Variation of Sperm Morphology in Pacific Oyster Precludes Its Use As a Species Marker but Enables Intraspecific Geo-Authentifica
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Biochemical Composition and Condition of Crassostrea Gigas (Thunberg, 1793) in Relation to Integrated Multi-Trophic Aquaculture (IMTA) Feed Sources
Biochemical composition and condition of Crassostrea gigas (Thunberg, 1793) in relation to integrated multi-trophic aquaculture (IMTA) feed sources vorgelegt von: Maximilian Felix Schupp geb. am 06.06.1990 in Lippstadt Erstgutachter: Zweitgutachter: Dr. Adrian Bischoff-Lang Prof. Dr. Bela H. Buck Universität Rostock Alfred-Wegener-Institut Agrar- und Umweltwissenschaftliche Helmholtz Zentrum für Polar Fakultät und Meeresforschung (AWI) Lehrstuhl Aquakultur und Sea-Ranching MASTERARBEIT im Studiengang Aquakultur und Sea-Ranching Agrar- und Umweltwissenschaftliche Fakultät Rostock, 2015 Directory 1 INTRODUCTION .................................................................................................. 1 2 BACKGROUND ..................................................................................................... 5 2.1 Biology of Crassostrea gigas ............................................................................................................. 5 2.2 Lipids and fatty acids...................................................................................................................... 10 3 MATERIALS AND METHODS ......................................................................... 12 3.1 Specimen .......................................................................................................................................... 12 3.2 Experimental setup ......................................................................................................................... 12 3.3 Determination of dry weight -
Annual Report Fy2016
ANNUAL REPORT FY2016 AFFILIATED WITH Affiliated with Cornell University PRI: WHO WE ARE Founded in 1932, the Paleontological Research Institution (PRI) pursues and integrates education and research, and interprets the history and systems of the Earth and its life. Our aim is to increase knowledge, educate society, and encourage wise stewardship of the Earth. PRI has two campuses and one large plot of forest property north of Ithaca, NY. Palmer Hall Museum of the Earth Named in honor of Katherine Palmer Opened in 2003, the Museum of the Earth (Director, 1952-1978), Palmer Hall is the is home to temporary and permanent Institution’s main building, housing PRI’s exhibitions that teach visitors about the collections, laboratories, library, and offices. history of life on Earth. Cayuga Nature Center Smith Woods The Cayuga Nature Center merged with Located in Trumansburg, NY, Smith Woods PRI in 2013. The Nature Center’s education is the largest plot of old-growth forest in programs and exhibitions focus on the central New York. More than 32 acres large, natural history of the Cayuga Lake basin, Smith Woods serves as a research and and are conducted in the Lodge and on the education resource for elementary through 120 acres of woodlands and fields on-site. graduate students. TABLE OF CONTENTS DIRECTOR’S AND PRESIDENT’S MESSAGE 2-3 PRI SERVES: 2016-2016 AT A GLANCE 4-5 RESEARCH 6-9 PUBLICATIONS 10-11 COLLECTIONS 12-13 EDUCATION 14-18 GRANTS 19 CORNELL UNIVERSITY RELATIONS 20-23 MUSEUM OF THE EARTH 24-25 CAYUGA NATURE CENTER 26-27 EXHIBITIONS 28-31 COMMUNITY ACCESSIBILITY 32-33 INTERNS AND VOLUNTEERS 34-35 DONOR SUPPORT 36-39 FINANCIAL ACTIVITY STATEMENT 40 BOARD OF TRUSTEES AND STAFF 41 FRONT COVER BACKGROUND IMAGE: Blue sky at the Cayuga Nature Center. -
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. -
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. -
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 -
Structure and Distribution of Chalky Deposits in the Pacific Oyster Using
