Observations on the Gymnosomatous Pteropod Clione Limacina (Phipps)
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Metabolic Response of Antarctic Pteropods (Mollusca: Gastropoda) to Food Deprivation and Regional Productivity
Vol. 441: 129–139, 2011 MARINE ECOLOGY PROGRESS SERIES Published November 15 doi: 10.3354/meps09358 Mar Ecol Prog Ser Metabolic response of Antarctic pteropods (Mollusca: Gastropoda) to food deprivation and regional productivity Amy E. Maas1,*, Leanne E. Elder1, Heidi M. Dierssen2, Brad A. Seibel1 1Department of Biological Sciences, University of Rhode Island, Kingston, Rhode Island 02881, USA 2Department of Marine Sciences, University of Connecticut, Groton, Connecticut 06340, USA ABSTRACT: Pteropods are an abundant group of pelagic gastropods that, although temporally and spatially patchy in the Southern Ocean, can play an important role in food webs and biochem- ical cycles. We found that the metabolic rate in Limacina helicina antarctica is depressed (~23%) at lower mean chlorophyll a (chl a) concentrations in the Ross Sea. To assess the specific impact of food deprivation on these animals, we quantified aerobic respiration and ammonia (NH3) produc- tion for 2 dominant Antarctic pteropods, L. helicina antarctica and Clione limacina antarctica. Pteropods collected from sites west of Ross Island, Antarctica were held in captivity for a period of 1 to 13 d to determine their metabolic response to laboratory-induced food deprivation. L. helicina antarctica reduced oxygen consumption by ~20% after 4 d in captivity. Ammonia excretion was not significantly affected, suggesting a greater reliance on protein as a substrate for cellular res- piration during starvation. The oxygen consumption rate of the gymnosome, C. li macina antarc- tica, was reduced by ~35% and NH3 excretion by ~55% after 4 d without prey. Our results indi- cate that there is a link between the large scale chl a concentrations of the Ross Sea and the baseline metabolic rate of pteropods which impacts these animals across multiple seasons. -
Life Cycle and Early Development of the Thecosomatous Pteropod Limacina Retroversa in the Gulf of Maine, Including the Effect of Elevated CO2 Levels
Life cycle and early development of the thecosomatous pteropod Limacina retroversa in the Gulf of Maine, including the effect of elevated CO2 levels Ali A. Thabetab, Amy E. Maasac*, Gareth L. Lawsona and Ann M. Tarranta a. Biology Department, Woods Hole Oceanographic Institution, Woods Hole, MA 02543 b. Zoology Dept., Faculty of Science, Al-Azhar University in Assiut, Assiut, Egypt. c. Bermuda Institute of Ocean Sciences, St. George’s GE01, Bermuda *Corresponding Author, equal contribution with lead author Email: [email protected] Phone: 441-297-1880 x131 Keywords: mollusc, ocean acidification, calcification, mortality, developmental delay Abstract Thecosome pteropods are pelagic molluscs with aragonitic shells. They are considered to be especially vulnerable among plankton to ocean acidification (OA), but to recognize changes due to anthropogenic forcing a baseline understanding of their life history is needed. In the present study, adult Limacina retroversa were collected on five cruises from multiple sites in the Gulf of Maine (between 42° 22.1’–42° 0.0’ N and 69° 42.6’–70° 15.4’ W; water depths of ca. 45–260 m) from October 2013−November 2014. They were maintained in the laboratory under continuous light at 8° C. There was evidence of year-round reproduction and an individual life span in the laboratory of 6 months. Eggs laid in captivity were observed throughout development. Hatching occurred after 3 days, the veliger stage was reached after 6−7 days, and metamorphosis to the juvenile stage was after ~ 1 month. Reproductive individuals were first observed after 3 months. Calcein staining of embryos revealed calcium storage beginning in the late gastrula stage. -
2015 Annual Report of a Comprehensive Assessment of Marine Mammal, Marine Turtle, and Seabird Abundance and Spatial Distribution
2015 Annual Report of a Comprehensive Assessment of Marine Mammal, Marine Turtle, and Seabird Abundance and Spatial Distribution in US Waters of the Western North Atlantic Ocean – AMAPPS II Short-beaked common dolphin (Delphinus delphis) Collected under MMPA Research permit #775-1875 Photo credit: NOAA/NEFSC/Allison Henry Northeast Fisheries Science Center 166 Water St. Woods Hole, MA 02543 Southeast Fisheries Science Center 75 Virginia Beach Dr. Miami, FL 33149 2015 Annual Report to A Comprehensive Assessment of Marine Mammal, Marine Turtle, and Seabird Abundance and Spatial Distribution in US Waters of the western North Atlantic Ocean – AMAPPS II Table of Contents BACKGROUND ........................................................................................................................... 3 SUMMARY OF 2015 ACTIVITIES ........................................................................................... 3 Appendix A: Northern leg of aerial abundance survey during December 2014 – January 2015: Northeast Fisheries Science Center .............................................................................................. 11 Appendix B: Southern leg of aerial abundance survey during January - March 2015: Southeast Fisheries Science Center ............................................................................................................... 21 Appendix C: Gray seal live capture, biological sampling, and tagging on Monomoy National Wildlife Refuge and Muskeget Island, January 2015: Northeast Fisheries Science Center -
