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GEOMAR Library Ocean Research Information Access

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  • OceanRep  (5)
  • OceanRep: Article in a Scientific Journal - without review  (4)
  • OceanRep: Thesis - not published by a publisher  (1)
Document type
  • OceanRep  (5)
Source
Publisher
Years
  • 1
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    Unknown
    Der ozeanische Kalkregen. (2004)
    Wissenschaftliche Verlagsgesellschaft
    In:  Naturwissenschaftliche Rundschau, 12 . pp. 686-688.
    Details
    Publication Date: 2017-03-20
    Type: Article , NonPeerReviewed
    Location Call Number Limitation Availability
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    OceanRep: Article in a Scientific Journal - without review
  • 2
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    Eis im Tropenklima der Kreide? (2008)
    Wissenschaftliche Verlagsgesellschaft
    In:  Naturwissenschaftliche Rundschau, 6 . pp. 299-300.
    Details
    Publication Date: 2017-03-20
    Type: Article , NonPeerReviewed
    Location Call Number Limitation Availability
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    OceanRep: Article in a Scientific Journal - without review
  • 3
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    Das andere CO2-Problem: Ozeanversauerung (2008)
    Wissenschaftliche Verlagsgesellschaft
    In:  Naturwissenschaftliche Rundschau, 11 . pp. 579-580.
    Details
    Publication Date: 2017-03-20
    Type: Article , NonPeerReviewed
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    OceanRep: Article in a Scientific Journal - without review
  • 4
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    Biological mechanism for enhanced carbon consumption in the ocean (2008)
    IFM-GEOMAR
    In:  IFM-GEOMAR Annual Report, 2007 . pp. 37-38.
    Details
    Publication Date: 2018-10-17
    Description: Throughout Earth’s history, the ocean has played a crucial role in modulating atmospheric carbon dioxide through a variety of physical, chemical and biological processes. The same processes are involved in the ocean’s response to anthropogenic perturbations of the global carbon cycle. A key process responsible for about three quarters of the surface to deep-ocean gradient in dissolved inorganic carbon (DIC) is the biological carbon pump. This transports carbon bound by photosynthesis from the sunlit surface layer to the deep ocean. Integrated over the global ocean, the bioticallydriven surface to deep-ocean DIC gradient corresponds to a carbon pool 3.5 times larger than the total amount of atmospheric carbon dioxide. Hence, small changes in this pool, for example, caused by biological responses to ocean change, would have a strong affect on atmospheric CO2.
    Type: Article , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
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    OceanRep: Article in a Scientific Journal - without review
  • 5
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    Cellular Inorganic Carbon Fluxes in the Coccolithosphore 〈em〉Emiliania huxleyi〈/em〉 and Its Relevance for Marine Carbon Cycling (2005)
    Details
    Publication Date: 2023-01-19
    Description: This thesis investigates several processes relevant for carboncycling on various time scales.The publications deal with processes on time scales ofmillions of years (climate change in the Pleistocene), hundreds andtens of thousands of years (impact of calcification on atmospheric CO2 atglacial/interglacial change), hours to minutes (CCM activity ofphytoplankton) to seconds and micro seconds (kinetics in the carbonate system).
    Type: Thesis , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
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    OceanRep: Thesis - not published by a publisher
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