Permafrost peatlands contain globally important amounts of soil organic carbon, owing to
cold conditions which suppress anaerobic decomposition. However, climate warming and …

Peatlands in northern permafrost regions store a significant proportion of global soil carbon.
Recent warming is accelerating peatland permafrost thaw and thermokarst collapse …

Permafrost peatlands are found in high-latitude regions and store globally-important
amounts of soil organic carbon. These regions are warming at over twice the global average …

Climate warming has inevitable impacts on the vegetation and hydrological dynamics of
high-latitude permafrost peatlands. These impacts in turn determine the role of these …

Peatlands within the northern permafrost region cover approximately 2 million km2 and are
characterized by organic soils that can be several meters thick, and a fine-scale mosaic of …

The history of permafrost aggradation and thaw in northern peatlands can serve as an
indicator of regional climatic history in regions where records are sparse. We infer regional …

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

Climate warming is leading to permafrost thaw in northern peatlands, and current
predictions suggest that thawing will drive greater surface wetness and an increase in …

Boreal peatlands in Canada have harbored relict permafrost since the Little Ice Age due to
the strong insulating properties of peat. Ongoing climate change has triggered widespread …

Climate warming in high‐latitude regions is thawing carbon‐rich permafrost soils, which can
release carbon to the atmosphere and enhance climate warming. Using a coupled model of …