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M. Debora Iglesias-Rodriguez,1*Paul R. Halloran,2*Rosalind E. M. Rickaby,2Ian R. Hall,3Elena Colmenero-Hidalgo,3John R. Gittins,1Darryl R. H. Green,1Toby Tyrrell,1Samantha J. Gibbs,1Peter von Dassow,4Eric Rehm,5E. Virginia Armbrust,5Karin P. Boessenkool3
Ocean acidification in response to rising atmospheric CO2 partialpressures is widely expected to reduce calcification by marineorganisms. From the mid-Mesozoic, coccolithophores have beenmajor calcium carbonate producers in the world's oceans, todayaccounting for about a third of the total marine CaCO3 production.Here, we present laboratory evidence that calcification andnet primary production in the coccolithophore species Emilianiahuxleyi are significantly increased by high CO2 partial pressures.Field evidence from the deep ocean is consistent with theselaboratory conclusions, indicating that over the past 220 yearsthere has been a 40% increase in average coccolith mass. Ourfindings show that coccolithophores are already responding andwill probably continue to respond to rising atmospheric CO2partial pressures, which has important implications for biogeochemicalmodeling of future oceans and climate.
1 National Oceanography Centre, Southampton, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK. 2 Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK. 3 School of Earth, Ocean and Planetary Sciences, Cardiff University, Main Building, Park Place, Cardiff CF10 3YE, UK. 4 Station Biologique de Roscoff, Place George Teissier, BP 74, 29682 Roscoff Cedex, France. 5 School of Oceanography, Box 357940, University of Washington, Seattle, WA 98195, USA.
* These authors contributed equally to this work.
Present address: Departamento de Geología, Facultad deCiencias, Universidad de Salamanca, 37008 Salamanca, Spain.
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