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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 4, issue 4 | Copyright
Biogeosciences, 4, 481-492, 2007
© Author(s) 2007. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  06 Jul 2007

06 Jul 2007

Assessing the potential long-term increase of oceanic fossil fuel CO2 uptake due to CO2-calcification feedback

A. Ridgwell1, I. Zondervan2, J. C. Hargreaves3, J. Bijma2, and T. M. Lenton4 A. Ridgwell et al.
  • 1School of Geographical Sciences, University of Bristol, Bristol, BS8 1SS UK
  • 2Biogeosciences, Alfred Wegener Institute for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany
  • 3Frontier Research Center for Global Change, 3173-25 Showa-machi, Kanazawa-ku, Yokohama, Kanagawa 236-0001, Japan
  • 4School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK

Abstract. Plankton manipulation experiments exhibit a wide range of sensitivities of biogenic calcification to simulated anthropogenic acidification of the ocean, with the "lab rat" of planktic calcifiers, Emiliania huxleyi apparently not representative of calcification generally. We assess the implications of this observational uncertainty by creating an ensemble of realizations of an Earth system model that encapsulates a comparable range of uncertainty in calcification response to ocean acidification. We predict that a substantial reduction in marine carbonate production is possible in the future, with enhanced ocean CO2 sequestration across the model ensemble driving a 4–13% reduction in the year 3000 atmospheric fossil fuel CO2 burden. Concurrent changes in ocean circulation and surface temperatures in the model contribute about one third to the increase in CO2 uptake. We find that uncertainty in the predicted strength of CO2-calcification feedback seems to be dominated by the assumption as to which species of calcifier contribute most to carbonate production in the open ocean.

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