Post-mesozoic rapid increase of seawater Mg/Ca due to enhanced mantle-seawater interaction.

Sci Rep · 2013 · PMC3783036 · PMID 24067442

Europe PMC DOI

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may be significantno p-value reported

Although, low-T MORP-seawater reactions at ridge flanks may be significant sources of Mg, we did not consider them, as they are difficult to quantify.

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