Evolutionary Transitions Among Dinosaurs: Examples from the Jurassic of China

Total Page:16

File Type:pdf, Size:1020Kb

Evolutionary Transitions Among Dinosaurs: Examples from the Jurassic of China Evo Edu Outreach (2009) 2:236–247 DOI 10.1007/s12052-009-0137-0 ORIGINAL SCIENTIFIC ARTICLE Evolutionary Transitions Among Dinosaurs: Examples from the Jurassic of China James M. Clark & Xing Xu Published online: 9 May 2009 # Springer Science + Business Media, LLC 2009 Abstract Dinosaurs have captured the popular imagination relationships and transitions. Familiar highly specialized more than any other extinct group of organisms and are animals such as Triceratops, Pachycephalosaurus, Stego- therefore a powerful tool in teaching evolutionary biology. saurus, Ankylosaurus, Tyrannosaurus, Brachiosaurus, and Most students are familiar with a wide variety of dinosaurs Parasaurolophus are joined in the fossil record by hundreds and the relative suddenness of their extinction, but few are of their relatives with less-specialized features (Weishampel aware of the tremendous longevity of their time on Earth et al. 2004). Together, they comprise a many-branched and the richness of their fossil record. We first review some evolutionary tree that flourished for over 160 million years. of the best-known groups of dinosaurs and discuss how Dinosaurs are found almost exclusively in sedimentary their less-specialized relatives elucidate the path through rocks formed in terrestrial, rather than marine, environ- which each evolved. We then discuss our recent discovery ments, indicating that they rarely ventured out into the sea. of Yinlong downsi, a distant relative of Triceratops, and These river and lake deposits formed layers, or strata, that other fossils from Jurassic deposits in China to exemplify are overlain by younger rocks and underlain by older ones. how the continuing discovery of fossils is filling out the By studying how these and other layers of rocks and their dinosaur family tree. entombed fossils are stacked, scientists called stratigraphers have been able to recognize the sequence in which Keywords Dinosaurs . Evolution . Transitional fossils . dinosaurs and other fossils occurred during the Earth’s Mesozoic . China . Jurassic history (Prothero and Schwab 2003). This led to the erection in the early nineteenth century of a timescale with Dinosaurs need no introduction, they are ubiquitous in now-familiar names for different time periods, including the popular media as symbols of the terrors of nature and how Mesozoic Era (popularly called the Age of Dinosaurs) and the mighty fall. But the richness and remarkable duration of its three subdivisions, from oldest to youngest, the Triassic, the fossil record of dinosaurs are less widely appreciated, Jurassic, and Cretaceous periods (for a fascinating account and the abundant fossil record of dinosaurs is an excellent of debates in the early nineteenth century over how the time example of how fossils provide evidence for evolutionary periods were recognized, see Rudwick 1985). However, these divisions reflected only the relative ages of these J. M. Clark (*) fossils, and it was not until the last 60 years that ways of Department of Biological Sciences, estimating the age in years of rocks and fossils were George Washington University, developed. These involve the decay of radioactive ele- Washington, DC 20052, USA ments, which are experimentally shown to occur at rates e-mail: [email protected] that take millions or billions of years to complete, depend- X. Xu ing on the element and isotope. Laboratory of Evolutionary Systematics of Vertebrates, Radiometric dating comprises a well-developed set of Institute of Vertebrate Paleontology and Paleoanthropology, techniques that are now capable of very high resolution Chinese Academy of Sciences, 142 Xiwai Street, (Macdougall 2008). Only relatively young fossils Beijing 100044, China (<50,000 years old) can be dated directly, by Carbon-14 Evo Edu Outreach (2009) 2:236–247 237 dating of bone or other carbonaceous fossils, so the dating the Dinosaur Park Formation of Canada (Holmes et al. of dinosaurs millions of years old relies upon dating of the 2001). More to the point, the periodic sampling of fossils rock layers above, below, and rarely within beds containing over millions of years is sufficient to provide documenta- fossils. The radioactive decay of isotopes of several tion of the sequential acquisition of specialized features in different elements (argon, potassium, and uranium) can be all of the major dinosaur lineages. used to date dinosaur-bearing rocks because they all have Fossiliferous rocks are more common near the end of the half-lives (the statistically estimated time it would take half dinosaur’s record, at the close of the Cretaceous Period, of a sample to decay) of the appropriate length, and the use than in the Jurassic and Triassic, so we know much more of different isotopes can provide independent checks on any about the dinosaurs that lived shortly before they went one date. extinct than those from earlier in their evolution. Neverthe- Radiometric dating estimates the age of a rock at