Permafrost mires are very sensitive to climate variations and can potentially release considerable amounts of carbon to the atmosphere due to permafrost degradation. On the other hand, permafrost degradation may promote mires development, leading to atmospheric carbon sequestration in the form of peat. In order to understand the dynamics of mire development in a continuous permafrost region, we used a multi-proxy paleoecological reconstruction based on 120-year-old peat deposit from Central Siberia. At the initial stages, a waterlogged forest at the border of a permafrost mire was subjected to burning that resulted in further waterlogging leading to a quick transition from waterlogged forest to a poor fen over ca. 15 years. Further accelerated mire development and corresponding rapid peat accumulation coincided with climate warming and were associated with a post-fire succession on the surrounding area. This resulted in a formation of a dry forested oligotrophic mire. Overall, our findings demonstrate a substantial potential for permafrost mires to develop in the marginal zone after forest disturbance with the subsequent establishment of a new equilibrium between forests and mires in accordance with the climatic conditions.
AndreevRNovenkoE (2025) Quantitative pollen-based reconstructions of climate characteristics and forest coverage for Northern Central Siberia: Evaluation of different techniques. Quaternary International739: 109879.
2.
BabeshkoKVShkurkoATsyganovAN, et al. (2021) A multi-proxy reconstruction of peatland development and regional vegetation changes in subarctic NE Fennoscandia (the Republic of Karelia, Russia) during the Holocene. Holocene31(3): 421–432.
3.
BallardCEMcIntyreNWheaterHS (2012) Effects of peatland drainage management on peak flows. Hydrology and Earth System Sciences16(7): 2299–2310.
4.
BarberKE (1993) Peatlands as scientific archives of past biodiversity. Biodiversity and Conservation2(5): 474–489.
5.
BengtssonFRydinHBaltzerJL, et al. (2021) Environmental drivers of sphagnum growth in peatlands across the holarctic region. Journal of Ecology109(1): 417–431.
6.
BennettKDWillisKJ (2001) Pollen. In: SmolJPBirksHJLastWM (eds) Tracking Environmental Change Using Lake Sediments. Volume 3: Terrestrial, Algal, and Siliceous Indicators. Dordrecht: Springer Netherlands, pp.5–32.
7.
BeugHJ (2004) Leitfaden der Pollenbestimmung für Mitteleuropa und angrenzende Gebiete. Munchen: Verlag Dr. Friedrich Pfeil.
8.
BlaauwMChristenJA (2011) Flexible paleoclimate age-depth models using an autoregressive gamma process. Bayesian Analysis6(3): 457–474.
9.
CamillP (1999) Patterns of boreal permafrost peatland vegetation across environmental gradients sensitive to climate warming. Canadian Journal of Botany77(5): 721–733.
10.
CamillPLynchJAClarkJS, et al. (2001) Changes in biomass, aboveground net primary production, and peat accumulation following permafrost thaw in the boreal peatlands of Manitoba, Canada. Ecosystems4(5): 461–478.
11.
ChambersFMBeilmanDWYuZ (2011) Methods for determining peat humification and for quantifying peat bulk density, organic matter and carbon content for palaeostudies of climate and peatland carbon dynamics. Mires and Peat7: 07.
12.
ChambersFMCharmanDJ (2004) Holocene environmental change: Contributions from the peatland archive. Holocene14(1): 1–6.
13.
ChudinovaSMFrauenfeldOWBarryRG, et al. (2006) Relationship between air and soil temperature trends and periodicities in the permafrost regions of Russia. Journal of Geophysical Research Earth Surface111(F2): 2005JF000342.
14.
ClymoRSHaywardPM (1982) The ecology of Sphagnum. In: SmithAJE (ed.) Bryophyte Ecology. Dordrecht: Springer Netherlands, pp.229–289.
15.
DanevčičTMandic-MulecIStresB, et al. (2010) Emissions of CO2, CH4 and N2O from Southern European peatlands. Soil Biology and Biochemistry42(9): 1437–1446.
16.
ElowsonSRytterL (1986) Soil characteristics of raised sphagnum bog in relation to intensively grown deciduous species: Peat bulk density, water content, and pH during the growing season. Scandinavian Journal of Forest Research1(1–4): 95–111.
17.
EnacheMDCummingBF (2006) Tracking recorded fires using charcoal morphology from the sedimentary sequence of Prosser Lake, British Columbia (Canada). Quaternary Research65(02): 282–292.
18.
GrabovikSINazarovaLE (2013) Linear increment of sphagnum mosses on Karelian mires (Russia). Arctoa22: 23–26.
19.
GrimmEC (1987) CONISS: A FORTRAN 77 program for stratigraphically constrained cluster analysis by the method of incremental sum of squares. Computational Geosciences13(1): 13–35.
