Exhibit Resource

Total Page:16

File Type:pdf, Size:1020Kb

Exhibit Resource Exhibit Resource Travel back to the Mesozoic Era and introduce your students to the most remarkable marine reptiles that once dominated the seas. Students will learn about these incredible sea monsters, come face-to-face with the mightiest marine reptile of the Jurassic seas and meet living creatures that have inhabited planet Earth for millions of years. Exhibit highlights include: Life-sized replicas of the most amazing species that ever lived, including 42-foot Elasmosaurus, 20-foot Kronosaurus, 21-foot Zygorhiza, 16-foot Dunkleosteus and 34-foot Liopleurodon. Interactive and educational stations where your students can explore a variety of prehistoric and living marine species, compare replicas of the largest sea turtles that ever lived and become an amateur paleontologist in a fossil research quarry. New live aquarium residents — the beautifully intricate chambered nautilus, the mysterious giant isopod, and the large and leggy Japanese spider crab. The Exhibit Resource includes: Mass Extinction and Moving Continents (Page 2) How Fossils Form and Make A Fossil Activity (Page 3) Animal Fossils Matching Game (Page 4): Answer Key Liopleurodon B Shark E Nautilus D Octopus A Sea Turtle C Tyrannosuarus F Dinosaur vs. Marine Reptile (Page 5) The First Invertebrates and Prehistoric Fish Scavenger Hunt (Page 6) Ancient Aquatic Animal Scavenger Hunt (Page 7) Answer Key Sea Anemone Cambrian Period Horseshoe Crab Devonian Period Shark Devonian Period Crocodile Triassic Period Sea Turtle Triassic Period Frog Triassic Period Penguin Paleocene Epoch Hippopotamus Miocene Epoch Orthoceros Ordovician Period Geologic Time Chart (Page 8) Web Resources http://www.adventureaquarium.com/What-to-do/Dinosaurs-of-the-Deep.aspx http://www.prehistoric-wildlife.com/ http://www.ucmp.berkeley.edu/help/timeform.php http://dinosaurs.about.com/od/aquaticdinosaurs/ 1 Moving Continents Over millions of years, Earth’s land masses have drifted slowly around the globe. Triassic Period Jurassic Period Cretaceous Period Earth Today All of the world’s land was part Pangea split into northern Shallow seas came and went, Today the continents are still of a great continent called Laurasia and southern dividing the continents into moving. Millions of years Pangea. The first dinosaurs Gondwana. their present form. from now the Earth will be appeared during this period. unrecognizable again. Mass Extinction Over 90% of all species that have ever lived on Earth are extinct. As they disappear, new ones evolve to take their place. Several extinction events have taken place in the past, each wiping out many species. The cause of each is a mystery but prime culprits seem to be extreme volcanic eruptions and impacts of massive objects from space, resulting in global climate change. *mya = millions of years ago The Five Largest Mass Extinctions: Ordovician-Silurian extinction 443 mya / 85% marine life lost. Late Devonian extinction 359 mya / 70% of marine species were lost Permian-Triassic extinction 248 mya / 96% of all species were lost. End Triassic extinction 200 mya / 52% animal species were lost. Cretaceous-Tertiary extinction 65 mya / 75% species lost including the dinosaurs. Is a mass extinction happening now? Scientists suggest that we are in the middle of a mass extinction event, the fastest in Earth's history. In 500 years, at least 322 types of animals have disappeared and over 20,000 species are now threatened with extinction. Humans will need to take responsibility— by the year 2100, human activities such as pollution, land clearing, and overfishing may have driven more than half of the world's marine and land species to extinction. Conservation is the key! To learn more, visit these websites: http://www.bbc.co.uk/nature/extinction_events http://www.smithsonianchannel.com/sc/web/show/3413789/mass-extinction-life-at-the-brink 2 How Fossils Form Fossils are the remains or an impression of an animal or plant that existed in the past. Fossilization depends on a series of chances: Step 1. Step 2. An animal dies and its body is The river floods and covers washed by a flood onto a river the bones in mud and other bank. Its flesh, guts and other soft sediment. This happens many parts are eaten by scavengers or times, burying the bones rotted away, leaving only bones. deeper. Step 3. Step 4. Minerals from the sediment seep Over millions of years, the into the bones, slowly replacing the forces of nature gradually bone and turning it to stone. wear away the upper Pressure increases within the many layers until the fossilized layers of sediment turning it into animal bones are finally solid rock. exposed. Make A Fossil Activity Directions: Stir together the coffee grounds, cold coffee, flour, and salt until well mixed. Knead the dough together and then flatten it out onto the waxed paper. Use the can or cup to cut out circles of the dough. Materials: Press an object firmly into the dough. When you take the object out, you 1 cup of used coffee grounds have an impression of your object. 