The Lepidosaurian Reptile Champsosaurus in North America

Total Page:16

File Type:pdf, Size:1020Kb

The Lepidosaurian Reptile Champsosaurus in North America Photograph bJ, fames Wagoner. LIFE RESTORATION OF CHAMPSOSAURUS HUNTING. Painting by J erome Connolly in The Science Museum of Minnesota. THE LEPIDOSAURIAN REPTILE CHAMPSOSAURUS IN NORTH AMERICA BRUCE R. ERICKSON CURATOR OF PALEONTOLOGY MONOGRAPH VOLUME 1: PALEONTOLOGY Published by THE SCIENCE MUSEUM OF MINNESOTA ST. PAUL: March 31, 1972 MONOGRAPH OF THE SCIENCE MUSEUM OF MINNESOTA VOLUME 1 Library of Congress Catalog Card Number 77-186470 Standard Boole Number 911338-78-0 CONTENTS Page Illustrations ......................................... 2 Introduction ................................................. 5 Species of Champsosaurus . 7 Skull of Cha;rnpsosauru.s gigas, New Species. 12 Postcranial Skeleton of Champsosaurus gigas, New Species ... 26 General Morphology . 52 Skull ................................................... 52 Postcranial Skeleton . 53 Some Aspects of Functional Morphology . 72 Responsive Functions . 75 Correlations and Distribution. 82 Phylogeny . 86 Summary ................................................... 89 Bibliography . 90 ILLUSTRATIONS FIGURES Page 1. Correlation Chart of Champsosaurs. 9 2. Skull of Champsosaurus gigas, dorsal view, PU 16239. 13 3. Skull of Champsosaurus gigas, ventral view, PU 16239. 14 4. Skull of Champsosaurus gigas, dorsal view, PU 16240. 15 5. Skull of Champsosaurus gigas, ventral view, PU 16240. 16 6. Restoration of skull, C hampsosaurus gig as, dorsal view. 19 7. Restoration of skull, Champsosaurus gigas, ventral view. 22 8. Occipital region of skull, Cha.mpsosaurus gigas. 23 9. Lateral view of mandible, Champsosaurus gigas. 25 10. Cervical vertebrae, Champsosa.urus gigas. 27 11. Pleurocentrum of atlas, Champsosaurus gigas. 28 12. Hypocentrum of atlas, Champsosaurus gigas. 28 13. Posterior cervical centrum, Champsosaurus gigas. 29 14. Intercentrum of cervical vertebra, Chmnpsosaurus gigas. 29 15. Dorsal vertebra, Champsosaurus gigas. 30 16. Sacrum, lateral view, Champsosaurus gigas. 32 17. Sacrum, dorsal view, Champsosaurus gigas. 33 18. Large sacral vertebra, Champsosaurus gigas. 33 19. Representative caudal vertebrae, Champsosaut·us gigas. 34 20. Second caudal vertebra, Champsosaurus gigas. 34 21. Typical chevrons, Champsosaurus gigas. 35 22. Cervical rib of Champsosaurus lara.miensis. 36 23. Dorsal rib with uncinate process, Champsosaurus gigas. 36 24. Posterior dorsal rib, Champsosaurus gigas. 37 25. First sacral rib and vertebra, Champsosa.urus gi_qas. 38 26. Second sacral rib, Champsosaurus gigas. 38 27. First caudals, Charnpsosaurus gigas. 38 28. First caudal, Charnpsosaurus gigas. 39 29. Scapula, Charnpsosaurus gigas. 39 30. Coracoid, Champsosaurus gigas. 40 31. Shoulder girdle, anterior view, Champsosaurus gigas. 42 32. Clavicle, dorsal view1 Champsosaurus gigas . ..................... 43 33. Interclavicle, dorsal view, Champsosaurus gigas . ................. 44 2 ILLUSTRATIONS Page 34. Humerus, Champsosaurus gigas . .............................. 45 35. Radius, Champsosauna; gigas . ................................ 46 36. Foreleg, Champsosaurus gigas . ..................... , , ....... , .. 46 37. Ilium, Champsosaurus gigas . ........... , ........... , ........ , . , 47 38. Ventral plates of pelvis, Champsosaurus gigas . , ............ , . , . , . 47 39. Femur, Chanipsosaurus gigas . ................................. 48 40. Tibia-fibula, Champsosaurus gigas . .. , ... , ..... , ... , ............ 49 41. Astragalus, Champsosaurus ,(Jigas . ............. , ............... 49 42. Metatarsal V, Champsosa·urus gigas . ........... , ............. , .. 49 43. Gastralia, Champsosaurus gigas . .............................. , 49 44. Age variation in axis pleurocentra . ............................ 56 45. Juvenile cervical vertebrae....... , ...... , ........... , ......... 56 46. Cervical vertebra, Chanipsosaurus lara1niensis . ................... 57 47. Mounted skeleton of Champsosaurus laramieusis. , ... , , ... , ...... , 59 48. Juvenile sacrum, Chanipsosaurus laraniiensis . ................... 61 49. Coracoid, Champsosaurus natator . ............................. 63 50. Humeri of different species, Champsosaurus . .. , . , ....... , , , ..... 64 51. Ontogenetic development of humerus, Chamvsosaurus . ............ 