Osteology, Variability, and Evolution of Metoposaurus, a Temnospondyl from the Late Triassic of Poland
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Amphibians 1) Transition to Land A) Life on Terrestrial Earth Is a Major
Amphibians 1) Transition to land a) Life on terrestrial earth is a major theme for all non-fish vertebrates also known as Tetrapoda b) Of Tetrapoda there are two major groups Amphibians and amniotes c) The movement form water to land is one of the most complicated and dramatic events of the evolution of animals i) Land is physically hazardous for an animal that evolved in water, is made mostly of water, and all cellular activities occur in water. ii) Plants, snails, and many arthropods made the transition before vertebrates, which provided a plentiful food source. iii) With the transition to land, vertebrates had to adapt every organ system. d) Oxygen on land i) Atmospheric air contains 20 times more oxygen than water and diffuses more rapidly through air than water. ii) By the Devonian period (400+ million years ago) fish had diversified greatly. Some of these adaptations became useful for a terrestrial life (1) Fish had evolved an air sack within their body called a swim bladder. This would allow a space for gas exchange between an organism and air (a) These early fishes were most likely freshwater. Freshwater systems are more likely to evaporate or deoxygenate compares to salt water habitats. So having a vascularized swim bladder or lung would be beneficial. (b) To this day scientist still debate heavily on whether the swim bladder evolved for buoyancy control or lung first. (2) Fish also had evolved external nares for chemoreception. In a terrestrial environment these nares can be used to draw in air to the swim bladder/lung (3) Both of these structures show great examples of evolution utilizing existing structures to turn into something new and more adapted e) However both of the characteristics are shared among fishes and tetrapods, the big shift came in the bone structure of the limbs. -
New Permian Fauna from Tropical Gondwana
ARTICLE Received 18 Jun 2015 | Accepted 18 Sep 2015 | Published 5 Nov 2015 DOI: 10.1038/ncomms9676 OPEN New Permian fauna from tropical Gondwana Juan C. Cisneros1,2, Claudia Marsicano3, Kenneth D. Angielczyk4, Roger M. H. Smith5,6, Martha Richter7, Jo¨rg Fro¨bisch8,9, Christian F. Kammerer8 & Rudyard W. Sadleir4,10 Terrestrial vertebrates are first known to colonize high-latitude regions during the middle Permian (Guadalupian) about 270 million years ago, following the Pennsylvanian Gondwanan continental glaciation. However, despite over 150 years of study in these areas, the bio- geographic origins of these rich communities of land-dwelling vertebrates remain obscure. Here we report on a new early Permian continental tetrapod fauna from South America in tropical Western Gondwana that sheds new light on patterns of tetrapod distribution. Northeastern Brazil hosted an extensive lacustrine system inhabited by a unique community of temnospondyl amphibians and reptiles that considerably expand the known temporal and geographic ranges of key subgroups. Our findings demonstrate that tetrapod groups common in later Permian and Triassic temperate communities were already present in tropical Gondwana by the early Permian (Cisuralian). This new fauna constitutes a new biogeographic province with North American affinities and clearly demonstrates that tetrapod dispersal into Gondwana was already underway at the beginning of the Permian. 1 Centro de Cieˆncias da Natureza, Universidade Federal do Piauı´, 64049-550 Teresina, Brazil. 2 Programa de Po´s-Graduac¸a˜o em Geocieˆncias, Departamento de Geologia, Universidade Federal de Pernambuco, 50740-533 Recife, Brazil. 3 Departamento de Cs. Geologicas, FCEN, Universidad de Buenos Aires, IDEAN- CONICET, C1428EHA Ciudad Auto´noma de Buenos Aires, Argentina. -
Stuttgarter Beiträge Zur Naturkunde
