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Dissolved organic carbon and major and trace elements in peat porewater of sporadic, discontinuous, and continuous permafrost zones of western Siberia

Spatial heterogeneity of soil acidity properties in peatlands of Western Siberia

Soil organic carbon storage in a mountain permafrost area of Central Asia (High Altai, Russia)

Seasonal and spatial variations of dissolved organic matter biodegradation along the aquatic continuum in the southern taiga bog complex, Western Siberia

Soil-ecological conditions of the north taiga flat-mound bog, Western Siberia on microform types. For some elements (e.g., DOC, Fe, Al, B, Si, Ti, V, Rb, Sb, Cs, REEs (rare earth elements

Colloidal organic carbon and trace elements in peat porewaters across a permafrost gradient in Western Siberia

Bacteria primarily metabolize at the active layer/permafrost border in the peat core from a permafrost region in western Siberia

Colloids in thermokarst lakes along a permafrost and climate gradient of permafrost peatlands in Western Siberia using in situ dialysis procedure in the colloidal fractions of DOC, Fe, Al, trivalent and tetravalent trace cations, Mn, Co, Ni, As, V, and U from

Permafrost thaw and climate warming may decrease the CO2, carbon, and metal concentration in peat soil waters of the Western Siberia Lowland

Dissolved carbon concentrations and emission fluxes in rivers and lakes of Central Asia (Sayan-Altai mountain region, Tyva)

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