MOLLUSCA Nudibranchs, Pteropods, Gastropods, Bivalves, Chitons, Octopus
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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. -
Trophic Interactions Within the Ross Sea Continental Shelf Ecosystem Walker O
Phil. Trans. R. Soc. B (2007) 362, 95–111 doi:10.1098/rstb.2006.1956 Published online 6 December 2006 Trophic interactions within the Ross Sea continental shelf ecosystem Walker O. Smith Jr1,*, David G. Ainley2 and Riccardo Cattaneo-Vietti3 1Virginia Institute of Marine Sciences, College of William and Mary, Gloucester Point, VA 23062, USA 2H.T. Harvey and Associates, 3150 Almaden Expressway, Suite 145, San Jose, CA 95118, USA 3Dipartimento per lo Studio del Territorio e delle sue Risorse, Universita` di Genova, Corso Europa 26, 16132 Genova, Italy The continental shelf of the Ross Sea is one of the Antarctic’s most intensively studied regions. We review the available data on the region’s physical characteristics (currents and ice concentrations) and their spatial variations, as well as components of the neritic food web, including lower and middle levels (phytoplankton, zooplankton, krill, fishes), the upper trophic levels (seals, penguins, pelagic birds, whales) and benthic fauna. A hypothetical food web is presented. Biotic interactions, such as the role of Euphausia crystallorophias and Pleuragramma antarcticum as grazers of lower levels and food for higher trophic levels, are suggested as being critical. The neritic food web contrasts dramatically with others in the Antarctic that appear to be structured around the keystone species Euphausia superba. Similarly, we suggest that benthic–pelagic coupling is stronger in the Ross Sea than in most other Antarctic regions. We also highlight many of the unknowns within the food web, and discuss the impacts of a changing Ross Sea habitat on the ecosystem. Keywords: Ross Sea; neritic food web; bio-physical coupling; ecosystem function; ecosystem structure; pelagic–benthic coupling 1. -
Taxonomy and Diversity of the Sponge Fauna from Walters Shoal, a Shallow Seamount in the Western Indian Ocean Region
Taxonomy and diversity of the sponge fauna from Walters Shoal, a shallow seamount in the Western Indian Ocean region By Robyn Pauline Payne A thesis submitted in partial fulfilment of the requirements for the degree of Magister Scientiae in the Department of Biodiversity and Conservation Biology, University of the Western Cape. Supervisors: Dr Toufiek Samaai Prof. Mark J. Gibbons Dr Wayne K. Florence The financial assistance of the National Research Foundation (NRF) towards this research is hereby acknowledged. Opinions expressed and conclusions arrived at, are those of the author and are not necessarily to be attributed to the NRF. December 2015 Taxonomy and diversity of the sponge fauna from Walters Shoal, a shallow seamount in the Western Indian Ocean region Robyn Pauline Payne Keywords Indian Ocean Seamount Walters Shoal Sponges Taxonomy Systematics Diversity Biogeography ii Abstract Taxonomy and diversity of the sponge fauna from Walters Shoal, a shallow seamount in the Western Indian Ocean region R. P. Payne MSc Thesis, Department of Biodiversity and Conservation Biology, University of the Western Cape. Seamounts are poorly understood ubiquitous undersea features, with less than 4% sampled for scientific purposes globally. Consequently, the fauna associated with seamounts in the Indian Ocean remains largely unknown, with less than 300 species recorded. One such feature within this region is Walters Shoal, a shallow seamount located on the South Madagascar Ridge, which is situated approximately 400 nautical miles south of Madagascar and 600 nautical miles east of South Africa. Even though it penetrates the euphotic zone (summit is 15 m below the sea surface) and is protected by the Southern Indian Ocean Deep- Sea Fishers Association, there is a paucity of biodiversity and oceanographic data. -
Supplementary Tales
