When investigating past peatland processes and related carbon cycle dynamics, it is
essential to identify and separate different peat environments: bogs, fens and permafrost …

Past vegetation assemblages, preserved in peat layers, are one of the key proxies when
reconstructing historical peatland dynamics. Northern peatlands can be divided into two …

Permafrost dynamics play an important role in high‐latitude peatland carbon balance and
are key to understanding the future response of soil carbon stocks. Permafrost aggradation …

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 …

Soil organic carbon (SOC) in permafrost terrain is vulnerable to climate change. Perennially
frozen peat deposits store large amounts of SOC, but we know little about its chemical …

Peatlands provide a widespread terrestrial archive of Holocene environmental change. The
taphon omy of peat is relatively simple, the range of evidence and proxies is wide, and …

Peatland vegetation is controlled primarily by the depth of the water table, making peat
paleovegetation a useful climate archive. We applied a biochemical approach to …

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 are an important natural archive for past climatic changes, primarily due to their
sensitivity to changes in the water balance and the dating possibilities of peat sediments. In …

Subarctic permafrost peatlands are important soil organic carbon pools, and improved
knowledge about peat properties and peatland sensitivity to past climate change is essential …