Et De Limacina Helicina (Phipps, 1774) Dans L’Arctique
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Validation of Holoplanktonic Molluscan Taxa from the Oligo- Miocene of the Maltese Archipelago, Introduced in Violation with ICZN Regulations
Cainozoic Research, 9(2), pp. 189-191, December 2012 ! ! ! Validation of holoplanktonic molluscan taxa from the Oligo- Miocene of the Maltese Archipelago, introduced in violation with ICZN regulations Arie W. Janssen Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA Leiden, The Netherlands; currently: 12 Triq tal’Hamrija, Xewkija XWK 9033, Gozo, Malta; email: [email protected] Received 29 August 2012, accepted 6 September 2012 Five gymnosomatous molluscan taxa were recently introduced applying ‘open generic nomenclature’ by using the indication ‘Genus Clionidarum’ instead of a formal genus name and therefore violating ICZN art. 11.9.3 of the Code. Herein those taxa are validated by placing them in the type genus of the family Clionidae, followed by a question mark indicating here that they might as well belong to any other of the known (or as yet unknown) genera in the family Clionidae . Introduction Clionidarum’ as used in my paper indeed cannot be con- sidered to be an unambiguous genus name. In my study of Maltese fossil holoplanktonic molluscs I herewith validate the new names by combining them with (Janssen, 2012) a number of new species of gymnosoma- the unambiguous genus name Clione, followed by a ques- tous larval shells were introduced, more or less resembling tion mark, indicating here that those species might as well the few Recent larval shells known from this group of Gas- belong to any other known or unknown genus in the tropoda, but obviously (also considering their ages) repre- Clionidae. senting undescribed species. Recent Gymnosomata are RGM-registration numbers refer to the collections of Natu- shell-less in the adult stage, and their larval shell is shed at ralis Biodiversity Center, Palaeontology Department (Lei- metamorphosis from larva to adult. -
Phylum MOLLUSCA
285 MOLLUSCA: SOLENOGASTRES-POLYPLACOPHORA Phylum MOLLUSCA Class SOLENOGASTRES Family Lepidomeniidae NEMATOMENIA BANYULENSIS (Pruvot, 1891, p. 715, as Dondersia) Occasionally on Lafoea dumosa (R.A.T., S.P., E.J.A.): at 4 positions S.W. of Eddystone, 42-49 fm., on Lafoea dumosa (Crawshay, 1912, p. 368): Eddystone, 29 fm., 1920 (R.W.): 7, 3, 1 and 1 in 4 hauls N.E. of Eddystone, 1948 (V.F.) Breeding: gonads ripe in Aug. (R.A.T.) Family Neomeniidae NEOMENIA CARINATA Tullberg, 1875, p. 1 One specimen Rame-Eddystone Grounds, 29.12.49 (V.F.) Family Proneomeniidae PRONEOMENIA AGLAOPHENIAE Kovalevsky and Marion [Pruvot, 1891, p. 720] Common on Thecocarpus myriophyllum, generally coiled around the base of the stem of the hydroid (S.P., E.J.A.): at 4 positions S.W. of Eddystone, 43-49 fm. (Crawshay, 1912, p. 367): S. of Rame Head, 27 fm., 1920 (R.W.): N. of Eddystone, 29.3.33 (A.J.S.) Class POLYPLACOPHORA (=LORICATA) Family Lepidopleuridae LEPIDOPLEURUS ASELLUS (Gmelin) [Forbes and Hanley, 1849, II, p. 407, as Chiton; Matthews, 1953, p. 246] Abundant, 15-30 fm., especially on muddy gravel (S.P.): at 9 positions S.W. of Eddystone, 40-43 fm. (Crawshay, 1912, p. 368, as Craspedochilus onyx) SALCOMBE. Common in dredge material (Allen and Todd, 1900, p. 210) LEPIDOPLEURUS, CANCELLATUS (Sowerby) [Forbes and Hanley, 1849, II, p. 410, as Chiton; Matthews. 1953, p. 246] Wembury West Reef, three specimens at E.L.W.S.T. by J. Brady, 28.3.56 (G.M.S.) Family Lepidochitonidae TONICELLA RUBRA (L.) [Forbes and Hanley, 1849, II, p. -
Seasonal and Interannual Patterns of Larvaceans and Pteropods in the Coastal Gulf of Alaska, and Their Relationship to Pink Salmon Survival
