Alkalothermophilic Iron-Reducing Bacteria of the Goryachinsk Thermal Water Basin

Abstract A study of iron-reducing prokaryotes that use the poorly crystalline mineral ferrihydrite as an electron acceptor revealed their widespread occurrence on the planet. However, the ability of iron reducers to develop under polyextreme conditions (at elevated values of pH and temperature) has not been previously demonstrated. To confirm the existence of alkalothermophilic iron reducers, we studied the water and sediment samples from the Goryachinsk nitrogen-rich thermal water basin. These springs are associated with young tectonic fractures in the Baikal rift zone; their water is characterized by low salinity, alkaline pH (8.8‒9.2) and temperature of 53‒55°C. Enrichment cultures reducing synthesized ferrihydrite were obtained by adding this mineral to the water and sediment samples from the Goryachinsk thermal springs, followed by anaerobic incubation at 50 and 55°C. The 16S rRNA gene profiling of the water and sediment samples and of the primary enrichment cultures revealed high taxonomic diversity, almost exclusively represented by bacterial taxa. Subsequent transfers with ferrihydrite and organic acids or hydrogen as electron donors resulted in stable enrichment cultures of organo- and lithotrophic alkalothermophilic iron reducers. Members of the genus Parvivirga , one of the first cultured representatives of the OPB41 group (now the order Anaerosomatales , phylum Actinomycetota ), constituted 30 to 50% of the total abundance.