Articles | Volume 15, issue 1
The Cryosphere, 15, 17–30, 2021
The Cryosphere, 15, 17–30, 2021

Research article 04 Jan 2021

Research article | 04 Jan 2021

Subglacial carbonate deposits as a potential proxy for a glacier's former presence

Matej Lipar et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (20 Oct 2020) by Chris R. Stokes
AR by Matej Lipar on behalf of the Authors (20 Oct 2020)  Author's response    Manuscript
ED: Publish as is (28 Oct 2020) by Chris R. Stokes
Short summary
The U–Th ages of subglacial carbonate deposits from a recently exposed surface previously occupied by the disappearing glacier in the SE European Alps suggest the glacier’s presence throughout the entire Holocene. These thin deposits, formed by regelation, would have been easily eroded if exposed during previous Holocene climatic optima. The age data indicate the glacier’s present unprecedented level of retreat and the potential of subglacial carbonates to act as palaeoclimate proxies.