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  • 1
    In: Aquatic microbial ecology, Oldendorf, Luhe : Inter-Research, 1995, 34(2004), 1, Seite 93-104, 1616-1564
    In: volume:34
    In: year:2004
    In: number:1
    In: pages:93-104
    Description / Table of Contents: The role of transparent exopolymer particles (TEP) and dissolved organic carbon (DOC) for organic carbon partitioning under different CO2 conditions was examined during a mesocosm experiment with the coccolithophorid Emiliania huxleyi. We designed 9 outdoor enclosures (~11 m3) to simulate CO2 concentrations of estimated ŒYear 2100£ (~710 ppm CO2), Œpresent (~410 ppm CO2) and Œglacial (~190 ppm CO2) environments, and fertilized these with nitrate and phosphate to favor bloom development. Our results showed fundamentally different TEP and DOC dynamics during the bloom. In all mesocosms, TEP concentration increased after nutrient exhaustion and accumulated steadily until the end of the study. TEP concentration was closely related to the abundance of E. huxleyi and accounted for an increase in POC concentration of 35 ± 2% after the onset of nutrient limitation. The production of TEP normalized to the cell abundance of E. huxleyi was highest in the Year 2100 treatment. In contrast, DOC concentration exhibited considerable short-term fluctuations throughout the study. In all mesocosms, DOC was neither related to the abundance of E. huxleyi nor to TEP concentration. A statistically significant effect of the CO2 treatment on DOC concentration was not determined. However, during the course of the bloom, DOC concentration increased in 2 of the 3 Year 2100 mesocosms and in 1 of the present mesocosms, but in none of the glacial mesocosms. It is suggested that the observed differences between TEP and DOC were determined by their different bioavailability and that a rapid response of the microbial food web may have obscured CO2 effects on DOC production by autotrophic cells.
    Type of Medium: Online Resource
    Pages: Ill., graph. Darst
    ISSN: 1616-1564
    Language: English
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  • 2
    Publication Date: 2019-09-23
    Description: Fertilization of the ocean by adding iron compounds has induced diatom-dominated phytoplankton blooms accompanied by considerable carbon dioxide drawdown in the ocean surface layer. However, because the fate of bloom biomass could not be adequately resolved in these experiments, the timescales of carbon sequestration from the atmosphere are uncertain. Here we report the results of a five-week experiment carried out in the closed core of a vertically coherent, mesoscale eddy of the Antarctic Circumpolar Current, during which we tracked sinking particles from the surface to the deep-sea floor. A large diatom bloom peaked in the fourth week after fertilization. This was followed by mass mortality of several diatom species that formed rapidly sinking, mucilaginous aggregates of entangled cells and chains. Taken together, multiple lines of evidence—although each with important uncertainties—lead us to conclude that at least half the bloom biomass sank far below a depth of 1,000 metres and that a substantial portion is likely to have reached the sea floor. Thus, iron-fertilized diatom blooms may sequester carbon for timescales of centuries in ocean bottom water and for longer in the sediments.
    Type: Article , PeerReviewed
    Format: text
    Format: text
    Format: text
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  • 3
    Publication Date: 2016-05-26
    Description: The role of transparent exopolymer particles (TEP) and dissolved organic carbon (DOC) for organic carbon partitioning under different CO2 conditions was examined during a mesocosm experiment with the coccolithophorid Emiliania huxleyi. We designed 9 outdoor enclosures (similar to11 m(3)) to simulate CO2 concentrations of estimated 'Year 2100' (similar to710 ppm CO2), 'present' (similar to410 ppm CO2) and 'glacial' (similar to190 ppm CO2) environments, and fertilized these with nitrate and phosphate to favor bloom development. Our results showed fundamentally different TEP and DOC dynamics during the bloom. In all mesocosms, TEP concentration increased after nutrient exhaustion and accumulated steadily until the end of the study. TEP concentration was closely related to the abundance of E. huxleyi and accounted for an increase in POC concentration of 35 2 % after the onset of nutrient limitation. The production of TEP normalized to the cell Abundance of E. huxleyi was highest in the Year 2100 treatment. In contrast, DOC concentration exhibited considerable short-term fluctuations throughout the study. In all mesocosms, DOC was neither related to the abundance of E. huxleyi nor to TEP concentration. A statistically significant effect of the CO2 treatment on DOC concentration was not determined. However, during the course of the bloom, DOC concentration increased in 2 of the 3 Year 2100 mesocosms and in 1 of the present mesocosms, but in none of the glacial mesocosms. It is suggested that the observed differences between TEP and DOC were determined by their different bioavailability and that a rapid response of the microbial food web may have obscured CO2 effects on DOC production by autotrophic cells.