Articles | Volume 12, issue 2
https://doi.org/10.5194/soil-12-1121-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Alpine wetland degradation reshapes the balance between hydrolytic and reductive soil nitrogen cycling enzyme potentials on the Qinghai–Tibetan Plateau
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- Final revised paper (published on 06 Nov 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 27 Jul 2026)
- 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-2026-3406', Anonymous Referee #1, 13 Aug 2026
- AC1: 'Reply on RC1', Wenhua Chang, 06 Sep 2026
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RC2: 'Comment on egusphere-2026-3406', Guang-Hui Yu, 16 Aug 2026
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AC2: 'Reply on RC2', Wenhua Chang, 06 Sep 2026
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RC3: 'Reply on AC2', Guang-Hui Yu, 07 Sep 2026
- AC3: 'Reply on RC3', Wenhua Chang, 07 Sep 2026
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RC3: 'Reply on AC2', Guang-Hui Yu, 07 Sep 2026
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AC2: 'Reply on RC2', Wenhua Chang, 06 Sep 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Submit a revised manuscript (13 Sep 2026) by Kairsty Topp
AR by Wenhua Chang on behalf of the Authors (26 Sep 2026)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (03 Oct 2026) by Kairsty Topp
RR by Guang-Hui Yu (09 Oct 2026)
ED: Publish as is (21 Oct 2026) by Kairsty Topp
ED: Publish as is (22 Oct 2026) by Jeanette Whitaker (Executive editor)
AR by Wenhua Chang on behalf of the Authors (30 Oct 2026)
Manuscript
General Comments
This manuscript investigates how alpine wetland degradation affects soil nitrogen (N) cycling through the lens of enzyme activities in the Gahai Wetland on the Qinghai-Tibet Plateau. The authors employ a three-year field study across four degradation stages, measuring four key N-cycling enzymes (urease, protease, nitrate reductase, nitrite reductase) and developing a novel Nitrogen Cycling Functional Balance (NCFB) index to assess the coordination between hydrolytic and reductive functions.
General Comment: Novelty and Contribution
This manuscript addresses an important knowledge gap concerning how alpine wetland degradation restructures soil nitrogen cycling, moving beyond descriptive assessments of individual enzyme activities to evaluate functional coordination between complementary N-transformation pathways. The novelty lies in three key aspects: (1) the development of a Nitrogen Cycling Functional Balance (NCFB) index that integrates hydrolytic and reductive enzyme functions into a single metric, providing a framework for quantifying functional reorganization rather than simply measuring activity levels; (2) the demonstration that degradation induces enzyme-specific divergent responses—urease and nitrate reductase increasing while protease and nitrite reductase decline—revealing that soil N cycling undergoes pathway-specific restructuring rather than uniform suppression; and (3) the multi-year temporal design that captures how interannual hydroclimatic variability, particularly drought, amplifies degradation-induced functional decoupling. The contribution is significant in providing a mechanistic understanding of how hydrological drying and resource depletion drive N-cycling destabilization in alpine wetlands, with implications for restoration priorities in these vulnerable ecosystems. The work is suitable for publication in SOIL, as it addresses soil biogeochemical cycling in a globally important ecosystem under anthropogenic pressure, though substantial revision is needed to address limitations related to potential enzyme assays, space-for-time substitution assumptions, and causal inference. With careful revision addressing these issues, the manuscript would make a valuable contribution to SOIL. The multi-year design, enzyme-specific responses, and functional balance approach are significant strengths that merit publication after substantial revision.
Major Comments
The authors measure potential enzyme activities under optimized laboratory conditions (24-hour incubation at constant temperature with excess substrate). However:
-Redox sensitivity: Nitrate reductase and nitrite reductase are particularly sensitive to redox conditions. Measuring them under aerobic laboratory conditions may not reflect in-situ activities in wetland soils, where anaerobic microsites and fluctuating redox conditions are critical for denitrification-related processes.
- Substrate availability: The NCFB index is calculated from potential activities measured under optimal conditions, not from actual rates constrained by in-situ substrate availability. This may overstate functional imbalances if the actual rates are co-limited by substrates.
- Enzyme stability: Some soil enzymes can remain active after extraction or in stored samples, potentially overestimating activity.
Required revisions:
- Add a dedicated subsection in the Discussion addressing the limitations of potential enzyme assays for inferring in-situ N cycling
- Discuss how potential activities might differ from in-situ rates, particularly for redox-sensitive enzymes
- Consider whether the NCFB index should be interpreted as "functional potential" rather than "functional balance"
- If possible, compare potential activities with any available in-situ rate measurements or cite literature on the relationship between potential and actual enzyme activities in similar systems
The authors use space-for-time substitution but do not adequately address its limitations. The four degradation stages are described as representing a degradation gradient, but:
- Were sites matched for parent material, topography, and historical land use?
