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Sauropareion Anoplus, with a Discussion of Possible Life History
The postcranial skeleton of the Early Triassic parareptile Sauropareion anoplus, with a discussion of possible life history MARK J. MACDOUGALL, SEAN P. MODESTO, and JENNIFER BOTHA−BRINK MacDougall, M.J., Modesto, S.P., and Botha−Brink, J. 2013. The postcranial skeleton of the Early Triassic parareptile Sauropareion anoplus, with a discussion of possible life history. Acta Palaeontologica Polonica 58 (4): 737–749. The skeletal anatomy of the Early Triassic (Induan) procolophonid reptile Sauropareion anoplus is described on the basis of three partial skeletons from Vangfontein, Middelburg District, South Africa. Together these three specimens preserve the large majority of the pectoral and pelvic girdles, articulated forelimbs and hindlimbs, and all but the caudal portion of the vertebral column, elements hitherto undescribed. Our phylogenetic analysis of the Procolophonoidea is consonant with previous work, positing S. anoplus as the sister taxon to a clade composed of all other procolophonids exclusive of Coletta seca. Previous studies have suggested that procolophonids were burrowers, and this seems to have been the case for S. anoplus, based on comparisons with characteristic skeletal anatomy of living digging animals, such as the presence of a spade−shaped skull, robust phalanges, and large unguals. Key words: Parareptilia, Procolophonidae, phylogenetic analysis, burrowing, Induan, Triassic, South Africa. Mark J. MacDougall [[email protected]], Department of Biology, Cape Breton University, Sydney, Nova Scotia, B1P 6L2, Canada and Department of Biology, University of Toronto at Mississauga, 3359 Mississauga Road, Ontario, L5L 1C6, Canada; Sean P. Modesto [[email protected]], Department of Biology, Cape Breton University, Sydney, Nova Scotia, B1P 6L2, Canada; Jennifer Botha−Brink [[email protected]], Karoo Palaeontology, National Museum, P.O. -
A Procolophonid (Parareptilia) from the Owl Rock Member, Chinle Formation of Utah, Usa
Palaeontologia Electronica http://palaeo-electronica.org A PROCOLOPHONID (PARAREPTILIA) FROM THE OWL ROCK MEMBER, CHINLE FORMATION OF UTAH, USA Nicholas C. Fraser, Randall B. Irmis*, and David K. Elliott ABSTRACT An isolated skull of a procolophonid is described from the Owl Rock Member of the Chinle Formation in the Abajo Mountains of southeast Utah. Although poorly pre- served, this specimen exhibits features that demonstrate a phylogenetic relationship with leptopleuronine procolophonids. These include the dentition, the greatly expanded orbitotemporal opening, the prominent quadratojugal spikes, and the shape of the jugal. Nicholas C. Fraser. Virginia Museum of Natural History, Martinsville, Virginia 24112, USA. [email protected] Randall B. Irmis. Department of Geology, Northern Arizona University, Flagstaff, Arizona 86011, USA. *Current Address: University of California Museum of Paleontology, 1101 Valley Life Sciences Building, Berkeley, California 94720-4780. [email protected] David K. Elliott. Department of Geology, Northern Arizona University, Flagstaff, Arizona 86011, USA. [email protected] KEY WORDS: Procolophonidae; Parareptilia; Late Triassic; Chinle Formation PE Article Number: 8.1.13 Copyright: Society of Vertebrate Paleontology. May 2005 Submission: 28 June 2004. Acceptance: 6 March 2005. INTRODUCTION skull has been described in detail (Kemp 1974; Carroll and Lindsay 1985). The first member of the The Procolophonidae are a group of small clade to be named was Leptopleuron from the parareptiles (sensu Laurin and Reisz -
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). -
Alpha Taxonomy of the Russian Permian Procolophonoid Reptiles