Seasonal and interannual patterns of larvaceans and pteropods in the coastal Gulf of Alaska, and their relationship to pink salmon survival Item Type Thesis Authors Doubleday, Ayla Download date 30/09/2021 16:15:58 Link to Item http://hdl.handle.net/11122/4451 SEASONAL AND INTERANNUAL PATTERNS OF LARVACEANS AND PTEROPODS IN THE COASTAL GULF OF ALASKA, AND THEIR RELATIONSHIP TO PINK SALMON SURVIVAL By Ayla Doubleday RECOMMENDED: __________________________________________ Dr. Rolf Gradinger __________________________________________ Dr. Kenneth Coyle __________________________________________ Dr. Russell Hopcroft, Advisory Committee Chair __________________________________________ Dr. Brenda Konar Head, Program, Marine Science and Limnology APPROVED: __________________________________________ Dr. Michael Castellini Dean, School of Fisheries and Ocean Sciences __________________________________________ Dr. John Eichelberger Dean of the Graduate School __________________________________________ Date iv SEASONAL AND INTERANNUAL PATTERNS OF LARVACEANS AND PTEROPODS IN THE COASTAL GULF OF ALASKA, AND THEIR RELATIONSHIP TO PINK SALMON SURVIVAL A THESIS Presented to the Faculty of the University of Alaska Fairbanks in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE By Ayla J. Doubleday, B.S. Fairbanks, Alaska December 2013 vi v Abstract Larvacean (=appendicularians) and pteropod (Limacina helicina) composition and abundance were studied with physical variables each May and late summer across 11 years (2001 to 2011), along one transect that crosses the continental shelf of the subarctic Gulf of Alaska and five stations within Prince William Sound (PWS). Collection with 53- µm plankton nets allowed the identification of larvaceans to species: five occurred in the study area. Temperature was the driving variable in determining larvacean community composition, yielding pronounced differences between spring and late summer, while individual species were also affected differentially by salinity and chlorophyll-a concentration. -
Canada's Arctic Marine Atlas
CANADA’S ARCTIC MARINE ATLAS This Atlas is funded in part by the Gordon and Betty Moore Foundation. I | Suggested Citation: Oceans North Conservation Society, World Wildlife Fund Canada, and Ducks Unlimited Canada. (2018). Canada’s Arctic Marine Atlas. Ottawa, Ontario: Oceans North Conservation Society. Cover image: Shaded Relief Map of Canada’s Arctic by Jeremy Davies Inside cover: Topographic relief of the Canadian Arctic This work is licensed under the Creative Commons Attribution-NonCommercial 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/4.0 or send a letter to Creative Commons, PO Box 1866, Mountain View, CA 94042, USA. All photographs © by the photographers ISBN: 978-1-7752749-0-2 (print version) ISBN: 978-1-7752749-1-9 (digital version) Library and Archives Canada Printed in Canada, February 2018 100% Carbon Neutral Print by Hemlock Printers © 1986 Panda symbol WWF-World Wide Fund For Nature (also known as World Wildlife Fund). ® “WWF” is a WWF Registered Trademark. Background Image: Phytoplankton— The foundation of the oceanic food chain. (photo: NOAA MESA Project) BOTTOM OF THE FOOD WEB The diatom, Nitzschia frigida, is a common type of phytoplankton that lives in Arctic sea ice. PHYTOPLANKTON Natural history BOTTOM OF THE Introduction Cultural significance Marine phytoplankton are single-celled organisms that grow and develop in the upper water column of oceans and in polar FOOD WEB The species that make up the base of the marine food Seasonal blooms of phytoplankton serve to con- sea ice. Phytoplankton are responsible for primary productivity—using the energy of the sun and transforming it via pho- web and those that create important seafloor habitat centrate birds, fishes, and marine mammals in key areas, tosynthesis. -
Pteropods (Gastropoda: Opisthobranchia) in the Southern
ICES CM 2009/A:16 Pteropods (Gastropoda: Opisthobranchia) in the Southern Ocean: First results from fatty acid and stable isotope analyses on the SYSTCO material Laura Würzberg*, Janna Peters, Enrico Schwabe, Svetlana Rodkina & Angelika Brandt Abstract The Antarctic Ocean is a complex ecosystem including planktonic herbivores like krill, salps, copepods a s w ell a s c arnivores l ike a mphipods, c tenophores, c nidarians and which are f ed upon by birds, fish, squids, seals and baleen whales. Although there are many reports about the che mical com ponents of t he Antarctic krill species Euphausia superba, as w ell as f or calanoid copepods, which are key organisms in the planktonic food web of the Antarctic Seas, there is yet little inf ormation available on the bi ochemical c onstituents of ot her c ommon species, like pteropods, which