Sauropodomorph Dinosaurs, with a Description of a New Taxon
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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. -
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’’. -
The Sauropodomorph Biostratigraphy of the Elliot Formation of Southern Africa: Tracking the Evolution of Sauropodomorpha Across the Triassic–Jurassic Boundary
Editors' choice The sauropodomorph biostratigraphy of the Elliot Formation of southern Africa: Tracking the evolution of Sauropodomorpha across the Triassic–Jurassic boundary BLAIR W. MCPHEE, EMESE M. BORDY, LARA SCISCIO, and JONAH N. CHOINIERE McPhee, B.W., Bordy, E.M., Sciscio, L., and Choiniere, J.N. 2017. The sauropodomorph biostratigraphy of the Elliot Formation of southern Africa: Tracking the evolution of Sauropodomorpha across the Triassic–Jurassic boundary. Acta Palaeontologica Polonica 62 (3): 441–465. The latest Triassic is notable for coinciding with the dramatic decline of many previously dominant groups, followed by the rapid radiation of Dinosauria in the Early Jurassic. Among the most common terrestrial vertebrates from this time, sauropodomorph dinosaurs provide an important insight into the changing dynamics of the biota across the Triassic–Jurassic boundary. The Elliot Formation of South Africa and Lesotho preserves the richest assemblage of sauropodomorphs known from this age, and is a key index assemblage for biostratigraphic correlations with other simi- larly-aged global terrestrial deposits. Past assessments of Elliot Formation biostratigraphy were hampered by an overly simplistic biozonation scheme which divided it into a lower “Euskelosaurus” Range Zone and an upper Massospondylus Range Zone. Here we revise the zonation of the Elliot Formation by: (i) synthesizing the last three decades’ worth of fossil discoveries, taxonomic revision, and lithostratigraphic investigation; and (ii) systematically reappraising the strati- graphic provenance of important fossil locations. We then use our revised stratigraphic information in conjunction with phylogenetic character data to assess morphological disparity between Late Triassic and Early Jurassic sauropodomorph taxa. Our results demonstrate that the Early Jurassic upper Elliot Formation is considerably more taxonomically and morphologically diverse than previously thought. -
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. -
Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships
438 Article 438 by Saswati Bandyopadhyay1* and Sanghamitra Ray2 Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships 1Geological Studies Unit, Indian Statistical Institute, 203 B. T. Road, Kolkata 700108, India; email: [email protected] 2Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur 721302, India; email: [email protected] *Corresponding author (Received : 23/12/2018; Revised accepted : 11/09/2019) https://doi.org/10.18814/epiiugs/2020/020028 The twelve Gondwanan stratigraphic horizons of many extant lineages, producing highly diverse terrestrial vertebrates India have yielded varied vertebrate fossils. The oldest in the vacant niches created throughout the world due to the end- Permian extinction event. Diapsids diversified rapidly by the Middle fossil record is the Endothiodon-dominated multitaxic Triassic in to many communities of continental tetrapods, whereas Kundaram fauna, which correlates the Kundaram the non-mammalian synapsids became a minor components for the Formation with several other coeval Late Permian remainder of the Mesozoic Era. The Gondwana basins of peninsular horizons of South Africa, Zambia, Tanzania, India (Fig. 1A) aptly exemplify the diverse vertebrate faunas found Mozambique, Malawi, Madagascar and Brazil. The from the Late Palaeozoic and Mesozoic. During the last few decades much emphasis was given on explorations and excavations of Permian-Triassic transition in India is marked by vertebrate fossils in these basins which have yielded many new fossil distinct taxonomic shift and faunal characteristics and vertebrates, significant both in numbers and diversity of genera, and represented by small-sized holdover fauna of the providing information on their taphonomy, taxonomy, phylogeny, Early Triassic Panchet and Kamthi fauna. -
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. -
West Antarctica: Tectonics and Paleogeography