1/2 cup of cold coffee Let your “fossil” dry overnight. 1 cup of flour 1/2 cup of salt Wax paper Celebrate the 5th Annual National Fossil Day Mixing bowl Small objects to make impressions in the dough October 14, 2015 Empty can or cup http://www.nature.nps.gov/geology/nationalfossilday/index.cfm (diameter larger than your objects ) 3 Animal Fossils What we know about animals in the past is mostly based on the fossils they leave behind. At Adventure Aquarium, you will find the animals below, either modern versions in one of our live animal exhibits or models/skeletons/images in the Dinosaurs of the Deep exhibit. Match the animals with the picture of their fossil. Seeing a photo or drawing of the animal can also help you figure it out. Learning more about each animal will help you understand the kind of fossil they would leave behind. A B Liopleurodon Fossil ______ D C Shark Fossil ______ Nautilus Fossil ______ Octopus Fossil ______ E Sea Turtle Fossil ______ F Tyrannosaurus Fossil ______ 4 What is a Dinosaur? Dinosaurs were the dominant terrestrial vertebrates of the Mesozoic Era. Unlike other reptiles, whose limbs splay out beneath them, dinosaurs walked either on 4 legs with their legs directly beneath their body or upright on 2 legs (like modern birds). Scientists are still debating whether dinosaurs were cold-blooded or warm-blooded. And dinosaurs were thought to be strictly terrestrial, but recent discoveries suggest that the largest-known carnivorous dinosaur, Spinosaurus, may also be the first-known swimming dinosaur! Chindesaurus Triceratops What is a Marine Reptile? Marine reptiles are reptiles which have become adapted for an aquatic or semi-aquatic life in the ocean. During the Mesozoic Era, while dinosaurs were dominating the land, several groups of reptiles became adapted to life in the seas, including turtles and crocodiles. Three reptile groups became top predators: Ichthyosaurs, Plesiosaurs and Mosasaurs. Ichthyosaur Mosasaur Plesiosaur Archelon Dakosaurus (Prehistoric (Prehistoric Sea Turtle) Crocodile) Liopleurodon Liopleurodon was a 34-foot long short-necked plesiosaur, with a massive head, big mouth and thick body making it perfectly adapted to attack and kill. “Lio” was the apex predator of the Jurassic seas. It could produce sudden bursts of speed when hunting, then use its powerful jaw muscles to drive 4 inch teeth into its prey. The extinction of the dinosaurs and large marine reptiles at the end of the Mesozoic Era favored the rise of other animal species. On the land, mammals would diversify and flourish, while sharks would become the apex predator of the seas. 5 The First Vertebrates Between 500 and 400 million years ago (mya), life on earth was dominated by prehistoric fish. The Devonian Period (419—359 mya) is often referred to as the “Age of Fishes” because major groups of fish evolved during this time, including sharks. Prehistoric fish established the template for later vertebrate evolution. For a quick lesson on vertebrate evolution watch this episode of Carl Sagan’s Cosmos on evolution. https://www.youtube.com/watch?v=gZpsVSVRsZk Here is a scavenger hunt for you to try when you visit Dinosaurs of the Deep. Older students: See if you can find modern fish with similar shapes and features. 6 Ancient Aquatic Animal Scavenger Hunt Many of the animal species found in Adventure Aquarium first evolved millions of years ago and are still around today. Look for these animals as you walk around the aquarium. When you find one, place a check in the box next to the picture. After each animal’s name is when they first appeared millions of years ago (“mya”). Sea Anemone 520 mya Horseshoe Crab 400 mya Shark 360 mya These flower-like animals are You can touch this ancient This apex predator can be found with clown fish. invertebrate during your visit. found in several locations. Time period __________________ Time period __________________ Time period __________________ Crocodile 225 mya Sea Turtle 220 mya Frog 200 mya She spends her day resting in This giant swims with the zebra Hop up to Kid Zone to find this the Orinoco River exhibit. and hammerhead sharks. little guy and his frog friends. Time period __________________ Time period __________________ Time period __________________ BONUS: This one is a little tricky. Find the fossil of this extinct ancestor of the octopus and nautilus. Penguin 60 mya Hippopotamus 15 mya You will need to step She’s easy to find—just head outside to visit this bird. for Hippo Haven. Time period __________________ Time period __________________ Orthoceros 450 mya Look for these fossilized shells in the floor of the Rotunda. OLDER STUDENTS: Use the Geological Time Chart to Time period __________________ determine which time period each animal first appeared.
