Dinosaurs, by William Diller Matthew
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SMITHSONIAN MISCELLANEOUS COLLECTIONS [Vol
THE DINOSAUR TRACHODON ANNECTENS By R a. LUCAS The skeleton of TracJiodon, or Claosanrns, recently placed on exhi- bition in the U. S. National Museum, is an unusually perfect example of that group of extinct reptiles, the dinosaurs. It was included in the Marsh collection and was one of two nearly complete skeletons obtained by Mr. J. B. Hatcher some years ago on Lance creek, Wyoming. The completeness of the specimen is due to the fact that the animal was either engulfed in quicksand, and so came to his end, or that by some favorable accident, such as a cloudburst or a freshet, the body was otherwise covered with sand immediately after death, and before decomposition had set in. Whatever may have happened, the result was that the bones remained in place, the ribs being attached to their respective vertebrae and the great thigh bones re- maining in their sockets, the legs even having the position they would take in walking. This is shown in pi. lxxii, for in mounting the skeleton the ends of the thigh bones were left as found. Some ex- amples of Trachodon have been obtained in which the impression of the skin was preserved in the surrounding rock, and from these it is known that this animal was covered with small, irregularly six-sided, horny plates, somewhat like those covering portions of the bodies of crocodiles. Unfortunately the wearing away of the rock in which the present specimen was contained had exposed some of the bones, and portions of them had been damaged and the front of the skull weathered away before its discovery in the summer of 1891. -
Studies on Continental Late Triassic Tetrapod Biochronology. I. the Type Locality of Saturnalia Tupiniquim and the Faunal Succession in South Brazil
Journal of South American Earth Sciences 19 (2005) 205–218 www.elsevier.com/locate/jsames Studies on continental Late Triassic tetrapod biochronology. I. The type locality of Saturnalia tupiniquim and the faunal succession in south Brazil Max Cardoso Langer* Departamento de Biologia, FFCLRP, Universidade de Sa˜o Paulo (USP), Av. Bandeirantes 3900, 14040-901 Ribeira˜o Preto, SP, Brazil Received 1 November 2003; accepted 1 January 2005 Abstract Late Triassic deposits of the Parana´ Basin, Rio Grande do Sul, Brazil, encompass a single third-order, tetrapod-bearing sedimentary sequence that includes parts of the Alemoa Member (Santa Maria Formation) and the Caturrita Formation. A rich, diverse succession of terrestrial tetrapod communities is recorded in these sediments, which can be divided into at least three faunal associations. The stem- sauropodomorph Saturnalia tupiniquim was collected in the locality known as ‘Waldsanga’ near the city of Santa Maria. In that area, the deposits of the Alemoa Member yield the ‘Alemoa local fauna,’ which typifies the first association; includes the rhynchosaur Hyperodapedon, aetosaurs, and basal dinosaurs; and is coeval with the lower fauna of the Ischigualasto Formation, Bermejo Basin, NW Argentina. The second association is recorded in deposits of both the Alemoa Member and the Caturrita Formation, characterized by the rhynchosaur ‘Scaphonyx’ sulcognathus and the cynodont Exaeretodon, and correlated with the upper fauna of the Ischigualasto Formation. Various isolated outcrops of the Caturrita Formation yield tetrapod fossils that correspond to post-Ischigualastian faunas but might not belong to a single faunal association. The record of the dicynodont Jachaleria suggests correlations with the lower part of the Los Colorados Formation, NW Argentina, whereas remains of derived tritheledontid cynodonts indicate younger ages. -
Dr. N. G. Kotadiya Dinosaurs
