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Mesozoic—Dinos!
MESOZOIC—DINOS! VOLUME 9, ISSUE 8, APRIL 2020 THIS MONTH DINOSAURS! • Dinosaurs ○ What is a Dinosaur? page 2 DINOSAURS! When people think paleontology, ○ Bird / Lizard Hip? page 5 they think of scientists ○ Size Activity 1 page 10 working in the hot sun of ○ Size Activity 2 page 13 Colorado National ○ Size Activity 3 page 43 Monument or the Badlands ○ Diet page 46 of South Dakota and ○ Trackways page 53 Wyoming finding enormous, ○ Colorado Fossils and fierce, and long-gone Dinosaurs page 66 dinosaurs. POWER WORDS Dinosaurs safely evoke • articulated: fossil terror. Better than any bones arranged in scary movie, these were Articulated skeleton of the Tyrannosaurus rex proper order actually living breathing • endothermic: an beasts! from the American Museum of Natural History organism produces body heat through What was the biggest dinosaur? be reviewing the information metabolism What was the smallest about dinosaurs, but there is an • metabolism: chemical dinosaur? What color were interview with him at the end of processes that occur they? Did they live in herds? this issue. Meeting him, you will within a living organism What can their skeletons tell us? know instantly that he loves his in order to maintain life What evidence is there so that job! It doesn’t matter if you we can understand more about become an electrician, auto CAREER CONNECTION how these animals lived. Are mechanic, dancer, computer • Meet Dr. Holtz, any still alive today? programmer, author, or Dinosaur paleontologist, I truly hope that Paleontologist! page 73 To help us really understand you have tremendous job more about dinosaurs, we have satisfaction, like Dr. -
A New Raptorial Dinosaur with Exceptionally Long Feathering Provides Insights Into Dromaeosaurid flight Performance
ARTICLE Received 11 Apr 2014 | Accepted 11 Jun 2014 | Published 15 Jul 2014 DOI: 10.1038/ncomms5382 A new raptorial dinosaur with exceptionally long feathering provides insights into dromaeosaurid flight performance Gang Han1, Luis M. Chiappe2, Shu-An Ji1,3, Michael Habib4, Alan H. Turner5, Anusuya Chinsamy6, Xueling Liu1 & Lizhuo Han1 Microraptorines are a group of predatory dromaeosaurid theropod dinosaurs with aero- dynamic capacity. These close relatives of birds are essential for testing hypotheses explaining the origin and early evolution of avian flight. Here we describe a new ‘four-winged’ microraptorine, Changyuraptor yangi, from the Early Cretaceous Jehol Biota of China. With tail feathers that are nearly 30 cm long, roughly 30% the length of the skeleton, the new fossil possesses the longest known feathers for any non-avian dinosaur. Furthermore, it is the largest theropod with long, pennaceous feathers attached to the lower hind limbs (that is, ‘hindwings’). The lengthy feathered tail of the new fossil provides insight into the flight performance of microraptorines and how they may have maintained aerial competency at larger body sizes. We demonstrate how the low-aspect-ratio tail of the new fossil would have acted as a pitch control structure reducing descent speed and thus playing a key role in landing. 1 Paleontological Center, Bohai University, 19 Keji Road, New Shongshan District, Jinzhou, Liaoning Province 121013, China. 2 Dinosaur Institute, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, USA. 3 Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China. 4 University of Southern California, Health Sciences Campus, BMT 403, Mail Code 9112, Los Angeles, California 90089, USA. -
Los Restos Directos De Dinosaurios Terópodos (Excluyendo Aves) En España
Canudo, J. I. y Ruiz-Omeñaca, J. I. 2003. Ciencias de la Tierra. Dinosaurios y otros reptiles mesozoicos de España, 26, 347-373. LOS RESTOS DIRECTOS DE DINOSAURIOS TERÓPODOS (EXCLUYENDO AVES) EN ESPAÑA CANUDO1, J. I. y RUIZ-OMEÑACA1,2 J. I. 1 Departamento de Ciencias de la Tierra (Área de Paleontología) y Museo Paleontológico. Universidad de Zaragoza. 