A New Addition to the Cretaceous Seaway of ND
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Tylosaurus and Pteranodon
Tylosaurus and Pteranodon Estimate size and measure to check estimate. OBJECTIVES Students will: 1. identify the Tylosaurus and Pteranodon as the two state fossils of Kansas, and 2. estimate and check the wingspan of the Pteranodon or the length of the Tylosaurus. MATERIALS FROM THE TRUNK Tylosaurus model Pteranodon model Fossil sample OTHER MATERIALS Ruler or tape measure Masking tape, post-its or something similar to mark measurements on floor TEACHER PREPARATION Decide which of the two fossils you will measure: Pteranodon had a 25-foot wingspan or the Tylosaurus was 49 feet long. Identify a location with 50 linear feet of space that can be used to measure the wingspan of the Pteranodon or the length of the Tylosaurus. Consider using a hallway, playground, or gym. Once a location is identified, use a tape measure to mark the beginning and end of a 25-foot linear space and a 49-foot linear space. This is where the students will measure the two state fossils. HISTORICAL BACKGROUND In 2014 the Kansas Legislature passed a bill making the Tylosaurus and the Pteranodon the state fossils of Kansas. Both of these reptiles lived at the time of dinosaurs, but neither are dinosaurs. Mike Everhart, adjunct curator of paleontology at the Sternberg Museum, geologist Alan Deitrich, and Steven Fisher, a 4-H geology project member, testified in support of the bill. Fossil hunters and natural history museums initiated the adoption of these state fossils. Kansas 4-H geology project members supported the bill. Pteranodon (teh-RAN-oh-don) – “Pteranodon, a great, winged pterosaur with a wingspread of more than 24 feet, which flew the skies of Kansas during the cretaceous period of the mesozoic era, is hereby designated as the official flying fossil of the state Kansas Symbols Traveling Resource Trunk KANSAS HISTORICAL SOCIETY www.kshs.org ©2014 61 of Kansas.” (House Bill 2595) The first Pteranodon specimens discovered in North America were found in western Kansas in 1870 by Othniel Charles Marsh. -
Jason P. Schein
Curriculum Vitae JASON P. SCHEIN EXECUTIVE DIRECTOR BIGHORN BASIN PALEONTOLOGICAL INSTITUTE 3959 Welsh Road, Ste. 208 Willow Grove, Pennsylvania 19090 Office: (406) 998-1390 Cell: (610) 996-1055 [email protected] EDUCATION Ph.D. Student Drexel University, Department of Biology, Earth and Environmental Science, 2005-2013 M.Sc., Auburn University, Department of Geology and Geography, 2004 B.Sc., Auburn University, Department of Geology and Geography, 2000 RESEARCH AND PROFESSIONAL INTERESTS Mesozoic vertebrate marine and terrestrial faunas, paleoecology, paleobiogeography, faunistics, taphonomy, biostratigraphy, functional morphology, sedimentology, general natural history, education and outreach, paleontological resource assessment, and entrepreneurial academic paleontology. ACADEMIC, PROFESSIONAL, & BOARD POSITIONS 2019-Present Member of the Board, Yellowstone-Bighorn Research Association 2017-Present Founding Executive Director, Bighorn Basin Paleontological Institute 2017-Present Member of the Board, Delaware Valley Paleontological Society 2016-Present Scientific and Educational Consultant, Field Station: Dinosaurs 2015-Present Graduate Research Associate, Academy of Natural Sciences of Drexel University 2007-2017 Assistant Curator of Natural History Collections and Exhibits, New Jersey State Museum 2015-2017 Co-founder, Co-leader, Bighorn Basin Dinosaur Project 2010-2015 International Research Associate, Palaeontology Research Team, University of Manchester 2010-2014 Co-leader, New Jersey State Museum’s Paleontology Field Camp 2007-2009 Interim Assistant Curator of Natural History, New Jersey State Museum 2006-2007 Manager, Dinosaur Hall Fossil Preparation Laboratory 2004-2005 Staff Environmental Geologist, Cobb Environmental and Technical Services, Inc. 1 FIELD EXPERIENCE 2010-2019 Beartooth Butte, Morrison, Lance, and Fort Union formations, Bighorn Basin, Wyoming and Montana, U.S.A. (Devonian, Jurassic, Late Cretaceous, and earliest Paleocene, respectively) 2010 Hell Creek Formation, South Dakota, U.S.A. -
Mosasaurs Continuing from Last Time…
