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Название: Potentiality of Charcoal as a Dendrochronological and Paleoclimatic Archive: Case Study of Archaeological Charcoal from Southeastern Altai, Russia
Авторы: Agatova, A.
Nepop, R.
Myglan, V.
Barinov, V.
Tainik, A.
Filatova, M.
Дата публикации: 2023
Издатель: Multidisciplinary Digital Publishing Institute (MDPI)
Библиографическое описание: 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
Аннотация: 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.
Ключевые слова: ARCHAEOLOGICAL CHARCOAL
DENDROCHRONOLOGY
IRON-SMELTING FURNACE
LONG TREE RING CHRONOLOGY
RUSSIAN ALTAI
URI: http://elar.urfu.ru/handle/10995/130686
Условия доступа: info:eu-repo/semantics/openAccess
cc-by
Текст лицензии: https://creativecommons.org/licenses/by/4.0/
Идентификатор SCOPUS: 85166402905
Идентификатор WOS: 001035180700001
Идентификатор PURE: 43280979
ISSN: 2225-1154
DOI: 10.3390/cli11070150
Сведения о поддержке: Russian Science Foundation, RSF
The study was supported by grant 22-27-00454 from the Russian Science Foundation.
Карточка проекта РНФ: 22-27-00454
Располагается в коллекциях:Научные публикации ученых УрФУ, проиндексированные в SCOPUS и WoS CC

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