Early Evolution of the Vertebrate Eye—Fossil Evidence
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PIR/PER) for the State Route 86 / Avenue 50 New Interchange Project, City of Coachella, Riverside County, California E-FIS 0801-000144 (EA 08-0C970
Combined Paleontological Identification Report / Paleontological Evaluation Report (PIR/PER) for the State Route 86 / Avenue 50 New Interchange Project, City of Coachella, Riverside County, California E-FIS 0801-000144 (EA 08-0C970) Submitted to: Kurt Heidelberg, Branch Chief Environmental Studies D California Department of Transportation, District 8 464 West 4th Street, 6th Floor, MS 825 San Bernardino, California 92401-1400 March 2018 EXECUTIVE SUMMARY The City of Coachella (City), in cooperation with the California Department of Transportation (Caltrans) District 8 and Coachella Valley Association of Governments (CVAG), proposes the construction of a new interchange at State Route 86 (SR-86) and Avenue 50 in the City of Coachella, Riverside County, California. The SR-86 /Avenue 50 New Interchange Project (Project) consists of converting a portion of SR-86 from an existing expressway to a freeway with a new overcrossing structure and access ramps. In addition, the proposed Project includes the realignment and widening of Avenue 50 and the realignment of portions of Tyler Street on both the east and west sides of SR-86. Finally, the Project would construct a new bridge over the Coachella Valley Stormwater Channel (CVSC) to replace the existing low water crossing. At the request of TranSystems, Applied EarthWorks, Inc. (Æ) performed a paleontological resource assessment in support of the proposed Project. The study consisted of a search of museum collections records maintained by the Natural History Museum of Los Angeles County, a comprehensive literature and geologic map review, a field reconnaissance survey, and preparation of this combined Paleontological Identification Report (PIR) / Paleontological Evaluation Report (PER). -
Class Myxini Order Myxiniformes Family Myxinidae (Hagfishes)
Class Myxini Order Myxiniformes Family Myxinidae (hagfishes) • Lacks jaws • Mouth not disk-like • barbels present • Unpaired fins as continuous fin-fold • Branchial skeleton not well developed • Eyes degenerate • 70-200 slime glands • Isoosmotic, simple kidneys, stenohayline, marine • Four rudimentary hearts • No true stomach • Unpaired gonads Class Petromyzontida Order Petromyzontiformes Family Petromyzontidae Class Myxini Order Myxiniformes Family Myxinidae (hagfishes) (Northern Lampreys) • Knot-tying behavior • 8 genera, 34 species • Scavengers • Dorsal fins continuous in • Rely heavily on cutaneous respiration adults • Global, deep sea distribution • Oral disc • Commercial interest – eelskin • 7 pairs of gill openings • Single nostril • Pineal body opening • No bone • No scales • No paired fins • No jaws 1 Class Petromyzontida Order Petromyzontiformes Family Petromyzontidae Class Petromyzontida Order Petromyzontiformes Family Petromyzontidae (Northern Lampreys) (Northern Lampreys) • Anadramous and freshwater • Ammocoete • Parasitic forms: – Non-parasitic forms often • Non-parasitic: freshwater – Parasitic forms often anadramous • Life history Class Conodonta, Conodonts Class Pteraspidiomorphi • Extinct, late Triassic • Extinct • First “teeth” • One of the earliest known vertebrates • No jaws • Dermal skeleton • Cranium and teeth • No jaws • Small, thought to be of paedomorphic origin • Little known, an extinct monophyletic lineage. 2 Class Anapsid Class Cephalaspidomorphi, osteostraci • Extinct, Silurian period • Extinct, early Silurian -
Biostratigraphic Precision of the Cruziana Rugosa Group: a Study from the Ordovician Succession of Southern and Central Bolivia
