Abstract
Throughout their species seasonal succession, diatoms of the Arctic Ocean experience a radical habitat transformation, from surviving the dimly lit winter within sea-ice or in the water column, to rapid growth under increasing irradiances, forming massive spring blooms beneath melting ice and later in open waters. Therefore, their evolutionary path has been moulded by the opposing challenges of maximizing light capture part of the year while maintaining highly efficient photoprotection capacities to limit photodamage upon bursts of supra-optimal illumination. Two main photoprotection mechanisms exist in diatoms i) nonphotochemical quenching (NPQ) supported primarily by the xanthophyll cycle (XC) and stress-related Lhcx antenna proteins and, ii) a rapid repair cycle of photosystem (PS) II core protein, PsbA, upon photodamage. Previous studies suggest that freezing temperatures slow protein turnover and favour photoprotection strategies that rely primarily upon XC-NPQ in polar taxa. We aim to revisit this hypothesis by dissecting the high-light response of five Arctic diatom species that dominate contrasting ecological niches: sea-ice, marginal ice-zone and open waters. We exposed each species to a high-light stress and subsequent recovery period under low light, with and without, inhibitors of XC-NPQ (dithiothreitol) or of plastid protein translation (lincomycin), blocking de novo replacement of PsbA. We confirmed the crucial role of XC-NPQ in protecting PSII but also report unexpected observations that challenge our current understanding of psychrophile species response to light stress. First, the impact of lincomycin on PSII photoinhibition was stronger than that of DTT, despite PsbA turnover being undetectable by immunoblots in most cases. Second, while our data support planktonic species showing better tolerance to high light than sympagic species, we found unsuspected diversity in photoprotection strategies. We hypothesize that these differences support a gradient from conservative strategies, possibly optimized for survival in the extreme sea-ice habitat of sympagic species, to productivity-oriented strategies in open water planktonic species dominating during the bloom period. In the transforming, brighter, Arctic Ocean, the adaptedness of this community-wide strategy scheme could be undermined, shaking up the historical dominance of certain diatom taxa.
Introduction
In the Arctic Ocean, microalgal growth is constrained by seasonal light availability characterized by extreme photoperiod cycles interacting with the snow and sea-ice cover formation and melt dynamics (). This radical seasonal habitat transformation leads to shifts in light intensity which can be stressful to photosynthetic life. Nonetheless, microalgae, and particularly diatoms (Pierella Karlusich et al., 2025), thrive in the winter-to-spring transition, and exploit the changing environment through a highly productive seasonal species succession () (Figure 1A). Typically, pennate diatoms overwhelmingly dominate sea-ice (sympagic) communities, whereas a mixture of pennate species (such as Fragilariopsis and Pseudo-nitzschia genera) and centric species (notably the Chaetoceros and Thalassiosira genera) are found in water beneath snow-covered ice (; ; Poulin et al., 2011; ), together with other phytoplankters such as Phaeocystis sp. (). As melting progresses, light penetrates deeper in the water column and most of the time, annual productivity climaxes in massive blooms consisting mostly of centric diatoms extending to the marginal ice-zone (ice-covers ≈50% of water) (Payne et al., 2024). In open waters, as nutrient concentrations decline and grazing pressure surges, different specialization patterns are observed among centric species, found either near the surface or in the deepening chlorophyll (Chl) a maximum (; ). Therefore, contrasted photoadaptation and photoprotection strategies, spanning a broad range of growth light optima and maximal growth rates, are observed in Arctic diatoms occupying different ecological niches (; ). Importantly, all Arctic diatoms’ show high plasticity enabling survival under both prolonged winter darkness (; ; ) and supra-optimal light conditions (; Leu et al., 2016; ; ; ). For example, sympagic species like Nitzschia frigida start growing under infinitesimal light intensities () and persist late into the melt season when averaged daily irradiance at the ice-water interface can exceed 100 µmol photons m-2 s-1 (; ). Likewise, Thalassiosira and Chaetoceros species start growing under the sea-ice cover but can experience illumination of up to 1,000 µmol photons m-2 s-1 in open waters (). Additionally, light fluctuations are caused by advective transport beneath snow-covered sea-ice with heterogenous optical properties (Tao et al., 2024), sudden mixing events induced by shelf break (Randelhoff et al., 2018) and wind driven mixing which is being amplified under climate change ().
