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  • 2000-2004  (17)
  • 2003  (17)
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  • 2000-2004  (17)
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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    FEMS microbiology ecology 46 (2003), S. 0 
    ISSN: 1574-6941
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Observations that the majority of silica dissolution occurs within the upper 200 m of the ocean, and that sedimentation rates of diatom frustules generally do not decrease significantly with depth, suggested reduced dissolution rates of diatoms embedded within sinking aggregates. To investigate this hypothesis, silica dissolution rates of aggregated diatom cells were compared to those of dispersed cells during conditions mimicking sedimentation below the euphotic zone. Changes in the concentrations of biogenic silica, silicic acid, cell numbers, chlorophyll a and transparent exopolymer particles (TEP) were monitored within aggregates and in the surrounding seawater (SSW) during two 42-day experiments. Whereas the concentration of dispersed diatoms decreased over the course of the experiment, the amount of aggregated cells remained roughly constant after an initial increase. Initially only 6% of cells were aggregated and at the end of the experiment more than 60% of cells were enclosed within aggregates. These data imply lower dissolution rates for aggregated cells. However, fluxes of silica between the different pools could not be constrained reliably enough to unequivocally prove reduced dissolution for aggregated cells.
    Type of Medium: Electronic Resource
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  • 2
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    In:  [Talk] In: EGS-AGU-EUG Joint Assembly 2003, 06.-11.04.2003, Nice, France .
    Publication Date: 2019-08-09
    Description: One particular task of marine ecosystem models is to simulate the biogenic transformation of dissolved inorganic carbon (DIC) into organic matter and hence to quantify the export of particulate organic carbon (POC) to deep oceanic layers. To date, environmental changes, such as increasing carbon dioxide concentrations (pCO_2) and temperature, are perceived to have an impact on the formation of organic carbon. However, well established nitrogen or phosphorus based ecosystem models are insensitive to variations in the carbonate system. In order to investigate biological responses to pCO_2 variations, ecosystem models need to distinguish between carbon, nitrogen, and/or phosphorus cycles. We present a simple biological model which decouples carbon from nitrogen fluxes such that carbon found in transparent exopolymer particles (TEP) is additionally accounted for. The model regards phytoplankton acclimation to varying environmental conditions, having included parameterizations for phytoplankton growth as proposed by Geider et al.~(1998, L&O). By means of data assimilation, an optimal parameter set is determined, which brings model results into agreement with experimental data. From the optimised model results it is infered that about 50% of dissolved organic carbon (DOC) exuded by phytoplankton is subsequently transformed into TEP, eventually influencing the amount of POC available for the export flux. Model sensitivity studies are performed at local sites and along a latitudinal transect (30^oN-60^oN at 19^oW) in the North Atlantic. As soon as CO_2 limitation for phytoplankton growth is explicitely considered in the model, the formation of POC shows great sensitivity to pCO_2 variations. Temperature variations alter remineralisation rates and growth efficiencies. With the current model version dependencies between biomass accumulation, the date of nutrient depletion to occur, and the exudation of organic compounds are acquired.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 3
    Publication Date: 2019-08-09
    Description: The export of organic carbon to the deep ocean is mediated by sinking of large particles, such as marine snow, the formation of which is enhanced in the presence of transparent exopolymer particles (TEP) . TEP form from dissolved and colloidal polysaccharides by aggregation processes. Especially when running into nutrient limitation phytoplankton organisms are a source of TEP in pelagic ecosystems as the cells release a significant amount of the assimilated carbon in the form of polysaccharides. Because CO_2 concentration influences carbon assimilation rates, we hypothesized that polysaccharide exudation and aggregation into TEP is related to CO_2 concentration under nutrient limiting conditions. We tested this hypothesis in several lab and outdoor experiments with natural populations and cultures of phytoplankton exposed to various levels of CO_2 concentrations. Our results indicate that TEP production increases with CO_2 concentration and provides an enhanced sink for carbon during phytoplankton blooms.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 4
    Publication Date: 2019-08-09
    Description: One of the most prominent consequences of human activities is the progressive rise in atmospheric pCO_2. This will also cause changes in seawater carbonate chemistry. However, to what extent anthropogenic perturbations in marine growth conditions will affect biological processes like species composition, ecosystem functioning, carbon production and vertical carbon export in the sea, as well as possible feedback mechanisms, is still under debate. In the present study, for the first time CO_2 effects were tested on a natural marine plankton community. In a series of floating mesocosms in a Norwegian fjord a phytoplankton bloom dominated by the coccolithophore Emiliania huxleyi was induced. By covering the enclosures by gas-tight domes, functioning as greenhouses, we were able to maintain CO_2 concentrations in the overlaying atmosphere ranging from pre-industrial to projected year 2100 levels over a three-week period. Here we present an overview of the experiment and report on the development of the bloom under different pCO_2 levels.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 5
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    Elsevier
    In:  FEMS Microbiology Ecology, 46 (3). pp. 247-255.
    Publication Date: 2020-03-20
    Description: Observations that the majority of silica dissolution occurs within the upper 200 m of the ocean, and that sedimentation rates of diatom frustules generally do not decrease significantly with depth, suggested reduced dissolution rates of diatoms embedded within sinking aggregates. To investigate this hypothesis, silica dissolution rates of aggregated diatom cells were compared to those of dispersed cells during conditions mimicking sedimentation below the euphotic zone. Changes in the concentrations of biogenic silica, silicic acid, cell numbers, chlorophyll a and transparent exopolymer particles (TEP) were monitored within aggregates and in the surrounding seawater (SSW) during two 42-day experiments. Whereas the concentration of dispersed diatoms decreased over the course of the experiment, the amount of aggregated cells remained roughly constant after an initial increase. Initially only 6% of cells were aggregated and at the end of the experiment more than 60% of cells were enclosed within aggregates. These data imply lower dissolution rates for aggregated cells. However, fluxes of silica between the different pools could not be constrained reliably enough to unequivocally prove reduced dissolution for aggregated cells.
    Type: Article , PeerReviewed
    Format: text
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  • 6
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    In:  [Poster] In: EGS-AGU-EUG Joint Assembly 2003, 06.-11.04.2003, Nice, France .
    Publication Date: 2019-08-09
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 7
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    In:  [Poster] In: IGBP/SCOR Open Science Meeting on Ocean Biogeochemistry and Ecosystems Analysis, 07.-10.01.2003, Paris, France .
    Publication Date: 2019-08-09
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 8
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    In:  [Poster] In: IGBP/SCOR Open Science Meeting on Ocean Biogeochemistry and Ecosystems Analysis, 07.-10.01.2003, Paris, France .
    Publication Date: 2019-08-09
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 9
    Publication Date: 2019-08-09
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 10
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    In:  EPIC3Fems microbiology ecology, 46, pp. 247-255, ISSN: 0168-6496
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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