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  • 1
    Keywords: Hochschulschrift ; Dimethylsulfoniumpropionat ; Geochemie
    Type of Medium: Online Resource
    Pages: Online-Ressource (PDF-Datei: 88 S., 0.67 MB) , Ill., graph. Darst.
    Language: German
    Note: Kiel, Univ., Diss., 2005
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  • 2
    Keywords: Hochschulschrift ; Dimethylsulfoniumpropionat ; Geochemie
    Description / Table of Contents: Kurzfassung ; Summary
    Type of Medium: Book
    Pages: 88 S , Ill., graph. Darst
    Language: German
    Note: Kiel, Univ., Diss., 2005
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  • 3
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    Elsevier
    In:  Journal of Marine Systems, 30 . pp. 241-261.
    Publication Date: 2017-07-12
    Description: Taxon-specific microzooplankton dynamics were studied along a transect through the North Atlantic Drift from 70°N 04°E to 40°N 20°W during July 1997 using serial dilution and nutrient-enrichment experiments. Nutrient concentrations and microzooplankton composition indicated postbloom conditions at 40°N, 47°N, and 50°N, a transitional system at 54°N, and bloom conditions at 62°N and 70°N. The ratio of microzooplankton to phytoplankton biomass was inversely related to nitrate and phosphate concentrations. Potential grazing thresholds were observed in four of nine experiments at 40–66% of the initial phytoplankton concentration. Grazing losses were determined for six pigment-specific classes of phytoplankton. Selective grazing losses of phytoplankton taxa ranged from 73% to 248% of the nonselective grazing losses predicted according to their biomass contributions. The grazing selectivity varied considerably between communities, with the microherbivores showing positive selection for cyanobacteria and dinoflagellates and predominantly avoidance of chlorophyta and bacillariophyceae. Microzooplankton did not show a preference for the dominant phytoplankton taxa, but grazed preferentially on fast-growing phytoplankton with minor contributions (〈15%) to the phytoplankton biomass. However, bacillariophyceae were the major contributors to phytoplankton biomass and accounted for major fractions of the total losses through microzooplankton grazing. Microzooplankton consumed the equivalent of 0.12–5.5 times their own biomass daily on a carbon basis, amounting to 65–197% of gross phytoplankton production. With the conservative assumption that 20% of the consumed phytoplankton was converted to microzooplankton biomass, the latter was estimated to contribute 27–381% to the net production of the entire microzooplankton community. We therefore conclude that the taxonomic structure and the net production of the microzooplankton communities were significantly affected by the intensity and selectivity of herbivorous microzooplankton grazing.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2018-05-08
    Description: Serial dilution experiments were conducted on JGOFS-North Atlantic cruise of RV 'Meteor' M36/2 at a 20° W transect in June and July 1996 to assess the role of microzooplankton grazing and nitrogen supply in controlling phytoplankton stocks in the subtropical and temperate northeast Atlantic. Rates of microzooplankton grazing ranged from 0.08 d-1 at 54° N to 0.53 d-1 at 40° N and mean growth rates of phytoplankton ranged from 0.19 d-1 at 54° N to 0.75 d-1 at 40° N. Both rates were positively related to seawater temperature, whereas the apparent growth yield of phytoplankton declined with increasing temperature from 0.19 µg chl a dm-3 d-1 at 54° N to 0.01 µg chl a dm-3 d-1 at 33° N. Complete nitrogen saturation of phytoplankton growth indicated light or non-nitrogenous limitation at the nitracline at 47° N and in the deep chlorophyll maximum at 33° N, whereas in the mixed layer at 47° N and 54° N the ambient nitrogen supply was sub-saturated and yielded 63 and 39% of nitrogen- saturated growth. Nitrogen supply of phytoplankton growth was dominated by external and cellular sources in nitrate-rich waters of the mixed layer at 54° N and at the nitracline at 47° N, whereas nitrogen regeneration dominated at the nitrate-depleted surface waters at 47° N. However, in the deep chlorophyll maxima at 33° N and 40° N phytoplankton growth was primarily maintained by nitrogen regeneration, although external nitrogen was sufficiently available. The recycling efficiency of the microbial community was defined as the ratio of regenerated growth yield to herbivorous grazing loss. Efficiencies of ~100% under post-bloom situations indicated tight coupling of predation, nitrogen supply and phytoplankton growth. We suggest that microzooplankton grazing has a high potential for nitrogen supply and biomass control of phytoplankton communities during summer in the temperate and subtropical northeast Atlantic.
    Type: Article , PeerReviewed
    Format: text
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  • 5
    Publication Date: 2023-01-17
    Description: The study contains three experimental investigations; laboratory experiments about the DMSP-Produktion in cultures of marine planktonalgae, a series of field experiments about the production and turnover of particulate DMSP in the North-Sea and a series of nutrient enrichment experiments about the microbial turnover of dissolved DMSP in the tropical Atlantic. The culture experiments focused on the species-specific and the nitrogen-related variability of the DMSP-production. The observed species-specific variability of the intracellular DMSP concentration and the DMSP-production were one to two orders of magnitude higher than the range of their nitrogen-related changes and highlighted the role of key species. The importance of key species and the effect of the nutrient supply on the DMSP-production was also apparent in the series of in situ experiments in the North-Sea. About 3/4 of the total DMSP-production between March and October happened during a phase of 45 days after the vernal diatom bloom during a bloom of Phaeocystis globosa (Haptophyta) and a subsequent development of mixotrophic flagellates (cryptophyta). The maxima of the Phaeocystis bloom and of the surface concentrations of particulate DMSP coincided with a temporal minimum of the consumption of particulate DMSP by microzooplankton grazing. Apart from the Phaeocystis bloom, the consumption of particulate DMSP by microzooplankton was closely related with its production by phytoplankton and accounted on average for about 94 % of the production. About 77% of the consumed DMSP was on average released as dissolved DMSP and was in most cases microbially degraded within less than 24h. The nutrient enrichment experiments with natural size-fractionated bacteria communities in the tropical Atlantic aimed at the nutrient related variability of the DMS-yield of the decomposition of dissolved DMSP. In experiments without nutrient enrichments the DMS yield was on average 21 %. The DMS yield increased in most experiments due to organic or inorganic nutrient enrichments. The highest DMS-yields were achieved by the combined enrichments of dissolved organic sulphur and nitrogen by methionine.
    Type: Thesis , NonPeerReviewed
    Format: text
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