The Big Dinosaur Dig Free

Total Page:16

File Type:pdf, Size:1020Kb

The Big Dinosaur Dig Free FREE THE BIG DINOSAUR DIG PDF Esther Ripley | 48 pages | 21 Sep 2009 | DK Publishing (Dorling Kindersley) | 9780756655952 | English | New York, NY, United States The Big Dinosaur Dig (DK READERS) - It's been million years since the last Jurassic dinosaurs roamed the planet. Millennia have The Big Dinosaur Dig and today on the prairies of northern Wyoming, USA, it is hot and arid. At a glance, away from the isolated towns, the landscape is devoid of The Big Dinosaur Dig save juniper, sagebrush and the occasional rattlesnake or black widow spider. But evidence of a prehistoric world filled with lush greenery, dinosaurs and a variety of other extinct animals are just below the rocky surface. In summerscientists from the Natural History Museum, Londonset out for Wyoming to help reveal what has been hidden for millions of years. Dinosaurs that lived during the Jurassic Period around million years ago are arguably some of the world's best known. They include DiplodocusStegosaurus and Allosaurus - or, as Museum dinosaur researcher Dr Susannah Maidment puts it, 'all of the ones you knew when you were seven'. But there is still plenty about these widely recognised animals and the world they lived in The Big Dinosaur Dig we don't fully understand. The first team from the Museum to arrive in Wyoming inled by Prof Paul Barrett, marked crossing the state border with a photo. Mission Jurassic is a project led by the Children's The Big Dinosaur Dig of Indianapolis, which aims not only to dig up dinosaur fossils for display, but also to learn as much as possible about what western North America was like million years ago. Two teams from the Natural History Museum joined the project in to help explore the The Big Dinosaur Dig Mile - a square mile in northern Wyoming - bringing along experts in fossil preparation, microvertebrates, palaeobotany, fossil fish and marine invertebrates. After two weeks on site, a second group from the Museum, led by Dr Susannah Maidment, took over from Prof Barrett and his team. Prof Barrett says, 'All of the Mission Jurassic partners brought with them people who are either specialists in different scientific areas or have expertise in doing these kinds of excavations. From approximately million years ago, a shallow sea known as the Sundance Sea covered much of western North America. It was connected to the ocean by a narrow channel that stretched north for over a thousand miles. As this sea withdrew, it was replaced by rivers and floodplains which deposited sediments and formed the rocks known as the Morrison Formation. Today only a small amount of this approximately 1. The Morrison Formation yellow stretches across roughly 1. The two dinosaur footprints on the map represent the The Big Dinosaur Dig location The Big Dinosaur Dig the Jurassic Mile in Wyoming orange. Dr Maidment says, 'During the Late Jurassic Period, about million years ago, this area of Wyoming was a broad, shallow plain inhabited by dinosaurs like StegosaurusDiplodocus and Allosaurus. There were forests and plants - it would have been quite a green landscape. On the Jurassic Mile, evidence of these prehistoric reptiles is scattered across the landscape, with fossilised bones naturally weathering out of rocks and tumbling down the hillsides almost everywhere you look, and even more being slowly dug out of two quarries. The Jurassic Mile is exceptionally rich in dinosaur fossils and the teams found lots of evidence of bones across the site. As well as the dinosaur- bearing Morrison Formation rocks, a large swathe of rocks laid down by the earlier sea are also exposed. Some of the rocks of the Sundance Formation were deposited within a calm lagoon in exceptionally thin layers called paper shales. Palaeontologists can gently tease the layered rocks apart by hand or with tools to find The Big Dinosaur Dig and ancient animals, such as small fish and insects, fossilised The Big Dinosaur Dig them. Fossil fish curator Emma Bernard says, 'The rock is very finely laminated. It's almost like the pages of a book. So we had to be really careful when we were excavating. The team also found abundances of belemnites, Gryphaea and oysters at different layers within the Sundance Formation, providing evidence of different marine environments. Fossil invertebrates curator Dr Tim The Big Dinosaur Dig explains, 'Oysters are strange animals that can live in parts of the sea that other animals find difficult, whether because of the salinity, temperature The Big Dinosaur Dig even the roughness of the water. As they are one of the few organisms capable of tolerating extreme environments and grow quite quickly, oysters can dominate an area. You can end up with very thick beds of oysters. The