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Limited oxygen production in the Mesoarchean ocean


"The Archean Eon was a time of predominantly anoxic Earth surface conditions, where anaerobic processes controlled bioessential element cycles. In contrast to “oxygen oases” well documented for the Neoarchean [2.8 to 2.5 billion years ago (Ga)], the magnitude, spatial extent, and underlying causes of possible Mesoarchean (3.2 to 2.8 Ga) surface-ocean oxygenation remain controversial. [...]"

Source: PNAS
Authors: Frantz Ossa Ossa et al.
DOI: 10.1073/pnas.1818762116

Read the full article here.