Master Document Template

Total Page:16

File Type:pdf, Size:1020Kb

Master Document Template Copyright by Blake Russell Chapman 2018 The Senior Honors Thesis Committee for Blake Russell Chapman Certifies that this is the approved version of the following Thesis: A new Assemblage of Mosasaurs from the Upper Cretaceous Savoy Pit, Austin Chalk, Northeast Texas APPROVED BY SUPERVISING COMMITTEE: Christopher J. Bell, Supervisor Christopher Lowery Charles Kerans A new Assemblage of Mosasaurs from the Upper Cretaceous Savoy Pit, Austin Chalk, Northeast Texas by Blake Russell Chapman Senior Honors Thesis Presented to the Faculty of the Jackson School of Geosciences of The University of Texas at Austin in Partial Fulfillment of the Requirements for the University Honors Research Program The University of Texas at Austin May 2018 Acknowledgements I thank my graduate student mentor Joshua Lively for the many hours he spent familiarizing me with the anatomy of lizards and mosasaurs, answering my numerous questions on mosasaur ecology and evolution, introducing me to mechanical preparatory work, and guiding my way as a paleontologist. I thank my undergraduate adviser Christopher J. Bell for all the knowledge he shared on the proper procedures for conducting science and ethics, spending long days and nights revising my abstracts and research thesis, and for his repeated financial support during my undergraduate career. I also thank Christopher Lowery, Charles Kerans, Michael J. Polcyn, and the Bell Lab Group for guidance and assistance on this project. Preparation that I did not complete myself was performed by Kenneth Bader, Alana Self, Paul Redman, Chase Shelburne, and Michael Chiappone. I thank Deborah E. Wagner for her advice on fossil preparation. I also thank the collections managers and staffs of the following institutions for J. Lively’s access to collections which by extension also benefitted me: Chris Sagebiel of the Vertebrate Paleontology Laboratory at The University of Texas at Austin, Dale A. Winkler of the Schuler Museum of Paleontology at Southern Methodist University Kansas University, Laura E. Wilson of the Sternberg Museum of Natural History at Fort Hays State University, Darrin Pagnac of the Museum of Geology at South Dakota School of Mines and Technology, Hans-Dieter Sues of the National Museum of Natural History at the Smithsonian, Michael J. Novacek of the American Museum of Natural History, Tim White of the Yale Peabody Museum, Ned Gilmore of The Academy of Natural iv Sciences of Drexel University, Mary Beth Prondzinski of the Alabama Museum of Natural History at The University of Alabama, Lamar Smith at the McWane Science Center, Rodney Scheetz of the Museum of Paleontology at Brigham Young University, Brandon Strilisky of the Royal Tyrrell Museum of Palaeontology, Michael W. Caldwell of the University of Alberta Laboratory for Vertebrate Paleontology, Patrick Leiggi of the Museum of the Rockies at Montana State University, Courtenay and District Museum and Palaeontology Centre, and Richard Hulbert of the Florida Museum of Natural History at the University of Florida. This work was partially funded by grants to J. Lively from the Evolving Earth Foundation, The Geological Society of America, The Texas Academy of Science, and the Jackson School of Geosciences. Additional financial support was provided by C. Bell. v Abstract A new Assemblage of Mosasaurs from the Upper Cretaceous Savoy Pit, Austin Chalk, Northeast Texas Blake Chapman, B.S. The University of Texas at Austin, 2018 Supervisor: Christopher J. Bell The fossil assemblage at the Savoy Pit (Fannin County, Texas) was collected in 1940 by participants in the Works Progress Administration working alongside personnel from the Bureau of Economic Geology at The University of Texas at Austin. The locality is contained within the Ector Chalk (lower Coniacian), an argillaceous limestone, of the Austin Group. Previously published taxa from the site include the bird Ichthyornis and fish such as Belonostomus and Laminospondylus transversus; several types of shark teeth and invertebrates (e.g., crustaceans, asteroids, and bivalves) also have been found. Several mosasaur specimens are present at the site and include isolated elements and associated skeletons that have yet to be described. My collaborator Joshua Lively and I scored the material from the Savoy Pit using published and novel morphological characters and compared our results to about 250 mosasaur specimens from North America and Sweden. We then ran a phylogenetic vi analysis using maximum parsimony to hypothesize the taxonomic composition of the mosasaur assemblage. At least three taxa are identified: a russellosaurine represented by a frontal resembling Russellosaurus coheni, an undetermined basal mosasaurine represented by a partial skull and vertebrae, and Tylosaurus nepaeolicus based on a premaxilla and quadrate. The mosasaurine possesses a unique combination of characters including synapomorphies of both Mosasaurinae (e.g., striated quadrate tympanic rim, dorsally constricted suprastapedial process) and Russellosaurina (e.g., short premaxilla- maxilla suture, low surangular coronoid buttress). In our phylogenetic analysis, we recovered this specimen as a basal mosasaurine that does not align with any published genus, and we recognize it as a new taxon. The russellosaurine synapomorphies possessed by the new taxon may represent the plesiomorphic state of Mosasaurinae; some of those characters are shared with Kourisodon puntledgensis. The presence of a russellosaurine resembling Russellosaurus coheni may extend the range of this species into the Coniacian. The new taxon helps to fill a stratigraphic gap of approximately six million years between the earliest known mosasaurine, Dallasaurus turneri, and ‘Clidastes liodontus.’ Identification of Tylosaurus nepaeolicus at the Savoy Pit extends the lineage into the Early Coniacian and represents one of the earliest occurrences of that genus. vii TABLE OF CONTENTS LIST OF FIGURES .............................................................................................................x INTRODUCTION ...............................................................................................................1 GEOLOGIC CONTEXT AND LOCALITY INFORMATION ..........................................3 MATERIALS AND METHODS .........................................................................................6 SYSTEMATIC PALEONTOLOGY AND DESCRIPTION...............................................7 TMM 31051-84, The new taxon .................................................................................7 Systematic Paleontology ....................................................................................7 Description .........................................................................................................9 Skull ..........................................................................................................9 Maxilla .............................................................................................9 Prefrontal........................................................................................12 Jugal ...............................................................................................13 Squamosal ......................................................................................14 Postorbitofrontal ............................................................................16 Palatine ...........................................................................................17 Pterygoid ........................................................................................18 Quadrate .........................................................................................19 Coronoid ........................................................................................21 Surangular ......................................................................................22 Angular ..........................................................................................25 Post-cranial Skeleton ..............................................................................25 Atlas ...............................................................................................26 viii Post-atlas Vertebrae .......................................................................27 Cervical Vertebrae ................................................................28 Trunk Vertebrae ....................................................................29 Ribs ................................................................................................30 TMM 31051-64, Tylosaurus nepaeolicus .................................................................31 Systematic Paleontology ..................................................................................31 Description .......................................................................................................31 Premaxilla ...............................................................................................31 Quadrate ..................................................................................................33 TMM 31051-59, Yaguarasaurinae cf. Russellosaurus coheni ..................................36 Systematic Paleontology ..................................................................................36 Description .......................................................................................................36 Frontal .....................................................................................................36
Recommended publications
  • Annotated Checklist of Fossil Fishes from the Smoky Hill Chalk of the Niobrara Chalk (Upper Cretaceous) in Kansas
    Lucas, S. G. and Sullivan, R.M., eds., 2006, Late Cretaceous vertebrates from the Western Interior. New Mexico Museum of Natural History and Science Bulletin 35. 193 ANNOTATED CHECKLIST OF FOSSIL FISHES FROM THE SMOKY HILL CHALK OF THE NIOBRARA CHALK (UPPER CRETACEOUS) IN KANSAS KENSHU SHIMADA1 AND CHRISTOPHER FIELITZ2 1Environmental Science Program and Department of Biological Sciences, DePaul University,2325 North Clifton Avenue, Chicago, Illinois 60614; and Sternberg Museum of Natural History, Fort Hays State University, 3000 Sternberg Drive, Hays, Kansas 67601;2Department of Biology, Emory & Henry College, P.O. Box 947, Emory, Virginia 24327 Abstract—The Smoky Hill Chalk Member of the Niobrara Chalk is an Upper Cretaceous marine deposit found in Kansas and adjacent states in North America. The rock, which was formed under the Western Interior Sea, has a long history of yielding spectacular fossil marine vertebrates, including fishes. Here, we present an annotated taxo- nomic list of fossil fishes (= non-tetrapod vertebrates) described from the Smoky Hill Chalk based on published records. Our study shows that there are a total of 643 referable paleoichthyological specimens from the Smoky Hill Chalk documented in literature of which 133 belong to chondrichthyans and 510 to osteichthyans. These 643 specimens support the occurrence of a minimum of 70 species, comprising at least 16 chondrichthyans and 54 osteichthyans. Of these 70 species, 44 are represented by type specimens from the Smoky Hill Chalk. However, it must be noted that the fossil record of Niobrara fishes shows evidence of preservation, collecting, and research biases, and that the paleofauna is a time-averaged assemblage over five million years of chalk deposition.
