Articles | Volume 11, issue 2
https://doi.org/10.5194/soil-11-911-2025
© Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.
Improved management increases soil mineral-protected organic carbon storage via plant-microbial-nutrient mediation in semi-arid grasslands
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- Final revised paper (published on 05 Nov 2025)
- Supplement to the final revised paper
- Preprint (discussion started on 24 Apr 2025)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on egusphere-2025-1711', Anonymous Referee #1, 05 May 2025
- AC3: 'Reply on RC1', Victor Rolo, 16 Jun 2025
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RC2: 'Comment on egusphere-2025-1711', Anonymous Referee #2, 15 May 2025
- AC1: 'Reply on RC2', Victor Rolo, 16 Jun 2025
- AC2: 'Reply on RC2', Victor Rolo, 16 Jun 2025
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (03 Jul 2025) by Katerina Georgiou
AR by Victor Rolo on behalf of the Authors (07 Jul 2025)
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ED: Referee Nomination & Report Request started (18 Jul 2025) by Katerina Georgiou
RR by Anonymous Referee #2 (28 Jul 2025)
RR by Anonymous Referee #1 (08 Aug 2025)
ED: Publish subject to minor revisions (review by editor) (23 Aug 2025) by Katerina Georgiou
AR by Victor Rolo on behalf of the Authors (03 Sep 2025)
Author's response
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ED: Publish subject to minor revisions (review by editor) (14 Sep 2025) by Katerina Georgiou
AR by Victor Rolo on behalf of the Authors (17 Sep 2025)
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ED: Publish subject to technical corrections (03 Oct 2025) by Katerina Georgiou
ED: Publish subject to technical corrections (04 Oct 2025) by Rémi Cardinael (Executive editor)
AR by Victor Rolo on behalf of the Authors (07 Oct 2025)
Author's response
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This manuscript presents an original and timely contribution to our understanding of soil carbon (SOC) dynamics in semi-arid grasslands, a topic of high relevance given the increasing threats of climate change and land degradation to these ecosystems. The study stands out for its comprehensive methodological approach, which combines field-scale experimentation with detailed plants, soil, and microbial analyses across an environmental gradient. The authors successfully integrate ecological, biochemical, and management dimensions to investigate how different grazing practices influence both particulate and mineral-associated organic carbon pools.
Despite the strengths outlined above, there are several methodological and interpretative aspects that require clarification or revision before the manuscript can be considered for publication.
Issues with chaOM fraction:
Figure 3a. The reported mean C/N ratio for the chaOM fraction is 4.41, and several values appear to fall between 0 and 2. These values are exceptionally low for any known pool of organic matter. I recommend that the authors clarify whether the C/N values presented for the soil fractions reflect total N or organic N (i.e., after subtracting inorganic N). If only total N was used, recalculating C/N based on organic N would likely provide a more accurate picture of the biochemical composition of these fractions.
The manuscript reports the use of a combined size-density fractionation protocol following Leuthold et al. (2024), in which the light fraction (<1.85 g cm⁻³) is separated from the heavier material. The latter is subsequently sieved at 53 μm to yield a coarse heavy-associated organic matter fraction (chaOM; >53 μm) and a fine mineral-associated organic matter fraction (MAOM; <53 μm). The chaOM and MAOM fractions were later combined and reported together as MAOM.
While the decision to include chaOM within MAOM appears justified based on the rationale provided in Leuthold et al. (2024), this approach diverges from the more widely accepted definition of MAOM as material denser than 1.6–1.85 g/cm³ and smaller than 50–63 μm (Lavallee et al., 2020). Consequently, this choice may limit the generalizability of the findings and their integration into broader syntheses. That said, since the chaOM fraction accounted for less than 5% of total SOM, the implications are likely minor.
Nonetheless, as emphasized by Lavallee et al. (2020), there is a pressing need for greater consistency in the operational definitions of POM and MAOM to facilitate comparability across studies. I recommend explicitly acknowledging that organic matter >53 μm is not typically included in the MAOM fraction.
L184-187. 2.2. Climatic variables. This section consists of a single sentence, which may not warrant a standalone subsection. I suggest either expanding it with additional context or incorporating it into a broader methodological section.
L248. SOC was already defined.
L249-250. It would be useful to specify whether inorganic carbon (e.g., carbonates) was measured or removed prior to C analysis.
Figure 4. Please add the slope of the regression line. This figure should be in the results section.
L299. This sentence should be included in another paragraph.
Figure 5
L322. … bulk density (BD). What was the range of BD? Was it similar across treatments? If not, equivalent mass corrections should be considered.
L340. Could you please clarify what is a direct and indirect effect?
L364-365. “…informing on lignin content and vegetation productivity, was negatively correlated with the POC, MAOC and SOC stocks and the microbial biomass”. Lignin content was negatively correlated with vegetation productivity. Therefore, those variables were negatively correlated with lignin, but positive correlated with vegetation productivity.
L430-432. “The silvopastoral character of our farms could explain the low MAOC/SOC ratios, as litter from scattered trees increases carbon stocks in woody grasslands, especially in the POM fraction”. This explanation is plausible; however, your results show that lignin and C/N were negatively correlated with POC. How do you reconcile this apparent inconsistency?
L439. I don’t see a saturation curve in Fig. 3 b. Figure 4 shows a better way to illustrate the C-saturation deficit. It would be interesting to compare the results with the maximum C-loading found by Georgiou (~ 86 mg C g silt+clay).
L497-498. However, roots promote MAOM formation not from root biomass but from rhizodeposition (see Sokol, N.W., Bradford, M.A., 2019. Microbial formation of stable soil carbon is more efficient from belowground than aboveground input. Nature Geosci 12, 46–53. https://doi.org/10.1038/s41561-018-0258-6; Villarino, S.H., Pinto, P., Jackson, R.B., Piñeiro, G., 2021. Plant rhizodeposition: A key factor for soil organic matter formation in stable fractions. Science Advances 7, eabd3176.)
L546. In line with my previous comment, bulk density values and changes should be reported. Previously, the acronym BD was used for apparent density.
L590. Mineral-associated organic carbon was previously defined as MAOM.