Molluscan Studies
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Impacts of Ocean Acidification on Marine Shelled Molluscs
Mar Biol DOI 10.1007/s00227-013-2219-3 ORIGINAL PAPER Impacts of ocean acidification on marine shelled molluscs Fre´de´ric Gazeau • Laura M. Parker • Steeve Comeau • Jean-Pierre Gattuso • Wayne A. O’Connor • Sophie Martin • Hans-Otto Po¨rtner • Pauline M. Ross Received: 18 January 2013 / Accepted: 15 March 2013 Ó Springer-Verlag Berlin Heidelberg 2013 Abstract Over the next century, elevated quantities of ecosystem services including habitat structure for benthic atmospheric CO2 are expected to penetrate into the oceans, organisms, water purification and a food source for other causing a reduction in pH (-0.3/-0.4 pH unit in the organisms. The effects of ocean acidification on the growth surface ocean) and in the concentration of carbonate ions and shell production by juvenile and adult shelled molluscs (so-called ocean acidification). Of growing concern are the are variable among species and even within the same impacts that this will have on marine and estuarine species, precluding the drawing of a general picture. This organisms and ecosystems. Marine shelled molluscs, which is, however, not the case for pteropods, with all species colonized a large latitudinal gradient and can be found tested so far, being negatively impacted by ocean acidifi- from intertidal to deep-sea habitats, are economically cation. The blood of shelled molluscs may exhibit lower and ecologically important species providing essential pH with consequences for several physiological processes (e.g. respiration, excretion, etc.) and, in some cases, increased mortality in the long term. While fertilization Communicated by S. Dupont. may remain unaffected by elevated pCO2, embryonic and Fre´de´ric Gazeau and Laura M. -
Bankia Setacea Class: Bivalvia, Heterodonta, Euheterodonta
Phylum: Mollusca Bankia setacea Class: Bivalvia, Heterodonta, Euheterodonta Order: Imparidentia, Myida The northwest or feathery shipworm Family: Pholadoidea, Teredinidae, Bankiinae Taxonomy: The original binomen for Bankia the presence of long siphons. Members of setacea was Xylotrya setacea, described by the family Teredinidae are modified for and Tryon in 1863 (Turner 1966). William Leach distiguished by a wood-boring mode of life described several molluscan genera, includ- (Sipe et al. 2000), pallets at the siphon tips ing Xylotrya, but how his descriptions were (see Plate 394C, Coan and Valentich-Scott interpreted varied. Although Menke be- 2007) and distinct anterior shell indentation. lieved Xylotrya to be a member of the Phola- They are commonly called shipworms (though didae, Gray understood it as a member of they are not worms at all!) and bore into many the Terdinidae and synonyimized it with the wooden structures. The common name ship- genus Bankia, a genus designated by the worm is based on their vermiform morphology latter author in 1842. Most authors refer to and a shell that only covers the anterior body Bankia setacea (e.g. Kozloff 1993; Sipe et (Ricketts and Calvin 1952; see images in al. 2000; Coan and Valentich-Scott 2007; Turner 1966). Betcher et al. 2012; Borges et al. 2012; Da- Body: Bizarrely modified bivalve with re- vidson and de Rivera 2012), although one duced, sub-globular body. For internal anato- recent paper sites Xylotrya setacea (Siddall my, see Fig. 1, Canadian…; Fig. 1 Betcher et et al. 2009). Two additional known syno- al. 2012. nyms exist currently, including Bankia Color: osumiensis, B. -
Mollusca, Pholadidae, Xylophagainae)
Turner: Xylopholas altenai 97 n. gen. n. sp. A new genus and species of deep water wood-boring bivalve (Mollusca, Pholadidae, Xylophagainae) by Ruth+D. Turner Museum ofComparativeZoology, Harvard University, Cambridge,Mass., U.S.A. The Xylophagainae are marine wood-boring bivalves which are confined than 150 largely to depths greater meters. They are not found the intertidal the sublittoral in zone, occur in only in higher latitudes, and are the sole wood-borers in depths over 200 meters. The greatest known depth for the invasion oftest wood by Teredini- dae is 200 meters (Tipper, 1968). The known depth range for the Xylophagainae extends from two meters below low tide in Millport, Scotland, to 7290 meters in the Banda Trench, off Ceram. Only occasionally are they found in drift wood, and this is usually after storms, the water logged wood having been lifted offthe bottom and carried ashore by strong waves. The discovery of the new genus and species described here is the result of a