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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...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group
2016
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4738325/ https://www.ncbi.nlm.nih.gov/pubmed/26838480 http://dx.doi.org/10.1038/srep20284 |