Abstract
In this work, the reconstruction of past vegetation and fire dynamics in northern Altai is performed by a pollen and charcoal investigation into the peat deposits of the Maly Labysh mire located in the upper reaches of the Kondoma River in Shorsky National Park. Lithology and radiocarbon dating have shown that the mire is of lacustrine origin. An oxbow lake originated about 3000 years ago, and about 2200 years ago it turned into a swamp. A spore–pollen (SP) analysis of lacustrine and peat deposits revealed repeated changes in the vegetation cover, probably caused by climate instability during the last 3000 years. In general, two humid millennial periods (3000–1800 cal yr BP and 550–200 cal yr BP) were identified when the role of fir increased in the forests, alternating with two drier periods (1600–900 cal yr BP and 200 cal yr BP—contemporary), when the fir gave way to birch forests. This article also represents data on the dynamics of paleofires in the area of the Maly Labysh mire based on micro- and macrocharcoal analyses. A comparison of the results of pollen and charcoal investigations with other paleoclimatic reconstructions in Western Siberia in the Holocene is given. A conclusion is drawn about the connection between paleofires and the dynamics of humidity of the climate, which together influenced the vegetation change in Gornaya Shoriya.
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1134%2FS1995425522020020/MediaObjects/12259_2022_8218_Fig1_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1134%2FS1995425522020020/MediaObjects/12259_2022_8218_Fig2_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1134%2FS1995425522020020/MediaObjects/12259_2022_8218_Fig3_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1134%2FS1995425522020020/MediaObjects/12259_2022_8218_Fig4_HTML.png)
Similar content being viewed by others
REFERENCES
Arkhipov, S.A. and Volkova, V.S., Geologicheskaya istoriya, landshafty i klimaty pleistotsena Zapadnoi Sibiri (Geological History, Landscapes, and Climates of the Pleistocene of Western Siberia), Novosibirsk: Ob”ed. Inst. Geol., Geofiz. Miner., Sib. Otd., Ross. Akad. Nauk, 1994.
Bezrukova, E.V., Vershinin, K.E., Orlova, L.A., Letunova, P.P., Krapivina, S.M., Chepinoga, V., Verkhozina, A.V., Dudareva, N.N., and Abzaeva, A.A., Vegetation and climate of the high-mountain zone of the Eastern Sayan in the late Holocene, Geol. Geofiz., 2003, vol. 44, no. 4, pp. 380–384.
Blaauw, M. and Christen, J.A., Flexible paleoclimate age-depth models using an 601 autoregressive gamma process, Bayesian Anal., 2011, vol. 6, pp. 457–474.
Blyakharchuk, T.A., Novye paleopalinologicheskie dannye o dinamike rastitel’nogo pokrova i klimata Zapadnoi Sibiri i prilegayushchikh territorii (New Paleopalinological Data on the Dynamics of Vegetation Cover and Climate in Western Siberia and Adjacent Territories in the Holocene), Novosibirsk: GEO, 2012.
Blyakharchuk, T.A. and Kurina, I.V., Late Holocene environmental and climatic changes in the Western Sayan Mountains based on high-resolution muliproxy data, Boreas, 2021, vol. 50, pp. 919–934. https://doi.org/. ISSN 0300-9483https://doi.org/10.1111/bor.12493
Blyakharchuk, T.A., Wright, H.E., Borodavko, P.S., van der Knaap, W.O., and Ammann, B., Late Glacial and Holocene vegetational changes on the Ulagan high-mountain plateau, Altai Mountains, southern Siberia, Palaeogeogr., Palaeoclimatol., Palaeoecol., 2004, vol. 209, pp. 259–279.
Blyakharchuk, T.A., Chernova, N.A., and Blyakharchuk, P.A., Mires of Mountain Shoria, Materialy XIII Mezhdunarodnoi nauchno-prakticheskoi konferentsii “Problemy botaniki Yuzhnoi Sibiri i Mongolii,” Barnaul, 20–23 oktyabrya 2014 g. (Proc. XIII Int. Sci.-Pract. Conf. “Botany of Southern Siberia and Mongolia,” Barnaul, October 20–23, 2014), Shmakov, A.I. and Kopytina, T.M., Eds., Barnaul: Kontsept, 2014, pp. 37–39.
Bobrov, A.E., Kupriyanova, A.U., Litvintseva, I.D., and Tarasevich, V.F., Spory paporotnikoobraznykh i odnodol’nykh rastenii flory evropeiskoi chasti SSSR (Spores of Ferns and Pollen of Gymnosperms and Monocotyledons of Flora of the European Part of the USSR), Leningrad: Nauka, 1983.
Christen, J.A. and Perez, E.S., A new robust statistical model for radiocarbon data, Radiocarbon, 2009, vol. 51, pp. 1047–1059.
Krivonogov, S.K., Yamamuro, M., Takahara, H., Kazansky, A.Y., Klimin, M.A., Bobrov, V.A., Safonova, I.Y., Phedorin, M.A., and Bortnikova, S.B., An abrupt ecosystem change in Lake Beloye, southern Western Siberia: palaeclimate versus local environment, Palaeogeogr., Palaeoclimatol., Palaeoecol., 2012, vols. 331–332, pp. 194–206.
