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M.A. TAYLOR 1 and R.D. CLARK 2 Methodology and Repositories
Ichthyosaurs from the Lower Lias (Lower Jurassic) of Banwell, Somerset ICHTHYOSAURS FROM THE LOWER LIAS (LOWER JURASSIC) OF BANWELL, SOMERSET M.A. TAYLOR 1 AND R.D. CLARK 2 Taylor, M.A. and Clark, R.D. 2016. Ichthyosaurs from the Lower Lias (Lower Jurassic) of Banwell, Somerset. Geoscience in South-West England, 14, 59–71. Two Lower Jurassic ichthyosaurs, lost in a 1940s air raid, are identified from archival records and surviving 19th century plaster casts distributed by their owner, the Bristol Institution for the Advancement of Science, Literature and the Arts. One was the type specimen of Ichthyosaurus latimanus Owen, 1840. The other, initially labelled Ichthyosaurus intermedius Conybeare, 1822, was the first ichthyosaur in which remains of the soft tissue of the tail fin were identified, confirming Richard Owen’s earlier prediction. Unfortunately Owen’s published account conflated the two specimens, apparently by the erroneous transposition of a passage of text. Owen possibly regarded the second specimen as the type of I. intermedius. In 1889 Richard Lydekker referred it to Ichthyosaurus conybeari Lydekker, 1888. For unknown reasons, he caused further confusion by suppressing the fact that both ichthyosaur specimens came from Banwell. Banwell is shown to have been a minor but significant source of Lower Lias fossil vertebrates, and also the type locality of the fish Tetragonolepis monilifer Agassiz, 1837, apparently from quarries in the lowermost Jurassic beds at Knightcott. The Bristol Institution assisted Edward Wilson (1808–1888) to obtain at least some of the West Country marine reptiles which his brother Dr Thomas Bellerby Wilson (1807–1865) donated to the Academy of Natural Sciences of Philadelphia, U.S.A. -
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’’. -
Silurian Rugose Corals of the Central and Southwest Great Basin
Silurian Rugose Corals of the Central and Southwest Great Basin GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 Silurian Rugose Corals of the Central and Southwest Great Basin By CHARLES W. MERRIAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 A stratigraphic-paleontologic investigation of rugose corals as aids in age detern2ination and correlation of Silurian rocks of the Great Basin with those of other regions UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-600082 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- Price $2.15 (paper cover) Stock Number 2401-00363 CONTENTS Page Page Abstract--------------------------------------------------------------------------- 1 Systematic and descriptive palaeontology-Continued Introduction -------------------------------------------------------------------- 1 Family Streptelasmatidae-Continued Purpose and scope of investigation------------------------------- 1 Dalmanophyllum ------------------------------------------------- 32 History of investigation ---------------------------------------------- 1 Family Stauriidae ------------------------------------------------------- 32 Methods of study------------------------------------------------------- 2 Cyathoph y llo ides-------------------------------------------------- 32 Acknowledgments------------------------------------------------------- 4 Palaeophyllum -
Mary Anning of Lyme Regis: 19Th Century Pioneer in British Palaeontology
Headwaters Volume 26 Article 14 2009 Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/headwaters Part of the Geology Commons, and the Paleontology Commons Recommended Citation Davis, Larry E. (2009) "Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology," Headwaters: Vol. 26, 96-126. Available at: https://digitalcommons.csbsju.edu/headwaters/vol26/iss1/14 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in Headwaters by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. LARRY E. DAVIS Mary Anning of Lyme Regis 19th Century Pioneer in British Palaeontology Ludwig Leichhardt, a 19th century German explorer noted in a letter, “… we had the pleasure of making the acquaintance of the Princess of Palaeontology, Miss Anning. She is a strong, energetic spinster of about 28 years of age, tanned and masculine in expression …” (Aurousseau, 1968). Gideon Mantell, a 19th century British palaeontologist, made a less flattering remark when he wrote in his journal, “… sallied out in quest of Mary An- ning, the geological lioness … we found her in a little dirt shop with hundreds of specimens piled around her in the greatest disorder. She, the presiding Deity, a prim, pedantic vinegar looking female; shred, and rather satirical in her conversation” (Curwin, 1940). Who was Mary Anning, this Princess of Palaeontology and Geological Lioness (Fig. -
A Re-Evaluation of the Enigmatic Dinosauriform Caseosaurus Crosbyensis from the Late Triassic of Texas, USA and Its Implications for Early Dinosaur Evolution