Dinosaurs The word dinosaur was given by SIR RICHARD OWEN and it means 'terrible lizards'. From the middle of Triassic to the end of cretaceous the dinosaurs dominated the earth. At the end of the cretaceous period the dinosaurs became extinct. The dinosaurs include two orders, namely Saurischia (Reptile-like dinosaurs) and Ornithischia (Bird-like dinosaurs) Mesozoic Reptiles Thecodonts Dinosaurs pterosaurs Marine Therapsids (Terrible lizards) (Flying reptiles) reptiles (Mammal-like reptiles) Representative Types The Mesozoic reptiles include the following types: Dinosaurs: 1. Ornithomimus 2. Tyrannosaurus 3. Ornitholestes 4. Coelophysis 5. Allosaurus 6. Brontosaurus 7. Diplodocus 8. Camptosaurus 9. Trachodonts 10. Iguanodon 11. Stegosaurus 12. Ankylosaurus 13. Monoclonius 14. Triceratops Pterosaurs: 15. Rhamphorhynchus 16. Pteranodon Marine reptiles: 17. Ichthyosaurus (fish reptiles) 18. Pliosaurus (Swan dragons) Mammal-like reptiles : 19. Varanosaurus 20. Edaphosaurus 21. Dimetrodon 22. Cynognathus 23. Tritylodon 24. Diarthrognathus Dinosaurs Tyrannosaurus (Tyrant dinosaur) Dinosaurs 1. Tyrannosaurus (Tyrant dinosaur) Tyrannosaurus was a Saurischian dinosaur about 6.09 metre tall and 15.24 meter long. It was the largest bipedal terrestrial dinosaur of the cretaceous period. The hind limbs were very strong but fore limbs and hands greatly reduced. The jaws were long with large dagger- like teeth. It was a carnivore well adapted for hunting and killing other large reptiles including other dinosaur. Dinosaurs Brontosaurus Dinosaurs 2. Brontosaurus Brontosaurus was a giant sauropod Saurischiar of the jurassic times. It was about 22.86 m long and weighed about 30-60 tons. It was a quadrupedal dinosaur with strong fore and hind limb. But the fore limbs were slightly shorter. The feet were very broad with large foot pads. -
Memorial to Carl Owen Dunbar 1891-1979 KARL M
Memorial to Carl Owen Dunbar 1891-1979 KARL M. WAAGE Peabody Museum, Yale University, P.O. Box 6666, New Haven, Connecticut 06511 Carl Owen Dunbar died suddenly at the age of 88 on April 7, 1979, while at the home of his son, just across the street from his own home in Dunedin, Florida. He is survived by his son, Carl Owen Dunbar, Jr.; his daughter, Mrs. Lora Louise Johnson of Atlanta, Geor gia; six grandchildren, and three great-grandchildren. His wife, Lora Beamer Dunbar, whom he married at Lawrence, Kansas, in September of 1914, predeceased him in December 1978. Carl was born January 1, 1891, to David and Emma Thomas Dunbar on their wheat ranch near Hal- lowell, Cherokee County, Kansas. The Dunbars were pioneer wheat farmers in Kansas Territory and among the first in that area to use powered farm machinery. From his early youth, Carl commonly ran the machines and, as he matured, served as foreman of the hired crews. Graduating from Cherokee County High School in 1909, he entered the University of Kansas the following Sep tember. Early in his undergraduate days a visiting uncle asked whether he would study any geology. “What’s geology? I never heard of it,” replied Carl. The uncle confessed that he didn’t know much about it himself, but he had a friend who was a geologist, and he thought it was great. According to Carl, “Three days later, I was enrolled in a geology course, and the instructor was W. H. Twenhofel.” Recruitment through the inspiration and encouragement of one interested individual is a familiar pattern in our profession. -
Newsletter Number 77
The Palaeontology Newsletter Contents 77 Association Business 2 Association Meetings 18 News 23 Advert: National Fossil Day 27 From our correspondents Invasion of the Dinosaur 28 PalaeoMath 101: Complex outlines 36 Future meetings of other bodies 46 Meeting Report Progressive Palaeontology 2011 54 Mystery Fossil 21: update 58 Obituary Frank K. McKinney 60 Reporter: a fossiliferous Countdown 62 Graduate opportunities in palaeontology 67 Book Reviews 68 Special Papers 85: Asteroidea 83 Palaeontology vol 54 parts 3 & 4 84–85 Discounts for PalAss members 86 Reminder: The deadline for copy for Issue no 78 is 3rd November 2011. On the Web: <http://www.palass.org/> ISSN: 0954-9900 Newsletter 77 2 Association Business Annual Meeting 2011 Notification is given of the 54th Annual General Meeting and Annual Address This will be held at the University of Plymouth on 18th December 2011, following the scientific sessions. AGENDA 1. Apologies for absence 2. Minutes of the 53rd AGM, University of Ghent 3. Trustees Annual Report for 2010 4. Accounts and Balance Sheet for 2010 5. Election of Council and vote of thanks to retiring members 6. Report on Council Awards 7. Annual address DRAFT AGM MINUTES 2010 Minutes of the Annual General Meeting held on Saturday, 18th December 2010 at the University of Ghent. 