Articles | Volume 22, issue 2
https://doi.org/10.5194/bg-22-435-2025
https://doi.org/10.5194/bg-22-435-2025
Research article
 | 
24 Jan 2025
Research article |  | 24 Jan 2025

Decomposing the Tea Bag Index and finding slower organic matter loss rates at higher elevations and deeper soil horizons in a minerogenic salt marsh

Satyatejas G. Reddy, W. Reilly Farrell, Fengrun Wu, Steven C. Pennings, Jonathan Sanderman, Meagan Eagle, Christopher Craft, and Amanda C. Spivak

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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-2024-1328', Anonymous Referee #1, 21 Jul 2024
  • RC2: 'Comment on egusphere-2024-1328', Anonymous Referee #2, 09 Aug 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (19 Oct 2024) by Nicolas Brüggemann
AR by Satyatejas Reddy on behalf of the Authors (21 Oct 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (22 Oct 2024) by Nicolas Brüggemann
RR by Anonymous Referee #1 (28 Oct 2024)
RR by Anonymous Referee #2 (07 Nov 2024)
ED: Publish subject to technical corrections (13 Nov 2024) by Nicolas Brüggemann
AR by Satyatejas Reddy on behalf of the Authors (18 Nov 2024)  Author's response   Manuscript 
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Short summary
Organic matter decay in salt marsh soils is not well understood. We used the Tea Bag Index, a standardized litter approach, to test how decay changes with soil depth, elevation, and time. The index overestimated decay, but one component, rooibos tea, produced comparable rates to natural litter. We found that decay was higher at shallower depths and lower marsh elevations, suggesting that hydrological setting may be a particularly important control on organic matter loss.
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