A coccolithophore concept for constraining the Cenozoic carbon cycle

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</sub>). To date, no direct proxy for past levels of pCO<sub>2</sub> exists beyond the reach of t...

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Main Authors: J. Henderiks, R. E. M. Rickaby
Format: Article
Language:English
Published: Copernicus Publications 2007-06-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/4/323/2007/bg-4-323-2007.pdf
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spelling doaj-9f2fcd96180648248ec4a6a8b43b10922020-11-24T21:25:11ZengCopernicus PublicationsBiogeosciences1726-41701726-41892007-06-014332332910.5194/bg-4-323-2007A coccolithophore concept for constraining the Cenozoic carbon cycleJ. Henderiks0R. E. M. Rickaby1Stockholm University, Department of Geology and Geochemistry, Svante Arrhenius väg 8C, SE-106 91 Stockholm, SwedenDepartment of Earth Sciences, Oxford University, Parks Road, Oxford OX1 3PR, UKAn 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</sub>). To date, no direct proxy for past levels of pCO<sub>2</sub> exists beyond the reach of the polar ice core records. We propose a new methodology for placing a constraint on pCO<sub>2</sub> 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 pCO<sub>2</sub> reflects an "evolutionary memory" of past atmospheric composition. The different times of evolution of certain morphospecies allows an upper constraint of past pCO<sub>2</sub> 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.http://www.biogeosciences.net/4/323/2007/bg-4-323-2007.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. Henderiks
R. E. M. Rickaby
spellingShingle J. Henderiks
R. E. M. Rickaby
A coccolithophore concept for constraining the Cenozoic carbon cycle
Biogeosciences
author_facet J. Henderiks
R. E. M. Rickaby
author_sort J. Henderiks
title A coccolithophore concept for constraining the Cenozoic carbon cycle
title_short A coccolithophore concept for constraining the Cenozoic carbon cycle
title_full A coccolithophore concept for constraining the Cenozoic carbon cycle
title_fullStr A coccolithophore concept for constraining the Cenozoic carbon cycle
title_full_unstemmed A coccolithophore concept for constraining the Cenozoic carbon cycle
title_sort coccolithophore concept for constraining the cenozoic carbon cycle
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2007-06-01
description 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</sub>). To date, no direct proxy for past levels of pCO<sub>2</sub> exists beyond the reach of the polar ice core records. We propose a new methodology for placing a constraint on pCO<sub>2</sub> 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 pCO<sub>2</sub> reflects an "evolutionary memory" of past atmospheric composition. The different times of evolution of certain morphospecies allows an upper constraint of past pCO<sub>2</sub> 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.
url http://www.biogeosciences.net/4/323/2007/bg-4-323-2007.pdf
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