the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 22 Jun 2022
DMS cycling in the Sea Surface Microlayer in the South West Pacific: 2. Processes and Rates
Abstract. As the sea surface microlayer (SML) is the uppermost oceanic layer and differs in biogeochemical composition to the underlying subsurface water (SSW), it is important to determine whether processes in the SML modulate gas exchange, particularly for climate reactive gases. Enrichment of dimethyl sulfide (DMS) and its precursor dimethylsulfoniopropionate (DMSP) have been reported in the SML, but it remains unclear how this is maintained whilst DMS is lost to the atmosphere. To examine this, a comprehensive study of DMS source and sink processes, including production, consumption and net response to irradiance, were carried out in deck-board incubations of SML water at five locations in different water masses in the South West Pacific east of New Zealand. Net consumption of DMSP and production of DMS in the light and dark occurred at all sites. The net response of DMS and DMSP to irradiance varied between stations but was always lower than conversion of DMSP to DMS in the dark. In addition, DMS photolytic turnover was slower than reported elsewhere, which was unexpected given high light exposure in the SML incubations. Although no relationships were apparent between DMS process rates and biogeochemical variables, including chlorophyll-a, bacteria and phytoplankton group, net bacterial DMSP consumption was correlated with DMSP and DMS concentrations, and also dinoflagellate and Gymnodinium spp. biomass, supporting the findings of a companion study that dinoflagellates play an important role in DMS cycling in the SML. However, net DMS production rates and accumulation were low relative to calculated air-sea DMS loss, confirming that the DMS cycling within the SML is unlikely to influence regional DMS emissions.
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RC1: 'Comment on egusphere-2022-504', Anonymous Referee #1, 15 Jul 2022
Review of: ‘DMS cycling in the Sea Surface Microlayer in the South West Pacific: 2 Processes and Rates’
Alexia D. Saint-Macary, Andrew Marriner1, Stacy Deppeler, Karl Safi, Cliff S. Law
https://doi.org/10.5194/egusphere-2022-504
Synopsis
The reported study was undertaken as a component of the Sea2Cloud campaign onboard the R/V Tangaroa in the region of the Chatham Rise east of NZ. The objective was to examine physical and biogeochemical processes affecting the SML to determine if DMS/P enrichment occurs there and, if so, how this might modulate air-sea exchange of DMS. The overall conclusion derived from the time and location of this study was that DMS/P accumulation in the SML was minimal and apparently did not influence air-sea flux/emission of DMS.
General comments
The SML is the interfacial surface zone where exchange of trace gases between the ocean and the atmosphere takes place. This zone, which contains the bacterioneuston, is a zone where accumulation of dissolved organic substances can occur, leading to enhanced biological abundance, activity and metabolic turn-over. It is a zone that may undergo dynamic enrichment of organic carbon, suspended particulates and biofilm material compared to the underlying water. In lines 53-57 of the introduction it is explained that DMS/P may be enriched in the SML where it can be stabilised through adsorption with dissolved organic compounds. Adsorption of DMS/P to organic compounds may provide an answer to the question posed in lines 11-12 of the abstract as to how enrichment of DMS may occur in the SML while it is also lost to the atmosphere. Organics that are least hydrophilic will partition into the SML where they may chemically interact with DMS to produce weakly-bound complexes, thereby lowering the Henry’s law volatility constant of DMS while the adsorption complex exists. Over time, photolysis and microbial catabolism of the organic component of the DMS-organic complex may lead to delayed release of DMS. A natural mechanism such as this is analogous to the analytical technique described at L135 where DMS was adsorbed onto Tenax to be ‘held up’ for later release by thermal desorption.
Through a delayed release mechanism DMS may be enriched in the SML while also being exchanged to the atmosphere. In my opinion, studies of the SML would require co-measurement of dissolved organics because DMS/P is likely to be a function of the dissolved organics content in the SML. The organic component of the SML can be collectively measured in the form of TOC/DOC; data which is unfortunately absent from the on-board incubation experiments to accompany the DMS/P data. This is an oversight of the experimental design that I suggest is considered to be included in future SML research. Comparison of the SML off-shore at the mouth of an estuary rich in dissolved organics with an open ocean location such as the Chatham Rise is more likely to show significantly contrasting SML properties and air-sea DMS turn-over rates.
