MANUS, SACRUM, and CAUDALS of by HENRY FAIRFIELD
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v^ Official Journal of the Biology Unit of the American Topical Association 10 Vol. 40(4) DINOSAURS ON STAMPS by Michael K. Brett-Surman Ph.D. Dinosaurs are the most popular animals of all time, and the most misunderstood. Dinosaurs did not fly in the air and did not live in the oceans, nor on lake bottoms. Not all large "prehistoric monsters" are dinosaurs. The most famous NON-dinosaurs are plesiosaurs, moso- saurs, pelycosaurs, pterodactyls and ichthyosaurs. Any name ending in 'saurus' is not automatically a dinosaur, for' example, Mastodonto- saurus is neither a mastodon nor a dinosaur - it is an amphibian! Dinosaurs are defined by a combination of skeletal features that cannot readily be seen when the animal is fully restored in a flesh reconstruction. Because of the confusion, this compilation is offered as a checklist for the collector. This topical list compiles all the dinosaurs on stamps where the actual bones are pictured or whole restorations are used. It excludes footprints (as used in the Lesotho stamps), cartoons (as in the 1984 issue from Gambia), silhouettes (Ascension Island # 305) and unoffi- cial issues such as the famous Sinclair Dinosaur stamps. The name "Brontosaurus", which appears on many stamps, is used with quotation marks to denote it as a popular name in contrast to its correct scientific name, Apatosaurus. For those interested in a detailed encyclopedic work about all fossils on stamps, the reader is referred to the forthcoming book, 'Paleontology - a Guide to the Postal Materials Depicting Prehistoric Lifeforms' by Fran Adams et. al. The best book currently in print is a book titled 'Dinosaur Stamps of the World' by Baldwin & Halstead. -
By HENRY FAIRFIELD OSBORN and CHARL
VoL. 6, 1920 PALAEONTOLOGY: OSBORN AND MOOK IS RECONSTRUCTION OF THE SKELETON OF THE SAUROPOD DINOSAUR CAMARASA URUS COPE (MOROSA URUS MARSH) By HENRY FAIRFIELD OSBORN AND CHARLES CRAIG MOOK AMERICAN MusEUM or NATURAL HISTORY, NEW YORK CITY Read before the Academy, November 11, 1919 The principles of modern research in vertebrate palaeontology are illustrated in the fifteen years' work resulting in the restoration of the massive sauropod dinosaur known as Camarasaurus, the "chambered saurian.." The animal was found near Canyon City, Colorado, in March, 1877. The first bones were described by Cope, August 23, 1877. The first at- tempted restoration was by Ryder, December 21, 1877. The bones analyzed by this research were found probably to belong to six individuals of Camarasaurus mingled with the remains of some carnivorous dinosaurs, all from the summit of the Morrison formation, now regarded as of Jurassic- Cretaceous age. In these two quarries Cope named nine new genera and fourteen new species of dinosaurs, none of which have found their way into. palaeontologic literature, excepting Camarasaurus. Out of these twenty-three names we unravel three genera, namely: One species of Camarasaurus, identical with Morosaurus Marsh. One species of Amphicaclias, close to Diplodocus Marsh. One species of Epanterias, close to Allosaurus Marsh. The working out of the Camarasaurus skeleton results in both the artica ulated restoration and the restoration of the musculature. The following are the principal characters: The neck is very flexible; anterior vertebrae of the back also freely movable; the division between the latter and the relatively rigid posterior dorsals is sharp. -
The Princeton Field Guide to Dinosaurs, Second Edition
