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Alteration of ocean crust provides a strong temperature dependent feedback on the geological carbon cycle and is a primary driver of the Sr-isotopic composition of seawater

Marine GeologyBiogeochemistryEngineeringChemical OceanographyPaleoceanographyGeological Carbon CycleSr-isotopic CompositionMarine ChemistryOceanographyGeochemistryOcean CrustCarbon CycleEarth Science