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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Detalles Bibliográficos
Autores principales: Castillo, Karl D., Ries, Justin B., Bruno, John F., Westfield, Isaac T.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society 2014
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4240989/
https://www.ncbi.nlm.nih.gov/pubmed/25377455
http://dx.doi.org/10.1098/rspb.2014.1856

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4240989/
https://www.ncbi.nlm.nih.gov/pubmed/25377455
http://dx.doi.org/10.1098/rspb.2014.1856

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