20.
GrimmTEGraphT (1990) PC spreadsheet and graphics software for pollen data. INQUA, Working Group on Data-Handling Methods. Newsletter4: 5–7.
21.
GuXTsyganovANMazeiNG, et al. (2025) Testate amoebae as paleohydrological indicators in the boreal and subarctic permafrost mires in the western part of the central Siberian Plateau. Quaternary Science Reviews349: 109108.
22.
HeadMJSteffenWFagerlindD, et al. (2022) The Great Acceleration is real and provides a quantitative basis for the proposed anthropocene Series/Epoch. Episodes45(4): 359–376.
23.
HuaQBarbettiMRakowskiAZ (2013) Atmospheric radiocarbon for the period 1950–2010. Radiocarbon55(4): 2059–2072.
24.
IgnatovMSIgnatovaEA (2003) Flora of Mosses of the Middle Part of European Russia. Moscow: KMK (in Russian).
25.
JensenKLynchEACalcoteR, et al. (2007) Interpretation of charcoal morphotypes in sediments from ferry Lake, Wisconsin, USA: Do different plant fuel sources produce distinctive charcoal morphotypes?Holocene17(7): 907–915.
Juselius-RajamäkiTVälirantaMKorholaA (2023) The ongoing lateral expansion of peatlands in Finland. Global Change Biology29(24): 7173–7191.
28.
KatzNYKatzSVSkobevaEI (1977) Atlas of Plant Remains in Peat. Moscow: Nedra-Press (in Russian).
29.
KharukVIRansonKJDvinskayaML (2008) Wildfires dynamic in the larch dominance zone. Geophysical Research Letters35(1): L01402.
30.
KirdyanovAVSaurerMSiegwolfR, et al. (2020) Long-term ecological consequences of forest fires in the continuous permafrost zone of Siberia. Environmental Research Letters15(3): 034061.
31.
KitsonEBellNGA (2020) The response of microbial communities to peatland drainage and rewetting. A review. Frontiers in Microbiology11: 582812.
32.
KnorreAAKirdyanovAVProkushkinAS, et al. (2019) Tree ring-based reconstruction of the long-term influence of wildfires on permafrost active layer dynamics in Central Siberia. Science of the Total Environment652: 314–319.
33.
KoretsMAProkushkinAS (2019) The GIS-based approach for the permafrost active layer depth mapping. Proceedings of the International Cartographic Association2: 1–6.
34.
KornilievNV (1959) Nizhny Tunguska forest fires and their control features. Forestry Journal5: 30–34 (in Russian).
35.
KrivobokovLVZverevAA (2017) Analysis of local flora in northern boreal subzone of middle Siberia (Tura settlement, middle course of Nizhnyaya Tunguska river). In: Proceedings of the VI international scientific conference dedicated to the 100th anniversary of the birth of A.V. Pologiy, Tomsk, Russia, 24-26 October, pp.60–63. Tomks: Publishing House of Tomsk State University (in Russian).
36.
KrivobokovLVZverevAAMukhortovaLV (2015) Floristic characteristics, types and ecology of larch forests of the middle Siberia of northern boreal subzone. Ecological Safety9: 190–198.
37.
KrügerJPLeifeldJGlatzelS, et al. (2015) Biogeochemical indicators of peatland degradation – A case study of a temperate bog in northern Germany. Biogeosciences12(10): 2861–2871.
38.
LapshinaED (2003) Flora of the Mires of the Southeast of Western Siberia. Tomsk: University Press (in Russian).
39.
Leal FilhoWDinisMAPNagyGJ, et al. (2023) On the (melting) rocks: Climate change and the global issue of permafrost depletion. Science of the Total Environment903: 166615.
40.
LeeHCalvinKDasguptaD, et al. (2023) Climate Change 2023: Synthesis Report. Contribution of Working Groups I, II and III to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change. Geneva: Intergovernmental Panel on Climate Change.
41.
LeifeldJKleinKWüst-GalleyC (2020) Soil organic matter stoichiometry as indicator for peatland degradation. Scientific Reports10(1): 7634.
42.
LoiselJGallego-SalaAVYuZ (2012) Global-scale pattern of peatland sphagnum growth driven by photosynthetically active radiation and growing season length. Biogeosciences9(7): 2737–2746.
43.
MauquoyDVan GeelB (2013) Plant macrofossil methods and studies: Mire and peat macros. In: EliasSAMockCJ (eds) Encyclopedia of Quaternary Science, 2nd edn. Amsterdam: Elsevier, pp.637–656.
44.
MazeiNGNovenkoEY (2021) The use of propionic anhydride in the sample preparation for pollen analysis. Nature Conservation Research6(3): 110–112 (In Russian).
