Prehistoric "Sea Monsters" of North Dakota John W
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Vertebral Morphology, Dentition, Age, Growth, and Ecology of the Large Lamniform Shark Cardabiodon Ricki
Vertebral morphology, dentition, age, growth, and ecology of the large lamniform shark Cardabiodon ricki MICHAEL G. NEWBREY, MIKAEL SIVERSSON, TODD D. COOK, ALLISON M. FOTHERINGHAM, and REBECCA L. SANCHEZ Newbrey, M.G., Siversson, M., Cook, T.D., Fotheringham, A.M., and Sanchez, R.L. 2015. Vertebral morphology, denti- tion, age, growth, and ecology of the large lamniform shark Cardabiodon ricki. Acta Palaeontologica Polonica 60 (4): 877–897. Cardabiodon ricki and Cardabiodon venator were large lamniform sharks with a patchy but global distribution in the Cenomanian and Turonian. Their teeth are generally rare and skeletal elements are less common. The centra of Cardabiodon ricki can be distinguished from those of other lamniforms by their unique combination of characteristics: medium length, round articulating outline with a very thick corpus calcareum, a corpus calcareum with a laterally flat rim, robust radial lamellae, thick radial lamellae that occur in low density, concentric lamellae absent, small circular or subovate pores concentrated next to each corpus calcareum, and papillose circular ridges on the surface of the corpus calcareum. The large diameter and robustness of the centra of two examined specimens suggest that Cardabiodon was large, had a rigid vertebral column, and was a fast swimmer. The sectioned corpora calcarea show both individuals deposited 13 bands (assumed to represent annual increments) after the birth ring. The identification of the birth ring is supported in the holotype of Cardabiodon ricki as the back-calculated tooth size at age 0 is nearly equal to the size of the smallest known isolated tooth of this species. The birth ring size (5–6.6 mm radial distance [RD]) overlaps with that of Archaeolamna kopingensis (5.4 mm RD) and the range of variation of Cretoxyrhina mantelli (6–11.6 mm RD) from the Smoky Hill Chalk, Niobrara Formation. -
Sea Monsters and Real Environmental Threats: Reconsidering the Famous Osborne, ‘Moha-Moha’, Valhalla, and ‘Soay Beast’ Sightings of Unidentified Marine Objects
IMAGINARY SEA MONSTERS AND REAL ENVIRONMENTAL THREATS: RECONSIDERING THE FAMOUS OSBORNE, ‘MOHA-MOHA’, VALHALLA, AND ‘SOAY BEAST’ SIGHTINGS OF UNIDENTIFIED MARINE OBJECTS R. L. FRANCE Dal Ocean Research Group Department of Plant, Food, and Environmental Sciences, Dalhousie University Abstract At one time, largely but not exclusively during the nineteenth century, retellings of encounters with sea monsters were a mainstay of dockside conversations among mariners, press reportage for an audience of fascinated landlubbers, and journal articles published by believing or sceptical natural scientists. Today, to the increasing frustration of cryptozoologists, mainstream biologists and environmental historians have convincingly argued that there is a long history of conflating or misidentifying known sea animals as purported sea monsters. The present paper provides, for the first time, a detailed, diachronic review of competing theories that have been posited to explain four particular encounters with sea monsters, which at the time of the sightings (1877, 1890, 1905, and 1959) had garnered worldwide attention and considerable fame. In so doing, insights are gleaned about the role played by sea monsters in the culture of late-Victorian natural science. Additionally, and most importantly, I offer my own parsimonious explanation that the observed ‘sea monsters’ may have been sea turtles entangled in pre-plastic fishing gear or maritime debris. Environmental history is therefore shown to be a valuable tool for looking backward in order to postulate the length of time that wildlife populations have been subjected to anthropogenic pressure. This is something of contemporary importance, given that scholars are currently involved in deliberations concerning the commencement date of the Anthropocene Era. -
Asteroid Impact, Not Volcanism, Caused the End-Cretaceous Dinosaur Extinction