accumulations of different fossils found throughout the Sundance Formation, on the Jurassic Mile and elsewhere, provide evidence that sea levels and conditions changed considerably over time. In one layer of the Sundance Formation, the team came across thousands of Gryphaea carpeting The Big Dinosaur Dig hillside. These now-extinct animals are also known as devil's toenails. Dinosaur hunting can be quite low-tech. Palaeontologists can spend hours walking through a site and staring at the ground, searching for clues that a dinosaur might be hidden in the rocks below. We don't just go outside and find beautiful skeletons lying on the surface. It takes The Big Dinosaur Dig bit of practice,' says Prof Barrett. Bernard explains, 'Sometimes it can be tough to tell a rock from a fossil, and you have to really get your eye in. But one of the best ways to tell is to try and find anything black and shiny in the rock - that can often be a good indication of a tooth or scale. Although the The Big Dinosaur Dig experts are seasoned professionals, finding a fossil in the field is still an exciting experience. But there are more than just dinosaurs in the Morrison Formation. Finding fossilised plants could help scientists to understand more about Jurassic ecosystems. Palaeobotanist Dr Paul Kenrick explains, 'One of the really nice things about the Jurassic Mile is that you've got the bones of dinosaurs together with the plants. That really gives us the context of where these animals lived. You commonly get leaves and fossilised wood. But one of the most common you can't actually see in the field - these are pollen grains and spores, which you have to take back to the lab and dissolve the rock. Plant life in Morrison time would have been much more productive than what is found in the semi-desert conditions of Wyoming today. There would have been predominantly tall conifers with an understory of ferns and small shrubs, as grass and flowering plants hadn't evolved million years ago. The Big Dinosaur Dig dinosaurs like Diplodocus and Brachiosaurus were huge animals. Understanding the The Big Dinosaur Dig these herbivores would have relied on The Big Dinosaur Dig help scientists to answer key questions, such as how these reptiles were able to grow to their colossal sizes. Although palaeontologists know that the rocks of the Jurassic Mile are around million years old, determining a more specific age is challenging - but that's exactly what Dr Maidment intends to do. In marine sediments, scientists can use fossilised microscopic organisms to correlate rocks from one place to another, sometimes accurately determining their age. But because the Morrison sediments were laid down on land, this approach won't work. But that's also difficult because there's not very much ash here,' explains Dr Maidment. Dr Maidment uses a hand lens to get an up-close look at a rock sample from The Big Dinosaur Dig bottom of the Morrison Formation. Instead she and PhD student Joe Bonsor have logged the style of sediments to help compare the terrestrial rocks to those in other The Big Dinosaur Dig. Bonsor says, 'We want to work out the geological history of the area. We want to know what the environment was like when the dinosaurs lived all those millions of years ago. We then piece all The Big Dinosaur Dig that together and that feeds into the wider picture'. The Jurassic Mile has been explored by the Children's Museum in previous years. When Prof Barrett and his crew arrived in Wyoming intheir first job was to begin clearing the site, which had spent the winter buried under a protective layer of rocks. Prof Barrett says, 'We got into the quarries and started shifting rock and sweeping down the surfaces so that we could see The Big Dinosaur Dig was The Big Dinosaur Dig on. Once they had reached the bone bed, they slowed down and began to painstakingly reveal ancient animals millimetre by millimetre - a job Dr Maidment and her crew continued when they arrived on site two weeks later. Mark Graham is the Natural History Museum's senior The Big Dinosaur Dig preparator. His day-to-day role involves working with the fossils that palaeontologists bring back from expeditions. But on Mission Jurassic, he got to dig The Big Dinosaur Dig the bones himself. He says, 'It was fantastic on the first day to uncover a scapula of one of these gigantic dinosaurs, and later to find a large claw bone. So exposing and stabilising them in the quarry is a slight role reversal for me. Finding large The Big Dinosaur Dig bones isn't easy, but it's nothing compared to uncovering those of smaller animals, such as amphibians and mammals, which lived alongside them. Finding microvertebrates is an important part of understanding what the environment would have been like in a particular area millions of years ago.