Pliosaurs and Mosasaurs Continuing From Last Time… • Pliosauridae: the big marine predators of the Jurassic Pliosauridae • Some of the largest marine predators of all time, these middle Jurassic sauropterygians include such giants as Kronosaurus, Liopleurodon, Macroplata, Peloneustes, Pliosaurus, and Brachauchenius Pliosaur Mophology • While the number of cervical vertebrae is less than in plesiosaurs, there is still variation: Macroplata (29) vs. Kronosaurus (13) Pliosaur Morphology • Larger pliosaurs adopted a more streamlined body shape, like modern whales, with a large skull and compact neck, and generally the hind limbs were larger than the front, while plesiosaurs had larger forelimbs Pliosaur Morphology • Powerful limb girdles and large (banana sized) conical teeth helped pliosaurs eat larger, quicker prey than the piscivorous plesiosaurs Liopleurodon • NOT 25 m long in general (average of 40 feet), though perhaps certain individuals could reach that size, making Liopleurodon ferox the largest carnivore to ever live • Recent skull studies indicate that Liopleurodon could sample water in stereo through nostrils, locating scents much as we locate sound Cretaceous Seas • Breakup of Gondwana causes large undersea mountain chains to form, raising sea levels everywhere • Shallow seas encourage growth of corals, which increases calcium abundance and chalk formation • Warm seas and a gentle thermal gradient yield a hospitable environment to rays, sharks, teleosts, and the first radiation of siliceous diatoms Kronosaurus • Early Cretaceous -
Allometric Growth in the Skull of Tylosaurus Proriger (Squamata: Mosasauridae) and Its Taxonomic Implications Robert F
Vertebrate Anatomy Morphology Palaeontology 6:75–90 75 ISSN 2292-1389 Allometric growth in the skull of Tylosaurus proriger (Squamata: Mosasauridae) and its taxonomic implications Robert F. Stewart1 and Jordan C. Mallon2,* 1Department of Earth Sciences, Carleton University, Ottawa, Ontario, Canada, K1S 5B6; [email protected] 2Palaeobiology, Canadian Museum of Nature, PO Box 3223, Station D, Ottawa, Ontario, Canada, K1P 6P4; [email protected] Abstract: Ontogeny—the growth and development of an organism—is among the more poorly understood aspects of the life history of mosasaurs, largely owing to a dearth of fossil material from young individuals. We describe the par- tial and nearly complete skulls of two subadult individuals of the mosasaurid Tylosaurus proriger from the upper Smoky Hills Chalk Member of the Niobrara Formation (upper Santonian) in Kansas. We include the more complete of the two specimens in an allometric analysis to better understand proportional changes in the skull through growth. Although our small sample size produces several instances of ‘soft isometry’, we recover the length of the edentulous rostrum as significantly negatively allometric, and quadrate height as significantly positively allometric. In light of our findings, we consider the question of whether T. kansasensis represents an immature ontogimorph of T. nepaeolicus, and find substan- tive evidence to reject this hypothesis. INTRODUCTION Seaway of North America (Williston 1898; Russell 1967; Everhart 2017). These are among the smallest skulls known Mosasauridae is a clade of carnivorous, mostly marine for the species, and they help to elucidate the allometric reptiles known from Upper Cretaceous deposits world- changes undergone by T. proriger through life. -
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. -
Educator Guide
Educator Guide BACKGROUND INFORMATION Welcome to the world of the late Cretaceous Period, filled with huge carnivorous marine reptiles with double-hinged jaws and teeth in the middle of their palates. Come see gigantic flesh-eating fish big enough to swallow an adult human being whole, flying reptiles with 3-foot skulls, and the biggest sea turtles to have ever lived. Many bizarre and gigantic forms of life populated the prehistoric waters of the late Cretaceous Period. The Midwest was actually underwater at one time. Kansas has only been above sea level for the last 65 million years. Before that, it was home to a variety of sea creatures, including a 45-foot long mosasaur, a sea turtle the size of a small truck, a giant carnivorous fish, and a long-necked plesiosaur. Although these prehistoric marine animals lived during the time of Tyrannosaurus and Triceratops, they are not dinosaurs. Dinosaurs lived on land and did not have wings for flying or fins for swimming. Many Cretaceous marine fossils have been found in Western Kansas. These fossils have been found in thousands of feet of marine sediments made up of shale, chalk, limestone, and sandstone. Common Questions When was the Cretaceous period? The Cretaceous Period extended from 144 to 65 million years ago. What is a mosasaur? A mosasaur is a large marine lizard with a long body and paddle-like limbs. Mosasaurs are not dinosaurs. The chief feature that distinguishes them from dinosaurs is the great flexibility and power of their jaws. Unlike most monstrous reptiles of the past, they still have living relatives, the giant monitor lizards such as the Komodo Dragons. -
