Tightly Shut: Flexible Valve Margins and Microstructural Asymmetry In
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Greening Phenomenon in Bivalve by Marennine Produced from Haslea Ostrearia and Its Consequences on Bivalve's Integrated Resp
Greening phenomenon in bivalve by marennine produced from Haslea ostrearia and its consequences on bivalve’s integrated response Fiddy Semba Prasetiya To cite this version: Fiddy Semba Prasetiya. Greening phenomenon in bivalve by marennine produced from Haslea os- trearia and its consequences on bivalve’s integrated response. Invertebrate Zoology. Université du Maine, 2015. English. NNT : 2015LEMA1017. tel-01279527 HAL Id: tel-01279527 https://tel.archives-ouvertes.fr/tel-01279527 Submitted on 26 Feb 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Fiddy SEMBA PRASETIYA Mémoire présenté en vue de l’obtention du grade de Docteur de l’Université du Maine sous le label de L’Université Nantes Angers Le Mans École doctorale : Végétale Environnement Nutrition Agro-alimentaire Mer (VENAM) Discipline : BIOLOGIÉ DES ORGANISMES Unité de recherche : MER MOLÉCULE ET SANTÉ (MMS) – EA n°2160, Université du Maine, UFR Sciences et Techniques, Avenue Olivier Messiaen 72085 Le Mans Cedex 9 Soutenue le 27 Novembre 2015 Greening phenomenon in bivalve by marennine -
Marine Bivalve Molluscs
Marine Bivalve Molluscs Marine Bivalve Molluscs Second Edition Elizabeth Gosling This edition first published 2015 © 2015 by John Wiley & Sons, Ltd First edition published 2003 © Fishing News Books, a division of Blackwell Publishing Registered Office John Wiley & Sons, Ltd, The Atrium, Southern Gate, Chichester, West Sussex, PO19 8SQ, UK Editorial Offices 9600 Garsington Road, Oxford, OX4 2DQ, UK The Atrium, Southern Gate, Chichester, West Sussex, PO19 8SQ, UK 111 River Street, Hoboken, NJ 07030‐5774, USA For details of our global editorial offices, for customer services and for information about how to apply for permission to reuse the copyright material in this book please see our website at www.wiley.com/wiley‐blackwell. The right of the author to be identified as the author of this work has been asserted in accordance with the UK Copyright, Designs and Patents Act 1988. All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, except as permitted by the UK Copyright, Designs and Patents Act 1988, without the prior permission of the publisher. Designations used by companies to distinguish their products are often claimed as trademarks. All brand names and product names used in this book are trade names, service marks, trademarks or registered trademarks of their respective owners. The publisher is not associated with any product or vendor mentioned in this book. Limit of Liability/Disclaimer of Warranty: While the publisher and author(s) have used their best efforts in preparing this book, they make no representations or warranties with respect to the accuracy or completeness of the contents of this book and specifically disclaim any implied warranties of merchantability or fitness for a particular purpose. -
Paleontology and Sedimentology of Middle Eocene Rocks in Lago Argentino Area, Santa Cruz Province, Argentina
AMEGHINIANA (Rev. Asoc. Paleontol. Argent.) - 46 (1): 27-47. Buenos Aires, 30-04-2009 ISSN 0002-7014 Paleontology and sedimentology of Middle Eocene rocks in Lago Argentino area, Santa Cruz Province, Argentina Silvio CASADÍO1,2, Miguel GRIFFIN1,2, Sergio MARENSSI3,2, Laura NET4, Ana PARRAS1,2, Martín RODRÍGUEZ RAISING5,2 and Sergio SANTILLANA3 Abstract. Sedimentological and paleontological study of the Man Aike Formation at the Estancia 25 de Mayo, SW of Santa Cruz Province, Argentina, represents the evolution of an incised valley from fluvial to marine environment during the late middle Eocene. At the base of the unit there is an unconformity that corresponds to fluvial channels which cut down into the underlying Maastrichtian sandstones of the Calafate Formation. The fauna of invertebrates (mostly molluscs) illustrated herein was collected from shell beds interpreted as tidal