While this study reports some unique information about DMSP process rates in the SML (L241), a major limitation of the study is the low number of samples that were collected. It is good to see that this limitation of the SML incubation experiment is made clear to the reader in lines 147-148. Even though a number of SML physico-chemical variables were examined in the current study, the lack of replicate information in the form of duplicates six hours apart (T0 and T6) restricts the confidence that can be applied to the findings. Consequently, statements about observed correlations and what they imply need to be made with caution and words such as “confirms” (L 340) & “confirm” (L344) should be avoided. The statement “…the current study confirm that SML DMS enrichment is rare in the SW Pacific” (L344) is based on very limited data made at one location east of NZ in one season that may not be so at other locations at other times of the year in the broad study region. Walker et al., (2016) state that enrichment of DMS in the SML can be variable and is influenced by particular conditions. Given that the overall finding of this particular study contrasts with the report of Walker et al., (2016) from the same study region, caution needs to be exercised in the concluding statements of this report.
In the results and discussion there is detailed analysis of the DMS process rates and turnovers (defined in Table 2) for the three seawater types sampled; however, clear conclusions derived from this analysis are lacking. I would like to see a conclusion (section 5) added that provides concise findings from the complex analysis of data undertaken. Currently section 4.5 brings together some conclusion-like comments on air-sea emission and processes occurring in the SML but I would like to see a conclusion that summarises all the processes examined. On looking for conclusions I focussed on section 4.5. The statement ‘Air-sea emission was the dominant process controlling DMS concentration in the SML’ (L319) is inevitable regardless of whether DMS is enriched in the SML or not because seawater is supersaturated in DMS relative to the atmosphere which maintains the net flux of DMS from the ocean. The statement at L321-323 “Consequently, despite net DMS accumulation in the SML (Table 4), the significantly greater air-sea loss should deplete DMS in the SML and so prevent enrichment (Table 5)” does not take into consideration the possibility that DMS may interact with organics in the SML to temporarily lower its volatility leading to enrichment.
This report is identified as a companion to a more substantial part-1 report referred to as SâM1 that is under revision (L85-86). The many references to S-M1 for methodology (e.g. details about the new sipper collection technique, L101-103) and DMS flux results (L158, 205-207) and references to S-M1 throughout the discussion leave the reader wondering about aspects of the study that are not available. The publication status of S-M1 is unclear. Is it possible to include an Ocean Science manuscript number or information that it has been or will be accepted for publication at L452?
Specific comments
Abstract
L11. “active” makes more sense than “reactive”
L12. Please change “have” to “has”
Introduction
L25. Again, “active” makes more sense than “reactive”. Change to “natural sulfate aerosol precursor …”
L26. Please change to “that has been hypothesized to contribute to the regulation of climate ...”
L38. I suggest to say “largely influenced by phytoplankton type and density”
L53-54. This statement requires clarification; I suggest saying “The SML also contributes to possible climate regulation when air-sea exchanged trace gases are oxidised leading to secondary organic aerosol, which may influence atmospheric radiative properties”
L56-57. I suggest it would be better to say “due to stabilization by dissolved organic substances …”. Please clarify what the dissolved DMSP is adsorbed to. I presume it is the stabilised dissolved organic substances?
L67. what sort of “material”? particulate organic materials?
L76. Please say “a SML sink for DMS” to clarify the aquatic compartment referred to here.
L79. Comment: The net effect of these enhanced but opposing processes in the SML may cancel each other out, so they might not be particularly significant in the SML.
L86 and L224. Please make it clear that the Walker et al., (2016) report was also a “South West Pacific regional study”.
