PALEONTOLOGY:T. Rex Was Fie
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Postcranial Skeletal Pneumaticity in Sauropods and Its
Postcranial Pneumaticity in Dinosaurs and the Origin of the Avian Lung by Mathew John Wedel B.S. (University of Oklahoma) 1997 A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Integrative Biology in the Graduate Division of the University of California, Berkeley Committee in charge: Professor Kevin Padian, Co-chair Professor William Clemens, Co-chair Professor Marvalee Wake Professor David Wake Professor John Gerhart Spring 2007 1 The dissertation of Mathew John Wedel is approved: Co-chair Date Co-chair Date Date Date Date University of California, Berkeley Spring 2007 2 Postcranial Pneumaticity in Dinosaurs and the Origin of the Avian Lung © 2007 by Mathew John Wedel 3 Abstract Postcranial Pneumaticity in Dinosaurs and the Origin of the Avian Lung by Mathew John Wedel Doctor of Philosophy in Integrative Biology University of California, Berkeley Professor Kevin Padian, Co-chair Professor William Clemens, Co-chair Among extant vertebrates, postcranial skeletal pneumaticity is present only in birds. In birds, diverticula of the lungs and air sacs pneumatize specific regions of the postcranial skeleton. The relationships among pulmonary components and the regions of the skeleton that they pneumatize form the basis for inferences about the pulmonary anatomy of non-avian dinosaurs. Fossae, foramina and chambers in the postcranial skeletons of pterosaurs and saurischian dinosaurs are diagnostic for pneumaticity. In basal saurischians only the cervical skeleton is pneumatized. Pneumatization by cervical air sacs is the most consilient explanation for this pattern. In more derived sauropods and theropods pneumatization of the posterior dorsal, sacral, and caudal vertebrae indicates that abdominal air sacs were also present. -
Hierarchical Clustering Analysis Suppcdr.Cdr
Distance Hierarchical joiningclustering 3.0 2.5 2.0 1.5 1.0 0.5 Sinosauropteryx Caudipteryx Eoraptor Compsognathus Compsognathus Compsognathus Compsognathus Megaraptora basal Coelurosauria Noasauridae Neotheropoda non-averostran T non-tyrannosaurid Dromaeosauridae basalmost Theropoda Oviraptorosauria Compsognathidae Therizinosauria T A yrannosauroidea Compsognathus roodontidae ves Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Compsognathus Richardoestesia Scipionyx Buitreraptor Compsognathus Troodon Compsognathus Compsognathus Compsognathus Juravenator Sinosauropteryx Juravenator Juravenator Sinosauropteryx Incisivosaurus Coelophysis Scipionyx Richardoestesia Compsognathus Compsognathus Compsognathus Richardoestesia Richardoestesia Richardoestesia Richardoestesia Compsognathus Richardoestesia Juravenator Richardoestesia Richardoestesia Richardoestesia Richardoestesia Buitreraptor Saurornitholestes Ichthyornis Saurornitholestes Ichthyornis Richardoestesia Richardoestesia Richardoestesia Richardoestesia Richardoestesia Juravenator Scipionyx Buitreraptor Coelophysis Richardoestesia Coelophysis Richardoestesia Richardoestesia Richardoestesia Richardoestesia Coelophysis Richardoestesia Bambiraptor Richardoestesia Richardoestesia Velociraptor Juravenator Saurornitholestes Saurornitholestes Buitreraptor Coelophysis Coelophysis Ornitholestes Richardoestesia Richardoestesia Juravenator Saurornitholestes Velociraptor Saurornitholestes -
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. -
The Mesozoic Mesozoic Things to Think About
