Table of Contents

1. Calcium isotopes as a geochemical tracer of carbonate (bio)mineralization, deposition, and diagenesis; 2. Reconstructing the marine Ca cycle in the geologic past; 3. Materials and methods; 4. Case study – end-Permian mass extinction; 5. Future prospects; 6. Key papers.

Promotional Information

Calcium isotopes can be used as a geochemical tracer to quantify rates of carbonate diagenesis in marine sedimentary systems.