Arctic wetlands are known methane (CH4) emitters but recent studies suggest that the Arctic
CH4 sink strength may be underestimated. Here we explore the capacity of well-drained …

Respiration plays a key role in the terrestrial carbon cycle and is a fundamental metabolic
process in all plant tissues and cells. We review respiration from the perspective of plants …

Boreal peatlands represent a biogeochemically unique and diverse environment in high-
latitude landscape. They represent a long-term globally significant sink for carbon dioxide …

Past efforts to synthesize and quantify the magnitude and change in carbon dioxide (CO 2)
fluxes in terrestrial ecosystems across the rapidly warming Arctic-Boreal Zone (ABZ) have …

In view of climate considerations regarding the management of peatlands, there is a need to
assess whether rewetting can mitigate greenhouse gas (GHG) emissions, and notably how …

The focus of current water management in drained peatlands is to facilitate optimal
drainage, which has led to soil subsidence and a strong increase in greenhouse gas (GHG) …

Accurate prediction of soil respiration (Rs) under climate change requires a comprehensive
understanding of the dominant factors. However, the combined effects of multiple …

Mires form a large part of the boreal Swedish landscape and are important for biodiversity
and natural ecosystem processes. Historically, mires also played a key role for the …

Root phenology influences the timing of plant resource acquisition and carbon fluxes into
the soil. This is particularly important in fen peatlands, in which peat is primarily formed by …

Northern peatlands are globally significant carbon stores, but the sink strength varies from
year to year due to changes in environmental conditions. Ecosystem respiration (ER) is …