Alpha taxonomy of the Russian Permian procolophonoid reptiles LAURA K. SÄILÄ Säilä, L.K. 2009. Alpha taxonomy of the Russian Permian procolophonoid reptiles. Acta Palaeontologica Polonica 54 (4): 599–608. doi:10.4202/app.2009.0017 European Russia has been the source of many procolophonoid taxa from both the Permian and Triassic, and a Permian or− igin for the procolophonoid family Procolophonidae has been based on the Russian taxon Microphon exiguus. Recently, this taxon was reclassified as a seymouriamorph and, in its place, the taxa Nyctiphruretus, Suchonosaurus, and Kinelia from the Middle and Upper Permian of Russia were suggested as “procolophons”, using evolutionary−systematic classifi− cation methods. In recent phylogenies, however, Nyctiphruretus has been recovered as a non–procolophonoid para− reptile, whereas Kinelia and Suchonosaurus have never been included in a phylogenetic study. Re−examination indicates that Suchonosaurus is a member of the procolophonoid subfamily Procolophonidae based on the shape of the maxillary bone and the external naris, the laterally visible maxillary depression, and the number and type of maxillary teeth. Kinelia, on the other hand, is excluded from the Procolophonoidea because of its subpleurodont dental attachment and lack of any procolophonoid features. Thus, Suchonosaurus is the only confirmed Permian procolophonid from the Permian of Rus− sia. Additionally, re−examination of the holotype of Microphon exiguus confirms that it is identical to the seymouria− morph specimens recently included in the genus Microphon and that it lacks procolophonoid features. The earliest un− equivocal record of the subfamily Procolophonidae is confirmed from the Late Permian of Russia, making Russia the only region where, with certainty, both Permian and Triassic procolophonids have been discovered. -
Chinese Pareiasaurs
Benton, M. J. (2016). The Chinese pareiasaurs. Zoological Journal of the Linnean Society, 177(4), 813-853. https://doi.org/10.1111/zoj.12389 Peer reviewed version License (if available): Unspecified Link to published version (if available): 10.1111/zoj.12389 Link to publication record in Explore Bristol Research PDF-document This is the author accepted manuscript (AAM). The final published version (version of record) is available online via Wiley at http://onlinelibrary.wiley.com/doi/10.1111/zoj.12389/abstract. Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Page 1 of 85 Zoological Journal of the Linnean Society 1 1 2 3 1 [Abstract] 4 5 2 6 3 Pareiasaurs were important medium- to large-sized herbivores in the Middle and Late 7 8 4 Permian, some 268-252 million years (Myr) ago. They are best known from abundant remains 9 10 5 of several taxa each in South Africa and Russia, with isolated finds from other parts of the 11 6 world. Six genera and species of pareiasaurs have been described from China, and yet they 12 13 7 have not been reviewed. Of these six, Tsiyuania may be a synonym of Honania, but this taxon 14 15 8 is not further considered here. The other four, which were named for separate finds from the 16 9 Sunjiagou Formation (Changhsingian, 254-252 Myr) show considerable similarities. -
Origin of the Unique Ventilatory Apparatus of Turtles
ARTICLE Received 8 Apr 2014 | Accepted 10 Sep 2014 | Published 7 Nov 2014 DOI: 10.1038/ncomms6211 Origin of the unique ventilatory apparatus of turtles Tyler R. Lyson1,2,3, Emma R. Schachner4,5, Jennifer Botha-Brink6,7, Torsten M. Scheyer8, Markus Lambertz9, G.S. Bever3,10,11, Bruce S. Rubidge3 & Kevin de Queiroz2 The turtle body plan differs markedly from that of other vertebrates and serves as a model system for studying structural and developmental evolution. Incorporation of the ribs into the turtle shell negates the costal movements that effect lung ventilation in other air-breathing amniotes. Instead, turtles have a unique abdominal-muscle-based ventilatory apparatus whose evolutionary origins have remained mysterious. Here we show through broadly comparative anatomical and histological analyses that an early member of the turtle stem lineage has several turtle-specific ventilation characters: rigid ribcage, inferred loss of inter- costal muscles and osteological correlates of the primary expiratory muscle. Our results suggest that the ventilation mechanism of turtles evolved through a division of labour between the ribs and muscles of the trunk in which the abdominal muscles took on the primary ventilatory function, whereas the broadened ribs became the primary means of stabilizing the trunk. These changes occurred approximately 50 million years before the evolution of the fully ossified shell. 1 Department of Earth Sciences, Denver Museum of Nature and Science, Denver, Colorado 80205, USA. 2 Department of Vertebrate Zoology, National Museum of Natural History, Smithsonian Institution, Washington DC 20560, USA. 3 Evolutionary Studies Institute, University of the Witwatersrand, PO Wits 2050, Johannesburg, South Africa. -
