The DINOSAURS of Wyoming

Total Page:16

File Type:pdf, Size:1020Kb

The DINOSAURS of Wyoming 'The CVinosaurs of Wyoming By ROY L. MOODIE, Ph. D. Santa Monica, California Cl9he W yorning Geological Survey JOHN G. MARZEL Director and State Qeologist BULLETIN XXII '5he Dinosaurs of Wyoming 1930 Tragedy of the Mesozoic All the elements of deep tragedy were present during the closing stages of the Age of Reptiles. The ponderous dino­ saurian reptile, many feet long, and thousands of pounds in weight, was a failure. Mother Nature had, through millions of years, given the dinosaurs e\'ery chance to succeed in the development of a race, ancestral to later, higher forms. Ex­ periment after experiment, yielding the curious and the biz­ arre, had all failed. One by one dinosaur groups had ap­ peared, run their course, and disappeared in extinction. What more is needed in a successful tragic drama than the powerful pathos, inability of adjustment to changed environments, and certain disastrous end? The dinosaurian reptile, here de­ picted, was the last of his race, a sad hero of the Mesozoic. Yet provident Nature had not been idle nor thoughtless, for way back in the Triassic Period, when the dinosaurs began their earthly course, the Mammals, derived from other rep­ tiles, also had their beginning. They \'vere dominated by reptiles of sea, land and air throughout the Age of Reptiles, and during the entire Mesozoic the Mammals remained small and inconspicuous; many of them doubtless arboreal in the Cretaceous days and living their lives remote from the dino­ saurs. Others, resem bling the rodents, lived in holes in the ground, or in crevices among the rocks. So at the close of the great Age of Reptiles-The Mesozoic -the stage was set for a great tragedy, the extinction of th(' Dinosaurs! The Mammal (on the right), inconsiderable in size, whether marsupial, multituberculate or just any Meso­ zoic Mammal. specializing in brain power, stands ready tL assume, unafraid, a leadership of untold possibilities, whic"h he and his kind later maintained throughout tl:e Age of Mam­ mals, the Cenozoic. and still maintain in the Age of Man. \~ ci bD < r---......\.. \. \ \ ~ .5 Dedicated to My Teacher in Paleontology SAMUEL WENDELL WILLISTON in Memory of .... Our Many Fossil Hunts in WYOMING The DINOSAURS of Wyoming By ROY L. MOODIE, Ph. D., Santa Monica, California FIRST EDITION 500 COPIES WYOMING GEOLOGICAL SURVEY CHEYENNE, WYOMING 1930 Price $ /. 50 Post Paid .- The Capitol Press .~ Cheyenne, Wyoming .. CONTENTS Preface ............................................................................................ Xl I. V,That Are the Dinosaurs ? 14 II. The Geological Age of the Dinosaurs 17 III. Their Origin and Distribution Throughout the World 20 IV. Historical Account of the Discovery of Dino- saurs in Wyoming 26 V. Methods of Collecting Dinosaur Bones 29 VI. Some Famous Collectors and Collections of Dinosaurs 3S VII. Occurrence of Dinosaurs in the State of 'vVyo- ming _ 41 VIII. The Different Kinds of Dinosaurs 44 IX. The Dinosaur-Bearing Rocks of Wyoming 46 X. Evidences of Disease and Injury Among the Dinosaurs 48 XI. Structure of the Bones of Dinosaurs S6 XII. The "Sacral Brain" of Dinosaurs S9 XIII. Dinosaur Mummies 65 XIV. Footprints of Dinosaurs 67 XV. The Armored Dinosaurs in Wyoming and Else- where 70 XVI. The Amphibious Dinosauria 83 XVII. The Carnivorous Dinosauria and Their Food ProblelTI 88 XVIII. The Three-Horned Dinosauria 97 XIX. Animals 'Nhich Lived 'vVith the Dinosaurs 110 XX. Wyoming Dinosaurs Abroad 113 XXI. List of vVritings 115 XXII. Glossary c..