Fig. 1From: The role of environmental factors for the composition of microbial communities of saline lakes in the Novosibirsk region (Russia)Location map of saline lakes. Blue lines in the top panel show reconstructed limits of the West Siberian sea in different stages of the Palaeogene [18]: Latest Selandian-early Thanetian (a), Late Thanetian–Ypresian (b), Lutetian (c), and Bartonian-Priabonian (d). The panel below shows simplified geology. 1 Pre-Quaternary clay silt, clay, and loess, including those building the hills; 2,3 Lower-Middle Pleistocene lacustrine-fluvial clay silt, or less often silt and sand (2) and loess and lake sand, silt, and clay silt (3); 4 Middle-Upper Pleistocene lacustrine and fluvial sand, silt, clay silt, often muddy; 5–7 Upper Pleistocene-Holocene lacustrine clay silt (often muddy), silt, and sand (5), alluvium and slope wash (6), and lacustrine-bog peat, muddy clay silt, and sapropel (7); 8 Freshwater (a) and saline (b) lakes; 9 Sampling sitesBack to article page