?^Te.^I.^ OYSTER CULTURE-STATUS and PROSPECTS
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Field Identification Guide to the Living Marine Resources In
Guide to Families 29 BIVALVES Coastal species are of great interest to fisheries and have potential for exportation for eating purposes. Bivalves are caught mainly by divers and are also fished for pearls. Their flesh is of excellent quality. Since oysters remain alive out of the water for over 12 hours, they may exported to far destinations when still alive. Moreover, some species are collected for their nacreous shell and ability to develop pearls. The shell can be used in the mother of pearl industry. The “Guide to Families’’ andTECHNICAL ‘‘Guide to Species’’ TERMS include 5AND families MEASUREMENTS and 10 species, respectively. ligament Dorsal margin umbo posterior adductor cardinal tooth muscle scar lateral tooth Posterior Anterior margin margin shell height anterior adductor muscle scar pallial sinus pallial shell length line left valve (interior) Ventral margin ligament left valve right valve lunule umbo Adductor muscle: Byssus: Chomata: Muscle connecting the two valves of a shell, tending to draw them together. Hinge: Clump of horny threads spun by the foot, by which a Bivalve can anchor to a hard substrate. Ligament: Small denticles and corresponding pits located on the inner margin of the valves (Ostreidae and Gryphaeidae). Mantle: Top interlocking margin of the valves, often with shelly projections (teeth) and corresponding recesses (sockets). Muscle scar: Horny, elastic structure joining the two valves dorsally. Pallial line: Fleshy sheet surrounding vital organs and composed of two lobes, one lining and secreting each valve. Umbo: Impression marking the place of attachment of a muscle inside the shell. A line near the internal margin of valve, marking the site of attachment of the mantle edge. -
Systematics in Palaeontology
Systematics in palaeontology THOMAS NEVILLE GEORGE PRESIDENT'S ANNIVERSARY ADDRESS 1969 CONTENTS Fossils in neontological categories I98 (A) Purpose and method x98 (B) Linnaean taxa . x99 (e) The biospecies . 202 (D) Morphology and evolution 205 The systematics of the lineage 205 (A) Bioserial change 205 (B) The palaeodeme in phyletic series 209 (e) Palaeodemes as facies-controlled phena 2xi Phyletic series . 2~6 (A) Rates of bioserial change 2~6 (B) Character mosaics 218 (c) Differential characters 222 Phylogenetics and systematics 224 (A) Clade and grade 224 (a) Phylogenes and cladogenes 228 (e) Phylogenetic reconstruction 23 I (D) Species and genus 235 (~) The taxonomic hierarchy 238 5 Adansonian methods 240 6 References 243 SUMMARY A 'natural' taxonomic system, inherent in evolutionary change, pulses of biased selection organisms that themselves demonstrate their pressure in expanded and restricted palaeo- 'affinity', is to be recognized perhaps only in demes, and permutations of character-expres- the biospecies. The concept of the biospecies as sion in the evolutionary plexus impose a need a comprehensive taxon is, however, only for a palaeontologically-orientated systematics notional amongst the vast majority of living under which (in evolutionary descent) could organisms, and it is not directly applicable to be subsumed the taxa of the neontological fossils. 'Natural' systems of Linnaean kind rest moment. on assumptions made a priori and are imposed Environmentally controlled morphs, bio- by the systematist. The graded time-sequence facies variants, migrating variation fields, and of the lineage and the clade introduces factors typological segregants are sources of ambiguity into a systematics that cannot well be accommo- in a distinction between phenetic and genetic dated under pre-Darwinian assumptions or be fossil grades. -
Danise Et Al 2020 Gondwana Research.Docx.Pdf
