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Oldest Known Dinosaurian Nesting Site and Reproductive Biology of the Early Jurassic Sauropodomorph Massospondylus
Oldest known dinosaurian nesting site and reproductive biology of the Early Jurassic sauropodomorph Massospondylus Robert R. Reisza,1, David C. Evansb, Eric M. Robertsc, Hans-Dieter Suesd, and Adam M. Yatese aDepartment of Biology, University of Toronto Mississauga, Mississauga, ON L5L 1C6, Canada; bRoyal Ontario Museum, Toronto, ON M5S 2C6, Canada; cSchool of Earth and Environmental Sciences, James Cook University, Townsville, 4811 QLD, Australia; dDepartment of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC 20013; and eBernard Price Institute for Palaeontological Research, University of the Witwatersrand, Wits 2050, Johannesburg, South Africa Edited by Steven M. Stanley, University of Hawaii, Honolulu, HI, and approved December 16, 2011 (received for review June 10, 2011) The extensive Early Jurassic continental strata of southern Africa clutches and recognition of the earliest known dinosaurian nesting have yielded an exceptional record of dinosaurs that includes complex at the Rooidraai locality. scores of partial to complete skeletons of the sauropodomorph Massospondylus, ranging from embryos to large adults. In 1976 an Results incomplete egg clutch including in ovo embryos of this dinosaur, Our work at the Rooidraai locality has yielded multiple in situ the oldest known example in the fossil record, was collected from clutches of eggs as well as fragmentary eggshell and bones, all from a road-cut talus, but its exact provenance was uncertain. An exca- a 2-m-thick interval of muddy siltstone 25 m from the top of the vation program at the site started in 2006 has yielded multiple in Lower Jurassic Upper Elliot Formation (“Stormberg Group,” situ egg clutches, documenting the oldest known dinosaurian Karoo Supergroup) (11). -
Saurian Safari a Walk in the Jurassic Park
Dinosaur Safari Junior Introduction: The rules are a simplified variant Of the Saurian Safari rules developed by Chris Peers and originally published by HLBS publishing 2002, this an instructional aid used for the Smithsonian Summer camp program. The rules were developed for grades K – 5 but fun with older age groups. The instructor will act as a Game Master (GM) and will be responsible for preparing the character sheets and setting up the map. This custom version is for a fast moving with minimal book keeping or rolling on charts. Game time recommended for 45 – 60 minutes per scenario. A. Preparation: The GM will have printer character sheets and a six-sided die (D6) and a ten-sided die (D10). Each gamer will need a figure and character sheet. A large vinyl hex map crossed with a river is used for the camp. 1. Setup map. The GM will set up the hex map. Terrain types are forest, river or swamp, clear or hills. Follow guidelines for map set up listed for the scenario. The goal is represent the environment of the period. SAURIAN SAFARI JR: CHARACTER SHEET Name: Shooting Skill: (D6x10 + 40) Agility: (D6+ 4) Weapon: Range: Penetration: Damage: Trophies: Species Taken Other Information 2. Help gamers create a character. GM will to help gamers. Calculate the following and record on sheet. For name write gamers name. For Shooting skill roll 1 D6 multiple by 10 and add 40. For Agility roll D6 and add 4. Chose one weapon. Dinosaur Gun. Penetration 12 Damage 8 Nitro Express, double barrel, -5 subtracted from character accuracy. -
Re-Description of the Sauropod Dinosaur Amanzia (“Ornithopsis