A re-evaluation of the enigmatic dinosauriform Caseosaurus crosbyensis from the Late Triassic of Texas, USA and its implications for early dinosaur evolution MATTHEW G. BARON and MEGAN E. WILLIAMS Baron, M.G. and Williams, M.E. 2018. A re-evaluation of the enigmatic dinosauriform Caseosaurus crosbyensis from the Late Triassic of Texas, USA and its implications for early dinosaur evolution. Acta Palaeontologica Polonica 63 (1): 129–145. The holotype specimen of the Late Triassic dinosauriform Caseosaurus crosbyensis is redescribed and evaluated phylogenetically for the first time, providing new anatomical information and data on the earliest dinosaurs and their evolution within the dinosauromorph lineage. Historically, Caseosaurus crosbyensis has been considered to represent an early saurischian dinosaur, and often a herrerasaur. More recent work on Triassic dinosaurs has cast doubt over its supposed dinosaurian affinities and uncertainty about particular features in the holotype and only known specimen has led to the species being regarded as a dinosauriform of indeterminate position. Here, we present a new diagnosis for Caseosaurus crosbyensis and refer additional material to the taxon—a partial right ilium from Snyder Quarry. Our com- parisons and phylogenetic analyses suggest that Caseosaurus crosbyensis belongs in a clade with herrerasaurs and that this clade is the sister taxon of Dinosauria, rather than positioned within it. This result, along with other recent analyses of early dinosaurs, pulls apart what remains of the “traditional” group of dinosaurs collectively termed saurischians into a polyphyletic assemblage and implies that Dinosauria should be regarded as composed exclusively of Ornithoscelida (Ornithischia + Theropoda) and Sauropodomorpha. In addition, our analysis recovers the enigmatic European taxon Saltopus elginensis among herrerasaurs for the first time. -
The Bristol Dinosaur Project
Proceedings of the Geologists’ Association 123 (2012) 210–225 Contents lists available at ScienceDirect Proceedings of the Geologists’ Association jo urnal homepage: www.elsevier.com/locate/pgeola Teaching Perspective The Bristol Dinosaur Project Michael J. Benton *, Remmert Schouten, Edward J.A. Drewitt, Pedro Viegas School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, UK A R T I C L E I N F O A B S T R A C T Article history: Dinosaurs have been fascinating to the widest public since the 1840s, and that interest has grown step- Received 18 April 2011 wise ever since. Public interest has been harnessed over the years especially by museums in blockbuster Received in revised form 8 July 2011 exhibitions, and in the form of best-selling books and films. Here we describe a major educational Accepted 8 July 2011 initiative, the Bristol Dinosaur Project, which has run for ten years and has reached tens of thousands of Available online 5 August 2011 children and adults, supported by substantial funding. The Bristol Dinosaur Project focuses on the fourth dinosaur ever named in the world, Thecodontosaurus, discovered in Bristol in 1834, and named in 1836. Keywords: The dinosaur is not in itself spectacular, being only 1–2 m long, but its evolutionary role as one of the first Dinosaurs plant-eating dinosaurs in the world justifies our current research, and provides a strong theme for the Education Engagement public presentation. Further, the fact that the dinosaur is found as disarticulated bones in ancient tropical Outreach cave systems, allows us to develop numerous key themes with all age groups: the geological time scale, Geosciences education continental drift, reconstruction of ancient environments, modern landscape analogues, the rock cycle, evolution, biomechanics, and critical assessment of geological and palaeontological evidence. -
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. -
Dorset and East Devon Coast for Inclusion in the World Heritage List
Nomination of the Dorset and East Devon Coast for inclusion in the World Heritage List © Dorset County Council 2000 Dorset County Council, Devon County Council and the Dorset Coast Forum June 2000 Published by Dorset County Council on behalf of Dorset County Council, Devon County Council and the Dorset Coast Forum. Publication of this nomination has been supported by English Nature and the Countryside Agency, and has been advised by the Joint Nature Conservation Committee and the British Geological Survey. Maps reproduced from Ordnance Survey maps with the permission of the Controller of HMSO. © Crown Copyright. All rights reserved. Licence Number: LA 076 570. Maps and diagrams reproduced/derived from British Geological Survey material with the permission of the British Geological Survey. © NERC. All rights reserved. Permit Number: IPR/4-2. Design and production by Sillson Communications +44 (0)1929 552233. Cover: Duria antiquior (A more ancient Dorset) by Henry De la Beche, c. 1830. The first published reconstruction of a past environment, based on the Lower Jurassic rocks and fossils of the Dorset and East Devon Coast. © Dorset County Council 2000 In April 1999 the Government announced that the Dorset and East Devon Coast would be one of the twenty-five cultural and natural sites to be included on the United Kingdom’s new Tentative List of sites for future nomination for World Heritage status. Eighteen sites from the United Kingdom and its Overseas Territories have already been inscribed on the World Heritage List, although only two other natural sites within the UK, St Kilda and the Giant’s Causeway, have been granted this status to date. -