ravinement surfaces. The fauna includes terebratulid brachiopods, bivalves of the families Malletiidae, Mytilidae, Pinnidae, Ostreidae, Pectinidae, Carditidae, Crassatellidae, Lahillidae, Mactridae, Veneridae, and Hiatellidae, and gastropods of the families Trochidae and Calyptraeidae, and a member of Archaeogastropoda of uncertain affinities. The similarities of this fauna with that recorded in the Upper Member of the Río Turbio Formation, together with 87Sr/86Sr ages, sug- gest a late Middle Eocene age for the Man Aike Formation. Resumen. PALEONTOLOGÍA Y SEDIMENTOLOGÍA DE LAS ROCAS DEL EOCENO MEDIO EXPUESTAS EN EL ÁREA DE LAGO ARGENTINO, PROVINCIA DE SANTA CRUZ, ARGENTINA. Los estudios sedimentológicos y paleontológicos real- izados en rocas asignadas a la Formación Man Aike, expuestas en la estancia 25 de Mayo, al sur de Calafate, provincia de Santa Cruz, Argentina, sugieren que esta unidad representa la evolución de un valle inciso desde ambientes fluviales a marinos durante el Eoceno medio tardío. -
Larvae of Bivalve Mollusks of the Sevastopol Region of the Black Sea
W&M ScholarWorks Reports 1966 Larvae of bivalve mollusks of the Sevastopol region of the Black Sea K. A. Zakhvatkina Follow this and additional works at: https://scholarworks.wm.edu/reports Part of the Aquaculture and Fisheries Commons, Marine Biology Commons, and the Zoology Commons Recommended Citation Zakhvatkina, K. A. (1966) Larvae of bivalve mollusks of the Sevastopol region of the Black Sea. Translation series (Virginia Institute of Marine Science) ; no. 15. Virginia Institute of Marine Science, William & Mary. https://scholarworks.wm.edu/reports/39 This Report is brought to you for free and open access by W&M ScholarWorks. It has been accepted for inclusion in Reports by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. VIRGINIA INSTITUTE OF MARINE SCIENCE GLOUCESTER POINT, VIRGDHA .. LARVAE OF BIVALVE MOLLUSKS OF THE SEVASTOPOL REGION OF THE BLACK SEA TRANSlATION SLRIES NO· 15 1966 Virginia Institute of Marine Science Gloucester Point, Virginia URVhE OF BIVALVE hOLLUSKS OF THE SEVii.STOPOL REGION OF THE BLACK SEA By K. A· Zakhvatkina Original title: Lichinki dvustvorchatykh molliuskov sevastopol'skogo raiona Chernogo Moria From: Akademiia Nauk SSSR, Trudy Sevastopol1 skoi Biologicheskoi Stantsii, Tom XI, p• 108-152, 1959 Translated by Evelyn c. wells Edited by Paul Chanley TRANSLATION SERIES NO· 15 w. J. Hargis Director April 1966 Akad • Nauk SSSR, Trudy Sevastopol' skoi Biologicheskoi St.antsii Tom XI, P• 108-152, 1959 LJ.dtvii.E OF BIV;.,LVE HOLLUSKS. OF TH1 SLVJL.TOf'OL REGION OF THE BLACK SEA By K· A· Zakhvatkina Heretofore, the systematic relationships as well as the biology p•l08 and ecology of bivalve larvce have been poorly known• The work of A· Borisiak (1905), on the larv~e of bivalve mollusks, is of only historical interest since only four of the 20 forfus described were deter~mined to genus• Data on the reproduction of several species of bivalve mollusks, especially on spawning seasons, are given in the work of z. -
Clam Dissection Guideline
Clam Dissection Guideline BACKGROUND: Clams are bivalves, meaning that they have shells consisting of two halves, or valves. The valves are joined at the top, and the adductor muscles on each side hold the shell closed. If the adductor muscles are relaxed, the shell is pulled open by ligaments located on each side of the umbo. The clam's foot is used to dig down into the sand, and a pair of long incurrent and excurrent siphons that extrude from the clam's mantle out the side of the shell reach up to the water above (only the exit points for the siphons are shown). Clams are filter feeders. Water and food particles are drawn in through one siphon to the gills where tiny, hair-like cilia move the water, and the food is caught in mucus on the gills. From there, the food-mucus mixture is transported along a groove to the palps (mouth flaps) which push it into the clam's mouth. The second siphon carries away the water. The gills also draw oxygen from the water flow. The mantle, a thin membrane surrounding the body of the clam, secretes the shell. The oldest part of the clam shell is the umbo, and it is from the hinge area that the clam extends as it grows. I. Purpose: The purpose of this lab is to identify the internal and external structures of a mollusk by dissecting a clam. II. Materials: 2 pairs of safety goggles 1 paper towel 2 pairs of gloves 1 pair of scissors 1 preserved clam 2 pairs of forceps 1 dissecting tray 2 probes III. -
