Climate change is undoubtedly a pressing environmental issue challenging the entire world.
To mitigate climate change, various methods have been proposed to reduce net carbon …

The carbon (C) accumulation histories of peatlands are of great interest to scientists, land
users and policy makers. Because peatlands contain more than 500 billion tonnes of C, an …

Peatlands are globally important stores of carbon (C) that contain a record of how their rates
of C accumulation have changed over time. Recently, near-surface peat has been used to …

Peatlands contain around one third of the global soil carbon (C) and play an important role
in the C cycle. In particular, the response of the productivity-decay balance to climate …

When a peatland is drained and cultivated, it behaves as a notable source of CO2. However,
we lack temporally and spatially explicit estimates of carbon losses from cultivated …

Peatlands contain one-third of the world's soil carbon (C). If destabilized, decomposition of
this vast C bank could accelerate climate warming; however, the likelihood of this outcome …

Peatlands are significant carbon (C) stores, playing a key role in nature-based climate
change mitigation. While the effectiveness of non-forested peatlands as C reservoirs is …

Peatlands are a major terrestrial carbon store and a persistent natural carbon sink during the
Holocene, but there is considerable uncertainty over the fate of peatland carbon in a …

Northern peatlands have cooled the global climate by accumulating large quantities of soil
carbon (C) over thousands of years. Maintaining the C sink function of these peatlands and …

Peatlands at high latitudes have accumulated> 400 Pg carbon (C) because saturated soil
and cold temperatures suppress C decomposition. This substantial amount of C in Arctic and …