University of Plymouth PEARL https://pearl.plymouth.ac.uk Faculty of Science and Engineering School of Geography, Earth and Environmental Sciences 2020-06 Isotopic evidence for partial geochemical decoupling between a Jurassic epicontinental sea and the open ocean Danise, S http://hdl.handle.net/10026.1/15995 10.1016/j.gr.2019.12.011 Gondwana Research Elsevier BV All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. Please cite as: Danise, S., Price, G.D., Alberti, M., Holland S.M. 2020 Isotopic evidence for partial geochemical decoupling between a Jurassic epicontinental sea and the open ocean. Gondwana Research, 82, 97–107. Isotopic evidence for partial geochemical decoupling between a Jurassic epicontinental sea and the open ocean Silvia Danise a,b,⁎, Gregory D. Price a, Matthias Alberti c, Steven M. Holland d a School of Geography, Earth and Environmental Sciences, University of Plymouth, Drake Circus, Plymouth, Devon PL4 8AA, UK b Dipartimento di Sicenze della Terra, Università degli Studi di Firenze, via La Pira 4, 50121 Firenze, Italy c Institut für Geowissenschaften, Christian-Albrechts-Universität zu Kiel, Ludewig-Meyn-Straße 10, 24118 Kiel, Germany d Department of Geology, University of Georgia, Athens, GA 30602-2501, USA a b s t r a c t Article history: Received 21 October 2019 Received in revised form 20 December 2019 Accepted 20 December 2019 Available online 30 January 2020 Handling Editor: A. -
TREATISE ONLINE Number 48
TREATISE ONLINE Number 48 Part N, Revised, Volume 1, Chapter 31: Illustrated Glossary of the Bivalvia Joseph G. Carter, Peter J. Harries, Nikolaus Malchus, André F. Sartori, Laurie C. Anderson, Rüdiger Bieler, Arthur E. Bogan, Eugene V. Coan, John C. W. Cope, Simon M. Cragg, José R. García-March, Jørgen Hylleberg, Patricia Kelley, Karl Kleemann, Jiří Kříž, Christopher McRoberts, Paula M. Mikkelsen, John Pojeta, Jr., Peter W. Skelton, Ilya Tëmkin, Thomas Yancey, and Alexandra Zieritz 2012 Lawrence, Kansas, USA ISSN 2153-4012 (online) paleo.ku.edu/treatiseonline PART N, REVISED, VOLUME 1, CHAPTER 31: ILLUSTRATED GLOSSARY OF THE BIVALVIA JOSEPH G. CARTER,1 PETER J. HARRIES,2 NIKOLAUS MALCHUS,3 ANDRÉ F. SARTORI,4 LAURIE C. ANDERSON,5 RÜDIGER BIELER,6 ARTHUR E. BOGAN,7 EUGENE V. COAN,8 JOHN C. W. COPE,9 SIMON M. CRAgg,10 JOSÉ R. GARCÍA-MARCH,11 JØRGEN HYLLEBERG,12 PATRICIA KELLEY,13 KARL KLEEMAnn,14 JIřÍ KřÍž,15 CHRISTOPHER MCROBERTS,16 PAULA M. MIKKELSEN,17 JOHN POJETA, JR.,18 PETER W. SKELTON,19 ILYA TËMKIN,20 THOMAS YAncEY,21 and ALEXANDRA ZIERITZ22 [1University of North Carolina, Chapel Hill, USA, [email protected]; 2University of South Florida, Tampa, USA, [email protected], [email protected]; 3Institut Català de Paleontologia (ICP), Catalunya, Spain, [email protected], [email protected]; 4Field Museum of Natural History, Chicago, USA, [email protected]; 5South Dakota School of Mines and Technology, Rapid City, [email protected]; 6Field Museum of Natural History, Chicago, USA, [email protected]; 7North -
Upper Jurassic Mollusks from Eastern Oregon and Western Idaho
Upper Jurassic Mollusks from Eastern Oregon and Western Idaho GEOLOGICAL SURVEY PROFESSIONAL PAPER 483-D Upper Jurassic Mollusks from Eastern Oregon and Western Idaho By RALPH W. IMLAY CONTRIBUTIONS TO PALEONTOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 483-D Faunal evidence for the presence of Upper Jurassic sedimentary rocks in eastern Oregon and westernmost Idaho UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract.__________________________________________ Dl Ages and correlations Continued Introduction.______________________________________ 1 Trowbridge Formation of Lupher, 1941, in east- Biologic analysis..._________________________________ 2 central Oregon.__________---_-_-__-_-____---_ D9 Stratigraphic summary._____________________________ 2 Lonesome Formation of Lupher, 1941, in east-central Northeastern Oregon and adjoining Idaho. ________ 2 Oregon..________________-_--_____--_--_---__ 9 Mineral area, western Idaho.____________________ 2 Comparisons with other faunas.______________________ 10 East-central Oregon_____________________________ 4 Alaska and western British Columbia-____________ 10 Conditions of deposition.____________________________ 6 Calif ornia. ... _ __-_________--____-___-__---___-_ 10 Ages and correlations______________________________ 6 Unnamed beds in northeastern Oregon and adjoining Western interior of North America._______________ 10 Idaho_______________________________________ Geographic distribution________-_-_____---_---_-.__ 11 Unnamed beds near Mineral, Idaho.______________ Systematic descriptions..._--_--__-__________________ 13 Snowshoe Formation of Lupher, 1941, in east-central Literature cited_____-__-_____---------_-_--_--__-___ 17 Oregon._____________________________________ Index_.______________--____---------_-__---_-_-___ 21 ILLUSTRATIONS [Plates 1-4 follow index] PLATE 1. -