Geological Survey
DEPABTMENT OF THE INTEKIOR BULLETIN OF THE UNITED STATES GEOLOGICAL SURVEY N~o. 151 WASHINGTON GOVERNMENT PRINTING OFFICE 1898 UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIEECTOR THE LOWER CRETACEOUS GRYPMAS OF THK TEX.AS REGION ROBERT THOMAS HILL THOMAS WAYLA'ND VAUGHAN WASHINGTON GOVERNMENT FEINTING OFFICE 18.98 THE LOWER CRETACEOUS GRYPHJ1AS OF THE TEXAS REGION. BY I EOBEET THOMAS HILL and THOMAS WAYLAND VAUGHAN. CONTENTS. Page. Letter of transmittal....._..........._....._ ............................ 11 Introduction ...---._._....__................._....._.__............._...._ 13 The fossil oysters of the Texas region.._._.._.___._-..-._._......-..--.... 23 Classification of the Ostreidae. .. ...-...---..-.......-.....-.-............ 24 Historical statement of the discovery in the Texas region of the forms referred to Gryphsea pitcher! Morton ................................ 33 Gryphaea corrugata Say._______._._..__..__...__.,_._.________...____.._ 33 Gryphsea pitcheri Morton............................................... 34 Roemer's Gryphsea pitcheri............................................ 35 Marcou's Gryphsea pitcheri............................................ 35 Blake's Gryphaea pitcheri............................................. 36 Schiel's Gryphsea pitcheri...........................,.:................ 36 Hall's Gryphsea pitcheri (= G. dilatata var. tucumcarii Marcou) ...... 36 Heilprin's Gryphaea pitcheri.....'..................................... 37 Gryphaea pitcheri var. hilli Cragin................................... -
324170141.Pdf
Aquaculture Reports 17 (2020) 100347 Contents lists available at ScienceDirect Aquaculture Reports journal homepage: www.elsevier.com/locate/aqrep Economic feasibility of small-scale mabé pearl production in Tonga using T the winged pearl oyster, Pteria penguin William Johnstona,b,*, Sophie E. Gordonb,e, Max Wingfieldb,e, Tu’ikolongahau Halafihic, Damian Hined, Paul C. Southgateb,e a Queensland Department of Agriculture and Fisheries, 47 Mayers Road, Nambour, Queensland, 4560, Australia b School of Science & Engineering, University of the Sunshine Coast, 90 Sippy Downs Drive, Sippy Downs, Queensland, 4556, Australia c Science Division, Ministry of Fisheries, Nuku’alofa, Tongatapu, Tonga d University of Queensland Business School, The University of Queensland, 39 Blair Drive, St Lucia, Brisbane, Queensland, 4067, Australia e Australian Centre for Pacific Islands Research and School of Science and Engineering, University of the Sunshine Coast, 90 Sippy Downs Drive, Sippy Downs,Queensland, 4556, Australia ARTICLE INFO ABSTRACT Keywords: Mabé pearl culture is an increasingly important rural livelihood in south Pacific countries as it offers a low-cost, Mabé pearl low-tech alternative to round pearl culture. Mabé pearl production can be achieved by local people with ap- half-pearl propriate training, and the products offer further livelihood opportunities through value-adding and local pro- Pteria penguin duction of jewellery and handicraft items. The Kingdom of Tonga is unique among south Pacific pearl producing pearl economics countries in focusing primarily on mabé pearl, not round pearl, culture using the winged pearl oyster, Pteria pearl farm profitability penguin. The Tongan mabé pearl sector has developed rapidly over recent years and is sustained by routine hatchery production of spat and recently improved pearl culture methods. -
Early Ontogeny of Jurassic Bakevelliids and Their Bearing on Bivalve Evolution
