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The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
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. -
Ontogenetic Change in the Temporal Region of the Early Permian Parareptile Delorhynchus Cifellii and the Implications for Closure of the Temporal Fenestra in Amniotes
RESEARCH ARTICLE Ontogenetic Change in the Temporal Region of the Early Permian Parareptile Delorhynchus cifellii and the Implications for Closure of the Temporal Fenestra in Amniotes Yara Haridy*, Mark J. Macdougall, Diane Scott, Robert R. Reisz Department of Biology, University of Toronto Mississauga, Mississauga, Ontario, Canada * [email protected] a11111 Abstract A juvenile specimen of Delorhynchus cifellii, collected from the Early Permian fissure-fill deposits of Richards Spur, Oklahoma, permits the first detailed study of cranial ontogeny in this parareptile. The specimen, consisting of a partially articulated skull and mandible, exhib- OPEN ACCESS its several features that identify it as juvenile. The dermal tuberosities that ornament the dor- Citation: Haridy Y, Macdougall MJ, Scott D, Reisz sal side and lateral edges of the largest skull of D. cifellii specimens, are less prominent in RR (2016) Ontogenetic Change in the Temporal the intermediate sized holotype, and are absent in the new specimen. This indicates that the Region of the Early Permian Parareptile new specimen represents an earlier ontogenetic stage than all previously described mem- Delorhynchus cifellii and the Implications for bers of this species. In addition, the incomplete interdigitation of the sutures, most notably Closure of the Temporal Fenestra in Amniotes. PLoS ONE 11(12): e0166819. doi:10.1371/journal. along the fronto-nasal contact, plus the proportionally larger sizes of the orbit and temporal pone.0166819 fenestrae further support an early ontogenetic stage for this specimen. Comparisons Editor: Thierry Smith, Royal Belgian Institute of between this juvenile and previously described specimens reveal that the size and shape of Natural Sciences, BELGIUM the temporal fenestra in Delorhynchus appear to vary through ontogeny, due to changes in Received: July 18, 2016 the shape and size of the bordering cranial elements. -
From the Late–Middle Eocene of Eastern Thrace
G Model PALEVO-993; No. of Pages 15 ARTICLE IN PRESS C. R. Palevol xxx (2017) xxx–xxx Contents lists available at ScienceDirect Comptes Rendus Palevol www.sci encedirect.com General Palaeontology, Systematics and Evolution (Vertebrate Palaeontology) First occurrence of Palaeotheriidae (Perissodactyla) from the late–middle Eocene of eastern Thrace (Greece) Première occurrence de Palaeotheriidae (Perissodactyla) du Miocène moyen–tardif de Thrace orientale (Grèce) a,b,∗ a Grégoire Métais , Sevket Sen a CR2P, Paléobiodiversité et Paléoenvironnements, UMR 7207 (CNRS, MNHN, UPMC), Sorbonne Université, Muséum national d’histoire naturelle, 8, rue Buffon, 75005 Paris, France b Department of Ecology and Evolutionary Biology, University of Kansas, 66045 Lawrence, Kansas, USA a b s t r a c t a r t i c l e i n f o Article history: A detailed assessment of postcranial fossils collected at Balouk Keui (Thrace, Greece) in the Received 11 July 2016 mid-19th Century by the naturalist Auguste Viquesnel enabled us to identify the material Accepted after revision 10 January 2017 as pertaining to Palaeotherium sp., cf. P. magnum, which constitutes the easternmost occur- Available online xxx rence of the genus during the Eocene. We have constrained the geographic and stratigraphic provenance of the fossil by reassessing information about Viquesnel’s itinerary and observa- Handled by Lars vanden Hoek Ostende tions. Although the exact age of the fossil remains uncertain, the occurrence of a palaeothere in the Thrace Basin during the Eocene indicates a wider geographic distribution for the Keywords: genus, which had previously been restricted to western and central Europe. The palaeothere Palaeotherium of Balouk Keui confirms that the palaeogeographic range of this group included the Balkans Thrace during the middle–late Eocene. -