Schwarz et al. Swiss J Geosci (2020) 113:2 https://doi.org/10.1186/s00015-020-00355-5 Swiss Journal of Geosciences ORIGINAL PAPER Open Access Re-description of the sauropod dinosaur Amanzia (“Ornithopsis/Cetiosauriscus”) greppini n. gen. and other vertebrate remains from the Kimmeridgian (Late Jurassic) Reuchenette Formation of Moutier, Switzerland Daniela Schwarz1* , Philip D. Mannion2 , Oliver Wings3 and Christian A. Meyer4 Abstract Dinosaur remains were discovered in the 1860’s in the Kimmeridgian (Late Jurassic) Reuchenette Formation of Moutier, northwestern Switzerland. In the 1920’s, these were identifed as a new species of sauropod, Ornithopsis greppini, before being reclassifed as a species of Cetiosauriscus (C. greppini), otherwise known from the type species (C. stewarti) from the late Middle Jurassic (Callovian) of the UK. The syntype of “C. greppini” consists of skeletal elements from all body regions, and at least four individuals of diferent sizes can be distinguished. Here we fully re-describe this material, and re-evaluate its taxonomy and systematic placement. The Moutier locality also yielded a theropod tooth, and fragmen- tary cranial and vertebral remains of a crocodylomorph, also re-described here. “C.” greppini is a small-sized (not more than 10 m long) non-neosauropod eusauropod. Cetiosauriscus stewarti and “C.” greppini difer from each other in: (1) size; (2) the neural spine morphology and diapophyseal laminae of the anterior caudal vertebrae; (3) the length-to-height proportion in the middle caudal vertebrae; (4) the presence or absence of ridges and crests on the middle caudal cen- tra; and (5) the shape and proportions of the coracoid, humerus, and femur. -
A Stable Isotopic Investigation of Resource Partitioning Among Neosauropod Dinosaurs of the Upper Jurassic Morrison Formation
A stable isotopic investigation of resource partitioning among neosauropod dinosaurs of the Upper Jurassic Morrison Formation Benjamin T. Breeden, III SID: 110305422 [email protected] GEOL394H University of Maryland, College Park, Department of Geology 29 April 2011 Advisors: Dr. Thomas R. Holtz1, Jr., Dr. Alan Jay Kaufman1, and Dr. Matthew T. Carrano2 1: University of Maryland, College Park, Department of Geology 2: National Museum of Natural History, Department of Paleobiology ABSTRACT For more than a century, morphological studies have been used to attempt to understand the partitioning of resources in the Morrison Fauna, particularly between members of the two major clades of neosauropod (long-necked, megaherbivorous) dinosaurs: Diplodocidae and Macronaria. While it is generally accepted that most macronarians fed 3-5m above the ground, the feeding habits of diplodocids are somewhat more enigmatic; it is not clear whether diplodocids fed higher or lower than macronarians. While many studies exploring sauropod resource portioning have focused on differences in the morphologies of the two groups, few have utilized geochemical evidence. Stable isotope geochemistry has become an increasingly common and reliable means of investigating paleoecological questions, and due to the resistance of tooth enamel to diagenetic alteration, fossil teeth can provide invaluable paleoecological and behavioral data that would be otherwise unobtainable. Studies in the Ituri Rainforest in the Democratic Republic of the Congo, have shown that stable isotope ratios measured in the teeth of herbivores reflect the heights at which these animals fed in the forest due to isotopic variation in plants with height caused by differences in humidity at the forest floor and the top of the forest exposed to the atmosphere. -
Giants from the Past | Presented by the Field Museum Learning Center 2 Pre-Lesson Preparation
Giants from the Past Middle School NGSS: MS-LS4-1, MS-LS4-4 Lesson Description Learning Objectives This investigation focuses on the fossils of a particular • Students will demonstrate an understanding that group of dinosaurs, the long-necked, herbivores known as particular traits provide advantages for survival sauropodomorphs. Students will gain an understanding by using models to test and gather data about the of why certain body features provide advantages to traits’ functions. Background survival through the use of models. Students will analyze • Students will demonstrate an understanding of and interpret data from fossils to synthesize a narrative ancestral traits by investigating how traits appear for the evolution of adaptations that came to define a and change (or evolve) in the fossil record well-known group of dinosaurs. over time. • Students will demonstrate an understanding of how traits function to provide advantages Driving Phenomenon in a particular environment by inferring daily Several traits, inherited and adapted over