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Updated: Jul 3, 2025

Laboratory Simulation of an IronII-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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Oxygen rise in the tropical upper ocean during the Paleocene-Eocene Thermal Maximum

Simone Moretti1,2, Alexandra Auderset1,3, Curtis Deutsch4

  • 1Climate Geochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany.

Science (New York, N.Y.)
|February 15, 2024
PubMed

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