Recommended publications
  • 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]
  • A Reassessment of the Purported Ankylosaurian Dinosaur Bienosaurus Lufengensis from the Lower Lufeng Formation of Yunnan, China
    A reassessment of the purported ankylosaurian dinosaur Bienosaurus lufengensis from the Lower Lufeng Formation of Yunnan, China THOMAS J. RAVEN, PAUL M. BARRETT, XING XU, and SUSANNAH C.R. MAIDMENT Raven, T.J., Barrett, P.M., Xu, X., and Maidment, S.C.R. 2019. A reassessment of the purported ankylosaurian dinosaur Bienosaurus lufengensis from the Lower Lufeng Formation of Yunnan, China. Acta Palaeontologica Polonica 64 (2): 335–342. The earliest definitive ornithischian dinosaurs are from the Early Jurassic and are rare components of early dinosaur faunas. The Lower Lufeng Formation (Hettangian–Sinemurian) of Yunnan Province, China, has yielded a diverse Early Jurassic terrestrial vertebrate fauna. This includes several incomplete specimens have been referred to Ornithischia, including the type specimen of the thyreophoran “Tatisaurus” and other generically indeterminate material. The highly fragmentary Lufeng ornithischian Bienosaurus lufengensis was described briefly in 2001 and identified as an ankylo- saurian dinosaur. Recent studies have cast doubt on this hypothesis, however, and given that the referral of Bienosaurus to Ankylosauria would result in an extensive ghost-lineage extending between it and the first definitive eurypodans (ankylosaurs + stegosaurs) in the Middle Jurassic, the holotype specimen is re-examined and re-described. We identify Bienosaurus as a probable thyreophoran dinosaur, although the fragmentary nature of the material and the absence of autapomorphies means that the specimen should be regarded as a nomen dubium. Key words: Dinosauria, Ornithischia, Thyreophora, anatomy, Jurassic, Lufeng Formation, Yunnan, China. Thomas J. Raven [[email protected]], Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK; School of Environment and Technology, University of Brighton, Lewes Road, Brighton BN1 4JG, UK.
    [Show full text]
  • Abstracts Volume
    SPPC/GCG Conference Controlled exsiccation of fossilised remains in waterlogged marl: Slowly Slowly Dryee Squiddie LU ALLINGTON-JONES * 1 1 - The Natural History Museum, Conservation A fossil from a squid-like animal, preserved in Lower Jurassic argillaceous limestone or marl, was collected on the 8th March 2019 from Lyme Regis beach. The collectors kept the specimen wet by wrapping it in newspaper and plastic, and transported it to the Conservation Centre at the Natural History Museum in London (UK). Conservators partially immersed the block in water, with a few drops of thymol to prevent mould growth, whilst tests on samples of the matrix were undertaken. Two consolidants were selected from the field of waterlogged archaeological artefact conservation: Primal WS24 and PEG 400. Untreated and consolidated samples were variously dried rapidly in ambient lab conditions or dried slowly within Dartek C-917 semi-permeable cast nylon film microenvironments. Both consolidation and slow drying proved beneficial but insufficient to prevent cracking entirely. A double layer of film was then considered, to slow the drying-time even further. The entire specimen block was then consolidated by immersion in 10% and then 33% Primal WS24 before slow drying in a double-layer Dartek C-917 film microclimate. Primal WS24 was selected in preference to PEG 400 because the former would be compatible with Paraloid B72 in acetone (if future remedial conservation becomes necessary). After drying, parts of the surface of the block were prepared using a split-V ultrasonic tool, to expose more of the nacre layer, and the lower half of the block was removed using rotary tools to minimise vibration.
