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- Redox constraints on a Cenozoic imbalance in the organic carbon cycle
- A process-based ecosystem model (Paleo-BGC) to simulate the dynamic response of Late Carboniferous plants to elevated O2 and aridification
- The pedogenic formation of coal balls by CO2 degassing through the rootlets of arborescent lycopsids
- Analysis of gases in fossil amber
- Model based Paleozoic atmospheric oxygen estimates: a revisit to GEOCARBSULF
- Increase in predator-prey size ratios throughout the Phanerozoic history of marine ecosystems
- Tectonic controls on the long-term carbon isotope mass balance
- Sedimentary Sulfides
- Ocean and Atmosphere Geochemical Proxies Derived from Trace Elements in Marine Pyrite: Implications for Ore Genesis in Sedimentary Basins
- A modeling case for high atmospheric oxygen concentrations during the Mesozoic and Cenozoic
- A Pleistocene ice core record of atmospheric O2 concentrations
- The dipnoan buccal pump reconstructed in 3D and implications for air breathing in Devonian lungfishes
- Body-size reduction in vertebrates following the end-Devonian mass extinction
- The rise of fire: Fossil charcoal in late Devonian marine shales as an indicator of expanding terrestrial ecosystems, fire, and atmospheric change
- Long-term climate forcing by atmospheric oxygen concentrations
- When conifers took flight: a biomechanical evaluation of an imperfect evolutionary takeoff
- Error analysis of CO2 and O2 estimates from the long-term geochemical model GEOCARBSULF
- Kaolin: From Ancient Porcelains to Nanocomposites
- Paleobiological Perspectives on Early Eukaryotic Evolution
- Environmental changes in the Late Ordovician-early Silurian: Review and new insights from black shales and nitrogen isotopes
- Clay mineral evolution
- Natural history of a plant trait: branch-system abscission in Paleozoic conifers and its environmental, autecological, and ecosystem implications in a fire-prone world
- Authigenic Carbonate and the History of the Global Carbon Cycle
- From black mud to earth system science: A scientific autobiography
- On flying insect size and Phanerozoic atmospheric oxygen
- Environmental and biotic controls on the evolutionary history of insect body size
- Earth's Redox History
- Geologic constraints on the glacial amplification of Phanerozoic climate sensitivity
- Baseline intrinsic flammability of Earth's ecosystems estimated from paleoatmospheric oxygen over the past 350 million years
- Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fish