Several strains of a Gram-negative, anaerobic photoautotrophic, motile, rod-shaped bacterium, designated as B14B, A-7R, and A-7Y were isolated from biofilms of low-mineralized soda lakes in central Mongolia and Russia (southeast Siberia). They had lamellar stacks as photosynthetic structures and bacteriochlorophyll as the major photosynthetic pigment. The strains were found to grow at 25-35 °C, pH 7.5-10.2 (optimum, pH 9.0), and with 0-8% (/) NaCl (optimum, 0%). In the presence of sulfide and bicarbonate, acetate, butyrate, yeast extract, lactate, malate, pyruvate, succinate, and fumarate promoted growth. The DNA G + C content was 62.9-63.0 mol%. While the 16S rRNA gene sequences confirmed that the new strains belonged to the genus of the comparison of the genome nucleotide sequences of strains B14B, A-7R, and A-7Y revealed that the new isolates were remote from all described species both in dDDH (19.7-38.8%) and in ANI (75.0-89.4%). The new strains are also genetically differentiated by the presence of a nitric oxide reduction pathway that is lacking from all other . We propose to assign the isolates to the new species, sp. nov., with the type strain B14B (=DSM 116064 = KCTC 25542 = UQM 41491).
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http://dx.doi.org/10.3390/microorganisms11051336 | DOI Listing |
Microorganisms
May 2023
GEOMAR Helmholtz Centre for Ocean Research Kiel, Düsternbrooker Weg 20, D-24105 Kiel, Germany.
Several strains of a Gram-negative, anaerobic photoautotrophic, motile, rod-shaped bacterium, designated as B14B, A-7R, and A-7Y were isolated from biofilms of low-mineralized soda lakes in central Mongolia and Russia (southeast Siberia). They had lamellar stacks as photosynthetic structures and bacteriochlorophyll as the major photosynthetic pigment. The strains were found to grow at 25-35 °C, pH 7.
View Article and Find Full Text PDFA novel strain, SHET, of aerobic bacteriochlorophyll a-containing bacteria was isolated from the surface layer of bottom sediments from the soda lake Shuluutai-Ekhe-Torom (Chita oblast, Eastern Siberia, Russia). The lake water has a total mineralization of 3.0 g/l and a pH of 9.
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