millions of years, activities that the dinosaur would have performed provided advantages for a group of dinosaurs to evolve for survival. into the largest animals that ever walked the Earth. Giant dinosaurs called sauropods evolved over a period of 160 Time Requirements million years. • Four 40-45 minute sessions As paleontologists continue to uncover new specimens, Prerequisite Knowledge they see connections across time and geography that lead to a better understanding of how adaptations interact • Sedimentary rocks form in layers, the newer rocks with their environment to provide unique advantages are laid down on top of the older rocks. depending on when and where animals lived. -
Redalyc.Angolatitan Adamastor, a New Sauropod Dinosaur and the First Record from Angola
Anais da Academia Brasileira de Ciências ISSN: 0001-3765 [email protected] Academia Brasileira de Ciências Brasil MATEUS, OCTÁVIO; JACOBS, LOUIS L.; SCHULP, ANNE S.; POLCYN, MICHAEL J.; TAVARES, TATIANA S.; BUTA NETO, ANDRÉ; MORAIS, MARIA LUÍSA; ANTUNES, MIGUEL T. Angolatitan adamastor, a new sauropod dinosaur and the first record from Angola Anais da Academia Brasileira de Ciências, vol. 83, núm. 1, marzo, 2011, pp. 221-233 Academia Brasileira de Ciências Rio de Janeiro, Brasil Available in: http://www.redalyc.org/articulo.oa?id=32717681011 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative “main” — 2011/2/10 — 15:47 — page 221 — #1 Anais da Academia Brasileira de Ciências (2011) 83(1): 221-233 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 www.scielo.br/aabc Angolatitan adamastor, a new sauropod dinosaur and the first record from Angola , OCTÁVIO MATEUS1 2, LOUIS L. JACOBS3, ANNE S. SCHULP4, MICHAEL J. POLCYN3, TATIANA S. TAVARES5, ANDRÉ BUTA NETO5, MARIA LUÍSA MORAIS5 and MIGUEL T. ANTUNES6 1CICEGe, Faculdade de Ciências e Tecnologia, FCT, Universidade Nova de Lisboa, 2829-516 Caparica, Portugal 2Museu da Lourinhã, Rua João Luis de Moura, 2530-157 Lourinhã, Portugal 3Huffington Department of Earth Sciences, Southern Methodist University, Dallas, TX, 75275, USA 4Natuurhistorisch Museum Maastricht, de Bosquetplein 6-7, NL6211 KJ Maastricht, The Netherlands 5Geology Department, Universidade Agostinho Neto, Av. -
High European Sauropod Dinosaur Diversity During Jurassic–Cretaceous Transition in Riodeva (Teruel, Spain)
CORE Metadata, citation and similar papers at core.ac.uk Provided by RERO DOC Digital Library [Palaeontology, Vol. 52, Part 5, 2009, pp. 1009–1027] HIGH EUROPEAN SAUROPOD DINOSAUR DIVERSITY DURING JURASSIC–CRETACEOUS TRANSITION IN RIODEVA (TERUEL, SPAIN) by RAFAEL ROYO-TORRES*, ALBERTO COBOS*, LUIS LUQUE*, AINARA ABERASTURI*, , EDUARDO ESPI´LEZ*, IGNACIO FIERRO*, ANA GONZA´ LEZ*, LUIS MAMPEL* and LUIS ALCALA´ * *Fundacio´n Conjunto Paleontolo´gico de Teruel-Dino´polis. Avda. Sagunto s ⁄ n. E-44002 Teruel, Spain; e-mail: [email protected] Escuela Taller de Restauracio´n Paleontolo´gica II del Gobierno de Arago´n. Avda. Sagunto s ⁄ n. E-44002 Teruel, Spain Typescript received 13 December 2007; accepted in revised form 3 November 2008 Abstract: Up to now, more than 40 dinosaur sites have (CPT-1074) referring to the Diplodocidae clade. New been found in the latest Jurassic – earliest Cretaceous remains from the RD-28, RD-41 and RD-43 sites, of the sedimentary outcrops (Villar del Arzobispo Formation) of same age, among which there are caudal vertebrae, are Riodeva (Iberian Range, Spain). Those already excavated, assigned to Macronaria. New sauropod footprints from the as well as other findings, provide a large and diverse Villar del Arzobispo Formation complete the extraordinary number of sauropod remains, suggesting a great diversity sauropod record coming to light in the area. The inclusion for this group in the Iberian Peninsula during this time. of other sauropods from different contemporaneous expo- Vertebrae and ischial remains from Riodevan site RD-13 sures in Teruel within the Turiasauria clade adds new evi- are assigned to Turiasaurus riodevensis (a species described dence of a great diversity of sauropods in Iberia during in RD-10, Barrihonda site), which is part of the the Jurassic–Cretaceous transition. -
