Articles | Volume 19, issue 19
Biogeosciences, 19, 4655–4670, 2022
https://doi.org/10.5194/bg-19-4655-2022
Biogeosciences, 19, 4655–4670, 2022
https://doi.org/10.5194/bg-19-4655-2022
Research article
30 Sep 2022
Research article | 30 Sep 2022

Trace gas fluxes from tidal salt marsh soils: implications for carbon–sulfur biogeochemistry

Margaret Capooci and Rodrigo Vargas

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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-2022-101', Anonymous Referee #1, 30 May 2022
    • AC1: 'Reply on RC1', Rodrigo Vargas, 16 Jul 2022
  • RC2: 'Comment on bg-2022-101', Nathan McTigue, 24 Jun 2022
    • AC2: 'Reply on RC2', Rodrigo Vargas, 16 Jul 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (27 Jul 2022) by Tyler Cyronak
AR by Rodrigo Vargas on behalf of the Authors (08 Aug 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (19 Aug 2022) by Tyler Cyronak
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Short summary
Tidal salt marsh soil emits greenhouse gases, as well as sulfur-based gases, which play roles in global climate but are not well studied as they are difficult to measure. Traditional methods of measuring these gases worked relatively well for carbon dioxide, but less so for methane, nitrous oxide, carbon disulfide, and dimethylsulfide. High variability of trace gases complicates the ability to accurately calculate gas budgets and new approaches are needed for monitoring protocols.
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