Method
L97-99. It is stated here that were six workboat deployments but information is not included for 6 stations in Table 1. If the workboat went out isn’t there a sampling time and data from the vessel sampling system for the parameters given in Table 1 for 5-STW? Even though there was no deck-board incubation carried out for station 5 (L107) the reader would expect to see data in Table 1. I suggest that L107 in the caption for Fig 1 and L114-115 are moved together into L97-99 to explain up front the circumstances for station 5 (STW).
L110. change “5-m” to “5 m”. Table 1; Please include the number of measurements (n=?) for each parameter. Add units for salinity (PSU?). Specify time zone (±? h UTC).
L118. Grammar here; “was placed” or “systems were placed”
L127. Please comment on if the DMDS analysed for DMS impurity?
L135. What type of Tenax? TA? TC?
L136. Please change “chromatography” to “chromatograph”. Was a chromatography column used? If so please specify the column type and the applied chromatographic conditions.
L139. It should be explained for those unfamiliar with the analytical approach that DMSP is base catalysed to DMS by the addition of alkali that allows DMSP to be indirectly measured in the form of DMS on a molar conversion basis.
L140. Please say “with analysis of the liberated DMS within 24 h ….”
L141. add “DMS” before “calibration”. Add “water” after “Milli-Q”. Was it an actual Millipore water system? If not, say “deionised water”.
L150. There is inconsistency in the description “net DMSP dark bacterial consumption rate,” with what is shown in Table 2.
L154. There is inconsistency in the description “net DMS dark bacterial consumption rate,” with what is shown in Table 2.
Table 2. Air-sea turnover in minutes is not shown to be so where turnover is (d).
Results
L169. For clarity please state that the “frontal station” are stations 1 & 2.
L180. I suggest to change “showed” to “was indicated”
L185. The shading in Fig 2 is confusing because shading is usually used to represent nighttime periods on plots. This is most confusing for Fig 4 where light and dark treatments are compared. I recommend that the shading is removed and the water mass types are separated by vertical dashed and/or dotted lines in Figs 2, 3 and 4.
L220. Fig 4 caption. Specify “set A (light)” and “set B (dark)” in the caption to improve clarity.
Please comment on the significance of the average values shown in Tables 3 &4.
Discussion
L233. Please define “EF DMS” here in the caption. Was EF previously defined? I presume it means enrichment factor?
L274. Define the “SOAP” experiment and where it was conducted.
L339. State the correlation value/s.
L340. This sentence is not clear, remove “play”. Can you really say the correlation ‘confirms’ that these particular phytoplankton were responsible for the observation given that there are many other marine organisms and factors in play in the SML that were not measured?
L344. Again, can you really say ‘confirms’ here based solely on your Sea2 Cloud campaign findings?
Acknowledgements
L346. Please check the spelling of Theresa B?
References
Some of the references have DOIs inserted but many do not. Please complete the referencing by including all available DOIs.
L457 appears to be out of place and requires revision.
Supplementary Information
The SI requires the same attention to detail as the manuscript.
Please include a title and authors heading for the SI document.
Fig S1 caption. Please provide a legend to explain each abbreviation and also specify what the different treatments are, and I recommend changing the shading to vertical dashed lines to avoid night/day confusion.
Citation: https://doi.org/10.5194/egusphere-2022-504-RC1 -
AC1: 'Reply on RC1', Alexia Saint-Macary, 13 Sep 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-504/egusphere-2022-504-AC1-supplement.pdf
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AC1: 'Reply on RC1', Alexia Saint-Macary, 13 Sep 2022
-
RC2: 'Comment on egusphere-2022-504', Anonymous Referee #2, 29 Aug 2022
Review for the article id egusphere-2022-504 titled “DMS cycling in the Sea Surface Microlayer in the South West Pacific: 2. Processes and Rates” by Saint-Macary et al.
