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dc.contributor.authorGoslar, Tomasz
dc.contributor.authorKuc, Tadeusz
dc.contributor.authorPazdur, Mieczysław F.
dc.contributor.authorRalska-Jasiewiczowa, Magdalena
dc.contributor.authorRóżański, Kazimierz
dc.contributor.authorSzeroczynska, Krystyna
dc.contributor.authorWalanus, Adam
dc.contributor.authorWicik, Bogumił
dc.contributor.authorWięckowski, Kazimierz
dc.contributor.authorArnold, Maurice
dc.contributor.authorBard, Eduard
dc.date.accessioned2021-02-11T20:33:24Z
dc.date.available2021-02-11T20:33:24Z
dc.date.issued1992-01-01
dc.identifier.citationGoslar, T., Kuc, T., Pazdur, M. F., Ralska-Jasiewiczowa, M., Różański, K., Szeroczyńska, K., ... & Bard, E. (1992). Possibilities for reconstructing radiocarbon level changes during the late Glacial by using a laminated sequence of Goścíaż Lake. Radiocarbon, 34(3), 826-832.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200064134
dc.identifier.urihttp://hdl.handle.net/10150/653360
dc.descriptionFrom the 14th International Radiocarbon Conference held in Tucson, AZ, May 20-24, 1991.
dc.description.abstractLaminated sediments of Gościąż Lake can be used as an independent source of material for calibrating the radiocarbon time scale. The varve chronology is based on three long cores from the deepest part of the lake, with one additional core from the second deepest part. From pollen and Cladocera spectra and stable isotope and chemical content sequences, we have determined the Allerød(AL)/Younger Dryas(YD) and Younger Dryas/Preboreal(PB) boundaries in the three long cores with relatively good accuracy, and have tentatively defined the AL/YD boundary in the fourth core. The Younger Dryas period contains at least 1520 varves, with 980 varves in fragments well replicated in all four cores. The duration of the Younger Dryas as recorded in sediments of Gościąż Lake corresponds well to the duration derived from 230Th/234U and 14C dates on Barbados corals, but disagrees with estimates from Soppensee, Lake Holzmaar and Swedish varves. Two AMS dates of terrestrial macrofossils from the PB and YD periods seem to fit both the data obtained for Swiss lake sediments and Barbados corals.
dc.language.isoen
dc.publisherDepartment of Geosciences, The University of Arizona
dc.relation.urlhttp://radiocarbon.webhost.uits.arizona.edu/
dc.rightsCopyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved.
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.titlePossibilities for Reconstructing Radiocarbon Level Changes During the Late Glacial by Using a Laminated Sequence of Lake
dc.typeProceedings
dc.typetext
dc.identifier.journalRadiocarbon
dc.description.noteThis material was digitized as part of a cooperative project between Radiocarbon and the University of Arizona Libraries.
dc.description.collectioninformationThe Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information.
dc.eprint.versionFinal published version
dc.description.admin-noteMigrated from OJS platform February 2021
dc.source.volume34
dc.source.issue3
dc.source.beginpage826
dc.source.endpage832
refterms.dateFOA2021-02-11T20:33:24Z


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