The Dentition of Megalosaurid Theropods
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Basal abelisaurid and carcharodontosaurid theropods from the Lower Cretaceous Elrhaz Formation of Niger PAUL C. SERENO and STEPHEN L. BRUSATTE Sereno, P.C. and Brusatte, S.L. 2008. Basal abelisaurid and carcharodontosaurid theropods from the Lower Cretaceous Elrhaz Formation of Niger. Acta Palaeontologica Polonica 53 (1): 15–46. We report the discovery of basal abelisaurid and carcharodontosaurid theropods from the mid Cretaceous (Aptian– Albian, ca. 112 Ma) Elrhaz Formation of the Niger Republic. The abelisaurid, Kryptops palaios gen. et sp. nov., is repre− sented by a single individual preserving the maxilla, pelvic girdle, vertebrae and ribs. Several features, including a maxilla textured externally by impressed vascular grooves and a narrow antorbital fossa, clearly place Kryptops palaios within Abelisauridae as its oldest known member. The carcharodontosaurid, Eocarcharia dinops gen. et sp. nov., is repre− sented by several cranial bones and isolated teeth. Phylogenetic analysis places it as a basal carcharodontosaurid, similar to Acrocanthosaurus and less derived than Carcharodontosaurus and Giganotosaurus. The discovery of these taxa sug− gests that large body size and many of the derived cranial features of abelisaurids and carcharodontosaurids had already evolved by the mid Cretaceous. The presence of a close relative of the North American genus Acrocanthosaurus on Af− rica suggests that carcharodontosaurids had already achieved a trans−Tethyan distribution by the mid Cretaceous. Key words: Theropod, abelisaurid, allosauroid, carcharodontosaurid, Kryptops, Eocarcharia, Cretaceous, Africa. Paul C. Sereno [[email protected]], Department of Organismal Biology and Anatomy, University of Chicago, 1027 E. 57th Street, Chicago, Illinois, 60637, USA; Stephen L. Brusatte [[email protected]], Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, United Kingdom. -
Fused and Vaulted Nasals of Tyrannosaurid Dinosaurs: Implications for Cranial Strength and Feeding Mechanics
Fused and vaulted nasals of tyrannosaurid dinosaurs: Implications for cranial strength and feeding mechanics ERIC SNIVELY, DONALD M. HENDERSON, and DOUG S. PHILLIPS Snively, E., Henderson, D.M., and Phillips, D.S. 2006. Fused and vaulted nasals of tyrannosaurid dinosaurs: Implications for cranial strength and feeding mechanics. Acta Palaeontologica Polonica 51 (3): 435–454. Tyrannosaurid theropods display several unusual adaptations of the skulls and teeth. Their nasals are fused and vaulted, suggesting that these elements braced the cranium against high feeding forces. Exceptionally high strengths of maxillary teeth in Tyrannosaurus rex indicate that it could exert relatively greater feeding forces than other tyrannosaurids. Areas and second moments of area of the nasals, calculated from CT cross−sections, show higher nasal strengths for large tyrannosaurids than for Allosaurus fragilis. Cross−sectional geometry of theropod crania reveals high second moments of area in tyrannosaurids, with resulting high strengths in bending and torsion, when compared with the crania of similarly sized theropods. In tyrannosaurids trends of strength increase are positively allomeric and have similar allometric expo− nents, indicating correlated progression towards unusually high strengths of the feeding apparatus. Fused, arched nasals and broad crania of tyrannosaurids are consistent with deep bites that impacted bone and powerful lateral movements of the head for dismembering prey. Key words: Theropoda, Carnosauria, Tyrannosauridae, biomechanics, feeding mechanics, computer modeling, com− puted tomography. Eric Snively [[email protected]], Department of Biological Sciences, University of Calgary, 2500 University Drive NW, Calgary, Alberta T2N 1N4, Canada; Donald M. Henderson [[email protected]], Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, Alberta T0J 0Y0, Canada; Doug S. -
