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Cross-OSL and 14C Dating of Young Subaerial Deposits in the Sambia (Kaliningrad) Peninsula
The cross-instrumental dating of the Quaternary deposits in the Sambia (Kaliningrad) Peninsula has made it possible to obtain a time series that indicates the formation of a sequence overlapping the Last Glaciation deposits in the Late Holocene under subaerial conditions with active aeolian accumula...
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Published in: | Doklady earth sciences 2021, Vol.499 (2), p.639-642 |
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container_title | Doklady earth sciences |
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creator | Shvarev, S. V. Zaretskaya, N. E. Ruchkin, M. V. Lugovoi, N. N. Zazovskaya, E. P. Subetto, D. A. |
description | The cross-instrumental dating of the Quaternary deposits in the Sambia (Kaliningrad) Peninsula has made it possible to obtain a time series that indicates the formation of a sequence overlapping the Last Glaciation deposits in the Late Holocene under subaerial conditions with active aeolian accumulation starting from 450–400 BP. The earlier established fluvioglacial genesis and Late Glacial age of the surface deposits need to be revised. Greater aeolian activity is presumably related to climate changes during the Little Ice Age. OSL dating of very young (Late Holocene) subaerial deposits demonstrates the reliable results supported by agreement with the radiocarbon analysis data and the stratigraphic position of the dated sequences. |
doi_str_mv | 10.1134/S1028334X21080158 |
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OSL dating of very young (Late Holocene) subaerial deposits demonstrates the reliable results supported by agreement with the radiocarbon analysis data and the stratigraphic position of the dated sequences.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X21080158</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Carbon 14 ; Climate change ; Dating ; Deposits ; Earth and Environmental Science ; Earth Sciences ; Glacial deposits ; Glaciation ; Glaciology ; Holocene ; Ice ages ; Lithology ; Little Ice Age ; Quaternary ; Quaternary deposits ; Radiocarbon dating ; Sequences ; Stratigraphy</subject><ispartof>Doklady earth sciences, 2021, Vol.499 (2), p.639-642</ispartof><rights>Pleiades Publishing, Ltd. 2021. ISSN 1028-334X, Doklady Earth Sciences, 2021, Vol. 499, Part 2, pp. 639–642. © Pleiades Publishing, Ltd., 2021. 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OSL dating of very young (Late Holocene) subaerial deposits demonstrates the reliable results supported by agreement with the radiocarbon analysis data and the stratigraphic position of the dated sequences.</description><subject>Carbon 14</subject><subject>Climate change</subject><subject>Dating</subject><subject>Deposits</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Glacial deposits</subject><subject>Glaciation</subject><subject>Glaciology</subject><subject>Holocene</subject><subject>Ice ages</subject><subject>Lithology</subject><subject>Little Ice Age</subject><subject>Quaternary</subject><subject>Quaternary deposits</subject><subject>Radiocarbon dating</subject><subject>Sequences</subject><subject>Stratigraphy</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp1UE1Lw0AQXUTBWv0B3ha86CG6s9nJJkdJ_cJChSiolzBJNjUlTepucvDfu6WCBxEG5sF7bz4eY6cgLgFCdZWBkHEYqlcJIhaA8R6bAIYQxCGqfY89HWz5Q3bk3EoIpRQmE_ae2t65YJHNOXUVB5XyGQ1Nt-R9zd_60YNsLMjYhlo-M5veNYPjTceHD8MzWhcN8fNHapvOeyxVF_zJeOjGlo7ZQU2tMyc_fcpebm-e0_tgvrh7SK_nQekvjwMFhJUsINJJjaBQKyyEkoXRWlWJ0SWKokqquqQISyhrXwINRIaINEoMp-xsN3dj-8_RuCFf9aPt_MpcohagpI60V8FOVW4ftqbON7ZZk_3KQeTbCPM_EXqP3Hmc13ZLY38n_2_6BpSacRI</recordid><startdate>2021</startdate><enddate>2021</enddate><creator>Shvarev, S. 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subjects | Carbon 14 Climate change Dating Deposits Earth and Environmental Science Earth Sciences Glacial deposits Glaciation Glaciology Holocene Ice ages Lithology Little Ice Age Quaternary Quaternary deposits Radiocarbon dating Sequences Stratigraphy |
title | Cross-OSL and 14C Dating of Young Subaerial Deposits in the Sambia (Kaliningrad) Peninsula |
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