Osteological Revision of the Holotype of the Middle
Osteological revision of the holotype of the Middle Jurassic sauropod dinosaur Patagosaurus fariasi (Sauropoda: Cetiosauridae) BONAPARTE 1979 Femke Holwerda, Oliver W.M. Rauhut, Pol Diego To cite this version: Femke Holwerda, Oliver W.M. Rauhut, Pol Diego. Osteological revision of the holotype of the Middle Jurassic sauropod dinosaur Patagosaurus fariasi (Sauropoda: Cetiosauridae) BONAPARTE 1979. 2020. hal-02977029 HAL Id: hal-02977029 https://hal.archives-ouvertes.fr/hal-02977029 Preprint submitted on 27 Oct 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Osteological revision of the holotype of the Middle Jurassic sauropod 2 dinosaur Patagosaurus fariasi (Sauropoda: Cetiosauridae) 3 BONAPARTE 1979 4 5 Femke M Holwerda1234, Oliver W M Rauhut156, Diego Pol78 6 7 1 Staatliche Naturwissenscha�liche Sammlungen Bayerns (SNSB), Bayerische Staatssamlung für 8 Paläontologie und Geologie, Richard-Wagner-Strasse 10, 80333 München, Germany 9 10 2 Department of Geosciences, Utrecht University, Princetonlaan, 3584 CD Utrecht, 10 Netherlands 11 12 3 Royal Tyrrell Museum of Palaeontology, Drumheller, AlbertaT0J 0Y0, Canada (current) 13 14 4 Fachgruppe Paläoumwelt, GeoZentrum Nordbayern, Friedrich-Alexander-Universität Erlangen- 15 Nürnberg, Loewenichstr. 28, 91054 Erlangen, Germany 16 17 5 Department für Umwelt- und Geowissenscha�en, Ludwig-Maximilians-Universität München, Richard- 18 Wagner-Str. -
MEMORIAL to BARNUM BROWN (1873-1963) G. EDWARD LEWIS U. S. Geological Survey, Denver, Colorado Barnum Brown, the Last and Most S
MEMORIAL TO BARNUM BROWN (1873-1963) G. EDWARD LEWIS U. S. Geological Survey, Denver, Colorado Barnum Brown, the last and most successful of the great fossil hunters who led expeditions to the far corners of the earth during the Golden Age of vertebrate paleontological exploration, died on 5 February, 1963. Nothing short of a book would be adequate to do justice to this remarkable man's full life, his explora- tions, and other scientific achievements: he was associated with the American Museum of Natural History in New York from 1897 to 1963; although he did not explore the South Sea Islands, Madagas- car, or the Antipodes, he ranged far and wide over the major continents of the world and covered vast areas literally step by step. Barnum's parents were of old American stock: William Brown was a Virginian, born in 1833, who travelled westward to Wisconsin, where he married Clara Silver near Monticello, where she was born in 1840. They loaded their possessions into an ox-drawn covered wagon in 1859 and headed westward with their first child, Clara Melissa. They averaged 10 miles a day on the way to Kansas Territory where, near Lickskillet in Osage County, a second daughter, Alice Elizabeth, was born on 4 January 1860. Nearby in the same county was a place underlain by coal where they built a one-room cabin on Carbon Hill, to the west of which Carbondale sprang up some years later. The cabin doors were closed by flaps of canvas; the windows were covered with greased paper; there were cots, packing boxes, and barrel chairs for furniture. -
BROWN, BARNUM (1873–1963) Dinosaur Fossil Collector Amed After the Great Showman P
BRoWn, BaRnUM (1873–1963) Dinosaur Fossil collector amedafterthegreatshowmanP.T.Barnum,indefatigabledinosaurdiggerBarnum Brownassembledhisownversionof“The Greatest Showon Earth”:aparadeofgiant n dinosaurfossilswrenchedfromthecliffsandarroyosoftheAmericanWest.Brown’s -lastingcontribution—hundredsoftonsofdinosaurfossils—formedthenucleusoftheAmeri .canMuseumofnaturalHistory’sworld-famouscollection during the 1960s, Brown, nearly 90, could still be seen leading visitors around the crammeddinosaurhalls,announcing,“Here’sanotheroneofmychildren,”ashepointed outthebonesofasauriangiant.Butwhenhebeganhiscareerin1897,themuseumhad .notasingledinosaur AsachildinCarbondale, Kansas,Browncollectedfossilsfromfreshlyplowedfields.He -attendedtheUniversityof Kansas,thenmovedto New YorkCity,wherehestudiedpaleontol ogyatColumbiaUniversityandbeganworkingatthemuseumwhilehewasstillagraduate student. Forhisfirstfieldassignment,themuseum’sdirector,HenryFairfield Osborn,sentBrown BONE hUNTER barnum brown, when almost ninety, toComoBluff,Wyoming,toprospectitsrichJurassicdeposits.Brownandhiscolleagues supervised construction of discoverednewbedscontainingenormousquantitiesoffossils,includingtheApatosaurus .sinclair oil’s lifesize dino- (thencalled Brontosaurus)thatstilldominatesoneofthemuseum’shugedinosaurhalls saur models, shown below However, yale paleontologist othniel C. Marsh was furious about his former sites being being barged down the hud- .workedandbeganabitterfeudwithosbornthatlastedtotheendofhislife son river to the 1964 new york World’s fair. -