PALEONTOLOGY and BIOSTRATIGRAPHY of MONGOLIA the JOINT SOVIET-MONGOLIAN PALEONTOLOGICAL EXPEDITION (Transactions, Vol
PALEONTOLOGY AND BIOSTRATIGRAPHY OF MONGOLIA THE JOINT SOVIET-MONGOLIAN PALEONTOLOGICAL EXPEDITION (Transactions, vol. 3) EDITORIAL BOARD: N. N. Kramarenko (editor-in-chief) B. Luvsandansan, Yu. I. Voronin, R. Barsbold, A. K. Rozhdestvensky, B. A. Trofimov, V. Yu. Reshetov 1976 S. M. Kurzanov A NEW CARNOSAUR FROM THE LATE CRETACEOUS OF NOGON-TSAV, MONGOLIA* The Upper Cretaceous locality of Nogon-Tsav, located in the Zaltaika Gobi, 20 km NW of Mt. Ongon-Ulan-Ula, was discovered by geologists of the MNR. Then, in a series of years (1969–1971, 1973) the joint Soviet-Mongolian Geological Expedition investigated the site. According to the oral report of B. Yu. Reshetova, the deposits in this region are composed basically of sandstone and clay, clearly subdivided into two deposits. The lower great thickness contains many complete skulls, separate bones of tarbosaurs, ornithomimids, and claws of therizinosaurs. The upper red-colored beds are characterized only by scattered fragments of skulls. The fragments described below are of a new carnivorous dinosaur, Alioramus remotus (coll. South Goby region), from the family Tyrannosauridae, which occurs in the lower gray beds. Genus Alioramus Kurzanov, gen. nov. G e n u s n a m e from alius (Lat.) – other, ramus (Lat.) – branch; masc. G e n o t y p e — A. remotus Kurzanov, sp. nov., Upper Cretaceous, Nemegetinskaya suite, southern Mongolia. D i a g n o s i s . Tyrannosaurid of average size. Skull low, with highly elongated jaws. Nasals with well-developed separate crests of 1–l.5 cm height. Second antorbital fenestrae displaced forward, reaching the anterior end of the 5th tooth. -
A Computational Analysis of Limb and Body Dimensions in Tyrannosaurus Rex with Implications for Locomotion, Ontogeny, and Growth
A Computational Analysis of Limb and Body Dimensions in Tyrannosaurus rex with Implications for Locomotion, Ontogeny, and Growth John R. Hutchinson1*, Karl T. Bates2, Julia Molnar1, Vivian Allen1, Peter J. Makovicky3 1 Structure and Motion Laboratory, Department of Veterinary Basic Sciences, The Royal Veterinary College, Hatfield, Hertfordshire, United Kingdom, 2 Department of Musculoskeletal Biology, Institute of Aging and Chronic Disease, University of Liverpool, Liverpool, United Kingdom, 3 Department of Geology, Field Museum of Natural History, Chicago, Illinois, United States of America Abstract The large theropod dinosaur Tyrannosaurus rex underwent remarkable changes during its growth from ,10 kg hatchlings to .6000 kg adults in ,20 years. These changes raise fascinating questions about the morphological transformations involved, peak growth rates, and scaling of limb muscle sizes as well as the body’s centre of mass that could have influenced ontogenetic changes of locomotion in T. rex. Here we address these questions using three-dimensionally scanned computer models of four large, well-preserved fossil specimens as well as a putative juvenile individual. Furthermore we quantify the variations of estimated body mass, centre of mass and segment dimensions, to characterize inaccuracies in our reconstructions. These inaccuracies include not only subjectivity but also incomplete preservation and inconsistent articulations of museum skeletons. Although those problems cause ambiguity, we conclude that adult T. rex had body masses around 6000–8000 kg, with the largest known specimen (‘‘Sue’’) perhaps ,9500 kg. Our results show that during T. rex ontogeny, the torso became longer and heavier whereas the limbs became proportionately shorter and lighter. Our estimates of peak growth rates are about twice as rapid as previous ones but generally support previous methods, despite biases caused by the usage of scale models and equations that underestimate body masses. -