Geol. Mag. 144 (2), 2007, pp. 289–303. c 2007 Cambridge University Press 289 doi:10.1017/S0016756807003093 First published online 9 February 2007 Printed in the United Kingdom Biostratigraphic precision of the Cruziana rugosa group: a study from the Ordovician succession of southern and central Bolivia SVEN O. EGENHOFF∗, BERND WEBER†, OLIVER LEHNERT‡ &JORG¨ MALETZ§ ∗Colorado State University, Department of Geosciences, 322 Natural Resources Building, Fort Collins, CO 80523-1482, USA †Freie Universitat¨ Berlin, Institut fur¨ Geologische Wissenschaften, Fachrichtung Geologie, Malteserstrasse 74-100, D-12249 Berlin, Germany ‡University of Erlangen, Institute of Geology and Mineralogie, Schlossgarten 5, D-91054 Erlangen, Germany §Department of Geology, State University of New York at Buffalo, 772 Natural Sciences and Mathematics Complex, Buffalo, New York 14260-3050, USA (Received 10 October 2005; revised version received 1 May 2006; accepted 22 May 2006) Abstract – Cruziana ichnospecies have been repeatedly reported to have biostratigraphic significance. This study presents a re-evaluation of the arthropod ichnotaxa of the Cruziana rugosa Group from bio- and/or lithostratigraphically well-defined Lower to Upper Ordovician siliciclastic sections of southern and central Bolivia. With the exception of Cruziana rouaulti, the ichnofaunas contain all the members of the Cruziana rugosa Group throughout the Ordovician (Arenig to Caradoc) successions in Bolivia. The Bolivian material therefore indicates that these arthropod ichnofossil assemblages are suitable for recognizing Ordovician strata in Bolivia. These findings cast doubt on their use as reliable indicators for a global intra-Ordovician (Arenig to Caradoc) biozonation of Peri-Gondwanan sedimentary successions. Keywords: Cruziana, biostratigraphy, Bolivia, Ordovician. 1. Introduction to the present study. -
Timeline of the Evolutionary History of Life
Timeline of the evolutionary history of life This timeline of the evolutionary history of life represents the current scientific theory Life timeline Ice Ages outlining the major events during the 0 — Primates Quater nary Flowers ←Earliest apes development of life on planet Earth. In P Birds h Mammals – Plants Dinosaurs biology, evolution is any change across Karo o a n ← Andean Tetrapoda successive generations in the heritable -50 0 — e Arthropods Molluscs r ←Cambrian explosion characteristics of biological populations. o ← Cryoge nian Ediacara biota – z ← Evolutionary processes give rise to diversity o Earliest animals ←Earliest plants at every level of biological organization, i Multicellular -1000 — c from kingdoms to species, and individual life ←Sexual reproduction organisms and molecules, such as DNA and – P proteins. The similarities between all present r -1500 — o day organisms indicate the presence of a t – e common ancestor from which all known r Eukaryotes o species, living and extinct, have diverged -2000 — z o through the process of evolution. More than i Huron ian – c 99 percent of all species, amounting to over ←Oxygen crisis [1] five billion species, that ever lived on -2500 — ←Atmospheric oxygen Earth are estimated to be extinct.[2][3] Estimates on the number of Earth's current – Photosynthesis Pong ola species range from 10 million to 14 -3000 — A million,[4] of which about 1.2 million have r c been documented and over 86 percent have – h [5] e not yet been described. However, a May a -3500 — n ←Earliest oxygen 2016 -
PALEONTOLOGICAL TECHNICAL REPORT: 6Th AVENUE and WADSWORTH BOULEVARD INTERCHANGE PHASE II ENVIRONMENTAL ASSESSMENT, CITY of LAKEWOOD, JEFFERSON COUNTY, COLORADO
PALEONTOLOGICAL TECHNICAL REPORT: 6th AVENUE AND WADSWORTH BOULEVARD INTERCHANGE PHASE II ENVIRONMENTAL ASSESSMENT, CITY OF LAKEWOOD, JEFFERSON COUNTY, COLORADO Prepared for: TEC Inc. 1746 Cole Boulevard, Suite 265 Golden, CO 80401 Prepared by: Paul C. Murphey, Ph.D. and David Daitch M.S. Rocky Mountain Paleontology 4614 Lonespur Court Oceanside, CA 92056 303-514-1095; 760-758-4019 www.rockymountainpaleontology.com Prepared under State of Colorado Paleontological Permit 2007-33 January, 2007 TABLE OF CONTENTS 1.0 SUMMARY............................................................................................................................. 3 2.0 INTRODUCTION ................................................................................................................... 4 2.1 DEFINITION AND SIGNIFICANCE OF PALEONTOLOGICAL RESOURCES........... 4 3.0 METHODS .............................................................................................................................. 6 4.0. LAWS, ORDINANCES, REGULATIONS AND STANDARDS......................................... 7 4.1. Federal................................................................................................................................. 7 4.2. State..................................................................................................................................... 8 4.3. County................................................................................................................................. 8 4.4. City..................................................................................................................................... -