A Fossil Sawfly of the Genus Athalia (Hymenoptera: Tenthredinidae
C. R. Palevol 4 (2005) 7–16 http://france.elsevier.com/direct/PALEVO/ Systematic Palaeontology A fossil sawfly of the genus Athalia (Hymenoptera: Tenthredinidae) from the Eocene–Oligocene boundary of Altkirch, France Torsten Wappler a,*, Sebastian Hinsken b, Jochen J. Brocks c, Andreas Wetzel b, Christian A. Meyer d a Hessisches Landesmuseum, Department of Geology, Palaeontology & Mineralogy, Friedensplatz 1, 64283 Darmstadt, Germany b Geological & Paleontological Institute, University Basel, Bernoullistraße 32, CH-4056 Basel, Switzerland c Department of Organismic and Evolutionary Biology, Harvard University, 26 Oxford Street, Cambridge MA 02138, USA d Museum of Natural History Basel, Augustinergasse 2, CH-4001 Basel, Switzerland Received 2 August 2004; revised and accepted 8 December 2004 Available online 20 january 2005 Written on incitation of the Editorial Board Abstract A new species of coleseed sawfly (Tenthredinidae: Athaliini) is described and figured from the Eocene–Oligocene ‘Rebberg’ quarry within the Fossiliferous Zone, a member of the Middle Salt Formation. Athalia vetuecclesiae n. sp. is the first represen- tative of the Athalia group from the geological record. The new species is most similar to members of the A. vollenhoveni-group represented by only six species from Africa, but can be distinguished by details of antennal structure and length of spurs of the hind tibia. The phylogenetic position of the fossil within the Tenthredinidae*, its palaeoenvironmental implication, and the geological setting of the quarry are briefly discussed. To cite this article: T. Wappler et al., C. R. Palevol 4 (2005). © 2004 Académie des sciences. Published by Elsevier SAS. All rights reserved. Résumé Une espèce de symphyte (Tenthredinidae: Athaliini) est décrite pour la première fois en enregistrement fossile, dans la « zone fossilifère » de la carrière Rebberg d’Altkirch (Sud de l’Alsace, France). -
A Reassessment of the Taxonomic Position of Mesosaurs, and a Surprising Phylogeny of Early Amniotes
GENERAL COMMENTARY published: 03 December 2018 doi: 10.3389/feart.2018.00220 Response: Commentary: A Reassessment of the Taxonomic Position of Mesosaurs, and a Surprising Phylogeny of Early Amniotes Michel Laurin 1* and Graciela Piñeiro 2 1 CR2P (UMR 7207), CNRS/MNHN Sorbonne Université, “Centre de Recherches sur la Paléobiodiversité et les Paléoenvironnements”, Muséum National d’Histoire Naturelle, Paris, France, 2 Departamento de Paleontología, Facultad de Ciencias, Montevideo, Uruguay Keywords: Mesosauridae, Parareptilia, Synapsida, Sauropsida, Amniota, Paleozoic, temporal fenestration A Commentary on Commentary: A Reassessment of the Taxonomic Position of Mesosaurs, and a Surprising Phylogeny of Early Amniotes by MacDougall, M. J., Modesto, S. P., Brocklehurst, N., Verrière, A., Reisz, R. R., and Fröbisch, J. (2018). Front. Earth Sci. 6:99. doi: 10.3389/feart.2018.00099 INTRODUCTION Edited by: Corwin Sullivan, University of Alberta, Canada Mesosaurs, known from the Early Permian of southern Africa, Brazil, and Uruguay, are the oldest known amniotes with a primarily, though probably not strictly, aquatic lifestyle (Nuñez Demarco Reviewed by: et al., 2018). Despite having attracted the attention of several prominent scientists, such as Wegener Tiago Simoes, University of Alberta, Canada (1966), who used them to support his theory of continental drift, and the great anatomist and paleontologist von Huene (1941), who first suggested the presence of a lower temporal fenestra *Correspondence: Michel Laurin in Mesosaurus, several controversies still surround mesosaurs. One concerns the presence of the [email protected] lower temporal fenestra in mesosaurs, which we accept (Piñeiro et al., 2012a; Laurin and Piñeiro, 2017, p. 4), contrary to Modesto (1999, 2006) and MacDougall et al. -
