A Glyptosaurine Lizard from the Eocene
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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. -
Publications (Published, in Press, Accepted, Or in Revision). * Indicates Undergraduate Mentee
Publications (published, in press, accepted, or in revision). * indicates undergraduate mentee 14. Scarpetta SG. Iguanian lizards from the Split Rock Formation, Wyoming: exploring the modernization of the North American lizard fauna. Journal of Systematic Palaeontology. In press. 13. Scarpetta SG, Ledesma DT, Llauger FO, White BA. 2020. Evolution of North American lizards. eLS 1(4), 705-717. https://doi.org/10.1002/9780470015902.a0029078. Invited submission. All authors contributed equally to this work. 12. Scarpetta SG. 2020. Effects of phylogenetic uncertainty on fossil identification illustrated by a new and enigmatic Eocene iguanian. Scientific Reports 10(1), 1-10. https://doi.org/10.1038/s41598-020-72509-2 11. Scarpetta SG. 2020. Combined-evidence analyses of ultraconserved elements and morphological data: an empirical example in iguanian lizards. Biology Letters 16(8), 20200356. https://doi.org/10.1098/rsbl.2020.0356 10. Scarpetta SG. 2020. Unusual lizard fossil from the Miocene of Nebraska and a minimum age for cnemidophorine teiids. Royal Society Open Science 7(8), 200317. http://dx.doi.org/10.1098/rsos.200317 9. Scarpetta SG, Bell CJ. 2020. Novel and bizarre abnormalities of the tooth row in side- blotched lizards (Uta) and rock lizards (Petrosaurus). The Anatomical Record 303, 2014-2025. https://doi.org/10.1002/ar.24279 8. Scarpetta SG. 2019. The first known fossil Uma: Ecological evolution and the origins of North American fringe-toed lizards. BMC Evolutionary Biology 19(178), 1-22. https://doi.org/10.1186/s12862-019-1501-5 7. Scarpetta SG. 2019. Aneides hardii (Sacramento Mountains Salamander). Catalogue of American Amphibians and Reptiles 921, 1-23. -
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Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Graduate School of Arts and Sciences COLUMBIA UNIVERSITY 2016 © 2015 Kaori Tsukui All rights reserved ABSTRACT Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui The age of the Bridgerian/Uintan boundary has been regarded as one of the most important outstanding problems in North American Land Mammal “Age” (NALMA) biochronology. The Bridger Basin in southwestern Wyoming preserves one of the best stratigraphic records of the faunal boundary as well as the preceding Bridgerian NALMA. In this dissertation, I first developed a chronological framework for the Eocene Bridger Formation including the age of the boundary, based on a combination of magnetostratigraphy and U-Pb ID-TIMS geochronology. Within the temporal framework, I attempted at making a regional correlation of the boundary-bearing strata within the western U.S., and also assessed the body size evolution of three representative taxa from the Bridger Basin within the context of Early Eocene Climatic Optimum. Integrating radioisotopic, magnetostratigraphic and astronomical data from the early to middle Eocene, I reviewed various calibration models for the Geological Time Scale and intercalibration of 40Ar/39Ar data among laboratories and against U-Pb data, toward the community goal of achieving a high precision and well integrated Geological Time Scale. In Chapter 2, I present a magnetostratigraphy and U-Pb zircon geochronology of the Bridger Formation from the Bridger Basin in southwestern Wyoming. -
The Sclerotic Ring: Evolutionary Trends in Squamates
