Abstract
The structural features of a cyanobacterial mat from Lake Khilganta (Southeastern Transbaikal Region) developing at different values of salinity and pH were determined based on our long-term investigation of the natural community, as well as results obtained during experimentation with its laboratory analogue. At water mineralization of 40–50 g/l, Microcoleus chthonoplastes and Phormidium molle play a key role in the formation of the cyanobacterial mat. As water mineralization increases, the diversity of cyanobacteria in the natural mat increases as well, reaches its maximum at 80 g/l NaCl, and decreases at 100 g/l. In the laboratory community, Nodularia sp. prevailed. It was able to form matlike structures within a broad pH range and at a salinity of up to 50 g/l NaCl. As the water mineralization level increased up to 100 g/l or higher, a replacement of the dominant complexes occurred both in the laboratory and natural communities: cyanobacterial species were substituted with green algae.
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Original Russian Text © D.D. Tsyrenova, A.V. Bryanskaya, L.P. Kozyreva, Z.B. Namsaraev, B.B. Namsaraev, 2011, published in Mikrobiologiya, 2011, Vol. 80, No. 2, pp. 251–257.
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Tsyrenova, D.D., Bryanskaya, A.V., Kozyreva, L.P. et al. Structure and formation properties of the haloalkaliphilic community of Lake Khilganta. Microbiology 80, 237–243 (2011). https://doi.org/10.1134/S0026261711020172
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DOI: https://doi.org/10.1134/S0026261711020172