45.
MazeiNGProkushkinASKupriyanovDA, et al. (2021) Impact of fires on the dynamics of forest ecosystems in central Evenkia during the last 3.5 ka. Lomonosov Geography Journal5: 78–90 (In Russian).
46.
MazeiYATsyganovANBobrovskyMV, et al. (2020) Peatland development, vegetation history, climate change and human activity in the Valdai uplands (Central European Russia) during the Holocene: A multi-proxy palaeoecological study. Diversity12(12): 462.
47.
MazeiYATsyganovANBubnovaOA (2007) Structure of a community of testate amoebae in a Sphagnum dominated bog in upper sura flow (Middle Volga territory). Biology Bulletin34: 382–394.
48.
MazeiYATsyganovANErshovaEG, et al. (2023) Multi-proxy paleoecological reconstruction of peatland initiation, development and restoration in an urban area (Moscow, Russia). Diversity15(3): 448.
49.
McCartyJLAaltoJPaunuV-V, et al. (2021) Reviews and syntheses: Arctic fire regimes and emissions in the 21st century. Biogeosciences Discussions18: 5053–5083.
50.
MoazeniSCerdàA (2024) The impacts of forest fires on watershed hydrological response. A review. Trees, Forests and People18: 100707.
51.
MooneySDTinnerW (2011) The analysis of charcoal in peat and organic sediments. Mires and Peat7: 09.
MukhortovaLPashenovaNMetelevaM, et al. (2021) Temperature sensitivity of CO2 and CH4 fluxes from coarse woody debris in northern boreal forests. Forests12(5): 624.
54.
MustaphiCJCPisaricMFJ (2014) A classification for macroscopic charcoal morphologies found in Holocene lacustrine sediments. Progress in Physical Geography: Earth and Environment38(6): 734–754.
55.
NielsenRW (2018) Mathematical analysis of anthropogenic signatures: The Great Deceleration. arXiv preprint arXiv:1803.06935.
56.
NielsenRW (2021) The great deceleration and proposed alternative interpretation of the anthropocene. Episodes44(2): 107–114.
57.
NobleIR (1993) A model of the responses of ecotones to climate change. Ecological Applications3(3): 396–403.
58.
NovenkoEMazeiNShatunovA, et al. (2024) Modern pollen–vegetation relationships: A view from the larch forests of Central Siberia. Land13(11): 1939.
59.
NovenkoERudenkoOMazeiN, et al. (2023) Effects of climate change and fire on the middle and late Holocene forest history in Yenisei Siberia. Forests14(12): 2321.
60.
NovenkoEYMazeiNGKupriyanovDA, et al. (2021) Subfossil spore–pollen spectra from larch forests of Central Evenkia: Special aspects of interpretation for paleoecological research purposes. Russian Journal of Ecology52(6): 429–437.
61.
ParmuzinYP (1979) Tundrolesie SSSR. Moscow: Mysl (in Russian).
62.
PolozhigoAV (1983) Flora Krasnoyarskogo Kraya. Tomsk: TGU-Press (in Russian).
PrevidiMSmithKLPolvaniLM (2021) Arctic amplification of climate change: A review of underlying mechanisms. Environmental Research Letters16(9): 093003.
65.
ProkushkinASGavrilenkoIVAbaimovAP, et al. (2006) Dissolved organic carbon in upland forested watersheds underlain by continuous permafrost in Central Siberia. Mitigation and Adaptation Strategies for Global Change11: 223–240.
66.
QinYPayneRGuY, et al. (2017) Short-term response of testate amoebae to wildfire. Applied Soil Ecology116: 64–69.
67.
RatcliffeJLPayneRJSloanTJ, et al. (2018) Holocene carbon accumulation in the peatlands of northern Scotland. Mires and Peat23: 03–30.
68.
R Core Team (2025) _R: A Language and Environment for Statistical Computing_. Vienna: R Foundation for Statistical Computing, Available at: https://www.R-project.org/ (accessed 16 April 2025).
69.
ReilleM (1999) Pollen et spores d’Europe et d’Afrique du Nord. Marseille: FeniXX réédition numérique (Laboratoire de botanique historique et palynologie).
70.
ReimerPJAustinWENBardE, et al. (2020) The IntCal20 Northern Hemisphere radiocarbon age calibration curve (0–55 cal kBP). Radiocarbon62(4): 725–757.
71.
SchippergesBRydinH (1998) Response of photosynthesis of sphagnum species from contrasting microhabitats to tissue water content and repeated desiccation. New Phytologist140(4): 677–684.
72.
