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Luminescence and radiocarbon ages from laminated Lateglacial aeolian sediments in western Jutland, Denmark
Uppsala University, Disciplinary Domain of Science and Technology, Earth Sciences, Department of Earth Sciences. (Naturgeografi)
Uppsala University, Disciplinary Domain of Science and Technology, Technology, Department of Engineering Sciences, Ion Physics.
2007 (English)In: Boreas, ISSN 0300-9483, E-ISSN 1502-3885, Vol. 36, no 3, 314-325 p.Article in journal (Refereed) Published
Abstract [en]

The chronology of two adjacent Danish Lateglacial sedimentary sequences with well- developed layering of alternating aeolian sand and organic matter has been investigated using both Optically Stimulated Luminescence (OSL) and Accelerator Mass Spectrometry (C-14). Both sites are known to cover at least the period Bolling to Younger Dryas, with the so- called older and younger coversand types present at both localities. Typical overall uncertainties with the OSL data are about two to five times those of the C-14 ages, but both data sets contain clear outliers. When these are excluded, OSL ages appear to be systematically slightly younger than the C-14 ages, by about 10%; possible reasons for this are discussed. The investigation stresses the importance of making several age estimates from any single locality. The older coversand type makes up the pre- Bolling and most, or possibly all, of the Bolling (which also has the highest net accumulation rate). Deposits of the younger coversand type are dominant in layers younger than the Bolling.

Place, publisher, year, edition, pages
2007. Vol. 36, no 3, 314-325 p.
National Category
Earth and Related Environmental Sciences Engineering and Technology
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URN: urn:nbn:se:uu:diva-25110DOI: 10.1080/03009480601024606ISI: 000248080600007OAI: oai:DiVA.org:uu-25110DiVA: diva2:52884
Available from: 2008-05-15 Created: 2008-05-15 Last updated: 2017-12-07Bibliographically approved

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Kolstrup, ElsePossnert, Göran

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