Please use this identifier to cite or link to this item: http://elar.urfu.ru/handle/10995/130686
Title: Potentiality of Charcoal as a Dendrochronological and Paleoclimatic Archive: Case Study of Archaeological Charcoal from Southeastern Altai, Russia
Authors: Agatova, A.
Nepop, R.
Myglan, V.
Barinov, V.
Tainik, A.
Filatova, M.
Issue Date: 2023
Publisher: Multidisciplinary Digital Publishing Institute (MDPI)
Citation: Agatova, A, Nepop, R, Myglan, V, Barinov, V, Tainik, A & Filatova, M 2023, 'Potentiality of Charcoal as a Dendrochronological and Paleoclimatic Archive: Case Study of Archaeological Charcoal from Southeastern Altai, Russia', Climate, Том. 11, № 7, 150. https://doi.org/10.3390/cli11070150
Agatova, A., Nepop, R., Myglan, V., Barinov, V., Tainik, A., & Filatova, M. (2023). Potentiality of Charcoal as a Dendrochronological and Paleoclimatic Archive: Case Study of Archaeological Charcoal from Southeastern Altai, Russia. Climate, 11(7), [150]. https://doi.org/10.3390/cli11070150
Abstract: Archaeological charcoal from ancient nomad iron-smelting furnaces collected in the highland southeastern Russian Altai has great potential as a material for tree ring analysis. Dendrochronological dating was applied to 355 viable samples (>80% of the 448 collected ones), prepared using a new protocol. Individual tree ring series of 155 (~43%) samples were used to construct nine floating chronologies from 76 to 290 rings long. The archaeological and radiocarbon data on charcoal that fueled the hearths of the Kosh-Agach type bracket the floating tree ring chronologies between the second and tenth centuries AD. The results demonstrate that long tree ring “steppe” chronologies can be obtained for intermontane basins in the arid zone of Southern Siberia, using the analysis of charcoal samples. A strong climate signal imprinted in the annual growth of trees allowed for crossdating samples with relatively few rings. The revealed common climate signal for larches from different locations indicates similar paleoclimate conditions of their growth despite the strong modern southeastward aridization trend in the region, which was not so pronounced ca. 1.5 ka ago. The further matching of these chronologies to the calendar timeline will provide reference for the precise comparison of climatic conditions in the floors of intermontane basins and in the flanking mountains. © 2023 by the authors.
Keywords: ARCHAEOLOGICAL CHARCOAL
DENDROCHRONOLOGY
IRON-SMELTING FURNACE
LONG TREE RING CHRONOLOGY
RUSSIAN ALTAI
URI: http://elar.urfu.ru/handle/10995/130686
Access: info:eu-repo/semantics/openAccess
cc-by
License text: https://creativecommons.org/licenses/by/4.0/
SCOPUS ID: 85166402905
WOS ID: 001035180700001
PURE ID: 43280979
ISSN: 2225-1154
DOI: 10.3390/cli11070150
metadata.dc.description.sponsorship: Russian Science Foundation, RSF
The study was supported by grant 22-27-00454 from the Russian Science Foundation.
RSCF project card: 22-27-00454
Appears in Collections:Научные публикации ученых УрФУ, проиндексированные в SCOPUS и WoS CC

Files in This Item:
File Description SizeFormat 
2-s2.0-85166402905.pdf3,6 MBAdobe PDFView/Open


This item is licensed under a Creative Commons License Creative Commons