Chapter 2 West Antarctica: Tectonics and Paleogeography The origin of West Antarctica (WANT) can be traced back to the Terra Australis orogenesis that began between 520 Ma and 510 Ma—shortly after the terminal suturing of Gondwana (Boger 2011). The onset of this event was responsible for the termination of passive margin sedimentation along much of the Pacific margin of Gondwana and marks the beginning of widespread and broadly coeval deforma- tion and arc-type plutonism. It also began a long-lived process of accretion that added much of the crust that defines eastern Australia, West Antarctica (domain 5 of Boger 2011, Fig. 2.1), and western South America (Cawood 2005, 2009). Post-Gondwana accretionary growth—the Terra Australis and Gondwanide Orogenies—The suturing of the West Gondwana and Australo–Antarctic plates along the Kuunga Orogen brought to an end the long-lived process of convergence between the pre-collision components of Gondwana. The result was a reconfigura- tion of the early to middle Cambrian plate system and the consequent transfer of ocean floor consumption from between the pre-Gondwana cratons to the outboard Pacific margin of newly formed Gondwana supercontinent (Cawood2005 ). This led to the establishment of the accretionary Terra Austrais Orogen (Cawood 2005), a general name given to the orogenic belt that stretched continuously from north- ern South America to northern Australia and which began in the early to middle Cambrian and lasted until the late Carboniferous. In Antarctica Terra Australis (Ross) orogenesis also deformed and variably metamorphosed the pre-Gondwana passive margin (Fig. 2.2). The Gondwana supercontinent underwent a sequential fragmentation over approximately 165 Ma. -
Teen Activity Book
For Teens! Color me in! This Activity Book is yours to use however you’d like! Complete all of the pages or just a few. Draw and write all over it. DinoFest is a celebration of all things dinosaur at NHMU. Visit the virtual fun at https://nhmu.utah.edu/polar-dinofest Find a rubber band and pencil, or another thin, firm object (like a stick). 1. Make sure the pages are together and the holes are lined up. Put one end of the rubber band around the pencil. Thread the other 2. end of the band through one of the holes on the front. From the back, thread the rubber end through the other hole on the front. Adjust the pencil to make a 3. nice, bound edge for your activity HOW TO book. Decorate your book with crayons, markers, or pens. Fill it out and learn something new along the 4. way! Activity Book 1 Build Your Own Dinosaur Need: Any Materials Around the House! Instructions 1. Find a dinosaur to use as a reference Collect materials such as: 2. • old cans • ribbons Dinosaur by Hazel, Teen Explainer • hot glue • paper plates • sticks • markers • feathers • tape Sketch out a design to build a dinosaur 3. out of your materials Follow your sketch and reference and attach the pieces of your dinosaur (with 4. the tape, hot glue, etc.) Here’s an example! This is based off See the back cover for ideas of how to of a Cryolophosaurus from the 5. share your dinosaur with others! Antarctic Dinosaurs Exhibit! 2 Carrie Levitt-Bussian is the Paleontology Collections Manager at the Natural History Museum of Utah. -
A New Basal Sauropodomorph Dinosaur from the Lower Jurassic Navajo Sandstone of Southern Utah
A New Basal Sauropodomorph Dinosaur from the Lower Jurassic Navajo Sandstone of Southern Utah Joseph J. W. Sertich1*, Mark A. Loewen2 1 Department of Anatomical Sciences, Stony Brook University, Stony Brook, New York, United States of America, 2 Utah Museum of Natural History, Salt Lake City, Utah, United States of America Abstract Background: Basal sauropodomorphs, or ‘prosauropods,’ are a globally widespread paraphyletic assemblage of terrestrial herbivorous dinosaurs from the Late Triassic and Early Jurassic. In contrast to several other landmasses, the North American record of sauropodomorphs during this time interval remains sparse, limited to Early Jurassic occurrences of a single well- known taxon from eastern North America and several fragmentary specimens from western North America. Methodology/Principal Findings: On the basis of a partial skeleton, we describe here a new basal sauropodomorph dinosaur from the Lower Jurassic Navajo Sandstone of southern Utah, Seitaad ruessi gen. et sp. nov. The partially articulated skeleton of Seitaad was likely buried post-mortem in the base of a collapsed dune foreset. The new taxon is characterized by a plate-like medial process of the scapula, a prominent proximal expansion of the deltopectoral crest of the humerus, a strongly inclined distal articular surface of the radius, and a proximally and laterally hypertrophied proximal metacarpal I. Conclusions/Significance: Phylogenetic analysis recovers Seitaad as a derived basal sauropodomorph closely related to plateosaurid or massospondylid ‘prosauropods’ and its presence in western North America is not unexpected for a member of this highly cosmopolitan clade. This occurrence represents one of the most complete vertebrate body fossil specimens yet recovered from the Navajo Sandstone and one of the few basal sauropodomorph taxa currently known from North America. -
The Pelvic and Hind Limb Anatomy of the Stem-Sauropodomorph Saturnalia Tupiniquim (Late Triassic, Brazil)
