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  • 2010-2014  (3)
  • 2005-2009  (4)
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  • 1
    Keywords: Meereskunde ; Kooperation
    Description / Table of Contents: This brochure introduces the German Marine Research Consortium (KDM) with its 15 member institutions.
    Type of Medium: Book
    Pages: [18] Bl. , zahlr. Ill. (farb.)
    Language: English
    Note: Dt. Ausg. u.d.T.: In Zukunft Meer
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  • 2
    Book
    Book
    Berlin : Konsortium Deutsche Meeresforschung
    Keywords: Meereskunde ; Kooperation
    Description / Table of Contents: Mit dieser Broschüre stellt sich das Konsortium Deutsche Meeresforschung e.V. (KDM) mit seinen 15 Mitgliedsinstituten vor.
    Type of Medium: Book
    Pages: [36] S. , zahlr. Ill.
    Language: German
    Note: Engl. Ausg. u.d.T.: Ours seas and oceans
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  • 3
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    Institut für Geowissenschaften der Christian-Albrechts-Universität Kiel
    In:  Berichte - Reports / Institut für Geowissenschaften, Christian-Albrechts-Universität zu Kiel, 23 . Institut für Geowissenschaften der Christian-Albrechts-Universität Kiel, Kiel, Germany, 99 pp.
    Publication Date: 2020-08-03
    Type: Report , NonPeerReviewed
    Format: text
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  • 4
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    PANGAEA
    In:  Supplement to: Bathmann, Ulrich; Peinert, Rolf; Noji, Thomas T; von Bodungen, Bodo (1990): Pelagic origin and fate of sedimenting particles in the Norwegian Sea. Progress in Oceanography, 24(1-4), 117-125, https://doi.org/10.1016/0079-6611(90)90024-V
    Publication Date: 2023-03-16
    Description: A 17 month record of vertical particle flux of dry weight, carbonate and organic carbon were 25.8, 9.4 and 2.4g/m**2/y, respectively. Parallel to trap deployments, pelagic system structure was recorded with high vertical and temporal resolution. Within a distinct seasonal cycle of vertical particle flux, zooplankton faecal pellets of various sizes, shapes and contents were collected by the traps in different proportions and quantities throughout the year (range: 0-4,500 10**3/m**2/d). The remains of different groups of organisms showed distinct seasonal variations in abundance. In early summer there was a small maximum in the diatom flux and this was followed by pulses of tinntinids, radiolarians, foraminiferans and pteropods between July and November. Food web interactions in the water column were important in controlling the quality and quantity of sinking materials. For example, changes in the population structure of dominant herbivores, the break-down of regenerating summer populations of microflagellates and protozooplankton and the collapse of a pteropod dominated community, each resulted in marked sedimentation pulses. These data from the Norwegian Sea indicate those mechanisms which either accelerate or counteract loss of material via sedimentation. These involve variations in the structure of the pelagic system and they operatè on long (e.g. annual plankton succession) and short (e.g. the end of new production, sporadic grazing of swarm feeders) time scales. Connecting investigation of the water column with a high resolution in time in parallel with drifting sediment trap deployments and shipboard experiments with the dominant zooplankters is a promising approach for giving a better understanding of both the origin and the fate of material sinking to the sea floor.
    Keywords: AWI_BioOce; Biological Oceanography @ AWI; DATE/TIME; Date/time end; Duration, number of days; Flux of total mass; Lithogenic, flux; Norwegian Sea; Sample code/label; Trap, sediment; TRAPS; VP-2_trap
    Type: Dataset
    Format: text/tab-separated-values, 55 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Peinert, Rolf; Antia, Avan N; Bauerfeind, Eduard; von Bodungen, Bodo; Haupt, Olaf; Krumbholz, Marita; Peeken, Ilka; Ramseier, René O; Voss, Maren; Zeitzschel, Bernt (2001): Particle flux variability in the polar and Atlantic biogeochemical provinces of the Nordic Seas. In: Schäfer, W; Ritzrau, M; Schlüter & J. Thiede (eds.) The Northern North Atlantic: A Changing Environment, Springer Verlag, Berlin, 500 pp, 53-68, https://doi.org/10.1007/978-3-642-56876-3_4
    Publication Date: 2023-01-13
    Description: A decade of particle flux measurements providse the basis for a comparison of the eastern and western province s of the Nordic Seas. Ice-related physical and biological seasonality as well as pelagic settings jointly control fluxes in the western Polar Province which receive s southward flowing water of Polar origin. Sediment trap data from this realm highlight a predominantly physical flux control which leads to exports of siliceous particle s within the biological marginal ice zone as a prominent contributor. In the northward flowing waters of the eastern Atlanti c Province, feeding strategies, life histories and the succession ofdominant mesozooplankters (copepods and pteropods) are central in controlling fluxes. Furthermore, more calcareous matter is exported here with a shift in flux seasonality towards summer I autumn. Dominant pelagic processes modeled numerically as to their impact on annual organic carbon exports for both provinces confirm that interannual flux variability is related to changes in the respecti ve control mechanisms. Annual organic carbon export s are strikingly similar in the Polar and Atlantic Province s (2.4 and 2.9 g/m**2/y at 500 m depth), despite major differences in flux control. The Polar and Atlantic Provinces, however, can be distinguished according to annual fluxes of opal (1.4 and 0.6 g/m**2/y) and carbonate (6.8 and 10.4 g/m**2/y). Interannual variability may blur this in single years. Thus, it is vital to use multi-annual data sets when including particle exports in general biogeochemical province descriptions. Vertical flux profiles (collections from 500 m, 1000 m in both provinces and 300-600 m above the seafloor deviate from the general vertical decline of fluxes due to particle degradation during sinking. At depths〉 1000 m secondary fluxes (laterally advectedlresuspended particles) are often juxtaposed to primary (pelagic) fluxes, a pattern which is most prominent in the Atlantic Province. Spatial variability within the Atlantic Province remains poorly understood, and the same holds true for interannual variability. No proxies are at hand for this province to quantitatively relate fluxes to physical or biological pelagic properties. For the seasonally ice-covered Polar Province a robust relationship exists between particle export and ambient ice-regime (Ramseier et al. this volume; Ramseier et al. 1999). Spatial flux patterns may be differentiated and interannual variability can be analyzed in this manner to impro ve our ability to couple pelagic export patterns with benthic and geochemical sedimentary processes in seasonally ice-covered seas.
    Keywords: Global Environmental Change: The Northern North Atlantic; SFB313
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
    Publication Date: 2023-01-14
    Keywords: Atlantic_Province; Calcium carbonate; Calcium carbonate, flux; Carbon, organic, particulate; Carbon, organic, particulate, flux per year; DATE/TIME; Date/time end; DEPTH, water; Global Environmental Change: The Northern North Atlantic; Lithogenic, flux; Lithogenic material; Particulate silica, flux; SFB313; Silica, particulate; Total, flux per year; Trap, sediment; TRAPS
    Type: Dataset
    Format: text/tab-separated-values, 150 data points
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  • 7
    Publication Date: 2023-01-14
    Keywords: Calcium carbonate; Calcium carbonate, flux; Carbon, organic, particulate; Carbon, organic, particulate, flux per year; DATE/TIME; Date/time end; DEPTH, water; Global Environmental Change: The Northern North Atlantic; Lithogenic, flux; Lithogenic material; Particulate silica, flux; Polar_Province; SFB313; Silica, particulate; Total, flux per year; Trap, sediment; TRAPS
    Type: Dataset
    Format: text/tab-separated-values, 110 data points
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