Metabarcoding reveals different zooplankton communities in northern and southern areas of the North Sea Jan Niklas Macher, Berry B. van der Hoorn, Katja T. C. A. Peijnenburg, Lodewijk van Walraven, Willem Renema Supplementary tables 1-5 Table S1: Sampling stations and recorded abiotic variables recorded during the NICO 10 expedition from the Dutch Coast to the Shetland Islands Sampling site name Coordinates (°N, °E) Mean remperature (°C) Mean salinity (PSU) Depth (m) S74 59.416510, 0.499900 8.2 35.1 134 S37 58.1855556, 0.5016667 8.7 35.1 89 S93 57.36046, 0.57784 7.8 34.8 84 S22 56.5866667, 0.6905556 8.3 34.9 220 S109 56.06489, 1.59652 8.7 35 79 S130 55.62157, 2.38651 7.8 34.8 73 S156 54.88581, 3.69192 8.3 34.6 41 S176 54.41489, 4.04154 9.6 34.6 43 S203 53.76851, 4.76715 11.8 34.5 34 Table S2: Species list and read number per sampling site Class Order Family Genus Species S22 S37 S74 S93 S109 S130 S156 S176 S203 Copepoda Calanoida Acartiidae Acartia Acartia clausi 0 0 0 72 0 170 15 630 3995 Copepoda Calanoida Acartiidae Acartia Acartia tonsa 0 0 0 0 0 0 0 0 23 Hydrozoa Trachymedusae Rhopalonematidae Aglantha Aglantha digitale 0 0 0 0 1870 117 420 629 0 Actinopterygii Trachiniformes Ammodytidae Ammodytes Ammodytes marinus 0 0 0 0 0 263 0 35 0 Copepoda Harpacticoida Miraciidae Amphiascopsis Amphiascopsis cinctus 344 0 0 992 2477 2500 9574 8947 0 Ophiuroidea Amphilepidida Amphiuridae Amphiura Amphiura filiformis 0 0 0 0 219 0 0 1470 63233 Copepoda Calanoida Pontellidae Anomalocera Anomalocera patersoni 0 0 586 0 0 0 0 0 0 Bivalvia Venerida -
Marc Slattery University of Mississippi Department of Pharmacognosy School of Pharmacy Oxford, MS 38677-1848 (662) 915-1053 [email protected]
Marc Slattery University of Mississippi Department of Pharmacognosy School of Pharmacy Oxford, MS 38677-1848 (662) 915-1053 [email protected] EDUCATION: Ph.D. Biological Sciences. University of Alabama at Birmingham (1994); Doctoral Dissertation: A comparative study of population structure and chemical defenses in the soft corals Alcyonium paessleri May, Clavularia frankliniana Roule, and Gersemia antarctica Kukenthal in McMurdo Sound, Antarctica. M.A. Marine Biology. San Jose State University at the Moss Landing Marine Laboratories (1987); Masters Thesis: Settlement and metamorphosis of red abalone (Haliotis rufescens) larvae: A critical examination of mucus, diatoms, and γ-aminobutyric acid (GABA) as inductive substrates. B.S. Biology. Loyola Marymount University (1981); Senior Thesis: The ecology of sympatric species of octopuses (Octopus fitchi and O. diguetti) at Coloraditos, Baja Ca. RESEARCH INTERESTS: Chemical defenses/natural products chemistry of marine & freshwater invertebrates, and microbes. Evolutionary ecology, and ecophysiological adaptations of organisms in aquatic communities; including coral reef, cave, sea grass, kelp forest, and polar ecosystems. Chemical signals in reproductive biology and larval ecology/recruitment, and their applications to aquaculture and biomedical sciences. Cnidarian, Sponge, Molluscan, and Echinoderm biology/ecology, population structure, symbioses and photobiological adaptations. Marine microbe competition and culture. Environmental toxicology. EMPLOYMENT: Professor of Pharmacognosy and -
Antarctic Sessile Marine Benthos: Colonisation and Growth on Artificial Substrata Over Three Years
MARINE ECOLOGY PROGRESS SERIES Vol. 316: 1–16, 2006 Published July 3 Mar Ecol Prog Ser OPENPEN ACCESSCCESS FEATURE ARTICLE Antarctic sessile marine benthos: colonisation and growth on artificial substrata over three years David A. Bowden*, Andrew Clarke, Lloyd S. Peck, David K. A. Barnes Natural Environment Research Council, British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK ABSTRACT: The development of sessile invertebrate assemblages on hard substrata has been studied exten- sively in temperate and tropical latitudes. Such studies provide insights into a range of ecological processes, and the global similarity of taxa recruiting to these assem- blages affords the potential for regional-scale com- parisons. However, few data exist for high latitude assemblages. This paper presents the first regularly resur- veyed study of benthic colonisation from within the Antarctic Circle. Acrylic panels were deployed horizon- tally on the seabed at 8 and 20 m depths at each of 3 loca- tions in Ryder Bay, Adelaide Island, SW Antarctic