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  • 1
    Publication Date: 2023-01-13
    Keywords: 3175MB93; 3175MB93/10-12; 3175MB93/12-15; 3175MB93/14-17; 3175MB93/16-19; 3175MB93/18-21; 3175MB93/20-23; 3175MB93/22-26; 3175MB93/2-3; 3175MB93/23-27; 3175MB93/24-28; 3175MB93/25-29; 3175MB93/26-30; 3175MB93/27-31; 3175MB93/28-33; 3175MB93/29-35; 3175MB93/30-38; 3175MB93/31-39; 3175MB93/34-42; 3175MB93/35-43; 3175MB93/37-44; 3175MB93/37-45; 3175MB93/38-46; 3175MB93/39-47; 3175MB93/40-48; 3175MB93/41-49; 3175MB93/42-50; 3175MB93/43-52; 3175MB93/44-53; 3175MB93/45-54; 3175MB93/4-6; 3175MB93/46-55; 3175MB93/47-56; 3175MB93/48-57; 3175MB93/49-58; 3175MB93/50-59; 3175MB93/52-61; 3175MB93/53-62; 3175MB93/58-67; 3175MB93/60-69; 3175MB93/64-73; 3175MB93/6-8; 3175MB93/68-78; 3175MB93/70-80; 3175MB93/73-83; 3175MB93/74-84; 3175MB93/75-85; 3175MB93/76-86; 3175MB93/77-87; 3175MB93/78-88; 3175MB93/80-90; 3175MB93/8-10; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Event label; Flow cytometry; Latitude of event; Longitude of event; Malcolm Baldrige; Prokaryotes
    Type: Dataset
    Format: text/tab-separated-values, 141 data points
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  • 2
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    Unknown
    PANGAEA
    Publication Date: 2023-01-13
    Keywords: 3175MB95_07; 3175MB95_07/223; 3175MB95_07/224; 3175MB95_07/228; 3175MB95_07/230; 3175MB95_07/233; 3175MB95_07/237; 3175MB95_07/240; 3175MB95_07/242; 3175MB95_07/247; 3175MB95_07/251; 3175MB95_07/256; 3175MB95_07/259; 3175MB95_07/263; 3175MB95_07/264; 3175MB95_07/265; 3175MB95_07/266; 3175MB95_07/269; 3175MB95_07/270; 3175MB95_07/272; 3175MB95_07/274; 3175MB95_07/278; 3175MB95_07/285; 3175MB95_07/286; 3175MB95_07/290; 3175MB95_07/294; 3175MB95_07/298; 3175MB95_07/303; 3175MB95_07/304; 3175MB95_07/307; 3175MB95_07/313; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Event label; Flow cytometry; Latitude of event; Longitude of event; Malcolm Baldrige; Prokaryotes
    Type: Dataset
    Format: text/tab-separated-values, 109 data points
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  • 3
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    Unknown
    Canadian Science Publishing
    In:  Canadian Journal of Zoology, 69 (4). pp. 1048-1070.
    Publication Date: 2020-07-24
    Description: The morphology and ultrastructure of four species of Cryothecomonas gen.nov. (Protista incertae sedis) in material from the Weddell Sea, Antarctica, and the Isefjord, Denmark, are described. These heterotrophic flagellates, which were initially observed in association with sea ice, display a unique combination of morphological characteristics. At present it is impossible to assign the new genus to an existing higher taxonomic level of protistan flagellates. Cryothecomonas species are furnished with a close-fitting multilayered theca. The two naked anterior flagella emerge through narrow thecal funnels. A transitional helix is part of the flagellar transition zone. A conspicuous cytostome is located in a posterior (lateral) position. Food uptake is mediated through the extension of cytostomal pseudopodia. The nucleus is anteriorly located and contains a conspicuous nucleolus and distinct areas of chromatin. Mitochondrial cristae are tubular. Cryothecomonas species feed on cells in the size range 2–4.5 μm (e.g., algal flagellates). Data are presented on the abundance of Cryothecomonas armigera sp.nov. in Antarctic waters.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract During the spring of 1996 we occupied a station on annual sea ice located several kilometers from Disko Island, West Greenland in water depths greater than 200 m. The goal of this 3-week field season was to characterize sea-ice communities and the underlying water column prior to, and during, ice break-up. A heavier than usual snow load depressed the sea ice below sea level and the snow-ice interface became flooded. Some of this flooded region subsequently refroze and the whole process repeated itself when additional snow accumulated. The infiltration phytoplankton and protozooplankton assemblages that developed in this region were abundant and diverse. Algal biomass in the infiltration layer was approximately an order of magnitude greater than in the underlying water column but an order of magnitude less than in the well-developed bottom ice community. The infiltration autotrophic assemblage resembled the bottom-ice assemblage while the protozooplankton assemblage was more similar to the water column assemblage.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Polar biology 9 (1989), S. 341-351 
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary Protozooplankton were sampled in the iceedge zone of the Weddell Sea during the austral spring of 1983 and the austral autumn of 1986. Protozooplankton biomass was dominated by flagellates and ciliates. Other protozoa and micrometazoa contributed a relatively small fraction to the heterotrophic biomass. During both cruises protozoan biomass, chlorophyll a concentrations, phytoplankton production and bacterial biomass and production were low at ice covered stations. During the spring cruise, protozooplankton, phytoplankton, and bacterioplankton reached high concentrations in a welldeveloped ice edge bloom ∼ 100 km north of the receding ice edge. During the autumn cruise, the highest concentrations of biomass were in open water well-separated from the ice edge. Integrated protozoan biomass was 〈12% of the biomass of phytoplankton during the spring cruise and in the autumn the percentages at some stations were 〉20%. Bacterial biomass exceeded protozooplankton biomass at ice covered stations but in open water stations during the fall cruise, protozooplankton biomass reached twice that of bacteria in the upper 100m of the water column. The biomass of different protozoan groups was positively correlated with primary production, chlorophyll a concentrations and bacterial production and biomass, suggesting that the protozoan abundances were largely controlled by prey availability and productivity. Population grazing rates calculated from clearance rates in the literature indicated that protozooplankton were capable of consuming significant portions of the daily phyto- and bacterioplankton production.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Polar biology 6 (1986), S. 237-239 
