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Modern Mineral Formation in the Thermal Lake Fumarolnoe (Uzon Caldera, Kamchatka) as a Key to Paleoreconstruction

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Abstract

Paleoreconstruction of events involved in the bottom sedimentation has been carried out on the basis of mineral composition of the section of the minor lake IV (Lake Fumarolnoe, Kamchatka) bottom sediments. The lower sediments are composed mainly of smectite in association with gypsum and jarosite; they are overlain by smectite–kaolinite with a large amount of framboidal pyrite and diatom shells. There is also a layer of sinter opal–pyrite units and calcite. It is concluded that initially the minor lake IV was a mud pit with sulfide-bearing solutions. Then, after the lowering of the water level and the partial exposure of the bottom sediments on the surface, the latter were oxidized. The subsequent phreatic explosion provided the covering of oxidized sediments with the reduced substance from the lower horizons of the pit. Further setting of sediment accumulation corresponded to a source with cyanobacterial community developing around the gryphon, and then it changed to that of a shallow-water lake similar to a contemporary one. Sediments also include two layers of pyroclastic material originated from eruptions of neighboring volcanoes.

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REFERENCES

  1. Bychkov, A.Yu., Geokhimicheskaya model’ sovremennogo rudoobrazovaniya v kal’dere Uzon (Kamchatka) (Geochemical Model of the Modern Ore Formation in the Uzon Caldera (Kamchatka)), Moscow: GEOS, 2009.

  2. Dobretsov, N.L., Lazareva, E.V., Zhmodik, S.M., Bryanskaya, A.V., Morozova, V.V., Tikunova, N.V., Peltek, S.E., Karpov, G.A., Taran, O.P., Ogorodnikova, O.L., Kirichenko, I.S., Rozanov, A.S., Babkin, I.V., Shuvaeva, O.V., and Chebykin, E.P., Geological, hydrogeochemical, and microbiological characteristics of the Oil Site of the Uzon caldera (Kamchatka), Russ. Geol. Geophys., 2015, vol. 56, pp. 39–63.

    Article  Google Scholar 

  3. Gazogidrotermy aktivnykh vulkanov kamchatki I Kurl’skikh ostrovovo: sostav, stroenite, genezis (Gaseous Hydrothermal Active Voclanoes of Kamchatka and Kuril Islands: Composition, Structure, and Genesis), Gaskova, O.L. and Manshtein, A.K., Novosibirsk” INGG SO RAN, 2013.

  4. Karpov, G.A., Pavlov, A.L., and Kuznetsov, V.A., Uzon–geizernaya girdotermal’naya rudoobrazuyushchaya Sistema Kamchatki. Fiziko-khimicheskoi ocherk (Uzon–Geyser Hydrothermal Ore-Forming System of Kamchatka. Physico-Chemical Essay), Novosibirsk: Nauka, 1976.

  5. Kirichenko, I.S., Lazareva, E.V., Zhmodik, S.M., Belyanin, D.K., Ogorodnikova, O.L., and Miroshnichenko, L.V., Geochemical and mineralogical features of the bottom sediment of the “Sizy” mud pit (caldera Uzon, Kamchatka). Geol. Miner. Res. Sibiri, 2014, no. 3c, pp. 80–85.

  6. Lazareva, E.V., Anisimova, N.S., Bryanskaya, A.V., Ogorodnikova, O.L., and Zhmodik, S.M., “Features of mineral formation in microbial communities developing along the outflow of Termofil’nyi vent (Uzon caldera, Kamchatka), Tr. Kronotsk. Gos. Biosfer. Zapovednika (Proc. Kronotsky State Biosphere Reserve), Mosolov, V.I., Eds., Petropavlovsk-Kamchatsky: Kamchatpress, 2012, pp. 143–156.

  7. Migdisov, A.A. and Bychkov, A.Y., The behaviour of metals and sulphur during the formation of hydrothermal mercury-antimony-arsenic mineralization, Uzon caldera, Kamchatka, Russia, J. Volcanol. Geotherm. Res., 1998, vol. 84, no. 1, pp. 153–171.

    Article  Google Scholar 

  8. Popa, R., Kinkle, B.K., and Badescu, A., Pyrite framboids as biomarkers for iron-sulfur systems, Geomicrobiol. J., 2004, vol. 21, no. 3, pp. 193–206.

    Article  Google Scholar 

  9. Vulkanizm, gidrotermal’nyi protsess i rudoobrazovanie (Volcanism, Hydrothermal Process, and Ore Formation), Naboko, S.I., Eds., Leningrad: Nedra, 1974.

    Google Scholar 

  10. Yeroshchev-Shak, V.A., Karpov, G.A., Kireyev, F.A., and Bochko, R.A., Thermal Lake Fumarol’noye: a basin of active ore deposition in Kamchatka, Int. Geol. Rev., 1985, vol. 27, no. 10, pp. 1135–1148.

    Article  Google Scholar 

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Funding

The work was carried out in the framework of State Contract no. VIII.72.2.3 (0330-2016-0011) in the Collective Multiple Element and Isotope Research Center of Scientific Studies, IGM SB RAS, and was supported by the Siberian branch program of the Russian Academy of Sciences (Interdisciplinary Integrated Research grant no. 51).

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Correspondence to I. S. Kirichenko.

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Translated by N. Astafiev

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Kirichenko, I.S., Lazareva, E.V., Zhmodik, S.M. et al. Modern Mineral Formation in the Thermal Lake Fumarolnoe (Uzon Caldera, Kamchatka) as a Key to Paleoreconstruction. Geol. Ore Deposits 61, 747–755 (2019). https://doi.org/10.1134/S1075701519080063

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