Nitrous oxide (N 2 O) is a potent greenhouse gas that contributes 6% to global warming (IPCC, 2013) and can cause ozone destruction in the stratosphere (Ravishankara et al., 2009). Northern peatlands have accumulated not only large stocks of organic carbon (C) but also a great amount of organic nitrogen (N), approaching 415 Pg C and 10 Pg N (Hugelius et al., 2020). Despite this large organic N storage, peatlands are nutrient-poor ecosystems because organic N is not like mineral N that can be absorbed by vegetation directly. This large amount of organic N has the potential to be mineralized and stimulate N 2 O production under future climate warming, elevated N deposition, and vegetation composition change.