Loading…

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...

Full description

Saved in:
Bibliographic Details
Published in:Doklady earth sciences 2021, Vol.499 (2), p.639-642
Main Authors: Shvarev, S. V., Zaretskaya, N. E., Ruchkin, M. V., Lugovoi, N. N., Zazovskaya, E. P., Subetto, D. A.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by
cites cdi_FETCH-LOGICAL-c1138-41a5d2b1679f5145745b042be774d9e7c50bd9dfca65c1cf1cf05e16eaaa75253
container_end_page 642
container_issue 2
container_start_page 639
container_title Doklady earth sciences
container_volume 499
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
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2570142767</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2570142767</sourcerecordid><originalsourceid>FETCH-LOGICAL-c1138-41a5d2b1679f5145745b042be774d9e7c50bd9dfca65c1cf1cf05e16eaaa75253</originalsourceid><addsrcrecordid>eNp1UE1Lw0AQXUTBWv0B3ha86CG6s9nJJkdJ_cJChSiolzBJNjUlTepucvDfu6WCBxEG5sF7bz4eY6cgLgFCdZWBkHEYqlcJIhaA8R6bAIYQxCGqfY89HWz5Q3bk3EoIpRQmE_ae2t65YJHNOXUVB5XyGQ1Nt-R9zd_60YNsLMjYhlo-M5veNYPjTceHD8MzWhcN8fNHapvOeyxVF_zJeOjGlo7ZQU2tMyc_fcpebm-e0_tgvrh7SK_nQekvjwMFhJUsINJJjaBQKyyEkoXRWlWJ0SWKokqquqQISyhrXwINRIaINEoMp-xsN3dj-8_RuCFf9aPt_MpcohagpI60V8FOVW4ftqbON7ZZk_3KQeTbCPM_EXqP3Hmc13ZLY38n_2_6BpSacRI</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2570142767</pqid></control><display><type>article</type><title>Cross-OSL and 14C Dating of Young Subaerial Deposits in the Sambia (Kaliningrad) Peninsula</title><source>Springer Nature</source><creator>Shvarev, S. V. ; Zaretskaya, N. E. ; Ruchkin, M. V. ; Lugovoi, N. N. ; Zazovskaya, E. P. ; Subetto, D. A.</creator><creatorcontrib>Shvarev, S. V. ; Zaretskaya, N. E. ; Ruchkin, M. V. ; Lugovoi, N. N. ; Zazovskaya, E. P. ; Subetto, D. A.</creatorcontrib><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.</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. Russian Text © The Author(s), 2021, published in Doklady Rossiiskoi Akademii Nauk. Nauki o Zemle, 2021, Vol. 499, No. 2, pp. 133–137.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c1138-41a5d2b1679f5145745b042be774d9e7c50bd9dfca65c1cf1cf05e16eaaa75253</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Shvarev, S. V.</creatorcontrib><creatorcontrib>Zaretskaya, N. E.</creatorcontrib><creatorcontrib>Ruchkin, M. V.</creatorcontrib><creatorcontrib>Lugovoi, N. N.</creatorcontrib><creatorcontrib>Zazovskaya, E. P.</creatorcontrib><creatorcontrib>Subetto, D. A.</creatorcontrib><title>Cross-OSL and 14C Dating of Young Subaerial Deposits in the Sambia (Kaliningrad) Peninsula</title><title>Doklady earth sciences</title><addtitle>Dokl. Earth Sc</addtitle><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.</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. V.</creator><creator>Zaretskaya, N. E.</creator><creator>Ruchkin, M. V.</creator><creator>Lugovoi, N. N.</creator><creator>Zazovskaya, E. P.</creator><creator>Subetto, D. A.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>2021</creationdate><title>Cross-OSL and 14C Dating of Young Subaerial Deposits in the Sambia (Kaliningrad) Peninsula</title><author>Shvarev, S. V. ; Zaretskaya, N. E. ; Ruchkin, M. V. ; Lugovoi, N. N. ; Zazovskaya, E. P. ; Subetto, D. A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c1138-41a5d2b1679f5145745b042be774d9e7c50bd9dfca65c1cf1cf05e16eaaa75253</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Carbon 14</topic><topic>Climate change</topic><topic>Dating</topic><topic>Deposits</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Glacial deposits</topic><topic>Glaciation</topic><topic>Glaciology</topic><topic>Holocene</topic><topic>Ice ages</topic><topic>Lithology</topic><topic>Little Ice Age</topic><topic>Quaternary</topic><topic>Quaternary deposits</topic><topic>Radiocarbon dating</topic><topic>Sequences</topic><topic>Stratigraphy</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Shvarev, S. V.</creatorcontrib><creatorcontrib>Zaretskaya, N. E.</creatorcontrib><creatorcontrib>Ruchkin, M. V.</creatorcontrib><creatorcontrib>Lugovoi, N. N.</creatorcontrib><creatorcontrib>Zazovskaya, E. P.</creatorcontrib><creatorcontrib>Subetto, D. A.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>Doklady earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Shvarev, S. V.</au><au>Zaretskaya, N. E.</au><au>Ruchkin, M. V.</au><au>Lugovoi, N. N.</au><au>Zazovskaya, E. P.</au><au>Subetto, D. A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Cross-OSL and 14C Dating of Young Subaerial Deposits in the Sambia (Kaliningrad) Peninsula</atitle><jtitle>Doklady earth sciences</jtitle><stitle>Dokl. Earth Sc</stitle><date>2021</date><risdate>2021</risdate><volume>499</volume><issue>2</issue><spage>639</spage><epage>642</epage><pages>639-642</pages><issn>1028-334X</issn><eissn>1531-8354</eissn><abstract>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.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1028334X21080158</doi><tpages>4</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1028-334X
ispartof Doklady earth sciences, 2021, Vol.499 (2), p.639-642
issn 1028-334X
1531-8354
language eng
recordid cdi_proquest_journals_2570142767
source Springer Nature
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
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-02T16%3A20%3A24IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Cross-OSL%20and%2014C%20Dating%20of%20Young%20Subaerial%20Deposits%20in%20the%20Sambia%20(Kaliningrad)%20Peninsula&rft.jtitle=Doklady%20earth%20sciences&rft.au=Shvarev,%20S.%20V.&rft.date=2021&rft.volume=499&rft.issue=2&rft.spage=639&rft.epage=642&rft.pages=639-642&rft.issn=1028-334X&rft.eissn=1531-8354&rft_id=info:doi/10.1134/S1028334X21080158&rft_dat=%3Cproquest_cross%3E2570142767%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c1138-41a5d2b1679f5145745b042be774d9e7c50bd9dfca65c1cf1cf05e16eaaa75253%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2570142767&rft_id=info:pmid/&rfr_iscdi=true