    [Show full text]
  • Estimating the Evolutionary Rates in Mosasauroids and Plesiosaurs: Discussion of Niche Occupation in Late Cretaceous Seas
    Estimating the evolutionary rates in mosasauroids and plesiosaurs: discussion of niche occupation in Late Cretaceous seas Daniel Madzia1 and Andrea Cau2 1 Department of Evolutionary Paleobiology, Institute of Paleobiology, Polish Academy of Sciences, Warsaw, Poland 2 Independent, Parma, Italy ABSTRACT Observations of temporal overlap of niche occupation among Late Cretaceous marine amniotes suggest that the rise and diversification of mosasauroid squamates might have been influenced by competition with or disappearance of some plesiosaur taxa. We discuss that hypothesis through comparisons of the rates of morphological evolution of mosasauroids throughout their evolutionary history with those inferred for contemporary plesiosaur clades. We used expanded versions of two species- level phylogenetic datasets of both these groups, updated them with stratigraphic information, and analyzed using the Bayesian inference to estimate the rates of divergence for each clade. The oscillations in evolutionary rates of the mosasauroid and plesiosaur lineages that overlapped in time and space were then used as a baseline for discussion and comparisons of traits that can affect the shape of the niche structures of aquatic amniotes, such as tooth morphologies, body size, swimming abilities, metabolism, and reproduction. Only two groups of plesiosaurs are considered to be possible niche competitors of mosasauroids: the brachauchenine pliosaurids and the polycotylid leptocleidians. However, direct evidence for interactions between mosasauroids and plesiosaurs is scarce and limited only to large mosasauroids as the Submitted 31 July 2019 predators/scavengers and polycotylids as their prey. The first mosasauroids differed Accepted 18 March 2020 from contemporary plesiosaurs in certain aspects of all discussed traits and no evidence Published 13 April 2020 suggests that early representatives of Mosasauroidea diversified after competitions with Corresponding author plesiosaurs.