••.....••••......••••...••: ••••... 118 vii LIST OF ILLUSTRATIONS Title Page Design.-Three-Horned Dinosaur. Frontispiece.-The Tragedy of the Mesozoic. Figure I.-Diagram of Geological History __ . _. __ . __ 19 Figure 2.--Map of the World Showing Dinosaur Localities and Prob- able Migratory Routes of the Sauropoda.__ . _. .. 21 Figure 3.-The Same Map Showing Localities and Migratory Routes of the Theropoda ._ . .. _. .. .. __ 23 Figure 4.-Amphibious Dinosaurs. A Dinosaur Skeleton in the Rocks.... .. __ .. __ ._ ..._._. .. 31 Figure 5.-Uncovering a Complete Dinosaur Skeleton .. __ .. 32 Figure 6.-Four Famous Paleontologists _.. _.. __ '_.__ . 37 Figure 7.-Map of Wyoming and Surrounding Territory \!\There Dinosaurs Have Been Found . .. __ _ __ __ 42 Figure 8.-Map of Niobrara County, vVyoming . __ .. _. 43 Figure 9.-Disease in the Tail of Diplodocus.. .. .... _. ... 48 Figure 1O.-Pathologic Lesions in Mesozoic Reptiles.. _.. > •••• _. • 49 Figure 11.-A Section Through a Dinosaur TumoL... 50 Figure 12.-Injuries Among DiI1osaurs.. .... .. __ . •. .... 51 Figure 13.-Tumors and Similar Growths . .. __ 52 Figure 14.-The only known Dinosaurian TumoL. __ ~... 53 Figure 15.-Microscopic Section of Dinosaur Bone.. .. .. 55 Figure 16.-Sections Through a Dinosaur TumoL. 57 Figure 17.-Photomicrographs of Dinosaur Bones____ 58 Head-piece for Section XIII :-Duck-bill DinosauL.__ _ > • __ • __ 64 Figure 17a.-Dinosaur Footprints _ __ ..__ . __ .. 68 Figure 18.-Marsh's Restoration of Stegosaurus.__ . __ .. 69 Figure 19.-A Model of the Stegosaurus _. .__ 71 Figure 20.-A Model of the Muscles of Stegosaurus .__ 72 Figure 21.-The Cranial ,and Sacral "Brains" ._ __ .._ 73 Figure 22.-Sections of the Neck and Body __ . __ _. 74 Figure 23.-Restoration of the Appearance of Stegosaurus_ _... 75 Figure 24.-Mounted Skeleton of a Predentate DinosauL. .. __ 77 Figure 25.-An Armored Dinosaur from Canada.... 78 Figure 26.-Some Recent Lizards._.. .______ __ _. 79 Figure 27.-Skull of an Armored DinosauL. _. _._ __ _81 Tail-piece.-Armored Saurian .__ . ...... ___ .... .____ 82 Figure 28.-The Bone Cabin 'Quarry in Wyoming . __ .._....... .. 84 Figure 29.-Bones from the Tail of a Dinosaur.__ ._. __ ._.____________________ 85 Figure 30.-0utIine of the Nervous System of a DinosauL..... _.____ 86 T'ail-piece.-A Sauropod .. _. _ _. ._ 87 Figure 31.-Ske1eton of the "\Vhip-tail" DinosauL._______ 88 yij~ LIST OF ILLUsTRA'frONS IX Figure 32.-The Largest of the Carnivorous Dinosaurs . 89 Figure 33.-·The Carnivore-Ceratosaurus .. 90 Figure 34.-V/here the Allosaur Bit the Brontosaur. 90 Figure 3S.-The Bird-Catching, Wyoming, Dinosaur. 91 Figure 36.-The Wyom,ing Allosaurus Feeding............... .. 92 Figure 37.-Three Animals Exhibiting Opisthotonos. .. 93· Figure 38.-Skeleton of Tyrannosaurus Rex.................. .. 96 Head-piece.-The Three-Horn .. 94 Figure 39.-Statuette of the Wyoming Triceratops.... .. 97 Figure 40.-Injuries to the Dinosaurs . 98 Figure 41.-Injuries to Fossil Vertebrates . ...100 Figure 42.-Illjuries to Fossil Vertebrates .. .. 103 Figure 43.-A Canadian Horned Dinosaur. .. .105 Figure 44.-Diagram of the Giant Dinosaur Migrations .. .106 Figure 4S.