The Veliger 31 (3/4):214-221 (October 3, 1988)
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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 -
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. -
What Are Molluscs?
The shells of molluscs from all over the world – on land, in lakes, and in the ocean – contain very detailed imprints of past climate change. Using isotope analysis, we can extract these signals and start to piece together long-term climate variations. You will never look at a garden snail in the same way again! What are molluscs? Molluscs are soft-bodied (invertebrate) organisms that are widespread in terrestrial, freshwater, and marine habitats. We can split them into two basic groups: Gastropods: Molluscs with up to one shell or ‘valve’ (such as snails or slugs) Bivalves: Molluscs with two-sided shells or ‘valves’ (such as clams, oysters, and mussels) Many molluscs (both gastropods and bivalves) build hard shells that are rich in calcium carbonate. We call these ‘calcareous shells’. Such shells are formed in distinct bands (like tree rings) growing outwards along the direction of growth – the oldest shell is at the edge. Over time, more bands are added to the shell as it grows and the organism is enlarged (Figure 1a-c). The environmental conditions in which the organism live are reflected in the types of isotopes that are present in its shell. This means that the shell contains a ‘geochemical’ signature of the mollusc’s habitat and lifestyle. When the organism dies, its shell can become buried and preserved in sediments at the bottom of the lake or ocean (Figure 1d-f). Once preserved, these shells provide us with a valuable record of environmental conditions at the time that the organism lived. We can analyse the isotopes within the shells to build up a picture of environmental conditions in the past. -
Methods and Materials for Aquaculture Production of Sea Scallops (Placopecten Magellanicus)
Methods and Materials for Aquaculture Production of Sea Scallops (Placopecten magellanicus) Dana L. Morse • Hugh S. Cowperthwaite • Nathaniel Perry • Melissa Britsch Contents Rationale and background. .1 Scallop biology . 1 Spat collection . 2 Nursery culture. 3 Growout. .4 Bottom cages . 4 Pearl nets. 5 Lantern nets. 5 Suspension cages . 6 Ear hanging. 6 Husbandry and fouling control. 7 Longline design and materials . 7 Moorings and mooring lines. 7 Longline (or backline) . 7 Tension buoys . 7 Marker buoys . 7 Compensation buoys . 8 Longline weights. 8 Site selection . 8 Economic considerations & recordkeeping . 8 Scallop products, biotoxins & public health . 8 Literature Cited. 9 Additional Reading. 9 Appendix I . 9 Example of an annual cash flow statement. 9 Acknowledgements . 9 Authors’ contact information Dana L. Morse Nathaniel Perry Maine Sea Grant and University of Maine Pine Point Oyster Company Cooperative Extension 10 Pine Ridge Road, Cape Elizabeth, ME 04107 193 Clark’s Cove Road, Walpole, ME 04573 [email protected] [email protected] Melissa Britsch Hugh S. Cowperthwaite University of Maine, Darling Marine Center Coastal Enterprises, Inc. 193 Clark’s Cove Road, Walpole, ME 04573 30 Federal Street, Brunswick, ME 04011 [email protected] [email protected] The University of Maine is an EEO/AA employer and does not discriminate on the grounds of race, color, religion, sex, sexual orientation, transgender status, gender expression, national origin, citizenship status, age, disability, genetic information or veteran’s status in employment, education, and all other programs and activities. The following person has been designated to handle inquiries regarding non-discrimination policies: Director of Equal Opportunity, 101 North Stevens Hall, University of Maine, Orono, ME 04469-5754, 207.581.1226, TTY 711 (Maine Relay System). -
THE FUNCTIONAL MORPHOLOGY of OTINA OTIS, a PRIMITIVE MARINE PULMONATE by J. E. Morton Department of Zoology, Queen Mary College, University of London
J. Mar. bioI.Ass. U.K. (1955) 34, II3-150 II3 Printed in Great Britain THE FUNCTIONAL MORPHOLOGY OF OTINA OTIS, A PRIMITIVE MARINE PULMONATE By J. E. Morton Department of Zoology, Queen Mary College, University of London (Text-figs. 1-12) The family Otinidae is the smallest and probably the least known among the pulmonates. Thiele (1931) places it at the base of the Basommatophora, the more primitive order of the subclass Pulmonata, in the Stirps Actophila. It contains a single species, Otina otis Turton, with a geographical range con- fined to the coasts of the British Isles and north-west France. Its northern distribution reaches as far as the Firth of Clyde, according to Jeffreys (1869), and over the greater part of its British range it appears to follow fairly closely the distribution of the barnacle Chthamalus