Peninsula (67° 35’ S, 68° 10’ W). Assemblages colonising upward- and downward-facing panel surfaces were photographed in situ from February 2001 to March 2004. Assemblages were dominated by bryozoans and spiror- Bowden and co-workers present the first successful benthic bid polychaetes. Total coverage after 3 yr ranged from 6 to colonisation study from within the Antarctic Circle. They 100% on downward-facing surfaces but was <10% on all describe a system governed by extremely slow and highly upward-facing surfaces. Overall colonisation rates were seasonal growth, and a range of post-settlement disturbances in which succession is more predictable than in comparable up to 3 times slower than comparable temperate latitude temperate or tropical assemblages. -
© Terra Antartica Publication Terra Antartica 2001, 8(4), 423-434
© Terra Antartica Publication Terra Antartica 2001, 8(4), 423-434 Palaeogene Macrofossils from CRP-3 Drillhole, Victoria Land Basin, Antarctica M. TAVIANI1* & A.G. BEU2 1Istituto di Geologia Marina, Consiglio Nazionale delle Ricerche, via Gobetti 101, I-40129 Bologna - Italy 2Institute of Geological & Nuclear Sciences, P.O. Box 30 368, Lower Hutt - New Zealand Received 5 March 2001; accepted in revised form 3 July 2001 Abstract - CRP-3 cored Palaeogene strata to 823 metres below the sea floor (mbsf), before passing through Devonian bedrock (Beacon Supergroup) to a depth of 939 mbsf. Palaeogene body fossils have been identified at 239 horizons in the core. The best preserved macrofossils from the core help elucidate the taxonomy, chronology and biogeography of Cenozoic ecosystems of Antarctica, although poor preservation prevents identification to species level in most cases. The lithostratigraphic unit (LSU) of the core top (LSU 1.1) contains an almost monospecific modiolid assemblage, similar to mussel beds recovered in the bottom part of the CRP-2/2A core. These semi-infaunal mussels appear to be conspecific, apparently indicating the same age (Early Oligocene) and environment, i.e., a deep muddy shelf characterized by high turbidity and dysoxic/anoxic bottom conditions (high H2S sediment content). LSU 1.2 contains reasonably diverse assemblages representing inner/middle shelf environments dominated by epifaunal suspension feeders. LSU 2.1 contains low-diversity assemblages of suspension feeders (bivalves, brachiopods and bryzoans), probably indicating inner/middle shelf environments. LSU 3.1 contains assemblages including infaunal and epifaunal suspension feeders (bivalves, including a scallop, ?Adamussium n.sp., and solitary corals) and infaunal deposit-feeders, possibly indicating deposition on a deep muddy shelf. -
Phylum MOLLUSCA Chitons, Bivalves, Sea Snails, Sea Slugs, Octopus, Squid, Tusk Shell
Phylum MOLLUSCA Chitons, bivalves, sea snails, sea slugs, octopus, squid, tusk shell Bruce Marshall, Steve O’Shea with additional input for squid from Neil Bagley, Peter McMillan, Reyn Naylor, Darren Stevens, Di Tracey Phylum Aplacophora In New Zealand, these are worm-like molluscs found in sandy mud. There is no shell. The tiny MOLLUSCA solenogasters have bristle-like spicules over Chitons, bivalves, sea snails, sea almost the whole body, a groove on the underside of the body, and no gills. The more worm-like slugs, octopus, squid, tusk shells caudofoveates have a groove and fewer spicules but have gills. There are 10 species, 8 undescribed. The mollusca is the second most speciose animal Bivalvia phylum in the sea after Arthropoda. The phylum Clams, mussels, oysters, scallops, etc. The shell is name is taken from the Latin (molluscus, soft), in two halves (valves) connected by a ligament and referring to the soft bodies of these creatures, but hinge and anterior and posterior adductor muscles. most species have some kind of protective shell Gills are well-developed and there is no radula. and hence are called shellfish. Some, like sea There are 680 species, 231 undescribed. slugs, have no shell at all. Most molluscs also have a strap-like ribbon of minute teeth — the Scaphopoda radula — inside the mouth, but this characteristic Tusk shells. The body and head are reduced but Molluscan feature is lacking in clams (bivalves) and there is a foot that is used for burrowing in soft some deep-sea finned octopuses. A significant part sediments. The shell is open at both ends, with of the body is muscular, like the adductor muscles the narrow tip just above the sediment surface for and foot of clams and scallops, the head-foot of respiration. -
