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Effects of lower surface ocean pH upon the stability of shallow water carbonate sediments

Tynan, Sarah; Opdyke, Bradley


It is predicted that surface ocean pH will reach 7.9, possibly 7.8 by the end of this century due to increased carbon dioxide (CO2) in the atmosphere and in the surface ocean. While aragonite-rich sediments don't begin to dissolve until a threshold pH of

CollectionsANU Research Publications
Date published: 2011
Type: Journal article
Source: Science of the Total Environment
DOI: 10.1016/j.scitotenv.2010.12.007


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