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Coccolithophores pp 99–125Cite as

Coccolithophores and the biological pump: responses to environmental changes

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Summary

Coccolithophores, which are considered to be the most productive calcifying organisms on earth, play an important role in the marine carbon cycle. The formation of calcite skeletons in the surface layer and their subsequent sinking to depth modifies upper-ocean alkalinity and directly affects air/sea CO2 exchange. Recent work indicates that the productivity and distribution of coccolithophores are sensitive to CO2-related changes in environmental conditions, both directly through acidification of surface seawater and indirectly through increasing upper-ocean thermal stratification. To assess possible responses of this group we examine the physiology and ecology of coccolithophores with regard to expected environmental changes. Potential feedbacks to atmospheric CO2 increase, as could arise from changes in photosynthesis and calcification as well as from a shift in the dominance of coccolithophores, may be crucial when trying to forecast future climate change.

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Authors and Affiliations

  1. Pelagic Ecosystems, Alfred Wegener Institute for Polar and Marine Research, Am Handelshafen 12, D-27570, Bremerhaven, Germany

    Björn Rost

  2. Marine Biogeochemistry, Institute for Marine Research, University of Kiel, Duesternbrooker Weg 20, 24105, Kiel, Germany

    Ulf Riebesell

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  1. Björn Rost
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Editors and Affiliations

  1. Geological Institute, ETH-Zentrum, 8092, Zürich, Switzerland

    Hans R. Thierstein

  2. Department of Palaeontology, The Natural History Museum, Cromwell Road, SW7 5BD, London, UK

    Jeremy R. Young

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Rost, B., Riebesell, U. (2004). Coccolithophores and the biological pump: responses to environmental changes. In: Thierstein, H.R., Young, J.R. (eds) Coccolithophores. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-06278-4_5

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  • DOI: https://doi.org/10.1007/978-3-662-06278-4_5

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