Critical Comments on the Genus Propachynolophus Lemoine, 1891 (Mammalia, Perissodactyla, Equoidea)
ARTICLE Critical comments on the genus Propachynolophus Lemoine, 1891 (Mammalia, Perissodactyla, Equoidea) JEAN A. REMY Institut des Sciences de l’Evolution, UMR 5554 CNRS, IRD, EPHE, Université de Montpellier, Place Eugène Bataillon, 34095 Montpellier cedex 5, France E-mail: [email protected] Abstract: The validity of Propachynolophus Lemoine, 1891, supposedly an intermediate between Hyracotherium Owen, 1841 and Pachynolophus Pomel, 1847, has been questioned for a long time. A detailed analysis of features on which this genus is based further supported by a formal cladistic analysis demonstrates that Propachynolophus is not a valid taxon. The type species, “Propachynolophus gaudryi Lemoine, 1891” shall be assigned to Propalaeotherium Gervais, 1849, under the new combination Propalaeotherium gaudryi (Lemoine, 1891). “Pachynolophus maldani Lemoine, 1878”, later assigned to Propachynolophus, typifies the new genus Orolophus, under the binomen Orolophus maldani (Lemoine, 1878). The other referred species, “Propachynolophus levei Hooker, 1994” and “P. remyi Checa-Soler, 1997” are poorly documented, and both species shall be provisionally referred to as “Hyracotherium” levei (Hooker, 1994) and “Hyracotherium” remyi (Checa-Soler, 1997), pending new discoveries. Keywords: Eocene, tooth morphology, Pachynolophus, Propalaeotherium, Eurohippus Submitted 8 December 2016, Accepted 3 August 2017 Published Online 27 September 2017, doi: 1018563/pv.41.1.e3 © Copyright Jean Remy September 2017 INTRODUCTION Propachynolophus gaudryi was “based upon miscellaneous isolated teeth and jaw fragments constituting a part of the fossil vertebrate sample collected in the vicinity of Epernay (Marne)” By their diversity and abundance, perissodactyls have played (Savage et al., 1965: 16), a sample known as the “Ageian a crucial role in the European Eocene mammalian faunas. -
Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming
Distribution and Stratigraphip Correlation of Upper:UB_ • Ju Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Iktman Formations, Southern Bighorn Basin* Wyoming U,S. GEOLOGICAL SURVEY PROFESS IONAL PAPER 1540 Cover. A member of the American Museum of Natural History 1896 expedition enter ing the badlands of the Willwood Formation on Dorsey Creek, Wyoming, near what is now U.S. Geological Survey fossil vertebrate locality D1691 (Wardel Reservoir quadran gle). View to the southwest. Photograph by Walter Granger, courtesy of the Department of Library Services, American Museum of Natural History, New York, negative no. 35957. DISTRIBUTION AND STRATIGRAPHIC CORRELATION OF UPPER PALEOCENE AND LOWER EOCENE FOSSIL MAMMAL AND PLANT LOCALITIES OF THE FORT UNION, WILLWOOD, AND TATMAN FORMATIONS, SOUTHERN BIGHORN BASIN, WYOMING Upper part of the Will wood Formation on East Ridge, Middle Fork of Fifteenmile Creek, southern Bighorn Basin, Wyoming. The Kirwin intrusive complex of the Absaroka Range is in the background. View to the west. Distribution and Stratigraphic Correlation of Upper Paleocene and Lower Eocene Fossil Mammal and Plant Localities of the Fort Union, Willwood, and Tatman Formations, Southern Bighorn Basin, Wyoming By Thomas M. Down, Kenneth D. Rose, Elwyn L. Simons, and Scott L. Wing U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1540 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director For sale by U.S. Geological Survey, Map Distribution Box 25286, MS 306, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. -
