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The Braincase, Brain and Palaeobiology of the Basal Sauropodomorph Dinosaur Thecodontosaurus Antiquus
applyparastyle “fig//caption/p[1]” parastyle “FigCapt” Zoological Journal of the Linnean Society, 2020, XX, 1–22. With 10 figures. Downloaded from https://academic.oup.com/zoolinnean/advance-article/doi/10.1093/zoolinnean/zlaa157/6032720 by University of Bristol Library user on 14 December 2020 The braincase, brain and palaeobiology of the basal sauropodomorph dinosaur Thecodontosaurus antiquus ANTONIO BALLELL1,*, J. LOGAN KING1, JAMES M. NEENAN2, EMILY J. RAYFIELD1 and MICHAEL J. BENTON1 1School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK 2Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PW, UK Received 27 May 2020; revised 15 October 2020; accepted for publication 26 October 2020 Sauropodomorph dinosaurs underwent drastic changes in their anatomy and ecology throughout their evolution. The Late Triassic Thecodontosaurus antiquus occupies a basal position within Sauropodomorpha, being a key taxon for documenting how those morphofunctional transitions occurred. Here, we redescribe the braincase osteology and reconstruct the neuroanatomy of Thecodontosaurus, based on computed tomography data. The braincase of Thecodontosaurus shares the presence of medial basioccipital components of the basal tubera and a U-shaped basioccipital–parabasisphenoid suture with other basal sauropodomorphs and shows a distinct combination of characters: a straight outline of the braincase floor, an undivided metotic foramen, an unossified gap, large floccular fossae, basipterygoid processes perpendicular to the cultriform process in lateral view and a rhomboid foramen magnum. We reinterpret these braincase features in the light of new discoveries in dinosaur anatomy. Our endocranial reconstruction reveals important aspects of the palaeobiology of Thecodontosaurus, supporting a bipedal stance and cursorial habits, with adaptations to retain a steady head and gaze while moving. -
[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. -
The Origin and Early Evolution of Dinosaurs
Biol. Rev. (2010), 85, pp. 55–110. 55 doi:10.1111/j.1469-185X.2009.00094.x The origin and early evolution of dinosaurs Max C. Langer1∗,MartinD.Ezcurra2, Jonathas S. Bittencourt1 and Fernando E. Novas2,3 1Departamento de Biologia, FFCLRP, Universidade de S˜ao Paulo; Av. Bandeirantes 3900, Ribeir˜ao Preto-SP, Brazil 2Laboratorio de Anatomia Comparada y Evoluci´on de los Vertebrados, Museo Argentino de Ciencias Naturales ‘‘Bernardino Rivadavia’’, Avda. Angel Gallardo 470, Cdad. de Buenos Aires, Argentina 3CONICET (Consejo Nacional de Investigaciones Cient´ıficas y T´ecnicas); Avda. Rivadavia 1917 - Cdad. de Buenos Aires, Argentina (Received 28 November 2008; revised 09 July 2009; accepted 14 July 2009) ABSTRACT The oldest unequivocal records of Dinosauria were unearthed from Late Triassic rocks (approximately 230 Ma) accumulated over extensional rift basins in southwestern Pangea. The better known of these are Herrerasaurus ischigualastensis, Pisanosaurus mertii, Eoraptor lunensis,andPanphagia protos from the Ischigualasto Formation, Argentina, and Staurikosaurus pricei and Saturnalia tupiniquim from the Santa Maria Formation, Brazil. No uncontroversial dinosaur body fossils are known from older strata, but the Middle Triassic origin of the lineage may be inferred from both the footprint record and its sister-group relation to Ladinian basal dinosauromorphs. These include the typical Marasuchus lilloensis, more basal forms such as Lagerpeton and Dromomeron, as well as silesaurids: a possibly monophyletic group composed of Mid-Late Triassic forms that may represent immediate sister taxa to dinosaurs. The first phylogenetic definition to fit the current understanding of Dinosauria as a node-based taxon solely composed of mutually exclusive Saurischia and Ornithischia was given as ‘‘all descendants of the most recent common ancestor of birds and Triceratops’’. -
A Basal Lithostrotian Titanosaur (Dinosauria: Sauropoda) with a Complete Skull: Implications for the Evolution and Paleobiology of Titanosauria
