Were Neoarchean atmospheric methane hazes and early Paleoproterozoic glaciations driven by the rise of oxygen in surface environments?
Anshuman Swain, Alan Jay Kaufman, Marcin Kalinowski, Stephanie A. Yarwood, William F. Fagan
The paper uses a dynamical model to show that oxygen rise drove methane cycle cyclicity, linking it to ancient climate and glacial events.
Earth and Planetary Science Letters · Oct 1, 2024Peer-reviewedSystems Biology