MASS ESTIMATES - DINOSAURS ETC (largely based on models) taxon k model femur length* model volume ml x specific gravity = model mass g specimen (modeled 1st):kilograms:femur(or other long bone length)usually in decameters kg = femur(or other long bone)length(usually in decameters)3 x k k = model volume in ml x specific gravity(usually for whole model) then divided/model femur(or other long bone)length3 (in most models femur in decameters is 0.5253 = 0.145) In sauropods the neck is assigned a distinct specific gravity; in dinosaurs with large feathers their mass is added separately; in dinosaurs with flight ablity the mass of the fight muscles is calculated separately as a range of possiblities SAUROPODS k femur trunk neck tail total neck x 0.6 rest x0.9 & legs & head super titanosaur femur:~55000-60000:~25:00 Argentinosaurus ~4 PVPH-1:~55000:~24.00 Futalognkosaurus ~3.5-4 MUCPv-323:~25000:19.80 (note:downsize correction since 2nd edition) Dreadnoughtus ~3.8 “ ~520 ~75 50 ~645 0.45+.513=.558 MPM-PV 1156:~26000:19.10 Giraffatitan 3.45 .525 480 75 25 580 .045+.455=.500 HMN MB.R.2181:31500(neck 2800):~20.90 “XV2”:~45000:~23.50 Brachiosaurus ~4.15 " ~590 ~75 ~25 ~700 " +.554=~.600 FMNH P25107:~35000:20.30 Europasaurus ~3.2 “ ~465 ~39 ~23 ~527 .023+.440=~.463 composite:~760:~6.20 Camarasaurus 4.0 " 542 51 55 648 .041+.537=.578 CMNH 11393:14200(neck 1000):15.25 AMNH 5761:~23000:18.00 juv 3.5 " 486 40 55 581 .024+.487=.511 CMNH 11338:640:5.67 Chuanjiesaurus ~4.1 “ ~550 ~105 ~38 ~693 .063+.530=.593 Lfch 1001:~10700:13.75 2 M. -
The Anatomy and Phylogenetic Relationships of Antetonitrus Ingenipes (Sauropodiformes, Dinosauria): Implications for the Origins of Sauropoda
THE ANATOMY AND PHYLOGENETIC RELATIONSHIPS OF ANTETONITRUS INGENIPES (SAUROPODIFORMES, DINOSAURIA): IMPLICATIONS FOR THE ORIGINS OF SAUROPODA Blair McPhee A dissertation submitted to the Faculty of Science, University of the Witwatersrand, in partial fulfilment of the requirements for the degree of Master of Science. Johannesburg, 2013 i ii ABSTRACT A thorough description and cladistic analysis of the Antetonitrus ingenipes type material sheds further light on the stepwise acquisition of sauropodan traits just prior to the Triassic/Jurassic boundary. Although the forelimb of Antetonitrus and other closely related sauropododomorph taxa retains the plesiomorphic morphology typical of a mobile grasping structure, the changes in the weight-bearing dynamics of both the musculature and the architecture of the hindlimb document the progressive shift towards a sauropodan form of graviportal locomotion. Nonetheless, the presence of hypertrophied muscle attachment sites in Antetonitrus suggests the retention of an intermediary form of facultative bipedality. The term Sauropodiformes is adopted here and given a novel definition intended to capture those transitional sauropodomorph taxa occupying a contiguous position on the pectinate line towards Sauropoda. The early record of sauropod diversification and evolution is re- examined in light of the paraphyletic consensus that has emerged regarding the ‘Prosauropoda’ in recent years. iii ACKNOWLEDGEMENTS First, I would like to express sincere gratitude to Adam Yates for providing me with the opportunity to do ‘real’ palaeontology, and also for gladly sharing his considerable knowledge on sauropodomorph osteology and phylogenetics. This project would not have been possible without the continued (and continual) support (both emotionally and financially) of my parents, Alf and Glenda McPhee – Thank you. -
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. -
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. -
Skull Remains of the Dinosaur Saturnalia Tupiniquim (Late Triassic, Brazil): with Comments on the Early Evolution of Sauropodomorph Feeding Behaviour
RESEARCH ARTICLE Skull remains of the dinosaur Saturnalia tupiniquim (Late Triassic, Brazil): With comments on the early evolution of sauropodomorph feeding behaviour 1 2 1 Mario BronzatiID *, Rodrigo T. MuÈ llerID , Max C. Langer * 1 LaboratoÂrio de Paleontologia, Faculdade de Filosofia Ciências e Letras de Ribeirão Preto, Universidade de a1111111111 São Paulo, Ribeirão Preto, São Paulo, Brazil, 2 Centro de Apoio à Pesquisa PaleontoloÂgica, Universidade Federal de Santa Maria, Santa Maria, Rio Grande do Sul, Brazil a1111111111 a1111111111 * [email protected] (MB); [email protected] (MCL) a1111111111 a1111111111 Abstract Saturnalia tupiniquim is a sauropodomorph dinosaur from the Late Triassic (Carnian±c. 233 OPEN ACCESS Ma) Santa Maria Formation of Brazil. Due to its phylogenetic position and age, it