50009 Zaragoza. [email protected] 2 Paleoymás, S. L. L. Nuestra Señora del Salz, 4, local, 50017 Zaragoza. [email protected] RESUMEN La mayoría de los restos fósiles de dinosaurios terópodos de España son dientes aislados y escasos restos postcraneales. La única excepción es el ornitomimosaurio Pelecanimimus polyodon, del Barremiense de Las Hoyas (Cuenca). Hay registro de terópodos en el Jurásico superior (Oxfordiense superior-Tithónico inferior), en el tránsito Jurásico-Cretácico (Tithónico superior- Berriasiense inferior) y en todos los pisos del Cretácico inferior, con excepción del Valanginiense. En el Cretácico superior únicamente hay restos en el Campaniense y Maastrichtiense. La mayor parte de las determinaciones son demasiado generales, lo que impide conocer algunas de las familias que posiblemente estén representadas. Se han reconocido: Neoceratosauria, Baryonychidae, Ornithomimosauria, Dromaeosauridae, además de terópodos indeterminados, y celurosaurios indeterminados (dientes pequeños sin dentículos). La mayoría de los restos son de Maniraptoriformes, siendo especialmente abundantes los dromeosáuridos. Las únicas excepciones son por el momento, el posible Ceratosauria del Jurásico superior de Asturias, los barionícidos del Hauteriviense-Barremiense de Burgos, Teruel y La Rioja, el posible carcharodontosáurido del Aptiense inferior de Morella y el posible abelisáurido del Campaniense de Laño. Además hay algunos terópodos incertae sedis, como los "paronicodóntidos" (entre los que se incluye Euronychodon), y Richardoestesia. -
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. -
Paleoherpetofauna Portuguesa
Rev. Esp. Herp. (2002): 17-35 17 Paleoherpetofauna Portuguesa E.G. CRESPO Centro de Biologia Ambiental – Fac. Ciências Univ. Lisboa Resumo: Nos últimos anos a importância da paleoherpetofauna portuguesa tem sido posta em evidência sobre- tudo através do seu grupo mais mediático, os dinossauros. As recentes descobertas em Portugal de vestígios de vários dinossauros, incluindo ossos, ovos, embriões, gastrólitos e pegadas, têm merecido ampla cobertura jorna- lística e têm sido oportunamente acompanhadas por intensas campanhas de divulgação, levadas a cabo pelo Mu- seu Nacional de História Natural de Lisboa, encabeçadas pelo geólogo, Professor Galopim de Carvalho. As pro- longadas e por vezes polémicas acções de sensibilização pública e política que foi necessário empreender para se preservarem muitos dos locais onde esses vestígios foram encontrados, contribuiram também para sustentar e até aumentar o interesse por este grupo de grandes répteis. A importância da paleoherpetofauna portuguesa está porém longe de se limitar apenas aos dinossauros! Em Portugal viveram muitos outros répteis e anfíbios de que existem vestígios desde o começo do Mesozói- co –Quelónios, Crocodilos, Ictiossauros, Plesiossauros, Pterossauros, Lepidossauros, “Estegossauros” e Lis- samphia– que, embora geralmente muito menos conhecidos, têm um significado evolutivo, paleogeográfico e paleoclimático extremamente importante. Na sua descoberta e estudo estiveram envolvidos, já desde o século passado, numerosos investigadores por- tugueses e estrangeiros, dos quais se destacam, entre outros, Georges Zbyszewski, Miguel Telles Antunes, Vei- ga Ferreira, H. Sauvage, A.F. Lapparent, L. Ginsburg, R.Thulborn, P. Galton. Muitos destes estudos encontram- se todavia dispersos por uma vasta gama de publicações em que, frequentemente, as referências aos répteis e aos anfíbios ou são laterais ou são apresentadas em contextos zoológicos mais abrangentes, pelo que, como parece que tem acontecido, têm passado praticamente despercebidos à maioria daqueles que se dedicam aos estudo da nossa herpetofauna actual. -
Xjiiie'icanj/Useum
XJiiie'ican1ox4tatreJ/useum PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK 24, N.Y. NUMBER 2I8I JUNE 4, I964 Relationships of the Saurischian Dinosaurs BY EDWIN H. COLBERT1 INTRODUCTION The word "Dinosauria" was coined by Sir Richard Owen in 1842 as a designation for various genera and species of extinct reptiles, the fossil bones of which were then being discovered and described in Europe. For many years this term persisted as the name for one order of reptiles and thus became well intrenched within the literature of paleontology. In- deed, since this name was associated with fossil remains that are frequently of large dimensions and spectacular shape and therefore of considerable interest to the general public, it in time became Anglicized, to take its proper place as a common noun in the English language. Almost every- body in the world is today more or less familiar with dinosaurs. As long ago as 1888, H. G. Seeley recognized the fact that the dino- saurs are not contained within a single reptilian order, but rather are quite clearly members of two distinct orders, each of which can be de- fined on the basis of many osteological characters. The structure of the pelvis is particularly useful in the separation of the two dinosaurian orders, and consequently Seeley named these two major taxonomic categories the Saurischia and the Ornithischia. This astute observation by Seeley was not readily accepted, so that for many years following the publication of his original paper proposing the basic dichotomy of the dinosaurs the 1 Chairman and Curator, Department ofVertebrate Paleontology, the American Museum of Natural History. -
