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. 2021 Apr 6;12:2069. doi: 10.1038/s41467-021-22258-1

Fig. 1. Graphical model of a proposed Archaean littoral oxygen oasis.

Fig. 1

a A diurnal tidal inflow of ferruginous seawater creates an anoxic Fe(II) layer over oxygenic phototrophic Cyanobacterial mats. Photosynthetic oxygen creates green rust (GR) in the upper boundary layer by partial oxidation of Fe(II) during the day. Closer to the Cyanobacterial mats, Fe(III) is the dominant species, as Fe(II) and precipitating GR is completely oxidised. b During the night time, no oxygen is produced by photosynthesis and the littoral zone becomes ferruginous with precipitated Fe(III) oxides and/or GR, produced in the daytime, at the bottom layer. c Tidal outflow transports GR and Fe(III) in the anoxic open ocean, where the remaining Fe(III) can react with Fe(II) to GR. GR and/or Fe(III) sink to the bottom and form deep ocean sediments. High oxygen levels during the day oxidise Fe(II) from the pelagic zone and thereby prevent Fe(II) from reaching the littoral zone. Surplus oxygen not consumed by the oxidation of Fe(II) escapes into the atmosphere leading to localised land weathering, thereby releasing additional nutrients. Additional weathering at the oxygen-rich microbe–mineral interface cannot be excluded. Image created from references6, 12, 13, 17, 18.