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Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition - Nature Communications

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Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition - Nature Communications

Continental-scale expansion of the East Antarctic Ice Sheet during the Eocene-Oligocene Transition (EOT) is one of the largest non-linear events in Earth's climate history. Declining atmospheric carbon dioxide concentrations and orbital variability triggered glacial expansion and strong feedbacks in the climate system. Prominent among these feedbacks was the repartitioning of biogeochemical cycles between the continental shelves and the deep ocean with falling sea level.

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Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition - Nature Communications

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Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition - Nature Communications

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