    [Show full text]
  • The Palaeontology Newsletter
    The Palaeontology Newsletter Contents100 Editorial 2 Association Business 3 Annual Meeting 2019 3 Awards and Prizes AGM 2018 12 PalAss YouTube Ambassador sought 24 Association Meetings 25 News 30 From our correspondents A Palaeontologist Abroad 40 Behind the Scenes: Yorkshire Museum 44 She married a dinosaur 47 Spotlight on Diversity 52 Future meetings of other bodies 55 Meeting Reports 62 Obituary: Ralph E. Chapman 67 Grant Reports 72 Book Reviews 104 Palaeontology vol. 62 parts 1 & 2 108–109 Papers in Palaeontology vol. 5 part 1 110 Reminder: The deadline for copy for Issue no. 101 is 3rd June 2019. On the Web: <http://www.palass.org/> ISSN: 0954-9900 Newsletter 100 2 Editorial This 100th issue continues to put the “new” in Newsletter. Jo Hellawell writes about our new President Charles Wellman, and new Publicity Officer Susannah Lydon gives us her first news column. New award winners are announced, including the first ever PalAss Exceptional Lecturer (Stephan Lautenschlager). (Get your bids for Stephan’s services in now; check out pages 34 and 107.) There are also adverts – courtesy of Lucy McCobb – looking for the face of the Association’s new YouTube channel as well as a call for postgraduate volunteers to join the Association’s outreach efforts. But of course palaeontology would not be the same without the old. Behind the Scenes at the Museum returns with Sarah King’s piece on The Yorkshire Museum (York, UK). Norman MacLeod provides a comprehensive obituary of Ralph Chapman, and this issue’s palaeontologists abroad (Rebecca Bennion, Nicolás Campione and Paige dePolo) give their accounts of life in Belgium, Australia and the UK, respectively.
    [Show full text]
  • New Finds of Stegosaur Tracks from the Upper Jurassic Lourinhã Formation, Portugal
    New finds of stegosaur tracks from the Upper Jurassic Lourinhã Formation, Portugal OCTÁVIO MATEUS, JESPER MILÀN, MICHAEL ROMANO, and MARTIN A. WHYTE Eleven new tracks from the Upper Jurassic of Portugal are the central−western part of Portugal and especially in the vicinity described and attributed to the stegosaurian ichnogenus of the small town of Lourinhã approximately 70 km north of Deltapodus. One track exhibits exceptionally well−preserved Lisboa (Fig. 1). The sediments of the Lourinhã Formation were impressions of skin on the plantar surface, showing the deposited in the Lusitanian Basin and comprise in excess of 400 stegosaur foot to be covered by closely spaced skin tubercles m of terrestrial sediments, deposited during the latest Jurassic of ca. 6 mm in size. The Deltapodus specimens from the (Late Kimmeridgian–Early Tithonian), during the initial rifting Aalenian of England represent the oldest occurrence of stage of the Atlantic Ocean (Hill 1989). stegosaurs and imply an earlier cladogenesis than is recog− The sediments predominantly consist of thick beds of red and nized in the body fossil record. green clay, interbedded with massive, fluvial sandstone bodies and heterolithic beds. The Lourinhã Formationhasyieldedanex− Introduction tensive vertebrate fauna (Lapparent and Zbyszewski 1957; Galton 1980; Antunes 1998; Antunes et al. 1998; Mateus et al. 1998, The European stegosaur track record is scarce, compared to the 2006; Antunes and Mateus 2003; Pereda−Superbiola et al. 2005; number of tracks described for other dinosaur groups. The Mateus 2006; Escaso et al. 2007) and abundant carbonized frag− track Deltapodus brodricki Whyte and Romano, 1994, descri− ments of plants and large fossilized logs (Pais 1998).