RESEARCH ARTICLE A Basal Lithostrotian Titanosaur (Dinosauria: Sauropoda) with a Complete Skull: Implications for the Evolution and Paleobiology of Titanosauria Rubén D. F. Martínez1*, Matthew C. Lamanna2, Fernando E. Novas3, Ryan C. Ridgely4, Gabriel A. Casal1, Javier E. Martínez5, Javier R. Vita6, Lawrence M. Witmer4 1 Laboratorio de Paleovertebrados, Universidad Nacional de la Patagonia San Juan Bosco, Comodoro Rivadavia, Chubut, Argentina, 2 Section of Vertebrate Paleontology, Carnegie Museum of Natural History, Pittsburgh, Pennsylvania, United States of America, 3 Laboratorio de Anatomía Comparada y Evolución de los Vertebrados, Museo Argentino de Ciencias Naturales, Buenos Aires, Argentina, 4 Department of Biomedical Sciences, Heritage College of Osteopathic Medicine, Ohio University, Athens, Ohio, United States of America, 5 Hospital Regional de Comodoro Rivadavia, Comodoro Rivadavia, Chubut, Argentina, 6 Resonancia Magnética Borelli, Comodoro Rivadavia, Chubut, Argentina * [email protected] OPEN ACCESS Citation: Martínez RDF, Lamanna MC, Novas FE, Ridgely RC, Casal GA, Martínez JE, et al. (2016) A Basal Lithostrotian Titanosaur (Dinosauria: Abstract Sauropoda) with a Complete Skull: Implications for the Evolution and Paleobiology of Titanosauria. PLoS We describe Sarmientosaurus musacchioi gen. et sp. nov., a titanosaurian sauropod dino- ONE 11(4): e0151661. doi:10.1371/journal. saur from the Upper Cretaceous (Cenomanian—Turonian) Lower Member of the Bajo Bar- pone.0151661 real Formation of southern Chubut Province in -
71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas. -
Massospondylus Carinatus Owen 1854 (Dinosauria: Sauropodomorpha) from the Lower Jurassic of South Africa: Proposed Conservation of Usage by Designation of a Neotype
Massospondylus carinatus Owen 1854 (Dinosauria: Sauropodomorpha) from the Lower Jurassic of South Africa: Proposed conservation of usage by designation of a neotype Adam M. Yates1* & Paul M. Barrett2 1Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, Private Bag 3, WITS, 2050 Johannesburg, South Africa 2Department of Palaeontology, The Natural History Museum, Cromwell Road, London, SW7 5BD, U.K. Received 17 February 2010. Accepted 12 November 2010 The purpose of this article is to preserve the usage of the binomen Massospondylus carinatus by designating a neotype specimen. Massospondylus is the most abundant basal sauropodomorph dinosaur from the Early Jurassic strata of southern Africa. This taxon forms the basis for an extensive palaeobiological literature and is the eponym of Massospondylidae and the nominal taxon of a biostratigraphical unit in current usage, the ‘Massospondylus Range Zone’. The syntype series of M. carinatus (five disarticulated and broken vertebrae) was destroyed during World War II, but plaster casts and illustrations of the material survive. Nonetheless, these materials cannot act as type material for this taxon under the rules of the ICZN Code. In order to avoid nomenclatural instability, we hereby designate BP/1/4934 (a skull and largely complete postcranial skeleton) as the neotype of Massospondylus carinatus. Keywords: Dinosauria, Sauropodomorpha, Massospondylidae, Massospondylus, Massospondylus carinatus, neotype, South Africa, upper Elliot Formation, Early Jurassic. INTRODUCTION same taxon, possibly even the same individual, as at least Richard Owen described and named Massospondylus some of the syntype series of Massospondylus carinatus. carinatus (1854, p. 97) with carinatus as the type species of Their initial separation from Massospondylus carinatus the genus by monotypy. -
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. -
Cáscaras De Huevos De Dinosaurios De La Formación Allen (Campaniano-Maastrichtiano), En Salitral Moreno, Provincia De Río Negro, Argentina
AMEGHINIANA (Rev. Asoc. Paleontol. Argent.) - 43 (3): 513-528. Buenos Aires, 30-9-2006 ISSN 0002-7014 Cáscaras de huevos de dinosaurios de la Formación Allen (Campaniano-Maastrichtiano), en Salitral Moreno, provincia de Río Negro, Argentina María Edith SIMÓN1 Abstract. DINOSAUR EGGSHELLS FROM THE ALLEN FORMATION (CAMPANIAN-MAASTRICHTIAN), AT SALITRAL MORENO, RÍO NEGRO PROVINCE, ARGENTINA. A detailed description of two morphotypes of dinosaur eggshells from Salitral Moreno, Rio Negro Province (Allen Formation, Upper Cretaceous) is presented. One of them is described as Patagoolithus salitralensis, a new oogenus et oospecies nov. belonging to the Megaloolithidae, and the second is referred as ?Faveoloolithidae, oogenus et oospecies