-Dillos:aur Eggs from Asia.. .. .. 109 Figure 46.-A Mesozoic Bird .. ..Ill INTRODUCTION The interest that has been displayed in regard to the dino­ saurs that formerly thrived in Wyoming prompted the pub­ lication of this bulletin. This interest is not surprising. Many million years ago the dinosaur family reached its maximum degree of development in or near the fresh 'water ponds and lakes that dotted the terrain we now call Wyoming. It may seem strange to relate that no work has recently appeared in 'which an attempt is made to review the suprem­ acy of Wyoming in bone and brawn development for all time. To rectify this outstanding omission Dr. Roy L. Moodie, the well-known paleontologist, anatomist and paleopath­ ologist was prevailed upon to write this book under title of "THE DINOSADRS OF WYOMING." Perhaps no savant was better qualified to undertake this important commission. As a hunter of dinosaur fossils, Dr. Moodie covered the most promising areas of \Vyoming during the past 25 year period. Most of this work was done for lead­ ing museums and educational foundations. To many scholars and to those residents of Wyoming who came in contact with him during his research work Dr. Moodie's name and stand­ ing as a scientist needs no further introduction. The composition of Dr. Moodie's manuscript is of the non-technical style, and being profusely illustrated with restorations of Wyoming material that now repose within the larger museums of the world, it is anticipated that this publication will prove to be unusually fascinating. JOH. T G. MARZEL, State Geologist. .- PREFACE The subject of dinosaurs in general, and the dinosaurs of Wyoming in particular, has interested me since the spring of 1904, when for the first time I dropped off the train at Rawlins for a summer's work in the fossil beds of the Wind River Mountain area. I found the party waiting, ready to start in a light wagon equipped with the bows for a canvas cover-a common sight. We soon started on our drive to Lander, one hundred and fifty miles away-a full week's journey in those days. After that summer I spent several more seasons in the Wyoming fossil fields, either vvith Dr. S. \V. Williston as com­ panion or working under his directions. In the many camps we had together Dr. Williston told me of his work at Como Bluffs, excavating dinosaur bones for Professor Marsh; a terribly lonely job during the early winter months of the late seventies. As an amateur dipterologist I had in my bag the second edition of vVilliston's Manual of Jorth American Diptera. I shall never forget the keen pleasure derived from hearing the author tell how in his des­ pair at not being allowed to write about dinosaurs, a form of activity which Professor Marsh reserved for himself, he had turned to the study of the Diptera, a study at which he be­ came famous. But ever mingled in with other talk there was always that background of the huge, ungainly dinosaurian . reptiles, making a unique appeal to our fancy. What were the dinosaurs? Where had they come from? Why had so many lived and left their bones in the area now called \iVyoming? What was their manner of life? To what reptilian group were they related? During the three years I spent in Williston's laboratory as Fellow in Vertebrate Paleontology at the University of Chicago, our discussions of dinosaurian affairs were of the greatest interest.