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2023-05-12
    Keywords: Europe, Norway; Mass spectrometer Europa Scientific 20/2; MESO; Mesocosm experiment; ORDINAL NUMBER; Raunefjord; δ13C, particulate organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 189 data points
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  • 5
    Publication Date: 2023-05-12
    Keywords: Europe, Norway; Mass spectrometer Europa Scientific 20/2; MESO; Mesocosm experiment; ORDINAL NUMBER; Raunefjord; δ13C, carbon dioxide, aquatic
    Type: Dataset
    Format: text/tab-separated-values, 198 data points
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  • 6
    Publication Date: 2023-05-12
    Keywords: Europe, Norway; Mass spectrometer Europa Scientific 20/2; MESO; Mesocosm experiment; ORDINAL NUMBER; Raunefjord; δ13C, dissolved inorganic carbon
    Type: Dataset
    Format: text/tab-separated-values, 91 data points
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  • 7
    Publication Date: 2023-05-12
    Keywords: Alkenone per cell Emiliania huxleyi; Europe, Norway; MESO; Mesocosm experiment; ORDINAL NUMBER; Pressurized liquid extraction; Raunefjord
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Benthien, Albert; Zondervan, Ingrid; Engel, Anja; Hefter, Jens; Terbrüggen, Anja; Riebesell, Ulf (2007): Carbon isotopic fractionation during a mesocosm bloom experiment dominated by Emiliania huxleyi: Effects of CO2 concentration and primary production. Geochimica et Cosmochimica Acta, 71(6), 1528-1541, https://doi.org/10.1016/j.gca.2006.12.015
    Publication Date: 2023-05-12
    Description: We investigated the effect of CO2 and primary production on the carbon isotopic fractionation of alkenones and particulate organic matter (POC) during a natural phytoplankton bloom dominated by the coccolithophore Emiliania huxleyi. In nine semi-closed mesocosms (~11 m**3 each), three different CO2 partial pressures (pCO2) in triplicate represented glacial (~180 ppmv CO2), present (380 ppmv CO2), and year 2100 (~710 ppmv CO2) CO2 conditions. The largest shift in alkenone isotopic composition (4-5 per mil) occurred during the exponential growth phase, regardless of the CO2 concentration in the respective treatment. Despite the difference of ~500 ppmv, the influence of pCO2 on isotopic fractionation was marginal (1-2 per mil). During the stationary phase, E. huxleyi continued to produce alkenones, accumulating cellular concentrations almost four times higher than those of exponentially dividing cells. Our isotope data indicate that, while alkenone production was maintained, the interaction of carbon source and cellular uptake dynamics by E. huxleyi reached a steady state. During stationary phase, we further observed a remarkable increase in the difference between d13C of bulk organic matter and of alkenones spanning 7-12 per mil. We suggest that this phenomenon is caused mainly by a combination of extracellular release of 13C-enriched polysaccharides and subsequent particle aggregation induced by the production of transparent exopolymer particles (TEP).
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 9
    Publication Date: 2023-12-12
    Description: Near-daily concentrations of Chlorophyll a and phaeopigments from RV Polarsterns underway water supply system (inlet at 11m water depth) collected during legs 1,3,4, and 5 of the MOSAiC (PS122) drift expedition in the central Arctic Ocean. 2-4L of water were filtered onto pre-combusted GF/F filters (nominal pore size 0.7µm) and frozen at -80°C. Samples were subsequently extracted in 90°C acetone, homogenized using a cell mill, and measured on the following day using a Turner flourometer, followed by an acidification step to determine phaeopigments (see Knap et al. 1996 for details and calculations). Samples were collected from end of October 2019 to beginning of October 2020, with a gap between mid-December and the end of February.