The sclerotic ring: Evolutionary trends in squamates by Jade Atkins A Thesis Submitted to Saint Mary’s University, Halifax, Nova Scotia in Partial Fulfillment of the Requirements for the Degree of Master of Science in Applied Science July, 2014, Halifax Nova Scotia © Jade Atkins, 2014 Approved: Dr. Tamara Franz-Odendaal Supervisor Approved: Dr. Matthew Vickaryous External Examiner Approved: Dr. Tim Fedak Supervisory Committee Member Approved: Dr. Ron Russell Supervisory Committee Member Submitted: July 30, 2014 Dedication This thesis is dedicated to my family, friends, and mentors who helped me get to where I am today. Thank you. ! ii Table of Contents Title page ........................................................................................................................ i Dedication ...................................................................................................................... ii List of figures ................................................................................................................. v List of tables ................................................................................................................ vii Abstract .......................................................................................................................... x List of abbreviations and definitions ............................................................................ xi Acknowledgements .................................................................................................... -
Varanid Lizard Venoms Disrupt the Clotting Ability of Human Fibrinogen Through Destructive Cleavage
toxins Article Varanid Lizard Venoms Disrupt the Clotting Ability of Human Fibrinogen through Destructive Cleavage James S. Dobson 1 , Christina N. Zdenek 1 , Chris Hay 1, Aude Violette 2 , Rudy Fourmy 2, Chip Cochran 3 and Bryan G. Fry 1,* 1 Venom Evolution Lab, School of Biological Sciences, University of Queensland, St Lucia, QLD 4072, Australia; [email protected] (J.S.D.); [email protected] (C.N.Z.); [email protected] (C.H.) 2 Alphabiotoxine Laboratory sprl, Barberie 15, 7911 Montroeul-au-bois, Belgium; [email protected] (A.V.); [email protected] (R.F.) 3 Department of Earth and Biological Sciences, Loma Linda University, Loma Linda, CA 92350, USA; [email protected] * Correspondence: [email protected] Received: 11 March 2019; Accepted: 1 May 2019; Published: 7 May 2019 Abstract: The functional activities of Anguimorpha lizard venoms have received less attention compared to serpent lineages. Bite victims of varanid lizards often report persistent bleeding exceeding that expected for the mechanical damage of the bite. Research to date has identified the blockage of platelet aggregation as one bleeding-inducing activity, and destructive cleavage of fibrinogen as another. However, the ability of the venoms to prevent clot formation has not been directly investigated. Using a thromboelastograph (TEG5000), clot strength was measured after incubating human fibrinogen with Heloderma and Varanus lizard venoms. Clot strengths were found to be highly variable, with the most potent effects produced by incubation with Varanus venoms from the Odatria and Euprepriosaurus clades. The most fibrinogenolytically active venoms belonged to arboreal species and therefore prey escape potential is likely a strong evolutionary selection pressure. -
Eocene Green River Formation, Western United States
Synoptic reconstruction of a major ancient lake system: Eocene Green River Formation, western United States M. Elliot Smith* Alan R. Carroll Brad S. Singer Department of Geology and Geophysics, University of Wisconsin, 1215 West Dayton Street, Madison, Wisconsin 53706, USA ABSTRACT Members. Sediment accumulation patterns than being confi ned to a single episode of arid thus refl ect basin-center–focused accumula- climate. Evaporative terminal sinks were Numerous 40Ar/39Ar experiments on sani- tion rates when the basin was underfi lled, initially located in the Greater Green River dine and biotite from 22 ash beds and 3 and supply-limited accumulation when the and Piceance Creek Basins (51.3–48.9 Ma), volcaniclastic sand beds from