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• W2057984558 startingPage "2031" @default.
• W2057984558 abstract "Ocean acidification is likely to impact the calcification potential of marine organisms. In part due to the covarying nature of the ocean carbonate system components, including pH and CO2 and CO32− levels, it remains largely unclear how each of these components may affect calcification rates quantitatively. We develop a process-based bioenergetic model that explains how several components of the ocean carbonate system collectively affect growth and calcification rates in Emiliania huxleyi, which plays a major role in marine primary production and biogeochemical carbon cycling. The model predicts that under the IPCC A2 emission scenario, its growth and calcification potential will have decreased by the end of the century, although those reductions are relatively modest. We anticipate that our model will be relevant for many other marine calcifying organisms, and that it can be used to improve our understanding of the impact of climate change on marine systems." @default.
• W2057984558 created "2016-06-24" @default.
• W2057984558 creator A5002628927 @default.
• W2057984558 creator A5062282222 @default.
• W2057984558 date "2014-04-15" @default.
• W2057984558 modified "2023-09-25" @default.
• W2057984558 title "Dynamic energy budget modeling reveals the potential of future growth and calcification for the coccolithophore<i>E</i><i>miliania huxleyi</i>in an acidified ocean" @default.
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• W2057984558 doi "https://doi.org/10.1111/gcb.12547" @default.
• W2057984558 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/24526588" @default.
• W2057984558 hasPublicationYear "2014" @default.
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