Chapter I Taxonomy
THE AMERICAN OYSTER CRASSOSTREA VIRGINICA GMELIN By PAUL S. GALTSOFF, Fishery Biologist BUREAU OF COMMERCIAL FISHERIES CHAPTER I TAXONOMY Page This broad characterization included a number Taxonomic characters _ 4 SheIL _ 4 of genera such as scallops, pen shells (Pinnidae), Anatomy _ 4 Sex and spawnlng _ limas (Limidae) and other mollusks which ob 4 Habitat _ 5 viously are not oysters. In the 10th edition of Larvll! shell (Prodlssoconch) _ 6 "Systema Naturae," Linnaeus (1758) wrote: The genera of living oysters _ 6 Genus 08trea _ 6 "Ostreae non orones, imprimis Pectines, ad Genus Cra8808trea _ 7 Genus Pycnodonte _ cardinem interne fulcis transversis numerosis 7 Bibliography _ 14 parallelis in utraque testa oppositis gaudentiquae probe distinguendae ab Areis polypleptoginglymis, The family Ostreidae consists of a large number cujus dentes numerosi alternatim intrant alterius of edibleand nonedible oysters. Their distribution sinus." Le., not all are oysters, in particular the is confined to a broad belt of coastal waters within scallops, which have many parallel ribs running the latitudes 64° N. and 44° S. With few excep crosswise inward toward the hinge on each shell tions oysters thrive in shallow water, their vertical on opposite sides; these should properly be dis distribution extending from a level approximately tinguished from Area polyleptoginglymis whose halfway between high and low tide levels to a many teeth alternately enter between the teeth depth of about 100 feet. Commercially exploited of the other side. oyster beds are rarely found below a depth of 40 In the same publication the European flat feet. oyster, Ostrea edulis, is described as follows: The· name "Ostrea" was given by Linnaeus "Vulgo Ostrea dictae edulis. -
An Assessment of Latest Cretaceous Pycnodonte Vesicularis (Lamarck, 1806) Shells As Records for Palaeoseasonality: a Multi-Proxy Investigation
Clim. Past, 14, 725–749, 2018 https://doi.org/10.5194/cp-14-725-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. An assessment of latest Cretaceous Pycnodonte vesicularis (Lamarck, 1806) shells as records for palaeoseasonality: a multi-proxy investigation Niels J. de Winter1,*, Johan Vellekoop1,2,*, Robin Vorsselmans2, Asefeh Golreihan2, Jeroen Soete2, Sierra V. Petersen3, Kyle W. Meyer3, Silvio Casadio4, Robert P. Speijer2, and Philippe Claeys1 1Analytical, Environmental and Geo-Chemistry (AMGC), Vrije Universiteit Brussel (VUB), Brussels, Belgium 2Department of Earth and Environmental Science, KU Leuven, Heverlee, Belgium 3Earth and Environmental Sciences Department, University of Michigan, Ann Arbor, Michigan, USA 4Escuela de Geología, Paleontología y Enseñanza de las Ciencias, Universidad Nacional de Río Negro, CONICET, General Roca, Argentina *These authors contributed equally to this work. Correspondence: Niels J. de Winter ([email protected]) Received: 26 September 2017 – Discussion started: 11 October 2017 Revised: 4 April 2018 – Accepted: 21 May 2018 – Published: 8 June 2018 Abstract. In order to assess the potential of the honey- tiate between well-preserved and diagenetically altered por- comb oyster Pycnodonte vesicularis for the reconstruction tions of the shells and provides an improved methodology for of palaeoseasonality, several specimens recovered from late reconstructing palaeoenvironmental conditions in deep time. Maastrichtian strata in the Neuquén Basin (Argentina) were While establishing a chronology for these shells was compli- subject to a multi-proxy investigation, involving scanning cated by growth cessations and diagenesis, cyclicity in trace techniques and trace element and isotopic analysis. Com- elements and stable isotopes allowed for a tentative interpre- bined CT scanning and light microscopy reveals two cal- tation of the seasonal cycle in late Maastrichtian palaeoen- cite microstructures in P. -
Farming Bivalve Molluscs: Methods for Study and Development by D
