Anoxic photogeochemical oxidation of manganese carbonate yields manganese oxide

Significance When oxygenic photosynthesis evolved is debated with an uncertainty of approximately 1 Gy. It is generally assumed that the oxidation of manganese minerals requires biological catalysis or molecular oxygen and therefore is often used as a proxy for the presence of oxygenic photosynthetic organisms. We show that anoxic, abiotic oxidation of the mineral rhodochrosite (MnCO3 ) by UV light forms H2 and manganite (γ-MnOOH). Our results reveal an alternative mechanism for producing manganese oxides from rhodochrosite in the absence of molecular oxygen. These results demonstrate the potential impact of photogeochemical processes on the redox state of transition metals and hence question the interpretation of the rise of atmospheric oxygen based on the oxidation of transition metals, such as Cr isotopes.