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Seawater carbonate chemistry, calcification and dissolution response, and ske...
Increasing atmospheric pCO2 reduces the saturation state of seawater with respect to the aragonite, high-Mg calcite (Mg/Ca > 0.04), and low-Mg calcite (Mg/Ca < 0.04)... -
Seawater carbonate chemistry and hydrogen ions and carbonate chemistry in cal...
A generalized physicochemical model of the response of marine organisms' calcifying fluids to CO2-induced ocean acidification is proposed. The model is based upon the hypothesis... -
Seawater carbonate chemistry and biological processes during experiments with...
Anthropogenic elevation of atmospheric pCO2 is predicted to cause the pH of surface seawater to decline by 0.3-0.4 units by 2100 AD, causing a 50% reduction in seawater [CO3]...