It has been shown that reactive soil minerals, specifically iron (III)(oxyhydr) oxides, can trap
organic carbon in soils overlying intact permafrost, and may limit carbon mobilization and …

Soil moisture is a known environmental factor influencing carbon dioxide (CO 2) emissions
and therefore represents an important variable in predictive models. Establishing …

In the Arctic, environmental factors governing microbial degradation of soil carbon (C) in
active layer and permafrost are poorly understood. Here we determined the functional …

Arctic tundra stores large quantities of soil organic matter under varying redox conditions. As
the climate warms, these carbon reservoirs are susceptible to increased rates of …

Molecular composition of the Arctic soil organic carbon (SOC) and its susceptibility to
microbial degradation are uncertain due to heterogeneity and unknown SOC compositions …

Abstract Nitrate (NO 3−) removal from aquatic ecosystems involves several microbially
mediated processes, including denitrification, dissimilatory nitrate reduction to ammonium …

Rapid temperature rise in Arctic permafrost impacts not only the degradation of stored soil
organic carbon (SOC) and climate feedback, but also the production and bioaccumulation of …

Mineral elements bind to dissolved organic carbon (DOC) in permafrost soils, and this may
contribute to the stabilization or the degradation of organic carbon along the soil to river …

Redox processes, aqueous and solid‐phase chemistry, and pH dynamics are key drivers of
subsurface biogeochemical cycling and methanogenesis in terrestrial and wetland …

The fate of soil organic carbon (SOC) stored in the Arctic permafrost is a key concern as
temperatures continue to rise in the northern hemisphere. Studies and conceptual models …