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Precise measurements of the Calcium (Ca) Isotopes have provided constraints on Ca cycling at global and local scales, and quantified rates of carbonate diagenesis in marine sedimentary systems.
These factors include variations in stable isotopic fractionation factors, the influe.
Key to applying Ca Isotopes as a geochemical tracer of Ca cycling, carbonate (bio)mineralization, and diagenesis is an understanding of the impact of multiple factors potentially impacting Ca Isotopes in the rock record.
Precise measurements of the Calcium (Ca) Isotopes have provided constraints on Ca cycling at global and local scales, and quantified rates of carbonate diagenesis in marine sedimentary systems
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