the less, the early fossil record of dinosaurs is reasonably well time that it crystallized, by comparing the amount of known and includes many complete or nearly complete “daughter” decay product to the original amount of the skeletons. These early fossils are important because older radioactive “mother” isotope (calculated as the amount of fossils are more likely to include the most basal members of decay product plus what remains of the mother isotope). evolutionary lineages, lacking most of the specializations of Rock layers such as tuffs that formed when volcanic ash, later forms (we use basal here to refer to members of a including recently formed tiny crystals, was ejected from a group that diverged earlier than other members). These volcano and blanketed the countryside, are ideal for dating. early dinosaurs are generally smaller than their later Many tuffs occur in dinosaur-bearing deposits or above or brethren and have only a few of the features distinguishing below them, so we have a good idea of how old most the lineage to which they belong. The search for early dinosaur fossils are (and can estimate all the others). dinosaurs is among the “hottest” areas of dinosaur research The oldest dinosaurs, from the Valley of the Moon in because such dinosaurs are not as common as later ones and Argentina, are dated at 227.8±0.3 million years (Rogers et hold great potential for elucidating the dinosaurs’ early al. 1993; a report of an older dinosaur from Madagascar is diversification into major evolutionary branches. being revised), and the extinction event 65.95±0.04 million A tally of dinosaurs published 3 years ago (Wang and years ago (Kuiper et al. 2008) apparently killed off all of Dodson 2006) recognized 527 genera, the vast majority the dinosaurs alive at that time while leaving their with only a single species. (Dinosaur paleontologists have a descendents, the birds. Dinosaurs were therefore on the partiality to naming new genera even when a new species is Earth for at least 161 million years, and their descendents closely related to an existing genus, something our the birds (reference to Padian contribution) continued on entomological colleagues find mildly disturbing.) For each for another 65.95 million years (and thankfully show few of these genera, a fossil exists with features that, theoret- signs of leaving us). To put this in perspective, the oldest ically, clearly differentiate it from every other known human fossils are six to seven million years old (Brunet et dinosaur genus. For some of these genera, skeletons of al. 2002), so the dinosaur fossil record is about 23 to 27 many individuals are known (e.g., Protoceratops, Psittaco- times longer than that of humans. saurus, Allosaurus, Coelophysis, and Iguanodon), some- As with the fossil record in general (Kidwell and times in the hundreds, and one remarkable bone bed in Holland 2002), the record of dinosaur fossils is not Alberta, Canada, preserves bones from thousands of consistent through time because the deposition of sedimen- individuals of Centrosaurus, a one-horned relative of tary rocks in the environments in which dinosaurs lived Triceratops. Wang and Dodson use the known number varied at different times in the Earth’s history. This of dinosaurs and the rate at which new genera are discovered depended both on local conditions and on global phenom- to estimate that 1,850 genera of dinosaurs had existed, in ena such as plate tectonics and sea level changes, as the which case less than a third have been discovered. mountain building that fueled sedimentation waxed and Evolutionary relationships are evident through the waned. The incomplete sampling of ancient species by the features shared by groups of organisms (Gregory 2008). sedimentary record, coupled with the episodic, greatly Just as a very high percentage of human DNA is identical incomplete record that was left of those sediments, could to that of our closest relatives, the chimpanzees, closely not possibly produce a series of forms showing all stages of related species of all kinds share similar DNA, anatomy, continuous change from one species to another (whether or and physiology. One of the main reasons the theory of not absolutely complete continuity in morphology ever evolution is accepted is that it provides an explanation for existed is an open question). But some examples of small why similar features are found in different organisms. To changes between very similar species over time exist, such cite just one example, the presence in all land-living as the three successive species of the horned dinosaur vertebrates of four limbs with digits (reference to Shubin Chasmosaurus over approximately 2.5 million years within contribution) is explained by the close evolutionary 238 Evo Edu Outreach (2009) 2:236–247 relationships of all tetrapods to each other, as members of Duck-Billed Dinosaurs The duck-billed dinosaurs, or hadro- the same lineages. Supposed alternative theories such as saurs, were abundant and diverse near the end of the Intelligent Design are mute in explaining these rampant Cretaceous and were among those groups that disappeared similarities.
