Peatlands have acted as net CO2 sinks over millennia, exerting a global climate cooling
effect. Rapid warming at northern latitudes, where peatlands are abundant, can disturb their …

Climate change threatens the capacity of peatlands to continue storing carbon (C)
belowground. Microorganisms are crucial in regulating the peatland C sink function, but how …

Permafrost thaw in northern peatlands often leads to increased methane (CH 4) emissions,
but gaps remain in our understanding of the underlying controls responsible for increased …

Climate change‐driven vegetation changes can alter the ecosystem functions of northern
peatlands. Several case studies have documented fen‐to‐bog transition (FBT) over recent …

Permafrost thaw in northern peatlands is likely to create a positive feedback to climate
change, as microbes transform soil carbon (C) into carbon dioxide (CO 2) or methane (CH …

Reconstructions of past climate impact, that is, radiative forcing (RF), of peatland carbon (C)
dynamics show that immediately after peatland initiation the climate warming effect of CH4 …

Peatland rewetting, a management effort to restore water levels in previously drained
peatlands, is important for re-establishing the role of these peatlands as carbon (C) sinks …

Peatland rewetting, which is a management effort to restore water levels in previously
drained peatlands, is important for re-establishing the role of peatlands as carbon (C) sinks …

Peatlands are unique ecosystems that support a wide range of very different ecological
functions and processes that provide essential ecosystem goods and services. Many …