indet. A detailed ultrastructural description of both morphotypes is provided, as well as, the chemical and mineralogical analysis of ?Faveoloolithidae oogen. et oospec. indet. In the studied sections, three eggshell-bearing levels were recognized. In the lower one (NH1) Patagoolithus salitralensis is associated to a diverse fauna of di- nosaurs, chelonians and invertebrates, and the few shell fragments are dispersed, suggesting deposition in an alluvial plain or disintegrated eggs. In NH2 and NH3, only eggshells of ?Faveoloolithidae oogenus et oospecies indet. were found. NH2 shows lateral variations in the inferred degree of transport and den- sity of the shell fragments in different sections. NH3 bears small shell fragments of the same morphotype decreasing in number towards the top. NH1 and NH3 bear rizolithes and alveolar structures, characteris- tic of calcretes, which could be indicative of palaeosoils. Resumen. En el presente trabajo se describen en detalle dos morfotipos de cáscaras de huevos de di- nosaurios hallados en Salitral Moreno (Formación Allen, Cretácico Superior), en la provincia de Río Negro. -
First Ornithopod Remains from the Bajo De La Carpa Formation (Santonian, Upper Cretaceous), Northern Patagonia, Argentina
Cretaceous Research 83 (2018) 182e193 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes First ornithopod remains from the Bajo de la Carpa Formation (Santonian, Upper Cretaceous), northern Patagonia, Argentina * Penelope Cruzado-Caballero a, , Leonardo S. Filippi b, Ariel H. Mendez a, Alberto C. Garrido c, d, Ignacio Díaz-Martínez a a Instituto de Investigacion en Paleobiología y Geología (CONICET-UNRN), Av. Roca 1242, General Roca, Río Negro, Argentina b Museo Municipal Argentino Urquiza, Jujuy y Chaco s/n, Rincon de los Sauces, Neuquen, Argentina c Museo Provincial de Ciencias Naturales “Prof. Dr. Juan Olsacher”, Direccion Provincial de Minería, Etcheluz y Ejercito Argentino, Zapala, Neuquen, Argentina d Departamento Geología y Petroleo, Facultad de Ingeniería, Universidad Nacional del Comahue, Buenos Aires 1400, Neuquen, Argentina article info abstract Article history: In the last decades, the Argentinian ornithopod record has been increased with new and diverse bone Received 29 March 2017 remains found along all the Upper Cretaceous. Most of them are very incomplete and represent taxa of Received in revised form different size. As result, the studies about the palaeobiodiversity of the Ornithopoda clade in South 24 July 2017 America are complex. In this paper, new postcranial remains of an indeterminate medium-sized Accepted in revised form 30 July 2017 ornithopod from the Santonian Bajo de la Carpa Formation (Rincon de los Sauces, Neuquen province) Available online 12 August 2017 are presented. They present diagnostic features of the Ornithopoda clade, and several characters that relate them with other Argentinian ornithopods, especially with the medium-sized members of the Keywords: Ornithischia Elasmaria clade sensu Calvo et al. -
Redalyc.A New Titanosaur Sauropod from the Atacama Desert, Chile
Anais da Academia Brasileira de Ciências ISSN: 0001-3765 [email protected] Academia Brasileira de Ciências Brasil KELLNER, ALEXANDER W.A.; RUBILAR-ROGERS, DAVID; VARGAS, ALEXANDER; SUÁREZ, MARIO A new titanosaur sauropod from the Atacama Desert, Chile Anais da Academia Brasileira de Ciências, vol. 83, núm. 1, marzo, 2011, pp. 211-219 Academia Brasileira de Ciências Rio de Janeiro, Brasil Available in: http://www.redalyc.org/articulo.oa?id=32717681010 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative “main” — 2011/2/10 — 15:28 — page 211 — #1 Anais da Academia Brasileira de Ciências (2011) 83(1): 211-219 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 www.scielo.br/aabc A new titanosaur sauropod from the Atacama Desert, Chile ALEXANDER W.A. KELLNER1, DAVID RUBILAR-ROGERS2, ALEXANDER VARGAS3 and MARIO SUÁREZ4 1Setor de Paleovertebrados, Departamento de Geologia e Paleontologia, Museu Nacional/Universidade Federal do Rio de Janeiro, Quinta da Boa Vista s/n, São Cristóvão, 20940-040 Rio de Janeiro, RJ, Brasil 2Área Paleontología, Museo Nacional de Historia Natural, Casilla 787, Santiago, Chile 3Departamento de Biología, Facultad de Ciencias, Universidad de Chile, Las Palmeras 3425, Ñuñoa, Casilla 653, Santiago, Chile 4Museo Paleontológico de Caldera, Av. Wheelwrigth 001, Caldera, Chile Manuscript received on December 22, 2010; accepted for publication on January 12, 2011 ABSTRACT Partial remains of a titanosaur sauropod collected in the Tolar Formation (Upper Cretaceous) at the Atacama Desert (Antofagasta Region), northern Chile, is described, and a new species, Atacamatitan chilensis gen. -