world-wide study of the Xylophagainae, a subfamily of the Pholadidae characterized by teredinid-like shells and a small, divided mesoplax. They lack apophyses (as do the Jouannetiinae) and do not produce a callum in the adult stage (as in the Phola- in dinae). They are unique among the Pholadidae having a wood- storing caecum. The author is grateful to Dr. Frederick Bayer, Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, Dr. J0r- gen Knudsen, Universitetets Zoologiske Museum, Copenhagen, Den- mark, and Dr. W. Adam, Institut Royal des Sciences Naturelles de Belgique, Brussels, Belgium, for the loan of specimens and the opportunity to remove specimens from dredged wood or other plant material in their collections. -
Embryonic and Larval Development of Ensis Arcuatus (Jeffreys, 1865) (Bivalvia: Pharidae)
EMBRYONIC AND LARVAL DEVELOPMENT OF ENSIS ARCUATUS (JEFFREYS, 1865) (BIVALVIA: PHARIDAE) FIZ DA COSTA, SUSANA DARRIBA AND DOROTEA MARTI´NEZ-PATIN˜O Centro de Investigacio´ns Marin˜as, Consellerı´a de Pesca e Asuntos Marı´timos, Xunta de Galicia, Apdo. 94, 27700 Ribadeo, Lugo, Spain (Received 5 December 2006; accepted 19 November 2007) ABSTRACT The razor clam Ensis arcuatus (Jeffreys, 1865) is distributed from Norway to Spain and along the British coast, where it lives buried in sand in low intertidal and subtidal areas. This work is the first study to research the embryology and larval development of this species of razor clam, using light and scanning electron microscopy. A new method, consisting of changing water levels using tide simulations with brief Downloaded from https://academic.oup.com/mollus/article/74/2/103/1161011 by guest on 23 September 2021 dry periods, was developed to induce spawning in this species. The blastula was the first motile stage and in the gastrula stage the vitelline coat was lost. The shell field appeared in the late gastrula. The trocho- phore developed by about 19 h post-fertilization (hpf) (198C). At 30 hpf the D-shaped larva showed a developed digestive system consisting of a mouth, a foregut, a digestive gland followed by an intestine and an anus. Larvae spontaneously settled after 20 days at a length of 378 mm. INTRODUCTION following families: Mytilidae (Redfearn, Chanley & Chanley, 1986; Fuller & Lutz, 1989; Bellolio, Toledo & Dupre´, 1996; Ensis arcuatus (Jeffreys, 1865) is the most abundant species of Hanyu et al., 2001), Ostreidae (Le Pennec & Coatanea, 1985; Pharidae in Spain. -
Wood-Boring Bivalves and Boring Linings
Wood-boring bivalves and boring linings SIÂN EVANS Evans, S. Wood-boring bivalves and boring linings. Bulletin of the Geological Society of Denmark, Vol. 45, pp. 130–134. Copenhagen, 1999–01–30. The anatomical features and morphology and lining of the borings of wood- boring bivalves are evaluated as taxobases. The aragonitic valves and pallets have poorer preservation potential than the calcitic boring linings that some forms secrete. These linings may be septate, containing retrusive caps. Key words: Wood-boring bivalves, Teredinidae, Xylophagainae, Cretaceous, bor- ing lining, taxonomy. S. Evans, Department of Palaeontology, The Natural History Museum, London SW7 5DB, U.K. 2 August 1998. The dominant agents of wood bioerosion throughout (Waterbury et al. 1983). Their valves are highly re- the Mesozoic and Cenozoic are pholadacean boring duced in size, hemispherical in shape and, like some bivalves. The Pholadacea comprise two families other pholadacean groups, bear an internal, rod-like (Turner 1969), the Teredinidae (shipworms) and the projection, the apophysis (Fig. 1F). Valve shape is Pholadidae (piddocks). The wood-boring habit occurs extremely conservative within the family and is of lim- in both families, but the most specialized, diverse and ited use in taxonomy (Turner 1966). Instead, unique successful wood-borers are teredinids. Extant teredi- structures, calcareous pallets which are secreted at the nids have so derived a morphology that their relation- distal end of the siphons, are used to distinguish gen- ships with other members of the Pholadacea are poorly era and species. The pallet is forced against a calcare- understood (Hoagland & Turner 1981). A detailed ous lining at the aperture of the boring to produce a understanding of fossil wood-borers may yield the seal (Fig. -
Brief Glossary and Bibliography of Mollusks