Early ontogeny of Jurassic bakevelliids and their bearing on bivalve evolution NIKOLAUS MALCHUS Malchus, N. 2004. Early ontogeny of Jurassic bakevelliids and their bearing on bivalve evolution. Acta Palaeontologica Polonica 49 (1): 85–110. Larval and earliest postlarval shells of Jurassic Bakevelliidae are described for the first time and some complementary data are given concerning larval shells of oysters and pinnids. Two new larval shell characters, a posterodorsal outlet and shell septum are described. The outlet is homologous to the posterodorsal notch of oysters and posterodorsal ridge of arcoids. It probably reflects the presence of the soft anatomical character post−anal tuft, which, among Pteriomorphia, was only known from oysters. A shell septum was so far only known from Cassianellidae, Lithiotidae, and the bakevelliid Kobayashites. A review of early ontogenetic shell characters strongly suggests a basal dichotomy within the Pterio− morphia separating taxa with opisthogyrate larval shells, such as most (or all?) Praecardioida, Pinnoida, Pterioida (Bakevelliidae, Cassianellidae, all living Pterioidea), and Ostreoida from all other groups. The Pinnidae appear to be closely related to the Pterioida, and the Bakevelliidae belong to the stem line of the Cassianellidae, Lithiotidae, Pterioidea, and Ostreoidea. The latter two superfamilies comprise a well constrained clade. These interpretations are con− sistent with recent phylogenetic hypotheses based on palaeontological and genetic (18S and 28S mtDNA) data. A more detailed phylogeny is hampered by the fact that many larval shell characters are rather ancient plesiomorphies. Key words: Bivalvia, Pteriomorphia, Bakevelliidae, larval shell, ontogeny, phylogeny. Nikolaus Malchus [[email protected]], Departamento de Geologia/Unitat Paleontologia, Universitat Autòno− ma Barcelona, 08193 Bellaterra (Cerdanyola del Vallès), Spain. -
Upper Cretaceous Deposits in the Northwest of Saratov Region, Part 2: Problems of Chronostratigraphy and Regional Geological History A
ISSN 0869-5938, Stratigraphy and Geological Correlation, 2008, Vol. 16, No. 3, pp. 267–294. © Pleiades Publishing, Ltd., 2008. Original Russian Text © A.G. Olfer’ev, V.N. Beniamovski, V.S. Vishnevskaya, A.V. Ivanov, L.F. Kopaevich, M.N. Ovechkina, E.M. Pervushov, V.B. Sel’tser, E.M. Tesakova, V.M. Kharitonov, E.A. Shcherbinina, 2008, published in Stratigrafiya. Geologicheskaya Korrelyatsiya, 2008, Vol. 16, No. 3, pp. 47–74. Upper Cretaceous Deposits in the Northwest of Saratov Region, Part 2: Problems of Chronostratigraphy and Regional Geological History A. G. Olfer’eva, V. N. Beniamovskib, V. S. Vishnevskayab, A. V. Ivanovc, L. F. Kopaevichd, M. N. Ovechkinaa, E. M. Pervushovc, V. B. Sel’tserc, E. M. Tesakovad, V. M. Kharitonovc, and E. A. Shcherbininab a Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117997 Russia b Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017 Russia c Saratov State University, Astrakhanskaya ul., 83, Saratov, 410012 Russia d Moscow State University, Vorob’evy Gory, Moscow, 119991 Russia Received November 7, 2006; in final form, March 21, 2007 Abstract—Problems of geochronological correlation are considered for the formations established in the study region with due account for data on the Mezino-Lapshinovka, Lokh and Teplovka sections studied earlier on the northwest of the Saratov region. New paleontological data are used to define more precisely stratigraphic ranges of some stratigraphic subdivisions, to consider correlation between standard and local zones established for different groups of fossils, and to suggest how the Upper Cretaceous regional scale of the East European platform can be improved. -
Olympia Oyster (Ostrea Lurida)
