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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Clough, Lisa; Ambrose, William G Jr; Cochran, James R; Barnes, C; Renaud, Paul E; Aller, Robert C (1997): Infaunal density, biomass and bioturbation in the sediments of the Arctic Ocean. Deep Sea Research Part II: Topical Studies in Oceanography, 44(8), 1683-1704, https://doi.org/10.1016/S0967-0645(97)00052-0
    Publication Date: 2023-09-19
    Description: Little is known about the benthic communities of the Arctic Ocean's slope and abyssal plains. Here we report on benthic data collected from box cores along a transect from Alaska to the Barents Abyssal Plain during the Arctic Ocean Section of 1994. We determined: (1) density and biomass of the polychaetes, foraminifera and total infauna; (2) concentrations of potential sources of food (pigment concentration and percent organic carbon) in the sediments; (3) surficial particle mixing depths and rates using downcore 210Pb profiles; and (4) surficial porewater irrigation using NaBr as an inert tracer. Metazoan density and biomass vary by almost three orders of magnitude from the shelf to the deep basins (e.g. 47 403 individuals m**-2 on the Chukchi Shelf to 95 individuals m**-2 in the Barents Abyssal Plain). Water depth is the primary determinant of infaunal density, explaining 39% of the total variability. Potential food concentration varies by almost two orders of magnitude during the late summer season (e.g. the phaeopigment concentration integrated to 10 cm varies from 36.16 mg m**-2 on the Chukchi Shelf to 0.94 mg m**-2 in the Siberia Abyssal Plain) but is not significantly correlated with density or biomass of the metazoa. Most stations show evidence of particle mixing, with mixing limited to 〈=3 cm below the sediment-water interface, and enhanced pore water irrigation occurs at seven of the nine stations examined. Particle mixing depths may be related to metazoan biomass, while enhanced pore water irrigation (beyond what is expected from diffusion alone) appears to be related to total phaeopigment concentration. The data presented here indicate that Arctic benthic ecosystems are quite variable, but all stations sampled contained infauna and most stations had indications of active processing of the sediment by the associated infauna.
    Keywords: ADEPD; ADEPDCruises; AOS94_1; AOS94_12; AOS94_13; AOS94_16; AOS94_17; AOS94_19; AOS94_21; AOS94_23; AOS94_24; AOS94_25; AOS94_26; AOS94_28; AOS94_30; AOS94_31; AOS94_32; AOS94_33; AOS94_6; AOS94_7; AOS94_8; Arlis Plateau; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Barents abyssal plain; BC; Box corer; Chukchi Abyssal Plain; Chukchi shelf; Chukchi solpe; Lomonosov Ridge, Arctic Ocean; Mendeleev Ridge, Arctic Ocean; Mendeleev slope; North Pole; Siberia Abyssal Plain; Wrangel Abyssal Plain
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-09-19
    Keywords: ADEPD; ADEPDCruises; AOS94_1; AOS94_13; AOS94_16; AOS94_17; AOS94_19; AOS94_21; AOS94_23; AOS94_24; AOS94_25; AOS94_26; AOS94_28; AOS94_30; AOS94_31; AOS94_32; AOS94_33; AOS94_6; AOS94_7; AOS94_8; Arlis Plateau; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Barents abyssal plain; BC; Box corer; Chukchi Abyssal Plain; Chukchi shelf; Chukchi solpe; DEPTH, sediment/rock; Elevation of event; Event label; Latitude of event; Lomonosov Ridge, Arctic Ocean; Longitude of event; Mendeleev Ridge, Arctic Ocean; Mendeleev slope; Mixing, enhanced irrigation; Mixing depth; Mixing rate; Mode, grain size; North Pole; Porosity; Siberia Abyssal Plain; Wrangel Abyssal Plain
    Type: Dataset
    Format: text/tab-separated-values, 83 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-09-19
    Keywords: ADEPD; ADEPDCruises; AOS94_1; AOS94_12; AOS94_13; AOS94_16; AOS94_17; AOS94_19; AOS94_21; AOS94_23; AOS94_24; AOS94_25; AOS94_26; AOS94_28; AOS94_30; AOS94_31; AOS94_32; AOS94_33; AOS94_6; AOS94_7; AOS94_8; Arlis Plateau; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Barents abyssal plain; BC; Box corer; Chukchi Abyssal Plain; Chukchi shelf; Chukchi solpe; Counting 〉250 µm fraction; DEPTH, sediment/rock; Event label; Foraminifera, benthic; Foraminifera, benthic, biomass as carbon; Infauna; Infauna, biomass as carbon; Lomonosov Ridge, Arctic Ocean; Meiofauna, abundance of metazoa; Meiofauna, metazoa, biomass as carbon; Mendeleev Ridge, Arctic Ocean; Mendeleev slope; North Pole; Polychaeta; Polychaeta, biomass as carbon; Siberia Abyssal Plain; Wrangel Abyssal Plain
    Type: Dataset
    Format: text/tab-separated-values, 150 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-01-08
    Keywords: ADEPD; ADEPDCruises; AOS94_1; AOS94_12; AOS94_13; AOS94_16; AOS94_17; AOS94_19; AOS94_21; AOS94_23; AOS94_24; AOS94_25; AOS94_26; AOS94_28; AOS94_30; AOS94_31; AOS94_32; AOS94_33; AOS94_6; AOS94_7; AOS94_8; Arlis Plateau; Atlantic Data Base for Exchange Processes at the Deep Sea Floor; Barents abyssal plain; BC; Box corer; Calculated; Carbon, organic, total; Chlorophyll a, areal concentration; Chukchi Abyssal Plain; Chukchi shelf; Chukchi solpe; DEPTH, sediment/rock; Element analyser CHN, LECO; Elevation of event; Event label; Fluorometric assay of acetone extraction (GF/F filtered); Latitude of event; Lomonosov Ridge, Arctic Ocean; Longitude of event; Mendeleev Ridge, Arctic Ocean; Mendeleev slope; Mixing depth; North Pole; Phaeopigments, areal concentration; Siberia Abyssal Plain; Wrangel Abyssal Plain
    Type: Dataset
    Format: text/tab-separated-values, 134 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2022-05-25
    Description: Author Posting. © Inter-Research, 2006. This article is posted here by permission of Inter-Research for personal use, not for redistribution. The definitive version was published in Marine Ecology Progress Series 310 (2006): 1-14, doi:10.3354/meps310001.