    [Show full text]
  • Ichthyodectiform Fishes from the Late Cretaceous
    Mesozoic Fishes 5 – Global Diversity and Evolution, G. Arratia, H.-P. Schultze & M. V. H. Wilson (eds.): pp. 247-266, 12 figs., 2 tabs. © 2013 by Verlag Dr. Friedrich Pfeil, München, Germany – ISBN 978-3-89937-159-8 Ichthyodectiform fi shes from the Late Cretaceous (Campanian) of Arkansas, USA Kelly J. IRWIN and Christopher FIELITZ Abstract Several specimens of the ichthyodectiform fishes Xiphactinus audax and Saurocephalus cf. S. lanciformis are reported from the Upper Cretaceous (Campanian) Brownstown Marl and Ozan formations of southwestern Arkansas, U.S.A. Seven individuals of Xiphactinus, based on incomplete specimens, are represented by various elements: disarticu- lated skull bones, jaw fragments, pectoral fin-rays, or vertebrae. The circular vertebral centra are diagnostic for X. audax rather than X. vetus. The specimen of Saurocephalus consists of a three-dimensional skull, lacking much of the skull roof bones. It is identified as Saurocephalus based on the shape of the predentary bone. This specimen provides the first record of entopterygoid teeth in Saurocephalus. These specimens represent new geographic and geologic distribution records of these taxa from the western Gulf Coastal Plain, which biogeographically links records from the eastern Gulf Coastal Plain with those from the Western Interior Sea. Introduction LEIDY (1854) was the first to report the presence of Cretaceous marine vertebrate fossils from Arkansas, yet in the intervening 150+ years, the body of work on the paleoichthyofauna of Arkansas remains limited (WILSON & BRUNER 2004). BARDACK (1965), GOODY (1976), CASE (1978), and RUSSELL (1988) re- ported geographic and geologic distributions for specific taxa, but few descriptive works on fossil fishes are available (see HUSSAKOF 1947; MEYER 1974; BECKER et al.
    [Show full text]
  • (Squamata: Mosasauridae) from the Late Cretaceous Of
    C. R. Palevol 14 (2015) 483–493 Contents lists available at ScienceDirect Comptes Rendus Palevol www.sci encedirect.com General Palaeontology, Systematics and Evolution (Vertebrate Palaeontology) An halisaurine (Squamata: Mosasauridae) from the Late Cretaceous of Patagonia, with a preserved tympanic disc: Insights into the mosasaur middle ear Un halisauriné (Squamata : Mosasauridae) du Crétacé supérieur de Patagonie, à disque tympanique conservé : un aperc¸ u de l’oreille moyenne des mosasaures a,∗ b Marta S. Fernández , Marianella Talevi a CONICET - División Paleontología Vertebrados, Museo de La Plata, Paseo del Bosque s/n, 1900 La Plata, Argentina b CONICET - Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, Isidro Lobo y Belgrano, 8332 General Roca, Río Negro, Argentina a b s t r a c t a r t i c l e i n f o Article history: Halisaurinae is a subfamily of enigmatic, small- to medium-sized mosasauroids, which Received 15 September 2014 retain a mosaic of primitive and derived features. The first record of a South American Hal- Accepted after revision 13 May 2015 isaurus with precise stratigraphic information includes a quadrate carrying a tympanic disc together with twelve vertebrae, collected in the Late Maastrichtian of Jagüel Formation Handled by Nathalie Bardet in northern Patagonia (Argentina). The preservation of a tympanic disc allows exploring and discussing the mechanisms of sound transmission in these mosasauroids. The loca- Keywords: tion of the tympanic disc resembles that one formed by the extracolumella of aquatic Halisaurus turtles and at least one extant lizard. Based on morphological comparison of the middle Patagonia ear we discuss previous hypotheses on the modification of the tympanic middle ear system Late Maastrichtian of mosasauroids for underwater hearing, in a manner similar to that observed in aquatic Cretaceous turtles.
