Abstract
Wildfires release substantial quantities of carbon (C) into the atmosphere but they also convert part of the burnt biomass into pyrogenic organic matter (Py OM ). This is richer in C and, overall, more resistant to environmental degradation than the original biomass, and, therefore, Py OM production is an efficient mechanism for C sequestration. The magnitude of this C sink, however, remains poorly quantified, and current production estimates, which suggest that ~1‐5% of the C affected by fire is converted to Py OM , are based on incomplete inventories. Here, we quantify, for the first time, the complete range of Py OM components found in‐situ immediately after a typical boreal forest fire. We utilized an experimental high‐intensity crown fire in a jack pine forest ( Pinus banksiana ) and carried out a detailed pre‐ and postfire inventory and quantification of all fuel components, and the Py OM (i.e., all visually charred, blackened materials) produced in each of them. Our results show that, overall, 27.6% of the C affected by fire was retained in Py OM (4.8 ± 0.8 t C ha −1 ), rather than emitted to the atmosphere (12.6 ± 4.5 t C ha −1 ). The conversion rates varied substantially between fuel components. For down wood and bark, over half of the C affected was converted to Py OM , whereas for forest floor it was only one quarter, and less than a tenth for needles. If the overall conversion rate found here were applicable to boreal wildfire in general, it would translate into a Py OM production of ~100 Tg C yr −1 by wildfire in the global boreal regions, more than five times the amount estimated previously. Our findings suggest that Py OM production from boreal wildfires, and potentially also from other fire‐prone ecosystems, may have been underestimated and that its quantitative importance as a C sink warrants its inclusion in the global C budget estimates.