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • New Heterodontosaurid Remains from the Cañadón Asfalto Formation: Cursoriality and the Functional Importance of the Pes in Small Heterodontosaurids
    Journal of Paleontology, 90(3), 2016, p. 555–577 Copyright © 2016, The Paleontological Society 0022-3360/16/0088-0906 doi: 10.1017/jpa.2016.24 New heterodontosaurid remains from the Cañadón Asfalto Formation: cursoriality and the functional importance of the pes in small heterodontosaurids Marcos G. Becerra,1 Diego Pol,1 Oliver W.M. Rauhut,2 and Ignacio A. Cerda3 1CONICET- Museo Palaeontológico Egidio Feruglio, Fontana 140, Trelew, Chubut 9100, Argentina 〈[email protected]〉; 〈[email protected]〉 2SNSB, Bayerische Staatssammlung für Paläontologie und Geologie and Department of Earth and Environmental Sciences, LMU München, Richard-Wagner-Str. 10, Munich 80333, Germany 〈[email protected]〉 3CONICET- Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, Museo Carlos Ameghino, Belgrano 1700, Paraje Pichi Ruca (predio Marabunta), Cipolletti, Río Negro, Argentina 〈[email protected]〉 Abstract.—New ornithischian remains reported here (MPEF-PV 3826) include two complete metatarsi with associated phalanges and caudal vertebrae, from the late Toarcian levels of the Cañadón Asfalto Formation. We conclude that these fossil remains represent a bipedal heterodontosaurid but lack diagnostic characters to identify them at the species level, although they probably represent remains of Manidens condorensis, known from the same locality. Histological features suggest a subadult ontogenetic stage for the individual. A cluster analysis based on pedal measurements identifies similarities of this specimen with heterodontosaurid taxa and the inclusion of the new material in a phylogenetic analysis with expanded character sampling on pedal remains confirms the described specimen as a heterodontosaurid. Finally, uncommon features of the digits (length proportions among nonungual phalanges of digit III, and claw features) are also quantitatively compared to several ornithischians, theropods, and birds, suggesting that this may represent a bipedal cursorial heterodontosaurid with gracile and grasping feet and long digits.