1 Apologies for absence: Prof. J. C. W. Cope 2 Minutes: Agreed a correct record 3 Trustees Annual Report for 2009. Proposed by Dr L. R. M. Cocks and seconded by Prof. G. D. Sevastopoulo, the report was agreed by unanimous vote of the meeting. 4 Accounts and Balance Sheet for 2009 . -
A Short History of Dinosaurian Osteocytes
Palaeont. afr., 34, 59-61 ( 1997) A SHORT HISTORY OF DINOSAURIAN OSTEOCYTES. by _ R.E.H. (Robin) Reid School of Geosciences, The Queen's University ofB elfast, Belfast BT7 INN, Northern Ireland. ABSRACT A recent supposed discovery of dinosauri an osteocytes by Fukuda and Obata ( 1993) ignored earli er records from more than 20 d inosaurs, dating back 150 years. Some of the bodies they identified as osteocytes are also more like ly to represent chondrocytes. KEYWORDS: Bone histology, osteocytes. INTRODUCTION Brontosaurus (pp. 302, 303), Diplodocus (pp. 304, In a recent paper, Fukuda and Obata (1993) claimed 306), Camarasaurus (p. 311, as "M orosaurus" pp. 322, the discovery of dinosaurian osteocytes, in the form of 324), Haplocanthosaurus (pp.313, 314), Allosaurus mineral casts of their lacunae and canaliculi seen in (pp. 315, 3 16), Stegosaurus (p. 321) Iguanodon (pp. hadrosaurid bones, and stated that, despite recent 326-328), Dryptosaurus (p. 344), Triceratops (p. 346), histological studies, " ... there is no information on and Anatosaurus (pp. 348-350), as "Trachodon". osteocytes in dinosaur bone ti ssues" (p. 99, para. 1). At Osteocyte Stegosaurus lacunae recorded as from that date, however, earlier studies outlined here Zanclodon (p. 262), which is now considered contained records from more than 20 dinosaurs, dating indeterminate, are probably from a prosauropod (c.f. back 150 years (Quelett 1849), and even electron Benton 1986, pp. 295-297). A preserved canalicular microscope photographs had been in print since 1966 network was noted in Brontosaurus (p. 302), though (Pawlicki, Korbel & Kubiak 1966). This note reviews a not illustrated, and lacunae affected by fungal range of relevant references, for readers not familiar enlargement, mineral infilling, loss of canaliculae or with them, and also shows that some bodies identified complete obliteration were reported from various as osteocytes by Fukuda and Obata in the articular genera. -
ZOOLOGY Exploring the Biodiversity of Colorado and Theworld
CHAPTER 4 — ZOOLOGY Exploring the Biodiversity of Colorado and the World CHAPTER 4 ZOOLOGY Exploring the Biodiversity of Colorado and the World Jeffrey T. Stephenson, Before the Museum Paula E. Cushing, The first collections of specimens that make up what is now the Denver John R. Demboski, and Museum of Nature & Science were actually established well before the Frank-T. Krell founding of the institution in 1900, the selection of a board of trustees, or the construction of a building to house and exhibit the specimens. Edwin Carter (1830–1900) (Fig. 4.1) collected Colorado birds and mammals from the 1860s through the 1890s. Born in New York in 1830, Carter arrived in Colorado in 1859 hoping to make it rich in the goldfields, but he soon became interested in the region’s natural history. He learned hide tanning and, as his prospects for hitting the mother lode faded, he earned his living selling buckskin clothing that he handcrafted. Carter supplemented these earnings by mar- keting foodstuffs and other provisions to the growing population of successful and (mostly) unsuccessful prospectors flooding the region. His interest in nature turned to concern as he observed dwindling numbers of mammals and birds, owing largely to habitat destruction and overhunting. Period photographs of the area’s mining district show a landscape largely denuded of vegetation. By the 1870s, Carter noted that many animal species were becoming scarce. The state’s forests were being devastated, ranches and farms were replacing open prairie, and some species, including the last native bison in Colorado, were on the verge of extirpation or extinction. -
