Landscape-scale changes in the Arctic as a result of climate change affect the soil thermal
regime and impact the depth to permafrost in vulnerable tundra watersheds. When top-down …

Permafrost predominates in polar and high mountain regions, encompassing nearly 15% of
the exposed land in the Northern Hemisphere. It denotes soil or rock that remains at or …

In the Arctic and subarctic, climate change is causing reduced snowpack extent and earlier
snowmelt. Shallower snowpack decreases the thermal insulation of underlying soil and …

Temporal variation in community composition is central to our understanding of the
assembly and functioning of microbial communities, yet the controls over temporal dynamics …

Permafrost regions, characterised by extensive belowground excess ice, are highly
vulnerable to rapid thaw, particularly in areas such as the Yedoma domain. This region is …

Abstract The Tri-Service Microbiome Consortium (TSMC) was founded to enhance
collaboration, coordination, and communication of microbiome research among DoD …

The purpose of this work is to study the structure of microbial communities, the
physicochemical characteristics of the burozems' profiles, and the soil material infilling the …

Based on the example of an exposure at Cape Maly Chukochi, a model has been
developed for the accumulation of the soil-sedimentary sequence of the ice complex in the …

Permafrost degradation leads to the formation of contrasting hydrological conditions such as
water-saturated anoxic and dry oxic soils, which significantly influence the bacterial …

Soil microorganisms interact with one another within soil pores and respond to external
conditions such as temperature. Data on microbial community composition and potential …