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...
Main Authors: | , , , , , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2021-08-01
|
Series: | Geosciences |
Subjects: | |
Online Access: | https://www.mdpi.com/2076-3263/11/8/342 |
id |
doaj-060c9d7af52947e3a7e934696ba1f3bc |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT dmitriiaganyushkin applicationofrockweatheringandcolonizationbybiotafortherelativedatingofmorainesfromthearidpartoftherussianaltaimountains AT sofianlessovaia applicationofrockweatheringandcolonizationbybiotafortherelativedatingofmorainesfromthearidpartoftherussianaltaimountains AT dmitriiyvlasov applicationofrockweatheringandcolonizationbybiotafortherelativedatingofmorainesfromthearidpartoftherussianaltaimountains AT gennadypkopitsa applicationofrockweatheringandcolonizationbybiotafortherelativedatingofmorainesfromthearidpartoftherussianaltaimountains AT laszloalmasy applicationofrockweatheringandcolonizationbybiotafortherelativedatingofmorainesfromthearidpartoftherussianaltaimountains AT kirillvchistyakov applicationofrockweatheringandcolonizationbybiotafortherelativedatingofmorainesfromthearidpartoftherussianaltaimountains AT elenagpanova applicationofrockweatheringandcolonizationbybiotafortherelativedatingofmorainesfromthearidpartoftherussianaltaimountains AT ekaterinaderkach applicationofrockweatheringandcolonizationbybiotafortherelativedatingofmorainesfromthearidpartoftherussianaltaimountains AT anastasiyaalekseeva applicationofrockweatheringandcolonizationbybiotafortherelativedatingofmorainesfromthearidpartoftherussianaltaimountains |
_version_ |
1721193109472149504 |