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Simulated effect of calcification feedback on atmospheric CO(2) and ocean acidification

Ocean uptake of anthropogenic CO(2) reduces pH and saturation state of calcium carbonate materials of seawater, which could reduce the calcification rate of some marine organisms, triggering a negative feedback on the growth of atmospheric CO(2). We quantify the effect of this CO(2)-calcification fe...

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Publicat a:Sci Rep
Autors principals: Zhang, Han, Cao, Long
Format: Artigo
Idioma:Inglês
Publicat: Nature Publishing Group 2016
Matèries:
Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC4738325/
https://ncbi.nlm.nih.gov/pubmed/26838480
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep20284
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