Cretaceous Blog
A Quick Look at the Cretaceous World David Lillis – 13 May 2020 e-mail: [email protected] The Extent of the Cretaceous The Cretaceous Period began about 144 million years ago and terminated with the well- known asteroid impact some 66 million years ago. Geologists subdivide it into 12 stages, each defined by particular rock formations, fossils and sediments at a specific locality called the type area. Several of these type areas are located in France (e.g. Cognac, France, is the type area for the Coniacian Stage). These stages lasted for several million years each, and much geological, climatic and evolutionary change took place within each of them. Figure 1 gives the time frames of the twelve Cretaceous stages. Figure 1: The Cretaceous and its twelve stages The Cretaceous stages vary in duration but average somewhat less than seven million years. The Aptian stage has the greatest duration, at about 12 million years; while the shortest stage is the Santonian, at below three million years. The final stage is known as the Maastrichtian (approximately 6.1 million years in duration), the stage that ended with the famous asteroid impact and mass extinction of dinosaurs and other life forms. Significant rock formations or the earliest appearance of particular organisms define both the lower and upper boundaries of these stages. For example, one marker for the base of the Maastrichtrian is the earliest occurrence of a marine mollusc, the ammonite Pachydiscus fresvillensis. 1 Figure 2 shows a fossilised Pachydiscus fresvillensis from Madagascar, dated at about 69 million years. Figure 2: A Pachydiscus fresvillensis fossil, about 69 million years old The Cretaceous lies within the Mesozoic Era, which we can think of as the age of dinosaurs. -
(Chelonioidea: Cheloniidae) from the Maastrichtian of the Harrana Fauna–Jordan
Kaddumi, Gigantatypus salahi n.gen., n.sp., from Harrana www.PalArch.nl, vertebrate palaeontology, 3, 1, (2006) A new genus and species of gigantic marine turtles (Chelonioidea: Cheloniidae) from the Maastrichtian of the Harrana Fauna–Jordan H.F. Kaddumi Eternal River Museum of Natural History Amman–Jordan, P.O. Box 11395 [email protected] ISSN 1567–2158 7 figures Abstract Marine turtle fossils are extremely rare in the Muwaqqar Chalk Marl Formation of the Harrana Fauna in comparison to the relatively rich variety of other vertebrate fossils collected from this locality. This paper reports and describes the remains of an extinct marine turtle (Chelonioidea) which will be tentatively assigned to a new genus and species of marine turtles (Cheloniidae Bonaparte, 1835) Gigantatypus salahi n.gen., n.sp.. The new genus represented by a single well–preserved right humerus, reached remarkably large proportions equivalent to that of Archelon Wieland, 1896 and represents the first to be found from this deposit and from the Middle East. The specimen, which exhibits unique combinations of features is characterized by the following morphological features not found in other members of the Cheloniidae: massive species reaching over 12 feet in length; a more prominently enlarged lateral process that is situated more closely to the head; a ventrally situated capitellum; a highly laterally expanded distal margin. The presence of these features may warrant the placement of this new species in a new genus. The specimen also retains some morphological features found in members of advanced protostegids indicating close affinities with the family. Several bite marks on the ventral surface of the fossilized humerus indicate shark–scavenging activities of possibly Squalicorax spp. -
The Tylosaurine Mosasaurs (Reptilia, Mosasauridae) from the Upper Cretaceous of Europe and Africa
