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dc.contributor.authorPazdur, Anna
dc.contributor.authorPazdur, M. F.
dc.contributor.authorGoslar, Tomasz
dc.contributor.authorWicik, Bogumił
dc.contributor.authorArnold, Maurice
dc.date.accessioned2021-02-11T20:33:32Z
dc.date.available2021-02-11T20:33:32Z
dc.date.issued1994-01-01
dc.identifier.citationPazdur, A., Pazdur, M. F., Goslar, T., Wicik, B., & Arnold, M. (1994). Radiocarbon chronology of Late Glacial and Holocene sedimentation and water-level changes in the area of the Gościąż Lake basin. Radiocarbon, 36(2), 187-202.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200040492
dc.identifier.urihttp://hdl.handle.net/10150/653385
dc.description.abstractWe obtained 14C ages on samples of lake marl and other sediments from cores taken in Gościąż Lake and its environs. Comparison of 14C dates of bulk samples of laminated sediment with varve chronology and available AMS dates of terrestrial macrofossils indicates a reservoir correction of 2000 +/120 yr for the basal series of lake sediments. 14C dates obtained on peat layers underlying the oldest lacustrine sediments in Gościąż and other lakes consistently locate the beginning of organogenic sedimentation in this area at ca. 13 ka BP. We distinguished three periods of lacustrine gyttja sedimentation in cores taken in Gościąż and adjacent lakes: 11.8-10.2 ka, 8-7 ka and 2.7-2.1 ka BP. From the 14C dates of lithological boundaries in these cores, we reconstruct a pattern of lake-level changes during the last 12 ka, remarkably similar to Swedish lakes and generally agreeing with available records from European and American lakes. The behavior of Gościąż Lake during the last 12 ka fairly well reflects global climate changes in the temperate zone during the Late Glacial and Holocene periods..
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.subjectlevels
dc.subjectPlock Depression
dc.subjectPlock Poland
dc.subjectVistulian
dc.subjectVistula River valley
dc.subjectLake Gościąż
dc.subjectterraces
dc.subjectbasins
dc.subjectlaminations
dc.subjectcorrections
dc.subjectclimate
dc.subjectgyttja
dc.subjectPoland
dc.subjectlacustrine environment
dc.subjectice sheets
dc.subjectplanar bedding structures
dc.subjectsedimentary structures
dc.subjectvarves
dc.subjectglobal change
dc.subjectsedimentation
dc.subjectclastic rocks
dc.subjectmarl
dc.subjectisotope ratios
dc.subjectHolocene
dc.subjectCentral Europe
dc.subjectlast glacial maximum
dc.subjectglacial geology
dc.subjectPleistocene
dc.subjectupper Pleistocene
dc.subjecttime scales
dc.subjectEurope
dc.subjectorganic residues
dc.subjectseeds
dc.subjectsediments
dc.subjectCenozoic
dc.subjectQuaternary
dc.subjectwood
dc.subjectC 14
dc.subjectcarbon
dc.subjectisotopes
dc.subjectradioactive isotopes
dc.subjectC 13 C 12
dc.subjectstable isotopes
dc.subjectabsolute age
dc.subjectsedimentary rocks
dc.titleRadiocarbon Chronology of Late Glacial and Holocene Sedimentation and Water-Level Changes in the Area of the Gościąż Lake Basin
dc.typeArticle
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.volume36
dc.source.issue2
dc.source.beginpage187
dc.source.endpage202
refterms.dateFOA2021-02-11T20:33:32Z


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