The Mesozoic Mesozoic Things to think about • Breakup of Pangea and its relationship to sealevel and climate • Dominance of reptiles • Origin of birds • Origin of mammals • Origin of flowers (angiosperms) • Expansion of insects • Life in the seas assumes an (almost) modern form 1 2 3 4 5 Triassic Period 248 to 206 Million Years Ago 6 The Connecticut River Valley 7 Dinosaur Footprints of the Connecticut Valley Edward Hitchcock Fossil Fish of the Connecticut Valley 8 Jurassic Period 206 to 144 Million Years Ago 9 Cretaceous Period 144 to 65 Million Years Ago 10 11 Mesozoic Ammonites 12 Cretaceous Heteromorph Ammonites Nipponites mirabilis Kamchatka, Russia Macroscaphites sp. Baculites sp. Didymoceras stevensoni Rudistid Bivalves: Jurassic- Cretaceous 13 Durania cornupastoris at Abu Roash, Western Desert near Gizah, Egypt Fringing Upper Cretaceous rudist reef reservoirs flanking basement highs, Augila oil field, eastern Libya Reef-forming rudist (Radiolites) from Sarvak Formation, Cenomanian, south Iran. 14 Biostrome of hippuritid rudists at Montagne des Cornes; Santonian, Pyrenees, France Rudistid Buildups 15 Biostrome of Vaccinites vesiculosus (Woodward, 1855); Campanian of Saiwan, Oman Monopleura marcida Albian, Viotía, Greece 16 Chalk 17 Pterosaurs Mosasaurs 18 Plesiosaurs Ichthyosaurs 19 A Dinosaur Family Tree (aka Phylogeny) 20 Sauropods Theropods 21 Dilong paradoxus Early Cretaceous, China A feathered tyrannosaurid? 22 A Dinosaur Family Tree (aka Phylogeny) Ornithopods (aka Hadrosaurs) 23 Thyreophorans (aka Ankylosaurs, etc) Margincephalians (aka Ceratopsians) 24 A Dinosaur Family Tree (aka Phylogeny) The Liaoning Fauna: An early Cretaceous Lagerstatten Some highlights: -- feathered dinosaurs -- preserved internal organs -- oldest placental mammal 25 The Liaoning Fauna The Liaoning Fauna Caudipteryx. Microraptor gui MICRORAPTOR zhaoianus. -
Body-Size Evolution in the Dinosauria
8 Body-Size Evolution in the Dinosauria Matthew T. Carrano Introduction The evolution of body size and its influence on organismal biology have received scientific attention since the earliest decades of evolutionary study (e.g., Cope, 1887, 1896; Thompson, 1917). Both paleontologists and neontologists have attempted to determine correlations between body size and numerous aspects of life history, with the ultimate goal of docu- menting both the predictive and causal connections involved (LaBarbera, 1986, 1989). These studies have generated an appreciation for the thor- oughgoing interrelationships between body size and nearly every sig- nificant facet of organismal biology, including metabolism (Lindstedt & Calder, 1981; Schmidt-Nielsen, 1984; McNab, 1989), population ecology (Damuth, 1981; Juanes, 1986; Gittleman & Purvis, 1998), locomotion (Mc- Mahon, 1975; Biewener, 1989; Alexander, 1996), and reproduction (Alex- ander, 1996). An enduring focus of these studies has been Cope’s Rule, the notion that body size tends to increase over time within lineages (Kurtén, 1953; Stanley, 1973; Polly, 1998). Such an observation has been made regarding many different clades but has been examined specifically in only a few (MacFadden, 1986; Arnold et al., 1995; Jablonski, 1996, 1997; Trammer & Kaim, 1997, 1999; Alroy, 1998). The discordant results of such analyses have underscored two points: (1) Cope’s Rule does not apply universally to all groups; and (2) even when present, size increases in different clades may reflect very different underlying processes. Thus, the question, “does Cope’s Rule exist?” is better parsed into two questions: “to which groups does Cope’s Rule apply?” and “what process is responsible for it in each?” Several recent works (McShea, 1994, 2000; Jablonski, 1997; Alroy, 1998, 2000a, 2000b) have begun to address these more specific questions, attempting to quantify patterns of body-size evolution in a phylogenetic (rather than strictly temporal) context, as well as developing methods for interpreting the resultant patterns. -
Dino Times! How Dinosaurs Lived What Did a Dinosaur’S World Look Like? Step Back in Time—About Eco-Quest 130 Million Years—To a Part of Eastern Asia Now Known As 1