www.nature.com/scientificreports OPEN Structure and distribution of chalky deposits in the Pacifc oyster using x‑ray computed tomography (CT) Roxanne M. W. Banker* & Dawn Y. Sumner Oysters are unusual among bivalves in that they possess chambers, often flled with soft, chalky calcite, that are irregularly scattered throughout the shell. Because the function of these so‑called chalky deposits is still unclear, evaluating the growth and distribution of chalk is important for elucidating the ecological function of this unique shell trait. Specimens of the Pacifc oyster Magallana gigas, an oyster well known for chalk expression, were grown in Bodega Harbor, Bodega Bay, CA. At the end of an 11 month growing period, specimens were culled and selected animals were submitted for x‑ray computed‑tomography imaging. Three‑dimensional reconstructions of oyster shells were used to assess the overall distribution of chalk, and also to better understand the relationship between chalk and other structures within the shell. Results indicate that chalky deposits underly sculptural features on the shell exterior, such as external ridges and changes in growth direction, and also that there is a relationship between chalk formation and oyster processes of cementation. Overall, chalk is useful for a cementing lifestyle because it enables morphological plasticity needed to conform to irregular substrates, but also acts as a cheap building material to facilitate rapid growth. Many researchers have used preserved remains of shells (molluscan or otherwise) to improve scientifc under- standing of paleoecosystems and organismal interactions in the fossil record1–3. Oysters (Bivalvia: Ostreidae) have utility in this setting because they are well preserved in the fossil record, and are widely geographically dis- tributed in paleo and modern ecosystems4. -
An Annotated Checklist of the Marine Macroinvertebrates of Alaska David T
NOAA Professional Paper NMFS 19 An annotated checklist of the marine macroinvertebrates of Alaska David T. Drumm • Katherine P. Maslenikov Robert Van Syoc • James W. Orr • Robert R. Lauth Duane E. Stevenson • Theodore W. Pietsch November 2016 U.S. Department of Commerce NOAA Professional Penny Pritzker Secretary of Commerce National Oceanic Papers NMFS and Atmospheric Administration Kathryn D. Sullivan Scientific Editor* Administrator Richard Langton National Marine National Marine Fisheries Service Fisheries Service Northeast Fisheries Science Center Maine Field Station Eileen Sobeck 17 Godfrey Drive, Suite 1 Assistant Administrator Orono, Maine 04473 for Fisheries Associate Editor Kathryn Dennis National Marine Fisheries Service Office of Science and Technology Economics and Social Analysis Division 1845 Wasp Blvd., Bldg. 178 Honolulu, Hawaii 96818 Managing Editor Shelley Arenas National Marine Fisheries Service Scientific Publications Office 7600 Sand Point Way NE Seattle, Washington 98115 Editorial Committee Ann C. Matarese National Marine Fisheries Service James W. Orr National Marine Fisheries Service The NOAA Professional Paper NMFS (ISSN 1931-4590) series is pub- lished by the Scientific Publications Of- *Bruce Mundy (PIFSC) was Scientific Editor during the fice, National Marine Fisheries Service, scientific editing and preparation of this report. NOAA, 7600 Sand Point Way NE, Seattle, WA 98115. The Secretary of Commerce has The NOAA Professional Paper NMFS series carries peer-reviewed, lengthy original determined that the publication of research reports, taxonomic keys, species synopses, flora and fauna studies, and data- this series is necessary in the transac- intensive reports on investigations in fishery science, engineering, and economics. tion of the public business required by law of this Department. -
USGS Professional Paper 1662, Chapter 4
Studies by the U.S. Geological Survey in Alaska, 2000 U.S. Geological Survey Professional Paper 1662 Late Triassic (Norian) Mollusks From the Taylor Mountains Quadrangle, Southwestern Alaska By Christopher A. McRoberts1 and Robert B. Blodgett2 Abstract Such paleobiogeographic data as those presented herein are extremely useful in constraining the past geographic positions We describe a diverse molluscan fauna of silicified fossils of these mobile terranes over time, and so are of utmost utility from two localities in the Taylor Mountains D–3 quadrangle of in unraveling the tectonic history of this part of Alaska. southwestern Alaska. The molluscan fauna consists of at least 8 species of bivalves, including 1 new species, Cassianella cordillerana McRoberts n.sp., and at least 11 species of gas- Geologic Setting tropods, including 2 new species, Neritaria nuetzeli Blodgett n.sp. and