Abstract
This article describes the lake basins of the Jom-Bolok volcanic region in the East Sayan (the largest manifestation of the Holocene eruptions in Central Asia). The geomorphological position, origins, aspects of the structure and development are reviewed considering its sedimentary filling. The limnic morphogenesis here develops under the conditions of contrasting relief, high energy of neotectonic and exogenous processes. We established that Lake Khara-Nur, formed as a result of lava-damming of the Jom-Bolok river valley, emerged in its present form approximately 6500 years ago. A complex record on the environment and climatic changes, acquired from its sediments, made it possible to determine for the first time in this region the long-term trends in the development of the Middle and Late Holocene mountain geosystems and also the distinction of several paleogeographic stages of the formation of the natural environment. An average geochemical record resolution for the bottom sediments of the lake was made uniquely for the East Siberian lake records and is equal to 35 years, while the palynological record approximates 110 years.
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Adamovich A F, Grossvald M G, Zonenshain L P, 1959. New data on Kropotkin and Peretolchin volcanoes. Transactions of All-Union Aerogeology Trust, 5: 79–90. (in Russian)
Amosova A A, Panteeva S V, Chubarov V M et al., 2016. Determination of major elements by wavelength-dispersive X-ray fluorescence spectrometry and trace elements by inductively coupled plasma mass spectrometry in igneous rocks from the same fused sample (110 mg). Spectrochimica Acta Part B: Atomic Spectroscopy, 122: 62–68.
Arzhannikov S G, Braucher R, Jolivet M et al., 2012. History of Late Pleistocene glaciations in the central Sayan-Tuva Upland (southern Siberia). Quaternary Science Reviews, 49: 16–32.
Arzhannikov S G, Ivanov A V, Arzhannikova A et al., 2017. Age of the Jom-Bolok lava fields according to denrochronological and radiocarbon data. Russian Geology and Geophysics, 1: 27–47.
Berger A, Loutre M F, 1991. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews, 10(4): 297–317.
Bezrukova E V, Abzaeva A A, Letunova P P et al., 2005. Post-glacial history of Siberian spruce (Picea obovata) in the Lake Baikal area and the significance of this species as a paleo-environmental indicator. Quaternary International, 136: 47–57.
Bezrukova E V, Shchetnikov A A, Kuzmin M I et al., 2016. First data on the environment and climate change within the Jom-Bolok Volcanic Field (Eastern Sayan Mountains) in the Middle-Late Holocene. Doklady Earth Science, 468(3): 527–531.
Bronk R C, 2009. Bayesian analysis of radiocarbon dates. Radiocarbon, 51(1): 337–360.
Colman S M, Jones G A, Rubin M et al., 1996. AMS radiocarbon analyses from Lake Baikal, Siberia: Challenges of dating sediments from a large, oligotrophic lake. Quaternary Science Reviews, 15: 669–684.
Demske D, Heumann G, Granoszewski W et al., 2005. Late glacial and Holocene vegetation and regional climate variability evidenced in high-resolution pollen records from Lake Baikal. Global and Planetary Change, 46: 255–279.
Faegri K, Iverson J, Kaland P E et al., 1989. Textbook of Pollen Analysis. New York: Wiley, 579.
Gillespie A R, Burke R M, Komatsu G et al., 2008. Late Pleistocene glaciers in Darhad basin, northern Mongolia. Quaternary Research, 69: 169–187.
Grimm E C, 1987. CONISS: A Fortran 77 program for stratigraphically constrained cluster analysis by the method of incremental sum of squares. Computer Geoscience, 13: 13–35.
Grosswald M G, 1965. Development of Relief in the Sayan-Tuva Highland. Moscow: Nauka, 166. (in Russian)
Heiri O, Lotter A F, 2001. Effects of low count sums on quantitative environmental reconstructions: An example using subfossil chironomids. Journal of Paleolimnology, 26: 343–350.
Ivanov A V, Arzhannikov S G, Demonterova E I et al., 2011. Jom-Bolok Holocene volcanic field in the East Sayan Mts., Siberia, Russia: Structure, style of eruptions, magma compositions, and radiocarbon dating. Bulletin of Volcanology, 73: 1279–1294.