    [Show full text]
  • Progressive Palaeontology 2007
    Progressive Palaeontology 2007 Thursday 12th – Saturday 14th April Department of Earth Sciences, University of Bristol 2 Welcome and acknowledgements We are pleased to welcome you to the Department of Earth Sciences at the University of Bristol for this year’s Progressive Palaeontology meeting. This appears to be the best attended and most presentation-packed Progressive Palaeontology on record – we are just shy of 60 delegates and there are 30 presentations in total (24 oral and 6 poster). As always Progressive Palaeontology’s aim is to provide a framework in which to present ideas and discuss work with those at a similar stage in their career. In order to achieve this the Friday presentation session is supplemented by two social events and a field trip. On Thursday evening there is a pre-conference gathering at the Berkeley pub (opposite the department on Queen’s Road) and following the presentation sessions on Friday there will also be an evening reception/dinner at Bristol Zoo. This year’s field trip will be to Aust Cliff (a site famous for its Late Triassic fish fossils – see the brief guide at the end of this booklet). We are lucky to have two experts on this site joining us on the day and we have scheduled a reasonably late start so please do come along if you have registered! We would also like to take this opportunity to thank the following individuals who have helped in supporting, preparing and running this year’s meeting: The Palaeontological Association and the University of Bristol Alumni Foundation for providing sponsorship.
    [Show full text]
  • Newsletter 94 2 Editorial
    The Palaeontology Newsletter Contents 94 Editorial 2 Association Business 3 Annual Meeting 2017 3 Prizes & Awards at Lyon 9 Association Meetings 21 PalAss is 60 23 News 27 Lyme Regis Fossil Festival 33 From our correspondents Legends of Rock: Isabel Cookson 34 Behind the scenes at the Museum 36 Brief Moments 40 R for palaeontologists 44 Advertisement: Hills of Hame 55 Future meetings of other bodies 56 Meeting Reports 63 Mystery Fossil 25 71 Outreach Report 72 Grant and Bursary Reports 74 Book Reviews 97 Careering off course! 103 Palaeontology vol. 60 parts 1 & 2 105–106 Papers in Palaeontology, Virtual Palaeontology 107 Reminder: The deadline for copy for Issue no. 95 is 5th June 2017. On the Web: <http://www.palass.org/> ISSN: 0954-9900 Newsletter 94 2 Editorial Welcome to the first issue of the PalAss Newsletter for 2017, and what a historic year this is: the 60th anniversary of the Association. From humble beginnings as an informal dining club, the Association has evolved into one of the premier global organisations for promoting palaeontology and its allied sciences. Of particular note is how the Association’s initial activities – the establishment of the journal Palaeontology, the Newsletter and a ‘Discussion Meeting’ – have expanded into a substantial portfolio of activities that, in addition to these early bastions of the Association, include an impressive array of grant programmes, awards and honours, support of palaeontology-themed sessions at meetings of other bodies, and a strong presence at key public outreach events for palaeontology, all of which can be explored via the newsletter or the Association’s website.
    [Show full text]
  • Notice of Annual General Meeting and Annual Address
    Notice of Annual General Meeting and Annual Address The 173rd Annual General Meeting will be held in the Neil Chalmers Seminar Room of the Natural History Museum, London, SW7 5BD, on Wednesday, 22nd April, 2020, at 4.00 pm. The Annual Report of Council will be presented, along with the Income and Expenditure Accounts for the year ended 31st December, 2019, and Council Members and Officers will be elected for the ensuing year. Tea and coffee will be available from 3.30 pm. This meeting is open to all members of the Society. The AGM will be followed by the Society’s Fourteenth Annual Lecture, to be given by Emeritus Professor Derek J. Siveter (University of Oxford). The event will be held in the Neil Chalmers Seminar Room of the Natural History Museum, Cromwell Road, London, SW7 5BD, at 4.15 pm. This event is open to members of the Society and other interested parties. -------------------------------------------------------------------------------------------------------------------------------------------- NEWSLETTER 36 1. Publications: Volume 172 (parts 651 and 652 for 2018) were published in March and April 2019, respectively. Volume 173 (parts 653 to 655) were published in August, November and December 2019, respectively. Vol. 172, for 2018 651. British Silurian myodocope ostracods, by V. Perrier, D.J. Siveter, M. Williams & D. Palmer (pp. 1-64, plates 1-17). 652. Llandovery brachiopods from England and Wales, by L.R.M. Cocks (pp. 1-262, plates 1-41). Vol. 173, for 2019 653. The Early Jurassic Bivalvia from the Hettangian and Lower Sinemurian of south-west Britain, Part 3, by P. Hodges (pp.113-143, plates 11-14).
