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    Dating Bones near the Limit of the Radiocarbon Dating Method: Study Case Mammoth from Niederweningen, ZH Switzerland

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    Author
    Hajdas, Irka
    Michczyński, Adam
    Bonani, Georges
    Wacker, Lukas
    Furrer, Heinz
    Issue Date
    2009-01-01
    
    Metadata
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    Citation
    Hajdas, I., Michczyński, A., Bonani, G., Wacker, L., & Furrer, H. (2009). Dating bones near the limit of the radiocarbon dating method: Study case mammoth from Niederweningen, ZH Switzerland. Radiocarbon, 51(2), 675-680.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    URI
    http://hdl.handle.net/10150/654185
    DOI
    10.1017/S0033822200056010
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    Preparation of bone material for radiocarbon dating is still a subject of investigation. In the past, the most problematic ages appeared to be the very old bones, i.e. those with ages close to the limit of the dating method. Development of preparative methods requires sufficient amounts of bone material as well as the possibility of verification of the ages. In the peat section at Niederweningen, ZH Switzerland, numerous bones of mammoth and other animals were found in the late 19th century. The first accelerator mass spectrometry (AMS) radiocarbon ages of those bones from 1890/1891 excavations placed the age between 33,000 and 35,000 BP. The excavations in 2003/2004 provided additional material for 14C dating. An age of 45,870 +/- 1080 BP was obtained on base (NaOH step) cleaned gelatin from mammoth bone, which was very close to the age of 45,430 +/- 1020 BP obtained for the peat layer that buried the mammoths. The 14C age of gelatin cleaned using the ultrafiltration method obtained in this study, 45,720 +/- 710 BP, is in a very good agreement with the previously obtained results. Moreover, the study shows that 3 pretreatment methods (base+Longin, Longin+ultrafiltration, and base+Longin+ultrafiltration) give ages consistent with each other and with the age of the peat section.
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200056010
    Scopus Count
    Collections
    Radiocarbon, Volume 51, Number 2 (2009)

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