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. -
The 17Th International Colloquium on Amphipoda
Biodiversity Journal, 2017, 8 (2): 391–394 MONOGRAPH The 17th International Colloquium on Amphipoda Sabrina Lo Brutto1,2,*, Eugenia Schimmenti1 & Davide Iaciofano1 1Dept. STEBICEF, Section of Animal Biology, via Archirafi 18, Palermo, University of Palermo, Italy 2Museum of Zoology “Doderlein”, SIMUA, via Archirafi 16, University of Palermo, Italy *Corresponding author, email: [email protected] th th ABSTRACT The 17 International Colloquium on Amphipoda (17 ICA) has been organized by the University of Palermo (Sicily, Italy), and took place in Trapani, 4-7 September 2017. All the contributions have been published in the present monograph and include a wide range of topics. KEY WORDS International Colloquium on Amphipoda; ICA; Amphipoda. Received 30.04.2017; accepted 31.05.2017; printed 30.06.2017 Proceedings of the 17th International Colloquium on Amphipoda (17th ICA), September 4th-7th 2017, Trapani (Italy) The first International Colloquium on Amphi- Poland, Turkey, Norway, Brazil and Canada within poda was held in Verona in 1969, as a simple meet- the Scientific Committee: ing of specialists interested in the Systematics of Sabrina Lo Brutto (Coordinator) - University of Gammarus and Niphargus. Palermo, Italy Now, after 48 years, the Colloquium reached the Elvira De Matthaeis - University La Sapienza, 17th edition, held at the “Polo Territoriale della Italy Provincia di Trapani”, a site of the University of Felicita Scapini - University of Firenze, Italy Palermo, in Italy; and for the second time in Sicily Alberto Ugolini - University of Firenze, Italy (Lo Brutto et al., 2013). Maria Beatrice Scipione - Stazione Zoologica The Organizing and Scientific Committees were Anton Dohrn, Italy composed by people from different countries. -
An Overview of the Fossil Record of Pteropoda (Mollusca, Gastropoda, Heterobranchia)
Cainozoic Research, 17(1), pp. 3-10 June 2017 3 An overview of the fossil record of Pteropoda (Mollusca, Gastropoda, Heterobranchia) Arie W. Janssen1 & Katja T.C.A. Peijnenburg2, 3 1 Naturalis Biodiversity Center, Marine Biodiversity, Fossil Mollusca, P.O. Box 9517, 2300 RA Leiden, The Nether lands; [email protected] 2 Naturalis Biodiversity Center, Marine Biodiversity, P.O. Box 9517, 2300 RA Leiden, The Netherlands; Katja.Peijnen [email protected] 3 Institute for Biodiversity and Ecosystem Dynamics (IBED), University of Amsterdam, P.O. Box 94248, 1090 GE Am sterdam, The Netherlands. Manuscript received 23 January 2017, revised version accepted 14 March 2017 Based on the literature and on a massive collection of material, the fossil record of the Pteropoda, an important group of heterobranch marine, holoplanktic gastropods occurring from the late Cretaceous onwards, is broadly outlined. The vertical distribution of genera is illustrated in a range chart. KEY WORDS: Pteropoda, Euthecosomata, Pseudothecosomata, Gymnosomata, fossil record Introduction Thecosomata Mesozoic Much current research focusses on holoplanktic gastro- pods, in particular on the shelled pteropods since they The sister group of pteropods is now considered to belong are proposed as potential bioindicators of the effects of to Anaspidea, a group of heterobranch gastropods, based ocean acidification e.g.( Bednaršek et al., 2016). This on molecular evidence (Klussmann-Kolb & Dinapoli, has also led to increased interest in delimiting spe- 2006; Zapata et al., 2014). The first known species of cies boundaries and distribution patterns of pteropods pteropods in the fossil record belong to the Limacinidae, (e.g. Maas et al., 2013; Burridge et al., 2015; 2016a) and are characterised by sinistrally coiled, aragonitic and resolving their evolutionary history using molecu- shells. -
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. -
Genetic Population Structure of the Pelagic Mollusk Limacina Helicina in the Kara Sea
Genetic population structure of the pelagic mollusk Limacina helicina in the Kara Sea Galina Anatolievna Abyzova1, Mikhail Aleksandrovich Nikitin2, Olga Vladimirovna Popova2 and Anna Fedorovna Pasternak1 1 Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia 2 Belozersky Institute for Physico-Chemical Biology, Lomonosov Moscow State University, Moscow, Russia ABSTRACT Background. Pelagic pteropods Limacina helicina are widespread and can play an important role in the food webs and in biosedimentation in Arctic and Subarctic ecosystems. Previous publications have shown differences in the genetic structure of populations of L. helicina from populations found in the Pacific Ocean and Svalbard area. Currently, there are no data on the genetic structure of L. helicina populations in the seas of the Siberian Arctic. We assessed the genetic structure of L. helicina from the Kara Sea populations and compared them with samples from around Svalbard and the North Pacific. Methods. We examined genetic differences in L. helicina from three different locations in the Kara Sea via analysis of a fragment of the mitochondrial gene COI. We also compared a subset of samples with L. helicina from previous studies to find connections between populations from the Atlantic and Pacific Oceans. Results. 