Please use this identifier to cite or link to this item: http://hdl.handle.net/10995/111693
Title: Archaeological Sites as Markers of Hydrosystem Transformation in the Kurai and Chuya Basins, Southeastern Altai, in the Late Pleistocene and Holocene. Summary of Findings and Paleogeographic Reconstructions
Authors: Agatova, A. R.
Nepop, R. K.
Slyusarenko, I. Y.
Issue Date: 2017
Publisher: Institute of Archaeology and Enthnography of the Siberian Branch of The Russian Academy of Sciences
Institute of Archaeology and Ethnography SB RAS
Citation: Agatova A. R. Archaeological Sites as Markers of Hydrosystem Transformation in the Kurai and Chuya Basins, Southeastern Altai, in the Late Pleistocene and Holocene. Summary of Findings and Paleogeographic Reconstructions / A. R. Agatova, R. K. Nepop, I. Y. Slyusarenko // Archaeology, Ethnology and Anthropology of Eurasia. — 2017. — Vol. 45. — Iss. 1. — P. 25-35.
Abstract: This paper is the second in a series of publications on various aspects of the relationships between man and environment in the highlands of southeastern Altai. In these studies, we assess the impact of climatic changes (evidenced by processes of glaciation and deglaciation, the emergence of ice-dammed and residual lakes, soil and peat formation, and seismic activity) on the succession of sedentary and nomadic cultures, and on the ranges of their distribution, in the Late Pleistocene and Holocene. Geochronological data on the evolution of Late Pleistocene ice-dammed lakes and Holocene residual lacustrine systems within the Kurai and Chuya intermountain basins, including our new findings based on geomorphological, geoarchaeological, and geochronological approaches, were summarized in the first paper of the series. Using Paleolithic sites for assessing the time in the Late Pleistocene when the Chuya paleolake emptied is unwarranted, because their estimated age limits are wide, many are likely redeposited, and most finds are random. However, analysis of the spatial distribution of in situ sites spanning the period from the Late Bronze Age to the Middle Ages has provided evidence regarding the transformation of Holocene hydrosystems. New radiocarbon dates indicate a substantial decrease of the Sartan glaciation before 14 ka cal BP, and desiccation of the last ice-dammed lakes within the Kurai and Chuya basins before 10 ka cal BP. The absence of Early Holocene archaeological sites in those areas may be due to the wide distribution of residual lakes in the bottoms of those depressions at that time. © 2017 A.R. Agatova, R.K. Nepop, I.Y. Slyusarenko.
Keywords: ARCHAEOLOGICAL SITES
HOLOCENE
HYDROSYSTEM TRANSFORMATION
ICE-DAMMED LAKES
INTERMOUNTAIN DEPRESSIONS
LATE PALEOLITHIC
LATE PLEISTOCENE
RADIOCARBON DATING
SOUTHEASTERN ALTAI
URI: http://hdl.handle.net/10995/111693
Access: info:eu-repo/semantics/openAccess
SCOPUS ID: 85112275343
PURE ID: 1988065
ISSN: 1563-0110
metadata.dc.description.sponsorship: Geomorphological studies, including radiocarbon dating, were performed under Public Contract (Project No. 0330-2016-0015) and supported by the Russian Foundation for Basic Research (Projects No. 15-05-06028 and 16-05-01035); archaeological studies were supported by the Russian Science Foundation (Project No. 14-50-00036).
Appears in Collections:Научные публикации, проиндексированные в SCOPUS и WoS CC

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