Recommended publications
  • Cranial Anatomy, Taxonomic Implications
    [Palaeontology, Vol. 55, Part 4, 2012, pp. 743–773] CRANIAL ANATOMY, TAXONOMIC IMPLICATIONS AND PALAEOPATHOLOGY OF AN UPPER JURASSIC PLIOSAUR (REPTILIA: SAUROPTERYGIA) FROM WESTBURY, WILTSHIRE, UK by JUDYTH SASSOON1, LESLIE F. NOE` 2 and MICHAEL J. BENTON1* 1School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, UK; e-mails: [email protected], [email protected] 2Geociencias, departamento de Fisica, Universidad de los Andes, Bogota´ DC, Colombia; e-mail: [email protected] *Corresponding author. Typescript received 5 December 2010; accepted in revised form 6 April 2011 Abstract: Complete skulls of giant marine reptiles of the genera. The two Westbury Pliosaurus specimens share many Late Jurassic are rare, and so the discovery of the 1.8-m- features, including the form of the teeth, but marked differ- long skull of a pliosaur from the Kimmeridge Clay Forma- ences in the snout and parietal crest suggest sexual dimor- tion (Kimmeridgian) of Westbury, Wiltshire, UK, is an phism; the present specimen is probably female. The large important find. The specimen shows most of the cranial size of the animal, the extent of sutural fusion and the and mandibular anatomy, as well as a series of pathological pathologies suggest this is an ageing individual. An erosive conditions. It was previously referred to Pliosaurus brachy- arthrotic condition of the articular glenoids led to pro- spondylus, but it can be referred reliably only to the genus longed jaw misalignment, generating a suite of associated Pliosaurus, because species within the genus are currently in bone and dental pathologies.
    [Show full text]
  • First Occurrence of a Gigantic Pliosaurid Plesiosaur in The
    Bull. Soc. géol. Fr., 2003, t. 174, no 3, pp. 271-278 First occurrence of a gigantic pliosaurid plesiosaur in the late Jurassic (Kimmeridgian) of Mexico MARIE-CÉLINE BUCHY1,EBERHARD FREY2,WOLFGANG STINNESBECK1 &JOSÉ GUADALUPE LÓPEZ-OLIVA3 Key words. – Kimmeridgian, Pliosauridae, Mexico, Palaeobiogeography. Abstract. – Reinvestigation of a partial vertebral column from the Kimmeridgian La Caja Formation of Mexico, housed in the University of Linares (Mexico), and previously attributed to a dinosaur, proves to be from a very large pliosaurid plesiosaur. This specimen represents the first plesiosaur described from the Jurassic of Mexico. Its length has been esti- mated at 15 metres and, as a juvenile, is considered to be one of the largest Jurassic marine reptiles. The remains of this animal are here described. The morphology of the vertebral column is not diagnostic beyond family level. Large pliosaur vertebrae of a similar size are known from the Upper Jurassic of Europe, and are often referred to the genera Liopleurodon or Simolestes but these identifications are based only upon the size of the centra and have no taxonomic justification. A portion of rostrum with teeth was discovered together with the vertebral column but is unfortunately now lost. The Mexican pliosaur fills geographical and chronological gaps between western Tethys and South American pliosaurs, and is an additional support to the hypothesis of a Hispanic corridor linking at least temporarily the NW Euro- pean marine province with the western South American marine (Pacific) realm during the late Jurassic. Première occurrence d’un plésiosaure pliosauride géant dans le Jurassique supérieur (Kimméridgien) du Mexique Mots clés.