A Brief Glossary of Molluscan Terms Compiled by Bruce Neville Bivalve. A member of the second most speciose class of Mollusca, generally bearing a shell of two valves, left and right, and lacking a radula. Commonly called clams, mussels, oysters, scallops, cockles, shipworms, etc. Formerly called pelecypods (class Pelecypoda). Cephalopoda. The third dominant class of Mollusca, generally without a true shell, though various internal hard structures may be present, highly specialized anatomically for mobility. Commonly called octopuses, squids, cuttles, nautiluses. Columella. The axis, real or imaginary, around and along which a gastropod shell grows. Dextral. Right-handed, with the aperture on the right when the spire is at the top. Most gastropods are dextral. Gastropod. A member of the largest class of Mollusca, often bearing a shell of one valve and an operculum. Commonly called snails, slugs, limpets, conchs, whelks, sea hares, nudibranchs, etc. Mantle. The organ that secretes the shell. Mollusk (or mollusc). A member of the second largest phylum of animals, generally with a non-segmented body divided into head, foot, and visceral regions; often bearing a shell secreted by a mantle; and having a radula. Operculum. A horny or calcareous pad that partially or completely closes the aperture of some gastropodsl. Periostracum. The proteinaceous layer covering the exterior of some mollusk shells. Protoconch. The larval shell of the veliger, often remains as the tip of the adult shell. Also called prodissoconch in bivlavles. Radula. A ribbon of teeth, unique to mollusks, used to procure food. Sinistral. Left-handed, with the aperture on the left when the spire is at the top. -
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 -
Mollusc Fauna of Iskenderun Bay with a Checklist of the Region
www.trjfas.org ISSN 1303-2712 Turkish Journal of Fisheries and Aquatic Sciences 12: 171-184 (2012) DOI: 10.4194/1303-2712-v12_1_20 SHORT PAPER Mollusc Fauna of Iskenderun Bay with a Checklist of the Region Banu Bitlis Bakır1, Bilal Öztürk1*, Alper Doğan1, Mesut Önen1 1 Ege University, Faculty of Fisheries, Department of Hydrobiology Bornova, Izmir. * Corresponding Author: Tel.: +90. 232 3115215; Fax: +90. 232 3883685 Received 27 June 2011 E-mail: [email protected] Accepted 13 December 2011 Abstract This study was performed to determine the molluscs distributed in Iskenderun Bay (Levantine Sea). For this purpose, the material collected from the area between the years 2005 and 2009, within the framework of different projects, was investigated. The investigation of the material taken from various biotopes ranging at depths between 0 and 100 m resulted in identification of 286 mollusc species and 27542 specimens belonging to them. Among the encountered species, Vitreolina cf. perminima (Jeffreys, 1883) is new record for the Turkish molluscan fauna and 18 species are being new records for the Turkish Levantine coast. A checklist of Iskenderun mollusc fauna is given based on the present study and the studies carried out beforehand, and a total of 424 moluscan species are known to be distributed in Iskenderun Bay. Keywords: Levantine Sea, Iskenderun Bay, Turkish coast, Mollusca, Checklist İskenderun Körfezi’nin Mollusca Faunası ve Bölgenin Tür Listesi Özet Bu çalışma İskenderun Körfezi (Levanten Denizi)’nde dağılım gösteren Mollusca türlerini tespit etmek için gerçekleştirilmiştir. Bu amaçla, 2005 ve 2009 yılları arasında sürdürülen değişik proje çalışmaları kapsamında bölgeden elde edilen materyal incelenmiştir. -
Studies on Molluscan Shells: Contributions from Microscopic and Analytical Methods
Micron 40 (2009) 669–690 Contents lists available at ScienceDirect Micron journal homepage: www.elsevier.com/locate/micron Review Studies on molluscan shells: Contributions from microscopic and analytical methods Silvia Maria de Paula, Marina Silveira * Instituto de Fı´sica, Universidade de Sa˜o Paulo, 05508-090 Sa˜o Paulo, SP, Brazil ARTICLE INFO ABSTRACT Article history: Molluscan shells have always attracted the interest of researchers, from biologists to physicists, from Received 25 April 2007 paleontologists to materials scientists. Much information is available at present, on the elaborate Received in revised form 7 May 2009 architecture of the shell, regarding the various Mollusc classes. The crystallographic characterization of Accepted 10 May 2009 the different shell layers, as well as their physical and chemical properties have been the subject of several investigations. In addition, many researches have addressed the characterization of the biological Keywords: component of the shell and the role it plays in the hard exoskeleton assembly, that is, the Mollusca biomineralization process. All these topics have seen great advances in the last two or three