Cover -- Title page -- Copyright page -- Local and Global Controls on Carbon Isotope Chemostratigraphy -- Contents -- 1 Introduction -- 2 Systematics of Carbon Isotope Chemostratigraphy -- 2.1 Development and History -- 2.2 One-box Model of the Carbon Cycle -- 3 Local Controls and Issues of Fidelity and Diagenesis -- 3.1 Local Variability in Carbon Sources and Sinks -- 3.1.1 Riverine Input -- 3.1.2 Submarine Groundwater Discharge -- 3.1.3 Diurnal Productivity -- 3.1.4 Air-Sea Gas Exchange -- 3.1.5 Redox and Authigenic Mineralization -- 3.2 Carbonate Mineralogy, Fractionation, and Mixing
3.3 Carbonate Diagenesis -- 3.3.1 Calcium Isotopes -- 4 Case Studies -- 4.1 Paleocene-Eocene Thermal Maximum -- 4.2 The Great Bahamas Bank -- 4.3 The Neoproterozoic -- 5 Future Prospects -- 6 Designated Key Papers -- References -- Acknowledgments
Summary
Over million-year timescales, the geologic cycling of carbon controls long-term climate and the oxidation of Earth's surface. Inferences about the carbon cycle can be made from time series of carbon isotopic ratios measured from sedimentary rocks
Bibliography
Includes bibliographical references
Notes
Description based on online resource; title from digital title page (viewed on April 15, 2022)