    [Show full text]
  • Carpenter 1999 EL PLESIOSAURIO DE VILLA DE LEYVA (BOYACÁ, COLOMBIA)
    Boletín de Geología Vol. 23, No. 38, Enero-Junio de 2001 Callawayasaurus colombiensis (Welles) Carpenter 1999 EL PLESIOSAURIO DE VILLA DE LEYVA (BOYACÁ, COLOMBIA). ¿UN NUEVO ESPÉCIMEN? Jerez Jaimes, J. H1.; Narváez Parra, E. X1. RESUMEN En los depósitos del Cretácico (Aptiano) de Villa de Leyva se han reportado dos especies de plesiosaurios, un pliosaurio Kronosaurus boyacensis Hampe 1992, y un plesiosaurio Callawayasaurus colombiensis (Welles) Carpenter, 1999 (= Alzadasaurus colombiensis Welles, 1962). Se realiza la determinación de un espécimen de elasmosaurio encontrado por los pobladores de la zona rural de Villa de Leyva en 1999 con base en material fotográfico del mismo, siendo muy probable que corresponda a la especie Callawayasaurus colombiensis (Welles) Carpenter, 1999. Palabras Claves: Cretácico, Plesiosaurios, Villa de Leyva. ABSTRACT In the deposits of the Cretaceous (Aptian) of Villa de Leyva two plesiosaurs species have been reported, a pliosaur Kronosaurus boyacensis Hampe 1992, and a plesiosaur Callawayasaurus colombiensis (Welles) Carpenter, 1999 (= Alzadasaurus colombiensis Welles, 1962). We carried out the determination of elasmosaur specimen found by the inhabitants of the rural area of Villa de Leyva in 1999, on the basis of photographic material of it. Probably it corresponds to the Callawayasaurus colombiensis specie (Welles) Carpenter, 1999. Key Words: Cretaceous, Plesiosaurs, Villa de Leyva. 1Biólogos, Calle 10A # 24-68 Bucaramanga, Santander (Colombia). Correo electrónico: [email protected] Callawayasaurus
    [Show full text]
  • Estimating the Evolutionary Rates in Mosasauroids and Plesiosaurs: Discussion of Niche Occupation in Late Cretaceous Seas
    Estimating the evolutionary rates in mosasauroids and plesiosaurs: discussion of niche occupation in Late Cretaceous seas Daniel Madzia1 and Andrea Cau2 1 Department of Evolutionary Paleobiology, Institute of Paleobiology, Polish Academy of Sciences, Warsaw, Poland 2 Independent, Parma, Italy ABSTRACT Observations of temporal overlap of niche occupation among Late Cretaceous marine amniotes suggest that the rise and diversification of mosasauroid squamates might have been influenced by competition with or disappearance of some plesiosaur taxa. We discuss that hypothesis through comparisons of the rates of morphological evolution of mosasauroids throughout their evolutionary history with those inferred for contemporary plesiosaur clades. We used expanded versions of two species- level phylogenetic datasets of both these groups, updated them with stratigraphic information, and analyzed using the Bayesian inference to estimate the rates of divergence for each clade. The oscillations in evolutionary rates of the mosasauroid and plesiosaur lineages that overlapped in time and space were then used as a baseline for discussion and comparisons of traits that can affect the shape of the niche structures of aquatic amniotes, such as tooth morphologies, body size, swimming abilities, metabolism, and reproduction. Only two groups of plesiosaurs are considered to be possible niche competitors of mosasauroids: the brachauchenine pliosaurids and the polycotylid leptocleidians. However, direct evidence for interactions between mosasauroids and plesiosaurs is scarce and limited only to large mosasauroids as the Submitted 31 July 2019 predators/scavengers and polycotylids as their prey. The first mosasauroids differed Accepted 18 March 2020 from contemporary plesiosaurs in certain aspects of all discussed traits and no evidence Published 13 April 2020 suggests that early representatives of Mosasauroidea diversified after competitions with Corresponding author plesiosaurs.