Recommended publications
  • Morrison Formation 37 Cretaceous System 48 Cloverly Formation 48 Sykes Mountain Formation 51 Thermopolis Shale 55 Mowry Shale 56
    THE STRUCTURAL AND STRATIGRAPHIC FRAMEWORK OF THE WARM SPRINGS RANCH AREA, HOT SPRINGS COUNTY, WYOMING By CHRISTOPHER JAY CARSON Bachelor of Science Oklahoma State University 1998 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE July, 2000 THE STRUCTURAL AND STRATIGRAPHIC FRAMEWORK OF THE WARM SPRINGS RANCH AREA, HOT SPRINGS COUNTY, WYOMING Thesis Approved: Thesis Advisor ~~L. ... ~. ----'-"'-....D~e~e:.-g-e----- II ACKNOWLEDGEMENTS I wish to express appreciation to my advisor Dr. Arthur Cleaves for providing me with the opportunity to compile this thesis, and his help carrying out the fieldwork portion of the thesis. My sincere appreciation is extended to my advisory committee members: Dr. Stan Paxton, Dr. Gary Stewart, and Mr. David Schmude. I wish to thank Mr. Schmude especially for the great deal of personal effort he put forth toward the completion of this thesis. His efforts included financial, and time contributions, along with invaluable injections of enthusiasm, advice, and friendship. I extend my most sincere thank you to Dr. Burkhard Pohl, The Big Hom Basin Foundation, and the Wyoming Dinosaur Center. Without whose input and financial support this thesis would not have been possible. In conjunction I would like to thank the staff of the Wyoming Dinosaur Center for the great deal of help that I received during my stay in Thermopolis. Finally I wish to thank my friends and family. To my friends who have pursued this process before me, and with me; thank you very much.
    [Show full text]
  • Dinosaur Wars Program Transcript
    Page 1 Dinosaur Wars Program Transcript Narrator: For more than a century, Americans have had a love affair with dinosaurs. Extinct for millions of years, they were barely known until giant, fossil bones were discovered in the mid-nineteenth century. Two American scientists, Edward Drinker Cope and Othniel Charles Marsh, led the way to many of these discoveries, at the forefront of the young field of paleontology. Jacques Gauthier, Paleontologist: Every iconic dinosaur every kid grows up with, apatosaurus, triceratops, stegosaurus, allosaurus, these guys went out into the American West and they found that stuff. Narrator: Cope and Marsh shed light on the deep past in a way no one had ever been able to do before. They unearthed more than 130 dinosaur species and some of the first fossil evidence supporting Darwin’s new theory of evolution. Mark Jaffe, Writer: Unfortunately there was a more sordid element, too, which was their insatiable hatred for each other, which often just baffled and exasperated everyone around them. Peter Dodson, Paleontologist: They began life as friends. Then things unraveled… and unraveled in quite a spectacular way. Narrator: Cope and Marsh locked horns for decades, in one of the most bitter scientific rivalries in American history. Constantly vying for leadership in their young field, they competed ruthlessly to secure gigantic bones in the American West. They put American science on the world stage and nearly destroyed one another in the process. Page 2 In the summer of 1868, a small group of scientists boarded a Union Pacific train for a sightseeing excursion through the heart of the newly-opened American West.
    [Show full text]
  • [PDF] Dinosaur Eggshell from the Red Sandstone Group of Tanzania
    Journal of Vertebrate Paleontology 24(2):494±497, June 2004 q 2004 by the Society of Vertebrate Paleontology NOTE DINOSAUR EGGSHELL FROM THE RED SANDSTONE GROUP OF TANZANIA MICHAEL D. GOTTFRIED1, PATRICK M. O'CONNOR2, FRANKIE D. JACKSON3, ERIC M. ROBERTS4, and REMEGIUS CHAMI5, 1Mich- igan State University Museum, East Lansing, Michigan, 48824, [email protected]; 2College of Osteopathic Medicine, Ohio University, Athens, Ohio, 45701; 3Department of Earth Sciences, Montana State University, Bozeman, Montana, 59717; 4Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah, 84112, 5Antiquities Unit, P.O. Box 2280, Dar es Salaam, Tanzania Investigations over the last several decades at Gondwanan Mesozoic Although the age of the Red Sandstone Group is poorly understood (see localities have signi®cantly expanded our knowledge of the diversity Damblon et al., 1998), a Cretaceous age is suggested at this site based and distribution of Southern Hemisphere dinosaurs. These records are on (1) the overall composition of the fauna, which includes titanosaurid? primarily based on skeletal remains, but included among them are in- sauropods and both avian and nonavian theropods, as well as osteo- stances of preserved eggshell, notably from Argentina (e.g., Calvo et glossomorph ®shes, and (2) the possibility that these deposits may be al., 1997; Chiappe et al., 1998) and India (e.g., Khosla and Sahni, 1995). approximately coeval with the Cretaceous dinosaur beds of Malawi (Ja- In general, however, dinosaur eggshell is relatively poorly known from cobs et al., 1990), which lie ca. 200 km southeast of the Mbeya region. Gondwana, and from Africa in particular.
