Articles | Volume 11, issue 2
https://doi.org/10.5194/soil-11-883-2025
© Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.
Contribution of soil microbial necromass carbon to soil organic carbon fractions and its influencing factors in different grassland types
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- Final revised paper (published on 22 Oct 2025)
- Supplement to the final revised paper
- Preprint (discussion started on 20 Mar 2025)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on egusphere-2025-1122', Anonymous Referee #1, 04 May 2025
- AC1: 'Reply on RC1', Jianbing Guo, 14 May 2025
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RC2: 'Comment on egusphere-2025-1122', Anonymous Referee #2, 13 May 2025
- AC2: 'Reply on RC2', Jianbing Guo, 29 May 2025
- AC3: 'Reply on RC2', Jianbing Guo, 29 May 2025
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (30 May 2025) by Ashish Malik
AR by Jianbing Guo on behalf of the Authors (04 Jun 2025)
Author's response
Author's tracked changes
Manuscript
ED: Publish subject to revisions (further review by editor and referees) (03 Jul 2025) by Ashish Malik
AR by Jianbing Guo on behalf of the Authors (03 Jul 2025)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (16 Jul 2025) by Ashish Malik
RR by Anonymous Referee #2 (23 Aug 2025)
ED: Publish subject to technical corrections (03 Sep 2025) by Ashish Malik
ED: Publish subject to technical corrections (03 Sep 2025) by Rémi Cardinael (Executive editor)
AR by Jianbing Guo on behalf of the Authors (05 Sep 2025)
Author's response
Manuscript
Chen et al. explored the contribution of soil fungal and bacterial necromass carbon to soil organic carbon fractions in different grassland types. Moreover, the influencing factors were explored using random forest modeling. The results showed the contents of MAOC and POC in the 0–100 cm soil layer were Meadow steppe > Typical steppe > Desert steppe > Steppe desert. FNC dominated both MAOC and POC, and its contribution was higher than the contribution of BNC. The results from this study help to understand the composition of SOC in an ecologically transitional zone. However, substantial revisions are needed to improve the MS quality.