    [Show full text]
  • Download Full Article in PDF Format
    comptes rendus palevol 2021 20 20 iles — Jean- pt Cl re au d d n e a R s a n g a e i — b i h P p a l a m e a o f b o i o y l h o p g a y r g a o n e d g p o i a l b a o e DIRECTEURS DE LA PUBLICATION / PUBLICATION DIRECTORS : Bruno David, Président du Muséum national d’Histoire naturelle Étienne Ghys, Secrétaire perpétuel de l’Académie des sciences RÉDACTEURS EN CHEF / EDITORS-IN-CHIEF : Michel Laurin (CNRS), Philippe Taquet (Académie des sciences) ASSISTANTE DE RÉDACTION / ASSISTANT EDITOR : Adenise Lopes (Académie des sciences ; [email protected]) MISE EN PAGE / PAGE LAYOUT : Fariza Sissi (Muséum national d’Histoire naturelle ; [email protected]) RÉVISIONS LINGUISTIQUES DES TEXTES ANGLAIS / ENGLISH LANGUAGE REVISIONS : Kevin Padian (University of California at Berkeley) RÉDACTEURS ASSOCIÉS / ASSOCIATE EDITORS : Micropaléontologie/Micropalaeontology Maria Rose Petrizzo (Università di Milano, Milano) Paléobotanique/Palaeobotany Cyrille Prestianni (Royal Belgian Institute of Natural Sciences, Brussels) Métazoaires/Metazoa Annalisa Ferretti (Università di Modena e Reggio Emilia, Modena) Paléoichthyologie/Palaeoichthyology Philippe Janvier (Muséum national d’Histoire naturelle, Académie des sciences, Paris) Amniotes du Mésozoïque/Mesozoic amniotes Hans-Dieter Sues (Smithsonian National Museum of Natural History, Washington) Tortues/Turtles Juliana Sterli (CONICET, Museo Paleontológico Egidio Feruglio, Trelew) Lépidosauromorphes/Lepidosauromorphs Hussam Zaher (Universidade de São Paulo) Oiseaux/Birds Eric Buffetaut (CNRS, École Normale Supérieure, Paris) Paléomammalogie (mammifères de moyenne et grande taille)/Palaeomammalogy (large and mid-sized mammals) Lorenzo Rook* (Università degli Studi di Firenze, Firenze) Paléomammalogie (petits mammifères sauf Euarchontoglires)/Palaeomammalogy (small mammals except for Euarchontoglires) Robert Asher (Cambridge University, Cambridge) Paléomammalogie (Euarchontoglires)/Palaeomammalogy (Euarchontoglires) K.
    [Show full text]
  • Russellosaurus Coheni N. Gen., N. Sp., a 92 Million-Year-Old Mosasaur from Texas (USA), and the Definition of the Parafamily Russellosaurina
    Netherlands Journal of Geosciences — Geologie en Mijnbouw | 84 - 3 | 321 - 333 | 2005 Russellosaurus coheni n. gen., n. sp., a 92 million-year-old mosasaur from Texas (USA), and the definition of the parafamily Russellosaurina M.J. Polcyn1'* & G.L. Bell Jr.2 1 Shuler Museum of Paleontology, Southern Methodist University, Dallas, Texas 75275, USA. 2 Guadalupe Mountains National Park, Salt Flat, Texas 79847, USA. * Corresponding author. Email: [email protected] Manuscript received: November 2004; accepted: January 2005 Abstract A new mosasaur, Russellosaurus coheni, is described from the Collignoniceras woollgari Zone (lower Middle Turonian) at Cedar Hill, Dallas County, Texas. At approximately 92 Ma, it is the oldest well-preserved mosasaur skull from North America. It possesses characters diagnostic of Plioplatecarpinae but retains numerous plesiomorphies as well. Phylogenetic analysis indicates a close relationship with Yaguarasaurus columbianus, and these two, together with Tethysaurus nopcsai, form a clade that occupies a position basal to the divergence of the subfamilies Tylosaurinae and Plioplatecarpinae. Russellosaurus coheni is proposed as the nominal taxon of a new mosasaur clade, parafamily taxon novum Russellosaurina, which includes Plioplatecarpinae, Tylosaurinae, their common ancestor and all descendants. Tethysaurus retains a plesiopedal limb and girdle morphology, and along with Russellosaurus and Yaguarasaurus, cranial plesiomorphies. Dallasaurus turneri, a temporally and geographically sympatric plesiopedal mosasaur, occupies a basal position within Mosasaurinae. This phyletic arrangement confirms that marine adaptations, such as development of paddle-like limbs, occurred independently in at least two lineages of mosasaurs, once within Mosasaurinae and once within Russellosaurina. Keywords: Mosasaur, Plioplatecarpinae, Tethysaurus, Turonian, Yaguarasaurus Introduction knowledge of the early evolutionary history of the group.