65 52. Forefoot of Cha1npsosau-rus larwmiensis . ........................ 66 53. Forefoot of Champsosaurus laramiensis (in situ) ................. 66 54, Ontogenetic development of ilium, Charnpsosaurus . , , . , ......... , . 67 55. Pubis of Champsosaurus gigas . , .... , ......................... 68 56. Hind foot of Champsosaw·us laramiensis . ............................... 70 57, Diagrammatic posture of head ...... , ............ , , ...... , ............. , 74 58. Transverse section of rib cage, C ham,psosaurus gigas .............. 76 59, Restoration of lungs in Champsosaurus . ................... , .... 77 60. Cross section of rib shaft, Champsosaurus gigas ............ , , .... 78 61. Juvenile cross section of rib shaft, Chamvsosaurus laramiensis, .... 79 62. Adult cross section of rib shaft, Chamvsosaurus laramiensis . .. , .... 79 63. Map, Cretaceous distribution of Champsosaurus . ................. 84 64. Map, Tertiary distribution of Charnpsosaurus . .................. , . 85 65. Phylogenetic Chart ........................................ , .. 87 TABLES 1. Measurements of Chanipsosanrus gigas . ......................... 50 2. Comparison of adult and juvenile proportions in Champsosaurus . ... 54 3 INTRODUCTION Remains of the moderate-s,ized eosuchian features. Age and individual variations reptile, Champsosaurus, are common in have definite trends as well that have been many late Cretaceous and early Tertiary helpful in the present overall study. Age deposits of western North America and in variations, however, are much easier to the Tertiary of Europe; yet, they are poor­ determine than the latter, which must be ly represented in major museum collections regarded as only suggestive. and, by and large, not identified to specific Most informative of this group is a very level. The prime limiting factor responsi­ large form from the late Paleocene that is ble for the latter situation is the incom­ herein referred to as the new species, pleteness of materials and the extreme mor­ Champsosaurus gigas. In being very abun­ phological uniformity that runs through­ dant and fairly complete, it presents much out the group. interesting morphological evidence-some new and some in a better light; hence, the During the course of several seasons, discussions of general morphology and the writer made extensive collections of functional morphology draw heavily from fossil vertebrates in western North Amer­ it. ica. A sizable quantity of champsosaurian The present study treats Champsosau­ material was included in these collections. rus, the long-snouted North American Confusion in trying to work out the tax­ form. Only brief reference is made to onomy of this material provided the in­ other champsosaurids. In addition to the centive for the initiation of the present rather large sample of Champsosaurus now study, in The Science Museum of Minnesota, ma­ terials from seven other institutions were Handicaps encountered by most workers examined. Certain other materials, namely, have been due chiefly to inadequate sam­ those in the Royal Ontario Museum, were ples resulting in much synonymy. It was not examined but are referred to in the felt, however, that if enough material was present work. analyzed, specific taxonomy could be im­ proved upon. As comparisons were made, In the present work, the term "Clark­ characters that are considered significant forkian" is used rather than Tiffanian in delineating species were found. Many (Wood, 1967) to designate the late Paleo­ are subtle in expression, yet are consistent cene span from Olive to the Eocene boun­ in their occurrence. Due to the lack of dary. Figure 1 is a correlation chart for skulls, most distinctions rest on postcranial North American champsosaurs. 