    [Show full text]
  • The 'Fabrosaurid' Ornithischian Dinosaurs of the Upper Elliot Formation (Lower Jurassic) of South Africa and Lesotho
    Blackwell Science, LtdOxford, UKZOJZoological Journal of the Linnean Society0024-4082The Lin- nean Society of London, 2005? 2005 1452 175218 REVIEW Article ‘FABROSAURIDS’ OF THE UPPER ELLIOT FORMATIONR. J. BUTLER Zoological Journal of the Linnean Society, 2005, 145, 175–218. With 26 figures The ‘fabrosaurid’ ornithischian dinosaurs of the Upper Elliot Formation (Lower Jurassic) of South Africa and Lesotho RICHARD J. BUTLER* Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK, and Department of Palaeontology, The Natural History Museum, Cromwell Road, London, SW7 5BD, UK Received October 2004; accepted for publication March 2005 The Upper Elliot Formation of South Africa and Lesotho contains the world’s most diverse fauna of early Jurassic ornithischian dinosaurs. Nevertheless, despite four decades of work on this fauna there remains significant taxonomic confusion and many important specimens remain undescribed. A review of the non-heterodontosaurid (‘fabrosaurid’) ornithischians of the Upper Elliot Formation is presented, following re-examination of all known orni- thischian material from the Elliot Formation. ‘Fabrosaurus australis’ is based upon a single undiagnostic dentary, and is here considered a nomen dubium. Lesothosaurus diagnosticus is considered to be valid and is rediagnosed based upon a unique combination of plesiomorphic and derived characteristics. Stormbergia dangershoeki gen. et. sp. nov. is described from three partial skeletons including numerous postcranial material. Stormbergia dan- gershoeki is significantly larger than previously described Elliot Formation ornithischians, and can be recognized on the basis of a unique combination of characters, the most important of which is the possession of a distinctive tab- shaped obturator process on the ischium.
    [Show full text]
  • Completeness of the Dinosaur Fossil Record: Disentangling Geological and Anthropogenic Biases
    COMPLETENESS OF THE DINOSAUR FOSSIL RECORD: DISENTANGLING GEOLOGICAL AND ANTHROPOGENIC BIASES by DANIEL DAVID CASHMORE A thesis submitted to the University of Birmingham for the degree of DOCTOR OF PHILOSOPHY September 2019 School of Geography, Earth and Environmental Sciences, College of Life and Environmental Sciences, University of Birmingham University of Birmingham Research Archive e-theses repository This unpublished thesis/dissertation is copyright of the author and/or third parties. The intellectual property rights of the author or third parties in respect of this work are as defined by The Copyright Designs and Patents Act 1988 or as modified by any successor legislation. Any use made of information contained in this thesis/dissertation must be in accordance with that legislation and must be properly acknowledged. Further distribution or reproduction in any format is prohibited without the permission of the copyright holder. Abstract Non-avian dinosaurs were a highly successful clade of terrestrial tetrapods that dominated Mesozoic ecosystems. Their public and scientific popularity makes them one of most intensely researched and understood fossil groups. Key to our understanding of their evolutionary history are interpretations of their changing diversity through geological time. However, spatiotemporal changes in fossil specimen completeness, diagnostic quality, and sampling availabil- ity can bias our understanding of a group’s fossil record. Methods quantifying the level of skeletal and phylogenetic information available for a fossil group have previously been used to assess potential bias. In this thesis, these meth- ods are used to critically assess the saurischian dinosaur fossil record, includ- ing an examination of changes in specimen completeness through research time.