    [Show full text]
  • A Revision of the Classification of the Plesiosauria with a Synopsis of the Stratigraphical and Geographical Distribution Of
    LUNDS UNIVERSITETS ARSSKRIFT. N. F. Avd. 2. Bd 59. Nr l. KUNGL. FYSIOGRAFISKA SÅLLSKAPETS HANDLINGAR, N. F. Bd 74. Nr 1. A REVISION OF THE CLASSIFICATION OF THE PLESIOSAURIA WITH A SYNOPSIS OF THE STRATIGRAPHICAL AND GEOGRAPHICAL DISTRIBUTION OF THE GROUP BY PER OVE PERSSON LUND C. W. K. GLEER UP Read before the Royal Physiographic Society, February 13, 1963. LUND HÅKAN OHLSSONS BOKTRYCKERI l 9 6 3 l. Introduction The sub-order Plesiosauria is one of the best known of the Mesozoic Reptile groups, but, as emphasized by KuHN (1961, p. 75) and other authors, its classification is still not satisfactory, and needs a thorough revision. The present paper is an attempt at such a revision, and includes also a tabular synopsis of the stratigraphical and geo­ graphical distribution of the group. Some of the species are discussed in the text (pp. 17-22). The synopsis is completed with seven maps (figs. 2-8, pp. 10-16), a selective synonym list (pp. 41-42), and a list of rejected species (pp. 42-43). Some forms which have been erroneously referred to the Plesiosauria are also briefly mentioned ("Non-Plesiosaurians", p. 43). - The numerals in braekets after the generic and specific names in the text refer to the tabular synopsis, in which the different forms are numbered in successional order. The author has exaroined all material available from Sweden, Australia and Spitzbergen (PERSSON 1954, 1959, 1960, 1962, 1962a); the major part of the material from the British Isles, France, Belgium and Luxembourg; some of the German spec­ imens; certain specimens from New Zealand, now in the British Museum (see LYDEK­ KER 1889, pp.
    [Show full text]
  • Climate Instability and Tipping Points in the Late Devonian
    Archived version from NCDOCKS Institutional Repository – http://libres.uncg.edu/ir/asu/ Sarah K. Carmichael, Johnny A. Waters, Cameron J. Batchelor, Drew M. Coleman, Thomas J. Suttner, Erika Kido, L.M. Moore, and Leona Chadimová, (2015) Climate instability and tipping points in the Late Devonian: Detection of the Hangenberg Event in an open oceanic island arc in the Central Asian Orogenic Belt, Gondwana Research The copy of record is available from Elsevier (18 March 2015), ISSN 1342-937X, http://dx.doi.org/10.1016/j.gr.2015.02.009. Climate instability and tipping points in the Late Devonian: Detection of the Hangenberg Event in an open oceanic island arc in the Central Asian Orogenic Belt Sarah K. Carmichael a,*, Johnny A. Waters a, Cameron J. Batchelor a, Drew M. Coleman b, Thomas J. Suttner c, Erika Kido c, L. McCain Moore a, and Leona Chadimová d Article history: a Department of Geology, Appalachian State University, Boone, NC 28608, USA Received 31 October 2014 b Department of Geological Sciences, University of North Carolina - Chapel Hill, Received in revised form 6 Feb 2015 Chapel Hill, NC 27599-3315, USA Accepted 13 February 2015 Handling Editor: W.J. Xiao c Karl-Franzens-University of Graz, Institute for Earth Sciences (Geology & Paleontology), Heinrichstrasse 26, A-8010 Graz, Austria Keywords: d Institute of Geology ASCR, v.v.i., Rozvojova 269, 165 00 Prague 6, Czech Republic Devonian–Carboniferous Chemostratigraphy Central Asian Orogenic Belt * Corresponding author at: ASU Box 32067, Appalachian State University, Boone, NC 28608, USA. West Junggar Tel.: +1 828 262 8471. E-mail address: [email protected] (S.K.