Categorical Versus Geometric Morphometric Approaches To
[Palaeontology, 2020, pp. 1–16] CATEGORICAL VERSUS GEOMETRIC MORPHOMETRIC APPROACHES TO CHARACTERIZING THE EVOLUTION OF MORPHOLOGICAL DISPARITY IN OSTEOSTRACI (VERTEBRATA, STEM GNATHOSTOMATA) by HUMBERTO G. FERRON 1,2* , JENNY M. GREENWOOD1, BRADLEY DELINE3,CARLOSMARTINEZ-PEREZ 1,2,HECTOR BOTELLA2, ROBERT S. SANSOM4,MARCELLORUTA5 and PHILIP C. J. DONOGHUE1,* 1School of Earth Sciences, University of Bristol, Life Sciences Building, Tyndall Avenue, Bristol, BS8 1TQ, UK; [email protected], [email protected], [email protected] 2Institut Cavanilles de Biodiversitat i Biologia Evolutiva, Universitat de Valencia, C/ Catedratic Jose Beltran Martınez 2, 46980, Paterna, Valencia, Spain; [email protected], [email protected] 3Department of Geosciences, University of West Georgia, Carrollton, GA 30118, USA; [email protected] 4School of Earth & Environmental Sciences, University of Manchester, Manchester, M13 9PT, UK; [email protected] 5School of Life Sciences, University of Lincoln, Riseholme Hall, Lincoln, LN2 2LG, UK; [email protected] *Corresponding authors Typescript received 2 October 2019; accepted in revised form 27 February 2020 Abstract: Morphological variation (disparity) is almost aspects of morphology. Phylomorphospaces reveal conver- invariably characterized by two non-mutually exclusive gence towards a generalized ‘horseshoe’-shaped cranial mor- approaches: (1) quantitatively, through geometric morpho- phology and two strong trends involving major groups of metrics; -
Phylum Arthropod Silvia Rondon, and Mary Corp, OSU Extension Entomologist and Agronomist, Respectively Hermiston Research and Extension Center, Hermiston, Oregon
Phylum Arthropod Silvia Rondon, and Mary Corp, OSU Extension Entomologist and Agronomist, respectively Hermiston Research and Extension Center, Hermiston, Oregon Member of the Phyllum Arthropoda can be found in the seas, in fresh water, on land, or even flying freely; a group with amazing differences of structure, and so abundant that all the other animals taken together are less than 1/6 as many as the arthropods. Well-known members of this group are the Kingdom lobsters, crayfish and crabs; scorpions, spiders, mites, ticks, Phylum Phylum Phylum Class the centipedes and millipedes; and last, but not least, the Order most abundant of all, the insects. Family Genus The Phylum Arthropods consist of the following Species classes: arachnids, chilopods, diplopods, crustaceans and hexapods (insects). All arthropods possess: • Exoskeleton. A hard protective covering around the outside of the body (divided by sutures into plates called sclerites). An insect's exoskeleton (integument) serves as a protective covering over the body, but also as a surface for muscle attachment, a water-tight barrier against desiccation, and a sensory interface with the environment. It is a multi-layered structure with four functional regions: epicuticle (top layer), procuticle, epidermis, and basement membrane. • Segmented body • Jointed limbs and jointed mouthparts that allow extensive specialization • Bilateral symmetry, whereby a central line can divide the body Insect molting or removing its into two identical halves, left and right exoesqueleton • Ventral nerve -
Micropaleontological Association from the Middle Miocene Badenian Gypsum Deposits of Paratethys
