The deep sea, the marine layer at depths of 200 meters and more, accounts for about 90 percent of the world's ocean volume. It forms the largest habitat on Earth and is home to the largest number of microorganisms. These microorganisms contribute significantly to the biogeochemical cycles. They extract organic material, for example from phytoplankton and zooplankton, transform it and make it available again to the ecosystem as nutrients. In this way, they play a major role in the fixation and cycling of carbon. Dissolved sulfur compounds are also converted by bacteria and returned to the material cycle.

UBA868: mixotrophic energy driving force in ecosystems

UBA868 plays a significant role in the oxidation of sulfur compounds and the fixation of carbon dioxide, thus contributing significantly to the energy balance in the deep sea. "Interestingly, UBA868 is mixotrophic. This means that it can both fix carbon from CO2 using the energy generated by oxidizing sulfur compounds and take up organic substances and use them for energy production" explains Federico Baltar. This finding refutes the previously held assumption that only autotrophic microorganisms (that can use CO2 as a carbon source) and heterotrophic microorganisms (that rely on organic carbon sources) are responsible for regulating the carbon cycle.

To investigate the role of UBA868 in the ocean, the team used a combination of genomic analysis methods, including single-cell genomics, community metagenomics, metatranscriptomics and single-cell activity measurements. Finally, analysis of gene libraries from multiple, worldwide expeditions confirmed the ubiquitous distribution and global importance of this bacterial group. This discovery contributes to our understanding of marine ecosystems and the ocean's ability to store carbon. At the same time, it shows how important it is to also put mixotrophic bacteria in the focus of research on the cycling of nutrients in the ocean.