Asteroid impact, not volcanism, caused the end-Cretaceous dinosaur extinction Alfio Alessandro Chiarenzaa,b,1,2, Alexander Farnsworthc,1, Philip D. Mannionb, Daniel J. Luntc, Paul J. Valdesc, Joanna V. Morgana, and Peter A. Allisona aDepartment of Earth Science and Engineering, Imperial College London, South Kensington, SW7 2AZ London, United Kingdom; bDepartment of Earth Sciences, University College London, WC1E 6BT London, United Kingdom; and cSchool of Geographical Sciences, University of Bristol, BS8 1TH Bristol, United Kingdom Edited by Nils Chr. Stenseth, University of Oslo, Oslo, Norway, and approved May 21, 2020 (received for review April 1, 2020) The Cretaceous/Paleogene mass extinction, 66 Ma, included the (17). However, the timing and size of each eruptive event are demise of non-avian dinosaurs. Intense debate has focused on the highly contentious in relation to the mass extinction event (8–10). relative roles of Deccan volcanism and the Chicxulub asteroid im- An asteroid, ∼10 km in diameter, impacted at Chicxulub, in pact as kill mechanisms for this event. Here, we combine fossil- the present-day Gulf of Mexico, 66 Ma (4, 18, 19), leaving a crater occurrence data with paleoclimate and habitat suitability models ∼180 to 200 km in diameter (Fig. 1A). This impactor struck car- to evaluate dinosaur habitability in the wake of various asteroid bonate and sulfate-rich sediments, leading to the ejection and impact and Deccan volcanism scenarios. Asteroid impact models global dispersal of large quantities of dust, ash, sulfur, and other generate a prolonged cold winter that suppresses potential global aerosols into the atmosphere (4, 18–20). These atmospheric dinosaur habitats. -
Papers in Press
Papers in Press “Papers in Press” includes peer-reviewed, accepted manuscripts of research articles, reviews, and short notes to be published in Paleontological Research. They have not yet been copy edited and/or formatted in the publication style of Paleontological Research. As soon as they are printed, they will be removed from this website. Please note they can be cited using the year of online publication and the DOI, as follows: Humblet, M. and Iryu, Y. 2014: Pleistocene coral assemblages on Irabu-jima, South Ryukyu Islands, Japan. Paleontological Research, doi: 10.2517/2014PR020. doi:10.2517/2018PR013 Features and paleoecological significance of the shark fauna from the Upper Cretaceous Hinoshima Formation, Himenoura Group, Southwest Japan Accepted Naoshi Kitamura 4-8-7 Motoyama, Chuo-ku Kumamoto, Kumamoto 860-0821, Japan (e-mail: [email protected]) Abstract. The shark fauna of the Upper Cretaceous Hinoshima Formation (Santonian: 86.3–83.6 Ma) of the manuscriptHimenoura Group (Kamiamakusa, Kumamoto Prefecture, Kyushu, Japan) was investigated based on fossil shark teeth found at five localities: Himedo Park, Kugushima, Wadanohana, Higashiura, and Kotorigoe. A detailed geological survey and taxonomic analysis was undertaken, and the habitat, depositional environment, and associated mollusks of each locality were considered in the context of previous studies. Twenty-one species, 15 genera, 11 families, and 6 orders of fossil sharks are recognized from the localities. This assemblage is more diverse than has previously been reported for Japan, and Lamniformes and Hexanchiformes were abundant. Three categories of shark fauna are recognized: a coastal region (Himedo Park; probably a breeding site), the coast to the open sea (Kugushima and Wadanohana), and bottom-dwelling or near-seafloor fauna (Kugushima, Wadanohana, Higashiura, and Kotorigoe). -
The Geologic Time Scale Is the Eon
Exploring Geologic Time Poster Illustrated Teacher's Guide #35-1145 Paper #35-1146 Laminated Background Geologic Time Scale Basics The history of the Earth covers a vast expanse of time, so scientists divide it into smaller sections that are associ- ated with particular events that have occurred in the past.The approximate time range of each time span is shown on the poster.The largest time span of the geologic time scale is the eon. It is an indefinitely long period of time that contains at least two eras. Geologic time is divided into two eons.The more ancient eon is called the Precambrian, and the more recent is the Phanerozoic. Each eon is subdivided into smaller spans called