Dinosauria: Ornithischia
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A Neoceratopsian Dinosaur from the Early Cretaceous of Mongolia And
ARTICLE https://doi.org/10.1038/s42003-020-01222-7 OPEN A neoceratopsian dinosaur from the early Cretaceous of Mongolia and the early evolution of ceratopsia ✉ Congyu Yu 1 , Albert Prieto-Marquez2, Tsogtbaatar Chinzorig 3,4, Zorigt Badamkhatan4,5 & Mark Norell1 1234567890():,; Ceratopsia is a diverse dinosaur clade from the Middle Jurassic to Late Cretaceous with early diversification in East Asia. However, the phylogeny of basal ceratopsians remains unclear. Here we report a new basal neoceratopsian dinosaur Beg tse based on a partial skull from Baruunbayan, Ömnögovi aimag, Mongolia. Beg is diagnosed by a unique combination of primitive and derived characters including a primitively deep premaxilla with four pre- maxillary teeth, a trapezoidal antorbital fossa with a poorly delineated anterior margin, very short dentary with an expanded and shallow groove on lateral surface, the derived presence of a robust jugal having a foramen on its anteromedial surface, and five equally spaced tubercles on the lateral ridge of the surangular. This is to our knowledge the earliest known occurrence of basal neoceratopsian in Mongolia, where this group was previously only known from Late Cretaceous strata. Phylogenetic analysis indicates that it is sister to all other neoceratopsian dinosaurs. 1 Division of Vertebrate Paleontology, American Museum of Natural History, New York 10024, USA. 2 Institut Català de Paleontologia Miquel Crusafont, ICTA-ICP, Edifici Z, c/de les Columnes s/n Campus de la Universitat Autònoma de Barcelona, 08193 Cerdanyola del Vallès Sabadell, Barcelona, Spain. 3 Department of Biological Sciences, North Carolina State University, Raleigh, NC 27695, USA. 4 Institute of Paleontology, Mongolian Academy of Sciences, ✉ Ulaanbaatar 15160, Mongolia. -
Way to Breathe
INSIGHT DINOSAURS A new, ‘hip’ way to breathe Ornithischians, one of the three major groups of dinosaurs, developed a unique mechanism to ensure airflow in the lungs. MARC R SPENCER the liver to create a motion that draws in air into Related research article Radermacher VJ, the lung. Fernandez V, Schachner ER, Butler RJ, Amongst dinosaurs, two groups (one extinct, Bordy EM, Hudgins MN, de Klerk WJ, the other which gave rise to birds) feature early Chapelle KEJ, Choiniere JN. 2021. A new species with gastralia, only to lose these bones Heterodontosaurus specimen elucidates in favor of other ventilatory mechanisms later in the unique ventilatory macroevolution of evolution (Claessens, 2004). On the other hand, ornithischian dinosaurs. eLife 10:e66036. gastralia had never been found in species doi: 10.7554/eLife.66036 belonging to the now-extinct third dinosaur group Ornithischia, which later on included spe- cies such as Triceratops and Stegosaurus. Now, in eLife, Viktor Radermacher and colleagues report having found, for the first time, gastralia reathe in... and out. As your chest rises in Ornithischia (Radermacher et al., 2021). The and falls, the diaphragm and several team, which is based in institutions in Canada, B lesser-known muscles create the reassur- South Africa, the United Kingdom, France and ing bellows-like motion that allows air to fill and the United States, spotted the bones in Hetero- leave the lungs (Perry et al., 2010). All living dontosaurus, one of the oldest-known mammals and many extinct relatives share the ornithischians. same respiratory muscles and ‘ventilation’ tech- Beyond the unique presence of these bones, this new Heterodontosaurus specimen from nique, but this is not the only way to breathe. -
CPY Document
