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  • 1
    Keywords: Hochschulschrift ; Ostsee ; Holozän ; Kieselalgen ; Palökologie ; Paläoozeanographie ; Paläogeografie ; Ostsee ; Kieselalgen ; Meeressediment ; Meeresökologie ; Meeresgeologie ; Stratigraphie ; Ostsee ; Holozän ; Kieselalgen ; Palökologie ; Paläoozeanographie ; Paläogeografie ; Ostsee ; Kieselalgen ; Meeressediment ; Meeresökologie ; Meeresgeologie ; Stratigraphie
    Type of Medium: Book
    Pages: 199 S. , Ill., graph. Darst., Kt.
    Series Statement: Berichte / Geologisch-Paläontologisches Institut und Museum, Christian-Albrechts-Universität Kiel 9
    Language: German
    Note: Zugl.: Kiel, Univ., Diss., 1985
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  • 2
    Keywords: Hochschulschrift
    Type of Medium: Book
    Pages: 73 Bl , Ill., graph. Darst., Kt , 1 Beil.
    Language: German
    Note: Kiel, Univ., Dipl.-Arb. (Teil I), 1978
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  • 3
    Keywords: Paläontologie ; Ozeanographie ; Sedimentation ; Polarmeer
    Type of Medium: Book
    Pages: VIII, 312 S , Ill., graph. Darst., Kt
    Language: German
    Note: [Umschlag-, Vort.:] Geologische Geschichte der Polarmeere
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Polar research 7 (1989), S. 0 
    ISSN: 1751-8369
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geography , Geosciences
    Notes: During the summer 1987 expedition of the polar research vessel‘Polarstern’in the Eurasian Basin of the Arctic Ocean, sea ice at about 84-86°N and 20-30°E was found to have high concentrations of particulate material. The particle-laden ice occurred in patches which often darkened more than half the ice surface at our northernmost positions. Much of this ice appeared to be within the Siberian Branch of the Transpolar Drift stream, which transports deformed, multi-year ice from the Siberian shelves westward across the Eurasian Basin. Lithogenic sediment, which is the major component of the particulate material, may have been incorporated during ice formation on the shallow Siberian seas. Diatoms collected from the particle-rich ice surfaces support this conclusion, as assemblages were dominated by a marine benthic species similar to that reported from sea ice off the coast of northeast Siberia. Based on drift trajectories of buoys deployed on the ice it appears that much of the particle-laden ice exited the Arctic Ocean through the Fram Strait and joined the East Greenland Current.Very different sea ice characteristics were found east of the Yermak Plateau and north of Svalbard and Frans Josef Land up to about 83-84°N. Here sea ice was thinner, less deformed, with lower amounts of lithogenic sediment and diatoms. The diatom assemblage was dominated by planktonic freshwater species. Trajectories of buoys deployed on sea ice in this region indicated a tendency for southward transport to the Yermak Plateau or into the Barents Sea.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Polar biology 12 (1992), S. 373-385 
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary This study gives a first inventory of radiolarian taxa collected with sediment traps in different areas of the Southern Ocean (Drake Passage, Powell Basin and Bransfield Strait). It includes 66 taxa or taxa groups of which 46 were already described. Two previously described species groups and 20, yet undescribed, taxa are documented. The name Protocystis bicornis (Haecker) is replaced by P. spinosus as it is a later homonym of P. bicornis (Borgert). The occurrence pattern of the radiolarian taxa indicates distinct differences in the species composition between neritic environments (Bransfield Strait and Powell Basin) and pelagic, open ocean conditions (Drake Passage).
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Polar biology 12 (1992), S. 357-372 
    ISSN: 1432-2056
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary The study of radiolarians collected during sediment trap experiments in the Drake Passage, the northern Powell Basin, and the King George Basin of the Bransfield Strait provides new information on the fluxes of radiolarian shells in Antarctic waters, on the annual flux pattern, the species distribution and its ecological significance, and on alteration processes of the radiolarian shells in the water column and at the sediment/water interface. A 28-month monitoring with time-series sediment traps in the Bransfield Strait indicates an annual flux pattern characterized by short-term flux pulses during austral summer, which reach daily fluxes of up to 5 × 103 shells m−2 and which account for more than 90% of the total annual flux. The distinct seasonal variations are linked to variations in the sea ice coverage. Other controlling factors are the production of phytoplankton and the impact by zooplankton grazers, e.g., krill. During the summer flux pulses the vertical fluxes of radiolarians range between ca. 3 and 21 × 104 shells m−2, values that are one or more orders of magnitudes lower than fluxes observed at sites in the tropical and northern high-latitude ocean. Significant lateral transport of radiolarians was documented during the austral summer in the Bransfield Strait by a factor of 10 increase of the radiolarian flux in the lower portion of the water column and the species composition trapped in deeper waters. Radiolarian assemblages associated with pelagic and neritic environments characterized by typical Antarctic taxa (Antarctissa spp.) and a group of species with bipolar distribution (e.g. Plectacantha oikiskos, Phormacantha hystrix), respectively, are distinguished. While the signal of polycystine radiolarians is relatively well recorded in the sediments, the shells of phaeodarians, which were observed at fluxes of up to 1 × 103 shells m−2day−1 in the upper portion of the water column, are almost completely dissolved during settling through the water column.