Dino Times! How Dinosaurs Lived What did a dinosaur’s world look like? Step back in time—about Eco-Quest 130 million years—to a part of eastern Asia now known as 1. What similarities can you find Liaoning (“lee-ow-NING”), China. Here, in fossilized lakebeds, between the bird (Confuciusornis scientists have uncovered thousands of fossil remains, including sanctus) and Sinosauropteryx plants, insects, frogs, fish, small mammals, and even feathered prima or Dilong paradoxus dinosaurs! Together this collection creates a more complete pic- dinosaurs? Are you surprised by ture of what a dinosaur ecosystem (its community of plants, the similarities? Why or why not? animals, landscape, and weather) probably looked like. 2. Scientists believe that Dilong How did these animals and plants live together? Check out the paradoxus had a thin coat of feathers, but like its featherless illustrations below of Liaoning species discovered. Then answer cousin, the T. rex, it couldn’t fly. the questions in “Eco-Quest” to the right. What function do you think its feathers served? Think about what modern animals use feath- ers for. 3. Repenomamus giganticus was a carnivorous mammal about the B. Sinosauropteryx prima (“SIGN- size of a cat. From the plants and no-sore-AHP-ter-ix PREE-ma”), A. Eomaia scansoria (“ee- animals pictured here, what do feathered dinosaur oh-MY-ah SCAN-sor-ee- you suppose it ate? (Hint: It was- ah”), ancient mammal D. Dilong paradoxus n’t insects.) (“dee-LONG pair- 4. Scientists studied plant fossils uh-DOX-us”), feathered cousin and determined that the Liaoning of T. -
Tyrannosaurus
Natural Sciences 360 Legacy of Life Lecture 16 Dr. Stuart S. Sumida Theropoda (Including Birds) Recall: Crocodylomorpha Pterosauria Eoraptor Herrerasauridae Saurischia Ornithischia Dinosauria Archosauria THEROPODA •Pronograde bipeds. •Pneumatic (hollow) bones. •Enlarged hand. •Vestigial digits IV and V on hand. •Highly extendable digits I-III on hand. •Compact, elongate, narrow foot – usually missing digit V. Theropod Feet: Note missing V. I IV II III CERATOSAURIA: COELOPHYSOIDEA Difficult to diagnose, as they retain many primitive features: •Pronograde bipeds. •Relatively small. •Skulls are narrow, not boxy in shape. •Many undifferentiated teeth. Best known taxa: Coelophysis Dilolphosaurus “Syntarsus” Dilophosaurus: a crested ceratosaur (No, they didn’t spit.) Coelophysis, skull Coelophysis: reconstructed in northern New Mexico Sauropodomorpha THEROPODA Coelophysoidea Saurischia * Abelisauridae Theropoda Spinosauroidea Allosauroidea Tetanurae Compsognathidae Tyrannosauroidea Coelurosauria Ornithomimosauria Oviraptorisauria Maniraptora Dromaeosauridae Ceratosauria * Troodontidae Avialae CERATOSAURIA: ABELISAURIDAE •Bony outgrowths over the orbits. •Relatively short skull compared to Coelophysoidea. •Blunt snout. •Ornamentation on skull •Reduced forelimbs (like T. rex), but retain a well-developed pectoral girdle. Bony outgrowths over the orbits. Blunt snout. Relatively short skull compared to Coelophysoidea. Carnotaurus Majungatholus Sauropodomorpha THEROPODA Coelophysoidea Saurischia * Abelisauridae Theropoda Spinosauroidea Allosauroidea -
A New Feather Type in a Nonavian Theropod and the Early Evolution of Feathers
A new feather type in a nonavian theropod and the early evolution of feathers Xing Xua,1, Xiaoting Zhengb, and Hailu Youc aLaboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, 142 Xiwai Street, Beijing 100044, China; bShandong Tianyu Museum of Nature, Pingyi, Shandong 273300, China; and cInstitute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China Edited by David B. Wake, University of California, Berkeley, CA, and approved December 8, 2008 (received for review October 7, 2008) All described feathers in nonavian theropods are composite struc- tures formed by multiple filaments. They closely resemble rela- tively advanced stages predicted by developmental models of the origin of feathers, but not the earliest stage. Here, we report a feather type in two specimens of the basal therizinosaur Beipiao- saurus, in which each individual feather is represented by a single broad filament. This morphotype is congruent with the stage I morphology predicted by developmental models, and all major predicted morphotypes have now been documented in the fossil record. This congruence between the full range of paleontological and developmental data strongly supports the hypothesis that feathers evolved and initially diversified in nonavian theropods before the origin of birds and the evolution of flight. Early Cretaceous ͉ filament ͉ display eathers have been documented in most nonavian coeluro- Fsaurian theropod groups, based mainly on recent discoveries of exceptionally well-preserved specimens from the Early Cre- taceous Jehol Group of western Liaoning, China (1–4). The feathers present in these specimens can be categorized into several morphotypes, but all of them are composite structures formed by multiple slender filaments (5–7). -