In the manuscript, the authors have presented a study on DMS cycling in sea surface microlayer in the southwest pacific, east of New Zealand. In-situ observations were made over a fortnight in austral autumn at six stations, with incubation experiments carried out at five stations. The manuscript explains the observed changes in DMS and DMSP concentrations during the incubation experiments and explores the effect of other environmental factors such as irradiance, biological species composition, etc. The manuscript is well structured and although there are missing details and most sectional conclusions are speculative, the main outcome that DMSP and DMS cycling in the SML are insufficient to maintain DMS enrichment concurrent with elevated air-sea loss is an important result. I recommend that the paper be published condition to some changes as suggested below.
Major points:
- The incubation experiments are performed under three conditions (a) In presence of irradiance, (b) dark, and (c) dark with DMDS added. The effect of other environmental stressors is not clear. For example, the variation of irradiance between the sites is mentioned as an uncertainty mentioned later in the paper, but should be made clear that it is not considered in the methodology section. It is also not clear what the role of wind is when comparing the onboard experiment with the sea-air fluxes from paper 1. Although the authors mention that the enrichment would not explain the sea-air fluxes of DMS, the contribution factor would also depend on the local wind speed, would it not?
- A problem with drawing the main conclusion is the low sample size. Most of the conclusions are derived from just two datapoints per sample (T0 and T6) and hence the validity of the results over a larger number of datapoints, or over different timescales can be questioned. Considering the contrasting results from previous studies in the same study region, one wonders whether those results and the current results are biased by sampling issues. It would be better for the authors to explain more in detail the differences from the earlier studies and the drivers of these differences, rather than say that this study confirms the lack of SML DMS playing a major role in the sea-air flux.
- The observations are taken during the austral autumn. Are the results valid for other seasons? The role of light is clearly shown through the incubation experiments and hence there should be a larger effect during the other months, providing that the other parameters stay the same. However, the biogeochemistry of the area could also show a change. Hence the title could be more specific to point the season – for example, ‘DMS cycling in the Sea Surface Microlayer during Austral Autumn in the South West Pacific: 2. Processes and Rates’.
- The manuscript is dependent on the publication of the SM1 submitted manuscript. It is not just heavily referenced in this paper, but several details regarding the setup and analysis are missing assuming the publication of the first manuscript. This assumption also means that the manuscript should not be published unless the first one is published.
Minor points:
Considering this is a sister paper to the first one which is also in review, it would be useful for the reader to highlight in the abstract what the results are with respect to the paper part one and also include what are the main results from the first paper.
L110. Change “5-m” to “5 m”. Table 1; Specify time zone.
Including all available DOIs in the references – these details are missing in multiple places.
L339. What are the correlation values?
L233. Please define “EF DMS.”
Label set A (light) and set B (dark) in figure 4 for quick understanding.
Figures 2a and 2b, also in figures 3a and 3b please mention which set? (A, B, or C)
In figure 4, where is set C?
L59 consumption ‘is’ also elevated
L118 photosynthetic irradiance recording system was placed next to the deck
L135 DMS pre-concentration at −110 â on a Tenex® trap
L-163,164 Which data is the normally and non-normally distributed data used in this experiment? Please provide proof that it was normally and non-normally distributed considering the small number of samples.
L-218 sets A and B at each station, except for 3-SAW where it was higher in set B (dark).
L-338 current study, which is consistent with previous regional estimates
L-354 There are no conflicts of interest.
L-28 emission to the atmosphere is the net result of production and consumption by various biological, photochemical
L-70,71 which may, directly and indirectly, influence DMSP and DMS
L-78 light may enhance both DMS production and consumption, and so the net effect of these processes may be particularly significant in the SML
L-79 Although solar radiation dose is an important factor in determining temporal
L-95 The Sea2Cloud voyage took place from the 16 to 28 March 2020 (austral autumn)
L-110 an Automatic Weather Station measured windspeed, 25.2 m above the sea level
Figure 1., color bar title?
L-118 photosynthetic irradiance recording system was placed next to the deck
L-136, 137 The detector's daily sensitivity and detection limit were confirmed using VICI®
Highlight the most important results in tables 3, 4, and 5.
