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A widely distributed hydrogenase oxidises atmospheric H2 during bacterial growth
Authors:Zahra F Islam  Caitlin Welsh  Katherine Bayly  Rhys Grinter  Gordon Southam  Emma J Gagen  Chris Greening
Institution:1.School of Biological Sciences, Monash University, Clayton, VIC 3800 Australia ;2.Department of Microbiology, Biomedicine Discovery Institute, Clayton, VIC 3800 Australia ;3.School of Earth and Environmental Sciences, University of Queensland, St Lucia, QLD 4072 Australia ;4.Australian Centre for Ecogenomics, School of Chemistry and Molecular Biosciences, University of Queensland, St Lucia, QLD 4072 Australia
Abstract:Diverse aerobic bacteria persist by consuming atmospheric hydrogen (H2) using group 1h NiFe]-hydrogenases. However, other hydrogenase classes are also distributed in aerobes, including the group 2a NiFe]-hydrogenase. Based on studies focused on Cyanobacteria, the reported physiological role of the group 2a NiFe]-hydrogenase is to recycle H2 produced by nitrogenase. However, given this hydrogenase is also present in various heterotrophs and lithoautotrophs lacking nitrogenases, it may play a wider role in bacterial metabolism. Here we investigated the role of this enzyme in three species from different phylogenetic lineages and ecological niches: Acidithiobacillus ferrooxidans (phylum Proteobacteria), Chloroflexus aggregans (phylum Chloroflexota), and Gemmatimonas aurantiaca (phylum Gemmatimonadota). qRT-PCR analysis revealed that the group 2a NiFe]-hydrogenase of all three species is significantly upregulated during exponential growth compared to stationary phase, in contrast to the profile of the persistence-linked group 1h NiFe]-hydrogenase. Whole-cell biochemical assays confirmed that all three strains aerobically respire H2 to sub-atmospheric levels, and oxidation rates were much higher during growth. Moreover, the oxidation of H2 supported mixotrophic growth of the carbon-fixing strains C. aggregans and A. ferrooxidans. Finally, we used phylogenomic analyses to show that this hydrogenase is widely distributed and is encoded by 13 bacterial phyla. These findings challenge the current persistence-centric model of the physiological role of atmospheric H2 oxidation and extend this process to two more phyla, Proteobacteria and Gemmatimonadota. In turn, these findings have broader relevance for understanding how bacteria conserve energy in different environments and control the biogeochemical cycling of atmospheric trace gases.Subject terms: Environmental microbiology, Biogeochemistry
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