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The reef-building coral Siderastrea siderea exhibits parabolic responses to ocean acidification and warming
Anthropogenic increases in atmospheric CO(2) over this century are predicted to cause global average surface ocean pH to decline by 0.1–0.3 pH units and sea surface temperature to increase by 1–4°C. We conducted controlled laboratory experiments to investigate the impacts of CO(2)-induced ocean acid...
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| Foilsithe in: | Proc Biol Sci |
|---|---|
| Main Authors: | , , , |
| Formáid: | Artigo |
| Teanga: | Inglês |
| Foilsithe: |
The Royal Society
2014
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| Ábhair: | |
| Rochtain Ar Líne: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4240989/ https://ncbi.nlm.nih.gov/pubmed/25377455 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rspb.2014.1856 |
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