5 INTRODUCTION ACKNOWLEDGMENTS The writer is indebted to numerous per­ staff artists of The Science Museum of sons who have assisted with the present Minnesota, with all of whom I have en­ work. Sincere thanks are extended to joyed working. I am indebted, first of all, Drs. Donald Baird of Princeton University to the late Alexander Oja who was respon­ and Rainer Zangerl of the Field Museum sible for figures 11, 13, 18, 26, 41, and 55; of Natural History for their encourage­ second to Chief Artist, Paul Snyder, who ment and suggestions, as well as providing contributed figures 25, 30, 58, and sug­ the loan of specimens critical to this study. gestions on others; and especially to James Without the loan of other materials as Wagoner who contributed the bulk of the well, this project would have suffered. For illustrations: 6-9, 12, 14, 16, 17, 20, 21, the loan of additional specimens from the 23, 28, 29, 32, 33, 35, 38, 42, 44-46, 48-53, following respective institutions, I wish to 56, and all photographs except figure 47. thank Drs. David Dunkle, formerly of the The frontispiece was painted by Jerome United States National Museum; Robert Connolly. Maps and figures 54, 57, 59, 60, W. Wilson of the South Dakota School of and 65 are the work of the writer who also Mines and Technology; Robert E. Sloan accepts the responsibility for all omissions of the University of Minnesota; and Mr. and inaccuracies in this publication. Fred G. Bard, director of the Saskatche­ Messrs. Ray and Eugene Lingk are to wan Museum of Natural History, Regina. be commended for their diligent
Recommended publications
  • Six Adventure Road Trips
    Easy Drives, Big Fun, and Planning Tips Six Adventure Road Trips DAY HIKES, FLY-FISHING, SKIING, HISTORIC SITES, AND MUCH MORE A custom guidebook in partnership with Montana Offi ce of Tourism and Business Development and Outside Magazine Montana Contents is the perfect place for road tripping. There are 3 Glacier Country miles and miles of open roads. The landscape is stunning and varied. And its towns are welcoming 6 Roaming the National Forests and alluring, with imaginative hotels, restaurants, and breweries operated by friendly locals. 8 Montana’s Mountain Yellowstone and Glacier National Parks are Biking Paradise the crown jewels, but the Big Sky state is filled with hundreds of equally awesome playgrounds 10 in which to mountain bike, trail run, hike, raft, Gateways to Yellowstone fish, horseback ride, and learn about the region’s rich history, dating back to the days of the 14 The Beauty of Little dinosaurs. And that’s just in summer. Come Bighorn Country winter, the state turns into a wonderland. The skiing and snowboarding are world-class, and the 16 Exploring Missouri state offers up everything from snowshoeing River Country and cross-country skiing to snowmobiling and hot springs. Among Montana’s star attractions 18 Montana on Tap are ten national forests, hundreds of streams, tons of state parks, and historic monuments like 20 Adventure Base Camps Little Bighorn Battlefield and the Lewis and Clark National Historic Trail. Whether it’s a family- 22 friendly hike or a peaceful river trip, there’s an Montana in Winter experience that will recharge your spirit around every corner in Montana.
    [Show full text]
  • The Transition from the Judith River Formation to the Bearpaw Shale
    The transition from the Judith River Formation to the Bearpaw Shale (Campanian), north-central Montana by Roger Elmer Braun A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences Montana State University © Copyright by Roger Elmer Braun (1983) Abstract: The upper 15 m of the Judith River Formation on and adjacent to the Fort Belknap Indian Reservation, north-central Montana is composed mostly of overbank mudrock, siltstone, fine-grained sandstone, and coal, with some cross-stratified channel sandstone in the lower part. The lower 15 m of the overlying Bearpaw Shale is a transgressive deposit composed primarily of concretionary silty shale with some clayey, silty sandstone zones and one bentonite bed. The source area for both formations was primarily in western Montana and Idaho, with the Elkhorn Mountains volcanics a major source of debris. The contact between the Judith River and Bearpaw formations is abrupt and lacks a transgressive sandstone facies. The transgression of the Bearpaw sea across the study area is considered to have been a nearly isochronous event because of the nature of the transition, small east-west differences in thickness between marker horizons, and similar elevations of the contact from east to west across undeformed parts of the study area. The Bearpaw transgression was caused mainly by tectonic thickening in the western Cordillera, which created subsidence primarily in the western and central portions of the Western Interior basin. The transgression was a nearly isochronous event that took place approximately 72 m.y. ago according to radiometric age dates on bentonite beds.