Kiselev A I, Medvedev M E, Golovko G A, 1979. Volcanism of the Baikal Rift Zone and Deep-Seated Magma Formation Problems. Moscow: Nauka, 164. (in Russian)
Komatsu G, Arzhannikov S G, Gillespie A R et al., 2009. Quaternary paleolake formation and cataclysmic flooding along the upper Yenisei River. Geomorphology, 104: 143–164.
Krivonogov S K, Sheinkman V S, Mistryukov A A, 2005. Ice damming of the Darhad paleolake (Northern Mongolia) during the late Pleistocene. Quaternary International, 136: 83–94.
Kropotkin P A, 1867. A trip to the Oka Guard Post. Memoirs of the Russian Geographical Society, Siberian Division. Irkutsk: Book, 9–10. (in Russian)
Mann M E, Zhang Z, Rutherford S et al., 2009. Global signatures and dynamical origins of the Little Ice Age and Medieval Climate Anomaly. Science, 326: 1256–1260.
Minyuk P S, Borkhodoev V Y, Wennrich V, 2014. Inorganic geochemistry data from Lake El’gygytgyn sediments: Marine isotope stages 6–11. Climate of the Past, 10: 467–485.
Moberg A, Sonechkin D M, Holmgren K et al., 2005. Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data. Nature, 433: 613–617.
Mortlock R A, Froelich P N, 1989. A simple method for the rapid determination of biogenic opal in pelagic marine sediments. Deep Sea Research, 36: 1415–1426.
Nesbitt H W, Young G M, 1982. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature, 299: 715–717.
Obruchev S V, Lurye M L, 1954. Kropotkin and Peretolchin volcanoes in East Sayan. Transactions Laboratory of Volcanology, 8: 210–225. (in Russian)
Pashkova G V, Aisueva T S, Finkelshtein A L et al., 2016. Analytical approaches for determination of bromine in sediment core samples by X-ray fluorescence spectrometry. Talanta, 160: 375–380.
Sharastepanov B D, 2007. Natural landscapes of the Oka Plateau and their use for tourist and recreational purposes. (Dr. Sci. (Geogr.) dissertation Thesis). 152. (in Russian)
Solovyova L N, 1976. Morphology of the Cryolithozone of the Sayan-Baikal Region. Novosibirsk: Nauka, 126. (in Russian)
Svensson A, Andersen K K, Bigler M et al., 2008. A 60 000 year Greenland stratigraphic ice core chronology. Climate of the Past, 4: 47–57.
Wang Y J, Cheng H, Edwards R L et al., 2001. A high-resolution absolute-dated Late Pleistocene Monsoon record from Hulu Cave, China. Science, 294: 2345–2348.
Yarmolyuk V V, Lebedev V I, Sugorakova A M, 2001. Eastern Tuva area of the youngest volcanism of Central Asia: Stages, products, and character of volcanic activity. Vulkanologiya i Seismologiya, 3: 3–32. (in Russian)
Yarmolyuk V V, Nikiforov A V, Ivanov V G, 2003. The structure, composition, sources and mechanism of Jombolok valley lava flows (Holocene, South-Baikal volcanic area). Vulkanologiya i Seismologiya, 5: 41–59. (in Russian)
Yuan D X, Cheng H, Edwards R L et al., 2004. Timing, duration, and transitions of the Last Interglacial Asian monsoon. Science, 304: 575–578.
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Foundation: The Ministry of Education and Science of the Russian Federation, the State Assignment No. IX.130.3.1. (0350-2016-0026), No. IX.136.2. (0346-2016-0005); Russian Science Foundation, No. 16-17-10079 (geomorphology, pollen and isotopic studies); Russian Foundation for Basic Research, No. 16-05-00586; The Project, No. 074-02-2018-334
Author: Shchetnikov Alexander, PhD and Senior Researcher, specialized in geomorphology and Quaternary geology.
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Shchetnikov, A., Bezrukova, E.V. Lakes of the Jom-Bolok Volcanoes Valley in the East Sayan Mts., Baikal region. J. Geogr. Sci. 29, 1823–1840 (2019). https://doi.org/10.1007/s11442-019-1681-3
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DOI: https://doi.org/10.1007/s11442-019-1681-3