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. -
Some Unpublished Correspondence of the Rev. W.B. Clarke D.F
Journal & Proceedings of the Royal Society of New South Wales, Vol. 141, p. 1–31, 2008 ISSN 0035-9173/08/02001–31 $4.00/1 Some Unpublished Correspondence of the Rev. W.B. Clarke d.f. branagan and t.g. vallance Abstract: Four previously unpublished letters, with memoranda of Rev. W.B. Clarke to W.S. Macleay, written between 1842 and 1845 clarify the ideas of both about the mode of formation of coal and the age of the stratigraphical succession in the Sydney Basin. Clarke makes the first mention of his discovery of the Lake Macquarie fossil forest, the first identification of the zeolite stilbite in New South Wales and gives details of his study of the volcanic rocks of the Upper Hunter Valley. Keywords: Clarke, Macleay, coal formation, Sydney Basin, stilbite INTRODUCTION essentially self-contained, although, of course, almost no letter can stand alone, but depends When Dr Thomas G. Vallance died in 1993 a on the correspondents. Each letter has some considerable amount of his historical jottings importance in dealing with aspects of Clarke’s and memorabilia on the history of Australian geological work, as will be noted. science, and particularly geology, was passed The first and longest letter, which is ac- on to me (David Branagan) through his wife, companied by a long series of memoranda and Hilary Vallance. For various reasons, only now a labelled sketch fits between two letters from have I been able to delve, even tentatively, into MacLeay (28 June & 4 July 1842) to Clarke. this treasure house. The present note con- Both these MacLeay letters have been repro- cerns four letters of the Reverend W.B. -
Mary Anning: Princess of Palaeontology and Geological Lioness
The Compass: Earth Science Journal of Sigma Gamma Epsilon Volume 84 Issue 1 Article 8 1-6-2012 Mary Anning: Princess of Palaeontology and Geological Lioness Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/compass Part of the Paleontology Commons Recommended Citation Davis, Larry E. (2012) "Mary Anning: Princess of Palaeontology and Geological Lioness," The Compass: Earth Science Journal of Sigma Gamma Epsilon: Vol. 84: Iss. 1, Article 8. Available at: https://digitalcommons.csbsju.edu/compass/vol84/iss1/8 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in The Compass: Earth Science Journal of Sigma Gamma Epsilon by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. Figure. 1. Portrait of Mary Anning, in oils, probably painted by William Gray in February, 1842, for exhibition at the Royal Academy, but rejected. The portrait includes the fossil cliffs of Lyme Bay in the background. Mary is pointing at an ammonite, with her companion Tray dutifully curled beside the ammonite protecting the find. The portrait eventually became the property of Joseph, Mary‟s brother, and in 1935, was presented to the Geology Department, British Museum, by Mary‟s great-great niece Annette Anning (1876-1938). The portrait is now in the Earth Sciences Library, British Museum of Natural History. A similar portrait in pastels by B.J.M. Donne, hangs in the entry hall of the Geological Society of London. -
Skull Remains of the Dinosaur Saturnalia Tupiniquim (Late Triassic, Brazil): with Comments on the Early Evolution of Sauropodomorph Feeding Behaviour
RESEARCH ARTICLE Skull remains of the dinosaur Saturnalia tupiniquim (Late Triassic, Brazil): With comments on the early evolution of sauropodomorph feeding behaviour 1 2 1 Mario BronzatiID *, Rodrigo T. MuÈ llerID , Max C. Langer * 1 LaboratoÂrio de Paleontologia, Faculdade de Filosofia Ciências e Letras de Ribeirão Preto, Universidade de a1111111111 São Paulo, Ribeirão Preto, São Paulo, Brazil, 2 Centro de Apoio à Pesquisa PaleontoloÂgica, Universidade Federal de Santa Maria, Santa Maria, Rio Grande do Sul, Brazil a1111111111 a1111111111 * [email protected] (MB); [email protected] (MCL) a1111111111 a1111111111 Abstract Saturnalia tupiniquim is a sauropodomorph dinosaur from the Late Triassic (Carnian±c. 233 OPEN ACCESS Ma) Santa Maria Formation of Brazil. Due to its phylogenetic position and age, it is important for studies focusing on the early evolution of both dinosaurs and sauropodomorphs. The Citation: Bronzati M, MuÈller RT, Langer MC (2019) Skull remains of the dinosaur Saturnalia tupiniquim osteology of Saturnalia has been described in a series of papers, but its cranial anatomy (Late Triassic, Brazil): With comments on the early remains mostly unknown. Here, we describe the skull bones of one of its paratypes (only in evolution of sauropodomorph feeding behaviour. the type-series to possess such remains) based on CT Scan data. The newly described ele- PLoS ONE 14(9): e0221387. https://doi.org/ ments allowed estimating the cranial length of Saturnalia and provide additional support for 10.1371/journal.pone.0221387 the presence of a reduced skull (i.e. two thirds of the femoral length) in this taxon, as typical Editor: JuÈrgen Kriwet, University of Vienna, of later sauropodomorphs.