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    Luminescence dating indicates radiocarbon age underestimation in late Pleistocene fluvial deposits from eastern England

    Briant, Rebecca M. and Bateman, M.D. (2009) Luminescence dating indicates radiocarbon age underestimation in late Pleistocene fluvial deposits from eastern England. Journal of Quaternary Science 24 (8), pp. 916-927. ISSN 0267-8179.

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    Abstract

    Robust geochronological control is crucial for interpreting and correlating the environmental record from fragmentary terrestrial sequences from the last glacial period. Traditional terrestrial stratigraphies are typically reliant on radiocarbon dating, although estimates of antiquity for samples older than 40 ka may be unreliable. Optically stimulated luminescence (OSL) dating of sediments is an alternative for dating the whole of the last glacial period and also provides the opportunity to independently test radiocarbon based chronologies. This paper presents a set of nine directly comparable paired OSL and accelerator mass spectrometry (AMS) radiocarbon ages from multiple sites within Devensian fluvial sediments in lowland Britain and shows that it is possible to obtain robust OSL age estimates throughout this time period. The two techniques agree well for ages younger than ca. 29 14C ka BP (ca. 35 cal. ka BP) but disagree beyond ca. 35 14C ka BP (ca. 40 cal. ka BP). This is thought to be due to radiocarbon ages on older organic material having been contaminated by low levels of modern carbon. It is therefore suggested that all conventionally pre-treated radiocarbon ages greater than 35 14C ka BP should be treated with extreme caution.

    Metadata

    Item Type: Article
    Keyword(s) / Subject(s): radiocarbon, optically stimulated luminescence, Devensian, fluvial
    School: Birkbeck Faculties and Schools > Faculty of Humanities and Social Sciences > School of Social Sciences
    Depositing User: Administrator
    Date Deposited: 17 Feb 2011 09:23
    Last Modified: 02 Aug 2023 16:54
    URI: https://eprints.bbk.ac.uk/id/eprint/3069

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