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- Reconciling atmospheric CO2, weathering, and calcite compensation depth across the Cenozoic
- Ocean and Atmosphere Geochemical Proxies Derived from Trace Elements in Marine Pyrite: Implications for Ore Genesis in Sedimentary Basins
- A Pleistocene ice core record of atmospheric O2 concentrations
- Long-term climate forcing by atmospheric oxygen concentrations
- Environmental changes in the Late Ordovician-early Silurian: Review and new insights from black shales and nitrogen isotopes
- Section 3. Introduction to the Geochemical Evolution of the Earth's Ecosphere
- Section 6. Deep Time: Modelling of Atmospheric CO2 and the Marine CO2-Carbonic Acid-Carbonate System
- Section 4. Deep Time: Observational Evidence from the Sedimentary Rock Record
- Section 7. Synthesis of Ocean-Atmosphere-Carbonate Sediment Evolution During the Phanerozoic
- Geologic constraints on the glacial amplification of Phanerozoic climate sensitivity
- Influences of alkalinity and pCO2 on CaCO3 nucleation from estimated Cretaceous composition seawater representative of "calcite seas"
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- Regulating continent growth and composition by chemical weathering
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- Comment: MAGic: A phanerozoic model for the geochemical cycling of major rock-forming components: (Comment on "MAGic: A Phanerozoic model for the geochemical cycling of major rock-forming components" by Rolf S. Arvidson, Fred T. Mackenzie and Michael Guidry, American Journal of Science, v. 306, p. 135 190.)
- Comment: Mesozoic Atmospheric Oxygen: (Comment on "MAGic: A phanerozoic model for the geochemical cycling of major rock-forming components" by Rolf S. Arvidson, Fred T. Mackenzie and Michael Guidry, American Journal of Science, v. 306, p. 135-190.)
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- The Weathering of Sedimentary Organic Matter as a Control on Atmospheric O2: II. Theoretical Modeling