    [Show full text]
  • John Bell Hatcher.1 Bokn October 11, 1861
    568 Obituary—J. B. Hatcher. " Description of a New Genus [Stelidioseris] of Madreporaria from the Sutton Stone of South "Wales": Quart. Journ. Geol. Soc, vol. xlix (1893), pp. 574-578, and pi. xx. " Observations on some British Cretaceous Madreporaria, with the Description of two New Species " : GEOL. MAG., 1899, pp. 298-307. " Description of a Species of Heteraslraa lrom the Lower Rhsetic of Gloucester- shire" : Quart. Journ. Geol. Soc, lix (1903), pp. 403-407, and figs, in text. JOHN BELL HATCHER.1 BOKN OCTOBER 11, 1861. DIED JULY 3, 1904. THE Editor of the Annals of the Carnegie Museum, Pittsburgh, Pennsylvania, U.S., records with deep regret the death, on July 3rd, 1904, of his trusted associate, Mr. John Bell Hatcher. Mr. Hatcher was born at Cooperstown, Brown County, Illinois, on October 11th, 1861. He was the son of John and Margaret C. Hatcher. The family is Virginian in extraction. In his boyhood his parents removed to Greene County, Iowa, where his father, who with his mother survive him, engaged in agricultural pursuits near the town of Cooper. He received his early education from his father, who in the winter months combined the work of teaching in the schools with labour upon his farm. He also attended the public schools of the neighbourhood. In 1880 he entered Grinnell College, Iowa, where he remained for a short time, and then went to Yale College, where he took the degree of Bachelor in Philosophy, in July, 1884. While a student at Yale his natural fondness for scientific pursuits asserted itself strongly, and he attracted the attention of the late Professor Othniel C.
    [Show full text]
  • Brains and Intelligence
    BRAINS AND INTELLIGENCE The EQ or Encephalization Quotient is a simple way of measuring an animal's intelligence. EQ is the ratio of the brain weight of the animal to the brain weight of a "typical" animal of the same body weight. Assuming that smarter animals have larger brains to body ratios than less intelligent ones, this helps determine the relative intelligence of extinct animals. In general, warm-blooded animals (like mammals) have a higher EQ than cold-blooded ones (like reptiles and fish). Birds and mammals have brains that are about 10 times bigger than those of bony fish, amphibians, and reptiles of the same body size. The Least Intelligent Dinosaurs: The primitive dinosaurs belonging to the group sauropodomorpha (which included Massospondylus, Riojasaurus, and others) were among the least intelligent of the dinosaurs, with an EQ of about 0.05 (Hopson, 1980). Smartest Dinosaurs: The Troodontids (like Troödon) were probably the smartest dinosaurs, followed by the dromaeosaurid dinosaurs (the "raptors," which included Dromeosaurus, Velociraptor, Deinonychus, and others) had the highest EQ among the dinosaurs, about 5.8 (Hopson, 1980). The Encephalization Quotient was developed by the psychologist Harry J. Jerison in the 1970's. J. A. Hopson (a paleontologist from the University of Chicago) did further development of the EQ concept using brain casts of many dinosaurs. Hopson found that theropods (especially Troodontids) had higher EQ's than plant-eating dinosaurs. The lowest EQ's belonged to sauropods, ankylosaurs, and stegosaurids. A SECOND BRAIN? It used to be thought that the large sauropods (like Brachiosaurus and Apatosaurus) and the ornithischian Stegosaurus had a second brain.