are frequently found in planktonic hols in the Southern Ocean. To find out more about the feeding ecology as well as the trophic position of these organisms, zooplankton samples were taken during the SYSTCO expedition, and preserved in order to conduct biochemical analyses, more precisely estimating stable isotope ratios and identifying fatty acid signatures. This approach will here be presented on four pteropod species (Clione limacina, Limacina helicina, Spongiobranchaea australis, Clio pyramidata sulcata). One aim of this study is to analyse and compare the fatty acid composition of these animals to discover possible adaptations to the polar environment as well as to identify the major food sources that are utilized. Furthermore, an approach is undertaken to define the trophic position of the studied animals. -
Sponge Biodiversity of the United Kingdom
Sponge Biodiversity of the United Kingdom A report from the Sponge Biodiversity of the United Kingdom project May 2008-May 2011 Claire Goodwin & Bernard Picton National Museums Northern Ireland Sponge Biodiversity of the United Kingdom Contents Page 1. Introduction 2 1.1 Project background 2 1.2 Project aims 2 1.3 Project outputs 2 2. Methods 3 2.1 Survey methodology 3 2.2 Survey locations 4 2.2.1 Firth of Lorn and Sound of Mull , Scotland 6 2.2.2 Pembrokeshire , Wales 6 2.2.3 Firth of Clyde , Scotland 6 2.2.4 Isles of Scilly , England 8 2.2.5 Sark, Channel Isles 8 2.2.6 Plymouth , England 8 2.3 Laboratory methodology 10 2.3.1 The identifi cation process 10 2.4 Data handling 11 3. Results 13 3.1 Notes on UK sponge communities 13 3.1.1 Scotland 13 3.1.2 Wales 13 3.1.3 Isles of Scilly 13 3.1.4 Sark 13 3.1.5 Sponge biogeography 15 3.2 Species of particular interest 15 4. Publications 34 4.1 Manuscripts in preparation 34 4.2 Published/accepted manuscripts 37 5. Publicity 37 5.1 Academic conference presentations 37 5.2 Public talks/events 38 5.3 Press coverage 38 6. Training Courses 39 7. Collaborations with other Organisations 42 8. Conclusions 44 8.1 Ulster Museum, National Museums Northern Ireland – a centre of excellence for sponge 44 taxonomy 8.2 Future work 44 8.2.1. Species requiring further work 45 9. Acknowledgements 46 10. -
Carotenoids of Sea Angels Clione Limacina and Paedoclione Doliiformis from the Perspective of the Food Chain
Mar. Drugs 2014, 12, 1460-1470; doi:10.3390/md12031460 OPEN ACCESS marine drugs ISSN 1660-3397 www.mdpi.com/journal/marinedrugs Article Carotenoids of Sea Angels Clione limacina and Paedoclione doliiformis from the Perspective of the Food Chain Takashi Maoka 1,*, Takashi Kuwahara 2 and Masanao Narita 3 1 Research Institute for Production Development, Shimogamo-Morimoto-cho 15, Sakyo-ku, Kyoto 606-0805, Japan 2 Okhotsk Sea Ice Museum of Hokkaido, Motomombetsu, Monbetsu, Hokkaido 094-0023, Japan; E-Mail: [email protected] 3 Hokkaido Research Organization, Abashiri Fisheries Research Institute, Minatomachi, Monbetsu, Hokkaido 094-0011, Japan; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +81-75-781-1107; Fax: +81-75-791-7659. Received: 16 January 2014; in revised form: 19 February 2014 / Accepted: 3 March 2014 / Published: 13 March 2014 Abstract: Sea angels, Clione limacina and Paedoclione doliiformis, are small, floating sea slugs belonging to Gastropoda, and their gonads are a bright orange-red color. Sea angels feed exclusively on a small herbivorous sea snail, Limacina helicina. Carotenoids in C. limacina, P. doliiformis, and L. helicina were investigated for comparative biochemical points of view. β-Carotene, zeaxanthin, and diatoxanthin were found to be major carotenoids in L. helicina. L. helicina accumulated dietary algal carotenoids without modification. On the other hand, keto-carotenoids, such as pectenolone, 7,8-didehydroastaxanthin, and adonixanthin were identified as major carotenoids in the sea angels C. limacina and P. doliiformis. Sea angels oxidatively metabolize dietary carotenoids and accumulate them in their gonads. -
Glione Limacina in Plymouth Waters. by Marie V