    Type of Medium: Electronic Resource
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  • 7
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    Pergamon Press
    In:  Deep Sea Research Part A. Oceanographic Research Papers, 39 (2). S525-S538.
    Publication Date: 2015-07-21
    Description: During R.V. Polarstern expeditions ARK IV/3 and ARK VI/1, well preserved diatom assemblages were recovered from particle-laden sea ice collected from the western Barents Shelf and the Arctic Ocean between Svalbard (81°N) and the Nansen-Gakkel Ridge (86°N). Distinct variations in the abundance pattern and species composition of diatoms were found north and south of ca 83°N. Highest diatom concentrations were encountered in multi-year sea ice in the core of the Transpolar Drift Stream between 83 and 86°N. In this area diatom assemblages are dominated by marine-?brackish benthic species. Apparently, these assemblages originate in shelf waters north and east of Siberia, where they are incorporated into the sea ice as a bottom ice assemblage. During the transport of the ice floes across the Eurasian Basin within the Transpolar Drift Stream, seasonal basal freezing and surface melting processes may have led to an accumulation of diatoms at the sea ice surface. South of ca 83°N the sea ice samples contained significantly lower numbers of diatoms, dominated by freshwater taxa. Between 83 and 81°N these assemblages are dominated by planktonic freshwater taxa, but on the Barents Sea Shelf east of Svalbard significant numbers of benthic freshwater taxa and benthic marine-?brackish species also are found. This ice may originate in the Barents Sea and/or the Kara Sea, which receive a large influx of freshwater from Siberian rivers.
    Type: Article , PeerReviewed
    Format: text
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  • 8
    Publication Date: 2016-02-15
    Description: A porcellanite layer, probably younger than 0.6-0.4 Ma, of a nearly monomineralic composition of opal-CT was sampled on the Southwest Indian Ridge during Polarstern cruise ANT-VI/3. The intense cementation of the rock, together with recent findings by the Ocean Drilling Program (Legs 113 and 120) and the occurrence of a unique older porcellanite from Eltanin Core 47-15, provides evidence of very early silica precipitation in pure diatom oozes of the Southern Ocean. Such porcellanites occur in shallowly buried young sediments and provide a contrast to the established concepts of porcellanite formation.
    Type: Article , PeerReviewed
    Format: text
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  • 9
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    Unknown
    In:  [Talk] In: First Bilateral Workshop on Russian-German Cooperation on Kurile-Kamchatka and the Aleutean Marginal Sea-Island Arc Systems, 27.04.-01.05, Petropavlovsk-Kamchatsky, Russia .
    Publication Date: 2012-02-23
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 10
    Publication Date: 2019-09-23
    Description: During the summer 1987 expedition of the polar research vessel‘Polarstern’in the Eurasian Basin of the Arctic Ocean, sea ice at about 84-86°N and 20-30°E was found to have high concentrations of particulate material. The particle-laden ice occurred in patches which often darkened more than half the ice surface at our northernmost positions. Much of this ice appeared to be within the Siberian Branch of the Transpolar Drift stream, which transports deformed, multi-year ice from the Siberian shelves westward across the Eurasian Basin. Lithogenic sediment, which is the major component of the particulate material, may have been incorporated during ice formation on the shallow Siberian seas. Diatoms collected from the particle-rich ice surfaces support this conclusion, as assemblages were dominated by a marine benthic species similar to that reported from sea ice off the coast of northeast Siberia. Based on drift trajectories of buoys deployed on the ice it appears that much of the particle-laden ice exited the Arctic Ocean through the Fram Strait and joined the East Greenland Current. Very different sea ice characteristics were found east of the Yermak Plateau and north of Svalbard and Frans Josef Land up to about 83-84°N. Here sea ice was thinner, less deformed, with lower amounts of lithogenic sediment and diatoms. The diatom assemblage was dominated by planktonic freshwater species. Trajectories of buoys deployed on sea ice in this region indicated a tendency for southward transport to the Yermak Plateau or into the Barents Sea.
    Type: Article , PeerReviewed
    Format: text
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