Carbon and nitrogen losses from degraded wetlands and methane emissions from flooded
wetlands are both important sources of greenhouse gas emissions. However, the net …

High-latitude peatlands are changing rapidly in response to climate change, including
permafrost thaw. Here, we reconstruct hydrological conditions since the seventeenth century …

This paper presents a review on more than hundred years of palaeoenvironmental research
in Sweden; from early descriptions of peat and tufa deposits in the late nineteenth and early …

Substantial amounts of money have been invested in peatland restoration over the last
decades to address the current challenges of global changes and to enhance biodiversity …

Northern peatlands are a major component of the global carbon (C) cycle. Widespread
climate‐driven ecohydrological changes in these ecosystems can have major …

Peatland rewetting has been proposed as a vital climate change mitigation tool to reduce
greenhouse gas emissions and to generate suitable conditions for the return of carbon (C) …

Northern aapa mire complexes are characterized by patterned fens with flarks (wet fen
surfaces) and bog zone margins with Sphagnum moss cover. Evidence exists of a recent …

We investigated recent changes in spatial patterning of fen and bog zones in five boreal
aapa mire complexes (mixed peatlands with patterned fen and bog parts) in a multiproxy …

Wetlands play a crucial role in the carbon cycle as they are the largest natural source of
methane, a potent greenhouse gas. Changes in wetland hydrology can alter the rate of …

Northern peatlands store 300–600 Pg C, of which approximately half are underlain by
permafrost. Climate warming and, in some regions, soil drying from enhanced evaporation …