Abstract

Interspecies hydrogen transfer in anoxic ecosystems is essential for the complete microbial breakdown of organic matter to methane. Acetogenic bacteria are key players in anaerobic food webs and have been considered as prime candidates for hydrogen cycling. We have tested this hypothesis by mutational analysis of the hydrogenase in the model acetogen Acetobacterium woodii. Hydrogenase-deletion mutants no longer grew on H2 + CO2 or organic substrates such as fructose, lactate, or ethanol. Heterotrophic growth could be restored by addition of molecular hydrogen to the culture, indicating that hydrogen is an intermediate in heterotrophic growth. Indeed, hydrogen production from fructose was detected in a stirred-tank reactor. The mutant grew well on organic substrates plus caffeate, an alternative electron acceptor that does not require molecular hydrogen but NADH as reductant. These data are consistent with the notion that molecular hydrogen is produced from organic substrates and then used as reductant for CO2 reduction. Surprisingly, hydrogen cycling in A. woodii is different from the known modes of interspecies or intraspecies hydrogen cycling. Our data are consistent with a novel type of hydrogen cycling that connects an oxidative and reductive metabolic module in one bacterial cell, “intracellular syntrophy.”

Highlights

  • Molecular hydrogen is present only in trace concentrations (550 parts per billion) in the Earth’s atmosphere [1], but plays an important part in the global carbon cycle and is a major constituent of microbial metabolism

  • To delete the genes coding for the two major subunits HydB (Awo_c26980) and HydA (Awo_c26970) of the electron-bifurcating hydrogenase encoded by the hydCEDBA operon (Awo_c27010Awo_c26970), the suicide plasmid pMTL_AW_KO2 was generated

  • Isolation of mutants using fructose as only carbon source failed. Since this may have been caused by the lack of molecular hydrogen produced by HydABCD, hydrogen was added to the culture

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Summary

Introduction

Molecular hydrogen is present only in trace concentrations (550 parts per billion) in the Earth’s atmosphere [1], but plays an important part in the global carbon cycle and is a major constituent of microbial metabolism In anoxic ecosystems it is rapidly produced and consumed by microorganisms resulting in a large turnover [2]. Hydrogen formation from reduced pyridine nucleotides or flavins is energetically unfavourable and growth according to Eq (1) requires removal of hydrogen by a syntrophic partner such as a sulfate reducing bacterium, a methanogenic archaeon or an acetogenic bacterium [5,6,7,8] The latter produces acetate according to Eq (2): 4H2þ2CO2 þ xADP þ xPiÀ!CH3COOH þ2H2O þ xATP ΔG00 1⁄4 −95 kJ=mol ð2Þ. Detailed studies in the acetogenic model organism Acetobacterium woodii estimated the amount of ATP to 0.3 mol per mol of acetate produced [9]

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