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  • 1
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    Leibniz Institut für Ostseeforschung Warnemünde
    In:  Leibniz Institut für Ostseeforschung Warnemünde, Rostock, Germany, 24 pp.
    Publication Date: 2015-02-13
    Description: Trials of pressure neutral system (DNS) within the Azores frontal region.
    Type: Report , NonPeerReviewed
    Format: text
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  • 2
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    Leibniz-Institut für Ostseeforschung Warnemünde
    In:  Leibniz-Institut für Ostseeforschung Warnemünde, Rostock, 20 pp.
    Publication Date: 2015-02-17
    Description: Lisbon (Portugal)- Vigo (Spain), 04.05.2013 to 19.05.2013
    Type: Report , NonPeerReviewed
    Format: text
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  • 3
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    IOW
    In:  IOW, Warnemünde, Germany, 15 pp.
    Publication Date: 2015-02-17
    Description: Dates of Cruise: from 02.09.2010 to 15.09.2010 Areas of Research: Physical Oceanography, Engineering Port Calls: Ponta Delgad (Acores), Funchal (Madeira)
    Type: Report , NonPeerReviewed
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  • 4
    Publication Date: 2018-01-19
    Description: Production and dispersion of coccolithophores are assessed within their ecologic and hydrographic context across enhanced spring chlorophyll production in the surface eastern North Atlantic. Within a 4 day period from 12 to 16 March 2004, a N-S transect from 47 degrees N to 33 degrees N was sampled along 20 degrees W. Water samples from defined depths down to 200 m were analyzed for coccolithophores from 0.45 mu m polycarbonate filters by scanning electron microscopy. At 47 degrees N coccolithophores flourished when euphotic conditions allowed new production at deep mixing, low temperatures, and high nutrient concentrations. Emiliania huxleyi flourished at high turbulence during an early stage of the phytoplankton succession and contributed half of the total coccolithophore assemblage, with up to 150 x 10(3) cells L(-1) and up to 12 x 10(9) cells m(-2) when integrated over the upper 200 m of the water column. Maximum chlorophyll concentrations occurred just north of the Azores Front, at 37 degrees N-39 degrees N, at comparatively low numbers of coccolithophores. To the south, at 35 degrees N-33 degrees N, coccolithophores were abundant within calm and stratified Subtropical Mode Waters, and E. huxleyi was the dominant species again. Although the cell densities of coccolithophores observed here remained below those typical of plankton blooms visible from satellite images, the depth-integrated total mass makes them significant producers of calcite and contributors to the total carbon sedimentation at a much wider range of ecological conditions during late winter and early spring than hitherto assumed.
    Type: Article , PeerReviewed
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  • 5
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    Elsevier
    In:  Deep Sea Research Part I: Oceanographic Research Papers, 57 (8). pp. 988-998.
    Publication Date: 2015-10-19
    Type: Article , PeerReviewed
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  • 6
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    De Gruyter
    In:  Open Geosciences, 4 (4). pp. 531-544.
    Publication Date: 2020-06-15
    Description: The Azores Current originating as a branch of the Gulf Stream is a highly dynamic system in the subtropical North Atlantic. The associated front forms the northeastern boundary of the North Atlantic Subtropical Gyre. In this study we analyzed 42 years of assimilated modeled temperature fields to localize the position of the Azores Front at 22°W and observed a fast north- and southward propagation between 30°N and 37°N on monthly to decadal time scales. The North Atlantic Oscillation with correlated changes of the wind direction was identified as one driving mechanism. As the front is acting as a guide for Rossby waves, the signal of the front’s propagation is transferred to the western Atlantic and, among other atmospheric forcing mechanisms, induces a shifting of the Northern Wall of the Gulf Stream with one year delay. Shallower mixed layer depths in the northern frontal region of the Azores Current caused by the rise of the isotherms lead to nutrient supply and primary production different from those found in the southern frontal region of the current system. A high interannual variability is manifested in deep ocean particle flux, derived from a sediment trap in 2000 m water depth at the mooring site KIEL276 (33°N, 22°W) from 1993 to 2008, which is directly related to the phytoplankton bloom in the euphotic zone. This variability is explained by the propagation of the front and strong variations in the catchment areas of the sediment trap due to the associated eddy activity in the frontal region.
    Type: Article , PeerReviewed
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  • 7
    Publication Date: 2016-05-25
    Description: Salinity is a major factor controlling the distribution of biota in aquatic systems, and most aquatic multicellular organisms are either adapted to life in saltwater or freshwater conditions. Consequently, the saltwater–freshwater mixing zones in coastal or estuarine areas are characterized by limited faunal and floral diversity. Although changes in diversity and decline in species richness in brackish waters is well documented in aquatic ecology, it is unknown to what extent this applies to bacterial communities. Here, we report a first detailed bacterial inventory from vertical profiles of 60 sampling stations distributed along the salinity gradient of the Baltic Sea, one of world's largest brackish water environments, generated using 454 pyrosequencing of partial (400 bp) 16S rRNA genes. Within the salinity gradient, bacterial community composition altered at broad and finer-scale phylogenetic levels. Analogous to faunal communities within brackish conditions, we identified a bacterial brackish water community comprising a diverse combination of freshwater and marine groups, along with populations unique to this environment. As water residence times in the Baltic Sea exceed 3 years, the observed bacterial community cannot be the result of mixing of fresh water and saltwater, but our study represents the first detailed description of an autochthonous brackish microbiome. In contrast to the decline in the diversity of multicellular organisms, reduced bacterial diversity at brackish conditions could not be established. It is possible that the rapid adaptation rate of bacteria has enabled a variety of lineages to fill what for higher organisms remains a challenging and relatively unoccupied ecological niche.
    Type: Article , PeerReviewed
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  • 8
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    GEOMAR Helmholtz-Zentrum für Ozeanforschung
    In:  GEOMAR Report, N. Ser. 013 . GEOMAR Helmholtz-Zentrum für Ozeanforschung, Kiel, Germany, 65 + Anh. pp.
    Publication Date: 2020-10-20
    Type: Report , NonPeerReviewed
    Format: text
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  • 9
    Publication Date: 2023-09-19
    Type: Report , NonPeerReviewed
    Format: text
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