the Greater basin was balanced fi lled to overfi lled. Sedi- then gradually migrated southward to the Green River, Piceance Creek, and Uinta ment accumulation in the Uinta Basin, at Uinta Basin (47.1–45.2 Ma). This history is Basins of Wyoming, Colorado, and Utah Indian Canyon, Utah, was relatively con- likely related to progressive southward con- constrain ~8 m.y. of the Eocene Epoch. Mul- stant at ~150 mm/k.y. during deposition of struction of the Absaroka Volcanic Prov- tiple analyses were conducted per sample over 5 m.y. of both evaporative and fl uctuat- ince, which constituted a major topographic using laser fusion and incremental heating ing profundal facies, which likely refl ects the and thermal anomaly that contributed to a techniques to differentiate inheritance, 40Ar basin-margin position of the measured sec- regional north to south hydrologic gradient. loss, and 39Ar recoil. -
Tiago Rodrigues Simões
Diapsid Phylogeny and the Origin and Early Evolution of Squamates by Tiago Rodrigues Simões A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in SYSTEMATICS AND EVOLUTION Department of Biological Sciences University of Alberta © Tiago Rodrigues Simões, 2018 ABSTRACT Squamate reptiles comprise over 10,000 living species and hundreds of fossil species of lizards, snakes and amphisbaenians, with their origins dating back at least as far back as the Middle Jurassic. Despite this enormous diversity and a long evolutionary history, numerous fundamental questions remain to be answered regarding the early evolution and origin of this major clade of tetrapods. Such long-standing issues include identifying the oldest fossil squamate, when exactly did squamates originate, and why morphological and molecular analyses of squamate evolution have strong disagreements on fundamental aspects of the squamate tree of life. Additionally, despite much debate, there is no existing consensus over the composition of the Lepidosauromorpha (the clade that includes squamates and their sister taxon, the Rhynchocephalia), making the squamate origin problem part of a broader and more complex reptile phylogeny issue. In this thesis, I provide a series of taxonomic, phylogenetic, biogeographic and morpho-functional contributions to shed light on these problems. I describe a new taxon that overwhelms previous hypothesis of iguanian biogeography and evolution in Gondwana (Gueragama sulamericana). I re-describe and assess the functional morphology of some of the oldest known articulated lizards in the world (Eichstaettisaurus schroederi and Ardeosaurus digitatellus), providing clues to the ancestry of geckoes, and the early evolution of their scansorial behaviour. -
Microsoft Word
LIST OF EXTANT INGROUP TAXA: Agamidae: Agama agama, Pogona vitticeps, Calotes emma, Physignathus cocincinus. Chamaeleonidae: Brookesia brygooi, Chamaeleo calyptratus. Corytophanidae: Basiliscus basiliscus, Corytophanes cristatus. Crotaphytidae: Crotaphytus collaris, Gambelia wislizenii. Hoplocercidae: Enyalioides laticeps, Morunasaurus annularis. Iguanidae: Brachylophus fasciatus, Dipsosaurus dorsalis, Sauromalus ater. Leiolepidae: Leiolepis rubritaeniata, Uromastyx hardwicki. Leiosauridae: Leiosaurus catamarcensis, Pristidactylus torquatus, Urostrophus vautieri. Liolaemidae: Liolaemus elongatus, Phymaturus palluma. Opluridae: Chalarodon madagascariensis, Oplurus cyclurus. Phrynosomatidae: Petrosaurus mearnsi, Phrynosoma platyrhinos, Sceloporus variabilis, Uma scoparia, Uta stansburiana. Polychrotidae: Anolis carolinensis, Polychrus marmoratus. Tropiduridae: Leiocephalus barahonensis, Stenocercus guentheri, Tropidurus plica, Uranoscodon superciliosus. Anguidae: Ophisaurus apodus, Anniella pulchra, Diploglossus enneagrammus, Elgaria multicarinata. Cordylidae: Chamaesaura anguina, Cordylus mossambicus. Dibamidae: Anelytropsis papillosus, Dibamus novaeguineae. Eublepharidae: Aeluroscalobates felinus, Coleonyx variegatus, Eublepharis macularius. "Gekkonidae": Teratoscincus przewalski, Diplodactylus ciliaris, Phyllurus cornutus, Rhacodactylus auriculatus, Gekko gecko, Phelsuma lineata. Gonatodes albogularis. Gerrhosauridae: Cordylosaurus subtesselatus, Zonosaurus ornatus. Gymnophthalmidae: Colobosaura modesta, Pholidobolus montium. Helodermatidae: -