The following references can also be added to state the effect of nutrients, and various environmental factors on the production of DMS from DMSP and also for the production of DMSP.
- Interactions of anthropogenic stress factors on marine phytoplankton https://doi.org/10.3389/fenvs.2015.00014
- Production of atmospheric sulfur by ocean plankton: biogeochemical, ecological and evolutionary links DOI:1016/s0169-5347(01)02152-8
- Biogenic production of DMSP and its degradation to DMS – their roles in the global sulfur cycle DOI:1007/s11427-018-9524-y
Citation: https://doi.org/10.5194/egusphere-2022-504-RC2 -
AC2: 'Reply on RC2', Alexia Saint-Macary, 13 Sep 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-504/egusphere-2022-504-AC2-supplement.pdf
Interactive discussion
Status: closed
-
RC1: 'Comment on egusphere-2022-504', Anonymous Referee #1, 15 Jul 2022
Review of: ‘DMS cycling in the Sea Surface Microlayer in the South West Pacific: 2 Processes and Rates’
Alexia D. Saint-Macary, Andrew Marriner1, Stacy Deppeler, Karl Safi, Cliff S. Law
https://doi.org/10.5194/egusphere-2022-504
Synopsis
The reported study was undertaken as a component of the Sea2Cloud campaign onboard the R/V Tangaroa in the region of the Chatham Rise east of NZ. The objective was to examine physical and biogeochemical processes affecting the SML to determine if DMS/P enrichment occurs there and, if so, how this might modulate air-sea exchange of DMS. The overall conclusion derived from the time and location of this study was that DMS/P accumulation in the SML was minimal and apparently did not influence air-sea flux/emission of DMS.
General comments
The SML is the interfacial surface zone where exchange of trace gases between the ocean and the atmosphere takes place. This zone, which contains the bacterioneuston, is a zone where accumulation of dissolved organic substances can occur, leading to enhanced biological abundance, activity and metabolic turn-over. It is a zone that may undergo dynamic enrichment of organic carbon, suspended particulates and biofilm material compared to the underlying water. In lines 53-57 of the introduction it is explained that DMS/P may be enriched in the SML where it can be stabilised through adsorption with dissolved organic compounds. Adsorption of DMS/P to organic compounds may provide an answer to the question posed in lines 11-12 of the abstract as to how enrichment of DMS may occur in the SML while it is also lost to the atmosphere. Organics that are least hydrophilic will partition into the SML where they may chemically interact with DMS to produce weakly-bound complexes, thereby lowering the Henry’s law volatility constant of DMS while the adsorption complex exists. Over time, photolysis and microbial catabolism of the organic component of the DMS-organic complex may lead to delayed release of DMS. A natural mechanism such as this is analogous to the analytical technique described at L135 where DMS was adsorbed onto Tenax to be ‘held up’ for later release by thermal desorption.
Through a delayed release mechanism DMS may be enriched in the SML while also being exchanged to the atmosphere. In my opinion, studies of the SML would require co-measurement of dissolved organics because DMS/P is likely to be a function of the dissolved organics content in the SML. The organic component of the SML can be collectively measured in the form of TOC/DOC; data which is unfortunately absent from the on-board incubation experiments to accompany the DMS/P data. This is an oversight of the experimental design that I suggest is considered to be included in future SML research. Comparison of the SML off-shore at the mouth of an estuary rich in dissolved organics with an open ocean location such as the Chatham Rise is more likely to show significantly contrasting SML properties and air-sea DMS turn-over rates.
While this study reports some unique information about DMSP process rates in the SML (L241), a major limitation of the study is the low number of samples that were collected. It is good to see that this limitation of the SML incubation experiment is made clear to the reader in lines 147-148. Even though a number of SML physico-chemical variables were examined in the current study, the lack of replicate information in the form of duplicates six hours apart (T0 and T6) restricts the confidence that can be applied to the findings. Consequently, statements about observed correlations and what they imply need to be made with caution and words such as “confirms” (L 340) & “confirm” (L344) should be avoided. The statement “…the current study confirm that SML DMS enrichment is rare in the SW Pacific” (L344) is based on very limited data made at one location east of NZ in one season that may not be so at other locations at other times of the year in the broad study region. Walker et al., (2016) state that enrichment of DMS in the SML can be variable and is influenced by particular conditions. Given that the overall finding of this particular study contrasts with the report of Walker et al., (2016) from the same study region, caution needs to be exercised in the concluding statements of this report.