65 individual L. helinica from the Kara Sea were sequenced to produce 19 different haplotypes. This is comparable with numbers of haplotypes found in Svalbard and Pacific samples (24 and 25, respectively). Haplotypes from different locations sampled around the Arctic and Subarctic were combined into two different groups: H1 and H2. The H2 includes sequences from the Kara Sea and Svalbard, was present only in the Atlantic sector of the Arctic. -
Gastropoda: Opisthobranchia)
University of New Hampshire University of New Hampshire Scholars' Repository Doctoral Dissertations Student Scholarship Fall 1977 A MONOGRAPHIC STUDY OF THE NEW ENGLAND CORYPHELLIDAE (GASTROPODA: OPISTHOBRANCHIA) ALAN MITCHELL KUZIRIAN Follow this and additional works at: https://scholars.unh.edu/dissertation Recommended Citation KUZIRIAN, ALAN MITCHELL, "A MONOGRAPHIC STUDY OF THE NEW ENGLAND CORYPHELLIDAE (GASTROPODA: OPISTHOBRANCHIA)" (1977). Doctoral Dissertations. 1169. https://scholars.unh.edu/dissertation/1169 This Dissertation is brought to you for free and open access by the Student Scholarship at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. INFORMATION TO USERS This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1.The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image. -
Outer Organic Layer and Internal Repair Mechanism Protects Pteropod Limacina Helicina from Ocean Acidification
Outer organic layer and internal repair mechanism protects pteropod Limacina helicina from ocean acidification Victoria L Peck1, Geraint A Tarling1, Clara Manno1, Elizabeth M Harper2, Eithne Tynan3. 1. British Antarctic Survey, High Cross, Madingley Rd, Cambridge, CB5 8NP, UK 2. Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK 3. Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK Scarred shells of polar pteropod Limacina helicina collected from the Greenland Sea in June 2012 reveal a history of damage, most likely failed predation, in earlier life stages. Evidence of shell fracture and subsequent re-growth is commonly observed in specimens recovered from the sub-Arctic and further afield. However, at one site within sea-ice on the Greenland shelf, shells that had been subject to mechanical damage were also found to exhibit considerable dissolution. It was evident that shell dissolution was localised to areas where the organic, periostracal sheet that covers the outer shell had been damaged at some earlier stage during the animal’s life. Where the periostracum remained intact, the shell appeared pristine with no sign of dissolution. Specimens which appeared to be pristine following collection were incubated for four days. Scarring of shells that received periostracal damage during collection only became evident in specimens that were incubated in waters undersaturated with respect to aragonite, Ar≤1. While the waters from which the damaged specimens were collected at the Greenland Sea sea-ice margin were not Ar ≤1, the water column did exhibit the lowest Ar values observed in the Greenland and Barents Seas, and was likely to have approachedAr≤1 during the winter months. -
Gastropoda, Pteropoda
BASTERIA 38: 19-26, 1974 Notes the adult and in Diacria on young stages (Gastropoda, Pteropoda) W.L. Panhorst & S. van der Spoel Institute of Taxonomic Zoology (Zoologisch Museum), Amsterdam INTRODUCTION The adults and minute stages of the Cavoliniidae as described earlier (Van der Spoel, 1967) have been distinguished chiefly by studying their soft parts; only a few notes were made on differences in the shells of young and older specimens (Van der Spoel, 1970). A large collection of 1 Diacria, made during the Ocean Acre Program in the Bermuda area, made possible a more careful study of their shells. Concerning the two forms in D. trispinosa, the second author (Van der Spoel, 1967: 84) stated ". both formae are sometimes collected in one and the same The rank to them is too low ." and sample. systematic given perhaps . (Van der Spoel, 1970: 105) "the largest specimens", of the forma trispinosa, "which are as long as tropical specimens of the closely related and larger forma major”. The differences between the two taxa forma are evidently small, but the rank is clearly too low as both are sympatric in space and time. This also implicates that we are not dealing with subspecies so that one is forced to consider both taxa of separate species. That two morphs of one species are present instead two species seems impossible as both show considerable geographic variation. Originally described as varieties (Boas, 1886) or subspecies (Tesch, 1913), and later considered formae (Van der Spoel, 1967), the two taxa now have to be considered distinct species: Diacria trispinosa (De Blainville, 1821) and Diacria major (Boas, 1886).