Archaeological Sites as Markers of Neopleistocene-Holocene Hydrological System Transformation in the Kurai and Chuya Basins, Southeastern Altai: Results of Geomorphological and Geoarchaeological Studies
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http://www.archaeology.nsc.ru/journarticleru/68/1026https://elib.sfu-kras.ru/handle/2311/70098
Автор:
Agatova, A. R.
Nepop, R. K.
Slyusarenko, I. Y.
Myglan, V. S.
Barinov, V. V.
Коллективный автор:
Гуманитарный институт
Научно-исследовательская часть
Междисциплинарная научно-исследовательская лаборатория "Естественно-научные методы в археологии и истории"
Дата:
2016-12Журнал:
ARCHAEOLOGY ETHNOLOGY AND ANTHROPOLOGY OF EURASIAКвартиль журнала в Scopus:
Q2Квартиль журнала в Web of Science:
без квартиляБиблиографическое описание:
Agatova, A. R. Archaeological Sites as Markers of Neopleistocene-Holocene Hydrological System Transformation in the Kurai and Chuya Basins, Southeastern Altai: Results of Geomorphological and Geoarchaeological Studies [Текст] / A. R. Agatova, R. K. Nepop, I. Y. Slyusarenko, V. S. Myglan, V. V. Barinov // ARCHAEOLOGY ETHNOLOGY AND ANTHROPOLOGY OF EURASIA. — 2016. — Т. 44 (№ 4). — С. 26-34Аннотация:
Multidisciplinary studies using geomorphological, geoarchaeological, and geochronological approaches indicate
contrasting environmental changes in Southeastern Altai, beginning in the Late Pleistocene. 29 new radiocarbon
dates from the subaerial complex overlying Late Neopleistocene sediments in the high-altitude Kurai and Chuya
basins confi rm the degradation of a single ice-dammed reservoir in that area before the Early Holocene. In the fi rst
half of the Holocene, those basins were fi lled with isolated lakes. At the mouth of the Baratal River in the western
Kurai basin, a reservoir with a water-level of at least 1480 m a.s.l. emerged ca 10–6.5 ka cal BP; whereas in the
Chuya depression, numerous residual lakes existed at least 8 ka cal BP. Landslide- and moraine-dammed lakes
between the depressions in the Chuya River valley existed until 7–3 ka cal BP, when they drained away. The state
of preservation of in situ archaeological sites, their cultural affi liation, and their locations within the depressions
and along the main Chuya valley attest to spatial and temporal changes in the hydrological system. This evolution
in the second half of the Holocene did not entail major consequences for humans. All cataclysmic fl ood events took
place (occurred) before 10–8 ka cal BP.
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