    [Show full text]
  • Compilation of Reported Sapphire Occurrences in Montana
    Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area ....................................
    [Show full text]
  • HOVASAURUS BOULEI, an AQUATIC EOSUCHIAN from the UPPER PERMIAN of MADAGASCAR by P.J
    99 Palaeont. afr., 24 (1981) HOVASAURUS BOULEI, AN AQUATIC EOSUCHIAN FROM THE UPPER PERMIAN OF MADAGASCAR by P.J. Currie Provincial Museum ofAlberta, Edmonton, Alberta, T5N OM6, Canada ABSTRACT HovasauTUs is the most specialized of four known genera of tangasaurid eosuchians, and is the most common vertebrate recovered from the Lower Sakamena Formation (Upper Per­ mian, Dzulfia n Standard Stage) of Madagascar. The tail is more than double the snout-vent length, and would have been used as a powerful swimming appendage. Ribs are pachyostotic in large animals. The pectoral girdle is low, but massively developed ventrally. The front limb would have been used for swimming and for direction control when swimming. Copious amounts of pebbles were swallowed for ballast. The hind limbs would have been efficient for terrestrial locomotion at maturity. The presence of long growth series for Ho vasaurus and the more terrestrial tan~saurid ThadeosauTUs presents a unique opportunity to study differences in growth strategies in two closely related Permian genera. At birth, the limbs were relatively much shorter in Ho vasaurus, but because of differences in growth rates, the limbs of Thadeosau­ rus are relatively shorter at maturity. It is suggested that immature specimens of Ho vasauTUs spent most of their time in the water, whereas adults spent more time on land for mating, lay­ ing eggs and/or range dispersal. Specilizations in the vertebrae and carpus indicate close re­ lationship between Youngina and the tangasaurids, but eliminate tangasaurids from consider­ ation as ancestors of other aquatic eosuchians, archosaurs or sauropterygians. CONTENTS Page ABREVIATIONS . ..... ... ......... .......... ... ......... ..... ... ..... .. .... 101 INTRODUCTION .
    [Show full text]
  • The First Possible Choristoderan Trackway from the Lower
    www.nature.com/scientificreports OPEN The frst possible choristoderan trackway from the Lower Cretaceous Daegu Formation of South Korea and its implications on choristoderan locomotion Yuong‑Nam Lee1*, Dal‑Yong Kong2 & Seung‑Ho Jung2 Here we report a new quadrupedal trackway found in the Lower Cretaceous Daegu Formation (Albian) in the vicinity of Ulsan Metropolitan City, South Korea, in 2018. A total of nine manus‑pes imprints show a strong heteropodous quadrupedal trackway (length ratio is 1:3.36). Both manus and pes tracks are pentadactyl with claw marks. The manus prints rotate distinctly outward while the pes prints are nearly parallel to the direction of travel. The functional axis in manus and pes imprints suggests that the trackmaker moved along the medial side during the stroke progressions (entaxonic), indicating weight support on the inner side of the limbs. There is an indication of webbing between the pedal digits. These new tracks are assigned to Novapes ulsanensis, n. ichnogen., n. ichnosp., which are well‑matched not only with foot skeletons and body size of Monjurosuchus but also the fossil record of choristoderes in East Asia, thereby N. ulsanensis could be made by a monjurosuchid‑like choristoderan and represent the frst possible choristoderan trackway from Asia. N. ulsanensis also suggests that semi‑aquatic choristoderans were capable of walking semi‑erect when moving on the ground with a similar locomotion pattern to that of crocodilians on land. South Korea has become globally famous for various tetrapod footprints from Cretaceous strata1, among which some clades such as frogs2, birds3 and mammals4 have been proved for their existences only with ichnological evidence.