    [Show full text]
  • Cretaceous–Paleogene Extinction Event (End Cretaceous, K-T Extinction, Or K-Pg Extinction): 66 MYA At
    Cretaceous–Paleogene extinction event (End Cretaceous, K-T extinction, or K-Pg extinction): 66 MYA at • About 17% of all families, 50% of all genera and 75% of all species became extinct. • In the seas it reduced the percentage of sessile animals to about 33%. • All non-avian dinosaurs became extinct during that time. • Iridium anomaly in sediments may indicate comet or asteroid induced extinctions Triassic–Jurassic extinction event (End Triassic): 200 Ma at the Triassic- Jurassic transition. • About 23% of all families, 48% of all genera (20% of marine families and 55% of marine genera) and 70-75% of all species went extinct. • Most non-dinosaurian archosaurs, most therapsids, and most of the large amphibians were eliminated • Dinosaurs had with little terrestrial competition in the Jurassic that followed. • Non-dinosaurian archosaurs continued to dominate aquatic environments • Theories on cause: 1.) Gradual climate change, perhaps with ocean acidification has been implicated, but not proven. 2.) Asteroid impact has been postulated but no site or evidence has been found. 3.) Massive volcanics, flood basalts and continental margin volcanoes might have damaged the atmosphere and warmed the planet. Permian–Triassic extinction event (End Permian): 251 Ma at the Permian-Triassic transition. Known as “The Great Dying” • Earth's largest extinction killed 57% of all families, 83% of all genera and 90% to 96% of all species (53% of marine families, 84% of marine genera, about 96% of all marine species and an estimated 70% of land species, • The evidence of plants is less clear, but new taxa became dominant after the extinction.
    [Show full text]
  • 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’’.
    [Show full text]
  • A Large Rhomaleosaurid Pliosaur from the Upper Lias of Rutland Richard Forrest
    A large Rhomaleosaurid Pliosaur from the Upper Lias of Rutland Richard Forrest Abstract: The fragmentary remains of a very large rhomaleosaurid pliosaur were retrieved during building works at Barnsdale Hall, Rutland. The limited material prevents clear identification at specific level, though on the basis of similarities of ratios of dimensions it shows closer affinity to Rhomaleosaurus arcuatus and R.victor than to R.cramptoni. Although scaling up from such fragmentary material is unreliable, the estimated length of this animal at 7.5 to 8 metres makes it possibly the largest Rhomaleosaurid pliosaur described to date. The fossil material broken end the shaft is oval in section, 148 mm wide and 96 mm deep. The head is 153 mm broad and The bones were excavated in 1988 by Mr. Roy 160 mm deep. Orientation can be determined by Draycott during construction of a retaining wall at rugosities from ridges for muscle attachment on the Barnsdale Hall, east of Rutland Water, in the county posterior side and the ventral surface. A deep hole in of the same name. An outer whorl of the ammonite the posterior muscle attachment presumably marks Hildoceras bifrons was found in association with the where a ligament was connected to the bone. There bones. It can therefore be placed with confidence in is slight taphonomic crushing around the trochanter. the bifrons Zone of the Upper Lias (Lower Jurassic, The surface is encrusted in places with a pyritised Toarcian, Whitbian). It is probable that much more deposit, which shows traces of tracks left by extensive remains of the animal were present at the scavengers post-mortem.
    [Show full text]
  • Evaluating the Frasnian-Famennian Mass Extinction: Comparing Brachiopod Faunas
    Evaluating the Frasnian-Famennian mass extinction: Comparing brachiopod faunas PAUL COPPER Copper, P. 1998. Evaluating the Frasnian-Famennian mass extinction: Comparing bra- chiopod faunas.- Acta Palaeontologica Polonica 43,2,137-154. The Frasnian-Famennian (F-F) mass extinctions saw the global loss of all genera belonging to the tropically confined order Atrypida (and Pentamerida): though Famen- nian forms have been reported in the literafure, none can be confirmed. Losses were more severe during the Givetian (including the extinction of the suborder Davidsoniidina, and the reduction of the suborder Lissatrypidina to a single genus),but ońgination rates in the remaining suborder surviving into the Frasnian kept the group alive, though much reduced in biodiversity from the late Earb and Middle Devonian. In the terminal phases of the late Palmatolepis rhenana and P linguifurmis zones at the end of the Frasnian, during which the last few Atrypidae dechned, no new genera originated, and thus the Atrypida were extĘated. There is no evidence for an abrupt termination of all lineages at the F-F boundary, nor that the Atrypida were abundant at this time, since all groups were in decline and impoverished. Atypida were well established in dysaerobic, muddy substrate, reef lagoonal and off-reef deeper water settings in the late Givetian and Frasnian, alongside a range of brachiopod orders which sailed through the F-F boundary: tropical shelf anoxia or hypońa seems implausible as a cause for aĘpid extinction. Glacial-interglacial climate cycles recorded in South Ameńca for the Late Devonian, and their synchronous global cooling effect in low latitudes, as well as loss of the reef habitat and shelf area reduction, remain as the most likely combined scenarios for the mass extinction events.
