This acidification occurs in a region with a naturally low carbonate ion concentration, and studies suggest that the surface of the Southern Ocean will become undersaturated with respect to
calcium carbonate minerals aragonite and calcite by the end of the century.
Not exact matches
Another important element affecting calcification rates of corals is the
calcium carbonate saturation state of the
mineral aragonite (Cohen et al., 2009; Gattuso et al., 1998; Marshall & Clode, 2002).
While nearly all corals, shells, algae and the like are formed of
calcium carbonate CaCo, most are in the form of the
mineral aragonite, which is stable in the marine environment.
The material that makes up pteropod shells is
aragonite, a common
mineral form of
calcium carbonate, which is also secreted by other marine organisms to form external skeletal material.