eras.The Precambrian eon is divided from most ancient into the Hadean era, Archean era, and Proterozoic era. See Figure 1. Precambrian Eon Proterozoic Era 2500 - 550 million years ago Archaean Era 3800 - 2500 million years ago Hadean Era 4600 - 3800 million years ago Figure 1. Eras of the Precambrian Eon Single-celled and simple multicelled organisms first developed during the Precambrian eon. There are many fos- sils from this time because the sea-dwelling creatures were trapped in sediments and preserved. The Phanerozoic eon is subdivided into three eras – the Paleozoic era, Mesozoic era, and Cenozoic era. An era is often divided into several smaller time spans called periods. For example, the Paleozoic era is divided into the Cambrian, Ordovician, Silurian, Devonian, Carboniferous,and Permian periods. Paleozoic Era Permian Period 300 - 250 million years ago Carboniferous Period 350 - 300 million years ago Devonian Period 400 - 350 million years ago Silurian Period 450 - 400 million years ago Ordovician Period 500 - 450 million years ago Cambrian Period 550 - 500 million years ago Figure 2. -
Short Communication a Remarkable Case of a Shark
Journal of Vertebrate Paleontology 30(2):592–597, March 2010 © 2010 by the Society of Vertebrate Paleontology SHORT COMMUNICATION A REMARKABLE CASE OF A SHARK-BITTEN ELASMOSAURID PLESIOSAUR ∗ KENSHU SHIMADA, ,1,2 TAKANOBU TSUIHIJI,3 TAMAKI SATO,4 and YOSHIKAZU HASEGAWA5; 1Environmental Science Program and Department of Biological Sciences, DePaul University, 2325 North Clifton Avenue, Chicago, Illinois 60614, U.S.A., [email protected]; 2Sternberg Museum of Natural History, Fort Hays State University, 3000 Sternberg Drive, Hays, Kansas 67601, U.S.A.; 3National Museum of Nature and Science, 3-23-1 Hyakuhin-cho, Shinjuku-ku, Tokyo 169-0073, Japan, [email protected]; 4Department of Astronomy and Earth Sciences, Tokyo Gakugei University, 4-1-1 Nukui-Kita-Machi, Koganei City, Tokyo 184-8501, Japan, [email protected]; 5Gunma Museum of Natural History, 1674-1 Kamikuroiwa, Tomimoka, Gunma 370-2345, Japan, [email protected] Futabasaurus suzukii Sato, Hasegawa, and Manabe, 2006, is an is embedded near the anterodorsal corner of the right humerus elasmosaurid plesiosaur from the Upper Cretaceous in central immediately distal to its tuberosity (Fig. 3A). The labial face of Japan. The holotype and the only known specimen of this taxon Tooth 85 faces the posterior side of the right humerus, suggest- is a partial skeleton (Fig. 1), which co-occurred with “several tens ing that the shark bit the forelimb from its anterior side. Two of shark teeth” (Sato et al., 2006:468). The shark teeth were pre- teeth, Teeth 83 and 84, are embedded in the posterodorsal cor- viously identified as those of ‘Odontaspis sp.’ (e.g., Obata et al., ner of the neural spine of “Vertebra #34,” a posterior cervical 1970), but we re-identified them as an extinct lamniform shark, vertebra (Fig. -
Cretaceous - Tertiary Mass Extinction Meteoritic Versus Volcanic Causes
GENERAL I ARTICLE Cretaceous - Tertiary Mass Extinction Meteoritic Versus Volcanic Causes P V Sukumaran The bolide impact theory for mass extinctions at the Cretaceous-tertiary (K-T) boundary was a revolutionary concept. This theory was contested by short duration global volcanism as a possible alternative cause for the K-T extinction. Though there is a converging evidence for an extra-terrestrial impact coinciding with the P V Sukumaran took his terminal Cretaceous, the causative link between the M Tech degree in impact and the K-T mass extinction is debatable. Thus, Applied Geology from the while the impact theory is re-emerging, available evidence University of Saugar and has been with the is still insufficient to rule out either of the two hypotheses. Geological Survey of India since 1974. His interests Introduction include geochemistry, petrology and palae oceanography. He is It is now widely believed that life on earth began very early in presently posted to the its geological history, probably about 4000 My (million years) Marine Wing of the ago (Mojzsis and others, 1996). Since then it underwent Department and has participated in many several evolutionary branchings to the complex diversity as scientific cruises both as we see today. Nevertheless, it was not a smooth voyage for life Chief Scientist and as a all along, the evolution was punctuated by geologically participating scientist. ins tan taneous events of mass mortality. New species emerged at the expense of their predecessors following each extinction event and life went on evolving ever more vibrantly. In the geologic record of rock strata, such mass extinction events are identifiable based on sudden absence and reduction in diversity of fossil assemblage across stratigraphic boundaries. -