Advances in World Aquaculture, Volume 1 Managing Editor, Paul A. Sandifer Farming Bivalve Molluscs: Methods for Study and Development by D. B. Quayle Department of Fisheries and Oceans Fisheries Research Branch Pacific Biological Station Nanaimo, British Columbia V9R 5K6 Canada and G. F. Newkirk Department of Biology Dalhousie University Halifax, Nova Scotia B3H 471 Canada Published by THE WORLD AQUACULTURE SOCIETY in association with THE INTERNATIONAL DEVELOPMENT RESEARCH CENTRE The World Aquaculture Society 16 East Fraternity Lane Louisiana State University Baton Rouge, LA 70803 Copyright 1989 by INTERNATIONAL DEVELOPMENT RESEARCH CENTRE, Canada All rights reserved. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form by any means, electronic, mechanical, photocopying, recording, or otherwise, without the prior written permission of the publisher, The World Aquaculture Society, 16 E. Fraternity Lane, Louisiana State University, Baton Rouge, LA 70803 and the International Development Research Centre, 250 Albert St., P.O. Box 8500, Ottawa, Canada K1G 3H9. ; t" ary of Congress Catalog Number: 89-40570 tI"624529-0-4 t t lq 7 i ACKNOWLEDGMENTS The following figures are reproduced with permission: Figures 1- 10, 12, 13, 17,20,22,23, 32, 35, 37, 42, 45, 48, 50 - 54, 62, 64, 72, 75, 86, and 87 from the Fisheries Board of Canada; Figures 11 and 21 from the United States Government Printing Office; Figure 15 from the Buckland Founda- tion; Figures 18, 19,24 - 28, 33, 34, 38, 41, 56, and 65 from the International Development Research Centre; Figures 29 and 30 from the Journal of Shellfish Research; and Figure 43 from Fritz (1982). -
Zoologische Mededelingen Uitgegeven Door Het
ZOOLOGISCHE MEDEDELINGEN UITGEGEVEN DOOR HET RIJKSMUSEUM VAN NATUURLIJKE HISTORIE TE LEIDEN (MINISTERIE VAN CULTUUR, RECREATIE EN MAATSCHAPPELIJK WERK) Deel 53 no. 13 25 oktober 1978 THE MARINE MOLLUSCAN ASSEMBLAGES OF PORT SUDAN, RED SEA by M. MASTALLER Ruhr-Universität Bochum, Lehrstuhl für Spez. Zoologie Bochum, West-Germany With one text-figure and one table ABSTRACT This study summarizes field observations and collections of the molluscan fauna of the coastal and offshore reefs in the area of Port Sudan, Central Red Sea. In spite of the fact that some families of this group were described from several areas of the Red Sea, there exists only little information on the entire faunal composition of this region. 282 species of Amphineura, Gastropoda, and Bivalvia, collected and studied in nine localities are listed according to their habitats. Moreover, descriptions of the prominent members of typical molluscan assemblages are given for 13 habitats and microhabitats which differ in their morphological structures and in their hydrographic and physiographic conditions. Emphasis is placed on further studies on the trophic interactions within certain habitats. INTRODUCTION Although there is a considerable number of taxonomie literature on some molluscan families in the Indo-West-Padfic (Abbott, i960; Burgess, 1970; Cernohorsky, 1967; Habe, 1964; Kira, 1962; Powell, 1964; Rosewater, 1965), there is comparatively scarce information for the Red Sea. After the exten• sive surveys and descriptions of Issel, 1869, Hall & Standen, 1907, Jickeli, 1874, Shopland, 1902, and Sturany, 1901, 1903, in more recent times only a few studies were published on the entire faunal composition of molluscs in this region. Most of these publications deal with certain families, sometimes they also give information about their zoogeographical distribution in the Red Sea: Thus the cypraeids seem to yield the best information on their occurrence throughout the region (Foin, 1972; Mienis, 1971b; O'Malley, 1971; Schilder, 1965). -
Mainstreaming Biodiversity for Sustainable Development
Mainstreaming Biodiversity for Sustainable Development Dinesan Cheruvat Preetha Nilayangode Oommen V Oommen KERALA STATE BIODIVERSITY BOARD Mainstreaming Biodiversity for Sustainable Development Dinesan Cheruvat Preetha Nilayangode Oommen V Oommen KERALA STATE BIODIVERSITY BOARD MAINSTREAMING BIODIVERSITY FOR SUSTAINABLE DEVELOPMENT Editors Dinesan Cheruvat, Preetha Nilayangode, Oommen V Oommen Editorial Assistant Jithika. M Design & Layout - Praveen K. P ©Kerala State Biodiversity Board-2017 All rights reserved. No part of this book may be reproduced, stored in a retrieval system, transmitted in any form or by any means-graphic, electronic, mechanical