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. -
Implications for Predatory Dinosaur Macroecology and Ontogeny in Later Late Cretaceous Asiamerica
Canadian Journal of Earth Sciences Theropod Guild Structure and the Tyrannosaurid Niche Assimilation Hypothesis: Implications for Predatory Dinosaur Macroecology and Ontogeny in later Late Cretaceous Asiamerica Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2020-0174.R1 Manuscript Type: Article Date Submitted by the 04-Jan-2021 Author: Complete List of Authors: Holtz, Thomas; University of Maryland at College Park, Department of Geology; NationalDraft Museum of Natural History, Department of Geology Keyword: Dinosaur, Ontogeny, Theropod, Paleocology, Mesozoic, Tyrannosauridae Is the invited manuscript for consideration in a Special Tribute to Dale Russell Issue? : © The Author(s) or their Institution(s) Page 1 of 91 Canadian Journal of Earth Sciences 1 Theropod Guild Structure and the Tyrannosaurid Niche Assimilation Hypothesis: 2 Implications for Predatory Dinosaur Macroecology and Ontogeny in later Late Cretaceous 3 Asiamerica 4 5 6 Thomas R. Holtz, Jr. 7 8 Department of Geology, University of Maryland, College Park, MD 20742 USA 9 Department of Paleobiology, National Museum of Natural History, Washington, DC 20013 USA 10 Email address: [email protected] 11 ORCID: 0000-0002-2906-4900 Draft 12 13 Thomas R. Holtz, Jr. 14 Department of Geology 15 8000 Regents Drive 16 University of Maryland 17 College Park, MD 20742 18 USA 19 Phone: 1-301-405-4084 20 Fax: 1-301-314-9661 21 Email address: [email protected] 22 23 1 © The Author(s) or their Institution(s) Canadian Journal of Earth Sciences Page 2 of 91 24 ABSTRACT 25 Well-sampled dinosaur communities from the Jurassic through the early Late Cretaceous show 26 greater taxonomic diversity among larger (>50kg) theropod taxa than communities of the 27 Campano-Maastrichtian, particularly to those of eastern/central Asia and Laramidia. -
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. -
The Nonavian Theropod Quadrate II: Systematic Usefulness, Major Trends and Cladistic and Phylogenetic Morphometrics Analyses
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/272162807 The nonavian theropod quadrate II: systematic usefulness, major trends and cladistic and phylogenetic morphometrics analyses Article · January 2014 DOI: 10.7287/peerj.preprints.380v2 CITATION READS 1 90 3 authors: Christophe Hendrickx Ricardo Araujo University of the Witwatersrand Technical University of Lisbon 37 PUBLICATIONS 210 CITATIONS 89 PUBLICATIONS 324 CITATIONS SEE PROFILE SEE PROFILE Octávio Mateus University NOVA of Lisbon 224 PUBLICATIONS 2,205 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Nature and Time on Earth - Project for a course and a book for virtual visits to past environments in learning programmes for university students (coordinators Edoardo Martinetto, Emanuel Tschopp, Robert A. Gastaldo) View project Ten Sleep Wyoming Jurassic dinosaurs View project All content following this page was uploaded by Octávio Mateus on 12 February 2015. The user has requested enhancement of the downloaded file. The nonavian theropod quadrate II: systematic usefulness, major trends and cladistic and phylogenetic morphometrics analyses Christophe Hendrickx1,2 1Universidade Nova de Lisboa, CICEGe, Departamento de Ciências da Terra, Faculdade de Ciências e Tecnologia, Quinta da Torre, 2829-516, Caparica, Portugal. 2 Museu da Lourinhã, 9 Rua João Luis de Moura, 2530-158, Lourinhã, Portugal. s t [email protected] n i r P e 2,3,4,5 r Ricardo Araújo P 2 Museu da Lourinhã, 9 Rua João Luis de Moura, 2530-158, Lourinhã, Portugal. 3 Huffington Department of Earth Sciences, Southern Methodist University, PO Box 750395, 75275-0395, Dallas, Texas, USA. -
