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  • 1
    Publication Date: 2008-04-19
    Description: Ocean acidification in response to rising atmospheric CO2 partial pressures is widely expected to reduce calcification by marine organisms. From the mid-Mesozoic, coccolithophores have been major calcium carbonate producers in the world's oceans, today accounting for about a third of the total marine CaCO3 production. Here, we present laboratory evidence that calcification and net primary production in the coccolithophore species Emiliania huxleyi are significantly increased by high CO2 partial pressures. Field evidence from the deep ocean is consistent with these laboratory conclusions, indicating that over the past 220 years there has been a 40% increase in average coccolith mass. Our findings show that coccolithophores are already responding and will probably continue to respond to rising atmospheric CO2 partial pressures, which has important implications for biogeochemical modeling of future oceans and climate.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Iglesias-Rodriguez, M Debora -- Halloran, Paul R -- Rickaby, Rosalind E M -- Hall, Ian R -- Colmenero-Hidalgo, Elena -- Gittins, John R -- Green, Darryl R H -- Tyrrell, Toby -- Gibbs, Samantha J -- von Dassow, Peter -- Rehm, Eric -- Armbrust, E Virginia -- Boessenkool, Karin P -- New York, N.Y. -- Science. 2008 Apr 18;320(5874):336-40. doi: 10.1126/science.1154122.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉National Oceanography Centre, Southampton, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18420926" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; *Calcification, Physiologic ; Calcium Carbonate/analysis ; *Carbon Dioxide ; Eukaryota/growth & development/*physiology ; Geologic Sediments/chemistry ; Hydrogen-Ion Concentration ; Oceans and Seas ; Photosynthesis ; Phytoplankton/growth & development/*physiology
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2011-04-09
    Description: Erba et al. (Reports, 23 July 2010, p. 428) attributed calcareous nannofossil morphology and assemblage changes across Cretaceous Oceanic Anoxic Event 1a to the effects of surface ocean acidification. We argue that the quality of carbonate preservation in these sequences, the unsupported assumptions of the biotic response to acidity, and the absence of independent proxy estimates for ocean pH or atmospheric pCO(2) render this conclusion questionable.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Gibbs, Samantha J -- Robinson, Stuart A -- Bown, Paul R -- Jones, Tom Dunkley -- Henderiks, Jorijntje -- New York, N.Y. -- Science. 2011 Apr 8;332(6026):175; author reply 175. doi: 10.1126/science.1199459.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉School of Ocean and Earth Sciences, National Oceanography Centre, Southampton, European Way, Southampton, SO14 3ZH, UK. sxg@noc.soton.ac.uk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21474738" target="_blank"〉PubMed〈/a〉
    Keywords: Adaptation, Physiological ; Atmosphere ; *Calcification, Physiologic ; Calcium Carbonate/analysis/*chemistry ; Carbon Dioxide ; *Ecosystem ; *Fossils ; Geologic Sediments ; Hydrogen-Ion Concentration ; Oceans and Seas ; Oxygen ; *Plankton/cytology/physiology ; Seawater/*chemistry ; Time
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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