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Coupling of ferredoxin and heterodisulfide reduction via electron bifurcation in hydrogenotrophic methanogenic archaea

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Kaster,  A. K.
Department of Biochemistry, Alumni, Max Planck Institute for Terrestrial Microbiology, Max Planck Society;

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Moll,  J.
Department of Biochemistry, Alumni, Max Planck Institute for Terrestrial Microbiology, Max Planck Society;

Parey,  K.
Max Planck Society;

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Thauer,  R. K.
Emeriti Biochemistry of Anaerobic Microorganisms, Max Planck Institute for Terrestrial Microbiology, Max Planck Society;

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Citation

Kaster, A. K., Moll, J., Parey, K., & Thauer, R. K. (2011). Coupling of ferredoxin and heterodisulfide reduction via electron bifurcation in hydrogenotrophic methanogenic archaea. PNAS, 108(7), 2981-2986. doi:10.1073/pnas.1016761108.


Cite as: https://hdl.handle.net/21.11116/0000-0007-C245-0
Abstract
In methanogenic archaea growing on H-2 and CO2 the first step in methanogenesis is the ferredoxin-dependent endergonic reduction of CO2 with H-2 to formylmethanofuran and the last step is the exergonic reduction of the heterodisulfide CoM-S-S-CoB with H-2 to coenzyme M (CoM-SH) and coenzyme B (CoB-SH). We recently proposed that in hydrogenotrophic methanogens the two reactions are energetically coupled via the cytoplasmic MvhADG/HdrABC complex. It is reported here that the purified complex from Methanothermobacter marburgensis catalyzes the CoM-S-S-CoB-dependent reduction of ferredoxin with H-2. Per mole CoM-S-S-CoB added, 1 mol of ferredoxin (Fd) was reduced, indicating an electron bifurcation coupling mechanism: 2H(2) + Fd(ox) + CoM-S-S-CoB -> Fd(red)(2-) + CoM-SH + CoB-SH + 2H(+): This stoichiometry of coupling is consistent with an ATP gain per mole methane from 4 H-2 and CO2 of near 0.5 deduced from an H-2-threshold concentration of 8 Pa and a growth yield of up to 3 g/mol methane.