“…For example, in Alberta alone, wildfire impacts an average of ∼208,000 ha every year (2006–2015; Government of Alberta, 2017) with fires liberating large quantities of the C stored in peatlands across the province to the atmosphere (approximately 4.7 × 10 9 g of C released per year; Turetsky et al, ). With fire frequency expected to roughly double by the end of the century, from enhanced warming and longer fire seasons (Wotton & Flannigan, ; Flannigan, Stocks, Turetsky, & Wotton, ; Flannigan et al ., ; Kirchmeier‐Young, Zwiers, Gillet, & Cannon, ; Hanes, Wang, Jain, Parisien, & Little, ), as well as an increase in the number of large high‐intensity wildfires (Tymstra et al ., ), boreal peatlands may be vulnerable to changes in wildfire regime under a rapidly changing climate. Despite these increasing pressures, the impact of fire on DOC concentration, quality, and export across boreal peatlands is not always consistent, with studies showing an increase (McEachern, Prepas, Gibson, & Dinsmore, ), no change (Carignan, D'Arcy, & Lamontagne, ; Lamontagne, Carignan, D'Arcy, Prairie, & Paré, ; Marchand et al ., ), or decrease (Betts & Jones, ) in DOC concentration in surface waters.…”