Articles | Volume 6, issue 1
Earth Surf. Dynam., 6, 121–140, 2018
https://doi.org/10.5194/esurf-6-121-2018
Earth Surf. Dynam., 6, 121–140, 2018
https://doi.org/10.5194/esurf-6-121-2018

Research article 05 Mar 2018

Research article | 05 Mar 2018

U–Th and 10Be constraints on sediment recycling in proglacial settings, Lago Buenos Aires, Patagonia

Antoine Cogez et al.

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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 Antoine Cogez on behalf of the Authors (22 Nov 2017)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (04 Jan 2018) by Jane Willenbring
AR by Antoine Cogez on behalf of the Authors (16 Jan 2018)  Author's response    Manuscript
ED: Publish as is (17 Jan 2018) by Jane Willenbring
ED: Publish as is (07 Feb 2018) by A. Joshua West(Editor)
AR by Antoine Cogez on behalf of the Authors (07 Feb 2018)  Author's response    Manuscript
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Short summary
Sediments produced by glaciers are transported by rivers and wind toward the ocean. During their journey, these sediments are weathered, and we know that this has an impact on climate. One key factor is time, but the duration of this journey is largely unknown. We were able to measure the average time that sediment spends only in the glacial area. This time is 100–200 kyr, which is long and allows a lot of processes to act on sediments during their journey.