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. -
Reproductive Success in Antarctic Marine Invertebrates
University of Southampton Research Repository ePrints Soton Copyright © and Moral Rights for this thesis are retained by the author and/or other copyright owners. A copy can be downloaded for personal non-commercial research or study, without prior permission or charge. This thesis cannot be reproduced or quoted extensively from without first obtaining permission in writing from the copyright holder/s. The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the copyright holders. When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given e.g. AUTHOR (year of submission) "Full thesis title", University of Southampton, name of the University School or Department, PhD Thesis, pagination http://eprints.soton.ac.uk UNIVERSITY OF SOUTHAMPTON FACULTY OF SCIENCE School of Ocean and Earth Science Reproductive Success in Antarctic Marine Invertebrates By Laura Joanne Grange (BSc. Hons) Thesis for the degree of Doctor of Philosophy July 2005 Dedicated to my Mum, Dad, Sam and my one and only Mike. UNIVERSITY OF SOUTHAMPTON ABSTRACT FACULTY OF SCIENCE SCHOOL OF OCEAN AND EARTH SCIENCE Doctor of Philosophy REPRODUCTIVE SUCCESS IN ANTARCTIC MARINE INVERTEBRATES By Laura Joanne Grange The nearshore Antarctic marine environment is unique, characterised by low but constant temperatures that contrast with an intense peak in productivity. As a result of this stenothermal environment, energy input has a profound ecological effect. These conditions have developed over several millions of years and have resulted in an animal physiology that is highly stenothermal and sometimes closely coupled with the seasonal food supply, e.g. -
Diel Vertical Distribution Patterns of Zooplankton Along the Western Antarctic Peninsula
W&M ScholarWorks Presentations 10-9-2015 Diel Vertical Distribution Patterns of Zooplankton along the Western Antarctic Peninsula Patricia S. Thibodeau Virginia Institute of Marine Science John A. Conroy Virginia Institute of Marine Science Deborah K. Steinberg Virginia Institute of Marine Science Follow this and additional works at: https://scholarworks.wm.edu/presentations Part of the Environmental Monitoring Commons, Marine Biology Commons, Oceanography Commons, and the Terrestrial and Aquatic Ecology Commons Recommended Citation Thibodeau, Patricia S.; Conroy, John A.; and Steinberg, Deborah K.. "Diel Vertical Distribution Patterns of Zooplankton along the Western Antarctic Peninsula". 10-9-2015. VIMS 75th Anniversary Alumni Research Symposium. This Presentation is brought to you for free and open access by W&M ScholarWorks. It has been accepted for inclusion in Presentations by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. Diel Vertical Distribution Patterns of Zooplankton along the Western Antarctic Peninsula Patricia S. Thibodeau, John A. Conroy & Deborah K. Steinberg Introduction & Objectives Results: vertically migrating zooplankton Conclusions The Western Antarctic Peninsula (WAP) region has undergone significant Metridia gerlachei (copepod) Ostracods • Regardless of near continuous light in austral summer, some zooplankton warming and decrease in sea ice cover over the past several decades species still undergo DVM along the WAP. This is supported by one other (Ducklow et al. 2013). The ongoing Palmer Antarctica Long-Term Ecological North North study (Marrari et al., 2011) for a location in Marguerite Bay. Research (PAL LTER) study indicates these environmental changes are • The strength of DVM differed along a latitudinal gradient with some species affecting the WAP marine pelagic ecosystem, including long-term and spatial showing stronger migration in the north (e.g., krill) and some in the south shifts in relative abundances of some dominant zooplankton (Ross et al.