The Dinosaurs of North America
FEOM THE SIXTEENTH ANNUAL KEPOKT OF THE U. S, GEOLOGICAL SURVEY THE DINOSAURS OF NORTH AMERICA OTHNIEL CHARLES MARSH TALE UNIVERSITY WASHINGTON 1896 ^33/^, I/BRAKt 4 ,\ . THE DINOSAURS OF NORTH AMERICA. BY OTHNIEL CHARLES MARSH. 133 CONTENTS. Pajje. Introduction 143 Part I. —Triassic dinosaurs 146 Theropoda 146 Anchisaurida? 147 Anchisaurus 147 The skull 148 The fore limbs 149 The hind limbs 149 Anchisaurus solus 149 Amniosaurus rTT 150 Eestoration of Anchisaurus 150 Dinosaurian footprints 151 Distribution of Triassic dinosaurs 152 Part II. —Jurassic dinosaurs 152 Theropoda : 153 Hallopus 153 Fore and hind limbs 154 Coelurus _ 155 The vertebra:- 155 The hind limbs 156 Ceratosaurus 156 The skull 157 The brain 159 The lower iaws 159 The vertebra: 159 The scapular arch 160 The pelvic arch 160 The metatarsals 162 Eestoration of Ceratosaurus 163 Allosaurus 163 European Theropoda 163 Sauropoda 164 Atlantosaurus beds 164 Families of Sauropoda 165 Atlantosauridie 166 Atlantosaurus 166 Apatosaurus 166 The sacral cavity 166 The vertebra- 167 Brontosaurus 168 The scapular arch 168 The cervical vertebra.- 169 The dorsal vertebree 169 The sacrum 170 The caudal vertebra- 171 The pelric arch 172 The fore limbs 173 The hind limbs 173 135 136 CONTENTS. Part II. —Jurassic dinosaurs—Continued. Page. Sauropoda—Continued. Atlantosaurida? —Continued. Restoration of Brontosaurus 173 Barnsaurus 174 Diplodoeida? 175 Diplodocus 175 The skull 175 The brain 178 The lower jaws 178 The teeth 179 The vertebra; 180 The sternal bones 180 The pelvic girdle 180 Size and habits 180 Morosaurida? 181 Morosaurus 181 The skull 181 The vertebra? 181 The fore limbs 182 The pelvis 182 The hind limbs 183 Pleuroccelida? : 183 Pleurocoelus 183 The skull 183 The vertebras 183 Distribution of the Sauropoda 185 Comparison with European forms 185 Predentata ». -
Back Matter (PDF)
Index Note: Page numbers in italic denote figures. Page numbers in bold denote tables. Abel, Othenio (1875–1946) Ashmolean Museum, Oxford, Robert Plot 7 arboreal theory 244 Astrodon 363, 365 Geschichte und Methode der Rekonstruktion... Atlantosaurus 365, 366 (1925) 328–329, 330 Augusta, Josef (1903–1968) 222–223, 331 Action comic 343 Aulocetus sammarinensis 80 Actualism, work of Capellini 82, 87 Azara, Don Felix de (1746–1821) 34, 40–41 Aepisaurus 363 Azhdarchidae 318, 319 Agassiz, Louis (1807–1873) 80, 81 Azhdarcho 319 Agustinia 380 Alexander, Annie Montague (1867–1950) 142–143, 143, Bakker, Robert. T. 145, 146 ‘dinosaur renaissance’ 375–376, 377 Alf, Karen (1954–2000), illustrator 139–140 Dinosaurian monophyly 93, 246 Algoasaurus 365 influence on graphic art 335, 343, 350 Allosaurus, digits 267, 271, 273 Bara Simla, dinosaur discoveries 164, 166–169 Allosaurus fragilis 85 Baryonyx walkeri Altispinax, pneumaticity 230–231 relation to Spinosaurus 175, 177–178, 178, 181, 183 Alum Shale Member, Parapsicephalus purdoni 195 work of Charig 94, 95, 102, 103 Amargasaurus 380 Beasley, Henry Charles (1836–1919) Amphicoelias 365, 366, 368, 370 Chirotherium 214–215, 219 amphisbaenians, work of Charig 95 environment 219–220 anatomy, comparative 23 Beaux, E. Cecilia (1855–1942), illustrator 138, 139, 146 Andrews, Roy Chapman (1884–1960) 69, 122 Becklespinax altispinax, pneumaticity 230–231, Andrews, Yvette 122 232, 363 Anning, Joseph (1796–1849) 14 belemnites, Oxford Clay Formation, Peterborough Anning, Mary (1799–1847) 24, 25, 113–116, 114, brick pits 53 145, 146, 147, 288 Benett, Etheldred (1776–1845) 117, 146 Dimorphodon macronyx 14, 115, 294 Bhattacharji, Durgansankar 166 Hawker’s ‘Crocodile’ 14 Birch, Lt.