Abstract
According to data of dendrochronological investigations of larch trees that had grown on the Patom crater (Irkutsk oblast, Bodaibinskii district) and near its base, the initial period of the formation of the crater can be dated back to the late 15th‒early 16th centuries. In 1841‒1842, the trees under investigation recorded in annual rings a catastrophic event which caused a disturbance to their root systems, damage to tree stems, and the formation of compression wood. It is obvious that the event is associated with the time of formation of the late stage ring swell on which sparse larch trees are 93‒101 years of age, and on the central mound emerging upon completion of the formation of the Patom crater the age of the oldest tree is 7 years. Thus dendrochronological investigations confirm a long-lasting and multievent formation of the Patoma crater. In some periods, the deposition cone was evolving with a different intensity, sometime showing an explosive character. X-ray fluorescent analysis revealed a double Sr enrichment of larch wood at the time of significant activity of crater formation (1852‒1859) when plutonic fluids from the igneous source were able to enter the upper horizons of the Earth’s crust at the time of magma intrusion into water-containing rocks. The fluids were enriched with CO2 and transported significant amounts of Sr, as a result of which the 87Sr/86Sr ratios in carbonate and terrigenous rocks assumed higher values in sandstone and schists on the early stage ring swell of the Patoma crater. The findings, coupled with geological data, suggest that the Patom crater emerged as a result of a phreatic explosion that occurred either at the time of magma intrusion into water-containing rocks or as a consequence of the fault and decompression of heated water-containing rocks.
Similar content being viewed by others
REFERENCES
Kolpakov, V.V., A Mysterious Crater in the Patoma Highlands, Priroda, 1951, nos. 1–2, pp. 58–61 [in Russian].
Portnov, A.M., On the Crater on the Patoma Highlands, Meteoritika, 1964, issue 25, pp. 194–195 [in Russian].
Portnov, A.M., The Patoma Crater – Evidence of the Tunguska Event? Zemlya i Vselennaya, 1993, no. 1, pp. 77–81 [in Russian].
Cook E.R., Kairiukstis L.A. Methods of Dendrochronology: Applications in the Environmental Sciences, E.R. Cook and L.A. Kairiukstis, Eds., Dordrecht: Springer Science+Business Media, 1990.
Rinn, F., TSAP v. 3.5. Reference Manual. Computer Program for Tree-Ring Analysis and Presentation, Heidelberg: Frank Rinn Distrib., 1996.
Campelo, F., García-González, I., and Nabais, C., DetrendeR – A Graphical User Interface to Process and Visualize Tree-Ring Data Using R, Dendrochronologia, 2012, vol. 30, issue 1, pp. 57–60.
Gorchakovskii, P.L. and Shiyatov, S.G., Phytoindication of Environmental Conditions and Natural Processes in High Mountains, Moscow: Nauka, 1985 [in Russian].
Agatova, A.R., Nepop, R.K., Barinov, V.V., Nazarov, A.N., and Myglan, V.S., A New Aspect of Application of Dendrological Analysis for Dating Strong Earthquakes of the Past: A Case Study of the Altai Mountains, Doklady Earth Sci., 2014, vol. 455, issue 1, pp. 243–245.
Paleoseismology, J.P. McCalpin, Ed., 2nd Ed., San Diego: Elsevier Science Publishing Co. Inc., 2009.
Antipin, V.S., Voronin, V.I., and Fedorov, A.M., The Patom Crater in Eastern Siberia, Priroda, 2008, no. 9, pp. 69–75 [in Russian].
Antipin, V.S., Pokrovsky, B.G., and Fedorov, A.M., Formation of the Patom Crater by Phreatic Explosion: Geological and Isotope-Geochemical Evidence, Lithol. Miner. Resour., 2015, vol. 50, issue 6, pp. 478–487.
Antipin, V.S., Dmitriev, A.G., Yazev, S.A., and Voronin, V.I., The Patom Crater in Eastern Siberia: History of Study and Results of Recent Comprehensive Investigations, Abstracts Int. Conf. “!00 Years Since Tunguska Phenomenon: Past, Present, Future” (June 26–28, 2008, Moscow), Moscow: Izd. Inst. Dinamiki Geosfer RAN, 2008, p. 163 [in Russian].
Vaganov, E.A., Naurzbaev, M.M., and Eger’, I.V., The Ultimate Age of Larch Trees in Siberia, Lesovedenie, 1999, no. 6, pp. 65–75 [in Russian].
Ruzhich, V.V., San’kov, V.A., and Dneprovskii, Yu.I., Dendrochronological Dating of Seismogenic Faults in the Stanovoi Highlands, Geolog. Geofiz., 1982, no. 8, pp. 62–69 [in Russian].
Smiley, T.L., The Geology and Dating of Sunset Crater, Flagstaff, Arizona: New Mexico Geological Society, Ninth Field Conference Guidebook, Socorro, 1958, pp. 186–190.
Eggler, W.A., Plant Communities in the Vicinity of the Volcano El Paricutin, Mexico, After Two and a Half Years of Eruption, Ecology, 1948, vol. 29, issue 4, pp. 415–436.
Vaganov, E.A., Grachev, A.M., Shishov, V.V., Panyushkina, I.P., Leavitt, S.W., Knorre, E.P., Chebykin, E.P., and Menyalo, O.V., Elemental Composition of Tree Rings: A New Perspective in Biogeochemistry, Doklady Biol. Sci., vol. 453, issue 6, pp. 375–379.
Rikhvanov, L.P., Arkhangel’skaya, T.A., and Zamyatina, Yu.L., Dendroradiography as a Method of Retrospective Assessment of the Radioecological Situation, Tomsk: Del’taplan, 2015 [in Russian].
Wedepohl, K.H., Primäre und diagenetische Strontiumgehalte von Karbonatgesteinen, Ber. dtsch. Ges. geol. Wiss., 1969, R. B. Min. Lagerstättenforsch., Bd. 14, Hft. I, pp. 17–23.
Antipin, V.S., Fedorov, A.M., Dril’, S.I., and Voronin, V.I., The New Data on the Origin of the Patom Crater (East Siberia), Doklady Earth Sci., 2011, vol. 440, part 2, pp. 1391–1395.
Author information
Authors and Affiliations
Corresponding authors
Additional information
Translated by V.B.Sochava Institute of Geography SB RAS
Rights and permissions
About this article
Cite this article
Voronin, V.I., Antipin, V.S., Oskolkov, V.A. et al. The Age of the Patom Crater: Dendrochronological and Biogeochemical Investigations. Geogr. Nat. Resour. 41, 390–398 (2020). https://doi.org/10.1134/S1875372841040101
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1134/S1875372841040101