Reconciling evidence of oxidative weathering and atmospheric anoxia on Archean Earth

Aleisha C. Johnson, Chadlin M. Ostrander, Stephen J. Romaniello, Christopher T. Reinhard, Allison T. Greaney, Timothy W. Lyons, Ariel D. Anbar

Research output: Contribution to journalArticlepeer-review

Abstract

Evidence continues to emerge for the production and low-level accumulation of molecular oxygen (O2) at Earth's surface before the Great Oxidation Event. Quantifying this early O2 has proven difficult. Here, we use the distribution and isotopic composition of molybdenum in the ancient sedimentary record to quantify Archean Mo cycling, which allows us to calculate lower limits for atmospheric O2 partial pressures (PO2) and O2 production fluxes during the Archean. We consider two end-member scenarios. First, if O2 was evenly distributed throughout the atmosphere, then PO2 > 10-6.9 present atmospheric level was required for large periods of time during the Archean eon. Alternatively, if O2 accumulation was instead spatially restricted (e.g., occurring only near the sites of O2 production), then O2 production fluxes >0.01 Tmol O2/year were required. Archean O2 levels were vanishingly low according to our calculations but substantially above those predicted for an abiotic Earth system.

Original languageEnglish (US)
Article numberabj0108
JournalScience Advances
Volume7
Issue number40
DOIs
StatePublished - Oct 2021

ASJC Scopus subject areas

  • General

Fingerprint

Dive into the research topics of 'Reconciling evidence of oxidative weathering and atmospheric anoxia on Archean Earth'. Together they form a unique fingerprint.

Cite this