FIGURE 1
While increasing light transmission to the Arctic Ocean (through shrinking sea-ice cover) has supported greater diatom productivity in recent years (Lewis et al., 2020), thus possibly more biomass being transferred to upper trophic levels, high-light stress can also decrease their nutritive quality (Leu et al., 2010;
Firstly, the deployment of mechanisms favouring dissipation of excess absorbed light energy by PSII as heat — at the expense of competing processes like photochemistry and fluorescence — collectively termed nonphotochemical quenching (NPQ) (
Secondly, photoinhibition is countered by the PSII repair cycle, in which the FtsH hexameric protease degrades damaged PsbA/PsbD allowing replacement by functional ones (
Consequently, to understand how divergent photoadaptive strategies support diatoms ecological success in the Arctic, and in turn impact the rest of the trophic chain (Leu et al., 2016), it is not sufficient to study their growth under stable light conditions (
Materials and methods
Diatoms culturing and acclimation
The same five Arctic diatom strains typical of contrasting seasonal light niches as in (
Experimental design and variable fluorescence approach
A Water-PAM fluorometer (Walz) was used to monitor minimal fluorescence, F0 (open reaction centres), with a blue modulated measuring light and maximal fluorescence, FM, probed with the same measuring light while a saturating multiple turnover flash (6,000 µmol photons m-2 s-1, 600 ms) reduces all PSII electron acceptors (closed reaction centres). To let enough time for sustained XC-NPQ to relax and measure the true maximal dark-adapted quantum yield of PSII, FV/FM, calculated as (FM-F0)/FM, we incubated cultures of different species to varying time in darkness which we had previously defined in (
At different time points (see Results), 3 mL aliquots were sampled and transferred into the Water-PAM cuvette and left in the dark for 15 s before measuring minimal and maximal fluorescence, termed F0’ and FM’ respectively. In this context, FV’/FM’ represents the potential quantum yield of PSII in the dark, for a given NPQ state, rather than a true maximal (FV/FM) or effective (ΔF/FM’ or ϕPSII) quantum yield, measured under actinic light. We note that 15 s is possibly not long enough for full reoxidation of PSII acceptors in the context of high-light stress (which would increase the measured F0’), therefore we limited our analysis of variations in FV’/FM’ to the subsequent recovery period under low light (5 µmol photons m-1 s-1). We made this compromise — using a short 15 s in the dark before measuring variable fluorescence — to avoid underestimating NPQ due to the potential relaxation of fast NPQ components. The quantum yield of NPQ (φNPQ) was calculated as F0’/FM’- F0’/FM and NPQ as FM/FM’-1. Because some Arctic diatom species show sustained XC-NPQ relaxation overlapping with times characteristic of PSII-repair, it is not possible to distinguish XC-NPQ from qI simply by analysing relaxation kinetics as in temperate organisms (
Where FS is the minimal fluorescence in steady-state under actinic light, and F0’ is the minimal fluorescence expected if all reaction centres were open while NPQ remains active. The crucial F0’ is often unavailable experimentally, but can be derived experimentally as (Oxborough and Baker, 1997):if it is assumed that all decrease in maximal fluorescence (FM’) is imputable to a Stern-Volmer-like quencher. In our case, with samples exposed to low light during recovery and then incubated 15 s in darkness, we have access to a measured F0’ which can be compared to its theoretical value. Therefore, in:qPd gives variable fluorescence during low light relaxation, normalized to what it would be if the only process influencing FM’ and F0’ was a Stern-Volmer-type