geosciences Article A New Preparation Method of Microfauna from Gypsum: Micropaleontological Association from the Middle Miocene Badenian Gypsum Deposits of Paratethys Hans-Peter Bojar 1, Claudia Antoniade 2, Victor Barbu 3 and Ana-Voica Bojar 1,4,5,* 1 Studienzentrum Naturkunde—Mineralogie, Universalmuseum Joanneum, Weinzöttlstraße 16, 8045 Graz, Austria; [email protected] 2 OMV Petrom, Research and Design Institute of Technology Petrom Câmpina, Culturii Bldv 29, Câmpina, 15600 Prahova, Romania; [email protected] 3 OMV Petrom, Coralilor str. 22, 013329 Bucharest, Romania; [email protected] 4 Department Geographie und Geologie, Geologie, University of Salzburg, Hellbrunnerstraße 34, 5020 Salzburg, Austria 5 Faculty of Physics, Department of Structure of Matter, Earth and Atmospheric Physics and Astrophysics, University of Bucharest, Bulevardul Regina Elisabeta 4-12, 030018 Bucharest, Romania * Correspondence: [email protected] Received: 23 March 2020; Accepted: 26 April 2020; Published: 28 April 2020 Abstract: Evaporitic gypsum deposits represent an important paleoenvironmental record of the Miocene Badenian of the Carpathian Mountains belt. In this study, we developed a nontoxic method to concentrate calcareous microfossils from gypsum (CaSO 2H O), by treating the sulfate with 4· 2 ammonium acetate. We applied the newly developed method to gypsum collected from the Evaporitic Formation outcropping northward of Slănic-Prahova in the Eastern Carpathians. For the first time for this formation, we describe a calcareous microfossil assemblage characterized by the presence of planktonic foraminifera as well as cysts and fragments of calcareous algae. Keywords: chemical preparation method; gypsum deposits; calcareous microfossil assemblage; Miocene; Eastern Carpathians 1. Introduction In the Earth’s history, sulfate rich marine waters are known for late Precambrian (Vendian), Pennsylvanian-Triassic, Miocene to Quaternary [1]. -
001-012 Primeras Páginas
PUBLICACIONES DEL INSTITUTO GEOLÓGICO Y MINERO DE ESPAÑA Serie: CUADERNOS DEL MUSEO GEOMINERO. Nº 9 ADVANCES IN TRILOBITE RESEARCH ADVANCES IN TRILOBITE RESEARCH IN ADVANCES ADVANCES IN TRILOBITE RESEARCH IN ADVANCES planeta tierra Editors: I. Rábano, R. Gozalo and Ciencias de la Tierra para la Sociedad D. García-Bellido 9 788478 407590 MINISTERIO MINISTERIO DE CIENCIA DE CIENCIA E INNOVACIÓN E INNOVACIÓN ADVANCES IN TRILOBITE RESEARCH Editors: I. Rábano, R. Gozalo and D. García-Bellido Instituto Geológico y Minero de España Madrid, 2008 Serie: CUADERNOS DEL MUSEO GEOMINERO, Nº 9 INTERNATIONAL TRILOBITE CONFERENCE (4. 2008. Toledo) Advances in trilobite research: Fourth International Trilobite Conference, Toledo, June,16-24, 2008 / I. Rábano, R. Gozalo and D. García-Bellido, eds.- Madrid: Instituto Geológico y Minero de España, 2008. 448 pgs; ils; 24 cm .- (Cuadernos del Museo Geominero; 9) ISBN 978-84-7840-759-0 1. Fauna trilobites. 2. Congreso. I. Instituto Geológico y Minero de España, ed. II. Rábano,I., ed. III Gozalo, R., ed. IV. García-Bellido, D., ed. 562 All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage and retrieval system now known or to be invented, without permission in writing from the publisher. References to this volume: It is suggested that either of the following alternatives should be used for future bibliographic references to the whole or part of this volume: Rábano, I., Gozalo, R. and García-Bellido, D. (eds.) 2008. Advances in trilobite research. Cuadernos del Museo Geominero, 9. -
Chordates (Phylum Chordata)
A short story Leathem Mehaffey, III, Fall 201993 The First Chordates (Phylum Chordata) • Chordates (our phylum) first appeared in the Cambrian, 525MYA. 94 Invertebrates, Chordates and Vertebrates • Invertebrates are all animals not chordates • Generally invertebrates, if they have hearts, have dorsal hearts; if they have a nervous system it is usually ventral. • All vertebrates are chordates, but not all chordates are vertebrates. • Chordates: • Dorsal notochord • Dorsal nerve chord • Ventral heart • Post-anal tail • Vertebrates: Amphioxus: archetypal chordate • Dorsal spinal column (articulated) and skeleton 95 Origin of the Chordates 96 Haikouichthys Myllokunmingia Note the rounded extension to Possibly the oldest the head bearing sensory vertebrate: showed gill organs bars and primitive vertebral elements Early and primitive agnathan vertebrates of the Early Cambrian (530MYA) Pikaia Note: these organisms were less Primitive chordate, than an inch long. similar to Amphioxus 97 The Cambrian/Ordovician Extinction • Somewhere around 488 million years ago something happened to cause a change in the fauna of the earth, heralding the beginning of the Ordovician Period. • Rather than one catastrophe, the late-Cambrian extinction seems to be a series of smaller extinction events. • Historically the change in fauna (mostly trilobites as the index species) was thought to be due to excessive warmth and low oxygen. • But some current findings point to an oxygen spike due perhaps to continental drift into the tropics, driving rapid speciation and consequent replacement of old with new organisms. 98 Welcome to the Ordovician YOU ARE HERE 99 The Ordovician Sea, 488 million years 100 ago The Ordovician Period lasted almost 45 million years, from 489 to 444 MYA. -
