the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Drivers of CO2 emissions during the dry phase of Mediterranean and Temperate ponds
Abstract. Pond ecosystems play an important role in the global carbon cycle with the potential to act as both sinks and sources. Emissions of CO2 during their dry phases remain largely overlooked, despite growing evidence that climate change-induced shifts in temperature and precipitation will likely result in longer and more frequent dry periods. Here we assess CO2 emissions from dry pond sediments in relation to climatic region, seasonal changes, and hydroperiod duration. Specifically, we aimed to identify the key environmental drivers shaping CO2 fluxes during the dry phase. We measured CO2 emissions from air-exposed sediments in 30 ponds across Mediterranean and Temperate regions. Ponds acted as sources of CO2 during dry phases, with emissions ranging from 127 to 4889 mg C m⁻² d⁻¹ (mean ± SD = 1398 ± 1201). Although mean emissions did not differ significantly between climate regions, hydroperiod length interacted with climate and season, showing a significant effect in summer, particularly in Mediterranean ponds, where longer hydroperiods led to higher emissions. Emissions were considerably higher in summer than in autumn, primarily driven by an interaction between sediment temperature and water content. The highest fluxes occurred at c. 27 °C and sediment water content between 27 % and 44 %. Additionally, ponds in better conservation status and with lower carbonate content emitted more CO2. Our findings improve understanding of CO2 emissions during increasingly common dry phases and highlight how climate modulates local sediment conditions, thereby influencing the magnitude of these emissions. This underscores the need for comprehensive assessments of carbon fluxes that incorporate dry-phase emissions, accounting for climate, hydroperiod, and both direct and indirect effects of local environmental drivers.
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Status: open (until 06 Nov 2025)
- RC1: 'Comment on egusphere-2025-3725', Anonymous Referee #1, 26 Sep 2025 reply
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RC2: 'Comment on egusphere-2025-3725', Ji-Hyung Park, 09 Oct 2025
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Please note that this referee report is provided by Associate Editor to expedite the delayed review process.
General comments
The manuscript presents two-season field measurements of CO₂ emissions from air-exposed sediments in 30 ponds across Mediterranean and temperate climate zones. Based on the significant relationship between hydroperiod lengths and CO2 emissions in Mediterranean ponds in summer, the authors suggest that longer hydroperiods play a critical role in creating temporary conditions for higher CO2 emissions. Using various statistical approaches, they further identified key drivers of sediment CO2 emissions, including temperature and sediment contents of water and carbonate. The key findings from the well-designed study are novel and invite further study to elucidate the large temporal variability in CO2 emissions from ponds, which have been understudied compared to other freshwater systems. Despite the novelty and significance of the key findings, the manuscript shows weakness in linking and interpreting these findings, as well as a lack of detail in several areas, as described below. I hope my comments will help the authors improve the logical flow and clarity of the manuscript.
1. Hypotheses and data interpretation
Although hydroperiods and sediment water contents are suggested as the primary controls on sediment CO2 emissions, descriptions across Introduction, Results, and Discussion appear not consistent, and in some cases contradictory. First, hypotheses (2) and (3) need to provide more interrelated and mechanistic predictions. Higher sediment contents might be influenced more directly by more recent precipitation events (like 1-month or 1-week antecedent precipitation) than the yearly hydroperiod as considered here. Please provide a more detailed explanation of the relationship between hydroperiods and water contents. Any rationale for using hydroperiod rather than other drought indices would also be helpful. Second, the findings shown in Fig. 4 indicate the significant relationship between hydroperiods and CO2 emissions only for Mediterranean ponds in summer, and the significance appears controlled by a few sites with very long hydroperiods. However, this hydroperiod effect is emphasized too much across the R & D sections, with some of them having inconsistent connotations: for instance, refer to L 275-276 (“Mediterranean ponds exhibited higher air and sediment temperatures, shorter hydroperiods, typically drying in summer. They also showed lower sediment water content, and reduced macrophyte coverage, consistent with an earlier drying period.”). Please check the consistency of descriptions across R & D (sections 4.1 and 4.2 appear to address two separate stories regarding the hydroperiod effect) to provide a more coherent explanation for the relationship between hydroperiods and sediment water contents.