    [Show full text]
  • Papers Resulting from the First Moasaur Meeting, Maastricht, the Netherlands, May 2004
    Papers resulting from the First Moasaur Meeting, Maastricht, The Netherlands, May 2004. Bardet, N., Pereda Suberbiola, X., Iarochène, M., Amalik M., and Bouya, B. 2005. Durophagous Mosasauridae (Squamata) from the Upper Cretaceous phosphates of Morocco, with description of a new species of Globidens. Netherlands Journal of Geosciences / Geologie en Mijnbouw, 84(3), p. 167-176. Bell, G.L. Jr. and Polcyn, M.J. 2005. Dallasaurus turneri, a new primitive mosasauroid from the Middle Turonian of Texas and comments on the phylogeny of Mosasauridae (Squamata). Netherlands Journal of Geosciences / Geologie en Mijnbouw, 84(3), p. 177-194. Buchy, M.-C., Smith, K.T., Frey, E., Stinnesbeck, W., González González, A.H., Ifrim, C., López-Oliva, J.G. and Porras-Muzquiz, H. 2005. Annotated catalogue of marine squamates (Reptilia) from the Upper Cretaceous of northeastern Mexico. Netherlands Journal of Geosciences / Geologie en Mijnbouw, 84(3), p. 195-206. Caldwell, M.W. and Bell, G.L. Jr. 2005. Of German princes and North American rivers: Harlan’s lost mosasaur snout rediscovered. Netherlands Journal of Geosciences / Geologie en Mijnbouw, 84(3), p. 207-212. Caldwell, M.W. and Diedrich, C. G. 2005. Remains of Clidastes Cope, 1868, an unexpected mosasaur in the upper Campanian of NW Germany. Netherlands Journal of Geosciences / Geologie en Mijnbouw, 84(3), p. 213-220. Dutchak, A.R. 2005. A review of the taxonomy and systematics of aigialosaurs. Netherlands Journal of Geosciences / Geologie en Mijnbouw, 84(3), p. 221-230. Everhart. M.J. 2005. Tylosaurus kansasensis, a new species of tylosaurine (Squamata, Mosasauridae) from the Niobrara Chalk of western Kansas, USA.
    [Show full text]
  • Copyrighted Material
    06_250317 part1-3.qxd 12/13/05 7:32 PM Page 15 Phylum Chordata Chordates are placed in the superphylum Deuterostomia. The possible rela- tionships of the chordates and deuterostomes to other metazoans are dis- cussed in Halanych (2004). He restricts the taxon of deuterostomes to the chordates and their proposed immediate sister group, a taxon comprising the hemichordates, echinoderms, and the wormlike Xenoturbella. The phylum Chordata has been used by most recent workers to encompass members of the subphyla Urochordata (tunicates or sea-squirts), Cephalochordata (lancelets), and Craniata (fishes, amphibians, reptiles, birds, and mammals). The Cephalochordata and Craniata form a mono- phyletic group (e.g., Cameron et al., 2000; Halanych, 2004). Much disagree- ment exists concerning the interrelationships and classification of the Chordata, and the inclusion of the urochordates as sister to the cephalochor- dates and craniates is not as broadly held as the sister-group relationship of cephalochordates and craniates (Halanych, 2004). Many excitingCOPYRIGHTED fossil finds in recent years MATERIAL reveal what the first fishes may have looked like, and these finds push the fossil record of fishes back into the early Cambrian, far further back than previously known. There is still much difference of opinion on the phylogenetic position of these new Cambrian species, and many new discoveries and changes in early fish systematics may be expected over the next decade. As noted by Halanych (2004), D.-G. (D.) Shu and collaborators have discovered fossil ascidians (e.g., Cheungkongella), cephalochordate-like yunnanozoans (Haikouella and Yunnanozoon), and jaw- less craniates (Myllokunmingia, and its junior synonym Haikouichthys) over the 15 06_250317 part1-3.qxd 12/13/05 7:32 PM Page 16 16 Fishes of the World last few years that push the origins of these three major taxa at least into the Lower Cambrian (approximately 530–540 million years ago).