is important for studies focusing on the early evolution of both dinosaurs and sauropodomorphs. The Citation: Bronzati M, MuÈller RT, Langer MC (2019) Skull remains of the dinosaur Saturnalia tupiniquim osteology of Saturnalia has been described in a series of papers, but its cranial anatomy (Late Triassic, Brazil): With comments on the early remains mostly unknown. Here, we describe the skull bones of one of its paratypes (only in evolution of sauropodomorph feeding behaviour. the type-series to possess such remains) based on CT Scan data. The newly described ele- PLoS ONE 14(9): e0221387. https://doi.org/ ments allowed estimating the cranial length of Saturnalia and provide additional support for 10.1371/journal.pone.0221387 the presence of a reduced skull (i.e. two thirds of the femoral length) in this taxon, as typical Editor: JuÈrgen Kriwet, University of Vienna, of later sauropodomorphs. -
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. -
Terræ Evidências Da Origem E Ascensão Dos Dinossauros
Terræ ARTIGO 10.20396/td.v16i0.8657367 Didatica Evidências da origem e ascensão dos dinossauros sauropodomorfos preservadas em leitos fossilíferos do Triássico do Sul do Brasil EVIDENCE OF THE ORIGIN AND RISE OF SAUROPODOMORPH DINOSAURS PRESERVED IN TRIASSIC BEDS FROM SOUTHERN BRAZIL RODRIGO TEMP MÜLLER1, MAURÍCIO SILVA GARCIA2, SÉRGIO DIAS-DA-SILVA2 1 - CENTRO APOIO PESQ. PALEONT. DA QUARTA COLÔNIA, UNIV. FED. SANTA MARIA, SÃO JOÃO DO POLÊSINE, BRASIL. 2 - LABORATÓRIO DE PALEOBIODIVERSIDADE TRIÁSSICA, DEPARTAMENTO DE ECOLOGIA E EVOLUÇÃO, UNIV. FED. SANTA MARIA, SANTA MARIA, BRASIL. E-MAIL: [email protected], [email protected], [email protected] Abstract: Although the sauropodomorph dinosaur group is widely known due to the giant sauropods, Citation/Citação: Müller, R. T., Garcia, their origin is still poorly understood due to the scarcity of complete skeletons and precise dating. M. S., & Silva, S. D. (2020). Evidências However, new findings and dating performed in Triassic rocks from Brazil have brought forth valuable da origem e ascensão dos dinossauros information regarding this matter. The combination of new data and more advanced investigation sauropodomorfos preservadas em leitos techniques (e.g. CT scans) have enabled the establishment of macroevolutionary patterns that guided fossilíferos do Triássico do Sul do Brasil. the initial evolution of the group. Through discoveries made in Triassic beds of Rio Grande do Sul Terræ Didatica, 16, 1-13, e020013. state, we can understand in more detail how sauropodomorphs went from small and not abundant doi:10.20396/td.v16i0.8657367 animals to the largest animals that ever walked the Earth. Keywords: Dinosauria. Evolution. Mesozoic Resumo: Embora o grupo dos dinossauros sauropodomorfos seja amplamente conhecido em virtude Era. -
Overview of Sauropod Phylogeny and Evolution
One Overview of Sauropod Phylogeny and Evolution Jeffrey A. Wilson SAUROPOD STUDIES FROM OWEN TO long bones” and “the toes being terminated by THE PRESENT strong claws” (Owen 1842:102), but this assess- ment was based on limited anatomical evidence This year marks the one hundred sixty-fourth (Owen 1875:27). Key data emerged with the dis- anniversary of Richard Owen’s (1841) description covery of abundant Cetiosaurus bones in of the first sauropod—Cetiosaurus, the “whale Oxfordshire by John Phillips. Thomas Huxley lizard”—on the basis of vertebrae and limb ele- examined this “splendid series of remains” ments from localities across England. Although before the publication of Phillips’ (1871) mono- these remains “had been examined by Cuvier graph and was the first to place Cetiosaurus within and pronounced to be cetaceous” (Buckland Dinosauria (Iguanodontidae [Huxley, 1869:35]). 