decades, Shell microstructures expanding our knowledge on the shell properties, in terms of structure, functions and composition. This Electron microscopy Infrared spectroscopy involved the use of a range of specialized and modern techniques, integrating microscopic methods with X-ray diffraction biochemistry, molecular biology procedures and spectroscopy. However, the factors governing synthesis Electron diffraction of a specific crystalline carbonate phase in any particular layer of the shell and the interplay between organic and inorganic components during the biomineral assembly are still not widely known. This present survey deals with microstructural aspects of molluscan shells, as disclosed through use of scanning electron microscopy and related analytical methods (microanalysis, X-ray diffraction, electron diffraction and infrared spectroscopy). -
Guide to Estuarine and Inshore Bivalves of Virginia
W&M ScholarWorks Dissertations, Theses, and Masters Projects Theses, Dissertations, & Master Projects 1968 Guide to Estuarine and Inshore Bivalves of Virginia Donna DeMoranville Turgeon College of William and Mary - Virginia Institute of Marine Science Follow this and additional works at: https://scholarworks.wm.edu/etd Part of the Marine Biology Commons, and the Oceanography Commons Recommended Citation Turgeon, Donna DeMoranville, "Guide to Estuarine and Inshore Bivalves of Virginia" (1968). Dissertations, Theses, and Masters Projects. Paper 1539617402. https://dx.doi.org/doi:10.25773/v5-yph4-y570 This Thesis is brought to you for free and open access by the Theses, Dissertations, & Master Projects at W&M ScholarWorks. It has been accepted for inclusion in Dissertations, Theses, and Masters Projects by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. GUIDE TO ESTUARINE AND INSHORE BIVALVES OF VIRGINIA A Thesis Presented to The Faculty of the School of Marine Science The College of William and Mary in Virginia In Partial Fulfillment Of the Requirements for the Degree of Master of Arts LIBRARY o f the VIRGINIA INSTITUTE Of MARINE. SCIENCE. By Donna DeMoranville Turgeon 1968 APPROVAL SHEET This thesis is submitted in partial fulfillment of the requirements for the degree of Master of Arts jfitw-f. /JJ'/ 4/7/A.J Donna DeMoranville Turgeon Approved, August 1968 Marvin L. Wass, Ph.D. P °tj - D . dvnd.AJlLJ*^' Jay D. Andrews, Ph.D. 'VL d. John L. Wood, Ph.D. William J. Hargi Kenneth L. Webb, Ph.D. ACKNOWLEDGEMENTS The author wishes to express sincere gratitude to her major professor, Dr. -
Developmental Aspects of Biomineralisation in the Polynesian Pearl Oyster Pinctada Margaritifera Var
OCEANOLOGICA ACTA ⋅ VOL. 24 – Supplement Developmental aspects of biomineralisation in the Polynesian pearl oyster Pinctada margaritifera var. cumingii Lydie MAO CHEa,b, Stjepko GOLUBICc, Thérèse LE CAMPION-ALSUMARDd, Claude PAYRIa* a Laboratoire d’écologie marine, université de Polynésie française, BP 6570, Faaa, Tahiti, French Polynesia b Service des ressources marines, BP 20, Papeete, Tahiti, French Polynesia c Department of Biology, Boston University, 5 Cummington Street, Boston, MA 02125, USA d Centre d’océanologie de Marseille, UMR CNRS 6540, université de la Méditerranée, rue de la Batterie-des-Lions, 13007 Marseille, France Received 25 February 1999; revised 6 October 1999; accepted 17 February 2000 Abstract − The shell biomineralisation with special reference to the nacreous region is observed during the development of the Polynesian pearl oyster. Ultrastructural changes were studied and timed for the first time from planktonic larval shells to two-year-old adult shells. During the first two weeks following fertilization, the prodissoconch-I shell structure is undifferentiated and uniformly granular. The prodissoconch-II stage which develops during the next two weeks acquires a columnar organization. Metamorphosis is characterized by the formation of the dissoconch shell with all the elements of an adult shell and marks the onset of the development of the nacre. Nucleation starts within an organic matrix from point sources forming ‘crystal germs’ which expand circularly until they fuse. The orientation of the contour lines of scalariform growth margins indicates the direction of shell growth. Five zones of growth (Z) were characterized. One-month-old shells show a homogenous zone, without particular figures (Z0). The contour lines are initially parallel to the growing shell edge (Z1), later becoming labyrinthic (finger prints, Z2) or perpendicular to the edge (Z3). -
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).