2020
DOI: 10.31951/2658-3518-2020-a-4-971
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Microbial community diversity in hot springs of the Baikal rift zone

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“…Layers of calcium carbonate formed in the photozone undergo a number of transformations associated with the activity of microorganisms. On the one hand, Ca mobilization during organic acid formation by primary anaerobes is possible here; on the other hand, decomposition of organic acids by secondary anaerobes, methanogens and sulfidogens can lead to new deposition of CaCO3 [19]. The microbial communities of the Verkhne-Paratunsky springs and the orange microbial mat of the Malkinsky thermal waters show small to medium deposition of magnetite.…”
Section: Materials For Power Electronics Construction and Environment...mentioning
confidence: 97%
“…Layers of calcium carbonate formed in the photozone undergo a number of transformations associated with the activity of microorganisms. On the one hand, Ca mobilization during organic acid formation by primary anaerobes is possible here; on the other hand, decomposition of organic acids by secondary anaerobes, methanogens and sulfidogens can lead to new deposition of CaCO3 [19]. The microbial communities of the Verkhne-Paratunsky springs and the orange microbial mat of the Malkinsky thermal waters show small to medium deposition of magnetite.…”
Section: Materials For Power Electronics Construction and Environment...mentioning
confidence: 97%