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It is generally accepted that most of the oceanic CaCO3 production is biogenic, whereas homogeneous, inorganic CaCO3 nucleation and precipitation from seawater is inhibited by the presence of other seawater constituents, including dissolved organic carbon. Notwithstanding, heterogeneous CaCO3 precipitation (HCP) from supersaturated seawater onto solid surfaces is well documented, evidence for HCP...
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