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Changes in coccolith calcification under stable atmospheric CO2 ArchiMer
Bauke, C.; Meier, Kjs; Kinkel, H.; Baumann, K-h.
Coccolith calcification is known to respond to ocean acidification in culture experiments as well as in present and past oceans. Previous studies basically focus on changes in coccolith weight due to increasing CO2 and the resulting changes in the carbonate system but pay little attention to the influence of other environmental factors. In order to untangle changes in coccolithophore calcification due to environmental factors such as temperature and/or productivity from changes caused by increasing pCO2 and carbonate ion concentration we here present a study on coccolith calcification from the Holocene North Atlantic Ocean. The pre-industrial Holocene with its predominantly stable carbonate system provides the conditions for such a comprehensive analysis....
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Ano: 2013 URL: http://archimer.ifremer.fr/doc/00182/29278/27695.pdf
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