    [Show full text]
  • Rule Booklet
    Dig for fossils, build skeletons, and attract the most visitors to your museum! TM SCAN FOR VIDEO RULES AND MORE! FOSSILCANYON.COM Dinosaurs of North America edimentary rock formations of western North America are famous for the fossilized remains of dinosaurs The rules are simple enough for young players, but and other animals from the Triassic, Jurassic, and serious players can benefit Cretaceous periods of the Mesozoic Era. Your objective from keeping track of the cards that is to dig up fossils, build complete skeletons, and display have appeared, reasoning about them in your museum to attract as many visitors as possible. probabilities and expected returns, and choosing between aggressive Watch your museum’s popularity grow using jigsaw-puzzle and conservative plays. scoring that turns the competition into a race! GAME CONTENTS TM 200,000300,000 160,000 VISITORS VISITORS PER YEAR 140,000 VISITORS PER YEAR 180,000 VISITORS PER YEAR 400,000 VISITORS PER YEAR Dig for fossils, build skeletons, and 340,000 VISITORS PER YEAR RD COLOR ELETONS CA GENUS PERIODDIET SK FOSSIL VISITORSPARTS 360,000 VISITORS PER YEAR PER YEAR attract the most visitors to your museum! VISITORS PER YEAR PER YEAR Tyrannosaurus K C 1 4 500,000 Brachiosaurus J H 1 3 400,000 ON YOUR TURN: TM SCAN FOR VIDEO Triceratops K H 1 3 380,000 RULES AND MORE! Allosaurus J C 2 Dig3 a first360,000 card. If it is a fossil, keep it hidden. FOSSILCANYON.COM Ankylosaurus K H 2 If it3 is an340,000 action card, perform the action.
    [Show full text]
  • Florida State University Libraries
    Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2017 Fossil Excavation, Museums, and Wyoming: American Paleontology, 1870-1915 Marlena Briane Cameron Follow this and additional works at the DigiNole: FSU's Digital Repository. For more information, please contact [email protected] FLORIDA STATE UNIVERSITY COLLEGE OF ARTS AND SCIENCES FOSSIL EXCAVATION, MUSEUMS, AND WYOMING: AMERICAN PALEONTOLOGY, 1870-1915 By MARLENA BRIANE CAMERON A Thesis submitted to the Program in the History and Philosophy of Science in partial fulfillment of the requirements for the degree of Master of Arts 2017 Marlena Cameron defended this thesis on July 17, 2017. The members of the supervisory committee were: Ronald E. Doel Professor Directing Thesis Michael Ruse Committee Member Kristina Buhrman Committee Member Sandra Varry Committee Member The Graduate School has verified and approved the above-named committee members, and certifies that the thesis has been approved in accordance with university requirements. ii TABLE OF CONTENTS List of Figures ................................................................................................................................ iv Abstract ............................................................................................................................................v 1. INTRODUCTION ......................................................................................................................1 2. THE BONE WARS ....................................................................................................................9
    [Show full text]
  • The Systematic Position of the Enigmatic Thyreophoran Dinosaur Paranthodon Africanus, and the Use of Basal Exemplifiers in Phyl
    1 The systematic position of the enigmatic thyreophoran dinosaur Paranthodon africanus, 2 and the use of basal exemplifiers in phylogenetic analysis 3 4 Thomas J. Raven1,2 ,3 and Susannah C. R. Maidment2 ,3 5 61Department of Earth Science & Engineering, Imperial College London, UK 72School of Environment & Technology, University of Brighton, UK 8 3Department of Earth Sciences, Natural History Museum, London, UK 9 10Corresponding author: Thomas J. Raven 11 12Email address: [email protected] 13 14 15 16 17 18 19 20 21ABSTRACT 22 23The first African dinosaur to be discovered, Paranthodon africanus was found in 1845 in the 24Lower Cretaceous of South Africa. Taxonomically assigned to numerous groups since discovery, 25in 1981 it was described as a stegosaur, a group of armoured ornithischian dinosaurs 26characterised by bizarre plates and spines extending from the neck to the tail. This assignment 27that has been subsequently accepted. The type material consists of a premaxilla, maxilla, a nasal, 28and a vertebra, and contains no synapomorphies of Stegosauria. Several features of the maxilla 29and dentition are reminiscent of Ankylosauria, the sister-taxon to Stegosauria, and the premaxilla 30appears superficially similar to that of some ornithopods. The vertebral material has never been 31described, and since the last description of the specimen, there have been numerous discoveries 32of thyreophoran material potentially pertinent to establishing the taxonomic assignment of the 33specimen. An investigation of the taxonomic and systematic position of Paranthodon is therefore 34warranted. This study provides a detailed re-description, including the first description of the 35vertebra. Numerous phylogenetic analyses demonstrate that the systematic position of 36Paranthodon is highly labile and subject to change depending on which exemplifier for the clade 37Stegosauria is used.
