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Magnesium isotopes in permafrost-dominated Central Siberian larch forest watersheds

Изотопы углерода и азота в лесных почвах среднетаежной подзоны Средней Сибири

Biogeochemistry of carbon, major and trace elements in watersheds of northern Eurasia drained to the Arctic Ocean: The change of fluxes, sources and mechanisms under the climate warming prospective

The Impact of Climatic Factors on CО2 Emissions from Soils of Middle-Taiga Forests in Central Siberia: Emission as a Function of Soil Temperature and Moisture of central Siberia during five growing seasons. It is shown that, throughout a vast area covered by pine

DYNAMICS OF THE SOIL CO2 EMISSION DURING SNOW-FREE PERIOD IN THE IN MIDDLE TAIGA FORESTS IN CENTRAL SIBERIA

Mercury stable isotope composition of lichens and mosses from Northern Eurasia reveals Hg deposition pathways and sources are near zero, indicating a dominant (63%) atmospheric Hg0 origin followed by HgII wet and dry deposition

Atmospheric CO2 and CH4 fluctuations over the continent-sea interface in the Yenisei River sector of the Kara Sea reflecting a signal caused pan-Arctic and not very much influenced by the local processes, we analyzed

Dissolved carbon concentrations and emission fluxes in rivers and lakes of Central Asia (Sayan-Altai mountain region, Tyva) strongly impacted by ongoing climate change. Towards a better understanding of C storage, transport

Hydroclimatic controls on the isotopic (δ18 O, δ2 H, d-excess) traits of Pan-Arctic summer rainfall events key tundra, subarctic, maritime, and continental climate zones. Here, we present a first assessment

Influence of precipitation on CO 2 soil emission in pine forests of the Central Siberia boreal zone

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