v^ Official Journal of the Biology Unit of the American Topical Association 10 Vol. 40(4) DINOSAURS ON STAMPS by Michael K. Brett-Surman Ph.D. Dinosaurs are the most popular animals of all time, and the most misunderstood. Dinosaurs did not fly in the air and did not live in the oceans, nor on lake bottoms. Not all large "prehistoric monsters" are dinosaurs. The most famous NON-dinosaurs are plesiosaurs, moso- saurs, pelycosaurs, pterodactyls and ichthyosaurs. Any name ending in 'saurus' is not automatically a dinosaur, for' example, Mastodonto- saurus is neither a mastodon nor a dinosaur - it is an amphibian! Dinosaurs are defined by a combination of skeletal features that cannot readily be seen when the animal is fully restored in a flesh reconstruction. Because of the confusion, this compilation is offered as a checklist for the collector. This topical list compiles all the dinosaurs on stamps where the actual bones are pictured or whole restorations are used. It excludes footprints (as used in the Lesotho stamps), cartoons (as in the 1984 issue from Gambia), silhouettes (Ascension Island # 305) and unoffi- cial issues such as the famous Sinclair Dinosaur stamps. The name "Brontosaurus", which appears on many stamps, is used with quotation marks to denote it as a popular name in contrast to its correct scientific name, Apatosaurus. For those interested in a detailed encyclopedic work about all fossils on stamps, the reader is referred to the forthcoming book, 'Paleontology - a Guide to the Postal Materials Depicting Prehistoric Lifeforms' by Fran Adams et. al. The best book currently in print is a book titled 'Dinosaur Stamps of the World' by Baldwin & Halstead. -
And the Origin and Evolution of the Ankylosaur Pelvis
Pelvis of Gargoyleosaurus (Dinosauria: Ankylosauria) and the Origin and Evolution of the Ankylosaur Pelvis Kenneth Carpenter1,2*, Tony DiCroce3, Billy Kinneer3, Robert Simon4 1 Prehistoric Museum, Utah State University – Eastern, Price, Utah, United States of America, 2 Geology Section, University of Colorado Museum, Boulder, Colorado, United States of America, 3 Denver Museum of Nature and Science, Denver, Colorado, United States of America, 4 Dinosaur Safaris Inc., Ashland, Virginia, United States of America Abstract Discovery of a pelvis attributed to the Late Jurassic armor-plated dinosaur Gargoyleosaurus sheds new light on the origin of the peculiar non-vertical, broad, flaring pelvis of ankylosaurs. It further substantiates separation of the two ankylosaurs from the Morrison Formation of the western United States, Gargoyleosaurus and Mymoorapelta. Although horizontally oriented and lacking the medial curve of the preacetabular process seen in Mymoorapelta, the new ilium shows little of the lateral flaring seen in the pelvis of Cretaceous ankylosaurs. Comparison with the basal thyreophoran Scelidosaurus demonstrates that the ilium in ankylosaurs did not develop entirely by lateral rotation as is commonly believed. Rather, the preacetabular process rotated medially and ventrally and the postacetabular process rotated in opposition, i.e., lateral and ventrally. Thus, the dorsal surfaces of the preacetabular and postacetabular processes are not homologous. In contrast, a series of juvenile Stegosaurus ilia show that the postacetabular process rotated dorsally ontogenetically. Thus, the pelvis of the two major types of Thyreophora most likely developed independently. Examination of other ornithischians show that a non-vertical ilium had developed independently in several different lineages, including ceratopsids, pachycephalosaurs, and iguanodonts. -
Two New Stegosaur Specimens from the Upper Jurassic Morrison Formation of Montana, USA
Editors' choice Two new stegosaur specimens from the Upper Jurassic Morrison Formation of Montana, USA D. CARY WOODRUFF, DAVID TREXLER, and SUSANNAH C.R. MAIDMENT Woodruff, D.C., Trexler, D., and Maidment, S.C.R. 2019. Two new stegosaur specimens from the Upper Jurassic Morrison Formation of Montana, USA. Acta Palaeontologica Polonica 64 (3): 461–480. Two partial skeletons from Montana represent the northernmost occurrences of Stegosauria within North America. One of these specimens represents the northernmost dinosaur fossil ever recovered from the Morrison Formation. Consisting of fragmentary cranial and postcranial remains, these specimens are contributing to our knowledge of the record and distribution of dinosaurs within the Morrison Formation from Montana. While the stegosaurs of the Morrison Formation consist of Alcovasaurus, Hesperosaurus, and