4.6 Article

Candidatus Hydrogenisulfobacillus filiaventi strain R50 gen. nov. sp. nov., a highly efficient producer of extracellular organic compounds from H2 and CO2

Journal

FRONTIERS IN MICROBIOLOGY
Volume 14, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/fmicb.2023.1151097

Keywords

acidophilic; autotroph; hydrogenase; amino acids; volcanic soil; Hydrogenisulfobacillus

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The production of organic molecules can be achieved by synthesizing them from CO2 and a cheap energy source, instead of relying on fossil fuels. Volcanic and geothermal areas, which have abundant CO2 and reduced inorganic gases, provide habitats where novel chemolithoautotrophic microorganisms for organic compound synthesis can be discovered. A thermoacidophilic, autotrophic H-2-oxidizing microorganism called Candidatus Hydrogenisulfobacillus filiaventi R50 was found to fix CO2 and produce more than 0.54 mol of organic carbon per mole of fixed CO2. This discovery opens up possibilities for the sustainable production of important biomolecules using chemolithoautotrophic microorganisms.
Production of organic molecules is largely depending on fossil fuels. A sustainable alternative would be the synthesis of these compounds from CO2 and a cheap energy source, such as H-2, CH4, NH3, CO, sulfur compounds or iron(II). Volcanic and geothermal areas are rich in CO2 and reduced inorganic gasses and therefore habitats where novel chemolithoautotrophic microorganisms for the synthesis of organic compounds could be discovered. Here we describe Candidatus Hydrogenisulfobacillus filiaventi R50 gen. nov., sp. nov., a thermoacidophilic, autotrophic H-2-oxidizing microorganism, that fixed CO2 and excreted no less than 0.54 mol organic carbon per mole fixed CO2. Extensive metabolomics and NMR analyses revealed that Val, Ala and Ile are the most dominant form of excreted organic carbon while the aromatic amino acids Tyr and Phe, and Glu and Lys were present at much lower concentrations. In addition to these proteinogenic amino acids, the excreted carbon consisted of homoserine lactone, homoserine and an unidentified amino acid. The biological role of the excretion remains uncertain. In the laboratory, we noticed the production under high growth rates (0.034 h(-1), doubling time of 20 h) in combination with O-2-limitation, which will most likely not occur in the natural habitat of this strain. Nevertheless, this large production of extracellular organic molecules from CO2 may open possibilities to use chemolithoautotrophic microorganisms for the sustainable production of important biomolecules.

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