Carnivorous Dinocephalian from the Middle Permian of Brazil and Tetrapod Dispersal in Pangaea
Carnivorous dinocephalian from the Middle Permian of Brazil and tetrapod dispersal in Pangaea Juan Carlos Cisnerosa,1, Fernando Abdalab, Saniye Atayman-Güvenb, Bruce S. Rubidgeb, A. M. Celâl Sxengörc,1, and Cesar L. Schultzd aCentro de Ciências da Natureza, Universidade Federal do Piauí, 64049-550 Teresina, Brazil; bBernard Price Institute for Palaeontological Research, University of the Witwatersrand, WITS 2050 Johannesburg, South Africa; cAvrasya Yerbilimleri Estitüsü, İstanbul Teknik Üniversitesi, Ayazaga 34469, Istanbul, Turkey; and dDepartamento de Paleontologia e Estratigrafia, Universidade Federal do Rio Grande do Sul, 91540-000 Porto Alegre, Brazil Contributed by A. M. Celâlx Sengör, December 5, 2011 (sent for review September 29, 2011) The medial Permian (∼270–260 Ma: Guadalupian) was a time of fragmentary to further explore their affinities with confidence. Here important tetrapod faunal changes, in particular reflecting a turn- we present a diagnosable dinocephalian species from the Permian over from pelycosaurian- to therapsid-grade synapsids. Until now, of South America, based on a complete and well-preserved cra- most knowledge on tetrapod distribution during the medial Perm- nium. This fossil is a member of the carnivorous clade Ante- ian has come from fossils found in the South African Karoo and the osauridae, and provides evidence for Pangaea-wide distribution Russian Platform, whereas other areas of Pangaea are still poorly of carnivorous dinocephalians during the Guadalupian. known. We present evidence for the presence of a terrestrial car- nivorous vertebrate from the Middle Permian of South America Results based on a complete skull. Pampaphoneus biccai gen. et sp. nov. Systematic Paleontology. Synapsida Osborn, 1903; Therapsida was a dinocephalian “mammal-like reptile” member of the Ante- Broom, 1905; Dinocephalia Seeley, 1894; Anteosauridae Boon- osauridae, an early therapsid predator clade known only from the stra, 1954; Syodontinae Ivakhnenko, 1994; Pampaphoneus biccai Middle Permian of Russia, Kazakhstan, China, and South Africa. -
A Reassessment of the Taxonomic Position of Mesosaurs, and a Surprising Phylogeny of Early Amniotes
ORIGINAL RESEARCH published: 02 November 2017 doi: 10.3389/feart.2017.00088 A Reassessment of the Taxonomic Position of Mesosaurs, and a Surprising Phylogeny of Early Amniotes Michel Laurin 1* and Graciela H. Piñeiro 2 1 CR2P (UMR 7207) Centre de Recherche sur la Paléobiodiversité et les Paléoenvironnements (Centre National de la Recherche Scientifique/MNHN/UPMC, Sorbonne Universités), Paris, France, 2 Departamento de Paleontología, Facultad de Ciencias, University of the Republic, Montevideo, Uruguay We reassess the phylogenetic position of mesosaurs by using a data matrix that is updated and slightly expanded from a matrix that the first author published in 1995 with his former thesis advisor. The revised matrix, which incorporates anatomical information published in the last 20 years and observations on several mesosaur specimens (mostly from Uruguay) includes 17 terminal taxa and 129 characters (four more taxa and five more characters than the original matrix from 1995). The new matrix also differs by incorporating more ordered characters (all morphoclines were ordered). Parsimony Edited by: analyses in PAUP 4 using the branch and bound algorithm show that the new matrix Holly Woodward, Oklahoma State University, supports a position of mesosaurs at the very base of Sauropsida, as suggested by the United States first author in 1995. The exclusion of mesosaurs from a less inclusive clade of sauropsids Reviewed by: is supported by a Bremer (Decay) index of 4 and a bootstrap frequency of 66%, both of Michael S. Lee, which suggest that this result is moderately robust. The most parsimonious trees include South Australian Museum, Australia Juliana Sterli, some unexpected results, such as placing the anapsid reptile Paleothyris near the base of Consejo Nacional de Investigaciones diapsids, and all of parareptiles as the sister-group of younginiforms (the most crownward Científicas y Técnicas (CONICET), Argentina diapsids included in the analyses). -