Stegosaurus, the only positively identified stegosaur from Montana thus far is Hesperosaurus. Unfortunately, neither of these new specimens exhibit diagnostic autapomorphies. Nonetheless, these specimens are important data points due to their geographic significance, and some aspects of their morphologies are striking. In one specimen, the teeth express a high degree of wear usually unobserved within this clade—potentially illuminating the progression of the chewing motion in derived stegosaurs. Other morphologies, though not histologically examined in this analysis, have the potential to be important indicators for maturational inferences. In suite with other specimens from the northern extent of the formation, these specimens contribute to the ongoing discussion that body size may be latitudinally significant for stegosaurs—an intriguing geographical hypothesis which further emphasizes that size is not an undeviating proxy for maturity in dinosaurs. Key words: Dinosauria, Thyreophora, Stegosauria, Jurassic, Morrison Formation, USA, Montana. -
By Howard Zimmerman
by Howard Zimmerman DINO_COVERS.indd 4 4/24/08 11:58:35 AM [Intentionally Left Blank] by Howard Zimmerman Consultant: Luis M. Chiappe, Ph.D. Director of the Dinosaur Institute Natural History Museum of Los Angeles County 1629_ArmoredandDangerous_FNL.ind1 1 4/11/08 11:11:17 AM Credits Title Page, © Luis Rey; TOC, © De Agostini Picture Library/Getty Images; 4-5, © John Bindon; 6, © De Agostini Picture Library/The Natural History Museum, London; 7, © Luis Rey; 8, © Luis Rey; 9, © Adam Stuart Smith; 10T, © Luis Rey; 10B, © Colin Keates/Dorling Kindersly; 11, © Phil Wilson; 12L, Courtesy of the Royal Tyrrell Museum, Drumheller, Alberta; 12R, © De Agostini Picture Library/Getty Images; 13, © Phil Wilson; 14-15, © Phil Wilson; 16-17, © De Agostini Picture Library/The Natural History Museum, London; 18T, © 2007 by Karen Carr and Karen Carr Studio; 18B, © photomandan/istockphoto; 19, © Luis Rey; 20, © De Agostini Picture Library/The Natural History Museum, London; 21, © John Bindon; 23TL, © Phil Wilson; 23TR, © Luis Rey; 23BL, © Vladimir Sazonov/Shutterstock; 23BR, © Luis Rey. Publisher: Kenn Goin Editorial Director: Adam Siegel Creative Director: Spencer Brinker Design: Dawn Beard Creative Cover Illustration: Luis Rey Photo Researcher: Omni-Photo Communications, Inc. Library of Congress Cataloging-in-Publication Data Zimmerman, Howard. Armored and dangerous / by Howard Zimmerman. p. cm. — (Dino times trivia) Includes bibliographical references and index. ISBN-13: 978-1-59716-712-3 (library binding) ISBN-10: 1-59716-712-6 (library binding) 1. Ornithischia—Juvenile literature. 2. Dinosaurs—Juvenile literature. I. Title. QE862.O65Z56 2009 567.915—dc22 2008006171 Copyright © 2009 Bearport Publishing Company, Inc. All rights reserved. -
An Ankylosaurid Dinosaur from Mongolia with in Situ Armour and Keratinous Scale Impressions
An ankylosaurid dinosaur from Mongolia with in situ armour and keratinous scale impressions VICTORIA M. ARBOUR, NICOLAI L. LECH−HERNES, TOM E. GULDBERG, JØRN H. HURUM, and PHILIP J. CURRIE Arbour, V.M., Lech−Hernes, N.L., Guldberg, T.E., Hurum, J.H., and Currie P.J. 2013. An ankylosaurid dinosaur from Mongolia with in situ armour and keratinous scale impressions. Acta Palaeontologica Polonica 58 (1): 55–64. A Mongolian ankylosaurid specimen identified as Tarchia gigantea is an articulated skeleton including dorsal ribs, the sacrum, a nearly complete caudal series, and in situ osteoderms. The tail is the longest complete tail of any known ankylosaurid. Remarkably, the specimen is also the first Mongolian ankylosaurid that preserves impressions of the keratinous scales overlying the bony osteoderms. This specimen provides new information on the shape, texture, and ar− rangement of osteoderms. Large flat, keeled osteoderms are found over the pelvis, and osteoderms along the tail include large keeled osteoderms, elongate osteoderms lacking distinct apices, and medium−sized, oval osteoderms. The specimen differs in some respects from other Tarchia gigantea specimens, including the morphology of the neural spines of the tail club handle and several of the largest osteoderms. Key words: Dinosauria, Ankylosauria, Ankylosauridae, Tarchia, Saichania, Late Cretaceous, Mongolia. Victoria M. Arbour [[email protected]] and Philip J. Currie [[email protected]], Department of Biological Sciences, CW 405 Biological Sciences Building, University of Alberta, Edmonton, Alberta, Canada, T6G 2E9; Nicolai L. Lech−Hernes [nicolai.lech−[email protected]], Bayerngas Norge, Postboks 73, N−0216 Oslo, Norway; Tom E. Guldberg [[email protected]], Fossekleiva 9, N−3075 Berger, Norway; Jørn H. -
