Small, D. and Fabel, D. (2015) A Lateglacial 10Be production rate from glacial lake shorelines in Scotland. Journal of Quaternary Science, 30(6), pp. 509-513. (doi: 10.1002/jqs.2804)
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Abstract
The identification of tephra within varved deposits of a former ice-dammed lake that existed in Scotland during the Younger Dryas provides an opportunity to calibrate 10Be production rates using previously published 10Be concentrations from the lake shoreline and independently derived ages for the tephra’s derived from the Greenland Ice Core records. The best-estimate ages of the tephras yield indistinguishable 10Be production rate values for spallation with an average value of 4.26 ± 0.21 atoms g-1 a-1 using the ‘Lm’ scaling scheme. These values are in best agreement with the most proximal reference 10Be production rate from Norway.
Item Type: | Articles |
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Additional Information: | This is the peer reviewed version of the following article: Small, D., and Fabel, D. (2015) A Lateglacial 10Be production rate from glacial lake shorelines in Scotland. Journal of Quaternary Science, 30(6), pp. 509-513, which has been published in final form at http://dx.doi.org/10.1002/jqs.2804. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Self-Archiving. |
Status: | Published |
Refereed: | Yes |
Glasgow Author(s) Enlighten ID: | Small, Dr David and Fabel, Dr Derek |
Authors: | Small, D., and Fabel, D. |
Subjects: | G Geography. Anthropology. Recreation > GB Physical geography |
College/School: | College of Science and Engineering > School of Geographical and Earth Sciences > Geography College of Science and Engineering > Scottish Universities Environmental Research Centre |
Journal Name: | Journal of Quaternary Science |
Publisher: | John Wiley & Sons Ltd. |
ISSN: | 0267-8179 |
ISSN (Online): | 1099-1417 |
Published Online: | 26 August 2016 |
Copyright Holders: | Copyright © 2015 John Wiley & Sons, Ltd. |
First Published: | First published in Journal of Quaternary Science 30(6):509-513 |
Publisher Policy: | Reproduced in accordance with the copyright policy of the publisher |
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