In 1988, Rouviere and Wolfe (1) suggested that methane formation from H2 and CO2 by methanogenic archaea could be a cyclical process. Indirect evidence indicated that the first step, the reduction of CO2 to formylmethanofuran, was somehow coupled to the last step, the reduction of the heterodisulfide (CoM-S-S-CoB) to coenzyme M (CoM-SH) and coenzyme B (CoB-SH). Over 2 decades passed until the coupling mechanism was unraveled in 2011: Via flavin-based electron bifurcation, the reduction of CoM-S-S-CoB with H2 provides the reduced ferredoxin (Fig. 1h) required for CO2 reduction to formylmethanofuran (2) (Fig. 1a). However, one question still remained unanswered: How are the intermediates replenished that are removed for the biosynthesis of cell components from CO2 (orange arrows in Fig. 1)? This anaplerotic (replenishing) reaction has recently been identified by Lie et al. (3) as the sodium motive force-driven reduction of ferredoxin with H2 catalyzed by the energy-converting hydrogenase EhaA-T (green arrow in Fig. 1).