Articles | Volume 19, issue 17
Biogeosciences, 19, 4331–4349, 2022
https://doi.org/10.5194/bg-19-4331-2022
Biogeosciences, 19, 4331–4349, 2022
https://doi.org/10.5194/bg-19-4331-2022
Research article
14 Sep 2022
Research article | 14 Sep 2022

Spatial and temporal variation in δ13C values of methane emitted from a hemiboreal mire: methanogenesis, methanotrophy, and hysteresis

Janne Rinne et al.

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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-2022-76', Anonymous Referee #1, 15 Apr 2022
    • AC1: 'Reply on RC1', Janne Rinne, 25 May 2022
  • RC2: 'Comment on bg-2022-76', Edward Hornibrook, 06 May 2022
    • AC2: 'Reply on RC2', Janne Rinne, 25 May 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (30 May 2022) by Ben Bond-Lamberty
AR by Janne Rinne on behalf of the Authors (22 Jun 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (04 Jul 2022) by Ben Bond-Lamberty
RR by Anonymous Referee #1 (26 Jul 2022)
ED: Publish subject to technical corrections (01 Aug 2022) by Ben Bond-Lamberty
AR by Janne Rinne on behalf of the Authors (05 Aug 2022)  Author's response    Manuscript
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Short summary
The study uses the stable isotope 13C of carbon in methane to investigate the origins of spatial and temporal variation in methane emitted by a temperate wetland ecosystem. The results indicate that methane production is more important for spatial variation than methane consumption by micro-organisms. Temporal variation on a seasonal timescale is most likely affected by more than one driver simultaneously.
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