Abstract

A small number of ecological-trophic groups of bacteria are noted in saline groundwater’s (30-50 g/L). The obtained data show, that thionic and halophilic forms of saprophytic bacteria dominated, developing in presence of 10% NaCl. Among saprophytic microorganisms, rod-shaped forms of the genus Microbacterium sp. significantly dominated. A significant accumulation of Cu, Co and light REEs by brine microbial communities is shown.

Highlights

  • The Rechitsa saline groundwater manifestation is located in the coastal area of Sukhodol Bay in the valley of the Sukhodol River [1,2]

  • The study results of physico-chemical composition carried out earlier showed that saline waters (total dissolved solids (TDS) = 31.8-50 g/L) are cold (10.3–12.1o C), neutral pH (6.74–7.63) and have chloride calcium and chloride sodium - calcium composition (Cl 20.2-22.3 g/L)

  • Microbiological studies of underground saline waters revealed the presence of small amount of functional groups of bacteria (4-5 out of 13), as well as their low number, which averaged 1.3×102 cells/ml (09.2013) - 4.1×102 cells/ml (07.2013) and their number was higher in summer periods

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Summary

Introduction

The Rechitsa saline groundwater manifestation is located in the coastal area of Sukhodol Bay in the valley of the Sukhodol River [1,2]. Bacteria in groundwater play a great role in geochemical circulation of substances and are an important biotic factor. They actively impact on chemical composition of deep waters, mineral formation and metamorphism of rocks. Despite long-term observations of temperature and chemical composition of brines [1,2,3,4], there is no information about the microorganisms inhabiting them In this regard, the aim of this work was to study the distribution, number, composition of various ecological-trophic groups of bacteria, as well as the participation of microbial communities in accumulation of trace elements in the cold saline groundwater’s of Rechitsa

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