S^5 ( © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at Stuttgarter Beiträge zur Naturkunde Serie B (Geologie und Paläontologie) Herausgeber: Staatliches Museum für Naturkunde, Rosenstein 1, D-70191 Stuttgart Stuttgarter Beitr. Naturk. Ser. B Nr. 278 175 pp., 4pls., 54figs. Stuttgart, 30. 12. 1999 Comparative osteology oi Mastodonsaurus giganteus (Jaeger, 1828) from the Middle Triassic (Lettenkeuper: Longobardian) of Germany (Baden-Württemberg, Bayern, Thüringen) By Rainer R. Schoch, Stuttgart With 4 plates and 54 textfigures Abstract Mastodonsaurus giganteus, the most abundant and giant amphibian of the German Letten- keuper, is revised. The study is based on the excellently preserved and very rieh material which was excavated during road construction in 1977 near Kupferzeil, Northern Baden- Württemberg. It is shown that there exists only one diagnosable species of Mastodonsaurus, to which all Lettenkeuper material can be attributed. All finds from other horizons must be referred to as Mastodonsauridae gen. et sp. indet. because of their fragmentary Status. A sec- ond, definitely diagnostic genus of this family is Heptasaurus from the higher Middle and Upper Buntsandstein. Finally a diagnosis of the family Mastodonsauridae is provided. Ä detailed osteological description of Mastodonsaurus giganteus reveals numerous un- known or formerly inadequately understood features, yielding data on various hitherto poor- ly known regions of the skeleton. The sutures of the skull roof, which could be studied in de- tail, are significantly different from the schemes presented by previous authors. The endocra- nium and mandible are further points of particular interest. The palatoquadrate contributes a significant part to the formation of the endocranium by an extensive and complicated epi- pterygoid. -
Cacopsamphibiala373bolt.Pdf
v UNIVtRSlT Cp ILLINOIS I 5RARY AT URBANA-CHAMPAIGN L IOLOGY CO CO /&£^<-*x~*yw FIELDIANA Geology Published by Field Museum of Natural History Volume 37, No. 3 June 30, 1977 Cacops (Amphibia: Labyrinthodontia) From the Fort Sill Locality, Lower Permian of Oklahoma the The Library of John R. Bolt Assistant Curator, Fossil Reptiles and Amphibians 1978 Field Museum of Natural History MRRU ABSTRACT at Urbana-ChamP«* The armored dissorophid (Super family Dissorophoidea ) labyrinthodont amphi- bian Cacops aspidephorus is unusual in having a large otic notch closed posteriorly by the tabular. Cacops was previously known only from the "Cacops Bone Bed," Lower Permian of Texas. Poor preservation makes this material difficult to study. Excellently preserved, though disarticulated, Cacops material has now been recov- ered from the Fort Sill fissure fills, which are probably very close in age to the "Ca- cops Bone Bed." Identification of the Fort Sill material as Cacops is based on pala- tines (primarily), armor scutes, and quadrates; the latter are here described for the first time from Fort Sill. The Cacops quadrate resembles that of other dissorophoids in having a posterodorsal process, which is unusual in the marked anterior expan- sion of its dorsal end. Comparison with other dissorophoids having a closed otic notch shows that Cacops is not unique in this anterior expansion of the process. Orientation of the process can apparently be used to distinguish trematopsids with a slit-like, closed (by the tabular) otic notch, from dissorophids. At least one such trematopsid occurs at Fort Sill, and resembles Cacops in anterior expansion of the process. -
Phylogeny and Evolution of the Dissorophoid Temnospondyls
Journal of Paleontology, 93(1), 2019, p. 137–156 Copyright © 2018, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/15/0088-0906 doi: 10.1017/jpa.2018.67 The putative lissamphibian stem-group: phylogeny and evolution of the dissorophoid temnospondyls Rainer R. Schoch Staatliches Museum für Naturkunde, Rosenstein 1, D-70191 Stuttgart, Germany 〈[email protected]〉 Abstract.—Dissorophoid temnospondyls are widely considered to have given rise to some or all modern amphibians (Lissamphibia), but their ingroup relationships still bear major unresolved questions. An inclusive phylogenetic ana- lysis of dissorophoids gives new insights into the large-scale topology of relationships. Based on a TNT 1.5 analysis (33 taxa, 108 characters), the enigmatic taxon Perryella is found to nest just outside Dissorophoidea (phylogenetic defintion), but shares a range of synapomorphies with this clade. The dissorophoids proper are found to encompass a first dichotomy between the largely paedomorphic Micromelerpetidae and all other taxa (Xerodromes). Within the latter, there is a basal dichotomy between the large, heavily ossified Olsoniformes (Dissorophidae + Trematopidae) and the small salamander-like Amphibamiformes (new taxon), which include four clades: (1) Micropholidae (Tersomius, Pasawioops, Micropholis); (2) Amphibamidae sensu stricto (Doleserpeton, Amphibamus); (3) Branchiosaur- idae (Branchiosaurus, Apateon, Leptorophus, Schoenfelderpeton); and (4) Lissamphibia. The genera Platyrhinops and Eos- copus are here found to nest at the base of Amphibamiformes. Represented by their basal-most stem-taxa (Triadobatrachus, Karaurus, Eocaecilia), lissamphibians nest with Gerobatrachus rather than Amphibamidae, as repeatedly found by former analyses. -