SerrezeMCBarryRG (2011) Processes and impacts of Arctic amplification: A research synthesis. Global and Planetary Change77(1–2): 85–96.
73.
ShabalinaOMGrenaderovaAVBezkorovaynayaIN, et al. (2021) Conjugated dynamics of vegetation and testate amoebae associations restoration on burned-out areas in central Evenkia forests. Lesovedenie3: 278–289.
74.
SimpsonGL (2007) Analogue methods in palaeoecology: Using the analogue package. Journal of Statistical Software22(2): 1–29.
75.
SirinAA (2022) Mires and peatlands: Carbon, greenhouse gases, and climate change. Biology Bulletin Reviews12(2): 123–139.
76.
SimardMLecomteNBergeronY, et al. (2007) Forest productivity decline caused by successional paludification of boreal soils. Ecological Applications17: 1619–1637.
77.
SmithAJGoetzEM (2021) Climate change drives increased directional movement of landscape ecotones. Landscape Ecology36(11): 3105–3116.
78.
SofronovMA (1988) Pyrological characteristic of vegetation in the upper part of the river Turukhan basin. In: GlavatskiyGD (ed.) Forest Fires and Their Fighting. Moscow: VNIILM, pp.106–116 (in Russian).
StockmarrJ (1971) Tables with spores used in absolute pollen analysis. Pollen et Spores13: 615–621.
81.
SwindlesGTMorrisPJMullanDJ, et al. (2019) Widespread drying of European peatlands in recent centuries. Nature Geoscience12(11): 922–928.
82.
TrofimovVTVasilchukYBaulinVV, et al. (1989) Geocryology of the USSR. Moscow: Nedra (In Russian).
83.
TsyganovANZarovEAMazeiYA, et al. (2021) Key periods of peatland development and environmental changes in the middle taiga zone of western Siberia during the Holocene. Ambio50(11): 1896–1909.
84.
TuretskyMRBenscoterBPageS, et al. (2015) Global vulnerability of peatlands to fire and carbon loss. Nature Geoscience8(1): 11–14.
85.
TuretskyMRDonahueWFBenscoterBW (2011) Experimental drying intensifies burning and carbon losses in a northern peatland. Nature Communications2(1): 514.
86.
TuretskyMRWiederRKVittDH, et al. (2007) The disappearance of relict permafrost in boreal north America: Effects on peatland carbon storage and fluxes. Global Change Biology13(9): 1922–1934.
87.
UpdegraffKBridghamSDPastorJ, et al. (2001) Response of CO2 and CH4 emissions from peatlands to warming and water table manipulation. Ecological Applications11(2): 311–326.
88.
VeraverbekeSDelcourtCJKukavskayaE, et al. (2021) Direct and longer-term carbon emissions from arctic-boreal fires: A short review of recent advances. Current Opinion in Environmental Science and Health23: 100277.
89.
VinogradovaAASmirnovNSKorotkovVN, et al. (2015) Forest fires in Siberia and the far East: Emissions and atmospheric transport of black carbon to the Arctic. Atmospheric and Oceanic Optics28(6): 566–574.
90.
VoigtCMarushchakMEMastepanovM, et al. (2019) Ecosystem carbon response of an arctic peatland to simulated permafrost thaw. Global Change Biology25(5): 1746–1764.
91.
WalkerMJCBerkelhammerMBjörckS, et al. (2012) Formal subdivision of the Holocene Series/Epoch: A discussion paper by a Working Group of INTIMATE (Integration of ice-core, marine and terrestrial records) and the Subcommission on Quaternary Stratigraphy (International Commission on Stratigraphy). Journal of Quaternary Science27(7): 649–659.
92.
WicklandKPStrieglRGNeffJC, et al. (2006) Effects of permafrost melting on CO2 and CH4 exchange of a poorly drained black spruce lowland. Journal of Geophysical Research Biogeosciences111(2): 2005JG000099.
93.
XuJMorrisPJLiuJ, et al. (2018) PEATMAP: Refining estimates of global peatland distribution based on a meta-analysis. CATENA160: 134–140.
94.
YangZPOuYHXuXL, et al. (2010) Effects of permafrost degradation on ecosystems. Acta Ecologica Sinica30(1): 33–39.
95.
YoshikawaKHinzmanLD (2003) Shrinking thermokarst ponds and groundwater dynamics in discontinuous permafrost near council, Alaska. Permafrost and Periglacial Processes14(2): 151–160.
96.
YuZC (2012) Northern peatland carbon stocks and dynamics: A review. Biogeosciences9(10): 4071–4085.
97.
ZhangHVälirantaMSwindlesGT, et al. (2022) Recent climate change has driven divergent hydrological shifts in high-latitude peatlands. Nature Communications13(1): 4959.
