There is an extremely significant difference in change of pH, HCO 3 – , CO 3 2– , Ca 2+ , and Mg 2+ ion concentrations and SI between different Mg/Ca ratios at the same time ( Supplementary Tables 1 – 6 ). 3.2.
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The incorporation of Mg<sup>2+</sup> ions into aragonite during biomineralization: Implications for the dolomitization of aragonite.
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