting the Development of the Karoo Basin
    Palaeon!. afr., 33,41-54 (1997) THE ROLE OF FOSSILS IN INTERPRETING THE DEVELOPMENT OF THE KAROO BASIN by P. J. Hancox· & B. S. Rubidge2 IGeology Department, University of the Witwatersrand, Private Bag 3, Wits 2050, South Africa 2Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, Private Bag 3, Wits 2050, South Africa ABSTRACT The Permo-Carboniferous to Jurassic aged rocks oft1:J.e main Karoo Basin ofSouth Africa are world renowned for the wealth of synapsid reptile and early dinosaur fossils, which have allowed a ten-fold biostratigraphic subdivision ofthe Karoo Supergroup to be erected. The role offossils in interpreting the development of the Karoo Basin is not, however, restricted to biostratigraphic studies. Recent integrated sedimentological and palaeontological studies have helped in more precisely defming a number of problematical formational contacts within the Karoo Supergroup, as well as enhancing palaeoenvironmental reconstructions, and basin development models. KEYWORDS: Karoo Basin, Biostratigraphy, Palaeoenvironment, Basin Development. INTRODUCTION Invertebrate remains are important as indicators of The main Karoo Basin of South Africa preserves a facies genesis, including water temperature and salinity, retro-arc foreland basin fill (Cole 1992) deposited in as age indicators, and for their biostratigraphic potential. front of the actively rising Cape Fold Belt (CFB) in Fossil fish are relatively rare in the Karoo Supergroup, southwestern Gondwana. It is the deepest and but where present are useful indicators of gross stratigraphically most complete of several depositories palaeoenvironments (e.g. Keyser 1966) and also have of Permo-Carboniferous to Jurassic age in southern biostratigraphic potential (Jubb 1973; Bender et al. Africa and reflects changing depositional environments 1991).
    [Show full text]
  • A Beaked Herbivorous Archosaur with Dinosaur Affinities from the Early Late Triassic of Poland
    Journal of Vertebrate Paleontology 23(3):556±574, September 2003 q 2003 by the Society of Vertebrate Paleontology A BEAKED HERBIVOROUS ARCHOSAUR WITH DINOSAUR AFFINITIES FROM THE EARLY LATE TRIASSIC OF POLAND JERZY DZIK Instytut Paleobiologii PAN, Twarda 51/55, 00-818 Warszawa, Poland, [email protected] ABSTRACTÐAn accumulation of skeletons of the pre-dinosaur Silesaurus opolensis, gen. et sp. nov. is described from the Keuper (Late Triassic) claystone of KrasiejoÂw in southern Poland. The strata are correlated with the late Carnian Lehrberg Beds and contain a diverse assemblage of tetrapods, including the phytosaur Paleorhinus, which in other regions of the world co-occurs with the oldest dinosaurs. A narrow pelvis with long pubes and the extensive development of laminae in the cervical vertebrae place S. opolensis close to the origin of the clade Dinosauria above Pseudolagosuchus, which agrees with its geological age. Among the advanced characters is the beak on the dentaries, and the relatively low tooth count. The teeth have low crowns and wear facets, which are suggestive of herbivory. The elongate, but weak, front limbs are probably a derived feature. INTRODUCTION oped nutrient foramina in its maxilla. It is closely related to Azendohsaurus from the Argana Formation of Morocco (Gauf- As is usual in paleontology, with an increase in knowledge fre, 1993). The Argana Formation also has Paleorhinus, along of the fossil record of early archosaurian reptiles, more and with other phytosaurs more advanced than those from Krasie- more lineages emerge or extend their ranges back in time. It is joÂw (see Dutuit, 1977), and it is likely to be somewhat younger.
    [Show full text]
  • Elachistosuchus Huenei Janensch, 1949 (Reptilia: Diapsida) from the Upper Triassic of Germany and Its Relevance for the Origin of Sauria
    RESEARCH ARTICLE Anatomy of the Enigmatic Reptile Elachistosuchus huenei Janensch, 1949 (Reptilia: Diapsida) from the Upper Triassic of Germany and Its Relevance for the Origin of Sauria Gabriela Sobral1☯*, Hans-Dieter Sues2☯, Johannes Müller1☯ 1 Museum für Naturkunde Berlin, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Berlin, Germany, 2 Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, MRC 121, Washington, DC, United States of America ☯ These authors contributed equally to this work. * [email protected] OPEN ACCESS Citation: Sobral G, Sues H-D, Müller J (2015) Abstract Anatomy of the Enigmatic Reptile Elachistosuchus huenei Janensch, 1949 (Reptilia: Diapsida) from the The holotype and only known specimen of the enigmatic small reptile Elachistosuchus hue- Upper Triassic of Germany and Its Relevance for the nei Janensch, 1949 from the Upper Triassic (Norian) Arnstadt Formation of Saxony-Anhalt Origin of Sauria. PLoS ONE 10(9): e0135114. μ doi:10.1371/journal.pone.0135114 (Germany) is redescribed using CT scans of the material. This re-examination revealed new information on the morphology of this taxon, including previously unknown parts of the Editor: Shree Ram Singh, National Cancer Institute, UNITED STATES skeleton such as the palate, braincase, and shoulder girdle. Elachistosuchus is diagnosed especially by the presence of the posterolateral process of the frontal, the extension of the Received: January 27, 2015 maxillary tooth row to the posterior margin of the orbit, the free posterior process of the Accepted: July 19, 2015 jugal, and the notched anterior margin of the interclavicle. Phylogenetic analyses using two Published: September 9, 2015 recently published character-taxon matrices recovered conflicting results for the phyloge- Copyright: This is an open access article, free of all netic position of Elachistosuchus–either as an archosauromorph, as a lepidosauromorph or copyright, and may be freely reproduced, distributed, as a more basal, non-saurian diapsid.