Index of Subjects
Cambridge University Press 978-1-108-47594-5 — Dinosaurs 4th Edition Index More Information INDEX OF SUBJECTS – – – A Zuul, 275 276 Barrett, Paul, 98, 335 336, 406, 446 447 Ankylosauridae Barrick, R, 383–384 acetabulum, 71, 487 characteristics of, 271–273 basal dinosauromorph, 101 acromial process, 271, 273, 487 cladogram of, 281 basal Iguanodontia, 337 actual diversity, 398 defined, 488 basal Ornithopoda, 336 adenosine diphosphate, see ADP evolution of, 279 Bates, K. T., 236, 360 adenosine triphosphate, see ATP ankylosaurids, 275–276 beak, 489 ADP (adenosine diphosphate), 390, 487 anpsids, 76 belief systems, 474, 489 advanced characters, 55, 487 antediluvian period, 422, 488 Bell, P. R., 162 aerobic metabolism, 391, 487 anterior position, 488 bennettitaleans, 403, 489 – age determination (dinosaur), 354 357 antorbital fenestra, 80, 488 benthic organisms, 464, 489 Age of Dinosaurs, 204, 404–405 Arbour, Victoria, 277 Benton, M. J., 2, 104, 144, 395, 402–403, akinetic movement, see kinetic movement Archibald, J. D., 467, 469 444–445, 477–478 Alexander, R. M., 361 Archosauria, 80, 88–90, 203, 488 Berman, D. S, 236–237 allometry, 351, 487 Archosauromorpha, 79–81, 488 Beurien, Karl, 435 altricial offspring, 230, 487 archosauromorphs, 401 bidirectional respiration, 350 Alvarez, Luis, 455 archosaurs, 203, 401 Big Al, 142 – Alvarez, Walter, 442, 454 455, 481 artifacts, 395 biogeography, 313, 489 Alvarezsauridae, 487 Asaro, Frank, 455 biomass, 415, 489 – alvarezsaurs, 168 169 ascending process of the astragalus, 488 biosphere, 2 alveolus/alveoli, -
Limb Design, Function and Running Performance in Ostrich-Mimics and Tyrannosaurs
GAIA Nº 15, LISBOA/LISBON, DEZEMBRO/DECEMBER 1998, pp. 257-270 (ISSN: 0871-5424) LIMB DESIGN, FUNCTION AND RUNNING PERFORMANCE IN OSTRICH-MIMICS AND TYRANNOSAURS Gregory S. PAUL 3109 N Calvert St. Side Apt., BALTIMORE MD 21218. USA ABSTRACT: Examination of the limb morphology of small ornithomimids and large tyranno- saurids shows that they remained remarkably constant in design regardless of size. The changes that were present were consistent with maintaining limb strength and function constant with size. It is concluded that ornithomimid and tyrannosaurid legs functioned in a similar manner, and always exhibit the features normally associated with a fast running gait. This is in contrast to modern animals, in which elephants as gigantic as large tyranno- saurids have limbs that are modified for a slow walking gait. INTRODUCTION to run observed in elephants. The hypothesis can be challenged if it can be shown that at least some ex- Because they had long, gracile, bird-like legs, it tinct giants retained the skeletal adaptations for run- has long been accepted that the smaller predatory ning observed in smaller species, and in their own dinosaurs were swift runners (O [& GREG- SBORN offspring. In turn, the hypothesis that giants can run ], 1916; COLBERT, 1961; RUSSELL, 1972; ORY fast if they retain limbs similar to smaller runners can C , 1978; THULBORN, 1982; PAUL, 1988; OOMBS be challenged if it is shown that the skeleton is too H , 1994). Much more controversial has been OLTZ vulnerable to structural failure. the locomotory abilities of their giant relatives, which have been restored as no faster than elephants BODY MASSES (LAMBE, 1917; HALSTEAD &HALSTEAD, 1981; THUL- BORN, 1982; BARSBOLD, 1983), able to run at only Sources for mass data for extinct and extant ani- modest speeds (COOMBS, 1978; MOLNAR &FAR- mals include PAUL (1988, 1997), NOWAK (1991) and LOW, 1990; HORNER &LESSEM, 1993; FARLOW, MATTHEWS (1994). -
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.