Heber Den Archegosaurus Der Stciiikohleiiforntatioii. Wenn Auch
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Palaeontographica - Beiträge zur Naturgeschichte der Vorzeit Jahr/Year: 1851 Band/Volume: 1 Autor(en)/Author(s): Meyer Hermann Christian Erich von Artikel/Article: Ueber den Archegosaurus der Steinkohlenformation. 209-215 © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at Heber den Archegosaurus der Stciiikohleiiforntatioii. Von Hermann von Meyer. Die Nachrichten über das Vorkommen von Reptilien in Gebilden älter als die Formation des Zechsteins hatten sich bei genauerer Prüfung immer als unhaltbar bewiesen. Man glaubte sich daher um so mehr berechtigt, anzunehmen, dass im Zechstein die ältesten Reptilien begraben lägen, als während der Versammlung der Naturforscher in Mainz Dr. Gergens und Alex. Braun mir eine Wirbelthier- Versteinerung aus dem der Steinkohlenformation angehörigen, durch seine Fische berühmten Schieferthon von Münster- Appel in der bayerschen Pfalz vorlegten, deren Beschaffenheit mehr auf ein Wirbelthier mit Füssen als auf einen Fisch schliessen Hess. Dieses merkwürdige kleine Geschöpf habe ich Anfangs 1844, es Apateon pedestris nennend, beschrieben (Jahrb. f. Min. 1844. S. 336), später aber in den Palaeontographicis (1. S. 152. Taf. 20. Fig. t.) dargelegt. Drei Jahre darauf gelang es dem Berghauptmann v. Dechen in den Sphärosideritnieren der Steinkohlenformation zu Lebach im Saarbrücken'schen, woraus zuvor ebenfalls nur Fische bekannt waren , Ueberreste zu entdecken , welche an die Gegenwart von Sauriern in diesem Ge- bilde glauben Hessen. Mit dem zu Münster-Appel gefundenen Thier stimmten sie nicht überein. Die erste Nachricht darüber theilte Goldfuss in der Niederrheinischen Gesellschaft für Natur- und Heilkunde in Bonn am 18. Februar 1847 mit. -
Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha)
Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) by Richard Kissel A thesis submitted in conformity with the requirements for the degree of doctor of philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto © Copyright by Richard Kissel 2010 Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha) Richard Kissel Doctor of Philosophy Graduate Department of Ecology & Evolutionary Biology University of Toronto 2010 Abstract Based on dental, cranial, and postcranial anatomy, members of the Permo-Carboniferous clade Diadectidae are generally regarded as the earliest tetrapods capable of processing high-fiber plant material; presented here is a review of diadectid morphology, phylogeny, taxonomy, and paleozoogeography. Phylogenetic analyses support the monophyly of Diadectidae within Diadectomorpha, the sister-group to Amniota, with Limnoscelis as the sister-taxon to Tseajaia + Diadectidae. Analysis of diadectid interrelationships of all known taxa for which adequate specimens and information are known—the first of its kind conducted—positions Ambedus pusillus as the sister-taxon to all other forms, with Diadectes sanmiguelensis, Orobates pabsti, Desmatodon hesperis, Diadectes absitus, and (Diadectes sideropelicus + Diadectes tenuitectes + Diasparactus zenos) representing progressively more derived taxa in a series of nested clades. In light of these results, it is recommended herein that the species Diadectes sanmiguelensis be referred to the new genus -
Early Tetrapod Relationships Revisited
Biol. Rev. (2003), 78, pp. 251–345. f Cambridge Philosophical Society 251 DOI: 10.1017/S1464793102006103 Printed in the United Kingdom Early tetrapod relationships revisited MARCELLO RUTA1*, MICHAEL I. COATES1 and DONALD L. J. QUICKE2 1 The Department of Organismal Biology and Anatomy, The University of Chicago, 1027 East 57th Street, Chicago, IL 60637-1508, USA ([email protected]; [email protected]) 2 Department of Biology, Imperial College at Silwood Park, Ascot, Berkshire SL57PY, UK and Department of Entomology, The Natural History Museum, Cromwell Road, London SW75BD, UK ([email protected]) (Received 29 November 2001; revised 28 August 2002; accepted 2 September 2002) ABSTRACT In an attempt to investigate differences between the most widely discussed hypotheses of early tetrapod relation- ships, we assembled a new data matrix including 90 taxa coded for 319 cranial and postcranial characters. We have incorporated, where possible, original observations of numerous taxa spread throughout the major tetrapod clades. A stem-based (total-group) definition of Tetrapoda is preferred over apomorphy- and node-based (crown-group) definitions. This definition is operational, since it is based on a formal character analysis. A PAUP* search using a recently implemented version of the parsimony ratchet method yields 64 shortest trees. Differ- ences between these trees concern: (1) the internal relationships of aı¨stopods, the three selected species of which form a trichotomy; (2) the internal relationships of embolomeres, with Archeria -