The Princeton Field Guide to Dinosaurs, Second Edition
MASS ESTIMATES - DINOSAURS ETC (largely based on models) taxon k model femur length* model volume ml x specific gravity = model mass g specimen (modeled 1st):kilograms:femur(or other long bone length)usually in decameters kg = femur(or other long bone)length(usually in decameters)3 x k k = model volume in ml x specific gravity(usually for whole model) then divided/model femur(or other long bone)length3 (in most models femur in decameters is 0.5253 = 0.145) In sauropods the neck is assigned a distinct specific gravity; in dinosaurs with large feathers their mass is added separately; in dinosaurs with flight ablity the mass of the fight muscles is calculated separately as a range of possiblities SAUROPODS k femur trunk neck tail total neck x 0.6 rest x0.9 & legs & head super titanosaur femur:~55000-60000:~25:00 Argentinosaurus ~4 PVPH-1:~55000:~24.00 Futalognkosaurus ~3.5-4 MUCPv-323:~25000:19.80 (note:downsize correction since 2nd edition) Dreadnoughtus ~3.8 “ ~520 ~75 50 ~645 0.45+.513=.558 MPM-PV 1156:~26000:19.10 Giraffatitan 3.45 .525 480 75 25 580 .045+.455=.500 HMN MB.R.2181:31500(neck 2800):~20.90 “XV2”:~45000:~23.50 Brachiosaurus ~4.15 " ~590 ~75 ~25 ~700 " +.554=~.600 FMNH P25107:~35000:20.30 Europasaurus ~3.2 “ ~465 ~39 ~23 ~527 .023+.440=~.463 composite:~760:~6.20 Camarasaurus 4.0 " 542 51 55 648 .041+.537=.578 CMNH 11393:14200(neck 1000):15.25 AMNH 5761:~23000:18.00 juv 3.5 " 486 40 55 581 .024+.487=.511 CMNH 11338:640:5.67 Chuanjiesaurus ~4.1 “ ~550 ~105 ~38 ~693 .063+.530=.593 Lfch 1001:~10700:13.75 2 M. -
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 Phylogenetic Analysis of the Basal Ornithischia (Reptilia, Dinosauria)
A PHYLOGENETIC ANALYSIS OF THE BASAL ORNITHISCHIA (REPTILIA, DINOSAURIA) Marc Richard Spencer A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements of the degree of MASTER OF SCIENCE December 2007 Committee: Margaret M. Yacobucci, Advisor Don C. Steinker Daniel M. Pavuk © 2007 Marc Richard Spencer All Rights Reserved iii ABSTRACT Margaret M. Yacobucci, Advisor The placement of Lesothosaurus diagnosticus and the Heterodontosauridae within the Ornithischia has been problematic. Historically, Lesothosaurus has been regarded as a basal ornithischian dinosaur, the sister taxon to the Genasauria. Recent phylogenetic analyses, however, have placed Lesothosaurus as a more derived ornithischian within the Genasauria. The Fabrosauridae, of which Lesothosaurus was considered a member, has never been phylogenetically corroborated and has been considered a paraphyletic assemblage. Prior to recent phylogenetic analyses, the problematic Heterodontosauridae was placed within the Ornithopoda as the sister taxon to the Euornithopoda. The heterodontosaurids have also been considered as the basal member of the Cerapoda (Ornithopoda + Marginocephalia), the sister taxon to the Marginocephalia, and as the sister taxon to the Genasauria. To reevaluate the placement of these taxa, along with other basal ornithischians and more derived subclades, a phylogenetic analysis of 19 taxonomic units, including two outgroup taxa, was performed. Analysis of 97 characters and their associated character states culled, modified, and/or rescored from published literature based on published descriptions, produced four most parsimonious trees. Consistency and retention indices were calculated and a bootstrap analysis was performed to determine the relative support for the resultant phylogeny. The Ornithischia was recovered with Pisanosaurus as its basalmost member. -
