Microbial Processes and Microbial Communities in the Water Column of the Polar Meromictic Lake Bol’shie Khruslomeny at the White Sea Coast

Abstract

Microbiological, molecular ecological, biogeochemical, and isotope geochemical research was carried out at the polar Lake Bol'shie Khruslomeny at the coast of the Kandalaksha Bay, White Sea in March and September 2017. The uppermost mixolimnion was oxic, with low salinity (3-5%). The lower chemocline layer was browngreen colored, with very high content of particulate organic matter (up to 11.8 mg C L −1). The lowermost monimolimnion had marine salinity (22-24%) and very high concentrations of sulfide (up to 18 mmol L −1) and CH 4 (up to 1.8 mmol L −1). In the chemocline, total microbial abundance and the rate of anoxygenic photosynthesis were 8.8 × 10 6 cells mL −1 and 34.4 µmol C L −1 day −1 , respectively. Both in March and September, sulfate reduction rate increased with depth, peaking (up to 0.6-1.1 µmol S L −1 day −1) in the lower chemocline. Methane oxidation rates in the chemocline were up to 85 and 180 nmol CH 4 L −1 day −1 in March and September, respectively; stimulation of this process by light was observed in September. The percentages of cyanobacteria and methanotrophs in the layer where light-induced methane oxidation occurred were similar, ∼2.5% of the microbial community. Light did not stimulate methane oxidation in deeper layers. The carbon isotope composition of particulate organic matter (δ 13 C-Corg), dissolved carbonates (δ 13 C-DIC), and methane (δ 13 C-CH 4) indicated high microbial activity in the chemocline. Analysis of the 16S rRNA gene sequences revealed predominance of Cyanobium cyanobacteria (order Synechococcales) in the mixolimnion. Green sulfur bacteria Chlorobium phaeovibrioides capable of anoxygenic photosynthesis constituted ∼20% of the chemocline community both in March and in September. Methyloprofundus gammaptoteobacteria (family Methylomonaceae) were present in the upper chemocline, where active methane oxidation occurred. During winter, cyanobacteria were less abundant in the chemocline, while methanotrophs occurred in higher horizons, including the under-ice layer. Chemolithotrophic gammaproteobacteria of the genus Thiomicrorhabdus, oxidizing

Establishment of microbial model communities capable of removing trace organic chemicals for biotransformation mechanisms research

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Heavy Metals in Sediments of Subarctic Meromictic Lakes of the White Sea as Possible Tracers of Environmental Changes

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“…Consequently, a meromictic structure emerged in this lake. Beneath the halocline, situated at a depth of 2-3 m, a sulfide water mass developed around 4-4.5 m deep [29].…”

Single-cell genomics-based analysis reveals a vital ecological role of Thiocapsa sp. LSW in the meromictic Lake Shunet, Siberia

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