BULLETIN DE L'INSTITUT ROYAL DES SCIENCES NATURELLES DE BELGIQUE, SCIENCES DE LA TERRE, 62: 171-194, 1992 BULLETIN VAN H ET KONINKLIJK BELGISCH INSTITUT VOOR NATUURWETENSCH APPEN, AARDWETENSCHAPPEN, 62: 171-194, 1992 The Tylosaurine Mosasaurs (Reptilia, Mosasauridae) from the Upper Cretaceous of Europe and Africa by THEAGARTEN LINGHAM-SOLIAR Abstract La biomécanique du crâne des tylosauriens est examinée principale• ment suite à l'hypothèse selon laquelle le grand rostre servait à atta• quer les proies (RUSSELL, 1967). Divers autres aspects du comporte• This study represents the first relatively extensive description of the ment prédateur des tylosauriens sont aussi mentionnés. PUUM Hainosaurus Dono, 1885. The description of H. bernardi DOLLO, 1885 is based on the holotype and on a previously undescri- Mots-clefs: Hainosaurus, Tylosaurus, Leiodon, prédation, plongée. bed specimen. A new specimen of H. gaudryi (THEVENIN, 1896) from France is also described. Mosasaurus iembeensis TELLES-ANTUNES, 1964, from the Turonian of Angola is reassigned to the genus Tylosau• rus MARSH, 1872. The only other tylosaurine species from Africa, T. Introduction capensis (BROOM, 1912) is also briefly described. The biomechanics of the skull of tylosaurines is examined primarily The gigantic tylosaurine Hainosaurus bernardi DOLLO, because of the hypothesis that the large rostrum was used in ramming 1885 was the first mosasaur to be discovered in Belgium. prey (RUSSELL, 1967). Various other aspects of tylosaurine predatory behaviour are also mentioned. Almost the entire skeleton was found intact, although considerably abraded, in the Ciply Phosphatic Chalk in Key-words: Hainosaurus, Tylosaurus, Leiodon, ramming, ambush- a region known as "La Malogne" (Fig.l). -
A Mosasaur from the Lewis Shale
(1974)recently reported a number of ammo- nites and other invertebratesfrom the Lewis A mosasaurfrom the Lewis Shale Shale along the easternedge of the San Juan Basin. UNM-V-070 is southeastof their lo- (UpperGretaceous), northwestern cality D4l5l and northeastof their locality D5067. Both D4l5l and D5087 are strati- graphically higher in the Lewis Shale than NewMexico Uf.ftU-V-OZOand are placed by Cobban and History,Yale University' others (1974) in the Late Campanian Didy- by'NewHaven,CT,andPeterK.Reser,OiiartmentotAnthropology,University0fNewMexico,Albuquerque,NMSpencer G Lucas,Department of Geology and Geophysics and Peabody Museum of Natural mocerascheyennense ammonite zone. Prob- ably UNM-V-070 is Late Campanianin age (no older strata are known in the Lewis Shale) Mosasaursare an extinct group of giant The following abbreviationsare usedin the (Cobban and others, 1974)and older than the a marinelizards that flourishedduring the Late text: AMNH-Department of VertebratePa- D. cheyennense zone. Unfortunately, out- Cretaceous. Their fossilized remains are leontology, American Museum of Natural diligent searchof the limited Lewis Shale yielded un- known from all the continentsexcept Antarc- History, New York; UNM-Department of crops around UNM-V-070 only tica; the largestand best known collections Geology,University of New Mexico, Albu- diagnostic fragments of inoceramid shells; precisely come from the Niobrara Formation in Kan- querque;YPM-Peabody Museumof Natural hence,its age cannot be more deter- sas. Although marine sediments of Late History,Yale University, New Haven. mined. cretaceousage are exposedthroughout large areas of New Mexico, only three mosasaur LewisShale and its fauna specimenshave previously been reported from The Lewis Shale was named by Cross and the state. -
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. -
Kansas University Quarterly
r'S.i \:t*^ 7/ jr>?^^^ mm„'^:^^'::n >v<V i^i^M^ f-.v#:v;:^M' 1^ HARVARD UNIVERSITY. LIBRARY OF THE MUSEUM OF COMPARATIVE ZOOLOGY. i2MrIMS ,]LoikAlS ^"t^mmiitJLU.l'i^^ THE Kansas University Quarterly. DEVOTED TO THE PUBLICATION OF THE RESULTS OF RESEARCH BY MEMBERS OF THE UNIVERSITY OF KANSAS. SERIES A.— SCIENCE AND MATHEMATICS. VOL. VIII LAWRENCE, KANSAS: PUBLISHED BY THE UNIVERSITY. 1899. COMMITTEE OF PUBLICATION. E. H. S. BAILEY. F. W. BLACKMAR. E. MILLER. C. G. DUNLAP. H. B. NEWSON. S. W. WILLISTON. W. H. CARRUTH, Managing Editor.. FEB 15 1902 Kansas University Quarterly. Volume YIII. 1899. Series A. TABLE OF CONTENTS. JVo. 1. PAGE The Coccid.e of Kansas, i>. J. Hunier 1 The Characters or Bison occidentalis, the Fossil Bison of Kansas and Alaska, F. A . Lucas 17 A Preliminary Description of the Opercular and Other Cranial Bones OF XiPHACTiNus Leidy, Alhan Stewart 19 Diphtheria in Kansas, Marshall A . Barber 23 Pachyrhizodus minimus, a New Species of Fish from the Cretaceous of Kansas, Alban Stetcart 37 Some Additional Characters of the Mosasaurs, .S'. W. WilUston 39 JVo. S. The Five Types of Transformations of the Plane, Henry B. Nevson . 43 The Coccid.e of Kansas, II, S. J. Hunter 67 Description of Some New Forms of Pseudomonotis from the Upper Coal Measures of Kansas, J. W. Becde 79 Note on the Yellow Helium Line, A. St. C. Dunstan and M. E. Rice. 85 Some Additions to the Cretaceous Invertebrates of Kansas, W. X. Logan 87 On Tetracaulodon shepardii Cope, George Wagner 99 CuPRO GOSLARiTE, A New Variety OF ZiNC SuLPHATE, Austiu F.