Precision of Phytoplankton Pigment Analysis by High Performance Liquid Chromatography: An Assessment of the Global Ocean Color Validation Dataset Analyzed by NASA
Abstract. Space-borne ocean color sensors capable of measuring phytoplankton pigments, such as chlorophyll a, have greatly expanded our understanding of oceanic biological processes. The ability to generate such measurements in a way that satisfies the requirements of climate-quality data records is contingent in part on the quality of the in situ ground or sea truth observations that serve as datasets for vicarious calibration and algorithm validation activities. The National Aeronautics and Space Administration (NASA) has a mandate to collect and distribute in situ data of the highest quality to support data product validation for ocean color missions; hence the agency uses a centralized, quality-assured laboratory to perform high performance liquid chromatography (HPLC) analysis of pigment samples collected by NASA-affiliated investigators. Since its establishment in 2011, the facility at NASA’s Goddard Space Flight Center has processed over 30,000 samples collected in all the major ocean basins. We evaluated the replicate sample precision, measured as the percent coefficient of variation among replicates, for total chlorophyll a and all primary, secondary, and tertiary pigments to investigate the sources of variability in analytical measurements. Mean analytical precision (CV %) ranged from 3.2 % for divinyl chlorophyll a to 17.1 % for chlorophyllide a. The analytical precision performance benchmarks for total chlorophyll a (5 %) and primary pigments (8 %), established for legacy ocean color missions, were met for total chlorophyll a and for 10 of 12 primary pigments. Two primary pigments exceeded the 8 % benchmark: diatoxanthin (8.6 %) and peridinin (9.2 %). No performance benchmarks have been established for secondary or tertiary pigments. Precision was evaluated against average sample concentration, pigment mass injected into the HPLC instrument, filtered volume, estimated phytoplankton size-fractions (micro-, nano-, and picoplankton), and sample origin (coastal versus oceanic) using multivariate regression and non-parametric approaches. Neither concentration nor pigment mass appeared as significant drivers of precision variability across their ranges. Precision showed minimal variation across concentration ranges for total chlorophyll a and primary pigments but deteriorated toward detection limits for secondary and tertiary pigments when samples with invariant replicates (CV % = 0) were excluded from analysis. Filtration volumes >1000 mL generally improved precision, though it degraded at higher volumes for some pigments in censored datasets, suggesting physical stresses during extended filtration. For most pigments, sample precision was statistically poorer in coastal versus oceanic samples, though previous interlaboratory comparisons suggest this reflects methodological rather than biogeochemical factors. Multivariate regression models explained ≤ 3.0 % of precision variability in full datasets but up to 44 % when invariant replicates were excluded, indicating that analytical precision is primarily governed by methodological factors rather than systematic dependencies on sample characteristics. The distinction between analytical precision and sample heterogeneity emerged as a possible factor, with increased variability at low concentrations for rare taxa likely reflecting stochastic cell capture during filtration rather than analytical limitations. These findings demonstrate that rigorous quality assurance protocols achieve precision performance suitable for climate-quality ocean color validation, with pre-analytical sample processing and field replication strategies identified as priorities for further improvements.
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).