2. Realigning paragraphs
Although the manuscript was easy to follow on a sentence-by-sentence level, the use of very long or several scattered short paragraphs made it difficult to grasp the overall logical structure. In the Introduction, for example, the page-long initial paragraph is followed by five short paragraphs. A thorough revision of the manuscript is recommended to reorganize the long and short paragraphs in accordance with a coherent logical flow.
3. Clarity of tables and figures
There are numerous missing or inaccurate details that could be improved through careful revision. Please refer to the specific comments below.
Specific comments
- Title: A slight change would enhance clarity: for example, Drivers of CO2 emissions during the dry phase “in” Mediterranean and Temperate ponds or Drivers of CO2 emissions “from” Mediterranean and Temperate ponds “during the dry phase”
- Line (L) 17: sources of carbon (or CO2)?
- L 17 “remain largely overlooked”: This statement overlooks the decadal research on this topic.
- L 25: “the” interaction
- L 35-38: Please provide some estimates of CO2 and CH4 emissions from ponds to describe their role more quantitatively.
- L 85: Please define “hydroperiod length”.
- L 96: Without the above-mentioned definition, it is difficult to understand “shorter hydroperiods leading to lower emissions due to reduced sediment water content”.
- L 99: Can you illustrate “conservation status” using an example?
- L 117: Did 23 sites also include semi-permanent and permanent ponds? In the latter case, the described bare sediment would be contradictory to the definition of permanent ponds (L 110).
- L 130 “water presence”: Do you mean rainy days or literal water presence in ponds?
- L 154 (throughout the manuscript): not Chlorophyll a, but chlorophyll a
- L 167: Please provide key details on the chamber design, including the used material, size, ventilation, etc.
- L 174-177: It would provide useful information for assessing the accuracy of sensor data if you compare sensor and additional GC measurements.
- L 195: Please provide a relevant reference for this carbonation estimation.
- L 224: How did you test the normal distribution of your datasets?
- L 265: Are these negative values from partially water-flooded sediments where phytoplankton take up CO2? Please elaborate on the site characteristics and discuss the meaning of these values (if outside measurement error ranges).
- L 284-286: Please clarify whether you are talking about the proportion of each component based on unit mass of sediment or DOC.
- L 288-293: These sentences are good examples of unnecessary separation mentioned before.
- L 300: Given the significance of the hydroperiod effect, it would be helpful to elaborate more as to how “the effect of hydroperiod was season-specific and climate-dependent” as displayed in Fig 4.
- L 301: Was the summer trend also significant for the temperate sites?
- L 320-330: In a sense, this part seems secondary, but covers the bulk of section 3.2. More space could be saved for more relevant drivers.
- L 354 “all ponds emitted CO₂ during the dry phase”: This statement is contradictory to the result descriptions (Fig. 2).
- L 357: “shaped” or “was shaped by”?
- L 445: It would help readers to compare the magnitudes of plant uptake vs. CO2 emissions if you provide some literature values estimating plant C uptake.
- L 417: Fig 5 shows the generally highest levels of CO2 emissions across the highest temperature ranges.
- L 460 “ponds with more permanent hydroperiod”: This is quite confusing, given your descriptions of your sites. Did you mean simply “longer hydroperiod”?
- Fig 1 caption: Countries “are”
- Fig 2: Please complete the vertical axis title with the second parenthesis.
- Table 2: If this displays the same data as Fig 2, please think about removing or revising it to avoid double presentation.
- Fig 4: Please indicate the significance levels for the depicted regressions. It would be easier to find out the significance if only significant regressions were shown as regression lines.
- Tables 3, 4, 5: Please explain in the caption the abbreviations including SE, df, CL, AIC, BIC, and CI.
- 5: What is ORQ? Are all the depicted trends statistically significant?
- Table 5: What about showing the employed models in a separate column?
- Table “6” (page 18): Please also correct the unnecessary values below the decimal point.
Citation: https://doi.org/10.5194/egusphere-2025-3725-RC2
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Review of the manuscript “Drivers of CO2 emissions during the dry phase of Mediterranean and Temperate ponds” by Frutos-Aragón et. al for Biogeosciences:
The study examines CO₂ fluxes of dry sediments from 14 temperate and 16 Mediterranean ponds in Europe during their dry phase in summer and/or autumn of 2022. These fluxes were measured using chambers. Additionally, sediment and water analyses were conducted to characterize the sites and to investigate the differences.
I read the manuscript with great interest and believe that the study is promising, but that some improvements are necessary.
General comments or questions:
Detailed comments and suggestions: