Articles | Volume 11, issue 2
https://doi.org/10.5194/soil-11-991-2025
https://doi.org/10.5194/soil-11-991-2025
Original research article
 | 
28 Nov 2025
Original research article |  | 28 Nov 2025

Availability of labile carbon controls the temperature-dependent response of soil organic matter decomposition in alpine soils

Dario Püntener, Tatjana C. Speckert, Yves-Alain Brügger, and Guido L. B. Wiesenberg

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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-2025-1546', Anonymous Referee #1, 30 May 2025
    • AC1: 'Response to the comments of Anonymous Referee #1', Dario Püntener, 31 Jul 2025
  • RC2: 'Comment on egusphere-2025-1546', Anonymous Referee #2, 16 Jun 2025
    • AC2: 'Response to the comments of Anonymous Referee #2', Dario Püntener, 31 Jul 2025

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (19 Aug 2025) by Kate Buckeridge
AR by Dario Püntener on behalf of the Authors (12 Sep 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (06 Oct 2025) by Kate Buckeridge
RR by Anonymous Referee #1 (16 Oct 2025)
ED: Publish subject to minor revisions (review by editor) (27 Oct 2025) by Kate Buckeridge
AR by Dario Püntener on behalf of the Authors (28 Oct 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (10 Nov 2025) by Kate Buckeridge
ED: Publish as is (10 Nov 2025) by Rémi Cardinael (Executive editor)
AR by Dario Püntener on behalf of the Authors (10 Nov 2025)  Manuscript 
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Short summary
Alpine soils store much carbon but warming and changes in vegetation could reverse this by turning them into carbon sources. In a one-year laboratory study, we examined alpine forest and pasture soils and added fresh grass litter marked with a carbon tracer to track decomposition under different temperatures. Our findings reveal that fresh plant material drives soil breakdown more than temperature alone, offering new insights into how climate change may affect carbon storage in mountain regions.
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