Allosauroid (Dinosauria: Theropoda) Phylogeny: Conflict, Consensus, and a New Cladistic Analysis
Edinburgh Research Explorer Phylogeny of Allosauroidea (Dinosauria Citation for published version: Brusatte, SL & Sereno, PC 2008, 'Phylogeny of Allosauroidea (Dinosauria: Theropoda): Comparative analysis and resolution', Journal of Systematic Palaeontology, vol. 6, no. 2, pp. 155-182. https://doi.org/10.1017/S1477201907002404 Digital Object Identifier (DOI): 10.1017/S1477201907002404 Link: Link to publication record in Edinburgh Research Explorer Document Version: Peer reviewed version Published In: Journal of Systematic Palaeontology Publisher Rights Statement: This is an Author's Accepted Manuscript of an article published in Journal of Systematic Palaeontology copyright Taylor & Francis (2008) available online at: http://www.tandfonline.com/ (10.1080/08957950902747411) General rights Copyright for the publications made accessible via the Edinburgh Research Explorer is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The University of Edinburgh has made every reasonable effort to ensure that Edinburgh Research Explorer content complies with UK legislation. If you believe that the public display of this file breaches copyright please contact [email protected] providing details, and we will remove access to the work immediately and investigate your claim. Download date: 27. Sep. 2021 Authors Post-Print Version. Final article was published in Journal of Systematic Palaeontology by Taylor and Francis (2008) Cite As: Brusatte, SL & Sereno, PC 2008, 'Phylogeny of Allosauroidea (Dinosauria: Theropoda): Comparative analysis and resolution' Journal of Systematic Palaeontology, vol 6, no. 2, pp. 155- 182. DOI: 10.1017/S1477201907002404 PHYLOGENY OF ALLOSAUROIDEA (DINOSAURIA: THEROPODA): COMPARATIVE ANALYSIS AND RESOLUTION Stephen L. -
ON the PURPORTED PRESENCE of FOSSILIZED COLLAGEN FIBRES in an ICHTHYOSAUR and a THEROPOD DINOSAUR by FIANN M
[Palaeontology, Vol. 60, Part 3, 2017, pp. 409–422] ON THE PURPORTED PRESENCE OF FOSSILIZED COLLAGEN FIBRES IN AN ICHTHYOSAUR AND A THEROPOD DINOSAUR by FIANN M. SMITHWICK1 ,GERALDMAYR2 ,EVANT.SAITTA1 , MICHAEL J. BENTON1 and JAKOB VINTHER1,3 1School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, UK; [email protected] 2Ornithological Section, Senckenberg Research Institute and Natural History Museum, Senckenberganlage 25, Frankfurt, 60325, Germany 3School of Biological Sciences, University of Bristol, Bristol, BS8 1TQ, UK Typescript received 13 December 2016; accepted in revised form 3 March 2017 Abstract: Since the discovery of exceptionally preserved view, showing that integumentary structures have been mis- theropod dinosaurs with soft tissues in China in the 1990s, interpreted based on sedimentary features and preparation there has been much debate about the nature of filamen- marks, and that these errors have led to incorrect conclu- tous structures observed in some specimens. Sinosauropteryx sions being drawn about the existence of collagen in Sino- was the first non-avian theropod to be described with these sauropteryx and the ichthyosaur Stenopterygius. We find that structures, and remains one of the most studied examples. there is no evidence to support the idea that the integu- Despite a general consensus that the structures represent mentary structures seen in the two taxa are collagen fibres, feathers or feather homologues, a few identify them as and confirm that the most parsimonious interpretation of degraded collagen fibres derived from the skin. This latter fossilized structures that look like feather homologues in view has been based on observations of low-quality images Sinosauropteryx is that they are indeed the remains of of Sinosauropteryx, as well as the suggestion that because feather homologues. -