- Is there evidence that the sites represent a true chronosequence (e.g., historical aerial photos, local knowledge of degradation timing)?
- Could differences among sites reflect inherent spatial heterogeneity rather than degradation stage?
Required revisions:
- Provide more information on how degradation stages were delineated (Table S1 is mentioned but not shown in the main text)
- Discuss the assumptions of space-for-time substitution and how the study design mitigates potential confounding factors
- If available, provide evidence that the sites represent a degradation trajectory (e.g., historical data, local knowledge)
The NCFB index is a central contribution, but its interpretation requires clarification:
- Why is the balance defined as hydrolytic minus reductive functions? This assumes that higher values are "better" (more coordinated), but this is a value judgment that may not be universally valid.
- What is the ecological significance of the shift from negative to positive correlation between hydrolytic and reductive functions (Figure S4)? The authors note this change but do not fully explain its meaning.
- Could the NCFB shift simply reflect changes in the relative abundance of different microbial groups rather than functional reorganization?
Required revisions:
- Provide a more explicit justification for the NCFB index formulation
- Explain what a "balanced" vs. "imbalanced" N-cycling system means in terms of ecosystem function
- Discuss alternative interpretations of the NCFB shift (e.g., microbial community composition changes, not just functional reorganization)
The SEM shows that SOC has a direct negative effect on NCFB (Figure 5b), which seems counterintuitive—higher SOC is associated with lower NCFB. This requires explanation:
- Is this a statistical artifact or a real ecological relationship?
- Does the negative relationship between SOC and NCFB reflect the fact that SOC includes recalcitrant carbon that does not support microbial activity?
- The authors focus on hydrological limitation but the SEM suggests more complex interactions with carbon availability.
Required revisions:
- Provide a more detailed interpretation of the negative SOC-NCFB relationship
- Consider whether the measure of SOC (total organic carbon) adequately captures the labile carbon fraction that drives microbial enzyme production
- Discuss whether the model should be refined to include a labile carbon pool
The authors identify year 2020 as dry and 2021 as wet (implied), but the precipitation data are in the supplement (Figure S1) and the specific values are not presented in the main text:
- What were the actual precipitation amounts for 2019, 2020, and 2021?
- Are these departures from long-term averages significant?
- The conclusion that "drier conditions amplifying degradation effects" is important but needs quantitative support.
Required revisions:
- Present key precipitation statistics in the main text or clearly reference the supplement
- If possible, quantify the interaction between year (wet/dry) and degradation stage using statistical tests (the mixed models in Table 2 do not include year × degradation interactions)
- Discuss the implications of these findings for projections of future climate change effects on alpine wetlands
Minor Comments
- Why were Tukey's HSD tests used for multiple comparisons rather than, say, Dunnett's test (which compares each treatment to a control)?
- Were data transformation and the assumptions of the mixed models (normality, homogeneity of variance) checked and reported?
- The linear mixed models are described but the model specification (random intercepts only? random slopes?) is not fully detailed.
- The y-axis scales differ substantially among enzymes, making comparisons difficult. Consider adding a supplementary figure with standardized scales or including the ranges in the caption.
- The statistical comparisons are based on data aggregated across years and depths. Consider whether this aggregation masks important variation.
- The RDA explains 66.2% and 8.62% of variation on axes 1 and 2, but the interpretation of axis 2 is not discussed.
- The "circle size" in Figure 4c is visually informative but the legend should clearly explain what it represents.
Editorial/Technical Comments
- Line 37: "wetland health and soil functional status" - consider defining "health" more precisely
- Line 27 and 96: "overgrazing" - the introduction mentions overgrazing as a driver but the methods do not describe how grazing intensity was assessed or whether grazing was controlled across sites. Please clarify.
- Line 101: "space-for-time substitution" - this approach is used but the justification for assuming that sites represent a degradation trajectory needs more clarification.
- Line 107: The sampling design is described but the number of replicates and the randomization scheme should be clarified
- Lines 172-174: The statement that "non-degraded wetlands maintained substantially higher SWC, NH₄⁺-N, and MBN" is supported by the data in Table 1, but the declines are large (SWC from 0.45 to 0.14 m³·m³; MBN from 45.26 to 29.45 mg·kg⁻¹). The ecological implications of these magnitudes could be discussed more explicitly.