    [Show full text]
  • Hastings & District Geological Society Journal
    Hastings & District Geological Society Journal Hastings and District Geological Society affiliated to the Geologists’ Association President Professor G. David Price, UCL Founded 1992 Cliffs beyond Ecclesbourne Glen with fallen block of ripple-marked sandstone in the foreground Volume 21 December 2015 Cover picture: Cliffs beyond Ecclesbourne Glen with fallen block of ripple-marked sandstone in the foreground - photo: Peter Austen This Journal is issued free to members of the Hastings & District Geological Society (HDGS) and is also freely available on the HDGS website. Contributions for next year’s Journal would be appreciated and should be submitted by the October 2016 meeting. Please contact Peter Austen on: tel: 01323 899237 or e-mail: [email protected] The Hastings & District Geological Society does not accept responsibility for the views expressed by individual authors in this Journal. Taxonomic/Nomenclatural Disclaimer - This publication is not deemed to be valid for taxonomic/nomenclatural purposes. CONTENTS - Vol. 21, December 2015 2015 Officials and Committee …………………………………………………………………………………… 1 In Conversation with the Past - by Siân Evans …………………………………………………………………... 2 Réunion Island - by Margaret A. Dale …………………………………………………………………………… 4 William Smith and the Castle Hill Section - Part 2 - by Anthony Brook …………………….………………….. 7 How Britain became an island - by Professor Sanjeev Gupta - reported by Peter Austen ………………………. 12 The Cretaceous Greenhouse World and its Impact on the Evolution of Land Vertebrates - by Professor Paul Upchurch ……………….. 14 News from the Weald …………………….……………………………………………………………………… 16 Smokejacks Brickworks - by Peter Austen …………………….………………………………………………… 18 HDGS/GA field meeting: Rock-a-Nore to past Ecclesbourne Glen, Sunday, 26th July 2015 - by Ken Brooks, Peter Austen and Ed Jarzembowski ………….. 21 Langhurstwood Quarry, Warnham - by Peter Austen …………………….……………………………………..
    [Show full text]
  • 17 July 2021 Aperto
    AperTO - Archivio Istituzionale Open Access dell'Università di Torino MORPHOLOGY, TAXONOMY, AND PHYLOGENETIC RELATIONSHIPS OF THE MONTEVIALE CROCODYLIANS (OLIGOCENE, ITALY). This is the author's manuscript Original Citation: Availability: This version is available http://hdl.handle.net/2318/1703198 since 2019-05-29T10:01:05Z Publisher: Samson, R., et al. Terms of use: Open Access Anyone can freely access the full text of works made available as "Open Access". Works made available under a Creative Commons license can be used according to the terms and conditions of said license. Use of all other works requires consent of the right holder (author or publisher) if not exempted from copyright protection by the applicable law. (Article begins on next page) 09 October 2021 The 66th Symposium on Vertebrate Palaeontology and Comparative Anatomy Universities of Manchester September 5th-8th 2018 PROGRAMME AND ABSTRACTS Welcome to Manchester for SVPCA and SPPC 2018, the 66th Symposium on Vertebrate Palaeontology and Comparative Anatomy with the Symposium of Palaeontological Preparation. Herein you will find information about the schedule and programme of events including the line-up of oral and poster presentations, details about the social events, and a guide to the conference. The abstract booklet is available as a PDF only (emailed to delegates and at www.svpca.org) Local Host Committee: Robert Sansom, University of Manchester (Chair) Robin Beck, University of Salford Charlotte Brassey, Manchester Metropolitan University Robert Brocklehurst,
    [Show full text]