    [Show full text]
  • Palaeoecology and Depositional Environments of the Tendaguru Beds (Late Jurassic to Early Cretaceous, Tanzania)
    Mitt. Mus. Nat.kd. Berl., Geowiss. Reihe 5 (2002) 19-44 10.11.2002 Palaeoecology and depositional environments of the Tendaguru Beds (Late Jurassic to Early Cretaceous, Tanzania) Martin Aberhan ', Robert Bussert2, Wolf-Dieter Heinrich', Eckhart Schrank2, Stephan Schultkal, Benjamin Sames3, Jiirgen =wet4 & Saidi Kapilima5 With 6 figures, 2 tables, and 2 plates Abstract The Late Jurassic to Early Cretaceous Tendaguru Beds (Tanzania, East Africa) have been well known for nearly a century for their diverse dinosaur assemblages. Here, we present sedimentological and palaeontological data collected by the German- Tanzanian Tendaguru Expedition 2000 in an attempt to reconstruct the palaeo-ecosystems of the Tendaguru Beds at their type locality. Our reconstructions are based on sedimentological data and on a palaeoecological analysis of macroinverte- brates, microvertebrates, plant fossils and microfossils (ostracods, foraminifera, charophytes, palynomorphs). In addition, we included data from previous expeditions, particularly those on the dinosaur assemblages. The environmental model of the Tendaguru Beds presented herein comprises three broad palaeoenvironmental units in a marginal marine setting: (1) Lagoon-like, shallow marine environments above fair weather wave base and with evidence of tides and storms. These formed behind barriers such as ooid bar and siliciclastic sand bar complexes and were generally subject to minor salinity fluctuations. (2) Extended tidal flats and low-relief coastal plains. These include low-energy, brackish coastal lakes and ponds as well as pools and small fluvial channels of coastal plains in which the large dinosaurs were buried. Since these environments apparently were, at best, poorly vegetated, the main feeding grounds of giant sauropods must have been elsewhere.
    [Show full text]
  • AMERICAN MUSEUM NOVITATES Published by of NATURAL HISTORY Dec
    AMERICAN MUSEUM NOVITATES Published by OF NATURAL HISTORY Dec. 4, 1933 Number 679 THE AMERICAN NewMUSEUMYork City 56.81, 9 (117:51.7) TWO NEW DINOSAURIAN REPTILES FROM MONGOLIA WITH NOTES ON SOME FRAGMENTARY SPECIMENS' BY CHARLES W. GILMORE2 CONTENTS PAGE INTRODUCTION......................................................... 1 DESCRIPTION OF GENERA AND SPECIES................................... 3 Order Orthopoda.................................................... 3 Family Nodosauridae............................................. 3 Pinacosaurus grangeri, new genus, new species. 3 Order Saurischia.................................................... 9 . Mongolosaurus haplodon, new genus, new species .. .. 11 NOTES ON OTHER DINOSAURIAN OCCURRENCES IN MONGOLIA................ 16 Family Deinodontidae.............................................. 16 Family Ornithomimidae............................................. 17 Family Hadrosauridae.............................................. 18 Family Ceratopsidae............................................... 19 BIBLIOGRAPHY............. 20 INTRODUCTION The present paper gives the results of a study of the residue of the dinosaur collections made in Mongolia by various Asiatic expeditions of The American Museum of Natural History. All of the material is frag- mentary, but diagnostic parts of two of the specimens are sufficiently preserved to be worthy of detailed description. One records the presence of a new genus and species of the Nodosauridae, the other a new genus and species of the Sauropoda. The
    [Show full text]
  • Reference Site Taphofacies Lithology Paleontology Weathering Transport
