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    Evidence that modern fires may be unprecedented during the last 3400 years in permafrost zone of Central Siberia, Russia
/ E. Y. Novenko, D. A. Kupryanov, N. G. Mazei [et al.] // Environ. Res. Lett. - 2022. - Vol. 17, Is. 2. - Ст. 025004, DOI 10.1088/1748-9326/ac4b53. - Cited References:48. - Field work and macroscopic charcoal analysis in the Putorana Plateau and Tura area were supported by the project 'Holocene climate and environmental records from the Central Siberian Plateau' funded by the Swiss Polar Institute. Field work and macroscopic charcoal analysis in Igarka area, data analysis and paper preparation were supported by Russian Science Foundation, Project 20-17-00043. . - ISSN 1748-9326
РУБ Environmental Sciences + Meteorology & Atmospheric Sciences

Аннотация: Recent climate change in Siberia is increasing the probability of dangerous forest fires. The development of effective measures to mitigate and prevent fires is impossible without an understanding of long-term fire dynamics. This paper presents the first multi-site palaeo-fire reconstruction based on macroscopic charcoal data from peat and lake sediment cores located in different landscapes across the permafrost area of central Siberia. The obtained results show similar temporal patterns of charcoal accumulation rates in the cores under study, and near synchronous changes in fire regimes. The paleo-fire record revealed moderate biomass burning between 3.4 and 2.6 ka BP, followed by the period of lower burning occurring from 2.6 to 1.7 ka BP that coincided with regional climate cooling and moistening. Minimal fire activity was also observed during the Little Ice Age (0.7-0.25 ka BP). Fire frequencies increased during the interval from 1.7 to 0.7 ka BP and appears to be partly synchronous with climate warming during the Medieval Climate Anomaly. Regional reconstructions of long-term fire history show that recent fires are unprecedented during the late Holocene, with modern high biomass burning lying outside millennial and centennial variability of the last 3400 years.

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Держатели документа:
Lomonosov Moscow State Univ, Fac Geog, Dept Phys Geog & Landscape Sci, Moscow, Russia.
Russian Acad Sci, Dept Quaternary Res, Inst Geog, Moscow, Russia.
Krasnoyarsk Sci Ctr SB RAS, Sukachev Inst Forest SB RAS, Fed Res Ctr, Krasnoyarsk, Russia.
Siberian Fed Univ, Krasnoyarsk, Russia.
Univ Edinburgh, Sch Geosci, Edinburgh, Midlothian, Scotland.
Univ Lausanne, Inst Earth Surface Dynam, Lausanne, Switzerland.
HSE Univ, Fac Geog & Geoinformat Technol, Moscow, Russia.

Доп.точки доступа:
Novenko, Elena Yu; Kupryanov, Dmitry A.; Mazei, Natalia G.; Prokushkin, Anatoly S.; Phelps, Leanne N.; Buri, Aline; Davis, Basil A. S.; Swiss Polar Institute; Russian Science FoundationRussian Science Foundation (RSF) [20-17-00043]