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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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| Publicado no: | Proc Biol Sci |
|---|---|
| Main Authors: | , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
The Royal Society
2014
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| Assuntos: | |
| Acesso em linha: | 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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