    Keywords: Acidification method according to Knap et al. (1996); Activity description; Arctic Ocean; Cast number; CHLa; Chl-a; Chlorophyll a; DATE/TIME; DEPTH, water; Device type; Event label; LATITUDE; Leg Number; LONGITUDE; Mosaic; MOSAiC; MOSAiC_ECO; MOSAiC20192020; Multidisciplinary drifting Observatory for the Study of Arctic Climate; North Greenland Sea; Phaeopigments; pigments; Pigments, Turner fluorometer; Polarstern; PS122/1; PS122/1_10-109; PS122/1_10-84; PS122/1_10-85; PS122/1_10-86; PS122/1_10-87; PS122/1_10-88; PS122/1_10-89; PS122/1_11-14; PS122/1_11-2; PS122/1_11-26; PS122/1_11-36; PS122/1_11-48; PS122/1_5-42; PS122/1_5-44; PS122/1_5-87; PS122/1_6-88; PS122/1_6-89; PS122/1_6-90; PS122/1_6-91; PS122/1_6-92; PS122/1_6-94; PS122/1_7-115; PS122/1_7-116; PS122/1_7-117; PS122/1_7-118; PS122/1_7-119; PS122/1_7-132; PS122/1_8-127; PS122/1_8-89; PS122/1_8-90; PS122/1_8-91; PS122/1_8-92; PS122/1_8-93; PS122/1_9-112; PS122/1_9-82; PS122/1_9-83; PS122/1_9-84; PS122/1_9-85; PS122/1_9-86; PS122/3; PS122/3_29-78; PS122/3_29-89; PS122/3_30-15; PS122/3_30-49; PS122/3_30-51; PS122/3_30-63; PS122/3_30-80; PS122/3_30-93; PS122/3_31-14; PS122/3_31-27; PS122/3_31-40; PS122/3_31-48; PS122/3_31-58; PS122/3_31-74; PS122/3_31-83; PS122/3_32-20; PS122/3_32-35; PS122/3_32-4; PS122/3_32-47; PS122/3_32-49; PS122/3_32-69; PS122/3_32-87; PS122/3_33-16; PS122/3_33-49; PS122/3_33-54; PS122/3_33-6; PS122/3_33-77; PS122/3_33-94; PS122/3_33-95; PS122/3_34-19; PS122/3_34-33; PS122/3_34-44; PS122/3_34-48; PS122/3_34-6; PS122/3_34-73; PS122/3_34-82; PS122/3_35-101; PS122/3_35-109; PS122/3_35-27; PS122/3_35-45; PS122/3_35-6; PS122/3_35-68; PS122/3_35-86; PS122/3_36-100; PS122/3_36-126; PS122/3_36-136; PS122/3_36-33; PS122/3_36-36; PS122/3_36-7; PS122/3_36-71; PS122/3_37-10; PS122/3_37-106; PS122/3_37-107; PS122/3_37-113; PS122/3_37-13; PS122/3_37-43; PS122/3_37-54; PS122/3_38-153; PS122/3_38-154; PS122/3_38-156; PS122/3_38-23; PS122/3_38-29; PS122/3_38-73; PS122/3_39-118; PS122/3_39-119; PS122/3_39-120; PS122/3_39-121; PS122/3_39-122; PS122/3_39-123; PS122/3_39-124; PS122/3_40-23; PS122/3_40-24; PS122/3_40-25; PS122/3_40-56; PS122/3_40-57; PS122/3_40-58; PS122/3_40-59; PS122/3_41-28; PS122/3_41-29; PS122/3_41-30; PS122/3_41-31; PS122/3_41-39; PS122/3_41-43; PS122/3_41-49; PS122/3_42-15; PS122/3_42-2; PS122/3_42-22; PS122/3_42-36; PS122/3_42-37; PS122/3_42-46; PS122/3_42-54; PS122/3_42-59; PS122/3_42-7; PS122/4; PS122/4_44-104; PS122/4_44-117; PS122/4_44-132; PS122/4_44-148; PS122/4_44-163; PS122/4_44-168; PS122/4_44-176; PS122/4_44-192; PS122/4_44-20; PS122/4_44-21; PS122/4_44-212; PS122/4_44-33; PS122/4_44-40; PS122/4_44-41; PS122/4_44-55; PS122/4_44-66; PS122/4_44-84; PS122/4_44-86; PS122/4_44-93; PS122/4_44-94; PS122/4_45-109; PS122/4_45-110; PS122/4_45-111; PS122/4_45-134; PS122/4_45-27; PS122/4_45-28; PS122/4_45-49; PS122/4_46-10; PS122/4_46-156; PS122/4_46-157; PS122/4_46-158; PS122/4_46-159; PS122/4_46-34; PS122/4_46-54; PS122/4_47-141; PS122/4_47-142; PS122/4_47-15; PS122/4_47-30; PS122/4_47-78; PS122/4_47-79; PS122/4_47-95; PS122/4_48-107; PS122/4_48-108; PS122/4_48-109; PS122/4_48-110; PS122/4_48-16; PS122/4_48-181; PS122/4_48-182; PS122/4_49-104; PS122/4_49-13; PS122/4_49-41; PS122/4_49-42; PS122/4_49-60; PS122/4_49-65; PS122/4_49-84; PS122/4_50-15; PS122/4_50-23; PS122/4_50-33; PS122