Griffith, Elizabeth M. (Ohio State University), Fantle, Matthew S. (Pennsylvania State University)
Omschrijving
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. Key to applying Ca isotopes as a geochemical tracer is understanding the impact of multiple factors potentially impacting Ca isotopes in the rock record.
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