1841:96), Owen (1841:458–459) demonstrated Phillips (1871) interpreted Cetiosaurus as a plant- the saurian affinities of Cetiosaurus on the basis eating dinosaur and hypothesized that its limb of several features, including the absence of epi- bones were “suited for walking.” He could not physes (growth plates) on caudal vertebrae (fig. rule out the possibility that it was amphibious, 1.1). He differentiated Cetiosaurus from other however, concluding that it was a “marsh-loving extinct saurians on the basis of its large size and or riverside animal.” Owen (1875:27) later acqui- characteristics of its vertebrae (see Upchurch esced, referring Cetiosaurus to the Dinosauria and Martin 2003:215). Owen (1841:462) con- because of its four sacral vertebrae. He admitted cluded his initial description with this assess- that it may have had some terrestrial capabilities ment: “The vertebræ, as well as the bones of the but concluded that Cetiosaurus was an estuarine extremities, prove its marine habits . -
Download Teacher's Guide
dinosaurs teacher’s guide University of Nebraska State Museum The Dinosaurs Encounter Kit has been generously funded by the Nebraska Federation of Women’s Clubs This kit was developed by the Public Programs Division of the University of Nebraska State Museum. It’s development was made possible by the input and guidance of Rosemary Thornton, Science Teacher, Lincoln Public Schools, Dr. George F. Engelmann, University of Nebraska-Omaha, and Curator of Paleontology, Mike Voorhies at the University of Nebraska State Museum. © 2001 University of Nebraska, Lincoln, Nebraska Permission is given to educators to reproduce only the UNSM activities in this booklet for classroom and training purposes. Dear Colleague, The goal of the Dinosaur Encounter Kit is to bring hands-on materials from the University of Nebraska State Museum and inquiry based activities to the classroom. It is designed to introduce some of the lesser-known aspects of the fascinating world of dinosaurs to students. It will complement and enrich existing dinosaur curricula. The objectives of this Encounter Kit are for students to: 1. investigate the diversity among dinosaurs by developing different strategies for grouping dinosaurs; 2. explore how scientists use distribution of dinosaur fossils to understand the movements of the continents; 3. obtain a better grasp of geologic time and important events that happened in earth’s history; 4. practice excavation skills and train their eyes to distinguish dinosaur bone from rock; 5. explore dinosaur behavior by creating dinosaur track records. The activities range inlength from 45 to 60 minutes. Some of the activities are more appropriate for younger students, while others are better for 4th grade and above. -
Short Review of the Present Knowledge of the Sauropoda
PRESENT KNOWLEDGE OF THE SAUROl'ODA.-HUENE. 121 SHORT REVIEW OF THE PRESENT KNOWLEDGE OF THE SAUROPODA. BY DR. FRIEDRICH BARON HUENE, PROFESSOR AT THE UNIVERSITY OF TUBINGEN, GERMANY. THE Sauropoda are the hugest continental animals the earth has ever seen. They lived from the middle Jurassic to the Danian period of the upper most Cretaceous. Much has been written about them, but nevertheless their natura! classification and development do not yet appear in a desirable clearness. In this respect the immense size of the Sauropoda has been an obstacle. The satisfactory excavation of such gigant.ic skeletons is difficult, and the preparation, which is still more important, needs trained, skilful men working for years. The scientific value of a skeleton is determined in advance by the degree of care by which, during the excavation, the original articulation or the original positions of the bones to each other in the rock is dealt "\vith by sketch-plans in scale as to make sure specially the sequence of the vertebræ. Because of the failure of this in many cases, we still know so astonishingly little about the natura! classification of the Sauropoda as a whole. Most has been written and spoken on the North American Sauropoda. Too little has been done with the earlier Sauropoda. The knowledge of the Upper Cretaceous Sauropoda until now is quite insufficient. The large amount of Tendaguru Sauropoda at Berlin and the recent excavations of the Carnegie Museum at Pittsburgh have not yet been described ; they will probably complete and alter our ideas of the development and classification of the Sauropoda.