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  • 1
    Publication Date: 2023-05-12
    Keywords: Area/locality; Chlorophyll a; Chlorophyll a, standard deviation; CTD, Seacat; CTD-S; Dana10_FB2_1; Dana10_FB3.5_1; Dana10_GF1_1; Dana10_GF10_1; Dana10_GF10bis; Dana10_GF11_1; Dana10_GF2_1; Dana10_GF3_1; Dana10_GF6_1; Dana10_K2_1; Dana10_K4_1; Dana10/1; Dana II; Date/Time of event; DEPTH, water; Event label; Fyllas Banke, West Greenland; Godthåbsfjord, West Greenland; Kapisigdlit, West Greenland; Latitude of event; Longitude of event; Sampling date; Station label; Temperature, technical
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2023-07-10
    Keywords: Amphidinium sphenoides, biomass as carbon; Amphidinium sphenoides, standard deviation; Chaetoceros spp., biomass as carbon; Chaetoceros spp., standard deviation; Ciliates, biomass as carbon; Ciliates, standard deviation; CTD, Seacat; CTD-S; Dana10_GF10bis; Dana10_GF11_1; Dana10_K2_1; Dana10_K4_1; Dana10/1; Dana II; Date/Time of event; DEPTH, water; Diatoms, centrales, biomass as carbon; Diatoms, pennales, biomass as carbon; Diatoms, standard deviation; Dinobryon spp., biomass as carbon; Dinobryon spp., standard deviation; Dinoflagellates, biomass as carbon; Dinoflagellates, standard deviation; Dinophysis spp., biomass as carbon; Dinophysis spp., standard deviation; Event label; Godthåbsfjord, West Greenland; Gyrodinium spp., biomass as carbon; Gyrodinium spp., standard deviation; Kapisigdlit, West Greenland; Katodinium glaucum, biomass as carbon; Katodinium glaucum, standard deviation; Laboea strobila, biomass as carbon; Laboea strobila, standard deviation; Latitude of event; Longitude of event; Nanoflagellates, biomass as carbon; Nanoflagellates, standard deviation; Phaeocystis sp., biomass as carbon; Phaeocystis sp., standard deviation; Protoperidinium spp., biomass as carbon; Protoperidinium spp., standard deviation; Pseudo-nitzschia spp., biomass as carbon; Pseudo-nitzschia spp., standard deviation; Strombidium spp., biomass as carbon; Strombidium spp., standard deviation; Thalassiosira spp., biomass as carbon; Thalassiosira spp., standard deviation; Tintinnid, biomass as carbon; Tintinnid, standard deviation; Torodinium robustum, biomass as carbon; Torodinium robustum, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 168 data points
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  • 3
    Publication Date: 2023-07-11
    Keywords: CTD, Seacat; CTD-S; Dana10_FB2_1; Dana10_FB3.5_1; Dana10_GF1_1; Dana10_GF10_1; Dana10_GF10bis; Dana10_GF11_1; Dana10_GF2_1; Dana10_GF3_1; Dana10_GF6_1; Dana10_K2_1; Dana10_K4_1; Dana10/1; Dana II; Event label; Feeding experiment; FX; Fyllas Banke, West Greenland; Godthåbsfjord, West Greenland; Kapisigdlit, West Greenland; Method comment; Mortality; Number; Phytoplankton growth rate; Primary production of chlorophyll a per day; Primary production removed/grazed; Size fraction; Station label
    Type: Dataset
    Format: text/tab-separated-values, 138 data points
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  • 4
    Publication Date: 2023-07-11
    Keywords: CTD, Seacat; CTD-S; Dana10_GF11_1; Dana10_GF6_1; Dana10_K2_1; Dana10/1; Dana II; Event label; Feeding experiment; FX; Godthåbsfjord, West Greenland; Kapisigdlit, West Greenland; Mortality; Number; Phytoplankton growth rate; Size fraction; Station label
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Calbet, Albert; Riisgaard, Karen; Saiz, Enric; Zamora, Sara; Stedmon, Colin A; Nielsen, Torkel Gissel (2011): Phytoplankton growth and microzooplankton grazing along a sub-Arctic fjord (Godthabsfjord, west Greenland). Marine Ecology Progress Series, 442, 11-22, https://doi.org/10.3354/meps09343
    Publication Date: 2023-12-13
