Articles | Volume 14, issue 11
Clim. Past, 14, 1607–1624, 2018
https://doi.org/10.5194/cp-14-1607-2018
Clim. Past, 14, 1607–1624, 2018
https://doi.org/10.5194/cp-14-1607-2018

Research article 02 Nov 2018

Research article | 02 Nov 2018

Leaf wax n-alkane distributions record ecological changes during the Younger Dryas at Trzechowskie paleolake (northern Poland) without temporal delay

Bernhard Aichner et al.

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Interactive discussion

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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 (18 Jun 2018) by Denis-Didier Rousseau
AR by Bernhard Aichner on behalf of the Authors (18 Jun 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (25 Jun 2018) by Denis-Didier Rousseau
RR by Anonymous Referee #2 (09 Jul 2018)
RR by Anonymous Referee #3 (21 Sep 2018)
ED: Publish subject to technical corrections (30 Sep 2018) by Denis-Didier Rousseau
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Short summary
Abundances of plant biomarkers are compared with pollen data in a 3000-year climate archive covering the Late Glacial to Holocene transition in northern Poland. Both parameters synchronously show the rapid onset (12680–12600 yr BP) and termination (11580–11490 yr BP) of the Younger Dryas cold interval in the study area. This demonstrates the suitability of such proxies to record pronounced changes in vegetation cover without significant delay.