    [Show full text]
  • How Plesiosaurs Swam: New Insights Into Their Underwater Flight Using “Ava”, a Virtual Pliosaur
    Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 9 October 2019 doi:10.20944/preprints201910.0094.v1 How Plesiosaurs Swam: New Insights into Their Underwater Flight Using “Ava”, a Virtual Pliosaur Max Hawthorne1,*, Mark A. S. McMenamin 2, Paul de la Salle3 1Far From The Tree Press, LLC, 4657 York Rd., #952, Buckingham, PA, 18912, United States 2Department of Geology and Geography, Mount Holyoke College, South Hadley, Massachusetts, United States 3Swindon, England *Correspondence: [email protected]; Tel.: 267-337-7545 Abstract Analysis of plesiosaur swim dynamics by means Further study attempted to justify the use of all four flippers of a digital 3D armature (wireframe “skeleton”) of a simultaneously via the use of paddle-generated vortices, pliosauromorph (“Ava”) demonstrates that: 1, plesiosaurs which require specific timing to achieve optimal additional used all four flippers for primary propulsion; 2, plesiosaurs thrust. These attempts have largely relied on anatomical utilized all four flippers simultaneously; 3, respective pairs studies of strata-compressed plesiosaur skeletons, and/or of flippers of Plesiosauridae, front and rear, traveled through preconceived notions as pertains to the paddles’ inherent distinctive, separate planes of motion, and; 4, the ability to ranges of motion [8, 10-12]. What has not been considered utilize all four paddles simultaneously allowed these largely are the opposing angles of the pectoral and pelvic girdles, predatory marine reptiles to achieve a significant increase in which strongly indicate varied-yet-complementing relations acceleration and speed, which, in turn, contributed to their between the front and rear sets of paddles, both in repose and sustained dominance during the Mesozoic.
    [Show full text]
  • Petrified Forest U.S
    National Park Service Petrified Forest U.S. Department of the Interior Petrified Forest National Park Petrified Forest, Arizona Triassic Dinosaurs and Other Animals Fossils are clues to the past, allowing researchers to reconstruct ancient environments. During the Late Triassic, the climate was very different from that of today. Located near the equator, this region was humid and tropical, the landscape dominated by a huge river system. Giant reptiles and amphibians, early dinosaurs, fish, and many invertebrates lived among the dense vegetation and in the winding waterways. New fossils come to light as paleontologists continue to study the Triassic treasure trove of Petrified Forest National Park. Invertebrates Scattered throughout the sedimentary species forming vast colonies in the layers of the Chinle Formation are fossils muddy beds of the ancient lakes and of many types of invertebrates. Trace rivers. Antediplodon thomasi is one of the fossils include insect nests, termite clam fossils found in the park. galleries, and beetle borings in the petrified logs. Thin slabs of shale have preserved Horseshoe crabs more delicate animals such as shrimp, Horseshoe crabs have been identified by crayfish, and insects, including the wing of their fossilized tracks (Kouphichnium a cockroach! arizonae), originally left in the soft sediments at the bottom of fresh water Clams lakes and streams. These invertebrates Various freshwater bivalves have been probably ate worms, soft mollusks, plants, found in the Chinle Formation, some and dead fish. Freshwater Fish The freshwater streams and rivers of the (pictured). This large lobe-finned fish Triassic landscape were home to numerous could reach up to 5 feet (1.5 m) long and species of fish.
    [Show full text]