Andangularia wilsoni Blodgett n.sp. Bivalve and gastropod affinities suggest an early Norian age, with taxo- The Farewell terrane of southwestern and west-central nomic similarities to several southern Alaskan tectonostrati- Alaska (fig. 1) was established by Decker and others (1994) graphic terranes (for example, Alexander and Chulitna), as as a tectonostratigraphic entity incorporating three previously well as to the South American Cordillera of Peru. The mol- named, genetically related terranes (Nixon Fork, Dillinger, lusks are associated with numerous brachiopods that also sup- and Mystic) that are relegated the status of subterranes of the port a Norian -
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. -
D9.1 Report on Environmental Impacts from Brine Discharge
D9.1 Report on environmental impacts from brine discharge October 2020 Draft Deliverable 9.1 Report on environmental impacts from brine discharge Related Work Package WP9 – Subtask 9.2.2 Deliverable lead University of Aberdeen (ABDN) Author(s) Sergio Carlos Garcia Gomez, Taxonomist Contact [email protected] [email protected] Reviewer Frithjof Kuepper Grant Agreement Number 730390 Instrument Horizon 2020 Framework Programme Start date 1.6.2017 Duration 48 months Type of Delivery (R, DEM, DEC, Other)1 R Dissemination Level (PU, CO, Cl)2 PU Date last update 9 October 2020 Website www.zerobrine.eu Name of researcher(s) with roles Eleni Avramidi, Honorary Research Fellow, School of Biological Sciences (ABDN) Prof. Frithjof Kuepper, Chair in Marine Biodiversity, School of Biological Sciences (ABDN) 1 R=Document, report; DEM=Demonstrator, pilot, prototype; DEC=website, patent fillings, videos, etc.; OTHER=other 2 PU=Public, CO=Confidential, only for members of the consortium (including the Commission Services), CI=Classified ZERO BRINE – Industrial Wastewater – Resource Recovery – Circular Economy 1 Revision Date Description Author(s) no 0.1 30 May 2020 First draft Prof. Frithjof Kuepper (ABDN) Eleni Avramidi (ABDN) Sergio Carlos Garcia Gomez, Taxonomist 0.2 14 Oct. 2020 Second draft Prof. Frithjof Kuepper (ABDN) The chapters “Executive summary” Eleni Avramidi (ABDN) and “Conclusions” have been Sergio Carlos Garcia Gomez, included. The comments of the Taxonomist internal review have been incorporated. The ZERO BRINE project has received funding from the European Commission under the Horizon 2020 programme, Grant Agreement no. 730390. The opinions expressed in this document reflect only the author’s view and in no way reflect the European Commission’s opinions. -
Environmental Setting of Deep-Water Oysters in the Bay of Biscay
Deep Sea Research Part I: Oceanographic Archimer Research Papers http://archimer.ifremer.fr December 2010, Volume 57 (12), pp. 1561-1572 http://dx.doi.org/10.1016/j.dsr.2010.09.002 © 2010 Elsevier Ltd. All rights reserved. ailable on the publisher Web site Environmental setting of deep-water oysters in the Bay of Biscay D. Van Rooija, *, L. De Mola, E. Le Guillouxb, M. Wisshakc, V.A.I. Huvenned, R. Moeremanse, a, J.-P. Henrieta a Renard Centre of Marine Geology, Ghent University, Krijgslaan 281 S8, B-9000 Gent, Belgium b IFREMER, Laboratoire Environnement Profond, BP70, F-29280 Plouzané, France c GeoZentrum Nordbayern, Erlangen University, Loewenichstr. 28, D-91054 Erlangen, Germany d Geology and Geophysics Group, National Oceanography Centre, European Way, SO14 3 ZH Southampton, UK e Scripps Institution of Oceanography, UCSD, La Jolla, CA, United States of America blisher-authenticated version is av *: Corresponding author : David Van Rooij, Tel.: +32 9 2644583 ; fax: +32 9 2644967 ; email address : [email protected] Abstract : We report the northernmost and deepest known occurrence of deep-water pycnodontine oysters, based on two surveys along the French Atlantic continental margin to the La Chapelle continental slope (2006) and the Guilvinec Canyon (2008). The combined use of multibeam bathymetry, seismic profiling, CTD casts and a remotely operated vehicle (ROV) made it possible to describe the physical habitat and to assess the oceanographic control for the recently described species Neopycnodonte zibrowii. These oysters have been observed in vivo in depths from 540 to 846 m, colonizing overhanging banks or escarpments protruding from steep canyon flanks.