    [Show full text]
  • (Diapsida: Saurosphargidae), with Implications for the Morphological Diversity and Phylogeny of the Group
    Geol. Mag.: page 1 of 21. c Cambridge University Press 2013 1 doi:10.1017/S001675681300023X A new species of Largocephalosaurus (Diapsida: Saurosphargidae), with implications for the morphological diversity and phylogeny of the group ∗ CHUN LI †, DA-YONG JIANG‡, LONG CHENG§, XIAO-CHUN WU†¶ & OLIVIER RIEPPEL ∗ Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, PO Box 643, Beijing 100044, China ‡Department of Geology and Geological Museum, Peking University, Beijing 100871, PR China §Wuhan Institute of Geology and Mineral Resources, Wuhan, 430223, PR China ¶Canadian Museum of Nature, PO Box 3443, STN ‘D’, Ottawa, ON K1P 6P4, Canada Department of Geology, The Field Museum, 1400 S. Lake Shore Drive, Chicago, IL 60605-2496, USA (Received 31 July 2012; accepted 25 February 2013) Abstract – Largocephalosaurus polycarpon Cheng et al. 2012a was erected after the study of the skull and some parts of a skeleton and considered to be an eosauropterygian. Here we describe a new species of the genus, Largocephalosaurus qianensis, based on three specimens. The new species provides many anatomical details which were described only briefly or not at all in the type species, and clearly indicates that Largocephalosaurus is a saurosphargid. It differs from the type species mainly in having three premaxillary teeth, a very short retroarticular process, a large pineal foramen, two sacral vertebrae, and elongated small granular osteoderms mixed with some large ones along the lateral most side of the body. With additional information from the new species, we revise the diagnosis and the phylogenetic relationships of Largocephalosaurus and clarify a set of diagnostic features for the Saurosphargidae Li et al.
    [Show full text]
  • Montana State Parks Guide Reservations for Camping and Other Accommodations: Toll Free: 1-855-922-6768 Stateparks.Mt.Gov
    For more information about Montana State Parks: 406-444-3750 TDD: 406-444-1200 website: stateparks.mt.gov P.O. Box 200701 • Helena, MT 59620-0701 Montana State Parks Guide Reservations for camping and other accommodations: Toll Free: 1-855-922-6768 stateparks.mt.gov For general travel information: 1-800-VISIT-MT (1-800-847-4868) www.visitmt.com Join us on Twitter, Facebook & Instagram If you need emergency assistance, call 911. To report vandalism or other park violations, call 1-800-TIP-MONT (1-800-847-6668). Your call can be anonymous. You may be eligible for a reward. Montana Fish, Wildlife & Parks strives to ensure its programs, sites and facilities are accessible to all people, including those with disabilities. To learn more, or to request accommodations, call 406-444-3750. Cover photo by Jason Savage Photography Lewis and Clark portrait reproductions courtesy of Independence National Historic Park Library, Philadelphia, PA. This document was produced by Montana Fish Wildlife & Parks and was printed at state expense. Information on the cost of this publication can be obtained by contacting Montana State Parks. Printed on Recycled Paper © 2018 Montana State Parks MSP Brochure Cover 15.indd 1 7/13/2018 9:40:43 AM 1 Whitefish Lake 6 15 24 33 First Peoples Buffalo Jump* 42 Tongue River Reservoir Logan BeTableaverta ilof Hill Contents Lewis & Clark Caverns Les Mason* 7 16 25 34 43 Thompson Falls Fort3-9 Owen*Historical Sites 28. VisitorMadison Centers, Buff Camping,alo Ju mp* Giant Springs* Medicine Rocks Whitefish Lake 8 Fish Creek 17 Granite11-15 *Nature Parks 26DisabledMissouri Access Headw ibility aters 35 Ackley Lake 44 Pirogue Island* WATERTON-GLACIER INTERNATIONAL 2 Lone Pine* PEACE PARK9 Council Grove* 18 Lost Creek 27 Elkhorn* 36 Greycliff Prairie Dog Town* 45 Makoshika Y a WHITEFISH < 16-23 Water-based Recreation 29.