    [Show full text]
  • Cranial Anatomy of a Maastrichtian (Upper Cretaceous) Mosasaur (Squamata, Mosasauridae) from North-East Mexico
    Revista Mexicana de Ciencias Geológicas,Cranial anatomy v. 24, núm.of a Maastrichtian 1, 2007, p. 89-103 mosasaur from north-east Mexico 89 Cranial anatomy of a Maastrichtian (Upper Cretaceous) mosasaur (Squamata, Mosasauridae) from north-east Mexico Marie-Céline Buchy1,*, Eberhard Frey2, Wolfgang Stinnesbeck3, and José Guadalupe López-Oliva4 1 Universität Karlsruhe, Geologisches Institut, Postfach 6980, D-76128 Karlsruhe, Germany. Current address: Museo del Desierto, Apartado Postal 307, 25000 Saltillo, Coahuila, Mexico. 2 Geowissenschaftliche Abteilung, Staatliches Museum für Naturkunde, Erbprinzenstrasse 13, D-76133 Karlsruhe, Germany. 3 Universität Karlsruhe, Geologisches Institut, Postfach 6980, D-76128 Karlsruhe, Germany. 4 Universidad Autónoma de Nuevo León, Facultad de Ciencias de la Tierra, Apartado Postal 104, 67700 Linares, N.L., Mexico. * [email protected] ABSTRACT We here describe the first mosasaur from Mexico known by significant cranial remains, from the late Early Maastrichtian Méndez Formation of Nuevo León, north-east Mexico. The specimen comprises a fragmentary skull and parts of the mandibles. Some anatomical features suggest a juvenile animal. The skull possesses a rostral tuberosity on the premaxilla, as well as a combination of features known from different mosasaur genera, like its frontopremaxillary suture situated caudal to the external naris, its prefrontal and postorbitofrontal being in contact lateral to the orbit, associated with the supra- and infrastapedial processes of its quadrate which almost contact one another. Despite being clearly distinct from any hitherto described mosasaur, the affinities of this specimen with other mosasaurs remain obscure, not only because of incompleteness, but also because of the poorly understood biological significance of the characters used for the classification of Mosasauridae.
    [Show full text]
  • Considerations About the Late Cretaceous Genus Chirocentrites
    BULLETIN DE L’INSTITUT ROYAL DES SCIENCES NATURELLES DE BELGIQUE SCIENCES DE LA TERRE, 78: 209-228, 2008 BULLETIN VAN HET KONINKLIJK BELGISCH INSTITUUT VOOR NATUURWETENSCHAPPEN AARDWETENSCHAPPEN, 78: 209-228, 2008 Considerations about the Late Cretaceous genus Chirocentrites and erection of the new genus Heckelichthys (Teleostei, Ichthyodectiformes) - A new visit inside the ichthyodectid phylogeny by Louis TAVERNE TAVERNE, L., 2008 – Considerations about the Late Cretaceous Cretaceous (Maastrichtian)(1), presenting an almost genus Chirocentrites and erection of the new genus Heckelichthys worldwide distribution. Their representatives were (Teleostei, Ichthyodectiformes) - A new visit inside the ichthyodectid long-bodied, with a dorsal fin shifted backward to near phylogeny. In: STEURBAUT, E., JAGT, J.W.M. & JAGT-YAZYKOVA, E.A. (Editors), Annie V. Dhondt Memorial Volume. Bulletin de the tail, opposite to the anal fin, and with a protruded l’Institut royal des Sciences naturelles de Belgique, Sciences de lower jaw, which led to their nickname of “bull-dog” la Terre, 78: 209-228, 10 figs, 1 table, Brussels, October 31, 2008 fishes (Fig. 1). These fishes, the size of which ranged – ISSN 0374-6291. from a few centimetres to almost six meters, were among the major predators within the Cretaceous marine fish communities, as shown by their frequently enlarged dentition. In the floor of the nasal fossa they Abstract possess a very peculiar endochondral bone, the latero- basal ethmoid (= ethmopalatine), not present in other The author describes briefly the osteology of the three valid species of the Late Cretaceous genus Chirocentrites. He shows that only teleosts, except in their osteoglossomorph close allies, the type species, C.