PaleoBios 23(2):1–30, July 15, 2003 © 2003 University of California Museum of Paleontology The pelvic and hind limb anatomy of the stem-sauropodomorph Saturnalia tupiniquim (Late Triassic, Brazil) MAX CARDOSO LANGER Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, BS8 1RJ Bristol, UK. Current address: Departamento de Biologia, Universidade de São Paulo (USP), Av. Bandeirantes, 3900 14040-901 Ribeirão Preto, SP, Brazil; [email protected] Three partial skeletons allow a nearly complete description of the sacrum, pelvic girdle, and hind limb of the stem- sauropodomorph Saturnalia tupiniquim, from the Late Triassic Santa Maria Formation, South Brazil. The new morphological data gathered from these specimens considerably improves our knowledge of the anatomy of basal dinosaurs, providing the basis for a reassessment of various morphological transformations that occurred in the early evolution of these reptiles. These include an increase in the number of sacral vertebrae, the development of a brevis fossa, the perforation of the acetabulum, the inturning of the femoral head, as well as various modifications in the insertion of the iliofemoral musculature and the tibio-tarsal articulation. In addition, the reconstruction of the pelvic musculature of Saturnalia, along with a study of its locomotion pattern, indicates that the hind limb of early dinosaurs did not perform only a fore-and-aft stiff rotation in the parasagittal plane, but that lateral and medial movements of the leg were also present and important. INTRODUCTION sisting of most of the presacral vertebral series, both sides Saturnalia tupiniquim was described in a preliminary of the pectoral girdle, right humerus, partial right ulna, right fashion by Langer et al. -
Download the Explorer Corps Passport
PASSPORT to Utah’s Natural History A Special Thanks Sponsors Supporting Partners YOUR PASSPORT TO ADVENTURE IS HERE! Join us in celebrating Utah’s remarkable natural history by visiting uniquely-Utah locations throughout the state. With a marker placed in every county, and a quest to find them all, that’s 29 unforgettable destinations to check out! How many can you find, and what will you discover? Follow and share #explorercorps or visit nhmu.utah.edu/explorer-corps 1 JOIN EXPLORER CORPS Bring this passport with you as you discover all Utah has to offer! Each page is dedicated to one of Utah’s 29 counties. You’ll find directions to the marker (and GPS coordinates if that’s your thing), fast facts about the area celebrated in that county, plus great suggestions for going further and digging deeper. Use the Travel Log inside the back cover to track your progress and the Field Journal in the back of this passport to capture notes from the markers you visit. A couple of tips: n Download our Explorer Corps app for iPhone and Android and use augmented reality to bring Utah’s natural history to life. n Visit local libraries for books and additional resources. n Enter our Race to 29! and Explorer Corps Weekly Giveaways for your chance to win great prizes, receive Explorer Corps badges, and more. Visit nhmu.utah.edu/explorer-corps for full details. The adventure is yours—good luck! 2 WE HONOR NATIVE LAND Places have a complex and layered history. That is true for the locations and specimens highlighted in this passport. -
Giants from the Past | Presented by the Field Museum Learning Center 2 Pre-Lesson Preparation
Giants from the Past Middle School NGSS: MS-LS4-1, MS-LS4-4 Lesson Description Learning Objectives This investigation focuses on the fossils of a particular • Students will demonstrate an understanding that group of dinosaurs, the long-necked, herbivores known as particular traits provide advantages for survival sauropodomorphs. Students will gain an understanding by using models to test and gather data about the of why certain body features provide advantages to traits’ functions. Background survival through the use of models. Students will analyze • Students will demonstrate an understanding of and interpret data from fossils to synthesize a narrative ancestral traits by investigating how traits appear for the evolution of adaptations that came to define a and change (or evolve) in the fossil record well-known group of dinosaurs. over time. • Students will demonstrate an understanding of how traits function to provide advantages Driving Phenomenon in a particular environment by inferring daily Several traits, inherited and adapted over millions of years, activities that the dinosaur would have performed provided advantages for a group of dinosaurs to evolve for survival. into the largest animals that ever walked the Earth. Giant dinosaurs called sauropods evolved over a period of 160 Time Requirements million years. • Four 40-45 minute sessions As paleontologists continue to uncover new specimens, Prerequisite Knowledge they see connections across time and geography that lead to a better understanding of how adaptations interact • Sedimentary rocks form in layers, the newer rocks with their environment to provide unique advantages are laid down on top of the older rocks. depending on when and where animals lived.