Articles | Volume 4, issue 3
Biogeosciences, 4, 323–329, 2007
Biogeosciences, 4, 323–329, 2007

  19 Jun 2007

19 Jun 2007

A coccolithophore concept for constraining the Cenozoic carbon cycle

J. Henderiks1 and R. E. M. Rickaby2 J. Henderiks and R. E. M. Rickaby
  • 1Stockholm University, Department of Geology and Geochemistry, Svante Arrhenius väg 8C, SE-106 91 Stockholm, Sweden
  • 2Department of Earth Sciences, Oxford University, Parks Road, Oxford OX1 3PR, UK

Abstract. An urgent question for future climate, in light of increased burning of fossil fuels, is the temperature sensitivity of the climate system to atmospheric carbon dioxide (pCO>sub>2). To date, no direct proxy for past levels of pCO2 exists beyond the reach of the polar ice core records. We propose a new methodology for placing a constraint on pCO2 over the Cenozoic based on the physiological plasticity of extant coccolithophores. Specifically, our premise is that the contrasting calcification tolerance of various extant species of coccolithophore to raised pCO2 reflects an "evolutionary memory" of past atmospheric composition. The different times of evolution of certain morphospecies allows an upper constraint of past pCO2 to be placed on Cenozoic timeslices. Further, our hypothesis has implications for the response of marine calcifiers to ocean acidification. Geologically "ancient" species, which have survived large changes in ocean chemistry, are likely more resilient to predicted acidification.

Final-revised paper