In the results and discussion there is detailed analysis of the DMS process rates and turnovers (defined in Table 2) for the three seawater types sampled; however, clear conclusions derived from this analysis are lacking. I would like to see a conclusion (section 5) added that provides concise findings from the complex analysis of data undertaken. Currently section 4.5 brings together some conclusion-like comments on air-sea emission and processes occurring in the SML but I would like to see a conclusion that summarises all the processes examined. On looking for conclusions I focussed on section 4.5. The statement ‘Air-sea emission was the dominant process controlling DMS concentration in the SML’ (L319) is inevitable regardless of whether DMS is enriched in the SML or not because seawater is supersaturated in DMS relative to the atmosphere which maintains the net flux of DMS from the ocean. The statement at L321-323 “Consequently, despite net DMS accumulation in the SML (Table 4), the significantly greater air-sea loss should deplete DMS in the SML and so prevent enrichment (Table 5)” does not take into consideration the possibility that DMS may interact with organics in the SML to temporarily lower its volatility leading to enrichment.
This report is identified as a companion to a more substantial part-1 report referred to as SâM1 that is under revision (L85-86). The many references to S-M1 for methodology (e.g. details about the new sipper collection technique, L101-103) and DMS flux results (L158, 205-207) and references to S-M1 throughout the discussion leave the reader wondering about aspects of the study that are not available. The publication status of S-M1 is unclear. Is it possible to include an Ocean Science manuscript number or information that it has been or will be accepted for publication at L452?
Specific comments
Abstract
L11. “active” makes more sense than “reactive”
L12. Please change “have” to “has”
Introduction
L25. Again, “active” makes more sense than “reactive”. Change to “natural sulfate aerosol precursor …”
L26. Please change to “that has been hypothesized to contribute to the regulation of climate ...”
L38. I suggest to say “largely influenced by phytoplankton type and density”
L53-54. This statement requires clarification; I suggest saying “The SML also contributes to possible climate regulation when air-sea exchanged trace gases are oxidised leading to secondary organic aerosol, which may influence atmospheric radiative properties”
L56-57. I suggest it would be better to say “due to stabilization by dissolved organic substances …”. Please clarify what the dissolved DMSP is adsorbed to. I presume it is the stabilised dissolved organic substances?
L67. what sort of “material”? particulate organic materials?
L76. Please say “a SML sink for DMS” to clarify the aquatic compartment referred to here.
L79. Comment: The net effect of these enhanced but opposing processes in the SML may cancel each other out, so they might not be particularly significant in the SML.
L86 and L224. Please make it clear that the Walker et al., (2016) report was also a “South West Pacific regional study”.
Method
L97-99. It is stated here that were six workboat deployments but information is not included for 6 stations in Table 1. If the workboat went out isn’t there a sampling time and data from the vessel sampling system for the parameters given in Table 1 for 5-STW? Even though there was no deck-board incubation carried out for station 5 (L107) the reader would expect to see data in Table 1. I suggest that L107 in the caption for Fig 1 and L114-115 are moved together into L97-99 to explain up front the circumstances for station 5 (STW).
L110. change “5-m” to “5 m”. Table 1; Please include the number of measurements (n=?) for each parameter. Add units for salinity (PSU?). Specify time zone (±? h UTC).
L118. Grammar here; “was placed” or “systems were placed”
L127. Please comment on if the DMDS analysed for DMS impurity?
L135. What type of Tenax? TA? TC?
L136. Please change “chromatography” to “chromatograph”. Was a chromatography column used? If so please specify the column type and the applied chromatographic conditions.
