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Integrative and Comparative Biology|October 9, 2018
The Temporal and Environmental Context of Early Animal Evolution: Considering All the Ingredients of an "Explosion"Erik A Sperling, Richard G StockeyCurrent Biology : CB|May 7, 2021
Metabolic tradeoffs control biodiversity gradients through geological timeThomas H Boag, William Gearty, Richard G StockeyProceedings of the National Academy of Sciences of the United States of America|October 5, 2021
Decreasing Phanerozoic extinction intensity as a consequence of Earth surface oxygenation and metazoan ecophysiologyRichard G Stockey, Alexandre Pohl, Andy Ridgwell, et al.Proceedings. Biological Sciences|April 10, 2019
Oxygen, temperature and the deep-marine stenothermal cradle of Ediacaran evolutionThomas H Boag, Richard G Stockey, Leanne E Elder, et al.Nature|August 17, 2022
Continental configuration controls ocean oxygenation during the PhanerozoicAlexandre Pohl, Andy Ridgwell, Richard G Stockey, et al.Nature Communications|April 15, 2020
Persistent global marine euxinia in the early SilurianRichard G Stockey, Devon B Cole, Noah J Planavsky, et al.Science Advances|September 3, 2025
Dynamic deep marine oxygenation during the Early and Middle PaleozoicChadlin M Ostrander, Jean Nikolas R Clemente, Richard G Stockey, et al.Science Advances|August 30, 2023
Why the Early Paleozoic was intrinsically prone to marine extinctionAlexandre Pohl, Richard G Stockey, Xu Dai, et al.The Biological Bulletin|December 22, 2022
Breathless through Time: Oxygen and Animals across Earth's HistoryErik A Sperling, Thomas H Boag, Murray I Duncan, et al.Proceedings of the National Academy of Sciences of the United States of America|July 6, 2026
Differences in physiological tolerance to global warming caused the Permian-Triassic transition between the Paleozoic and Modern faunasJ Andres Marquez, Justin L Penn, Richard G Stockey, et al.Pageof 2