Abstract Models predict that thaw of permafrost soils at northern high latitudes will release
tens of billions of tonnes of carbon (C) to the atmosphere by 2100 (refs,,). The effect on the …

Thawing of frozen peat in discontinuous permafrost zones may significantly modify the
environment at local (slumps and engineering damages) and global (greenhouse gases …

Mobilization of dissolved organic carbon (DOC) and related trace elements (TEs) from the
frozen peat to surface waters in the permafrost zone is expected to enhance under ongoing …

Peatlands have been widely studied in terms of their ecohydrology, carbon dynamics,
ecosystem services and palaeoenvironmental archives. However, several assumptions are …

Decay of palsas can indicate permafrost status, particularly in regions where air
temperatures have increased rapidly in recent decades. Using weather data, annual surveys …

Most northern peatlands developed during the Holocene, sequestering large amounts of
carbon in terrestrial ecosystems. However, recent syntheses have highlighted the gaps in …

Incipient warming of peatlands at high latitudes is expected to modify soil drainage and
hence the redox conditions, which has implications for Fe export from soils. This study uses …

Permafrost in peatlands strongly influences ecosystem characteristics, including vegetation
composition, hydrological functions, and carbon cycling. Large amounts of organic carbon …

High‐resolution analyses of plant macrofossils, testate amoebae, pollen, mineral content,
bulk density, and carbon and nitrogen were undertaken to examine the late Holocene …

Thaw of frozen peat in discontinuous permafrost zone produces a significant number of
thermokarst lakes, which are known to contribute to Green House Gases (GHG) emission in …