Articles | Volume 23, issue 19
https://doi.org/10.5194/bg-23-7043-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Precision of phytoplankton pigment analysis by high-performance liquid chromatography: an assessment of the global ocean color validation dataset analyzed by NASA
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- Final revised paper (published on 08 Oct 2026)
- Preprint (discussion started on 26 Mar 2026)
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-2026-1540', Anonymous Referee #1, 24 Apr 2026
- AC1: 'Reply on RC1', Joaquin Chaves, 22 Jun 2026
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RC2: 'Comment on egusphere-2026-1540', Anonymous Referee #2, 26 Apr 2026
- AC2: 'Reply on RC2', Joaquin Chaves, 22 Jun 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Submit a revised manuscript (30 Jun 2026) by Koji Suzuki
AR by Joaquin Chaves on behalf of the Authors (29 Jul 2026)
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ED: Referee Nomination & Report Request started (31 Jul 2026) by Koji Suzuki
RR by Anonymous Referee #3 (18 Aug 2026)
ED: Publish subject to minor revisions (review by editor) (22 Aug 2026) by Koji Suzuki
AR by Joaquin Chaves on behalf of the Authors (04 Sep 2026)
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ED: Reconsider after major revisions (11 Sep 2026) by Koji Suzuki
ED: Publish subject to minor revisions (review by editor) (23 Sep 2026) by Koji Suzuki
AR by Joaquin Chaves on behalf of the Authors (24 Sep 2026)
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ED: Publish as is (25 Sep 2026) by Koji Suzuki
AR by Joaquin Chaves on behalf of the Authors (29 Sep 2026)
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Review: “Precision of Phytoplankton Pigment Analysis by High Performance Liquid Chromatography: An Assessment of the Global Ocean Color Validation Dataset Analyzed by NASA” by Chaves et al.
This manuscript presents a comprehensive assessment of replicate-sample precision for phytoplankton pigment measurements obtained by HPLC. The authors make use of a very large and unique global dataset collected from 2011–2022 and provide a rigorous evaluation of analytical precision of pigments relevant to ocean color calibration and validation activities.
The article is clearly written, methodologically sound, and relevant in the context of prior SeaHARRE intercomparison exercises. The results show that the precision benchmarks for total chlorophyll a and most primary pigments are met, and that variability is dominated by pre-analytical and sampling-related factors rather than instrumental/analytical limitations. Overall, the manuscript is scientifically strong and represents a valuable contribution to the ocean color validation and phytoplankton pigment analysis and I recommend publication after a minor revision.
General comments:
Please provide information on the reporting practices, particularly for concentrations near LOD/LOQ, and on the number of significant digits reported. I am also missing an evaluation of how many datasets actually had CV=0%, and how many of these cases were associated with measurements at or below LOD/LOQ. Furthermore, please clarify how such numbers were reported: were concentrations replaced by LOD/LOQ values, e.g., 0.0001, or were zeros reported when pigments were not detected? This information is important for understanding the procedure used to exclude samples with invariant replicates (CV=0%).
Chlide a generally results from artificial degradation of Chl a during extraction and should therefore be added to Chl a. Since most Chlide a quantified by HPLC is not natural occurring it should not be interpreted independently and I suggest removing Chlide a from the figures and most of the text (see a later comment on it).
Specific comments:
L.80: “In the absence of standardized reference materials… intercalibrations are a necessary substitute”?: The use of standardized reference materials and participation in intercalibrations are complementary activities and should both be applied, where possible, to ensure robust quality assurance.
L. 110: one ancillary pigment? Which pigment? It is evident from Table 1. Also, the text states “two sets of pigment sums and ratios routinely reported”; however, Table 1 shows more than two pigment sums and no ratios. Please correct the text/table.
L. 114: “Tertiary pigments are a set of less frequently analyzed pigments” -less frequently reported pigments?
L. 114: Why specifically mention gyroxanthin diester (which is often present in certain regions) while other omitted pigments are not mentioned (dinoxanthin, myxoxanthophyll, C2-MGDG, etc.)?
L. 131: Please specify the extraction solvent (e.g. 90% acetone).
L. 144: 30,000 samples mentioned in the introduction?
L. 190: Correct “pigmen” to pigment.
Table 1: Correct Pheophtyin a to Pheophytin a.
L. 128: “a reference wavelength of 700 nm was added” Do you mean: “…a reference wavelength at 700 nm (±10 nm) was included and used for baseline correction of the 665 nm signal”?
L. 250, Fig. 2d: What is the rationale for comparing satellite data from 2002-2023 to TChl a from 2011-2022? Could the offset observed in Fig. 2d partly reflect the difference in time periods?
L. 257: Can you elaborate on why Diato and Perid in particular exceed the 8 % benchmark? Possible factors could include broad peaks, co‑elution, or generally small peak areas. Please expand on this in the discussion.
L. 293: (CV % >0 (excluding invariant replicates). One ”)” is missing.
Fig. 5, 6, and 7: It is difficult to see the details, especially the white lines. Can the figures be enlarged?
L. 383: As mentioned earlier, Chlide a is (mostly) an artifactual product from chlorophyll a formed during extraction due to water content in acetone. I suggest briefly describing this with references and then remove chlorophyllide a from the article (it would still be included in TChl a).
L. 400: “Volumes below 200 mL showed precision degradation in our dataset”: refer to Fig. 7? Where can it be seen that there will be minimal additional precision benefit above 1 L in high biomass waters?
L .430: “.The divergent behavior at high filtration volumes, where precision degrades despite greater sample volume, supports the interpretation that physical stresses during extended filtration (e.g., cell lysis, filter overloading) compound the natural heterogeneity already present”. When filtering large volumes in low Chl a concentration (oligotrophic) regions, e.g. 4-5000 mL, many pigments (e.g., prasinoxanthin, neoxanthin, lutein, alloxanthin) from algal species not abundant in these areas will still be detected near their LOD/LOQ, which means that there will be increased uncertainty on the determination of the peak areas. While natural pigment concentrations span ~4 orders of magnitude, the filtered volumes do not.
L. 447: At least part of the explanation may again relate to low cell numbers and the higher uncertainty associated with very small pigment peaks from sparsely represented taxa.
L. 452-455: Please provide further details on reporting practices near the LOD/LOQ (see general comments).
L. 463: The statement that larger filtration volumes reduce relative measurement error in oligotrophic environments is not clearly supported for all pigments in Fig. 7, although it may hold if even larger volumes were filtered (acknowledging practical limitations).
L. 479: iSeaHARRE-5 – should ”in” be added?
L. 487-which methodological factors are referred to here (e.g., calibration, peak-area integration)?
L. 503. Chlorophyllide a should not be mentioned here, as it is an extraction artefact (see comments above).