Chronological data from Estonian Pleistocene

V. Kalm
{"title":"Chronological data from Estonian Pleistocene","authors":"V. Kalm","doi":"10.3176/geol.2005.1.02","DOIUrl":null,"url":null,"abstract":". Pleistocene chronostratigraphy in Estonia is based on 60 radiocarbon ( 14 C, 14 C AMS), 63 TL/OSL, and 17 10 Be datings from 57 studied sites/sections that cover a time span from approximately 200 000 yr BP to the Pleistocene–Holocene chronostratigraphic boundary. For the first time all scattered data from 40 years of chronological study into Estonian Pleistocene are presented together and critically analysed in regard to validity of obtained ages. Half of the relatively abundant but scattered chronological data cover only the youngest 5000–6000 year part of the Late Weichselian. New OSL datings, together with the results of earlier palynological, carpological, and diatom studies, have invalidated almost one-third of the available 14 C dates, obtained mostly in the late 1960s and 1970s. Thermoluminescence ages from tills, available from the early 1980s, are very inconsistent within the studied sections and are considered to be unreliable because of questionable bleaching of the TL signal. The results of the 10 Be method, recently applied to the study of deglaciation chronology of the Estonian territory, do not contradict the earlier age estimations. However, due to relatively large uncertainties of the method, the results were not able to refine the existing Late-Glacial chronology in Estonia.","PeriodicalId":237994,"journal":{"name":"Proceedings of the Estonian Academy of Sciences. Geology","volume":"2 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings of the Estonian Academy of Sciences. Geology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3176/geol.2005.1.02","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 3

Abstract

. Pleistocene chronostratigraphy in Estonia is based on 60 radiocarbon ( 14 C, 14 C AMS), 63 TL/OSL, and 17 10 Be datings from 57 studied sites/sections that cover a time span from approximately 200 000 yr BP to the Pleistocene–Holocene chronostratigraphic boundary. For the first time all scattered data from 40 years of chronological study into Estonian Pleistocene are presented together and critically analysed in regard to validity of obtained ages. Half of the relatively abundant but scattered chronological data cover only the youngest 5000–6000 year part of the Late Weichselian. New OSL datings, together with the results of earlier palynological, carpological, and diatom studies, have invalidated almost one-third of the available 14 C dates, obtained mostly in the late 1960s and 1970s. Thermoluminescence ages from tills, available from the early 1980s, are very inconsistent within the studied sections and are considered to be unreliable because of questionable bleaching of the TL signal. The results of the 10 Be method, recently applied to the study of deglaciation chronology of the Estonian territory, do not contradict the earlier age estimations. However, due to relatively large uncertainties of the method, the results were not able to refine the existing Late-Glacial chronology in Estonia.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
爱沙尼亚更新世的年代资料
. 爱沙尼亚的更新世年代地层是基于57个研究地点/剖面的60个放射性碳(14c, 14c AMS), 63个TL/OSL和17个10be定年,涵盖了从大约20万年BP到更新世-全新世年代地层界线的时间跨度。对爱沙尼亚更新世进行了40年的年代学研究,首次将所有分散的数据放在一起,并对所得年龄的有效性进行了严格的分析。在相对丰富但分散的年代学资料中,有一半只涵盖了晚期魏奇塞利世最年轻的5000-6000年部分。新的OSL年代测定,加上早期孢粉学、湖泊学和硅藻研究的结果,已经使几乎三分之一的现有14c年代无效,这些年代大多是在20世纪60年代末和70年代获得的。从20世纪80年代初获得的tills热释光年龄在研究剖面中非常不一致,并且由于TL信号的可疑漂白而被认为是不可靠的。最近应用于爱沙尼亚领土消冰年表研究的10 Be方法的结果与早先的年龄估计并不矛盾。然而,由于该方法的不确定性相对较大,结果无法完善爱沙尼亚现有的晚冰期年表。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
Hydrogeological model of Estonia and its applications CHITINOZOAN BIOFACIES OF LATE EARLY LLANDOVERY (CORONOGRAPTUS CYPHUS) AGE IN THE EAST BALTIC WENLOCKIAN AND LUDLOVIAN SEDIMENTARY AND BIOTIC EVENTS IN THE MIDWESTERN CRATONIC AREA, U.S.A. PRELIMINARY RESULTS AND INTERPRETATIONS OF MINERAL MAGNETIC ANALYSES OF A HOLOCENE SEDIMENT SUCCESSION FROM LAKE MAARDU NEAR TALLINN, ESTONIA РАДОНОВЫЙ ФАКТОР РАДИАЦИОННОГО ФОНА В НАСЕЛЕННЫХ ПУНКТАХ СЕВЕРНОЙ ЭСТОНИИ (ЭКОГЕОЛОГИЧЕСКИЙ АСПЕКТ)
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1