    Description: We evaluated the role of microzooplankton (sensu latto, grazers 〈500 µm) in determining the fate of phytoplankton production (PP) along a glacier-to-open sea transect in the Greenland subarctic fjord, Godthabfjord. Based on the distribution of size fractionated chlorophyll a (chl a) concentrations we established 4 zones: (1) Fyllas Bank, characterized by deep chl a maxima (ca. 30 to 40 m) consisting of large cells, (2) the mouth and main branch of the fjord, where phytoplankton was relatively homogeneously distributed in the upper 30 m layer, (3) inner waters influenced by glacial melt water and upwelling, with high chl a concentrations (up to 12 µg/l) in the 〉10 µm fraction within a narrow (2 m) subsurface layer, and (4) the Kapisigdlit branch of the fjord, ice-free, and characterized with a thick and deep chl a maximum layer. Overall, microzooplankton grazing impact on primary production was variable and seldom significant in the Fyllas Bank and mouth of the fjord, quite intensive (up to 〉100% potential PP consumed daily) in the middle part of the main and Kapisigdlit branches of the fjord, and rather low and unable to control the fast growing phytoplankton population inhabiting the nutrient rich waters in the upwelling area in the vicinity of the glacier. Most of the grazing impact was on the 〈10 µm phytoplankton fraction, and the major grazers of the system seem to be 〉20 µm microzooplankton, as deducted from additional dilution experiments removing this size fraction. Overall, little or no export of phytoplankton out of the fjord to the Fyllas Bank can be determined from our data.
    Keywords: International Polar Year (2007-2008); IPY
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 6
    Publication Date: 2024-02-02
    Description: In temperate, subpolar and polar marine systems, the classical perception is that diatoms initiate the spring bloom and thereby mark the beginning of the productive season. Contrary to this view, here we document an pre-bloom of pico- and nanophytoplankton prior to the diatom bloom; a period with excess nutrients and deep convection of the water column. During repeated visits to stations in the deep Icelandic and the Norwegian Basins and the shallow Shetland Shelf (26 March to 29 April 2012), we investigated the succession and dynamics of 〈10 µm phytoplankton. Water samples were collected from CTD rosette 10 L Niskin bottles and fixed in glutaraldehyde (final conc. 5%), flash frozen in liquid Nitrogen and stored at -80°C until analysis.
    Keywords: Basin Scale Analysis, Synthesis and Integration; CTD/Rosette; CTD-RO; Date/Time of event; Deep Convection Cruise; DEPTH, water; EURO-BASIN; Event label; FACSCalibur flow-cytometer (Becton Dickinson); Latitude of event; Longitude of event; M87/1_421-1; M87/1_440-1; M87/1_449-1; M87/1_460-1; M87/1_466-1; M87/1_482-1; M87/1_487-1; M87/1_499-1; M87/1_516-1; M87/1_532-1; M87/1_541-1; M87/1_564-1; M87/1_572-1; M87/1_581-1; M87/1_586-1; M87/1_600-1; M87/1_608-1; M87/1_611-1; M87/1_618-1; M87/1_641-1; M87/1_659-1; M87/1_667-1; M87/1_672-1; M87/1_679-1; M87/1_689-1; M87/1a; M87/1b; Meteor (1986); Nanophytoplankton; Optional event label; Picophytoplankton; Station 1; Station 2; Station 3; Synechococcus
    Type: Dataset
    Format: text/tab-separated-values, 676 data points
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  • 7
    Publication Date: 2024-02-02
    Description: In temperate, subpolar and polar marine systems, the classical perception that bacteria are carbon limited by end of winter and respond in activity and abundance to the production of new carbon during the diatom spring bloom and post bloom. Contrary to this view, we here document an strong increase in bacterial abundance and activity (latter measured by increasing high nuclei acid (HNA) to low nuclei acid (LNA) bacteria ratio) during the winter-spring transition, where phytoplankton smaller than 10 µm dominate. Further DNA-virus were enumerated and revealed the virus to bacteria ratio (VBR) to be decreasing during winter-spring transition, indicating that the virus did not increase in number accordingly to bacteria. During repeated visits to stations in the deep Icelandic and the Norwegian Basins and the shallow Shetland Shelf (26 March to 29 April 2012), we investigated the abundance of bacteria and the succession of HNA:LNA bacteria and VBR. Water samples were collected from CTD rosette .10 L Niskin bottles and fixed in glutaraldehyde (final conc. 5%), flash frozen in liquid Nitrogen and stored at -80°C until analysis.
