Climate change has been partially mitigated by an increasing net land carbon sink in the
terrestrial biosphere; understanding the processes that drive this sink is thus essential for …

Peatlands are lands with a peat layer at the surface, containing a large proportion of organic
carbon. Such lands cover≈ 1 000 000 km2 in Europe, which is almost 10% of the total …

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

The northern peatland carbon sink plays a vital role in climate regulation; however, the
future of the carbon sink is uncertain, in part, due to the changing interactions of peatlands …

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

Water-table drawdown across peatlands increases carbon dioxide (CO2) and reduces
methane (CH4) emissions. The net climatic effect remains unclear. Based on global …

The water table and its dynamics are one of the key variables that control peatland
greenhouse gas exchange. Here, we tested the applicability of the Optical TRApezoid Model …

Long‐term carbon and nitrogen dynamics in peatlands are affected by both vegetation
production and decomposition processes. Here, we examined the carbon accumulation rate …

Wetlands are strategic areas for carbon uptake, but accurate assessments of their
sequestration ability are limited by the uncertainty and variability in their carbon balances …

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 …