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...
| Main Author: | |
|---|---|
| Other Authors: | |
| Published: |
University of Hawaii at Manoa
2009
|
| Online Access: | http://hdl.handle.net/10125/7017 |