    Keywords: Bacteria; Basin Scale Analysis, Synthesis and Integration; CTD/Rosette; CTD-RO; Date/Time of event; Deep Convection Cruise; DEPTH, water; EURO-BASIN; Event label; FACSCalibur flow-cytometer (Becton Dickinson); High nucleic acid bacteria/low nucleic acid bacteria ratio; Latitude of event; Longitude of event; M87/1_421-1; M87/1_424-1; M87/1_440-1; M87/1_449-1; M87/1_460-1; M87/1_466-1; M87/1_482-1; M87/1_487-1; M87/1_499-1; M87/1_516-1; M87/1_532-1; M87/1_541-1; M87/1_564-1; M87/1_572-1; M87/1_581-1; M87/1_586-1; M87/1_600-1; M87/1_608-1; M87/1_611-1; M87/1_618-1; M87/1_638-1; M87/1_641-1; M87/1_659-1; M87/1_667-1; M87/1_672-1; M87/1_679-1; M87/1_689-1; M87/1a; M87/1b; Meteor (1986); Optional event label; Station 1; Station 2; Station 3; Viral abundance; Virus/bacteria ratio
    Type: Dataset
    Format: text/tab-separated-values, 697 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Thoisen, Christina; Riisgaard, Karen; Lundholm, Nina; Nielsen, Torkel Gissel; Hansen, Per Juel (2015): Effect of acidification on an Arctic phytoplankton community from Disko Bay, West Greenland. Marine Ecology Progress Series, 520, 21-34, https://doi.org/10.3354/meps11123
    Publication Date: 2024-03-15
    Description: Long-term measurements (i.e. months) of in situ pH have not previously been reported from the Arctic; this study shows fluctuations between pH 7.5 and 8.3 during the spring bloom 2012 in a coastal area of Disko Bay, West Greenland. The effect of acidification on phytoplankton from this area was studied at both the community and species level in experimental pH treatments within (pH 8.0, 7.7 and 7.4) and outside (pH 7.1) in situ pH. The growth rate of the phytoplankton community decreased during the experimental acidification from 0.50 ± 0.01/day (SD) at pH 8.0 to 0.22 ± 0.01/day at pH 7.1. Nevertheless, the response to acidification was species-specific and divided into 4 categories: I, least affected; II, affected only at pH 7.1; III, gradually affected and IV, highly affected. In addition, the colony size and chain length of selected species were affected by the acidification. Our findings show that coastal phytoplankton from Disko Bay is naturally exposed to pH fluctuations exceeding the experimental pH range used in most ocean acidification studies. We emphasize that studies on ocean acidification should include in situ pH before assumptions on the effect of acidification on marine organisms can be made.
    Keywords: Alkalinity, total; Aragonite saturation state; Arctic; Bicarbonate ion; Bicarbonate ion, standard deviation; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, standard deviation; Chaetoceros sp.; Coulometric titration; Diameter; Entire community; EXP; Experiment; Figure; Frequency; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Growth rate; Growth rate, standard deviation; Laboratory experiment; Navicula granii; Navicula sp.; Navicula vanhoeffenii; OA-ICC; Ocean Acidification International Coordination Centre; Open ocean; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; Percentage; Percentage, standard deviation; pH; pH, standard deviation; Phaeocystis pouchetii; Polar; Potentiometric; Pyramimonas sp.; Qeqertarsuaq; Salinity; Species; Temperature, water; Thalassiosira sp.; Thalassiosira spp.; Time in days; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 2880 data points
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