[ 785 ] Glione limacina in Plymouth Waters. By Marie V. Lebour,D.Se., Naturalist at the Plymouth Laboratory. With Plates I and II. THEpteropod Olione limacina (Phipps), now regarded as one of the tecti- branchs, occurs at times in the neighbourhood of Plymouth. In 1930, however, it was extraordinarily abundant, especially in the summer, and was breeding freely. Although not specially recorded it has been seen singly or in small numbers in almost any month of the year, and for some years the eggs and larvffi(not recognised at the time as belonging to Clione) have been seen in summer. So far it is known from the British coasts in the North Sea and the west and extreme south-west of England. Its distribution, as known up to 1908, is given fully for the area of Inter- national Fisheries Invest:gations by Paulsen (1910). There it is shown that it is an Arctic-boreal species, spreading southwards nearly to the Bay of Biscay, which is about its southerly limit. It is known to occur in the northern and mid North Sea, but not in the southern North Sea, and at that time was only recorded from the Channel in the extreme west. It is also common in the Atlantic. Paulsen was led to infer that Clione limacina did not enter the North Sea from the Channel, but its prevalence sometimes at Plymouth shows that it can come a long way up the Channel and, as few samples are taken to the east and in the southern North Sea, this view should be carefully reconsidered. -
(Gulf Watch Alaska) Final Report the Seward Line: Marine Ecosystem
Exxon Valdez Oil Spill Long-Term Monitoring Program (Gulf Watch Alaska) Final Report The Seward Line: Marine Ecosystem monitoring in the Northern Gulf of Alaska Exxon Valdez Oil Spill Trustee Council Project 16120114-J Final Report Russell R Hopcroft Seth Danielson Institute of Marine Science University of Alaska Fairbanks 905 N. Koyukuk Dr. Fairbanks, AK 99775-7220 Suzanne Strom Shannon Point Marine Center Western Washington University 1900 Shannon Point Road, Anacortes, WA 98221 Kathy Kuletz U.S. Fish and Wildlife Service 1011 East Tudor Road Anchorage, AK 99503 July 2018 The Exxon Valdez Oil Spill Trustee Council administers all programs and activities free from discrimination based on race, color, national origin, age, sex, religion, marital status, pregnancy, parenthood, or disability. The Council administers all programs and activities in compliance with Title VI of the Civil Rights Act of 1964, Section 504 of the Rehabilitation Act of 1973, Title II of the Americans with Disabilities Action of 1990, the Age Discrimination Act of 1975, and Title IX of the Education Amendments of 1972. If you believe you have been discriminated against in any program, activity, or facility, or if you desire further information, please write to: EVOS Trustee Council, 4230 University Dr., Ste. 220, Anchorage, Alaska 99508-4650, or [email protected], or O.E.O., U.S. Department of the Interior, Washington, D.C. 20240. Exxon Valdez Oil Spill Long-Term Monitoring Program (Gulf Watch Alaska) Final Report The Seward Line: Marine Ecosystem monitoring in the Northern Gulf of Alaska Exxon Valdez Oil Spill Trustee Council Project 16120114-J Final Report Russell R Hopcroft Seth L. -
The Origin and Diversification of Pteropods Precede Past Perturbations in the Earth’S Carbon Cycle
The origin and diversification of pteropods precede past perturbations in the Earth’s carbon cycle Katja T. C. A. Peijnenburga,b,1, Arie W. Janssena, Deborah Wall-Palmera, Erica Goetzec, Amy E. Maasd, Jonathan A. Todde, and Ferdinand Marlétazf,g,1 aPlankton Diversity and Evolution, Naturalis Biodiversity Center, 2300 RA Leiden, The Netherlands; bDepartment Freshwater and Marine Ecology, Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, 1090 GE Amsterdam, The Netherlands; cDepartment of Oceanography, University of Hawai’iat Manoa, Honolulu, HI 96822; dBermuda Institute of Ocean Sciences, St. Georges GE01, Bermuda; eDepartment of Earth Sciences, Natural History Museum, London SW7 5BD, United Kingdom; fCentre for Life’s Origins and Evolution, Department of Genetics, Evolution and Environment, University College London, London WC1E 6BT, United Kingdom; and gMolecular Genetics Unit, Okinawa Institute of Science and Technology, Onna-son 904-0495, Japan Edited by John P. Huelsenbeck, University of California, Berkeley, CA, and accepted by Editorial Board Member David Jablonski August 19, 2020 (received for review