or otherwise, without the prior written permission of the publisher. Published by - Dr. Dinesan Cheruvat Member Secretary Kerala State Biodiversity Board ISBN No. 978-81-934231-1-0 Citation Dinesan Cheruvat, Preetha Nilayangode, Oommen V Oommen Mainstreaming Biodiversity for Sustainable Development 2017 Kerala State Biodiversity Board, Thiruvananthapuram 500 Pages MAINSTREAMING BIODIVERSITY FOR SUSTAINABLE DEVELOPMENT IntroduCtion The Hague Ministerial Declaration from the Conference of the Parties (COP 6) to the Convention on Biological Diversity, 2002 recognized first the need to mainstream the conservation and sustainable use of biological resources across all sectors of the national economy, the society and the policy-making framework. The concept of mainstreaming was subsequently included in article 6(b) of the Convention on Biological Diversity, which called on the Parties to the -
ASFIS ISSCAAP Fish List February 2007 Sorted on Scientific Name
ASFIS ISSCAAP Fish List Sorted on Scientific Name February 2007 Scientific name English Name French name Spanish Name Code Abalistes stellaris (Bloch & Schneider 1801) Starry triggerfish AJS Abbottina rivularis (Basilewsky 1855) Chinese false gudgeon ABB Ablabys binotatus (Peters 1855) Redskinfish ABW Ablennes hians (Valenciennes 1846) Flat needlefish Orphie plate Agujón sable BAF Aborichthys elongatus Hora 1921 ABE Abralia andamanika Goodrich 1898 BLK Abralia veranyi (Rüppell 1844) Verany's enope squid Encornet de Verany Enoploluria de Verany BLJ Abraliopsis pfefferi (Verany 1837) Pfeffer's enope squid Encornet de Pfeffer Enoploluria de Pfeffer BJF Abramis brama (Linnaeus 1758) Freshwater bream Brème d'eau douce Brema común FBM Abramis spp Freshwater breams nei Brèmes d'eau douce nca Bremas nep FBR Abramites eques (Steindachner 1878) ABQ Abudefduf luridus (Cuvier 1830) Canary damsel AUU Abudefduf saxatilis (Linnaeus 1758) Sergeant-major ABU Abyssobrotula galatheae Nielsen 1977 OAG Abyssocottus elochini Taliev 1955 AEZ Abythites lepidogenys (Smith & Radcliffe 1913) AHD Acanella spp Branched bamboo coral KQL Acanthacaris caeca (A. Milne Edwards 1881) Atlantic deep-sea lobster Langoustine arganelle Cigala de fondo NTK Acanthacaris tenuimana Bate 1888 Prickly deep-sea lobster Langoustine spinuleuse Cigala raspa NHI Acanthalburnus microlepis (De Filippi 1861) Blackbrow bleak AHL Acanthaphritis barbata (Okamura & Kishida 1963) NHT Acantharchus pomotis (Baird 1855) Mud sunfish AKP Acanthaxius caespitosa (Squires 1979) Deepwater mud lobster Langouste -
Saccostrea Cucullata (Von Born)
Larval Development of the Rock Oyster Saccostrea cucullata (von Born) P. SUKUMAR' were acclimatised in sea water of salinity 30%. for two M. MOHAN JOSEPH days. Equal quantities of sperm and egg suspensions in College of Fisheries, sterile seawater prepared by stripping were mixed. The University of Agircultural Sciences, fertilised eggs were washed free of attached sperms and Mangalore - 575 002, distributed in three sterile glass trays containing sterile Karnataka. seawater for further development. The D-veligers were transfered to and reared in round bottom glass vessels (20 I capacity) with mild aeration. Dead larvae settled at the ·Present address: centre of the culture vessels were siphoned off and Fisheries College, removed daily. Filtered and autoclaved seawater was used Tamil Nadu Agricultural University, Tuticorin - 628 008, Tamil Nadu. for embryonic and early larval development upto first week beyond which filtered , boiled and cooled sea water was used. Salinity was maintained at about 30%0 and seawater SUKUMAR, P.. and JOSEPH, M.M., 1988. Larval development of the rock changed once in 24 hours during the first week and once in oyster Saccostrea cucuJ/ata (von Born). In: M. Mohan Joseph (Ed.) 48 hours subsequently. Trimethoprim (2 mgll ) and The First Indian Fisheries Forum, Proceedings. Asian Fisheries Society, Indian Branch, Mangalore. pp. 255 _ 258. sulphamethoxazole ( 10 mgll ) were added during every change of water. A mixed diet of fsochrysis galbana and Tetraselmis gracilis was fed (at 37.5 to 50 mill of culture Abstract water) at a ratio (by voL) of 2:1 during first four days and The development of artificially fertilised eggs of the rock oyster, 1:1 thereafter.