Primates, Adapiformes) Skull from the Uintan (Middle Eocene) of San Diego County, California
AMERICAN JOURNAL OF PHYSICAL ANTHROPOLOGY 98:447-470 (1995 New Notharctine (Primates, Adapiformes) Skull From the Uintan (Middle Eocene) of San Diego County, California GREGG F. GUNNELL Museum of Paleontology, University of Michigan, Ann Arbor, Michigan 481 09-1079 KEY WORDS Californian primates, Cranial morphology, Haplorhine-strepsirhine dichotomy ABSTRACT A new genus and species of notharctine primate, Hespero- lemur actius, is described from Uintan (middle Eocene) aged rocks of San Diego County, California. Hesperolemur differs from all previously described adapiforms in having the anterior third of the ectotympanic anulus fused to the internal lateral wall of the auditory bulla. In this feature Hesperolemur superficially resembles extant cheirogaleids. Hesperolemur also differs from previously known adapiforms in lacking bony canals that transmit the inter- nal carotid artery through the tympanic cavity. Hesperolemur, like the later occurring North American cercamoniine Mahgarita steuensi, appears to have lacked a stapedial artery. Evidence from newly discovered skulls ofNotharctus and Smilodectes, along with Hesperolemur, Mahgarita, and Adapis, indicates that the tympanic arterial circulatory pattern of these adapiforms is charac- terized by stapedial arteries that are smaller than promontory arteries, a feature shared with extant tarsiers and anthropoids and one of the character- istics often used to support the existence of a haplorhine-strepsirhine dichot- omy among extant primates. The existence of such a dichotomy among Eocene primates is not supported by any compelling evidence. Hesperolemur is the latest occurring notharctine primate known from North America and is the only notharctine represented among a relatively diverse primate fauna from southern California. The coastal lowlands of southern California presumably served as a refuge area for primates during the middle and later Eocene as climates deteriorated in the continental interior. -
The Tiny Cretaceous Stem-Bird Oculudentavis Revealed As a Bizarre Lizard
bioRxiv preprint doi: https://doi.org/10.1101/2020.08.09.243048; this version posted August 10, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. The tiny Cretaceous stem-bird Oculudentavis revealed as a bizarre lizard Arnau Bolet1,2, Edward L. Stanley3, Juan D. Daza4*, J. Salvador Arias5, Andrej Čerňanský6, Marta Vidal-García7, Aaron M. Bauer8, Joseph J. Bevitt9, Adolf Peretti10, and Susan E. Evans11 Affiliations: 1 Institut Català de Paleontologia, Universitat Autònoma de Barcelona. Barcelona, Spain. 2 School of Earth Sciences, University of Bristol, Bristol, United Kingdom. 3 Department of Herpetology, Florida Museum of Natural History, Gainesville, Florida, United States. 4 Department of Biological Sciences, Sam Houston State University, Huntsville, Texas, United States. 5 Fundación Miguel Lillo, CONICET, San Miguel de Tucumán, Argentina. 6 Department of Ecology, Laboratory of Evolutionary Biology, Faculty of Natural Sciences, Comenius University in Bratislava, Bratislava, Slovakia. 7Department of Cell Biology & Anatomy, University of Calgary, Calgary, Canada. 8Department of Biology and Center for Biodiversity and Ecosystem Stewardship, Villanova University, Villanova, Pennsylvania, United States. 9Australian Centre for Neutron Scattering, Australian Nuclear Science and Technology Organisation, Sydney, Australia. 10GRS Gemresearch Swisslab AG and Peretti Museum Foundation, Meggen, Switzerland. 11Department of Cell and Developmental Biology, University College London, London, United Kingdom. *For correspondence: [email protected] 1 bioRxiv preprint doi: https://doi.org/10.1101/2020.08.09.243048; this version posted August 10, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. -
