Tree ring-based reconstruction of the long-terminfluence of wildfires on permafrost active layer dynamics in Central Siberia

• Published in: Science of The Total Environment
• Main Authors: Anastasia A. Knorre, Alexander V. Kirdyanov, Anatoly S. Prokushkin, Paul J. Krusic, Ulf, Büntgen
• Other Authors: Институт экологии и географии, Кафедра экологии и природопользования
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2019
• Subjects: Boreal forest; Ecological interaction; Ecosystem response; Seasonally thawing soil layer; Sphagnum; Larix gmelinii; 34.35; Active layer thickness; permafrost; Siberia
• Online Access: https://www.sciencedirect.com/science/article/pii/S0048969718340051; http://elib.sfu-kras.ru/handle/2311/129827; https://doi.org/10.1016/j.scitotenv.2018.10.124

Although it has been recognized that rising temperatures and shifts in the hydrological cycle affect the depth of the seasonally thawing upper permafrost stratum, it remains unclear towhat extent thefrequency and intensity ofwildfires, and subsequent changes in vegetation cover, influence the soil active layer on different spatiotemporal scales. Here, we use ring widthmeasurements of the subterranean stem part of 15 larch trees from a Sphagnum bog site in Central Siberia to reconstruct long-term changes in the thickness of the active layer since the lastwildfire occurred in 1899. Our approach reveals a three-step feedback loop between above- and belowground ecosystem components. After all vegetation is burned, direct atmospheric heat penetration over the first ~20 years caused thawing of the upper permafrost stratum. The slow recovery of the insulating ground vegetation reverses the process and initiates a gradual decrease of the active layer thickness. Due to the continuous spreading and thickening of the peat layer during the last decades, the upper permafrost horizon has increased by 0.52 cm/year. This study demonstrates the strength of annually resolved and absolutely dated tree-ring series to reconstruct the effects of historical wildfires on the functioning and productivity of boreal forest ecosystems at multi-decadal to centennial time-scale. In so doing, we show how complex interactions of above- and belowground components translate into successive changes in the active permafrost stratum. Our results are particularly relevant for improving long-term estimates of the global carbon cycle that strongly depends on the source and sink behavior of the boreal forest zone.