L139. It should be explained for those unfamiliar with the analytical approach that DMSP is base catalysed to DMS by the addition of alkali that allows DMSP to be indirectly measured in the form of DMS on a molar conversion basis.
L140. Please say “with analysis of the liberated DMS within 24 h ….”
L141. add “DMS” before “calibration”. Add “water” after “Milli-Q”. Was it an actual Millipore water system? If not, say “deionised water”.
L150. There is inconsistency in the description “net DMSP dark bacterial consumption rate,” with what is shown in Table 2.
L154. There is inconsistency in the description “net DMS dark bacterial consumption rate,” with what is shown in Table 2.
Table 2. Air-sea turnover in minutes is not shown to be so where turnover is (d).
Results
L169. For clarity please state that the “frontal station” are stations 1 & 2.
L180. I suggest to change “showed” to “was indicated”
L185. The shading in Fig 2 is confusing because shading is usually used to represent nighttime periods on plots. This is most confusing for Fig 4 where light and dark treatments are compared. I recommend that the shading is removed and the water mass types are separated by vertical dashed and/or dotted lines in Figs 2, 3 and 4.
L220. Fig 4 caption. Specify “set A (light)” and “set B (dark)” in the caption to improve clarity.
Please comment on the significance of the average values shown in Tables 3 &4.
Discussion
L233. Please define “EF DMS” here in the caption. Was EF previously defined? I presume it means enrichment factor?
L274. Define the “SOAP” experiment and where it was conducted.
L339. State the correlation value/s.
L340. This sentence is not clear, remove “play”. Can you really say the correlation ‘confirms’ that these particular phytoplankton were responsible for the observation given that there are many other marine organisms and factors in play in the SML that were not measured?
L344. Again, can you really say ‘confirms’ here based solely on your Sea2 Cloud campaign findings?
Acknowledgements
L346. Please check the spelling of Theresa B?
References
Some of the references have DOIs inserted but many do not. Please complete the referencing by including all available DOIs.
L457 appears to be out of place and requires revision.
Supplementary Information
The SI requires the same attention to detail as the manuscript.
Please include a title and authors heading for the SI document.
Fig S1 caption. Please provide a legend to explain each abbreviation and also specify what the different treatments are, and I recommend changing the shading to vertical dashed lines to avoid night/day confusion.
Citation: https://doi.org/10.5194/egusphere-2022-504-RC1 -
AC1: 'Reply on RC1', Alexia Saint-Macary, 13 Sep 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-504/egusphere-2022-504-AC1-supplement.pdf
-
AC1: 'Reply on RC1', Alexia Saint-Macary, 13 Sep 2022
-
RC2: 'Comment on egusphere-2022-504', Anonymous Referee #2, 29 Aug 2022
Review for the article id egusphere-2022-504 titled “DMS cycling in the Sea Surface Microlayer in the South West Pacific: 2. Processes and Rates” by Saint-Macary et al.
In the manuscript, the authors have presented a study on DMS cycling in sea surface microlayer in the southwest pacific, east of New Zealand. In-situ observations were made over a fortnight in austral autumn at six stations, with incubation experiments carried out at five stations. The manuscript explains the observed changes in DMS and DMSP concentrations during the incubation experiments and explores the effect of other environmental factors such as irradiance, biological species composition, etc. The manuscript is well structured and although there are missing details and most sectional conclusions are speculative, the main outcome that DMSP and DMS cycling in the SML are insufficient to maintain DMS enrichment concurrent with elevated air-sea loss is an important result. I recommend that the paper be published condition to some changes as suggested below.
Major points:
- The incubation experiments are performed under three conditions (a) In presence of irradiance, (b) dark, and (c) dark with DMDS added. The effect of other environmental stressors is not clear. For example, the variation of irradiance between the sites is mentioned as an uncertainty mentioned later in the paper, but should be made clear that it is not considered in the methodology section. It is also not clear what the role of wind is when comparing the onboard experiment with the sea-air fluxes from paper 1. Although the authors mention that the enrichment would not explain the sea-air fluxes of DMS, the contribution factor would also depend on the local wind speed, would it not?