COSEWIC Assessment and Status Report on the Olympia Oyster Ostrea lurida in Canada SPECIAL CONCERN 2011 COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC. 2011. COSEWIC assessment and status report on the Olympia Oyster Ostrea lurida in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. xi + 56 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Previous report(s): COSEWIC. 2000. COSEWIC assessment and status report on the Olympia Oyster Ostrea conchaphila in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vii + 30 pp. (www.sararegistry.gc.ca/status/status_e.cfm) Gillespie, G.E. 2000. COSEWIC status report on the Olympia Oyster Ostrea conchaphila in Canada in COSEWIC assessment and update status report on the Olympia Oyster Ostrea conchaphila in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-30 pp. Production note: COSEWIC acknowledges Graham E. Gillespie for writing the provisional status report on the Olympia Oyster, Ostrea lurida, prepared under contract with Environment Canada and Fisheries and Oceans Canada. The contractor’s involvement with the writing of the status report ended with the acceptance of the provisional report. Any modifications to the status report during the subsequent preparation of the 6-month interim and 2-month interim status reports were overseen by Robert Forsyth and Dr. Gerald Mackie, COSEWIC Molluscs Specialist Subcommittee Co-Chair. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: 819-953-3215 Fax: 819-994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Ếvaluation et Rapport de situation du COSEPAC sur l’huître plate du Pacifique (Ostrea lurida) au Canada. -
Spatial Variability in Recruitment of an Infaunal Bivalve
Spatial Variability in Recruitment of an Infaunal Bivalve: Experimental Effects of Predator Exclusion on the Softshell Clam (Mya arenaria L.) along Three Tidal Estuaries in Southern Maine, USA Author(s): Brian F. Beal, Chad R. Coffin, Sara F. Randall, Clint A. Goodenow Jr., Kyle E. Pepperman, Bennett W. Ellis, Cody B. Jourdet and George C. Protopopescu Source: Journal of Shellfish Research, 37(1):1-27. Published By: National Shellfisheries Association https://doi.org/10.2983/035.037.0101 URL: http://www.bioone.org/doi/full/10.2983/035.037.0101 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. Journal of Shellfish Research, Vol. 37, No. 1, 1–27, 2018. SPATIAL VARIABILITY IN RECRUITMENT OF AN INFAUNAL BIVALVE: EXPERIMENTAL EFFECTS OF PREDATOR EXCLUSION ON THE SOFTSHELL CLAM (MYA ARENARIA L.) ALONG THREE TIDAL ESTUARIES IN SOUTHERN MAINE, USA 1,2 3 2 3 BRIAN F. -
Phylogeographic Study of the Dwarf Oyster, Ostreola Stentina
Marine Biology Archimer, archive institutionnelle de l’Ifremer Volume 150, Number 1, October 2006 http://www.ifremer.fr/docelec/ http://dx.doi.org/10.1007/s00227-006-0333-1 ©2006 Springer Science+Business Media The original publication is available at http://www.springerlink.com ailable on the publisher Web site Phylogeographic study of the dwarf oyster, Ostreola stentina, from Morocco, Portugal and Tunisia: evidence of a geographic disjunction with the closely related taxa, Ostrea aupouria and Ostreola equestris Sylvie Lapègue1, Inès Ben Salah2, Frederico M. Batista3, 4, Serge Heurtebise1, Lassad Neifar2 and Pierre Boudry1 (1) Laboratoire de Génétique et Pathologie, IFREMER, 17390 La Tremblade, France blisher-authenticated version is av (2) Faculté des Sciences de Sfax, Laboratoire d’écobiologie Animale, BP 802, 3038 Sfax, Tunisia (3) Instituto Nacional de Investigação Agrária e das Pescas (INIAP/IPIMAR), CRIPSul, Av. 5 de Outubro, 8700-305 Olhao, Portugal (4) Instituto de Ciências Biomédicas Abel Salazar (ICBAS), Universidade do Porto, Largo Prof. Abel Salazar, 2, 4099-003 Porto, Portugal Corresponding author : [email protected] Abstract: Despite the economic importance of oysters due to the high aquaculture production of several species, the current knowledge of oyster phylogeny and systematics is still fragmentary. In Europe, Ostrea edulis, the European flat oyster, and Ostreola stentina, the Provence oyster or dwarf oyster, are both present along the European and African, Atlantic and Mediterranean, coasts. In order to document the relationship not only between O. stentina and O. edulis, but also with the other Ostrea and Ostreola species, we performed a sequence analysis of the 16S mitochondrial fragment (16S rDNA: the large subunit rRNA-coding gene) and the COI fragment (COI: cytochrome oxidase subunit I).