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Joachim Segschneider and Jørgen Bendtsen Temperature-dependent remineralization in a warming ocean increases surface pCO2 through changes in marine ecosystem composition Global Biogeochemical Cycles 27

Version of Record online: 3 DEC 2013 | DOI: 10.1002/2013GB004684

Key Points

  • Temperature-dependent remineralization included in an Earth System Model
  • Changes in marine ecosystem cause alkalinity-driven release of carbon
  • Oceanic carbon sink additionally reduced by 0.2 GtC per year by 2100

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