Teacher Guide
7 Dec 2018 - 5 May 2019 Teacher Guide Public Programs and Learning Contents Introduction 1 Exhibition Teacher Guide Overview 2 Relevant background information about dinosaurs 2 Dinosaurs featured in the exhibition 3 Organisation of this teacher guide 4 Throughlines 5 Before the Exhibition 6 Pre-exhibition learning activities 6 At the Exhibition 10 Exhibition learning activities 10 After the Exhibition 11 Post-exhibition learning activities 11 Resources for Inquiry 12 Acknowledgements TMAG thanks David Boon, Department of Education, Tasmania for his significant and valuable contribution to this guide. TMAG acknowledge the support of Gondwana Studios for the exhibition and also the use of some of their materials in this learning resource. ©Tasmanian Museum and Art Gallery 2018 All imagery, unless indicated owned by the Tasmanian Museum and Art Gallery. Disclaimer TMAG does not accept any responsibility for the accuracy or availability of any information or services on websites listed in this guide. Please note the TMAG exhibition may differ from the photographic images shown in this guide. Presenting partners Major partner Education partner Exhibition partner Media partners Cover image: Kosmoceratops and Triceratops by Luis V. Rey Introduction Today we know a lot about dinosaurs, but there is still plenty we do not know that poses outstanding questions. For example, we know that dinosaurs are not all big and that they are not all extinct, but how do we Notes: know what dinosaurs looked like? How have recent discoveries not only The exhibition activities are provided more information on what dinosaurs actually looked like, but based around a class spending also provided evidence of the evolutionary link between one group of an hour in the exhibition (four dinosaurs and modern birds? galleries). -
Unenlagiid Theropods: Are They Members of the Dromaeosauridae (Theropoda, Maniraptora)?
“main” — 2011/2/10 — 14:01 — page 117 — #1 Anais da Academia Brasileira de Ciências (2011) 83(1): 117-162 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 www.scielo.br/aabc Unenlagiid theropods: are they members of the Dromaeosauridae (Theropoda, Maniraptora)? , FEDERICO L. AGNOLIN1 2 and FERNANDO E. NOVAS1 1Laboratorio de Anatomía Comparada y Evolución de los Vertebrados Museo Argentino de Ciencias Naturales “Bernardino Rivadavia” Ángel Gallardo, 470 (1405BDB), Buenos Aires, Argentina 2Fundación de Historia Natural “Félix de Azara”, Departamento de Ciencias Naturales y Antropología CEBBAD, Universidad Maimónides, Valentín Virasoro 732 (1405BDB), Buenos Aires, Argentina Manuscript received on November 9, 2009; accepted for publication on June 21, 2010 ABSTRACT In the present paper we analyze the phylogenetic position of the derived Gondwanan theropod clade Unen- lagiidae. Although this group has been frequently considered as deeply nested within Deinonychosauria and Dromaeosauridae, most of the features supporting this interpretation are conflictive, at least. Modification of integrative databases, such as that recently published by Hu et al. (2009), produces significant changes in the topological distribution of taxa within Deinonychosauria, depicting unenlagiids outside this clade. Our analysis retrieves, in contrast, a monophyletic Avialae formed by Unenlagiidae plus Aves. Key words: Gondwana, Deinonychosauria, Dromaeosauridae, Unenlagiidae, Avialae. INTRODUCTION Until recently, the deinonychosaurian fossil record has been geographically restricted to the Northern Hemisphere (Norell and Makovicky 2004), but recent discoveries demonstrated that they were also present and highly diversified in the Southern landmasses, suggesting that an important adaptive radiation took place in Gondwana during the Cretaceous. Gondwanan dromaeosaurids have been documented from Turonian through Maastrichtian beds of Argentina (Makovicky et al.