    [Show full text]
  • A Revision of the Ceratopsia Or Horned Dinosaurs
    MEMOIRS OF THE PEABODY MUSEUM OF NATURAL HISTORY VOLUME III, 1 A.R1 A REVISION orf tneth< CERATOPSIA OR HORNED DINOSAURS BY RICHARD SWANN LULL STERLING PROFESSOR OF PALEONTOLOGY AND DIRECTOR OF PEABODY MUSEUM, YALE UNIVERSITY LVXET NEW HAVEN, CONN. *933 MEMOIRS OF THE PEABODY MUSEUM OF NATURAL HISTORY YALE UNIVERSITY Volume I. Odontornithes: A Monograph on the Extinct Toothed Birds of North America. By Othniel Charles Marsh. Pp. i-ix, 1-201, pis. 1-34, text figs. 1-40. 1880. To be obtained from the Peabody Museum. Price $3. Volume II. Part 1. Brachiospongidae : A Memoir on a Group of Silurian Sponges. By Charles Emerson Beecher. Pp. 1-28, pis. 1-6, text figs. 1-4. 1889. To be obtained from the Peabody Museum. Price $1. Volume III. Part 1. American Mesozoic Mammalia. By George Gaylord Simp- son. Pp. i-xvi, 1-171, pis. 1-32, text figs. 1-62. 1929. To be obtained from the Yale University Press, New Haven, Conn. Price $5. Part 2. A Remarkable Ground Sloth. By Richard Swann Lull. Pp. i-x, 1-20, pis. 1-9, text figs. 1-3. 1929. To be obtained from the Yale University Press, New Haven, Conn. Price $1. Part 3. A Revision of the Ceratopsia or Horned Dinosaurs. By Richard Swann Lull. Pp. i-xii, 1-175, pis. I-XVII, text figs. 1-42. 1933. To be obtained from the Peabody Museum. Price $5 (bound in cloth), $4 (bound in paper). Part 4. The Merycoidodontidae, an Extinct Group of Ruminant Mammals. By Malcolm Rutherford Thorpe. In preparation.
    [Show full text]
  • A Small Lepidosauromorph Reptile from the Early Triassic of Poland
    A SMALL LEPIDOSAUROMORPH REPTILE FROM THE EARLY TRIASSIC OF POLAND SUSAN E. EVANS and MAGDALENA BORSUK−BIAŁYNICKA Evans, S.E. and Borsuk−Białynicka, M. 2009. A small lepidosauromorph reptile from the Early Triassic of Poland. Palaeontologia Polonica 65, 179–202. The Early Triassic karst deposits of Czatkowice quarry near Kraków, southern Poland, has yielded a diversity of fish, amphibians and small reptiles. Two of these reptiles are lepido− sauromorphs, a group otherwise very poorly represented in the Triassic record. The smaller of them, Sophineta cracoviensis gen. et sp. n., is described here. In Sophineta the unspecial− ised vertebral column is associated with the fairly derived skull structure, including the tall facial process of the maxilla, reduced lacrimal, and pleurodonty, that all resemble those of early crown−group lepidosaurs rather then stem−taxa. Cladistic analysis places this new ge− nus as the sister group of Lepidosauria, displacing the relictual Middle Jurassic genus Marmoretta and bringing the origins of Lepidosauria closer to a realistic time frame. Key words: Reptilia, Lepidosauria, Triassic, phylogeny, Czatkowice, Poland. Susan E. Evans [[email protected]], Department of Cell and Developmental Biology, Uni− versity College London, Gower Street, London, WC1E 6BT, UK. Magdalena Borsuk−Białynicka [[email protected]], Institut Paleobiologii PAN, Twarda 51/55, PL−00−818 Warszawa, Poland. Received 8 March 2006, accepted 9 January 2007 180 SUSAN E. EVANS and MAGDALENA BORSUK−BIAŁYNICKA INTRODUCTION Amongst living reptiles, lepidosaurs (snakes, lizards, amphisbaenians, and tuatara) form the largest and most successful group with more than 7 000 widely distributed species. The two main lepidosaurian clades are Rhynchocephalia (the living Sphenodon and its extinct relatives) and Squamata (lizards, snakes and amphisbaenians).
