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In the ferruginous and anoxic early Earth oceans, photoferrotrophy drove most of the biological production before the advent of oxygenic photosynthesis, but its association with ferric iron (Fe 3+ ) dependent anaerobic methane (CH 4 ) oxidation (AOM) has been poorly investigated. We studied AOM in Kabuno Bay, a modern analogue to the Archean Ocean (anoxic bottom waters and dissolved Fe concentrations > 600 µmol L −1 ). Aerobic and anaerobic CH 4  oxidation rates up to 0.12 ± 0.03 and 51 ± 1 µmol L −1  d −1 , respectively, were put in evidence. In the Fe oxidation–reduction zone, we observed high concentration of Bacteriochlorophyll e (biomarker of the anoxygenic photoautotrophs), which co-occurred with the maximum CH 4  oxidation peaks, and a high abundance of Candidatus Methanoperedens, which can couple AOM to Fe 3+  reduction. In addition, comparison of measured CH 4  oxidation rates with electron acceptor fluxes suggest that AOM could mainly rely on Fe 3+  produced by photoferrotrophs. Further experiments specifically targeted to investigate the interactions between photoferrotrophs and AOM would be of considerable interest. Indeed, ferric Fe 3+ -driven AOM has been poorly envisaged as a possible metabolic process in the Archean ocean, but this can potentially change the conceptualization and modelling of metabolic and geochemical processes controlling climate conditions in the Early Earth.

The possible occurrence of iron-dependent anaerobic methane oxidation in an Archean Ocean analogue