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    Silicate weathering in anoxic marine sediments (2009)
    IFM-GEOMAR
    In:  IFM-GEOMAR Annual Report, 2008 . pp. 18-19.
    Details
    Publication Date: 2018-10-16
    Description: Weathering of silicate minerals is the major sink for atmospheric CO2 on geological time scales. It has commonly been assumed that this process is only occurring on land. New results, however, show that silicate minerals are also reactive within marine sediments. Most of the metabolic CO2 being produced in marine sediments enriched in organic matter is consumed by this reaction with major implications for the geological carbon cycle.
    Type: Article , NonPeerReviewed
    Format: text
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