Articles | Volume 23, issue 10
https://doi.org/10.5194/bg-23-3499-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Heavy precipitation-induced Yangtze River runoff greatly regulates heterotrophic prokaryotes production and induces P-limited growth in the northern East China Sea
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- Final revised paper (published on 21 May 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 25 Sep 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-2025-4211', Anonymous Referee #1, 13 Oct 2025
- AC1: 'Reply on RC1', Yong-Jae Baek, 14 Feb 2026
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RC2: 'Comment on egusphere-2025-4211', Anonymous Referee #2, 08 Dec 2025
- AC2: 'Reply on RC2', Yong-Jae Baek, 14 Feb 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Reconsider after major revisions (24 Feb 2026) by Liuqian Yu
AR by Yong-Jae Baek on behalf of the Authors (04 Mar 2026)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (05 Mar 2026) by Liuqian Yu
RR by Anonymous Referee #2 (18 Mar 2026)
RR by Anonymous Referee #1 (21 Mar 2026)
ED: Publish subject to technical corrections (26 Mar 2026) by Liuqian Yu
AR by Yong-Jae Baek on behalf of the Authors (31 Mar 2026)
Author's response
Manuscript
General comments
This manuscript presents a valuable three-year dataset (2020-2022) exploring how heavy precipitation and the resulting YRDW influence microbial carbon dynamics in the nECS. The authors integrate satellite-based salinity, PP, HPP, and FDOM measurements with nutrient-addition bioassays. The topic is timely and relevant to Biogeosciences, addressing the interaction between hydrological forcing and microbial processes in marginal seas.
The manuscript is well organized and clearly written, and the field observations are impressive in scope. However, several aspects of the analysis and interpretation require further clarification before the conclusions can be fully supported. In particular, the paper tends to extend beyond the range of the presented evidence, and the causal links between precipitation, DOM quality, and microbial carbon partitioning are not fully demonstrated.
I outline below the main points that, in my view, require attention:
1.The paper draws a direct causal chain from precipitation and YRDW variability to microbial carbon partitioning and trophic balance. While the correlation between hydrological forcing and microbial parameters is evident, the discussion extrapolates local observational patterns to ecosystem-scale mechanisms (e.g., "enhanced microbial loop and reduced food-web efficiency") without direct process measurements of carbon transfer (e.g., respiration or bacterial growth efficiency).
The authors are encouraged to clarify which interpretations are empirically supported and which remain conceptual or inferential. This distinction will help strengthen the credibility of the conclusions.
2. The use of the HPP:PP ratio as an indicator of microbial loop intensity is informative but limited. Without concurrent measurements of respiration or BGE, this ratio reflects only relative production rates rather than the efficiency of carbon transfer or sequestration. The authors briefly acknowledge this point in the manuscript, but a more explicit discussion in the main text would strengthen the interpretation and clarify the limitations of using HPP:PP as a mechanistic indicator.
3. The manuscript would benefit from a better balance between the Results and Discussion sections. The results are presented rather succinctly, whereas the discussion is extensive and mechanism-oriented. Presenting slightly more quantitative detail in the Results—especially regarding interannual trends and variability—would make the argumentation in the Discussion easier to follow and more persuasive.
4. The study attributes seasonal variability of HPP mainly to precipitation and phosphorus limitation. However, temperature, grazing pressure, or water-column stability may also influence microbial activity. A brief discussion acknowledging these potential co-drivers would provide a more balanced interpretation.
5. The nutrient-limitation bioassay (Fig. 7) is compelling; however, the differences between 12-h and 26.5-h incubations could affect comparability. Please discuss potential bias due to unequal incubation times.
Minor comments
1. It would be helpful to clarify whether HPP and PP were measured concurrently at the same sampling stations. If not, a short note on how this may affect the interpretation of HPP:PP ratios would be valuable.
2. The authors might consider adding a simple schematic summarizing how YRDW affects nutrient stoichiometry, DOM composition, and microbial carbon flow.
3. In the Conclusion, tone down generalizations such as “greatly regulates” or “strongly enhances”.
4. The use of 0.2 μm filtration followed by a 9:1 mixture of filtered and unfiltered seawater seems appropriate for reducing grazing while preserving the original bacterial assemblage. Still, the rationale could be clarified briefly in the Methods to help readers understand the intention behind this experimental setup.
Technical corrections
The panel labels (A–L) in Figure 1 seem unnecessary, as they are not mentioned in the main text. Consider removing them or clarifying their meaning in the caption.