quenching (qPd = 1 under this condition). Values of 1-qPd above 0 (i.e., F0’ > theo. F0’) indicate the extent of PSII photochemistry limitation caused by persistent reduced electron acceptors or photodamaged reaction centres, independently of NPQ level (see in plants (Ruban and Murchie, 2012)). Many reasons suggest this approach to distinguish decrease in FV’/FM’ mediated by NPQ from photoinhibition could be even more powerful in diatoms than in plants, and allow circumvention of some of the difficulties that sustained XC-NPQ entails in Arctic species; i) the theoretical relationship between NPQ and PSII photochemistry has been validated in some pennate diatoms (
Pigment sampling and quantification
Before, and at various time points during high-light stress and following low light recovery, sub-samples of 15 mL were collected and quickly filtered onto GF/F filters (Whatman®, 0.7 μm, 25 mm), flash frozen in liquid nitrogen and stored at −80 °C until analysis. Samples extracted in 100% methanol were mixed (70:30, vol:vol) with a buffer solution (tetrabutylammonium acetate (28 mmol L−1)) following a method adapted from Ras et al. (2008). Pigments content was measured using high-performance liquid chromatography with a Zorbax Eclipse XDB-C8 3.5 μm column (Agilent Technologies, Santa Clara, CA, United States). The de-epoxidation state (DES, in %) of the xanthophyll pool was calculated as:
Protein extraction and immunoblots
Samples of 25–35 mL were collected for characterization of protein allocation traits (before high-light stress or inhibitor addition). The number of replicates was always at least three (triplicate in control treatment) and extended up to 9 for some species/protein targets. Additionally, at various time points during high light experiments material was sampled to monitor PsbA degradation/repair kinetics, for all treatments (except only control in F. cylindrus) and possible regulation of Lhcx isoforms, for only the control treatment. Samples were filtered onto GF/F filters, flash frozen in liquid nitrogen and stored at −80 °C until extraction. Filters were thawed and placed in FastPrep lysing vials with 400 uL of 1X Protein Extraction Buffer (PEB, Agrisera (Sweden) AS08_300). Cells were lysed for 3 cycles of 60 s at 6.5 m s-1 with 60 s intervals on ice between cycles. The lysing vials were centrifuged at 16,100 x g for 5 min, the supernatant, which contained cell debris, was transferred to a 600 µL microcentrifuge tube and centrifuged again at 16,100 x g for 3 min. The resulting supernatant was transferred to another 600 uL microcentrifuge tube and stored at −80 °C until analysis. Immunoblots analysis was carried out as described in (Wu et al., 2012), except that the FCP6 blot was incubated overnight with a 1:5,000 dilution of the primary antibody in 2% ECL blocking solution immediately after transfer. Primary antibodies purchased from Agrisera were diluted as follows: PsbA/D1 (AS05 084) 1:10,000, RbcL (the large sub-unit of Rubisco) 1:10,000 (AS01 017), FtsH 1:5,000 (AS11 1789). The FCP6 antibody (provided by Dr. Erhard Rhiel) was diluted 1:5,000. The Anti-FCP6 detects all four Lhcx isoforms in Phaeodactylum tricornutum (
Curve fitting and statistical analysis
All curve fitting and statistical analyses were performed in R software version 4.3.0. The nls. multstart package (Padfield et al., 2021) was used to test different non-linear functions to fit φNPQ relaxation as a function of low light recovery time (t) and a Hill function was selected based on the lowest median Akaike Information Criterion across species Treatment (more details in Supplementary Figure S2):where φNPQM is the maximum extrapolated φNPQ value immediately at light extinction, t50 is the recovery time for which half of φNPQ has relaxed and n is a sigmoidicity factor.
We integrated this analysis in a comprehensive framework including previous studies on this species panel (
A Principal Component Analysis (PCA) on the 19 acclimation parameters across the 5 species (mean centred and scaled) was conducted to reduce dimensionality and visualize the top contributors in a biplot. We previously observed that during low light recovery, FV’/FM’ and qPd behave differently across species, thus providing complementary information (see Results). Therefore, we summed the value of both parameters after 5 and 60 min of low light recovery and divided them by four (giving a value bounded by 0 and 1) to obtain a comprehensive index of PSII inhibition for all species and treatments. We appended these computed PSII inhibition indices to their associated species treatments, resulting in a total of 22 parameters. We then calculated Pearson correlation coefficients among the parameters using cor() function in R.
Results
Protein allocation strategies
All protein allocation traits explored revealed significant differences between species (ANOVA and Tukey’s post-hoc test, P-value <0.05) (Figures 1B–D). The molar ratio between the PsbA PSII core protein and Chl a was the highest in the open water Chaetoceros gelidus (0.69 ± 0.26 mmol·mol-1) and the lowest in the dual sympagic/planktonic life form Fragilariopsis cylindrus (0.15 ± 0.07 mmol·mol-1) (Figure 1B). Nitzschia frigida, Thalassiosira gravida and C. neogracilis showed intermediate values (between 0.25 and 0.41 mmol·mol-1) significantly lower than in C. gelidus. The molar ratio between the large subunit of Rubisco and PsbA (a proxy of carbon fixation versus photochemistry capacities (Li and Campbell, 2017)) was significantly higher in C. neogracilis (222.91 ± 90.5 mol·mol-1) than in all species (as low as 21.14 mol·mol-1 in C. gelidus) except F. cylindrus (108.67 ± 36.83 mol·mol-1) (Figure 1C). A similar interspecific pattern was observed for the FtsH/PsbA molar ratio (a proxy for PSII turnover capacities (Li et al., 2016;
NPQ and xanthophyll cycle (XC) kinetics over high-light stress and low light recovery
Culture of the five species were submitted to high-light stress (2 h under 250 µmol photons m-2 s-1) in three different treatments; control, with addition of DTT (inhibiting diatoxanthin (DT) conversion to diadinoxanthin (DD)) and with addition of lincomycin (inhibiting plastid protein translation, and therefore de novo PsbA synthesis). We first focus on NPQ dynamics during the high-light stress. All species reached substantial φNPQ; C. gelidus reached the highest values, close to 0.8, while T. gravida displayed the lowest values, especially in the first hour of stress (0.4–0.5 φNPQ) (Figure 2A). Under DTT treatment, φNPQ was, unsurprisingly, much lower, remaining 0.2 in all species during the first 15 min (Figure 2B). Subsequently, φNPQ increased roughly linearly with time in all species despite DTT addition, with the steepest increase in N. frigida. Comparing lincomycin to control treatments, T. gravida was the only species showing a noticeable increase in φNPQ, reaching a final value of 0.6 (lincomycin) compared to 0.5 (control) (Figure 2C).
FIGURE 2

Kinetics of the quantum yield of nonphotochemical quenching (φNPQ) induction monitored over 2 h of high-light stress (250 µmol photons m-2 s-1) under control (A), with addition of dithiothreitol (DTT) (B) and with addition of lincomycin (C) treatments in all five Arctic diatom species investigated. Kinetics of φNPQ relaxation as a function of time over low light recovery (5 µmol photons m-2 s-1) under control (D), DTT (E) and lincomycin (F) treatments. Relaxation was tracked for at least 60 min (time values are log-transformed on the x-axis during recovery, log (60) is marked by a dashed vertical line) and extended until near-complete φNPQ relaxation in Nitzschia frigida and Thalassiosira gravida (up to 720 min, marked by a solid vertical line). φNPQ as a function of recovery time is fitted with a Hill function over the mean value of biological triplicates represented by the dashed coloured lines; fitted parameters and statistic outputs are found in Supplementary Figure S2.
During low light recovery (5 µmol photons m-2 s-1), N. frigida and T. gravida consistently showed slower φNPQ relaxation (Figures 2D–F, see also Supplementary Figure S2). Since φNPQ above 0.2 remained after 1 h of recovery in control treatment only for these species, we decided to keep monitoring ϕNPQ relaxation over a total of 6 h (N. frigida) and 12 h (T. gravida). Chaetoceros gelidus showed an outstandingly fast φNPQ relaxation half-time (t1/2) of ≈1.5 min under control and lincomycin treatments (Supplementary Figure S2). Excluding DTT treatments, this relaxation half-time is approximately one order of magnitude faster than the second fastest t1/2 measured, in C. neogracilis under lincomycin treatments (t1/2 not available for control treatment in this species). Despite slower φNPQ relaxation in the three ice-related species, near full relaxation was reached at their respective last measurement time point (Figure 2). Under DTT treatment, the starkest contrast in the reversibility of φNPQ was seen in C. gelidus, with φNPQ remaining at roughly 0.25 after 1 h of low light recovery. Stable Chl a concentrations over the treatments suggest persistent NPQ is not an artefact due to Chl a bleaching (Supplementary Figure S1). Chaetoceros gelidus also contrasted with the ice-related species in that its φNPQ relaxation was not slowed down by lincomycin addition (versus control treatment) (Supplementary Figure S2). However, despite slower φNPQ relaxation upon lincomycin addition for most species, no species showed a marked increase in non-reversible φNPQ between control and lincomycin treatments at the end of low light recovery.
Under control treatment, all species converted large amount of diadinoxanthin (DD) to diatoxanthin (DT) (Figure 3, the de-epoxidation state (DES) is shown in Supplementary Figure S3) via the XC. As expected in diatoms (
FIGURE 3

(A–E) Kinetics of diatoxanthin (DT) concentration per chlorophyll (Chl) a molecules over 2 h high-light stress (250 µmol photons m-2 s-1, yellow bar) and over subsequent low light recovery (5 µmol photons m-2 s-1, gray bar), under control (white), dithiothreitol (DTT, red) and lincomycin (Linc., purple) treatments in the five Arctic diatom species investigated. Recovery was tracked for at least 60 min and extended until near-complete NPQ relaxation in Nitzschia frigida(A) and Thalassiosira gravida(B), for which time values are log-transformed minutes on the x-axis, log (60) is marked by a dashed vertical line, and 720 min is marked by a solid vertical line. A similar representation of the de-epoxidation state as a function of time is found in Supplementary Figure S3 and DT relationships to NPQ are found in Supplementary Figure S4.
Quantum yield of PSII and photochemical quenching over low light recovery
In Arctic diatoms, XC-NPQ relaxation kinetically overlaps with typical hour-scale range of PSII repair usually associated to the reversal of the slow, qI, component of NPQ (Wu et al., 2011;
FIGURE 4

Kinetics of recovery under low light (5 µmol photons m-2 s-1) of the dark adapted maximal potential quantum yield of photosystem II (FV’/FM’), normalized to its pre-stress value (FV/FM), under control (A), dithiothreitol (DTT) (B) and lincomycin (C) treatments in all five Arctic diatom species investigated. Recovery was tracked for at least 60 min (time is log-transformed on the x-axis, 60 min is marked by a dashed vertical line) and extended until near-complete NPQ relaxation (see Figure 2) in Nitzschia frigida and Thalassiosira gravida (up to 720 min, marked by a solid vertical line).
With some caveats (see Material and methods), the potential photochemical quenching in the dark, i.e., qPd, can be used to assess decreases in PSII photochemistry beyond the effect of NPQ strictly arising from a Stern-Volmer-like mechanism (see Supplementary Figure S5 and (Ruban and Murchie, 2012;
FIGURE 5

Kinetics of recovery under low light (5 µmol photons m-2 s-1) of 1-qPd following high-light stress, under control (A), dithiothreitol (DTT) (B) and lincomycin (C) treatments in all five species investigated. 1-qPd, the potential photochemical quenching in the dark, serves as a proxy of photosystem (PS) II photochemical efficiency corrected for the effect of a Stern-Volmer nonphotochemical quenching (1-qPd=0 indicates that all PSII are unable to perform charge separation, see Material and methods). Recovery was tracked for at least 60 min (time is log-transformed on the x-axis, 60 min is marked by a dashed vertical line) and extended until near-complete NPQ relaxation (see Figure 2) in Nitzschia frigida and Thalassiosira gravida (up to 720 min, marked by a solid vertical line).
FIGURE 6

The dark adapted maximal potential quantum yield of photosystem (PS) II (FV’/FM’), normalized to its pre-stress value (FV/FM) (Figure 4), plotted as a function of 1-qPd (potential photochemical quenching in the dark (Figure 5)) for all data points measured during low light recovery following high-light stress under control (A), dithiothreitol (DTT) (B) and lincomycin (C) treatments in all five Arctic diatom species investigated. In the absence of processes competing with PSII photochemistry, such as xanthophyll cycle mediated nonphotochemical quenching (XC-NPQ) (inhibited in (B)), a direct relationship (dashed line) between norm. FV’/FM’ and 1-qPd is expected. Increasing 1-qPd represents more PSII being compromised for photochemistry from photodamage (or persistent reaction centre closure). Over low light recovery, PSII repair can restore photochemistry (inhibited in (C)) and 1-qPd trends toward 0. See Supplementary Figure S5 for more details on the theoretical relationships between norm. FV’/FM’, qPd and NPQ.
Overall, analysing both FV’/FM’ and 1-qPd allows to discriminate the influence of XC-NPQ — assumed to behave as a Stern-Volmer process — from that of other processes, including photodamages, on PSII photochemistry during low light recovery. The values of both FV’/FM’ and 1-qPd at 5 and 60 min of low light recovery were averaged to derive a comprehensive PSII inhibition index — ranging from 0 to 1 in all species and treatments combinations — and used in the multivariate analysis.
Protein kinetics; PsbA turnover and Lhcx expression
To determine if some long-lasting NPQ (qI), or loss of PSII photochemistry capacity (qPd<1), could be linked to photodamaged PsbA proteins, we sampled material to quantify PsbA via immunoblots over the high-light stress and low light recovery kinetics (four time points spread between t0 and after 1 h of recovery). Surprisingly, across all species and treatments, only C. gelidus under DTT treatment showed a negative correlation between PsbA/Chl a and time of experiment (P-value = 0.003, significant after Bonferroni correction for 13 relationships tested), with a modest slope leading to a ≈20% relative decrease in PsbA/Chl a at the end of low light recovery (Figure 7). This is in stark contrast with FV’/FM’ and 1-qPd often indicating 50%-to-75% loss of PSII photochemistry compared to pre-stress levels under both DTT and lincomycin treatments. We also attempted to detect increases in Lhcx isoforms accumulations (only for the control treatment) with a promiscuous Lhcx anti-body (FCP6) (
FIGURE 7

Linear regressions (forced y-intercepts to 1, dashed lines) of photosystem II reaction centre protein PsbA-to-chlorophyll (Chl) a ratios normalized to t0 as a function of time during high-light stress (250 µmol photons m-2 s-1, yellow bar) and low light recovery (5 µmol photons m-2 s-1, gray bar) under control (white), dithiothreitol (DTT, red) and lincomycin (Linc., purple) treatments in two species dominating the extreme of the succession; sea-ice specialist Nitzschia frigida(A) and the open water planktonic species; Chaetoceros gelidus(B) are shown. When applying a Bonferroni correction to the P-value significance threshold (13 comparisons across the five species), the relationship for C. gelidus DTT treatment is the only one that was significant (P-value <0.004). Example blots for one biological replicate for each treatment of both species are shown in (C,D). Relationships for all species and treatment are found in Supplementary Figure S6, their linear regressions output in Supplementary Data S3, and unedited blots in Supplementary Figure S7.