Grimm, E.C., TGView Version 2.0.41, Springfield: Illinois State Mus., 2004.
Kupriyanova, L.A. and Aleshina, L.A., Pyl’tsa dvudol’nykh rastenii flory evropeiskoi chasti SSSR (Pollen of Dicotyledonous Plants in Flora of the European Part of the USSR), Leningrad: Nauka, 1978.
Kur’ina, I.V. and Blyakharchuk, T.A., Analysis of the water cut level in the Malyi Labysh bog in the south of Western Siberia over the past two millennia, Trudy Mezhdunarodnoi konferentsii i shkoly molodykh uchenykh po izmereniyam, modelirovaniyu i informatsionnym sistemam dlya izucheniya okruzhayushchei sredy “Enviromis 2020,” Tomsk, 7–11 senyabrya 2020 g. (Proc. Int. Conf. and School of Young Scientists on Measurements, Modeling, and Information Systems for Study of Environment “Enviromis 2020,” Tomsk, September 7–11, 2020), Tomsk: Tomsk. Tsentr Nauchno-Tekh. Inf., 2020a, pp. 185–188.
Kurina, I.V. and Blyakharchuk, T.A., Analysis of surface wetness changes in the Maly Labysh mire in south of Western Siberia during the last two millennia, IOP Conf. Ser.: Earth Environ. Sci., 2020b, vol. 611, art. ID 012025
Kurina, I.V. and Li, H., Why do testate amoeba optima related to water table depth vary? Microb. Ecol., 2019, vol. 77, pp. 37–55.
Moore, P.D., Web, J.A., and Collinson, M.E., Pollen Analysis, London: Blackwell, 1991, 2nd ed.
Mikhailova, A.D., Grenaderova, A.V., Kurina, I.V., Shumilovskikh, L.S., and Stojko, T.G., Holocene vegetation and hydroclimate changes in the Kansk forest steppe, Yenisei River Basin, East Siberia, Boreas, 2021, vol. 50, no. 4, pp. 948–966. https://doi.org/10.1111/bor.12542
Mooney, S. and Tinner, W., The analysis of charcoal in peat and organic sediments, Mires Peat, 2011, vol. 7, pp. 1–18.
R Core Team, R: A Language and Environment for Statistical Computing, Vienna: R Found. Stat. Comput., 2017. http://www.R-project.org/.
Rudaya, N., Krivonogov, S., Słowiński, M., Cao, X., and Zhilich, S., Postglacial history of the Steppe Altai: climate, fire and plant diversity, Quat. Sci. Rev., 2020, vol. 249, art. ID 106616. https://doi.org/10.1016/j.quascirev.2020.106616
Volkova, V.S., Bakhareva, V.A., and Levina, T.P., Vegetation and climate of the Holocene of Western Siberia, in Paleoklimaty pozdnelednikov’ya i golotsena (Paleoclimates of the Late Glacial and Holocene), Khotinskii, N.A., Ed., Moscow: Nauka, 1989, pp. 90–95.
Whitlock, C. and Larsen, C., Charcoal as a fire proxy, in Tracking Environmental Change Using Lake Sediments: Terrestrial, Algal, and Siliceous Indicators, Dev. Paleoenviron. Res., vol. 3, Dordrecht: Springer-Verlag, 2002, pp. 75–97.
Zakkh, V.A., Volkov, I.N., Zimina, O.Yu., Skochina, S.N., Chikunova, I.Yu., Usacheva, I.V., and Tsebalyuk, S.I., Adaptation, transformation, and interaction of cultures in the Holocene of Tobol-Ishim in transitional periods, in Adaptatsiya narodov i kul’tur k izmeneniyam prirodnoi sredy (Adaptation of Peoples and Cultures to Changes of the Nature Environment), Derevyanko, A.P., Kudelin, A.B., and Tishkov, V.A., Eds., Moscow: Ross. Polit. Entsiklopediya, 2010, pp. 97–106.
Zhilich, S., Rudaya, N., Krivonogov, S., Nazarova, L., and Pozdnyakov, D., Environmental dynamics of the Baraba forest-steppe (Siberia) over the last 8000 years and their impact on the types of economic life of the population, Quat. Sci. Rev., 2017, vol. 163, pp. 152–161.
Funding
This work was supported by the Russian Foundation for Basic Research, grant no. 20-55-53015/GFEN_a, and the state budget theme of the IMCES SB RAS FWRG-2021-0003 no. 121031300226-5. We thank P.A. Blyakharchuk for help in field works and A.V. Grenaderova for providing a botanical analysis of peat.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Blyakharchuk, T.A., Pupysheva, M.A. Dynamics of Vegetation and Fires in Gornaya Shoriya (Northern Altai Mountains) in the Late Holocene According to Palynological and Charcoal Research into the Maly Labysh Mire. Contemp. Probl. Ecol. 15, 109–117 (2022). https://doi.org/10.1134/S1995425522020020
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1134/S1995425522020020