Articles | Volume 16, issue 4
https://doi.org/10.5194/cp-16-1347-2020
https://doi.org/10.5194/cp-16-1347-2020
Research article
 | 
28 Jul 2020
Research article |  | 28 Jul 2020

Climate impacts on vegetation and fire dynamics since the last deglaciation at Moossee (Switzerland)

Fabian Rey, Erika Gobet, Christoph Schwörer, Albert Hafner, Sönke Szidat, and Willy Tinner

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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
ED: Reconsider after major revisions (13 Jan 2020) by Nathalie Combourieu Nebout
AR by Fabian Rey on behalf of the Authors (07 Feb 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (03 Mar 2020) by Nathalie Combourieu Nebout
RR by Anonymous Referee #3 (15 May 2020)
ED: Reconsider after major revisions (02 Jun 2020) by Nathalie Combourieu Nebout
AR by Fabian Rey on behalf of the Authors (17 Jun 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (30 Jun 2020) by Nathalie Combourieu Nebout
AR by Fabian Rey on behalf of the Authors (02 Jul 2020)  Author's response   Manuscript 
ED: Publish as is (03 Jul 2020) by Nathalie Combourieu Nebout
AR by Fabian Rey on behalf of the Authors (03 Jul 2020)
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Short summary
We present a novel post Last Glacial Maximum sediment record from Moossee (Swiss Plateau, southern central Europe). For the first time, five major reorganizations of vegetation could be definitely linked to paramount postglacial temperature and/or moisture changes. Present-day beech-dominated forests have been resilient to long-term climate change and human land use. They may prevail in future if climate warming does not exceed the amplitude of Mid Holocene temperature and moisture variability.