Active processes of permafrost thaw in Western Siberia increase the number of soil
subsidencies, thermokarst lakes and thaw ponds. In continuous permafrost zones, this …

On-going permafrost thaw in discontinuous permafrost regions produces significant amounts
of small permafrost subsidence and depressions, while large lakes are likely to drain into …

Riverine export fluxes of organic carbon (OC), major and trace elements remain at the
forefront of environmental research in Arctic and subarctic regions, due mostly to high …

Significant and systematic variations of iron isotopic composition in surface water sample
fractions obtained by frontal cascade filtration and ultrafiltration have been recorded in (1) …

This work describes the hydrochemical composition of thermokarst lake and pond
ecosystems, which are observed in various sizes with different degrees of permafrost …

Despite relatively good knowledge of the biogeochemistry of Siberian thermokarst lakes
during summer base flow, their seasonal dynamics remains almost unexplored. This work …

This study assesses the potential use of Mg isotopes to trace Mg carbonate precipitation in
natural waters. Salda Lake (SW Turkey) was chosen for this study because it is one of the …

Assessing multi-annual riverine export fluxes of carbon, nutrients and metals from the
continent to the Arctic Ocean is crucial for constraining the current status and foreseeing …

The concentration and size fractionation of major and trace elements (TEs) linked to organo-
mineral colloids along the landscape gradient soil water–peat mire–humic lakes–river–large …

The riverine export fluxes of dissolved carbon, nutrient and metals from the land to the Arctic
Ocean are fairly well quantified for five large Arctic rivers but remain virtually unknown for …