Molecular Hydrogen, a Neglected Key Driver of Soil Biogeochemical Processes.

The atmosphere of the early Earth is hypothesized to have been rich in reducing gases such as hydrogen (H). H has been proposed as the first electron donor leading to ATP synthesis due to its ubiquity throughout the biosphere as well as its ability to easily diffuse through microbial cells and its low activation energy requirement. Even today, hydrogenase enzymes enabling the production and oxidation of H are found in thousands of genomes spanning the three domains of life across aquatic, terrestrial, and even host-associated ecosystems. Even though H has already been proposed as a universal growth and maintenance energy source, its potential contribution as a driver of biogeochemical cycles has received little attention. Here, we bridge this knowledge gap by providing an overview of the classification, distribution, and physiological role of hydrogenases. Distribution of these enzymes in various microbial functional groups and recent experimental evidence are finally integrated to support the hypothesis that H-oxidizing microbes are keystone species driving C cycling along O concentration gradients found in H-rich soil ecosystems. In conclusion, we suggest focusing on the metabolic flexibility of H-oxidizing microbes by combining community-level and individual-level approaches aiming to decipher the impact of H on C cycling and the C-cycling potential of H-oxidizing microbes, via both culture-dependent and culture-independent methods, to give us more insight into the role of H as a driver of biogeochemical processes.