Variability in Pulmonary Reduction and Asymmetry in a Serpentiform Lizard: the Sheltopusik, Pseudopus Apodus (Pallas, 1775)
68 (1): 21– 26 © Senckenberg Gesellschaft für Naturforschung, 2018. 19.4.2018 Variability in pulmonary reduction and asymmetry in a serpentiform lizard: The sheltopusik, Pseudopus apodus (Pallas, 1775) Markus Lambertz 1, 2, *, Nils Arenz 1 & Kristina Grommes 1 1 Institut für Zoologie, Rheinische Friedrich-Wilhelms-Universität Bonn, Poppelsdorfer Schloss, 53115 Bonn, Germany — 2 Sektion Herpetolo- gie, Zoologisches Forschungsmuseum Alexander Koenig, Adenauerallee 160, 53113 Bonn, Germany; [email protected] — * Correspond- ing author Accepted 4.ix.2017. Published online at www.senckenberg.de/vertebrate-zoology on 5.4.2018. Editor in charge: Uwe Fritz Abstract Besides snakes, numerous lineages of squamates gave rise to limb-reduced and elongated (serpentiform) species, indicating the evolution- ary success of this modification of the plesiomorphic lizard Bauplan. Concerted with a serpentiform habitus are several morphological adaptations, many of which also concern the structure and arrangement of the viscera, such as frequently a pronounced pulmonary asym- metry in which one lung is reduced or even absent. The European glass lizard or sheltopusik, Pseudopus apodus, is the largest species of the exclusively serpentiform Anguinae. Driven by pre-existing conflicting statements on pulmonary asymmetry, we examined the lungs of 14 sheltopusiks and compared the condition to 11 slow worms (Anguis fragilis). We consistently found the left lung pronouncedly shorter for the slow worm, but indeed a highly variable pulmonary asymmetry between left and right sides in the sheltopusik. This is the first verified case of such variability in pulmonary reduction for any serpentiform squamate and raises several questions about the underlying developmental program for this otherwise taxon-specifically conservative trait. -
Alphabetical List
LIST E - GEOLOGIC AGE (STRATIGRAPHIC) TERMS - ALPHABETICAL LIST Age Unit Broader Term Age Unit Broader Term Aalenian Middle Jurassic Brunhes Chron upper Quaternary Acadian Cambrian Bull Lake Glaciation upper Quaternary Acheulian Paleolithic Bunter Lower Triassic Adelaidean Proterozoic Burdigalian lower Miocene Aeronian Llandovery Calabrian lower Pleistocene Aftonian lower Pleistocene Callovian Middle Jurassic Akchagylian upper Pliocene Calymmian Mesoproterozoic Albian Lower Cretaceous Cambrian Paleozoic Aldanian Lower Cambrian Campanian Upper Cretaceous Alexandrian Lower Silurian Capitanian Guadalupian Algonkian Proterozoic Caradocian Upper Ordovician Allerod upper Weichselian Carboniferous Paleozoic Altonian lower Miocene Carixian Lower Jurassic Ancylus Lake lower Holocene Carnian Upper Triassic Anglian Quaternary Carpentarian Paleoproterozoic Anisian Middle Triassic Castlecliffian Pleistocene Aphebian Paleoproterozoic Cayugan Upper Silurian Aptian Lower Cretaceous Cenomanian Upper Cretaceous Aquitanian lower Miocene *Cenozoic Aragonian Miocene Central Polish Glaciation Pleistocene Archean Precambrian Chadronian upper Eocene Arenigian Lower Ordovician Chalcolithic Cenozoic Argovian Upper Jurassic Champlainian Middle Ordovician Arikareean Tertiary Changhsingian Lopingian Ariyalur Stage Upper Cretaceous Chattian upper Oligocene Artinskian Cisuralian Chazyan Middle Ordovician Asbian Lower Carboniferous Chesterian Upper Mississippian Ashgillian Upper Ordovician Cimmerian Pliocene Asselian Cisuralian Cincinnatian Upper Ordovician Astian upper