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Proceedings 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 of the National Academy of Sciences of the United States of America|May 22, 2013
Surviving rapid climate change in the deep sea during the Paleogene hyperthermalsLaura C Foster, Daniela N Schmidt, Ellen Thomas, et al.Nature Communications|May 28, 2026
Miocene ocean circulation shifted expansive oxygen deficient zones to the AtlanticJanet E Burke, Keyi Cheng, Andy Ridgwell, et al.Global Change Biology|October 27, 2021
Exploring the impact of climate change on the global distribution of non-spinose planktonic foraminifera using a trait-based ecosystem modelMaria Grigoratou, Fanny M Monteiro, Jamie D Wilson, et al.Proceedings of the National Academy of Sciences of the United States of America|December 15, 2020
Bistability in the redox chemistry of sediments and oceansSebastiaan J van de Velde, Christopher T Reinhard, Andy Ridgwell, et al.Science Advances|February 15, 2023
Volcanic CO2 degassing postdates thermogenic carbon emission during the end-Permian mass extinctionYuyang Wu, Ying Cui, Daoliang Chu, et al.Nature|August 17, 2022
Continental configuration controls ocean oxygenation during the PhanerozoicAlexandre Pohl, Andy Ridgwell, Richard G Stockey, et al.Nature|September 27, 2019
Diversity decoupled from ecosystem function and resilience during mass extinction recoverySarah A Alvarez, Samantha J Gibbs, Paul R Bown, et al.Science (New York, N.Y.)|March 12, 2021
Temperature controls carbon cycling and biological evolution in the ocean twilight zoneFlavia Boscolo-Galazzo, Katherine A Crichton, Andy Ridgwell, et al.Geobiology|February 18, 2020
The impact of marine nutrient abundance on early eukaryotic ecosystemsChristopher T Reinhard, Noah J Planavsky, Ben A Ward, et al.Pageof 4