Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai Mountains

For the Altai Mountains’ region, especially the arid southeastern part of the Russian Altai, the data on glacier fluctuations in the Pleistocene and Holocene are still inconsistent. The study area was the Kargy River’s valley (2288–2387 m a.s.l.), a location that is not currently affected by glaciat...

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Main Authors: Dmitrii A. Ganyushkin, Sofia N. Lessovaia, Dmitrii Y. Vlasov, Gennady P. Kopitsa, László Almásy, Kirill V. Chistyakov, Elena G. Panova, Ekaterina Derkach, Anastasiya Alekseeva
Format: Article
Language:English
Published: MDPI AG 2021-08-01
Series:Geosciences
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Online Access:https://www.mdpi.com/2076-3263/11/8/342
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spelling doaj-060c9d7af52947e3a7e934696ba1f3bc2021-08-26T13:47:27ZengMDPI AGGeosciences2076-32632021-08-011134234210.3390/geosciences11080342Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai MountainsDmitrii A. Ganyushkin0Sofia N. Lessovaia1Dmitrii Y. Vlasov2Gennady P. Kopitsa3László Almásy4Kirill V. Chistyakov5Elena G. Panova6Ekaterina Derkach7Anastasiya Alekseeva8Institute of Earth Sciences, St. Petersburg State University, Universitetskaya nab., d. 7/9, 199034 St. Petersburg, RussiaInstitute of Earth Sciences, St. Petersburg State University, Universitetskaya nab., d. 7/9, 199034 St. Petersburg, RussiaBiological Faculty, St. Petersburg State University, Universitetskaya nab., d. 7/9, 199034 St. Petersburg, RussiaB.P. Konstantinov Petersburg Nuclear Physics Institute NRC KI, Orlova roshcha, d. 1, 188300 Gatchina, RussiaCentre for Energy Research, Institute for Energy Security and Environmental Safety, Konkoly-Thege ut. 29–33, 1121 Budapest, HungaryInstitute of Earth Sciences, St. Petersburg State University, Universitetskaya nab., d. 7/9, 199034 St. Petersburg, RussiaInstitute of Earth Sciences, St. Petersburg State University, Universitetskaya nab., d. 7/9, 199034 St. Petersburg, RussiaInstitute of Earth Sciences, St. Petersburg State University, Universitetskaya nab., d. 7/9, 199034 St. Petersburg, RussiaInstitute of Earth Sciences, St. Petersburg State University, Universitetskaya nab., d. 7/9, 199034 St. Petersburg, RussiaFor the Altai Mountains’ region, especially the arid southeastern part of the Russian Altai, the data on glacier fluctuations in the Pleistocene and Holocene are still inconsistent. The study area was the Kargy River’s valley (2288–2387 m a.s.l.), a location that is not currently affected by glaciation and the glacial history of which is poorly studied. Field observations and geomorphological mapping were used to reveal the configuration of Pleistocene moraines. The relative dating method was applied to define the degree of weathering as an indicator of age. Three moraine groups of different ages (presumably MIS 6, MIS 4, and MIS 2) were identified based on a detailed investigation of their morphological features and the use of relative dating approaches. The latter were primarily based on weathering patterns. Data on the rock mineralogy, porosity, and specificity of biological colonization as an agent of weathering were obtained for the moraine debris. The studied moraines were composed of fine-grained schist, in which the specific surface area and fractality (self-similarity) were more developed in the older moraine. The growth of biota (crustose lichen and micromycetes) colonizing the rock surface led to rock disintegration and the accumulation of autochthonous fragments on the rock surface. Despite the fact that the initial stage(s) of moraine weathering affected by biota was fixed, the correlation trends of biota activity and moraine ages were not determined.https://www.mdpi.com/2076-3263/11/8/342biota colonizationweatheringrock porosityPleistocene morainesmoraine relative dating
collection DOAJ
language English
format Article
sources DOAJ
author Dmitrii A. Ganyushkin
Sofia N. Lessovaia
Dmitrii Y. Vlasov
Gennady P. Kopitsa
László Almásy
Kirill V. Chistyakov
Elena G. Panova
Ekaterina Derkach
Anastasiya Alekseeva
spellingShingle Dmitrii A. Ganyushkin
Sofia N. Lessovaia
Dmitrii Y. Vlasov
Gennady P. Kopitsa
László Almásy
Kirill V. Chistyakov
Elena G. Panova
Ekaterina Derkach
Anastasiya Alekseeva
Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai Mountains
Geosciences
biota colonization
weathering
rock porosity
Pleistocene moraines
moraine relative dating
author_facet Dmitrii A. Ganyushkin
Sofia N. Lessovaia
Dmitrii Y. Vlasov
Gennady P. Kopitsa
László Almásy
Kirill V. Chistyakov
Elena G. Panova
Ekaterina Derkach
Anastasiya Alekseeva
author_sort Dmitrii A. Ganyushkin
title Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai Mountains
title_short Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai Mountains
title_full Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai Mountains
title_fullStr Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai Mountains
title_full_unstemmed Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai Mountains
title_sort application of rock weathering and colonization by biota for the relative dating of moraines from the arid part of the russian altai mountains
publisher MDPI AG
series Geosciences
issn 2076-3263
publishDate 2021-08-01
description For the Altai Mountains’ region, especially the arid southeastern part of the Russian Altai, the data on glacier fluctuations in the Pleistocene and Holocene are still inconsistent. The study area was the Kargy River’s valley (2288–2387 m a.s.l.), a location that is not currently affected by glaciation and the glacial history of which is poorly studied. Field observations and geomorphological mapping were used to reveal the configuration of Pleistocene moraines. The relative dating method was applied to define the degree of weathering as an indicator of age. Three moraine groups of different ages (presumably MIS 6, MIS 4, and MIS 2) were identified based on a detailed investigation of their morphological features and the use of relative dating approaches. The latter were primarily based on weathering patterns. Data on the rock mineralogy, porosity, and specificity of biological colonization as an agent of weathering were obtained for the moraine debris. The studied moraines were composed of fine-grained schist, in which the specific surface area and fractality (self-similarity) were more developed in the older moraine. The growth of biota (crustose lichen and micromycetes) colonizing the rock surface led to rock disintegration and the accumulation of autochthonous fragments on the rock surface. Despite the fact that the initial stage(s) of moraine weathering affected by biota was fixed, the correlation trends of biota activity and moraine ages were not determined.
topic biota colonization
weathering
rock porosity
Pleistocene moraines
moraine relative dating
url https://www.mdpi.com/2076-3263/11/8/342
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