    [Show full text]
  • Stegosaurus Scelidosaurus Huayangosaurus Cheeks: No
    Huayangosaurus Scelidosaurus Stegosaurus Cheeks: No reptile has ever had a ‘buccinator’ muscle Answer: highly flexible tongue Brains 0.001% of stegosaur body weight Compared to 1.8% in humans (1000x larger per unit body weight!) Brains Brains Locomotion Graviportal Locomotion Elephantine hind feet (weight-bearing) Shin bones fused with astragalus/ calcaneum Femur: Long compared to humerus Columnar Facultative Tripodality? Stocky forelimbs- could be used for turning/posturing (Bakker) Dermal Armour? Pattern of plates and spines is species-specific Plates paired or staggered (Stegosaurus) Plates were probably not for defense... not tough enough Rotation? Surface markings => symmetrical. Rotation unlikely Potential uses: Thermoregulation? Warm up (ectotherms), Cool down (endotherms) Signaling? positioned for maximal lateral visibility Sexual Selection Mate Recognition Grooves for blood vessels Sexual dimorphism Differences between males and females of the same species **New finding** published in 2015 Stegosaurus Morrison formation, Colorado Dinosaur Sex Figuring out how Stegosaurus even could have mated is a prickly subject. Females were just as well-armored as males, and it is unlikely that males mounted the females from the back. A different technique was necessary. Perhaps they angled so that they faced belly to belly, some have guessed, or maybe, as suggested by Timothy Isles in a recent paper, males faced away from standing females and backed up (a rather tricky maneuver!). The simplest technique yet proposed is that the female lay down on her side and the male approached standing up, thereby avoiding all those plates and spikes. However the Stegosaurus pair accomplished the feat, though, it was most likely brief—only as long as was needed for the exchange of genetic material.
    [Show full text]
  • Luis V. Rey & Gondwana Studios
    EXHIBITION BY LUIS V. REY & GONDWANA STUDIOS HORNS, SPIKES, QUILLS AND FEATHERS. THE SECRET IS IN THE SKIN! Not long ago, our knowledge of dinosaurs was based almost completely on the assumptions we made from their internal body structure. Bones and possible muscle and tendon attachments were what scientists used mostly for reconstructing their anatomy. The rest, including the colours, were left to the imagination… and needless to say the skins were lizard-like and the colours grey, green and brown prevailed. We are breaking the mould with this Dinosaur runners, massive horned faces and Revolution! tank-like monsters had to live with and defend themselves against the teeth and claws of the Thanks to a vast web of new research, that this Feathery Menace... a menace that sometimes time emphasises also skin and ornaments, we reached gigantic proportions in the shape of are now able to get a glimpse of the true, bizarre Tyrannosaurus… or in the shape of outlandish, and complex nature of the evolution of the massive ornithomimids with gigantic claws Dinosauria. like the newly re-discovered Deinocheirus, reconstructed here for the first time in full. We have always known that the Dinosauria was subdivided in two main groups, according All of them are well represented and mostly to their pelvic structure: Saurischia spectacularly mounted in this exhibition. The and Ornithischia. But they had many things exhibits are backed with close-to-life-sized in common, including structures made of a murals of all the protagonist species, fully special family of fibrous proteins called keratin fleshed and feathered and restored in living and that covered their skin in the form of spikes, breathing colours.
    [Show full text]
  • New Tyrannosaur from the Mid-Cretaceous of Uzbekistan Clarifies Evolution of Giant Body Sizes and Advanced Senses in Tyrant Dinosaurs
    New tyrannosaur from the mid-Cretaceous of Uzbekistan clarifies evolution of giant body sizes and advanced senses in tyrant dinosaurs Stephen L. Brusattea,1, Alexander Averianovb,c, Hans-Dieter Suesd, Amy Muira, and Ian B. Butlera aSchool of GeoSciences, University of Edinburgh, Edinburgh EH9 3FE, United Kingdom; bZoological Institute, Russian Academy of Sciences, St. Petersburg 199034, Russia; cDepartment of Sedimentary Geology, Saint Petersburg State University, St. Petersburg 199178, Russia; and dDepartment of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560 Edited by Neil H. Shubin, The University of Chicago, Chicago, IL, and approved January 29, 2016 (received for review January 5, 2016) Tyrannosaurids—the familiar group of carnivorous dinosaurs in- We here report the first diagnostic tyrannosauroid from the mid- cluding Tyrannosaurus and Albertosaurus—were the apex predators Cretaceous, a new species from the Turonian (ca. 90–92 million in continental ecosystems in Asia and North America during the years ago) Bissekty Formation of Uzbekistan. This formation has latest Cretaceous (ca. 80–66 million years ago). Their colossal sizes recently emerged as one of the most important records of mid- and keen senses are considered key to their evolutionary and eco- Cretaceous dinosaurs globally (9–11). Possible tyrannosauroid logical success, but little is known about how these features devel- specimens from the Bissekty Formation were reported more than oped as tyrannosaurids evolved from smaller basal tyrannosauroids a half century ago (12), and, more recently, several isolated fossils that first appeared in the fossil record in the Middle Jurassic (ca. 170 were assigned to the group (9, 13), but none of these has been million years ago).