    [Show full text]
  • I Exploring the Relationship Between Paleobiogeography, Deep-Diving
    Exploring the Relationship between Paleobiogeography, Deep-Diving Behavior, and Size Variation of the Parietal Eye in Mosasaurs By Andrew M. Connolly Submitted to the graduate degree program in Geology and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Master of Arts. __________________________________ Stephen T. Hasiotis, Chairperson __________________________________ Rafe M. Brown __________________________________ Jennifer A. Roberts Date Defended: March 25, 2016 i The Thesis Committee for Andrew M. Connolly certifies that this is the approved version of the following thesis: Exploring the Relationship between Paleobiogeography, Deep-Diving Behavior, and Size Variation of the Parietal Eye in Mosasaurs __________________________________ Stephen T. Hasiotis, Chairperson Date Approved: March 25, 2016 ii ABSTRACT Andrew M. Connolly, M.S. Department of Geology, March 2015 University of Kansas The parietal eye (PE) in modern squamates (Reptilia) plays a major role in regulating body temperature, maintaining circadian rhythms, and orientation via the solar axis. This study is the first to determine the role, if any, of the PE in an extinct group of lizards. We analyzed variation in relative size of the parietal foramen (PF) of five mosasaur genera to explore the relationship between PF size and paleolatitudinal distribution. We also surveyed the same specimens for the presence of avascular necrosis—a result of deep- diving behavior—in the vertebrae. Plioplatecarpus had the largest PF followed by Platecarpus, Tylosaurus, Mosasaurus, and Clidastes. A weak relationship exists between paleolatitudinal distribution and PF size among genera, as Plioplatecarpus had the highest paleolatitudinal distribution (~78°N) and the largest PF among genera.
    [Show full text]
  • New Material and Phylogenetic Position of Aidachar Paludalis Nesov, 1981 (Actinopterygii, Ichthyodectiformes) from the Late Cretaceous of Uzbekistan
    Proceedings of the Zoological Institute RAS Vol. 315, No. 2, 2011, рр. 181–192 УДК 567.5 NEW MATERIAL AND PHYLOGENETIC POSITION OF AIDACHAR PALUDALIS NESOV, 1981 (ACTINOPTERYGII, ICHTHYODECTIFORMES) FROM THE LATE CRETACEOUS OF UZBEKISTAN T.G. Mkhitaryan1 and A.O. Averianov2* 1Department of Vertebrate Zoology, Faculty of Biology and Soil Sciences, Saint Petersburg State University, Universitetskaya Emb. 7/9, 199034 Saint Petersburg, Russia; e-mail: [email protected] 2Zoological Institute of the Russian Academy of Sciences, Universitetskaya Emb. 1, 199034 Saint Petersburg, Russia; e-mail: [email protected] ABSTRACT Aidachar paludalis Nesov, 1981 from the Upper Cretaceous (Turonian) Bissekty Formation of Uzbekistan is referable to the teleost order Ichthyodectiformes by combination of the following diagnostic characters: large and massive intercalar, forming part of the hyomandibular facet and a canal for the jugular vein; deep premaxilla- maxilla attachment; deep dentary symphysis; angled coronoid process of the dentary; teeth forming a single series in the jaws. It shares a unique character with Aidachar pankowskii (Forey et Cavin, 2007), comb. nov., from the Cenomanian of Morocco: hyomandibular facet clearly divided into two parts. Key words: Aidachar, Ichthyodectiformes, Late Cretaceous, Uzbekistan НОВЫЙ МАТЕРИАЛ И ФИЛОГЕНЕТИЧЕСКОЕ ПОЛОЖЕНИЕ AIDACHAR PALUDALIS NESOV, 1981 (ACTINOPTERYGII, ICHTHYODECTIFORMES) ИЗ ПОЗДНЕГО МЕЛА УЗБЕКИСТАНА T.Г. Мхитарян1 и A.O. Аверьянов2* 1Кафедра зоологии позвоночных, Биолого-почвенный факультет,
    [Show full text]