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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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| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
National Academy of Sciences
2008
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| Schlagworte: | |
| Online Zugang: | 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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