The Fighting Pair
THE FIGHTING PAIR ALLOSAURUS VS STEGOSAURUS — Allosaurus “jimmadsoni” and Hesperosaurus (Stegosaurus) mjosi Upper Jurassic Period, Kimmeridgian Stage, 155 million years old Morrison Formation Dana Quarry, Ten Sleep, Washakie County, Wyoming, USA. THE ALLOSAURUS The Official State Fossil of Utah, the Allosaurus was a large theropod carnosaur of the “bird-hipped” Saurischia order that flourished primarily in North America during the Upper Jurassic Period, 155-145 million years In the spring of 2007, at the newly-investigated Dana Quarry in the Morrison Formation of Wyoming, the team from ago. Long recognized in popular culture, it bears the distinction of being Dinosauria International LLC made an exciting discovery: the beautifully preserved femur of the giant carnivorous one of the first dinosaurs to be depicted on the silver screen, the apex Allosaur. As they kept digging, their excitement grew greater; next came toe bones, leg bones, ribs, vertebrae and predator of the 1912 novel and 1925 cinema adaptation of Conan Doyle’s finally a skull: complete, undistorted and, remarkably, with full dentition. It was an incredible find; one of the most The Lost World. classic dinosaurs, virtually complete, articulated and in beautiful condition. But that was not all. When the team got The Allosaurus possessed a large head on a short neck, a broad rib-cage the field jackets back to the preparation lab, they discovered another leg bone beneath the Allosaurus skull… There creating a barrel chest, small three-fingered forelimbs, large powerful hind limbs with hoof-like feet, and a long heavy tail to act as a counter-balance. was another dinosaur in the 150 million year-old rock. -
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). -
Cranial Anatomy of Allosaurus Jimmadseni, a New Species from the Lower Part of the Morrison Formation (Upper Jurassic) of Western North America
Cranial anatomy of Allosaurus jimmadseni, a new species from the lower part of the Morrison Formation (Upper Jurassic) of Western North America Daniel J. Chure1,2,* and Mark A. Loewen3,4,* 1 Dinosaur National Monument (retired), Jensen, UT, USA 2 Independent Researcher, Jensen, UT, USA 3 Natural History Museum of Utah, University of Utah, Salt Lake City, UT, USA 4 Department of Geology and Geophysics, University of Utah, Salt Lake City, UT, USA * These authors contributed equally to this work. ABSTRACT Allosaurus is one of the best known theropod dinosaurs from the Jurassic and a crucial taxon in phylogenetic analyses. On the basis of an in-depth, firsthand study of the bulk of Allosaurus specimens housed in North American institutions, we describe here a new theropod dinosaur from the Upper Jurassic Morrison Formation of Western North America, Allosaurus jimmadseni sp. nov., based upon a remarkably complete articulated skeleton and skull and a second specimen with an articulated skull and associated skeleton. The present study also assigns several other specimens to this new species, Allosaurus jimmadseni, which is characterized by a number of autapomorphies present on the dermal skull roof and additional characters present in the postcrania. In particular, whereas the ventral margin of the jugal of Allosaurus fragilis has pronounced sigmoidal convexity, the ventral margin is virtually straight in Allosaurus jimmadseni. The paired nasals of Allosaurus jimmadseni possess bilateral, blade-like crests along the lateral margin, forming a pronounced nasolacrimal crest that is absent in Allosaurus fragilis. Submitted 20 July 2018 Accepted 31 August 2019 Subjects Paleontology, Taxonomy Published 24 January 2020 Keywords Allosaurus, Allosaurus jimmadseni, Dinosaur, Theropod, Morrison Formation, Jurassic, Corresponding author Cranial anatomy Mark A. -