    Reference Site Taphofacies Lithology Paleontology Weathering Transport Groups Allosaurus Ceratosaurus Torvosaurus Small Theropod Camarosaurus Apatosaurus Barasaurus Diplodocus Haplocathosaurus Brachyosaurus Mymo Stegosaurus Dryosaurus Heterodontosaurus Camptosaurus Pterosaurus Crocodiles Turtle Frogs Fish Lizards Sphenodont Mammals Snails Unionids coarse grained sand- articulated partial conglomerate, trough skeletons, associated cross-bedding, fining by largegly Kirkland, 2006 FPA Channel sandstone upward sequences disarticulated X X X X X X X fine to coarse sand with mud and carbonate clasts, Mass accumulations, Dodson, 1980 Bone Cabin Quarry Channel sandstone common, poorly to mostly disarticulated X X X X X X X X X X fine to coarse sand with mud and carbonate clasts, Mass accumulations, Dodson, 1980 Quarry 13 Channel sandstone common, poorly to mostly disarticulated X X X X X X fine to coarse sand with mud and Mass accumulation, I - 17; II - 30; III - 60; carbonate clasts, mixed high to low scrap -37 (Layton Dodson, 1980 Dinosaur NM Channel sandstone common, poorly to articulation 0-1 (Fiorillo, 1994) (1977) X X X X X X X X X X fine to coarse sand with mud and Mass accumulation, I - 1205, II - 712, III - carbonate clasts, mixed high to low 279 (Richmond and Richmond and Morrison,Dry 1998 Mesa Channel sandstone common, poorly to articulation Morrison) X X X X X X X X X X X X X X X X fine to coarse sand with mud and carbonate clasts, Mass accumulation, Evanoff and Carpenter, Felch1998 Quarry 1 Channel sandstone common, poorly to mostly
    [Show full text]
  • A Census of Dinosaur Fossils Recovered from the Hell Creek and Lance Formations (Maastrichtian)
    The Journal of Paleontological Sciences: JPS.C.2019.01 1 TAKING COUNT: A Census of Dinosaur Fossils Recovered From the Hell Creek and Lance Formations (Maastrichtian). ______________________________________________________________________________________ Walter W. Stein- President, PaleoAdventures 1432 Mill St.. Belle Fourche, SD 57717. [email protected] 605-210-1275 ABSTRACT: A census of Hell Creek and Lance Formation dinosaur remains was conducted from April, 2017 through February of 2018. Online databases were reviewed and curators and collections managers interviewed in an effort to determine how much material had been collected over the past 130+ years of exploration. The results of this new census has led to numerous observations regarding the quantity, quality, and locations of the total collection, as well as ancillary data on the faunal diversity and density of Late Cretaceous dinosaur populations. By reviewing the available data, it was also possible to make general observations regarding the current state of certain exploration programs, the nature of collection bias present in those collections and the availability of today's online databases. A total of 653 distinct, associated and/or articulated remains (skulls and partial skeletons) were located. Ceratopsid skulls and partial skeletons (mostly identified as Triceratops) were the most numerous, tallying over 335+ specimens. Hadrosaurids (Edmontosaurus) were second with at least 149 associated and/or articulated remains. Tyrannosaurids (Tyrannosaurus and Nanotyrannus) were third with a total of 71 associated and/or articulated specimens currently known to exist. Basal ornithopods (Thescelosaurus) were also well represented by at least 42 known associated and/or articulated remains. The remaining associated and/or articulated specimens, included pachycephalosaurids (18), ankylosaurids (6) nodosaurids (6), ornithomimids (13), oviraptorosaurids (9), dromaeosaurids (1) and troodontids (1).
    [Show full text]