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. -
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. -
Phylogeny and Evolution of the Dissorophoid Temnospondyls
Journal of Paleontology, 93(1), 2019, p. 137–156 Copyright © 2018, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/15/0088-0906 doi: 10.1017/jpa.2018.67 The putative lissamphibian stem-group: phylogeny and evolution of the dissorophoid temnospondyls Rainer R. Schoch Staatliches Museum für Naturkunde, Rosenstein 1, D-70191 Stuttgart, Germany 〈[email protected]〉 Abstract.—Dissorophoid temnospondyls are widely considered to have given rise to some or all modern amphibians (Lissamphibia), but their ingroup relationships still bear major unresolved questions. An inclusive phylogenetic ana- lysis of dissorophoids gives new insights into the large-scale topology of relationships. Based on a TNT 1.5 analysis (33 taxa, 108 characters), the enigmatic taxon Perryella is found to nest just outside Dissorophoidea (phylogenetic defintion), but shares a range of synapomorphies with this clade. The dissorophoids proper are found to encompass a first dichotomy between the largely paedomorphic Micromelerpetidae and all other taxa (Xerodromes). Within the latter, there is a basal dichotomy between the large, heavily ossified Olsoniformes (Dissorophidae + Trematopidae) and the small salamander-like Amphibamiformes (new taxon), which include four clades: (1) Micropholidae (Tersomius, Pasawioops, Micropholis); (2) Amphibamidae sensu stricto (Doleserpeton, Amphibamus); (3) Branchiosaur- idae (Branchiosaurus, Apateon, Leptorophus, Schoenfelderpeton); and (4) Lissamphibia. The genera Platyrhinops and Eos- copus are here found to nest at the base of Amphibamiformes. Represented by their basal-most stem-taxa (Triadobatrachus, Karaurus, Eocaecilia), lissamphibians nest with Gerobatrachus rather than Amphibamidae, as repeatedly found by former analyses. -
A New Species of Cyclotosaurus (Stereospondyli, Capitosauria) from the Late Triassic of Bielefeld, NW Germany, and the Intrarelationships of the Genus
Foss. Rec., 19, 83–100, 2016 www.foss-rec.net/19/83/2016/ doi:10.5194/fr-19-83-2016 © Author(s) 2016. CC Attribution 3.0 License. A new species of Cyclotosaurus (Stereospondyli, Capitosauria) from the Late Triassic of Bielefeld, NW Germany, and the intrarelationships of the genus Florian Witzmann1,2, Sven Sachs3,a, and Christian J. Nyhuis4 1Department of Ecology and Evolutionary Biology, Brown University, Providence, G-B204, RI 02912, USA 2Museum für Naturkunde, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Invalidenstraße 43, 10115 Berlin, Germany 3Naturkundemuseum Bielefeld, Abteilung Geowissenschaften, Adenauerplatz 2, 33602 Bielefeld, Germany 4Galileo-Wissenswelt, Mummendorferweg 11b, 23769 Burg auf Fehmarn, Germany aprivate address: Im Hof 9, 51766 Engelskirchen, Germany Correspondence to: Florian Witzmann (fl[email protected]; fl[email protected]) Received: 19 January 2016 – Revised: 11 March 2016 – Accepted: 14 March 2016 – Published: 23 March 2016 Abstract. A nearly complete dermal skull roof of a capi- clotosaurus is the sister group of the Heylerosaurinae (Eo- tosaur stereospondyl with closed otic fenestrae from the mid- cyclotosaurus C Quasicyclotosaurus). Cyclotosaurus buech- dle Carnian Stuttgart Formation (Late Triassic) of Bielefeld- neri represents the only unequivocal evidence of Cycloto- Sieker (NW Germany) is described. The specimen is as- saurus (and of a cyclotosaur in general) in northern Germany. signed to the genus Cyclotosaurus based on the limited con- tribution of the frontal to the orbital margin via narrow lat- eral processes. A new species, Cyclotosaurus buechneri sp. nov., is erected based upon the following unique combina- 1 Introduction tion of characters: (1) the interorbital distance is short so that the orbitae are medially placed (shared with C.