Erik A. Sperling
Affiliations: | Stanford University, Palo Alto, CA |
Area:
paleobiologyGoogle:
"Erik Sperling"Parents
Sign in to add mentorDerek Ernest Gilmor Briggs | grad student | 2010 | Yale | |
(Molecular paleobiology and early animal evolution.) | ||||
David T Johnston | post-doc | 2010-2015 | (Chemistry Tree) |
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Publications
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Boag TH, Busch JF, Gooley JT, et al. (2024) Deep-water first occurrences of Ediacara biota prior to the Shuram carbon isotope excursion in the Wernecke Mountains, Yukon, Canada. Geobiology. 22: e12597 |
Wei GY, Zhao M, Sperling EA, et al. (2024) Lithium isotopic constraints on the evolution of continental clay mineral factory and marine oxygenation in the earliest Paleozoic Era. Science Advances. 10: eadk2152 |
Sperling EA, Boag TH, Duncan MI, et al. (2022) Breathless through Time: Oxygen and Animals across Earth's History. The Biological Bulletin. 243: 184-206 |
Spinks SC, Sperling EA, Thorne RL, et al. (2022) Mesoproterozoic surface oxygenation accompanied major sedimentary manganese deposition at 1.4 and 1.1 Ga. Geobiology |
Stockey RG, Pohl A, Ridgwell A, et al. (2021) Decreasing Phanerozoic extinction intensity as a consequence of Earth surface oxygenation and metazoan ecophysiology. Proceedings of the National Academy of Sciences of the United States of America. 118 |
Sperling EA, Melchin MJ, Fraser T, et al. (2021) A long-term record of early to mid-Paleozoic marine redox change. Science Advances. 7 |
Farrell ÚC, Samawi R, Anjanappa S, et al. (2021) The Sedimentary Geochemistry and Paleoenvironments Project. Geobiology |
Rooney AD, Cantine MD, Bergmann KD, et al. (2020) Calibrating the coevolution of Ediacaran life and environment. Proceedings of the National Academy of Sciences of the United States of America |
Laakso TA, Sperling EA, Johnston DT, et al. (2020) Ediacaran reorganization of the marine phosphorus cycle. Proceedings of the National Academy of Sciences of the United States of America |
Stockey RG, Cole DB, Planavsky NJ, et al. (2020) Persistent global marine euxinia in the early Silurian. Nature Communications. 11: 1804 |