/4_50-46; PS122/4_50-54; PS122/4_50-6; PS122/4_50-60; PS122/4_50-63; PS122/4_50-76; PS122/5; PS122/5_59-118; PS122/5_59-131; PS122/5_59-150; PS122/5_59-157; PS122/5_59-165; PS122/5_59-166; PS122/5_59-177; PS122/5_59-190; PS122/5_59-205; PS122/5_59-221; PS122/5_59-24; PS122/5_59-257; PS122/5_59-283; PS122/5_59-289; PS122/5_59-3; PS122/5_59-34; PS122/5_59-385; PS122/5_59-386; PS122/5_59-387; PS122/5_59-388; PS122/5_59-48; PS122/5_59-49; PS122/5_59-52; PS122/5_59-54; PS122/5_59-56; PS122/5_59-71; PS122/5_59-9; PS122/5_60-132; PS122/5_60-252; PS122/5_60-253; PS122/5_60-254; PS122/5_60-255; PS122/5_60-256; PS122/5_60-257; PS122/5_61-120; PS122/5_61-121; PS122/5_61-122; PS122/5_61-306; PS122/5_61-307; PS122/5_61-308; PS122/5_61-309; PS122/5_62-245; PS122/5_62-246; PS122/5_62-247; PS122/5_62-248; PS122/5_62-249; PS122/5_62-250; PS122/5_62-251; PS122/5_63-113; PS122/5_63-114; PS122/5_63-147; PS122/5_63-148; PS122/5_63-149; PS122/5_63-22; PS122/5_63-23; PS122/5_63-26; PS122/5_63-65; PS122/5_63-67; PS122/5_63-79; Tap; TAP; under ice; Underway water sampling; UWS; Volume
    Type: Dataset
    Format: text/tab-separated-values, 3863 data points
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  • 10
    Publication Date: 2023-12-12
    Description: Concentrations of Chlorophyll a and phaeopigments from CTD-rosette casts during the MOSAiC (PS122) drift expedition in the central Arctic Ocean. 2-4L of water were filtered onto precombusted GF/F filters (nominal pore size 0.7µm) and frozen at -80°C. Samples were subsequently extracted in 90°C acetone,homogenized using a cell mill, and meaured on the following day using a Turner flourometer, followed by an acidification step to determine pheopigments (see Knap et al. 1994 for details and calculations). Samples were collected roughly once per week from end of October 2019 to beginning of October 2020.
    Keywords: Acidification method according to Knap et al. (1996); Activity description; Arctic; Arctic Ocean; Cast number; Chl-a; Chlorophyll a; Collector; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; Device type; Event label; Feature; LATITUDE; Leg Number; LONGITUDE; MOSAiC; MOSAiC_ECO; MOSAiC20192020; Multidisciplinary drifting Observatory for the Study of Arctic Climate; phaeopigments; Phaeopigments; Phytoplankton; pigments; Pigments, Turner fluorometer; Polarstern; PS122/1; PS122/1_10-44; PS122/1_5-40; PS122/1_5-59; PS122/1_6-58; PS122/1_7-49; PS122/1_8-46; PS122/1_9-50; PS122/2; PS122/2_17-41; PS122/2_18-34; PS122/2_19-56; PS122/2_20-46; PS122/2_21-1; PS122/2_21-65; PS122/2_22-47; PS122/2_23-63; PS122/2_24-4; PS122/2_25-54; PS122/3; PS122/3_30-41; PS122/3_30-53; PS122/3_31-39; PS122/3_31-59; PS122/3_32-75; PS122/3_33-69; PS122/3_34-65; PS122/3_34-66; PS122/3_34-77; PS122/3_35-63; PS122/3_36-81; PS122/3_37-45; PS122/3_38-54; PS122/3_39-51; PS122/3_40-36; PS122/4; PS122/4_44-184; PS122/4_44-67; PS122/4_45-100; PS122/4_45-31; PS122/4_45-75; PS122/4_45-79; PS122/4_45-82; PS122/4_45-85; PS122/4_45-96; PS122/4_46-60; PS122/4_47-52; PS122/4_48-62; PS122/4_49-25; PS122/5; PS122/5_59-274; PS122/5_59-306; PS122/5_59-357; PS122/5_59-72; PS122/5_60-69; PS122/5_60-89; PS122/5_61-161; PS122/5_62-91; PS122/5_63-53; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 2273 data points
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