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University of Groningen

Duration of activity inestimable due to imprecision of the data

Dee, Michael W.; Kuitems, Margot

Published in:

Proceedings of the National Academy of Sciences of the United States of America

DOI:

10.1073/pnas.1914651116

IMPORTANT NOTE: You are advised to consult the publisher's version (publisher's PDF) if you wish to cite from

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Publication date:

2019

Link to publication in University of Groningen/UMCG research database

Citation for published version (APA):

Dee, M. W., & Kuitems, M. (2019). Duration of activity inestimable due to imprecision of the data.

Proceedings of the National Academy of Sciences of the United States of America, 116(46), 22907-22907.

https://doi.org/10.1073/pnas.1914651116

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LETTER

Duration of activity inestimable due to imprecision

of the data

Michael W. Deea,1and Margot Kuitemsa

Ledger et al. (1) report some exciting findings from the well-known site of L’Anse aux Meadows (LAM) in New-foundland. However, their eye-catching conclusion that “Norse activity at LAM may have endured for a century” is misleading and arises from a misinterpretation of the outputs of their chronological model, constructed in the program OxCal (2). To estimate the duration of Norse activity, they used OxCal’s Span function, which pro-duced a 2σ range (95% probability) of 0 to 195 y. This should not be regarded as evidence for a duration of “up to 195 y.” In fact, the most probable outcome is that Norse activity was only a matter of years or even less. The reason the tail of the probability density

function extends so far is because of the inherent un-certainty in the data. That is, the analysis is hindered by the fact there are too few high-precision dates available. This point is easily demonstrated by simulating some radiocarbon dates (using OxCal’s R_Simulate function) of comparable precision to those available from LAM. Even if all of the dates are simulated to come from the same calendar year, the Span function tends to produce a 2σ range that extends for more than a century. The situation is analogous to estimating the size of a crowd from an image made up of too few pixels. Resolving such periods of time on the basis of the data available is simply beyond the capability of OxCal.

1 P. M. Ledger, L. Girdland-Flink, V. Forbes, New horizons at L’Anse aux Meadows. Proc. Natl. Acad. Sci. U.S.A. 116, 15341–15343 (2019).

2 C. Bronk Ramsey, Radiocarbon calibration and analysis of stratigraphy: The OxCal program. Radiocarbon 37, 425–430 (1995).

aCentre for Isotope Research, University of Groningen, 9747 AG Groningen, The Netherlands

Author contributions: M.W.D. and M.K. wrote the paper. The authors declare no competing interest.

This open access article is distributed underCreative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND).

1

To whom correspondence may be addressed. Email: m.w.dee@rug.nl. First published October 16, 2019.

www.pnas.org/cgi/doi/10.1073/pnas.1914651116 PNAS | November 12, 2019 | vol. 116 | no. 46 | 22907

LETT

ER

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