Articles | Volume 20, issue 23
https://doi.org/10.5194/bg-20-4893-2023
https://doi.org/10.5194/bg-20-4893-2023
Research article
 | 
12 Dec 2023
Research article |  | 12 Dec 2023

Comparison of paleobotanical and biomarker records of mountain peatland and forest ecosystem dynamics over the last 2600 years in central Germany

Carrie L. Thomas, Boris Jansen, Sambor Czerwiński, Mariusz Gałka, Klaus-Holger Knorr, E. Emiel van Loon, Markus Egli, and Guido L. B. Wiesenberg

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on bg-2023-57', Anonymous Referee #1, 30 Apr 2023
    • AC1: 'Reply on RC1', Carrie Thomas, 09 Jul 2023
  • RC2: 'Comment on bg-2023-57', Anonymous Referee #2, 02 Jun 2023
    • AC2: 'Reply on RC2', Carrie Thomas, 09 Jul 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (31 Jul 2023) by Petr Kuneš
AR by Carrie Thomas on behalf of the Authors (06 Sep 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (09 Sep 2023) by Petr Kuneš
RR by Anonymous Referee #1 (10 Oct 2023)
ED: Publish subject to minor revisions (review by editor) (10 Oct 2023) by Petr Kuneš
AR by Carrie Thomas on behalf of the Authors (30 Oct 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (02 Nov 2023) by Petr Kuneš
AR by Carrie Thomas on behalf of the Authors (02 Nov 2023)  Manuscript 
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Short summary
Peatlands are vital terrestrial ecosystems that can serve as archives, preserving records of past vegetation and climate. We reconstructed the vegetation history over the last 2600 years of the Beerberg peatland and surrounding area in the Thuringian Forest in Germany using multiple analyses. We found that, although the forest composition transitioned and human influence increased, the peatland remained relatively stable until more recent times, when drainage and dust deposition had an impact.
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