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Southern Ocean acidification: A tipping point at 450-ppm atmospheric CO(2)
Southern Ocean acidification via anthropogenic CO(2) uptake is expected to be detrimental to multiple calcifying plankton species by lowering the concentration of carbonate ion (CO(3)(2−)) to levels where calcium carbonate (both aragonite and calcite) shells begin to dissolve. Natural seasonal varia...
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Main Authors: | , |
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Formato: | Artigo |
Idioma: | Inglês |
Publicado em: |
National Academy of Sciences
2008
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Assuntos: | |
Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC2596239/ https://ncbi.nlm.nih.gov/pubmed/19022908 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0806318105 |
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