Using an improved approach to investigate peatland carbon dynamics at different temporal scales across the pan-Arctic
The majority of northern peatlands were initiated during the Holocene around8,000 to 12,000 years ago. Owing to their mass imbalance, they have sequestered huge amounts of organic carbon in the terrestrial ecosystem. The distribution of soil organic carbon is widespread and uneven across the pan-Arctic (45-75ºN latitude).Recent syntheses have filled some existing gaps, however, the extent and remo
