THE ROLE OF SULFATE-REDUCING BACTERIA IN BIOMONITORING OF RIVER ECOSYSTEMS

D. Andreeva, L. Kondratyeva
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Abstract

Biomonitoring is one of the important stages in the consistent study of the sustainable development of aquatic ecosystems and their biological diversity. Against the background of the global impact on the hydrosphere, there is a need to select priority indicators and methods for determining the environmental risk in case of pollution of river ecosystems. Newly arriving substances are involved in complex biogeochemical processes in the water column, migrate as part of suspensions, or settle to the bottom. During the freezing period, a special place is occupied by cryogenic biochemical processes occurring in ice. Microbiological studies of the Amur River near the city of Khabarovsk showed that the water quality diff ered signifi cantly in winter. In the under-ice water and ice sampled off the coast, a diff erent composition of organic matter (OM) has been recorded for many years. After the fl oods (2013, 2019), a high number of sulfate- reducing bacteria was recorded in individual ice layers, which aff ect the dynamics of the transformation of natural and anthropogenic substances. This is due to the fact that in the area of Khabarovsk, during the period of ice cover formation, humifi ed OM spreads along the left bank, coming from the Zeya and Bureya reservoirs during technological discharges of water and from the fl oodplain, and along the right bank – waters contaminated with OM, mainly anthropogenic character. Long-term studies of the potential activity of sulfate- reducing bacteria in the Amur and its channels (Amurskaya, Pemzenskaya) make it possible to predict the formation of hydrogen sulfi de zones and the likelihood of mercury methylation over a wide temperature range. The indicator of resistance of cryomicrobial communities to high concentrations of mercury can be used for a retrospective assessment of the environmental risk of mercury pollution of rivers during the freeze-up period.
硫酸盐还原菌在河流生态系统生物监测中的作用
生物监测是水生生态系统可持续发展及其生物多样性一致性研究的重要环节之一。在全球水圈受到影响的背景下,有必要选择确定河流生态系统污染情况下环境风险的优先指标和方法。新到达的物质在水柱中参与复杂的生物地球化学过程,作为悬浮液的一部分迁移,或沉降到底部。在冷冻期间,冰中发生的低温生化过程占据了一个特殊的位置。对哈巴罗夫斯克市附近的阿穆尔河进行的微生物学研究表明,冬季的水质差异很大。在沿海的冰下水和冰样本中,多年来一直记录着不同的有机物组成(OM)。在洪水之后(2013年、2019年),个别冰层中记录到大量硫酸盐还原细菌,这些细菌影响了自然和人为物质的转化动态。这是由于在哈巴罗夫斯克地区,在冰盖形成期间,潮湿的有机质沿左岸扩散,来自技术排水期间的泽亚和布里亚水库和泛滥平原,而沿右岸则是受有机质污染的水域,主要是人为性质的。对阿穆尔河及其河道(Amurskaya, Pemzenskaya)中硫酸盐还原细菌潜在活性的长期研究使预测硫化氢带的形成和在宽温度范围内汞甲基化的可能性成为可能。低温微生物群落对高浓度汞的抗性指标可用于冻结期河流汞污染环境风险的回顾性评估。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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