Analysis of Hindlimb Muscle Moment Arms in Tyrannosaurus Rex Using a Three-Dimensional Musculoskeletal Computer Model: Implications for Stance, Gait, and Speed
Paleobiology, 31(4), 2005, pp. 676±701 Analysis of hindlimb muscle moment arms in Tyrannosaurus rex using a three-dimensional musculoskeletal computer model: implications for stance, gait, and speed John R. Hutchinson, Frank C. Anderson, Silvia S. Blemker, and Scott L. Delp Abstract.ÐMuscle moment arms are important determinants of muscle function; however, it is chal- lenging to determine moment arms by inspecting bone specimens alone, as muscles have curvilin- ear paths that change as joints rotate. The goals of this study were to (1) develop a three-dimen- sional graphics-based model of the musculoskeletal system of the Cretaceous theropod dinosaur Tyrannosaurus rex that predicts muscle-tendon unit paths, lengths, and moment arms for a range of limb positions; (2) use the model to determine how the T. rex hindlimb muscle moment arms varied between crouched and upright poses; (3) compare the predicted moment arms with previous assessments of muscle function in dinosaurs; (4) evaluate how the magnitudes of these moment arms compare with those in other animals; and (5) integrate these ®ndings with previous biome- chanical studies to produce a revised appraisal of stance, gait, and speed in T. rex. The musculo- skeletal model includes ten degrees of joint freedom (¯exion/extension, ab/adduction, or medial/ lateral rotation) and 33 main muscle groups crossing the hip, knee, ankle, and toe joints of each hindlimb. The model was developed by acquiring and processing bone geometric data, de®ning joint rotation axes, justifying muscle attachment sites, and specifying muscle-tendon geometry and paths. Flexor and extensor muscle moment arms about all of the main limb joints were estimated, and limb orientation was statically varied to characterize how the muscle moment arms changed. -
Dinosaurs.Pdf
DINOSAURS COMPILED BY HOWIE BAUM THIS IS THE FIRST OF 3 PAGES THAT HELP TO PUT THE 165 MILLION YEAR REIGN OF THE DINOSAURS, IN PERSPECTIVE. IT IS A CALENDAR THAT IS DESIGNED SO THAT ALL OF THE TIME, SINCE THE BIG BANG HAPPENED – 13.8 BILLION YEAR AGO, UP TO THE PRESENT TIME, IS COMPRESSED INTO 1 YEAR. period First Dinosaurs Dinosaurs lived for 165 million years !! Humans have only existed for 0.004% of the age of the Earth ! The rocks of the Cincinnatian series were deposited between approximately 451 and 443 million years ago, during the Ordovician period, when all the land was underwater ! BASIC DINOSAUR FACTS •Dinosaurs are a group of reptiles that have lived on Earth for about 165 million years. About 60% of dinosaurs ate plants (herbivores) and 40% ate meat (carnivores) •In 1842, the English naturalist Sir Richard Owen coined the term Dinosauria, derived from the Greek deinos, meaning “fearfully great,” and sauros, meaning “lizard.” •Dinosaur fossils have been found on all 7 continents. •All non-avian (non-bird) dinosaurs went extinct about 66 million years ago (MYA). •There are roughly 700 known species of extinct dinosaurs. •Modern birds are a kind of dinosaur because they share a common ancestor with non-avian dinosaurs. The Archosaurs consist of a diverse group of Triassic living and extinct reptiles that are subdivided into crocodiles, the 2 main types of dinosaurs, and pterosaurs. ORNITHISCHIAN AND SAURISCHIAN DINOSAURS As shown on the previous diagram, there are 2 types of Dinosaurs. Dinosaurs and reptiles have hip girdles, or pelvises, and all of them are composed of three bones: the ilium, ischium, and pubis.