Articles | Volume 21, issue 5
https://doi.org/10.5194/bg-21-1277-2024
https://doi.org/10.5194/bg-21-1277-2024
Research article
 | 
18 Mar 2024
Research article |  | 18 Mar 2024

Moisture and temperature effects on the radiocarbon signature of respired carbon dioxide to assess stability of soil carbon in the Tibetan Plateau

Andrés Tangarife-Escobar, Georg Guggenberger, Xiaojuan Feng, Guohua Dai, Carolina Urbina-Malo, Mina Azizi-Rad, and Carlos A. Sierra

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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-2023-210', Anonymous Referee #1, 23 Mar 2023
    • AC1: 'Reply on RC1', Andres Tangarife-Escobar, 07 Aug 2023
  • RC2: 'Comment on egusphere-2023-210', Anonymous Referee #2, 25 Jul 2023
    • AC2: 'Reply on RC2', Andres Tangarife-Escobar, 07 Aug 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (13 Aug 2023) by Anja Rammig
AR by Andres Tangarife-Escobar on behalf of the Authors (28 Aug 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (12 Sep 2023) by Anja Rammig
RR by Anonymous Referee #3 (15 Dec 2023)
ED: Publish subject to minor revisions (review by editor) (09 Jan 2024) by Anja Rammig
AR by Andres Tangarife-Escobar on behalf of the Authors (23 Jan 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (29 Jan 2024) by Anja Rammig
AR by Andres Tangarife-Escobar on behalf of the Authors (29 Jan 2024)  Manuscript 
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Short summary
Soil organic matter stability depends on future temperature and precipitation scenarios. We used radiocarbon (14C) data and model predictions to understand how the transit time of carbon varies under environmental change in grasslands and peatlands. Soil moisture affected the Δ14C of peatlands, while temperature did not have any influence. Our models show the correspondence between Δ14C and transit time and could allow understanding future interactions between terrestrial and atmospheric carbon
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