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • At Carowinds
    at Carowinds EDUCATOR’S GUIDE CLASSROOM LESSON PLANS & FIELD TRIP ACTIVITIES Table of Contents at Carowinds Introduction The Field Trip ................................... 2 The Educator’s Guide ....................... 3 Field Trip Activity .................................. 4 Lesson Plans Lesson 1: Form and Function ........... 6 Lesson 2: Dinosaur Detectives ....... 10 Lesson 3: Mesozoic Math .............. 14 Lesson 4: Fossil Stories.................. 22 Games & Puzzles Crossword Puzzles ......................... 29 Logic Puzzles ................................. 32 Word Searches ............................... 37 Answer Keys ...................................... 39 Additional Resources © 2012 Dinosaurs Unearthed Recommended Reading ................. 44 All rights reserved. Except for educational fair use, no portion of this guide may be reproduced, stored in a retrieval system, or transmitted in any form or by any Dinosaur Data ................................ 45 means—electronic, mechanical, photocopy, recording, or any other without Discovering Dinosaurs .................... 52 explicit prior permission from Dinosaurs Unearthed. Multiple copies may only be made by or for the teacher for class use. Glossary .............................................. 54 Content co-created by TurnKey Education, Inc. and Dinosaurs Unearthed, 2012 Standards www.turnkeyeducation.net www.dinosaursunearthed.com Curriculum Standards .................... 59 Introduction The Field Trip From the time of the first exhibition unveiled in 1854 at the Crystal
    [Show full text]
  • 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.
    [Show full text]
  • A New Crested Theropod Dinosaur from the Early Jurassic of Yunnan
    第55卷 第2期 古 脊 椎 动 物 学 报 pp. 177-186 2017年4月 VERTEBRATA PALASIATICA figs. 1-3 A new crested theropod dinosaur from the Early Jurassic of Yunnan Province, China WANG Guo-Fu1,2 YOU Hai-Lu3,4* PAN Shi-Gang5 WANG Tao5 (1 Fossil Research Center of Chuxiong Prefecture, Yunnan Province Chuxiong, Yunnan 675000) (2 Chuxiong Prefectural Museum Chuxiong, Yunnan 675000) (3 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044 * Corresponding author: [email protected]) (4 College of Earth Sciences, University of Chinese Academy of Sciences Beijing 100049) (5 Bureau of Land and Resources of Lufeng County Lufeng, Yunnan 650031) Abstract A new crested theropod, Shuangbaisaurus anlongbaoensis gen. et sp. nov., is reported. The new taxon is recovered from the Lower Jurassic Fengjiahe Formation of Shuangbai County, Chuxiong Yi Autonomous Prefecture, Yunnan Province, and is represented by a partial cranium. Shuangbaisaurus is unique in possessing parasagittal crests along the orbital dorsal rims. It is also distinguishable from the other two lager-bodied parasagittal crested Early Jurassic theropods (Dilophosaurus and Sinosaurus) by a unique combination of features, such as higher than long premaxillary body, elevated ventral edge of the premaxilla, and small upper temporal fenestra. Comparative morphological study indicates that “Dilophosaurus” sinensis could potentially be assigned to Sinosaurus, but probably not to the type species. The discovery of Shuangbaisaurus will help elucidate the evolution of basal theropods, especially the role of various bony cranial ornamentations had played in the differentiation of early theropods.
    [Show full text]
  • 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.
    [Show full text]