    Description: We assessed the digestibility and utilization of ice algae and phytoplankton by the shallow, subtidal benthos in Ny Ålesund (Kongsfjord) on Svalbard (79°N, 12°E) using chlorophyll a (chl a), essential fatty acids (EFAs) and stable isotopes as tracers of food consumption and assimilation. Intact benthic communities in sediment cores and individuals of dominant benthic taxa were given ice algae, phytoplankton, 13C-enriched ice algae or a no food addition control for 19 to 32 d. Ice algae and phytoplankton had significantly different isotopic signatures and relative concentrations of fatty acids. In the food addition cores, sediment concentrations of chl a and the EFA C20:5(n-3) were elevated by 80 and 93%, respectively, compared to the control after 12 h, but decreased to background levels by 19 d, suggesting that both ice algae and phytoplankton were rapidly consumed. Whole core respiration rates in the ice algae treatments were 1.4 times greater than in the other treatments within 12 h of food addition. In the ice algae treatment, both suspension and deposit feeding taxa from 3 different phyla (Mollusca, Annelida and Sipuncula) exhibited significant enrichment in δ13C values compared to the control. Deposit feeders (15% uptake), however, exhibited significantly greater uptake of the 13C-enriched ice algae tracer than suspension feeders (3% uptake). Our study demonstrates that ice algae are readily consumed and assimilated by the Arctic benthos, and may be preferentially selected by some benthic species (i.e. deposit feeders) due to their elevated EFA content, thus serving as an important component of the Arctic benthic food web.
    Description: Funding for this study came from the National Science Foundation (Grant numbers OPP- 0514115 to W.G.A.; OPP-0222410 to L.M.C.; OPP-0222408 to M.-Y.S.; OPP0222500 to G.R.L.), the Norwegian Research Council (Grant number 151815-720 to M.L.C.), the Howard Hughes Medical Institute through Bates College and the Maine Marine Research Fund.
    Keywords: Ice algae ; Phytoplankton ; Food quality ; Arctic benthos ; Climate change ; Stable isotopes ; Essential fatty acids ; Svalbard
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 6
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    Unknown
    In:  http://aquaticcommons.org/id/eprint/9645 | 403 | 2012-08-13 16:11:00 | 9645 | United States National Marine Fisheries Service
    Publication Date: 2021-07-08
    Description: Seasonal and cross-shelf patterns were investigated in larval fish assemblages on the continental shelf off the coast of Georgia. The influence of environmental factors onlarval distributions also was examined, and larval transport processes on the shelf were considered. Ichthyoplankton and environmental data were collected approximately every other month from spring 2000 to winter2002. Ten stations were repeatedly sampled along a 110-km cross-shelf transect, including four stations in the vicinity of Gray’s Reef National Marine Sanctuary. Correspondence analysis (CA) on untransformed communitydata identified two seasonal (warm weather [spring, summer, and fall] and winter) and three cross-shelf larval assemblages (inner-, mid-, and outer-shelf ). Five environmental factors (temperature, salinity, density,depth of the water column, and stratification) were related to larval cross-shelf distribution. Specifically,increased water column stratification was associated with the outer-shelf assemblage in spring, summer, and fall. The inner shelf assemblage was associated with generally lower temperatures and lower salinities in the spring and summer and higher salinities in the winter. The three cross-shelfregions indicated by the three assemblages coincided with the location of three primary water masses on the shelf. However, taxa occurring together within an assemblage weretransported to different parts of the shelf; thus, transport across the continental shelf off the coast of Georgia cannot be explained solely by twodimensionalphysical factors.
    Keywords: Biology ; Ecology ; Fisheries
    Repository Name: AquaDocs
    Type: article , TRUE
    Format: application/pdf
    Format: application/pdf
    Format: 108-129
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