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Abstract

The anaerobic ethane oxidation performed by seafloor archaea and sulfate-reducing partner bacteria involves largely uncharted biochemistry. This study deciphers the molecular basis of the CO2-generating steps by characterizing the native archaeal enzymes isolated from a thermophilic enrichment culture. While other microorganisms couple these steps to ferredoxin reduction, we found that the CO-dehydrogenase and the formylmethanofuran-dehydrogenase are bound to an F420-reductase module. The crystal structures of these multi-metalloenzyme complexes revealed a [4Fe-4S]-cluster networks electronic bridges coupling C1-oxidation to F420-reduction. Accordingly, both systems exhibit robust F420-reductase activities, which are not detected in methanogenic or methanotrophic relative organisms. We speculate that the whole catabolism of these archaea is reoriented towards F420-reduction, which facilitates the electron transfer to the sulfate-reducing partner, therefore representing the driving force of ethanotrophy.