Infrared radiofluorescence (IR-RF) dating of middle pleistocene fluvial archives of the Heidelberg Basin (Southwest Germany)

dc.bibliographicCitation.firstPage23eng
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.journalTitleGeochronometria : journal on methods and applications of absolute chronologyeng
dc.bibliographicCitation.lastPage33eng
dc.bibliographicCitation.volume38eng
dc.contributor.authorLauer, Tobias
dc.contributor.authorKrbetschek, Matthias
dc.contributor.authorFrechen, Manfred
dc.contributor.authorTsukamoto, Sumiko
dc.contributor.authorHoselmann, Christian
dc.contributor.authorWeidenfeller, Michael
dc.date.accessioned2022-02-18T07:20:07Z
dc.date.available2022-02-18T07:20:07Z
dc.date.issued2011
dc.description.abstractThe infrared radiofluorescence (IR-RF) dating technique was applied to eight fluvial samples that were collected from two sediment cores at the Heidelberg Basin located near Viernheim and Ludwigshafen in southwest Germany. Based on the IR-RF derived ages of the samples it was possible to establish a chronological framework for the Mid-Pleistocene fluvial deposits of the Heidelberg Basin. The results allow us to distinguish between four main periods of aggradation. The lowermost sample taken from 100 m core depth lead to an IR-RF age of 643 ± 28 ka pointing to a Cromerian period of aggradation (OIS 17-16). For the Elsterian it is now possible to distinguish between two aggradation periods, one occurring during the Lower Elsterian period (OIS 15) and a second during the Upper Elsterian period (OIS 12-11). For the so called Upper interlayer (or "Oberer Zwischenhorizont" - a layer of organic-rich and finer-grained deposits), the IR-RF results point to a deposition age of around 300 ka, with samples taken directly on top and out of this layer yielding IR-RF ages of 288 ± 19 ka and 302 ± 19 ka, respectively. Hence, the measured IR-RF ages clearly point to a deposition during the Lower Saalian period (OIS 9-8) whereas earlier studies assumed a Cromerian age for the sediments of the Upper Interlayer based on pollen records and also mollusc fauna. The new IR-RF dataset indicates that significant hiatuses are present within the fluvial sediment successions. In particular the Eemian and Upper Saalian deposits are missing in this part of the northern Upper Rhine Graben, as the 300 ka deposits are directly overlain by Weichselian fluvial sediments. It is obvious that time periods of increased fluvial aggradation were interrupted by time periods of almost no aggradation or erosion which should have been mainly triggered by phases of increased and decreased subsidence of the Heidelberg Basin. © 2011 Silesian University of Technology.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/8029
dc.identifier.urihttps://doi.org/10.34657/7070
dc.language.isoengeng
dc.publisherWarsaw : De Gruytereng
dc.relation.doihttps://doi.org/10.2478/s13386-011-0006-9
dc.relation.essn1897-1695
dc.rights.licenseCC BY-NC-ND 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/3.0/eng
dc.subject.ddc620eng
dc.subject.ddc690eng
dc.subject.otherFluvial archiveeng
dc.subject.otherHeidelberg basineng
dc.subject.otherInfrared radiofluorescenceeng
dc.subject.otherMiddle pleistoceneeng
dc.subject.otherRhine systemeng
dc.titleInfrared radiofluorescence (IR-RF) dating of middle pleistocene fluvial archives of the Heidelberg Basin (Southwest Germany)eng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorLIAGeng
wgl.subjectIngenieurwissenschafteneng
wgl.typeZeitschriftenartikeleng
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