A single extremely halophilic strain was isolated from salt brine produced when a fresh water lake flooded a large salt mine located beneath the lake. The water that entered this mine contained less than 0.34 M NaCl, but over time, this sealed brine became saturated by Cenozoic age salt (121-125 million-year BCE). The isolated strain requires at least 1.7 M NaCl for survival and grows optimally in 3.1 M NaCl. Therefore, it could not have survived or been present in the waters that flooded this salt mine. The strain grows at a pH range from 6.5 to 9.0 and has a wide tolerance to temperatures from 25 ℃ to at least 60 ℃. The comparison of 16S rRNA and rpoB' genes revealed that strain 1-13-28T is related to Halorubrum tebenquichense DSM 14210T showing 98.6% and 98.1% similarities, respectively. Phylogenetic analyses based on 16S rRNA, rpoB' genes and 122 concatenated archaeal genes show that the strain 1-13-28T consistently forms a cluster with Halorubrum tebenquichense of the genus Halorubrum. Strain 1-13-28T contained sulfated mannosyl glucosyl diether, and the polar lipid profile was identical to those of most Halorubrum species. Based on the overall combination of physiological, phylogenetic, polar lipids and phylogenomic characteristics, strain 1-13-28T (= ATCC 700083T = CGMCC 1.62627T) represents a newly identified species within the genus Halorubrum for which the name Halorubrum hochsteinianum is proposed.
Keywords: Ancient microbes; Halophile; Halorubrum; Salt mine; Taxonomy.
© 2023. The Author(s), under exclusive licence to Springer Nature Japan KK, part of Springer Nature.