From the Adamantina Formation, Bauru Group, Upper Cretaceous of Brazil and the Phylogenetic Relationships of Aeolosaurini
Zootaxa 3085: 1–33 (2011) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2011 · Magnolia Press ISSN 1175-5334 (online edition) A new sauropod (Macronaria, Titanosauria) from the Adamantina Formation, Bauru Group, Upper Cretaceous of Brazil and the phylogenetic relationships of Aeolosaurini RODRIGO M. SANTUCCI1 & ANTONIO C. DE ARRUDA-CAMPOS2 1Universidade de Brasília - Faculdade UnB Planaltina, Brasília-DF, 73300-000, Brazil. E-mail: [email protected] 2Museu de Paleontologia de Monte Alto, Praça do Centenário, s/n. Monte Alto-SP, 15910-000, Brazil. E-mail: [email protected] Table of contents Abstract . 1 Introduction . 2 Historical background . 2 Geological setting . 4 Systematic Palaeontology . 4 DINOSAURIA Owen, 1842 . 4 SAURISCHIA Seeley, 1887 . 4 SAUROPODA Marsh, 1878 . 4 MACRONARIA Wilson and Sereno, 1998. 4 TITANOSAURIFORMES Salgado, Coria and Calvo, 1997b. 4 TITANOSAURIA Bonaparte and Coria, 1993 . 4 AEOLOSAURINI Franco-Rosas, Salgado, Rosas and Carvalho, 2004 . 5 Aeolosaurus Powell, 1987 . 5 Aeolosaurus rionegrinus Powell, 1987 . 5 Aeolosaurus maximus sp. nov. 6 Phylogenetic analysis . 17 Comparison and discussion . 19 Conclusions . 25 Acknowledgements . 25 References . 26 APPENDIX 1. 29 APPENDIX 2. 29 Abstract Remains of a new titanosaur, Aeolosaurus maximus sp. nov., from the Adamantina Formation (Upper Cretaceous), Bauru Group, São Paulo State of Brazil are described. The new species is represented by a single partially articulated skeleton and is characterized by having a well-developed posterior protuberance below the articular area on the anterior and middle haemal arches and a lateral bulge on the distal portion of the articular process of the mid-posterior haemal arches. It shares with other Aeolosaurus species the presence of prezygapophyses curved downward on anterior caudal vertebrae and hae- mal arches with double articular facets set in a concave posterodorsal surface. -
Gastroliths in an Ornithopod Dinosaur
Brief report Acta Palaeontologica Polonica 53 (2): 351–355, 2008 Gastroliths in an ornithopod dinosaur IGNACIO A. CERDA Gastroliths (stomach stones) are known from many extant Institutional abbreviations.—MCSPv, Vertebrate paleontology and extinct vertebrates, including dinosaurs. Reported here collection of the Museo de Cinco Saltos, Río Negro Province, is the first unambiguous record of gastroliths in an ornitho− Argentina; MUCPv, Vertebrate paleontology collection of the pod dinosaur. Clusters of small stones found in the abdomi− Museo de la Universidad Nacional del Comahue, Neuquén nal region of three articulated skeletons of Gasparinisaura Province, Argentina. cincosaltensis were identified as gastroliths on the basis of taphonomic and sedimentologic evidence. The large number Material and geologic setting of stones found in each individual, their size, and the fact that Gasparinisaura cincosaltensis was herbivorous, all sug− Three specimens of Gasparinisaura cincosaltensis, MUCPv 213, gest that they were ingested as a result of lithophagy rather MCSPv 111, and MCSPv 112, were collected near the city of than accidental swallowing. Cinco Saltos (Río Negro Province, Patagonia, Argentina) (Fig. 1), in mudstones and sandstones of the early Campanian Anacleto Introduction Formation, in the uppermost portion of the Neuquén Group (Ramos 1981; Dingus et al. 2000). MUCPv 213 (Fig. 2A) consists Gastroliths or geo−gastroliths sensu Wings (2007) are known in of a partial skeleton that includes cranial and postcranial elements many taxa of extant and fossil vertebrates (Whittle and Everhart (see Salgado et al. 1997 for a detailed anatomical description). A 2000). Gastroliths have been occasionally reported in non−avian portion of the preserved elements (both incomplete humeri articu− dinosaurs (Wings 2004) but only few cases can withstand rigorous lated with both radii and ulnae, several posterior dorsal ribs from testing.