The Bulletin of Zoological Nomenclature
220 Bulletin of Zoological Nomenclature 58(3) September 2001 Case 3191 Pareiasaurus kavpinskii Amalitzky, 1922 (currently Scutosaurus karpinskii', Reptilia, Pareiasauria): proposed conservation of the specific name Michael S.Y. Lee Department of Palaeontology, The South Australian Museum, North Terrace, Adelaide 5000, Australia (e-mail: [email protected]) Abstract. The purpose of this application is to conserve the specific name and typification of the taxon currently known as Scutosaurus karpinskii (Amalitzky, 1922), an abundant fossil pareiasaurian reptile from the Russian Permian. The specific name karpinskii is threatened by the spelling variant karpinskyi, inadvertently published prematurely by Watson (1917) when the full description was delayed by war and the death of Amalitzky; if the name were attributed to the 1917 publication the name-bearing type would not be the skeleton designated as the holotype of Pareiasaurus karpinskii by Amalitzky (1922). Keywords. Nomenclature; taxonomy; Reptilia; Pareiasauria; pareiasauridae; Scutosaurus; Scutosaurus karpinskii; Permian; Russia. 1. The first specimens of the Permian pareiasaurian reptile currently known as Scutosaurus karpinskii (Amalitzky, 1922) were excavated from North Dvina (near Kotlas, north European Russia) around the beginning of the 20th-century by the palaeontologist Vladimir P. Amalitzky (Buffetaut, 1987; Ochev & Surkov, 2000). Amalitzky was preparing a full description of the entire North Dvina fauna, including the pareiasaur, but this was interrupted by the First World War and his sudden death in 1918 (Woodward, 1918; Buffetaut, 1987). 2. While Amalitzky's full description was delayed, his friend and colleague D.M.S. Watson (1917, p. 10) published a figure of a scapulocoracoid, labelling it Pariasaurus Karpinskyi, Amalitz'. -
A New Reptile from the Lower Permian of Brazil (Karutia Fortunata Gen
Journal of Systematic Palaeontology ISSN: (Print) (Online) Journal homepage: https://www.tandfonline.com/loi/tjsp20 A new reptile from the lower Permian of Brazil (Karutia fortunata gen. et sp. nov.) and the interrelationships of Parareptilia Juan Carlos Cisneros , Christian F. Kammerer , Kenneth D. Angielczyk , Jörg Fröbisch , Claudia Marsicano , Roger M. H. Smith & Martha Richter To cite this article: Juan Carlos Cisneros , Christian F. Kammerer , Kenneth D. Angielczyk , Jörg Fröbisch , Claudia Marsicano , Roger M. H. Smith & Martha Richter (2021): A new reptile from the lower Permian of Brazil (Karutiafortunata gen. et sp. nov.) and the interrelationships of Parareptilia, Journal of Systematic Palaeontology, DOI: 10.1080/14772019.2020.1863487 To link to this article: https://doi.org/10.1080/14772019.2020.1863487 View supplementary material Published online: 12 Jan 2021. Submit your article to this journal Article views: 107 View related articles View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=tjsp20 Journal of Systematic Palaeontology, 2021 http://dx.doi.org/10.1080/14772019.2020.1863487 A new reptile from the lower Permian of Brazil (Karutia fortunata gen. et sp. nov.) and the interrelationships of Parareptilia aà b c b,d Juan Carlos Cisneros , Christian F. Kammerer , Kenneth D. Angielczyk ,Jorg€ Frobisch€ , Claudia Marsicanoe,f , Roger M. H. Smithg,h and Martha Richteri aMuseu de Arqueologia e Paleontologia, Universidade Federal do Piauı, 64049-550 Teresina, Brazil; bPaleontology Unit, North Carolina Museum of Natural Sciences, Raleigh, NC 27601, USA; cNegaunee Integrative Research Center, Field Museum of Natural History, 1400 South Lake Shore Drive, Chicago, IL 60605, USA; dInstitut fur€ Biologie, Humboldt-Universitat€ zu Berlin, Invalidenstr. -
