Articles | Volume 13, issue 1
https://doi.org/10.5194/tc-13-97-2019
https://doi.org/10.5194/tc-13-97-2019
Research article
 | 
11 Jan 2019
Research article |  | 11 Jan 2019

Origin, burial and preservation of late Pleistocene-age glacier ice in Arctic permafrost (Bylot Island, NU, Canada)

Stephanie Coulombe, Daniel Fortier, Denis Lacelle, Mikhail Kanevskiy, and Yuri Shur

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Stephanie Coulombe on behalf of the Authors (20 Sep 2018)  Author's response    Manuscript
ED: Reconsider after major revisions (06 Oct 2018) by Julia Boike
AR by Svenja Lange on behalf of the Authors (08 Nov 2018)  Author's response
ED: Publish subject to technical corrections (23 Nov 2018) by Julia Boike
AR by Stephanie Coulombe on behalf of the Authors (23 Nov 2018)  Author's response    Manuscript
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Short summary
This study provides a detailed description of relict glacier ice preserved in the permafrost of Bylot Island (Nunavut). We demonstrate that the 18O composition (-34.0 0.4 ‰) of the ice is consistent with the late Pleistocene age ice in the Barnes Ice Cap. As most of the glaciated Arctic landscapes are still strongly determined by their glacial legacy, the melting of these large ice bodies could have significant impacts on permafrost geosystem landscape dynamics and ecosystems.