The Systematic Position of the Enigmatic Thyreophoran Dinosaur Paranthodon Africanus, and the Use of Basal Exemplifiers in Phyl
1 The systematic position of the enigmatic thyreophoran dinosaur Paranthodon africanus, 2 and the use of basal exemplifiers in phylogenetic analysis 3 4 Thomas J. Raven1,2 ,3 and Susannah C. R. Maidment2 ,3 5 61Department of Earth Science & Engineering, Imperial College London, UK 72School of Environment & Technology, University of Brighton, UK 8 3Department of Earth Sciences, Natural History Museum, London, UK 9 10Corresponding author: Thomas J. Raven 11 12Email address: [email protected] 13 14 15 16 17 18 19 20 21ABSTRACT 22 23The first African dinosaur to be discovered, Paranthodon africanus was found in 1845 in the 24Lower Cretaceous of South Africa. Taxonomically assigned to numerous groups since discovery, 25in 1981 it was described as a stegosaur, a group of armoured ornithischian dinosaurs 26characterised by bizarre plates and spines extending from the neck to the tail. This assignment 27that has been subsequently accepted. The type material consists of a premaxilla, maxilla, a nasal, 28and a vertebra, and contains no synapomorphies of Stegosauria. Several features of the maxilla 29and dentition are reminiscent of Ankylosauria, the sister-taxon to Stegosauria, and the premaxilla 30appears superficially similar to that of some ornithopods. The vertebral material has never been 31described, and since the last description of the specimen, there have been numerous discoveries 32of thyreophoran material potentially pertinent to establishing the taxonomic assignment of the 33specimen. An investigation of the taxonomic and systematic position of Paranthodon is therefore 34warranted. This study provides a detailed re-description, including the first description of the 35vertebra. Numerous phylogenetic analyses demonstrate that the systematic position of 36Paranthodon is highly labile and subject to change depending on which exemplifier for the clade 37Stegosauria is used. -
Síntesis Del Registro Fósil De Dinosaurios Tireóforos En Gondwana
ISSN 2469-0228 www.peapaleontologica.org.ar SÍNTESIS DEL REGISTRO FÓSIL DE DINOSAURIOS TIREÓFOROS EN GONDWANA XABIER PEREDA-SUBERBIOLA 1 IGNACIO DÍAZ-MARTÍNEZ 2 LEONARDO SALGADO 2 SILVINA DE VALAIS 2 1Universidad del País Vasco/Euskal Herriko Unibertsitatea, Facultad de Ciencia y Tecnología, Departamento de Estratigrafía y Paleontología, Apartado 644, 48080 Bilbao, España. 2CONICET - Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, Av. General Roca 1242, 8332 General Roca, Río Negro, Ar gentina. Recibido: 21 de Julio 2015 - Aceptado: 26 de Agosto de 2015 Para citar este artículo: Xabier Pereda-Suberbiola, Ignacio Díaz-Martínez, Leonardo Salgado y Silvina De Valais (2015). Síntesis del registro fósil de dinosaurios tireóforos en Gondwana . En: M. Fernández y Y. Herrera (Eds.) Reptiles Extintos - Volumen en Homenaje a Zulma Gasparini . Publicación Electrónica de la Asociación Paleon - tológica Argentina 15(1): 90–107. Link a este artículo: http://dx.doi.org/ 10.5710/PEAPA.21.07.2015.101 DESPLAZARSE HACIA ABAJO PARA ACCEDER AL ARTÍCULO Asociación Paleontológica Argentina Maipú 645 1º piso, C1006ACG, Buenos Aires República Argentina Tel/Fax (54-11) 4326-7563 Web: www.apaleontologica.org.ar Otros artículos en Publicación Electrónica de la APA 15(1): de la Fuente & Sterli Paulina Carabajal Pol & Leardi ESTADO DEL CONOCIMIENTO DE GUIA PARA EL ESTUDIO DE LA DIVERSITY PATTERNS OF LAS TORTUGAS EXTINTAS DEL NEUROANATOMÍA DE DINOSAURIOS NOTOSUCHIA (CROCODYLIFORMES, TERRITORIO ARGENTINO: UNA SAURISCHIA, CON ENFASIS EN MESOEUCROCODYLIA) DURING PERSPECTIVA HISTÓRICA. FORMAS SUDAMERICANAS. THE CRETACEOUS OF GONDWANA. Año 2015 - Volumen 15(1): 90-107 VOLUMEN TEMÁTICO ISSN 2469-0228 SÍNTESIS DEL REGISTRO FÓSIL DE DINOSAURIOS TIREÓFOROS EN GONDWANA XABIER PEREDA-SUBERBIOLA 1, IGNACIO DÍAZ-MARTÍNEZ 2, LEONARDO SALGADO 2 Y SILVINA DE VALAIS 2 1Universidad del País Vasco/Euskal Herriko Unibertsitatea, Facultad de Ciencia y Tecnología, Departamento de Estratigrafía y Paleontología, Apartado 644, 48080 Bilbao, España.