Articles | Volume 10, issue 6
https://doi.org/10.5194/tc-10-3091-2016
https://doi.org/10.5194/tc-10-3091-2016
Review article
 | 
21 Dec 2016
Review article |  | 21 Dec 2016

Radiocarbon dating of glacier ice: overview, optimisation, validation and potential

Chiara Uglietti, Alexander Zapf, Theo Manuel Jenk, Michael Sigl, Sönke Szidat, Gary Salazar, and Margit Schwikowski

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Chiara Uglietti on behalf of the Authors (26 Oct 2016)
ED: Referee Nomination & Report Request started (28 Oct 2016) by Shugui Hou
RR by Anonymous Referee #2 (09 Nov 2016)
RR by Anonymous Referee #1 (11 Nov 2016)
ED: Publish as is (14 Nov 2016) by Shugui Hou
AR by Chiara Uglietti on behalf of the Authors (14 Nov 2016)
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Short summary
A meaningful interpretation of the climatic history contained in ice cores requires a precise chronology. For dating the older and deeper part of the glaciers, radiocarbon analysis can be used when organic matter such as plant or insect fragments are found in the ice. Since this happens rarely, a complementary dating tool, based on radiocarbon dating of the insoluble fraction of carbonaceous aerosols entrapped in the ice, allows for ice dating between 200 and more than 10 000 years.