- A problem with drawing the main conclusion is the low sample size. Most of the conclusions are derived from just two datapoints per sample (T0 and T6) and hence the validity of the results over a larger number of datapoints, or over different timescales can be questioned. Considering the contrasting results from previous studies in the same study region, one wonders whether those results and the current results are biased by sampling issues. It would be better for the authors to explain more in detail the differences from the earlier studies and the drivers of these differences, rather than say that this study confirms the lack of SML DMS playing a major role in the sea-air flux.
- The observations are taken during the austral autumn. Are the results valid for other seasons? The role of light is clearly shown through the incubation experiments and hence there should be a larger effect during the other months, providing that the other parameters stay the same. However, the biogeochemistry of the area could also show a change. Hence the title could be more specific to point the season – for example, ‘DMS cycling in the Sea Surface Microlayer during Austral Autumn in the South West Pacific: 2. Processes and Rates’.
- The manuscript is dependent on the publication of the SM1 submitted manuscript. It is not just heavily referenced in this paper, but several details regarding the setup and analysis are missing assuming the publication of the first manuscript. This assumption also means that the manuscript should not be published unless the first one is published.
Minor points:
Considering this is a sister paper to the first one which is also in review, it would be useful for the reader to highlight in the abstract what the results are with respect to the paper part one and also include what are the main results from the first paper.
L110. Change “5-m” to “5 m”. Table 1; Specify time zone.
Including all available DOIs in the references – these details are missing in multiple places.
L339. What are the correlation values?
L233. Please define “EF DMS.”
Label set A (light) and set B (dark) in figure 4 for quick understanding.
Figures 2a and 2b, also in figures 3a and 3b please mention which set? (A, B, or C)
In figure 4, where is set C?
L59 consumption ‘is’ also elevated
L118 photosynthetic irradiance recording system was placed next to the deck
L135 DMS pre-concentration at −110 â on a Tenex® trap
L-163,164 Which data is the normally and non-normally distributed data used in this experiment? Please provide proof that it was normally and non-normally distributed considering the small number of samples.
L-218 sets A and B at each station, except for 3-SAW where it was higher in set B (dark).
L-338 current study, which is consistent with previous regional estimates
L-354 There are no conflicts of interest.
L-28 emission to the atmosphere is the net result of production and consumption by various biological, photochemical
L-70,71 which may, directly and indirectly, influence DMSP and DMS
L-78 light may enhance both DMS production and consumption, and so the net effect of these processes may be particularly significant in the SML
L-79 Although solar radiation dose is an important factor in determining temporal
L-95 The Sea2Cloud voyage took place from the 16 to 28 March 2020 (austral autumn)
L-110 an Automatic Weather Station measured windspeed, 25.2 m above the sea level
Figure 1., color bar title?
L-118 photosynthetic irradiance recording system was placed next to the deck
L-136, 137 The detector's daily sensitivity and detection limit were confirmed using VICI®
Highlight the most important results in tables 3, 4, and 5.
The following references can also be added to state the effect of nutrients, and various environmental factors on the production of DMS from DMSP and also for the production of DMSP.
- Interactions of anthropogenic stress factors on marine phytoplankton https://doi.org/10.3389/fenvs.2015.00014
- Production of atmospheric sulfur by ocean plankton: biogeochemical, ecological and evolutionary links DOI:1016/s0169-5347(01)02152-8
- Biogenic production of DMSP and its degradation to DMS – their roles in the global sulfur cycle DOI:1007/s11427-018-9524-y
Citation: https://doi.org/10.5194/egusphere-2022-504-RC2 -
AC2: 'Reply on RC2', Alexia Saint-Macary, 13 Sep 2022
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2022/egusphere-2022-504/egusphere-2022-504-AC2-supplement.pdf
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Alexia D. Saint-Macary
Andrew Marriner
Stacy Deppeler
Karl Safi
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