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. -
How to Tell a Sea Monster: Molecular Discrimination of Large Marine Animals of the North Atlantic
Reference: Biol. Bull. 202: 1–5. (February 2002) How To Tell a Sea Monster: Molecular Discrimination of Large Marine Animals of the North Atlantic S. M. CARR1,*, H. D. MARSHALL1, K. A. JOHNSTONE1, L. M. PYNN1, AND G. B. STENSON2 1Genetics, Evolution, and Molecular Systematics Laboratory, Department of Biology, Memorial University of Newfoundland, St. John’s, Newfoundland A1B 3X9, Canada; and 2Marine Mammals Section, Science, Oceans, and Environment Branch, Department of Fisheries and Oceans, PO Box 5667, St. John’s, Newfoundland A1C 5X1, Canada “Either we do know all the varieties of beings which people our planet, or we do not. If we do not know them all—if Nature has still secrets in the deeps for us, nothing is more conformable to reason than to admit the existence of fishes, or cetaceans of other kinds, or even of new species ...which an accident of some sort has brought at long intervals to the upper level of the ocean.” —Jules Verne, Twenty Thousand Leagues Under the Sea, 1870 Abstract. Remains of large marine animals that wash (1994) gives a contemporary list. Even in the first year of a onshore can be difficult to identify due to decomposition new century when the complete human genome has become and loss of external body parts, and in consequence may be known (International Human Genome Sequencing Consor- dubbed “sea monsters.” DNA that survives in such car- tium, 2001), the possibility that entirely new, previously casses can provide a basis of identification. One such crea- unknown species may unexpectedly present themselves re- ture washed ashore at St. -
Cretaceous Fossils from the Chesapeake and Delaware Canal
Cretaceous S;cial Publication No. 18 Fossils from the Chesapeake and Delaware Canal A Guide for Students and Collectors Edward M. Lauginiger / /~ / CRETACEOUS FOSSILS FROM THE CHESAPEAKE AND DELAWARE CANAL: A GUIDE FOR STUDENTS AND COLLECTORS By Edward M. Lauginiger Biology Teacher Academy Park High School Sharon Hill, Pennsylvania September 1988 Reprinted 1997 CONTENTS Page INTRODUCTION. • 1 ACKNOWLEDGMENTS 2 PREVIOUS STUDIES. 3 FOSSILS AND FOSSILIZATION 5 Requirements for Fossilization 6 Types of Fossilization 7 GEOLOGY •• 10 CLASSIFICATON OF FOSSILS. 12 Kingdom Monera • 13 Kindgom Protista 1 3 Kingdom Plantae. 1 4 Kingdom Animalia 15 Phylum Porifera 15 Phylum Cnidaria (Coelenterata). 16 Phylum Bryozoa. 16 Phylum Brachiopoda. 17 Phylum Mollusca • 18 Phylum Annelida •. 22 Phylum Arthropoda • 23 Phylum Echinodermata. 24 Phylum Chordata 24 COLLECTING LOCALITIES 28 FOSSIL CHECK LIST 30 BIBLIOGRAPHY. 33 PLATES. ••• 39 iii FIGURES Page Figure 1 • Index map of the Chesapeake and Delaware Canal Area. .. .. 2 Figure 2. Generalized stratigraphic column of the formations exposed at the C & D Canal. 11 Figure 3. Foraminifera 14 Figure 4. Porifera 16 Figure 5. Cnidaria 16 Figure 6. Bryozoa. 17 Figure 7. Brachiopoda. 18 Figure 8. Mollusca-Gastropoda. 19 Figure 9. Mollusca-Pelecypoda. 21 Figure 10. Mollusca-Cephalopoda 22 Figure 11. Annelida . 22 Figure 12. Arthropoda 23 Figure 13. Echinodermata. 25 Figure 1 4. Chordata . 27 Figure 1 5. Collecting localities at the Chesapeake and Delaware Canal . ... .. 29 v CRETACEOUS FOSSILS FROM THE CHESAPEAKE AND DELAWARE CANAL: A GUIDE FOR STUDENTS AND COLLECTORS Edward M. Lauginiger INTRODUCTION Fossil collectors have been attracted to Delaware since the late 1820s when the excavation of the Chesapeake and Delaware (C&D) Canal first exposed marine fossils of Cretaceous age (Fig. -
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