    [Show full text]
  • Reptile Family Tree - Peters 2017 1112 Taxa, 231 Characters
    Reptile Family Tree - Peters 2017 1112 taxa, 231 characters Note: This tree does not support DNA topologies over 100 Eldeceeon 1990.7.1 67 Eldeceeon holotype long phylogenetic distances. 100 91 Romeriscus Diplovertebron Certain dental traits are convergent and do not define clades. 85 67 Solenodonsaurus 100 Chroniosaurus 94 Chroniosaurus PIN3585/124 Chroniosuchus 58 94 Westlothiana Casineria 84 Brouffia 93 77 Coelostegus Cheirolepis Paleothyris Eusthenopteron 91 Hylonomus Gogonasus 78 66 Anthracodromeus 99 Osteolepis 91 Protorothyris MCZ1532 85 Protorothyris CM 8617 81 Pholidogaster Protorothyris MCZ 2149 97 Colosteus 87 80 Vaughnictis Elliotsmithia Apsisaurus Panderichthys 51 Tiktaalik 86 Aerosaurus Varanops Greererpeton 67 90 94 Varanodon 76 97 Koilops <50 Spathicephalus Varanosaurus FMNH PR 1760 Trimerorhachis 62 84 Varanosaurus BSPHM 1901 XV20 Archaeothyris 91 Dvinosaurus 89 Ophiacodon 91 Acroplous 67 <50 82 99 Batrachosuchus Haptodus 93 Gerrothorax 97 82 Secodontosaurus Neldasaurus 85 76 100 Dimetrodon 84 95 Trematosaurus 97 Sphenacodon 78 Metoposaurus Ianthodon 55 Rhineceps 85 Edaphosaurus 85 96 99 Parotosuchus 80 82 Ianthasaurus 91 Wantzosaurus Glaucosaurus Trematosaurus long rostrum Cutleria 99 Pederpes Stenocybus 95 Whatcheeria 62 94 Ossinodus IVPP V18117 Crassigyrinus 87 62 71 Kenyasaurus 100 Acanthostega 94 52 Deltaherpeton 82 Galechirus 90 MGUH-VP-8160 63 Ventastega 52 Suminia 100 Baphetes Venjukovia 65 97 83 Ichthyostega Megalocephalus Eodicynodon 80 94 60 Proterogyrinus 99 Sclerocephalus smns90055 100 Dicynodon 74 Eoherpeton
    [Show full text]
  • An Unusual Archosauromorph Archosauriform Tooth Increases
    An unusual archosauromorph archosauriform tooth increases known tetrapod diversity in the lower portion of the Chinle Formation (Late Triassic) of southeastern Utah, USA Lopez, Andres; St. Aude, Isabella; Alderete, David; Alvarez, David; Aultman, Hannah; Busch, Dominique; Bustamante, Rogelio; Cirks, Leah; Lopez, Martin; Moncada, Adriana; Ortega, Elizabeth; Verdugo, Carlos; Gay, Robert J *. Mission Heights Preparatory High School, 1376 E. Cottonwood Ln., Casa Grande, Arizona 85122 *[email protected] 520-836-9383 Abstract: An unusual tetrapod tooth was discovered in the Late Upper Triassic Chinle Formation of southeastern Utah. The tooth was originally thought hypothesized to belong pertain to Revueltosaurus, but further investigations have rejected that hypothesis. In this paper, we Comment [Anon1]: This is unnecessary unless it was published somewhere else? compare MNA V10668 to other known fossil teeth tooth crowns found infrom the Chinle Formation and identify assign the tooth to the least inclusive clade it may belongs tocurrently available, Archosauriformes, based on the presence of mesial and distal serrations, a distal keel, and a conical mesiodistal profile. Using data found in other publications and pictures of other teeth, we compare this specimen to other Triassic dental taxa. MNA V10668 shares some similarities with Crosbysaurus, Tecovasaurus, and several other named taxa, including a teardrop-shaped labiolingual profile, but possesses a unique combination of characteristics not found in other diapsid archosauromorph teeth. We conclude that it is most likely an archosauromorph and probably an archosauriform. This increases the known diversity of tetrapods archosauromorphs from the Chinle Formation and represents the first tooth of this morphotype completely unique toto be found from Utah in the Late Triassic Period.
    [Show full text]