FIGURE 8

Ratio to chlorophyll (Chl) a of Lhcx isoforms, detected with Anti-FCP6 (Lhcx1) antibody (same as in (
Statistical analysis
We added the protein allocation traits (Figure 1) to a list of 16 photoacclimation parameters related to growth, PSII integrity, productivity assessed with 14C-uptake curves and PSII electron transport, and the characteristics of NPQ and the XC, determined in the same species and growth light intensities in previous studies (see (
FIGURE 9

Principal Component Analysis (PCA) over the protein acclimation traits depicted in Figure 1, combined with 16 additional acclimation parameters retrieved from (
Discussion
Considering the number of species included, the three treatments used, and the biochemical quantification of proteins and pigments in parallel to PSII fluorescence monitoring, this study represents one of the most comprehensive analyses of Arctic diatoms’ (or any polar microalgae’s) high-light response. Additionally, the five species investigated each occupy a distinct ecological niche over their seasonal succession, allowing us to link light stress tolerance to Arctic diatoms’ unique ecology and with the support of our previous works on these same species (
The sympagic N. frigida and the marginal ice-zone planktonic, T. gravida, displayed heightened sensitivity to high-light stress, characterized by longer NPQ relaxation times (Figure 2), and severely compromised PSII photochemistry (Figures 4, 5). However, F. cylindrus, found in ice-covered waters and within sea-ice brine channels, showed strong tolerance to light stress, comparable with the two open water Chaetoceros species under the control treatment. Using specific inhibitors to abolish each photoprotective mechanism in the following treatments, we surprisingly observed that the magnitude of the effect of lincomycin (blocking plastid protein translation and PSII repair) was either comparable to, or more severe than, DTT (blocking XC-NPQ) in four out of the five species (see Supplementary Figure S8). This seriously undermines the prevailing notion that XC-NPQ is the dominant, and often solely considered, photoprotection mechanism at play in polar diatoms. Moreover, the only species which was clearly more affected by XC-NPQ inhibition than by lincomycin was C. gelidus, which is abundant at the end of the Arctic bloom season and in Atlantic influenced waters (
Therefore, a parsimonious working model consistent with our dataset must explain, on the one hand, how functional PSII photoinhibition can be so pronounced while the loss of PsbA (assessed via biochemistry) is often small or undetectable, and on the other, why this process is strongly exacerbated when lincomycin inhibits the translation of plastid-encoded proteins. Although counterintuitive at first, there are precedents in earlier findings of fluorometric indicators of PSII functional photoinhibition (sustained NPQ-qI and lower FV’/FM’) not directly correlating with a loss of PsbA in polar taxa (
Notably, even in temperate strains, inactivated PSII reaction centres awaiting recycling can account for up to 60% of the total PSII pool in diatoms (
While the effect of lincomycin is often narrowly interpreted as blocking PsbA turnover, it could also abolish regulatory strategies relying on other plastid-encoded protein synthesis that are crucial in Arctic diatoms’ extreme environment. Before entertaining this hypothesis further, we must ask if the timescale of our experiment, combined with low temperature, kinetically allow for protein translation to be a significant part of the strategy. Although Lhcx proteins are nuclear-encoded, our results confirm that, at least in N. frigida, rapid protein translation in response to high-light stress is possible at 0 °C in an Arctic species (Figure 8). This regulation at the protein level was is fast as in P. tricornutum during a similar high-light stress conducted at 20 °C (
