Climate change and anthropogenic effects on shallow-water carbonate biogeochemistry
As a consequence of anthropogenic activities, future projections suggest that the saturation state of surface ocean waters with respect to carbonate minerals will decline during the twenty-first century owing to increasing atmospheric CO2. As a result calcareous organisms could have difficulty calci...
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University of Hawaii at Manoa
2009
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| Online Access: | http://hdl.handle.net/10125/7017 |