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Ocean acidification may increase calcification rates, but at a cost
Ocean acidification is the lowering of pH in the oceans as a result of increasing uptake of atmospheric carbon dioxide. Carbon dioxide is entering the oceans at a greater rate than ever before, reducing the ocean's natural buffering capacity and lowering pH. Previous work on the biological cons...
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| Main Authors: | , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
The Royal Society
2008
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC2587798/ https://ncbi.nlm.nih.gov/pubmed/18460426 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rspb.2008.0343 |
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