Pareiasaurids from the Rio Do Rasto Formation, Southern Brazil: Biostratigraphic Implications for Permian Faunas of the Paraná Basin
Revista Brasileira deCISNEROS Paleontologia ET8(1):13-24, AL. – PAREIASAURIDSJaneiro/Abril 2005 FROM THE RIO DO RASTO FORMATION 13 2005 by the Sociedade Brasileira de Paleontologia PAREIASAURIDS FROM THE RIO DO RASTO FORMATION, SOUTHERN BRAZIL: BIOSTRATIGRAPHIC IMPLICATIONS FOR PERMIAN FAUNAS OF THE PARANÁ BASIN JUAN CARLOS CISNEROS, FERNANDO ABDALA Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, Private Bag 3, WITS 2050, Johannesburg, South Africa. [email protected], [email protected] MARIA C. MALABARBA Museu de Ciências e Tecnologia, PUCRS, Av. Ipiranga 6651, 90619-900, Porto Alegre, Brazil. [email protected] ABSTRACT – Comparison between pareiasaurid materials from Aceguá, originally assigned to Pareiasaurus americanus, and a new cranium from Posto Queimado indicates that they belong to the same taxon. Despite their size difference, the skulls from these localities show similarities in the maxillary dentition and dermal bone ornamentation. Dental and cranial characters confirm the difference between the Brazilian pareiasaurid and the South African Pareiasaurus, supporting the proposed allocation of the Brazilian form in the genus Provelosaurus. The Brazilian pareiasaurid has autapomorphies in the shape of the squamosal and the morphology and placement of the quadratojugal bosses. The presence of the same pareiasaurid in Posto Queimado and Aceguá strongly indicates that these faunas are contemporaneous. The record of dinocephalians and pareiasaurids in Posto Queimado suggests a correlation of the Posto Queimado-Aceguá assemblage with the Guadalupian Tapinocephalus Assemblage Zone of South Africa and Isheevo Assemblage of Eastern Europe. The presence of amphibians tentatively assigned to archegosaurids at Aceguá fauna however, represents a conflict because the last global record of this family is known from the Ocher fauna from Eastern Europe, which is regarded older than the South African Tapinocephalus Assemblage Zone. -
Granja Palmeiras, a New Fossiliferous Site for the Lower Triassic of Southern Brazil
Rev. bras. paleontol. 14(2):157-168, Maio/Agosto 2011 © 2011 by the Sociedade Brasileira de Paleontologia doi:10.4072/rbp.2011.2.04 GRANJA PALMEIRAS, A NEW FOSSILIFEROUS SITE FOR THE LOWER TRIASSIC OF SOUTHERN BRAZIL SÉRGIO DIAS-DA-SILVA Laboratório de Paleobiologia, UNIPAMPA, Campus São Gabriel, Av. Antônio Trilha, 1847, 97300-000, São Gabriel, RS, Brasil. [email protected] ÁTILA AUGUSTO STOCK DA-ROSA Laboratório de Estratigrafia e Paleobiologia, Departamento de Geociências, Centro de Ciências Naturais e Exatas, UFSM, 97105-900, Santa Maria, RS, Brasil. [email protected] ABSTRACT – A new fossiliferous locality, Granja Palmeiras, is described for the Sanga do Cabral Formation (Lower Triassic of Southern Brazil, Rosário do Sul Group, Paraná Basin). It consists on orange and reddish fine sandstones, with sandy and calcareous concretions and intercalated fossiliferous intraformational conglomerates. Its fossils are fragmentary and badly preserved. Nevertheless, among the 46 specimens collected so far, putative actinopterygians, temnospondyls, procolophonoids, archosauromorphs, and non-mammalian cynodonts were identified. Besides, several non-diagnostic appendicular elements are ascribed to Tetrapoda indet. The fossiliferous content found in Granja Palmeiras can provide a valuable new framework for future correlation with other Lower Triassic South American units as well as other continental tetrapod-bearing deposits from Gondwana. Key words: Sanga do Cabral Formation, Lower Triassic, Gondwana, vertebrates. RESUMO – Uma nova localidade fossilífera, Granja Palmeiras, é descrita para a Formação Sanga do Cabral (Triássico Inferior do sul do Brasil, Grupo Rosário do Sul, bacia do Paraná). Consiste em arenitos finos alaranjados e avermelhados, com concreções carbonáticas e arenosas, e conglomerados intraformacionais intercalados.