Note on the Sauropod and Theropod Dinosaurs from the Upper Cretaceous of Madagascar*
EXTRACT FROM THE BULLETIN DE LA SOCIÉTÉ GÉOLOGIQUE DE FRANCE 3rd series, volume XXIV, page 176, 1896. NOTE ON THE SAUROPOD AND THEROPOD DINOSAURS FROM THE UPPER CRETACEOUS OF MADAGASCAR* by Charles DEPÉRET. (PLATE VI). Translated by Matthew Carrano Department of Anatomical Sciences SUNY at Stony Brook, September 1999 The bones of large dinosaurian reptiles described in this work were brought to me by my good friend, Mr. Dr. Félix Salètes, primary physician for the Madagascar expedition, from the environs of Maevarana, where he was charged with installing a provisional hospital. This locality is situated on the right bank of the eastern arm of the Betsiboka, 46 kilometers south of Majunga, on the northwest coast of the island of Madagascar. Not having the time to occupy himself with paleontological studies, Dr. Salètes charged one of his auxiliary agents, Mr. Landillon, company sergeant-major of the marines, with researching the fossils in the environs of the Maevarana post. Thanks to the zeal and activity of Mr. Landillon, who was not afraid to gravely expose his health in these researches, I have been able to receive the precious bones of terrestrial reptiles that are the object of this note, along with an important series of fossil marine shells. I eagerly seize the opportunity here to thank Mr. Landillon for his important shipment and for the very precise geological data which he communicated to me concerning the environs of Maevarana, and of which I will now give a short sketch. 1st. Geology of Maevarana and placement of the localities. * Original reference: Depéret, C. -
Paleopathological Analysis of a Sub-Adult Allosaurus Fragilis (MOR
Paleopathological analysis of a sub-adult Allosaurus fragilis (MOR 693) from the Upper Jurassic Morrison Formation with multiple injuries and infections by Rebecca Rochelle Laws A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences Montana State University © Copyright by Rebecca Rochelle Laws (1996) Abstract: A sub-adult Allosaurus fragilis (Museum of the Rockies specimen number 693 or MOR 693; "Big Al") with nineteen abnormal skeletal elements was discovered in 1991 in the Upper Jurassic Morrison Formation in Big Horn County, Wyoming at what became known as the "Big Al" site. This site is 300 meters northeast of the Howe Quarry, excavated in 1934 by Barnum Brown. The opisthotonic position of the allosaur indicated that rigor mortis occurred before burial. Although the skeleton was found within a fluvially-deposited sandstone, the presence of mud chips in the sandstone matrix and virtual completeness of the skeleton showed that the skeleton was not transported very far, if at all. The specific goals of this study are to: 1) provide a complete description and analysis of the abnormal bones of the sub-adult, male, A. fragilis, 2) develop a better understanding of how the bones of this allosaur reacted to infection and trauma, and 3) contribute to the pathological bone database so that future comparative studies are possible, and the hypothesis that certain abnormalities characterize taxa may be evaluated. The morphology of each of the 19 abnormal bones is described and each disfigurement is classified as to its cause: 5 trauma-induced; 2 infection-induced; 1 trauma- and infection-induced; 4 trauma-induced or aberrant, specific origin unknown; 4 aberrant; and 3 aberrant, specific origin unknown. -
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. -
Coossified Tarsometatarsi in Theropod Dinosaurs and Their Bearing on the Problem of Bird Origins
