Articles | Volume 18, issue 13
https://doi.org/10.5194/bg-18-4185-2021
https://doi.org/10.5194/bg-18-4185-2021
Research article
 | 
14 Jul 2021
Research article |  | 14 Jul 2021

Wildfire history of the boreal forest of south-western Yakutia (Siberia) over the last two millennia documented by a lake-sediment charcoal record

Ramesh Glückler, Ulrike Herzschuh, Stefan Kruse, Andrei Andreev, Stuart Andrew Vyse, Bettina Winkler, Boris K. Biskaborn, Luidmila Pestryakova, and Elisabeth Dietze

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Cited articles

Aakala, T., Pasanen, L., Helama, S., Vakkari, V., Drobyshev, I., Seppä, H., Kuuluvainen, T., Stivrins, N., Wallenius, T., Vasander, H., and Holmström, L.: Multiscale variation in drought controlled historical forest fire activity in the boreal forests of eastern Fennoscandia, Ecol. Monogr., 88, 74–91, https://doi.org/10.1002/ecm.1276, 2018. 
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Alexander, H. D., Mack, M. C., Goetz, S., Beck, P. S. A., and Belshe, E. F.: Implications of increased deciduous cover on stand structure and aboveground carbon pools of Alaskan boreal forests, Ecosphere, 3, 1–21, https://doi.org/10.1890/ES11-00364.1, 2012. 
Andreev, A. A., Morozova, E., Fedorov, G., Schirrmeister, L., Bobrov, A. A., Kienast, F., and Schwamborn, G.: Vegetation history of central Chukotka deduced from permafrost paleoenvironmental records of the El'gygytgyn Impact Crater, Clim. Past, 8, 1287–1300, https://doi.org/10.5194/cp-8-1287-2012, 2012. 
Andreev, A. A., Tarasov, P. E., Wennrich, V., and Melles, M.: Millennial-scale vegetation history of the north-eastern Russian Arctic during the mid-Pliocene inferred from the Lake El'gygytgyn pollen record, Glob. Planet. Change, 186, 103111, https://doi.org/10.1016/j.gloplacha.2019.103111, 2020. 
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Data about past fire activity are very sparse in Siberia. This study presents a first high-resolution record of charcoal particles from lake sediments in boreal eastern Siberia. It indicates that current levels of charcoal accumulation are not unprecedented. While a recent increase in reconstructed fire frequency coincides with rising temperatures and increasing human activity, vegetation composition does not seem to be a major driver behind changes in the fire regime in the past two millennia.
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