Articles | Volume 23, issue 13
https://doi.org/10.5194/bg-23-4893-2026
https://doi.org/10.5194/bg-23-4893-2026
Research article
 | 
16 Jul 2026
Research article |  | 16 Jul 2026

Are ghost forest trees a substantial source of methane from reservoirs?

Johannes Dittmann, Damien T. Maher, Scott G. Johnston, Douglas R. Tait, Paula Gomez-Alvarez, Alistair Grinham, Katrin Sturm, and Luke C. Jeffrey

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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 egusphere-2025-5594', Anonymous Referee #1, 30 Dec 2025
    • AC1: 'Reply on RC1', Johannes Dittmann, 12 Mar 2026
  • RC2: 'Comment on egusphere-2025-5594', Anonymous Referee #2, 13 Feb 2026
    • AC2: 'Reply on RC2', Johannes Dittmann, 12 Mar 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Reconsider after major revisions (19 Mar 2026) by Edzo Veldkamp
AR by Johannes Dittmann on behalf of the Authors (26 Mar 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (15 Apr 2026) by Edzo Veldkamp
RR by Anonymous Referee #1 (27 Apr 2026)
RR by Anonymous Referee #2 (08 May 2026)
ED: Publish subject to minor revisions (review by editor) (12 May 2026) by Edzo Veldkamp
AR by Johannes Dittmann on behalf of the Authors (21 May 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (01 Jun 2026) by Edzo Veldkamp
AR by Johannes Dittmann on behalf of the Authors (09 Jun 2026)  Manuscript 
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Short summary
Reservoir dead trees (‘ghost forests’) are an overlooked methane (CH4) source in standing freshwaters. We measured CH4 fluxes from 34 trees at multiple stem heights, alongside aquatic CH4 fluxes and physicochemistry, across two field campaigns. Ghost forest CH4 fluxes were highest near reservoir inflows, with tree CH4 contributing extra emissions of 14–15 % on top of the commonly quantified pathways of ebullition and diffusion.
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