HALSZKA OSM6LSKA COOSSIFIED TARSOMETATARSI IN THEROPOD DINOSAURS AND THEIR BEARING ON THE PROBLEM OF BIRD ORIGINS OSM6LSKA, H. : Coossified tarsometatarsi in theropod dinosaurs and their bearing on the problem of bird origins, Palaeontologia Polonica, 42, 79-95, 1981. Limb remains of two small theropod dinosaurs from the Upper Cretaceous deposits of Mongolia display fused tarsometatarsi. Presence of fusion in the tarsometatarsus in some theropods is consi dered as additional evidence for the theropod origin of birds. E/misaurus rarus gen. et sp. n. is described based upon a fragmentary skeleton represented by limbs. Family Elmisauridae novo is erected to include Elmisaurus, Chirostenotes GlLMORE and Ma crophalangia STERNBERG. Key words: Dinosauria, Theropoda, bird origins, Upper Cretaceous, Mongolia. Halszka Osmolska , ZakladPaleobiologii, Polska Akademia Nauk, Al. Zw irki i Wigury 93,02-089 War szawa, Po/and. Received: June 1979. Streszczenie. - W pracy opisano szczatki malych dinozaur6w drapieznych z osad6w gornokredo wych Mongolii . Stopa tych dinozaur6w wykazuje obecnosc zrosnietego tarsomet atarsusa. Zrosniecie to stanowi dodatkowy dow6d na pochodzenie ptak6w od dinozaur6w drapieznych, Opisano nowy rodzaj i gatunek dinozaura drapieznego E/misaurus rarus, kt6ry zaliczono do nowej rodziny Elmisau ridae . Do rodziny tej, opr6cz Elmisaurus, naleza: Chirostenotes GILMORE i Macr opha/angia STERNBERG. Praca byla finansowana przez Polska Akademie Nauk w ramach problemu rniedzyresorto wego MR 11-6. INTRODUCTION During the Polish-Mongolian -
Science WORK PACK SCIENCE
SCIENCE SPECIFIC TOPICS FOR KEY STAGE 2 AGED 7 - 11 IN YEAR GROUPS 3 - 6 DINOSAURS science WORK PACK SCIENCE NOTES FOR TEACHERS SCIENCE-SPECIFIC TOPICS FOR KS2 CHILDREN AGED 7-11 IN YEAR GROUPS 3-6 Life Processes and Living Things G variation and classification G life processes G living things in their environment Mathematics / numeracy G arithmetic - addition G reasoning English / literacy G vocabulary extension General: The worksheets require: G observational skills G reading skills G arithmatic skills G The pupils need to apply some prior knowledge, but all the information required is on the sheets, posters or the actual exhibit, facilitating use on site or at school. G Specifically from the Dinosaur Family Tree worksheet, they will learn that organisms can be classified on the basis of their similarities, and that elementary arithmatic can be used to support (through quantification) observational (qualative) classification schemes. G Like with human families, family trees can be constructed over time periods.The Family Tree worksheet enables the children to place fifteen well known dinosaurs into a simplified Dinosaur Family Tree, by identifying (numerically) which line each individual sits on, and using the date given, its position on that line. G The tree also introduces the concept of geological time, and the large numbers used in its construction. Additionally, they will notice that geological time is divided and names given to those divisions. G The work can be extended, some children will notice that four distinct groupings of dinosaurs are formed as time blocks (Triassic, Late Jurassic, Early Cretaceous and Late Cretaceous). -
The Pelvic and Hind Limb Anatomy of the Stem-Sauropodomorph Saturnalia Tupiniquim (Late Triassic, Brazil)
PaleoBios 23(2):1–30, July 15, 2003 © 2003 University of California Museum of Paleontology The pelvic and hind limb anatomy of the stem-sauropodomorph Saturnalia tupiniquim (Late Triassic, Brazil) MAX CARDOSO LANGER Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, BS8 1RJ Bristol, UK. Current address: Departamento de Biologia, Universidade de São Paulo (USP), Av. Bandeirantes, 3900 14040-901 Ribeirão Preto, SP, Brazil; [email protected] Three partial skeletons allow a nearly complete description of the sacrum, pelvic girdle, and hind limb of the stem- sauropodomorph Saturnalia tupiniquim, from the Late Triassic Santa Maria Formation, South Brazil. The new morphological data gathered from these specimens considerably improves our knowledge of the anatomy of basal dinosaurs, providing the basis for a reassessment of various morphological transformations that occurred in the early evolution of these reptiles. These include an increase in the number of sacral vertebrae, the development of a brevis fossa, the perforation of the acetabulum, the inturning of the femoral head, as well as various modifications in the insertion of the iliofemoral musculature and the tibio-tarsal articulation. In addition, the reconstruction of the pelvic musculature of Saturnalia, along with a study of its locomotion pattern, indicates that the hind limb of early dinosaurs did not perform only a fore-and-aft stiff rotation in the parasagittal plane, but that lateral and medial movements of the leg were also present and important. INTRODUCTION sisting of most of the presacral vertebral series, both sides Saturnalia tupiniquim was described in a preliminary of the pectoral girdle, right humerus, partial right ulna, right fashion by Langer et al.