THE CLASSIFICATION and EVOLUTION of the HETEROSTRACI Since 1858, When Huxley Demonstrated That in the Histological Struc
ACTA PALAEONT OLOGICA POLONICA Vol. VII 1 9 6 2 N os. 1-2 L. BEVERLY TARLO THE CLASSIFICATION AND EVOLUTION OF THE HETEROSTRACI Abstract. - An outline classification is given of the Hetero straci, with diagnoses . of th e following orders and suborders: Astraspidiformes, Eriptychiiformes, Cya thaspidiformes (Cyathaspidida, Poraspidida, Ctenaspidida), Psammosteiformes (Tes seraspidida, Psarnmosteida) , Traquairaspidiformes, Pteraspidiformes (Pte ras pidida, Doryaspidida), Cardipeltiformes and Amphiaspidiformes (Amphiaspidida, Hiber naspidida, Eglonaspidida). It is show n that the various orders fall into four m ain evolutionary lineages ~ cyathaspid, psammosteid, pteraspid and amphiaspid, and these are traced from primitive te ssellated forms. A tentative phylogeny is pro posed and alternatives are discussed. INTRODUCTION Since 1858, when Huxley demonstrated that in the histological struc ture of their dermal bone Cephalaspis and Pteraspis were quite different from one another, it has been recognized that there were two distinct groups of ostracoderms for which Lankester (1868-70) proposed the names Osteostraci and Heterostraci respectively. Although these groups are generally considered to be related to on e another, Lankester belie ved that "the Heterostraci are at present associated with the Osteostraci because they are found in the same beds, because they have, like Cepha laspis, a large head shield, and because there is nothing else with which to associate them". In 1889, Cop e united these two groups in the Ostracodermi which, together with the modern cyclostomes, he placed in the Class Agnatha, and although this proposal was at first opposed by Traquair (1899) and Woodward (1891b), subsequent work has shown that it was correct as both the Osteostraci and the Heterostraci were agnathous. -
ORDOVICIAN FISH from the ARABIAN PENINSULA by IVAN J
[Palaeontology, Vol. 52, Part 2, 2009, pp. 337–342] ORDOVICIAN FISH FROM THE ARABIAN PENINSULA by IVAN J. SANSOM*, C. GILES MILLER , ALAN HEWARDà,–, NEIL S. DAVIES*,**, GRAHAM A. BOOTHà, RICHARD A. FORTEY and FLORENTIN PARIS§ *Earth Sciences, University of Birmingham, Birmingham B15 2TT, UK; e-mail: [email protected] Department of Palaeontology, The Natural History Museum, London SW7 5BD, UK; e-mails: [email protected] and [email protected] àPetroleum Development Oman, Muscat, Oman; e-mail: [email protected] §Ge´osciences, Universite´ de Rennes, 35042 Rennes, France; e-mail: fl[email protected] –Present address: Petrogas E&P, Muscat, Oman; e-mail: [email protected] **Present address: Earth Sciences, Dalhousie University, Halifax, Nova Scotia B3H 3J5, Canada; e-mail: [email protected] Typescript received 25 February 2008; accepted in revised form 19 May 2008 Abstract: Over the past three decades Ordovician pteras- morphs from the Arabian margin of Gondwana. These are pidomorphs (armoured jawless fish) have been recorded among the oldest arandaspids known, and greatly extend from the fringes of the Gondwana palaeocontinent, in par- the palaeogeographical distribution of the clade around the ticular Australia and South America. These occurrences are periGondwanan margin. Their occurrence within a very dominated by arandaspid agnathans, the oldest known narrow, nearshore ecological niche suggests that similar group of vertebrates with extensive biomineralisation of Middle Ordovician palaeoenvironmental settings should be the dermoskeleton. Here we describe specimens of arandas- targeted for further sampling. pid agnathans, referable to the genus Sacabambaspis Gagnier, Blieck and Rodrigo, from the Ordovician of Key words: Ordovician, pteraspidomorphs, Gondwana pal- Oman, which represent the earliest record of pteraspido- aeocontinent, Sacabambaspis, Oman.