November 27, 2019) Pteropods are a group of planktonic gastropods that are widely modern rise in ocean-atmosphere CO2 levels, global warming, and regarded as biological indicators for assessing the impacts of ocean acidification (16–18). Knowing whether major pteropod ocean acidification. Their aragonitic shells are highly sensitive to lineages have been exposed during their evolutionary history to acute changes in ocean chemistry. However, to gain insight into periods of high CO2 is important to extrapolate from current ex- their potential to adapt to current climate change, we need to perimental and observational studies to predictions of species-level accurately reconstruct their evolutionary history and assess their responses to global change over longer timescales. -
Social Social
CMYK RGB History of Geo- and Space Open Access Open Sciences Advances in Science & Research Open Access Proceedings Drinking Water Drinking Water Engineering and Science Engineering and Science Open Access Access Open Discussions Discussions Earth Syst. Sci. Data, 4, 167–186, 2012 Earth System Earth System www.earth-syst-sci-data.net/4/167/2012/ Science Science doi:10.5194/essd-4-167-2012 © Author(s) 2012. CC Attribution 3.0 License. Access Open Open Access Open Data Data Discussions Social Social Open Access Open Geography Open Access Open Geography The global distribution of pteropods and their contribution to carbonate and carbon biomass in the modern ocean N. Bednarsekˇ 1, J. Mozinaˇ 2, M. Vogt3, C. O’Brien3, and G. A. Tarling4 1NOAA Pacific Marine Environmental Laboratory, 7600 Sand Point Way NE, Seattle, WA 98115, USA 2University of Nova Gorica, Laboratory for Environmental Research, Vipavska 13, Roznaˇ Dolina, 5000 Nova Gorica, Slovenia 3Institute for Biogeochemistry and Pollutant Dynamics, ETH Zurich,¨ Universitaetstrasse 16, 8092 Zurich,¨ Switzerland 4British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge CB3 0ET, UK Correspondence to: N. Bednarsekˇ ([email protected]) Received: 20 March 2012 – Published in Earth Syst. Sci. Data Discuss.: 10 May 2012 Revised: 8 October 2012 – Accepted: 19 October 2012 – Published: 10 December 2012 Abstract. Pteropods are a group of holoplanktonic gastropods for which global biomass distribution patterns remain poorly described. The aim of this study was to collect and synthesise existing pteropod (Gymnosomata, Thecosomata and Pseudothecosomata) abundance and biomass data, in order to evaluate the global distribu- tion of pteropod carbon biomass, with a particular emphasis on temporal and spatial patterns. -
オホーツク海沿岸における Clione Limacina および Limacina Helicina の出現時期
オホーツク海沿岸における Clione limacina および Limacina helicina の出現時期 片倉 靖次・濱岡 莊司 紋別市役所 Occurrence and abundance of Clione limacina and Limacina helicina in coastal waters at Mombetsu in the Okhotsk Sea Seiji Katakura and Soshi Hamaoka City of Mombetsu ABSTRACT The occurrence and abundance of Clione limacina and Limacina helicina in coastal waters at Mombetsu, Hokkaido, in the Okhotsk Sea were examined over a sixteen year period 1997-2012. Plankton samples were vertically hauled from the bottom to the surface (9-0m) with a NORPAC Net (335μm mesh) near the Okhotsk Tower. Samples were collected nearly on daily basis in the morning from 13 April 1997 to 31 December 2012. Water temperatures and salinity were measured by CTD. The water was tentatively divided by salinity into three types: i.e. Okhotsk surface water (< 32.5psu), coastal water (32.5-33.6psu) and Soya warm water (33.6psu<), according to Takizawa (1982). Both species occurred throughout the year except in late summer and autumn. The season of high abundance differed between the two species and by their developmental stage. The veliger larvae of C. limacina were observed from November through the following July with high densities in December and July. The polytrochous larvae of C. limacina were observed from October through August with high densities in June. The adults of C. limacina appeared from December through April with high densities in February. L. helicina appeared throughout the year, with two high densities in November and June. A positive correlation was found in the abundance between L. helicina and polytrochous larvae of C.