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 -
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. -
SUPPLEMENTARY INFORMATION: Tables, Figures and References
Samuels, Regnault & Hutchinson, PeerJ Evolution of the patellar sesamoid bone in mammals SUPPLEMENTARY INFORMATION: Tables, Figures and References Supplementary Table S1: Mammaliaform patellar status$ Inclusive clades Genus and Stratigraphic age of Patellar Comments# (partial) species (and taxon, and location(s) state reference(s) used for 0/1/2 patellar status) (absent/ ‘patelloid’/ present) Sinoconodonta Sinoconodon Jurassic, China 0 Patellar groove absent, suggests no rigneyi (Kielan- patella Jaworowska et al., 2004) Sinoconodon is included on our phylogeny within tritylodontids. Morganucodonta Megazostrodon Late Triassic, southern 0 rudnerae (Jenkins Africa & Parrington, 1976) Morganucodonta Eozostrodon sp. Late Triassic, Wales 0 Asymmetric patellar groove, (Jenkins et al., specimens disarticulated so it is hard 1976) to assess the patella but appears absent Docodonta Castorocauda 164 Mya, mid-Jurassic, 0 Semi-aquatic adaptations lutrasimilis (Ji et China al., 2006) Docodonta Agilodocodon 164 Mya, mid-Jurassic, 0 scansorius (Meng China et al., 2015) Docodonta Docofossor 160 Mya, China 0 brachydactylus (Luo et al., 2015b) Docodonta Haldanodon 150-155 Mya, Late 0 Shallow patellar groove exspectatus Jurassic, Portugal (Martin, 2005b) Australosphenida Asfaltomylos Mid-Jurassic, South ? Postcranial material absent patagonicus America (Martin, 2005a) Australosphenida Ornithorhynchus Extant 2 Platypus, genome sequenced Monotremata anatinus (Warren, Hillier, Marshall Graves et (Herzmark, 1938; al., 2008) Rowe, 1988) Australosphenida Tachyglossus -
Cisneros2008.Pdf
Journal of Systematic Palaeontology 6 (3): 345–366 Issued 22 August 2008 doi:10.1017/S1477201907002350 Printed in the United Kingdom C The Natural History Museum ! Phylogenetic relationships of procolophonid parareptiles with remarks on their geological record Juan Carlos Cisneros∗ Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, South Africa SYNOPSIS The phylogenetic intrarelationships of procolophonid parareptiles are determined via a comprehensive cladistic analysis using a data matrix of 21 taxa and 58 characters. Most taxa are in- cluded for the first time in a phylogenetic analysis and 27 characters are novel. The relationships within the group are more firmly resolved than in previous analyses. Procolophoninae and Leptopleuron- inae, two of the three traditional subdivisions of the Procolophonidae, are valid monophyletic groups, but Spondylolestinae is polyphyletic. The Chinese genera Pentaedrusaurus and Neoprocolophon are the most primitive members of the Leptopleuroninae. A new group, Theledectinae, is erected. The latter clade consists of small procolophonids with a reduced marginal dentition and wide bulbous monocuspid teeth. Eumetabolodon from China and the former genus ‘Thelegnathus’ from South Africa are shown to be polyphyletic. The successful radiation of the Procolophonidae during the Triassic is likely to be related to the development of feeding adaptations that allowed exploration of various ecological niches, particularly the exploitation of high-fibre herbivory. The scarcity of Permian records of procolophonids is examined and the genus Spondylolestes from the Upper Permian of South Africa is considered to be a valid taxon with procolophonid affinities. Finally, a review of the records from the Middle and Upper Triassic reveals a procolophonid global hiatus of more than 15 Ma in Ladinian–Lower Carnian rocks.