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  • 1
    In: Earth and planetary science letters, Amsterdam [u.a.] : Elsevier, 1966, 260(2007), 3/4, Seite 505-515, 1385-013X
    In: volume:260
    In: year:2007
    In: number:3/4
    In: pages:505-515
    Type of Medium: Online Resource
    Pages: Ill., graph. Darst
    ISSN: 1385-013X
    Language: English
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  • 2
    In: Biogeosciences, Katlenburg-Lindau [u.a.] : Copernicus, 2004, 6(2009), 10, Seite 2145-2153, 1726-4189
    In: volume:6
    In: year:2009
    In: number:10
    In: pages:2145-2153
    Type of Medium: Electronic Resource
    Pages: graph. Darst
    ISSN: 1726-4189
    Language: English
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  • 3
    In: Biogeosciences, Katlenburg-Lindau [u.a.] : Copernicus, 2004, 6(2009), Seite 877885, 1726-4189
    In: volume:6
    In: year:2009
    In: pages:877885
    Description / Table of Contents: A CO2 enrichment experiment (PeECE III) was carried out in 9 mesocosms in which the seawater carbonate system was manipulated to achieve three different levels of pCO2. At the onset of the experimental period, nutrients were added to all mesocosms in order to initiate phytoplankton blooms. Primary production rates were measured by in-vitro incubations based on 14C-incorporation and oxygen production/consumption. Size fractionated particulate primary production was also determined by 14C incubation and is discussed in relation to phytoplankton composition. Primary production rates increased in response to nutrient addition and a net autotrophic phase with 14C-fixation rates up to 4 times higher than initial was observed midway through the 24 days experiment before net community production (NCP) returned to near-zero and 14C-fixation rates dropped below initial values. No clear heterotrophic phase was observed during the experiment. Based on the 14C-measurements we found higher cumulative primary production at higher pCO2 towards the end of the experiment. CO2 related differences were also found in size fractionated primary production. The most noticeable responses to CO2 treatments with respect to primary production rates occurred in the second half of the experiment when phytoplankton growth had become nutrient limited, and the phytoplankton community changed from diatom to flagellate dominance. This opens for two alternative hypotheses that the effects are either associated with mineral nutrient limited growth, and/or with a change in phytoplankton species composition. The lack of a clear net heterotrophic phase in the last part of the experiment supports the idea that a substantial part of production in the upper layer was not degraded locally, but either accumulated or exported vertically.
    Type of Medium: Online Resource
    Pages: graph. Darst
    ISSN: 1726-4189
    Language: English
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  • 4
    In: Global biogeochemical cycles, Hoboken, NJ : Wiley, 1987, 22(2008), 1944-9224
    In: volume:22
    In: year:2008
    In: extent:10
    Description / Table of Contents: The primary impacts of anthropogenic CO2 emissions on marine biogeochemical cycles predicted so far include ocean acidification, global warming induced shifts in biogeographical provinces, and a possible negative feedback on atmospheric CO2 levels by CO2-fertilized biological production. Here we report a new potentially significant impact on the oxygen-minimum zones of the tropical oceans. Using a model of global climate, ocean circulation, and biogeochemical cycling, we extrapolate mesocosm-derived experimental findings of a pCO2-sensitive increase in biotic carbon-to-nitrogen drawdown to the global ocean. For a simulation run from the onset of the industrial revolution until A.D. 2100 under a business-as-usualʺ scenario for anthropogenic CO2 emissions, our model predicts a negative feedback on atmospheric CO2 levels, which amounts to 34 Gt C by the end of this century. While this represents a small alteration of the anthropogenic perturbation of the carbon cycle, the model results reveal a dramatic 50% increase in the suboxic water volume by the end of this century in response to the respiration of excess organic carbon formed at higher CO2 levels. This is a significant expansion of the marine dead zonesʺ with severe implications not only for all higher life forms but also for oxygen-sensitive nutrient recycling and, hence, for oceanic nutrient inventories.
    Type of Medium: Online Resource
    Pages: 10 , graph. Darst
    ISSN: 1944-9224
    Language: English
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  • 5
    In: Science, Washington, DC : American Association for the Advancement of Science, 1880, 322(2008), 5907, Seite 1466, 1095-9203
    In: volume:322
    In: year:2008
    In: number:5907
    In: pages:1466
    Type of Medium: Online Resource
    Pages: graph. Darst
    ISSN: 1095-9203
    Language: English
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  • 6
    In: Aquatic microbial ecology, Oldendorf, Luhe : Inter-Research, 1995, 54(2009), 3, Seite 305-318, 1616-1564
    In: volume:54
    In: year:2009
    In: number:3
    In: pages:305-318
    Description / Table of Contents: Effects of elevated temperature on the formation and subsequent degradation of diatom aggregates were studied in a laboratory experiment with a natural plankton community from the Kiel Fjord (Baltic Sea). Aggregates were derived from diatom blooms that developed in indoor mesocosms at 2.5 and 8.5°C corresponding to the 1993 to 2002 mean winter in situ temperature of the Western Baltic Sea and the projected sea surface temperature during winter in 2100, respectively. Formation and degradation of diatom aggregates at these 2 temperatures in the dark were promoted with roller tanks over a period of 11 d. Comparison of the 2 temperature settings revealed an enhanced aggregation potential of diatom cells at elevated temperature, which was likely induced by an increased concentration of transparent exopolymer particles (TEP). The enhanced aggregation potential led to a significantly higher proportion of particulate organic matter in aggregates at 8.5°C Moreover, the elevated temperature favoured the growth of bacteria, bacterial biomass production, and the activities of sugar- and protein-degrading extracellular enzymes in aggregates. Stimulating effects of rising temperature on growth and metabolism of the bacterial community resulted in an earlier onset of aggregate degradation and silica dissolution. Remineralization of carbon in aggregates at elevated temperature was partially compensated by the formation of carbon-rich TEP during dark incubation. Hence, our results suggest that increasing temperature will affect both formation and degradation of diatom aggregates. We conclude that the vertical export of organic matter through aggregates may change in the future, depending on the magnitude and vertical depth penetration of warming in the ocean.
    Type of Medium: Online Resource
    Pages: graph. Darst
    ISSN: 1616-1564
    Language: English
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  • 7
    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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  • 8
    Type of Medium: Book
    Pages: 258 S , Ill. (farb.), graph. Darst.
    ISBN: 9789279111181
    Language: English
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  • 9
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: Online-Ressource (49 Seiten = 6 MB) , Illustrationen, Diagramme, Karten
    Language: English
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  • 10
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (97 Blatt = 2,3 MB) , Illustrationen, Diagramme, Karte
    Language: English
    Note: Zusammenfassung in deutscher und englischer Sprache
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