    [Show full text]
  • 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.
    [Show full text]
  • Judith Basin River Ranch
    JUDITH BASIN RIVER RANCH Judith Basin River Ranch Moccasin, Montana $745,000. Offered Exclusively By: Sonny Todd Real Estate 301 W First, PO Box 788 Big Timber, MT 59011 Office: (406) 932-6668 (406) 932-LAND Toll Free: 1-866-932-1031 Fax: (406) 932-4838 [email protected] www.sonnytoddrealestate.com Judith Basin River Ranch AGENTS NOTE: The JUDITH BASIN RIVER RANCH is right on the Judith River and exhibits a stunning over- look of the river with the Snowy Mountains as a spectacular backdrop. Step out on the deck over the river and look to the east to the Moccasin and Judith Mountains, south to view the Snowy-es, west to the Little Belts and NW to the Highwoods and Square Butte. This ranch is located at the end of a county road with no drive by traffic, yet only 20 minutes into nearby Lewistown including a modern hospital, an hour and a half from airplane connections in Great Falls, or just over 2 hours to Billings or Bozeman’s services. The home has three bedrooms with two baths, a large sewing room, great room and kitchen looking down on the river. Cen- tral air cools the home. Also, a convenient additional bath with attached garage. In addition, included is a simple guest cottage, plus a horse barn with an attached additional garage. Along the driveway coming in to the house you cross your own private spring feed fishing pond. Additional springs provide the home with an endless source of fresh drinking water. Bob Noel Justin Todd (406) 261-4474 (406) 223-5263 HORSE BARN DESCRIPTION: Acreage: 160+/- acres Elevation: 3,963’ Utilities: Power and telephone.
    [Show full text]
  • Reptile Family Tree - Peters 2017 1112 Taxa, 231 Characters
    Reptile Family Tree - Peters 2017 1112 taxa, 231 characters Note: This tree does not support DNA topologies over 100 Eldeceeon 1990.7.1 67 Eldeceeon holotype long phylogenetic distances. 100 91 Romeriscus Diplovertebron Certain dental traits are convergent and do not define clades. 85 67 Solenodonsaurus 100 Chroniosaurus 94 Chroniosaurus PIN3585/124 Chroniosuchus 58 94 Westlothiana Casineria 84 Brouffia 93 77 Coelostegus Cheirolepis Paleothyris Eusthenopteron 91 Hylonomus Gogonasus 78 66 Anthracodromeus 99 Osteolepis 91 Protorothyris MCZ1532 85 Protorothyris CM 8617 81 Pholidogaster Protorothyris MCZ 2149 97 Colosteus 87 80 Vaughnictis Elliotsmithia Apsisaurus Panderichthys 51 Tiktaalik 86 Aerosaurus Varanops Greererpeton 67 90 94 Varanodon 76 97 Koilops <50 Spathicephalus Varanosaurus FMNH PR 1760 Trimerorhachis 62 84 Varanosaurus BSPHM 1901 XV20 Archaeothyris 91 Dvinosaurus 89 Ophiacodon 91 Acroplous 67 <50 82 99 Batrachosuchus Haptodus 93 Gerrothorax 97 82 Secodontosaurus Neldasaurus 85 76 100 Dimetrodon 84 95 Trematosaurus 97 Sphenacodon 78 Metoposaurus Ianthodon 55 Rhineceps 85 Edaphosaurus 85 96 99 Parotosuchus 80 82 Ianthasaurus 91 Wantzosaurus Glaucosaurus Trematosaurus long rostrum Cutleria 99 Pederpes Stenocybus 95 Whatcheeria 62 94 Ossinodus IVPP V18117 Crassigyrinus 87 62 71 Kenyasaurus 100 Acanthostega 94 52 Deltaherpeton 82 Galechirus 90 MGUH-VP-8160 63 Ventastega 52 Suminia 100 Baphetes Venjukovia 65 97 83 Ichthyostega Megalocephalus Eodicynodon 80 94 60 Proterogyrinus 99 Sclerocephalus smns90055 100 Dicynodon 74 Eoherpeton
    [Show full text]