Microbial Community Composition as an Indicator of the State of Basins Located at the Sea Coast (Exemplified by the Kanda Bay, Kandalaksha Gulf, White Sea)

IF 1.3 4区 生物学 Q4 MICROBIOLOGY
A. S. Savvichev, N. A. Demidenko, V. V. Kadnikov, V. V. Belenkova, I. I. Rusanov, V. M. Gorlenko
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Abstract

Formation of the Kanda Bay resulted from construction of a railway dam (1916) and subsequent isolation of the sea lagoon from the main basin of the Kandalaksha Gulf, White Sea. Decreased action of tidal flows, which mix the water column of the lagoon, altered the hydrological regime of the basin. Decreased water exchange resulted in formation of oxygen-depleted near-bottom water and to sulfide contamination. A freshwater lake was, however, preserved in the southern part of the Kanda Bay. The composition of microbial communities was studied for the near-bottom water horizons at different sides of the Kanda Bay. The oxygen regime in this layer was found to change, with increasing concentrations of sulfide and methane and active processes of sulfate reduction and methane oxidation. The composition of the microbial community changed noticeably, with lower abundance of true marine and freshwater microorganisms and development of bacteria and archaea predominant in microbial communities of anoxic water in meromictic basins. Among the microbial diversity, indicator species with increased abundance were revealed. These are archaea of the genera Methanoregula and Methanosaeta (phylum Halobacterota). The sulfur cycle microorganisms, which were the indicators of stagnant marine water, included anoxygenic phototrophic bacteria of the class Chlorobia, (Chlorobium phaeovibrioides, Pelodictyon phaeoclathratiforme), Chloroflexi of the genus Chloronema, nonsulfur purple bacteria related to the genus Rhodoferax, colorless sulfur bacteria of the family Beggiatoaceae, and sulfur oxidizers of the genus Thiobacillus. Archaea of the genus Nitrosopumilus (phylum Crenarchaeota) and bacteria of the genus Woeseia may be considered opposites to the indicator microorganisms, since they were found only in the open sea water. In our opinion, stable water exchange through the dam will result in the stable composition of the Kanda Bay microbial community, with only seasonal variations and year-to-year fluctuations. The negative scenario supports prediction of conversion of the Kanda Bay into a stratified basin with anoxic near-bottom water and the microbial community similar to that found in meromictic lakes.

Abstract Image

微生物群落组成作为海岸盆地状况的指标(以坎大拉沙湾、白海的Kanda湾为例)
摘要:神达湾的形成是由于1916年修建了一座铁路大坝,随后将海泻湖与白海坎大拉沙湾的主要盆地隔离开来。潮汐流的作用减弱,混合了泻湖的水柱,改变了盆地的水文状况。水交换减少导致缺氧近底水的形成和硫化物污染。然而,在神田湾南部保留了一个淡水湖。对神田湾不同侧面近底水层的微生物群落组成进行了研究。随着硫化物和甲烷浓度的增加,以及硫酸盐还原和甲烷氧化的活跃过程,该层的氧状态发生了变化。微生物群落组成发生明显变化,真正的海洋和淡水微生物丰度较低,细菌和古菌的发育在分生盆地缺氧水体微生物群落中占主导地位。微生物多样性中,指示种丰度呈增加趋势。这些是产甲烷菌属和产甲烷菌属(盐细菌门)的古细菌。作为海水停滞状态指示物的硫循环微生物包括:绿藻纲无氧光养细菌(绿弧菌)、绿藻属的绿柔菌、红铁属的无硫紫色细菌、Beggiatoaceae的无色硫细菌和硫杆菌属的硫氧化菌。亚硝酸菌属的古细菌(绿古菌门)和Woeseia属的细菌可以被认为是指示微生物的对立面,因为它们只在开阔的海水中发现。我们认为,通过大坝稳定的水交换将导致神田湾微生物群落的稳定组成,只有季节变化和年波动。消极情景支持了神田湾转变为一个具有缺氧近底水和微生物群落类似于分生湖泊的分层盆地的预测。
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来源期刊
Microbiology
Microbiology 生物-微生物学
CiteScore
2.40
自引率
13.30%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Microbiology is an is an international peer reviewed journal that covers a wide range of problems in the areas of fundamental and applied microbiology. The journal publishes experimental and theoretical papers, reviews on modern trends in different fields of microbiological science, and short communications with descriptions of unusual observations. The journal welcomes manuscripts from all countries in the English or Russian language.
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