stellatus, which here reaches its northern limit. Otina otis is a tiny snail, and its external form is limpet-like. The shell, which is well described by Jeffreys (1869), and also by Ellis (1926), measures up to 2' 5 mm in length, with a short apical visceral coil at the posterior end. It is dark chestnut brown in colour, and most resembles a minute Haliotis. A description of the ecology of Otina otis has already appeared, as portion of a study of the crevice-dwelling animals of the upper intertidal zone at Wembury (Morton, 1954). Otina is rather restricted in its mode of occurrence as regards both vertical tidal range and selection of substratum. It lives a short distance within the mouths of crevices between layers offoliaceous rocks, such as Dartmouth Slate at Wembury and Whitsands, and felsite at Kingsands, and in fissures between blocks of Staddon Grit at Rum Bay and volcanic rocks at Drake's Island. -
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. -
Mechanics Unlocks the Morphogenetic Puzzle of Interlocking Bivalved Shells
Mechanics unlocks the morphogenetic puzzle of interlocking bivalved shells Derek E. Moultona,1 , Alain Gorielya , and Regis´ Chiratb aMathematical Institute, University of Oxford, Oxford, OX2 6GG, United Kingdom; and bCNRS 5276, LGL-TPE (Le Laboratoire de Geologie´ de Lyon: Terre, Planetes,` Environnement), Universite´ Lyon 1, 69622 Villeurbanne Cedex, France Edited by Sean H. Rice, Texas Tech University, Lubbock, TX, and accepted by Editorial Board Member David Jablonski November 11, 2019 (received for review September 24, 2019) Brachiopods and mollusks are 2 shell-bearing phyla that diverged tal events causing shell injuries. Yet, in all cases the interlocking from a common shell-less ancestor more than 540 million years ago. of the 2 shell edges is tightly maintained. These observations Brachiopods and bivalve mollusks have also convergently evolved imply that the interlocking pattern emerges as the result of epi- a bivalved shell that displays an apparently mundane, yet strik- genetic interactions modulating the behavior of the secreting ing feature from a developmental point of view: When the shell mantle during shell development. is closed, the 2 valve edges meet each other in a commissure that Here, we provide a geometric and mechanical explanation forms a continuum with no gaps or overlaps despite the fact that for this morphological trait based on a detailed analysis of the each valve, secreted by 2 mantle lobes, may present antisymmet- shell geometry during growth and the physical interaction of the ric ornamental patterns of varying regularity and size. Interlock- shell-secreting soft mantle with both the rigid shell edge and ing is maintained throughout the entirety of development, even the opposing mantle lobe. -
Filtering, Feeding, and Digestion in the Lamellibranch Lasaea Rubra
J. Mar. bioI.Ass. U.K. (1956) 35, 241-274 241 Printed in Great Britain FILTERING, FEEDING, AND DIGESTION IN THE LAMELLIBRANCH LASAEA RUBRA By Dorothy Ballantine The Plymouth Laboratory and J. E. Morton Department of Zoology, Queen Mary College, University of London (Text-figs. I-II) Lasaea rubra is the smallest and commonest of Plymouth bivalves. It is intertidal on rocky shores, often in immense numbers, in crevicesand other protected places, and in Pygmaeapumila (Colman, 1940).This bivalve is an excellent laboratory animal. It remains fully active for several days under laboratory conditions, and a large number of animals can be used in a single experiment, eliminating the variations in activity found when dealing with a few, or single.specimens of larger animals. Because of the relatively high position Lasaearubramay occupy on the shore its feeding cycleis broken by regular dry periods at each tide. Thus, for experiments relating to periodicity in feeding,we have an animalwhosetimes of feeding can easilybe ascertained and experimentallyvaried over a wide range. Lastly, in makingserial sections and in examiningtotal gut contents, in workon the digestivesystem,the small size of the animal is of obvious advantage. The present paper is devoted to an account of filtering rates with various food organisms, variations in filtering activity and the relation of filtering to feedingand digestion. Further workhasbeen completedby oneofus(J.E.M.) on the mechanism of digestionand the cycleof activity of the digestivegland, and experiments are in progress on respiration during submersion and exposure. We record our special thanks to Dr Mary Parke, botanist at the Plymouth Laboratory, for making availablethe unialgal cultures of the organismsused, and for her invariable kindness and sound advice. -
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 -
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.