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary When ice samples are melted, microorganisms living within the brine inclusions are subjected to rapid and extreme changes in salinities. This procedure results in substantial losses of flagellates and ciliates. Most of these losses can be prevented if ice samples are melted in larger volumes of sterile sea water to buffer salinity and osmotic changes. Since most studies on the ice biota have ignored, or have been unable to avoid this bias, current views of the composition and activity of sea ice communities are based on assemblages over-representing organisms with rigid cell material.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Polar biology 10 (1989), S. 211-219 
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary Pack ice surrounding Antarctica supports rich and varied populations of microbial organisms. As part of the Antarctic Marine Ecosystem Research in the Ice Edge Zone (AMERIEZ) studies, we have examined this community during the late spring, autumn, and winter. Although organisms are found throughout the ice, the richest concentrations often occur in the surface layer. The ice flora consists of diatoms and flagellates. Chrysophyte cysts (archaeomonads) of unknown affinity and dinoflagellate cysts are abundant and may serve as overwintering stages in ice. The ice fauna includes a variety of heterotrophic flagellates, ciliates, and micrometazoa. The abundance of heterotrophs indicates an active food web within the ice community. Ice may serve as a temporary habitat or refuge for many of the microbial forms and some of these appear to provide an inoculum for planktonic populations when ice melts. Larger consumers, such as copepods and the Antarctic krill, Euphausia superba are often found on the underside of ice floes and within weathered floes. The importance of the ice biota as a food resource for these pelagic consumers is unknown.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 306 (1983), S. 363-365 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] We collected samples of young sea ice and samples from the water column along the ice edge during February and March 19809. Ice samples were first melted and then processed as water samples. To estimate algal biomass we measured chlorophyll a of extracted pigments using a fluorometric method; we ...
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 403 (2000), S. 77-80 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] It is generally agreed that the origin and initial diversification of Eucarya occurred in the late Archaean or Proterozoic Eons when atmospheric oxygen levels were low and the risk of DNA damage due to ultraviolet radiation was high. Because deep water provides refuge against ultraviolet ...
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2022-05-25
    Description: Author Posting. © The Authors, 2009. This is the author's version of the work. It is posted here by permission of Blackwell for personal use, not for redistribution. The definitive version was published in Global Change Biology 15 (2009): 2078-2088, doi:10.1111/j.1365-2486.2008.01822.x.
    Description: Sequestration of carbon dioxide (CO2) in the ocean is being considered as a feasible mechanism to mitigate the alarming rate in its atmospheric rise. Little is known, however, about how the resulting hypercapnia and ocean acidification may affect marine fauna. In an effort to understand better the protistan reaction to such an environmental perturbation, the survivorship of benthic foraminifera, which is a prevalent group of protists, was studied in response to deep-sea CO2 release. The survival response of calcareous, agglutinated, and thecate foraminifera was determined in two experiments at ~3.1 and 3.3 km water depth in Monterey Bay (California, USA). Approximately five weeks after initial seafloor CO2 release, in situ incubations of the live-dead indicator CellTracker Green were executed within seafloor-emplaced pushcores. Experimental treatments included direct exposure to CO2 hydrate, two levels of lesser exposure adjacent to CO2 hydrate, and controls, which were far removed from the CO2 hydrate release. Results indicate that survivorship rates of agglutinated and thecate foraminifera were not significantly impacted by direct exposure but the survivorship of calcareous foraminifera was significantly lower in direct exposure treatments compared to controls. Observations suggest that, if large scale CO2 sequestration is enacted on the deep-sea floor, survival of two major groups of this prevalent protistan taxon will likely not be severely impacted, while calcareous foraminifera will face considerable challenges to maintain their benthic populations in areas directly exposed to CO2 hydrate.
    Description: This work was funded by the Monterey Bay Aquarium Research Institute (project 200002; to JPB), US Department of Energy grant # DE-FG02-03ER63696 (to J. P. Kennett and J.M.B.), and NSF OCE-0725966 (to J.M.B.).
    Keywords: Carbon dioxide sequestration ; CO2 injection ; Climate change ; Foraminifera ; Experiment ; Hypercapnia ; Meiofauna ; Monterey Bay ; Ocean acidification ; Protist
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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