Therefore, it is plausible that lincomycin’s impact reflects not only a direct constraint on the repair of PSII — i.e. reversing net photoinhibition — but also indirect effects that favour the occurrence of photodamage and gross photoinhibition (as assessed by PSII fluorescence). Diatoms’ plastid genome is remarkably conserved and contains relatively few genes, most of which encode subunits of major photosynthetic complexes (PSI and PSII, cytochrome b6f, Rubisco, among others) (Yu et al., 2018). Still, theoretically, the abundance of these complexes, or of specific subunits, might be rapidly adjusted to help cope with high-light stress. Crucially, the two potential bottlenecks to photosynthesis in microalgae, plastoquinol oxidation by the cytochrome b6f (Sukenik et al., 1987) or carboxylation by Rubisco, are reliant on plastid-encoded subunits. Interestingly, if the rate of plastoquinol oxidation can be accelerated via an increase in cytochrome b6f stoichiometry, it could additionally support enhanced capacity for cyclic electron flow (CEF), while strong XC-NPQ favours the oxidation of the plastoquinone pool (
Given the lack of clear PsbA degradation patterns across taxa, we turned to a broader statistical approach to scrutinize other key factors potentially influencing Arctic diatoms’ light stress resistance, combining the analysis of protein allocation traits shown in Figure 1 with our previous description of various photoacclimation parameters on the same species panel (
Nevertheless, these hypotheses remain based on a limited number of species and photoacclimation parameters analysed across our studies. Other important traits, for instance alternative electron flows (
Conclusion
Our findings confirm the crucial role of XC-NPQ in the high-light stress tolerance of Arctic diatoms, while also challenging the notion of a monolithic photoprotection strategy. We suggest an underappreciated role of xanthophylls not involved in NPQ (
Statements
Data availability statement
The raw data supporting the conclusions of this article will be made available by the authors, without undue reservation.
Author contributions
DC: Conceptualization, Formal Analysis, Investigation, Methodology, Writing – original draft, Writing – review and editing. SG: Investigation, Methodology, Writing – review and editing. MS: Formal Analysis, Methodology, Validation, Writing – review and editing. ND: Formal Analysis, Methodology, Writing – review and editing. MMA: Formal Analysis, Methodology, Visualization, Writing – review and editing. MB: Conceptualization, Funding acquisition, Resources, Supervision, Writing – review and editing. DAC: Conceptualization, Formal Analysis, Methodology, Resources, Supervision, Writing – review and editing. JL: Conceptualization, Formal Analysis, Funding acquisition, Methodology, Project administration, Resources, Supervision, Writing – review and editing.
Funding
The author(s) declared that financial support was received for this work and/or its publication. We thank the contribution of CNRS in the framework of the IRL 3376 Takuvik, the Canada Excellence Research Chair on Remote sensing of Canada’s new Arctic frontier (MB), NSERC Canada Discovery and Northern Supplement grants (RGPIN-2017-04505) (JL), the Sentinel North program of Université Laval (Canada First Research Excellence Fund) and the research network Québec-Océan for their financial support.
Acknowledgments
We thank F. Bruyant for technical support, V. Richard for her support with HPLC analyses, Prof. A. Juhl and E. Riel for kindly providing us with the N. frigida strain and the FCP6-antibody, respectively.
Conflict of interest
The author(s) declared that this work was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
The author JL declared that they were an editorial board member of Frontiers at the time of submission. This had no impact on the peer review process and the final decision.
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Supplementary material
The Supplementary Material for this article can be found online at: https://www.frontiersin.org/articles/10.3389/fphbi.2025.1745893/full#supplementary-material
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Summary
Keywords
Arctic Ocean, diatoms, lincomycin, nonphotochemical quenching (NPQ), photodamage and PSII repair cycle, photoprotection, seasonal succession, xanthophyll cycle (XC)
Citation
Croteau D, Guérin S, Savoie M, Donaher N, M. Amirian M, Babin M, Campbell DA and Lavaud J (2026) Nonphotochemical quenching and beyond: multi-layered photoprotection shapes light-stress tolerance across seasonal niches in Arctic diatoms. Front. Photobiol. 3:1745893. doi: 10.3389/fphbi.2025.1745893
Received
13 November 2025
Revised
16 December 2025
Accepted
19 December 2025
Published
21 January 2026
Volume
3 - 2025
Edited by
Rajagopal Subramanyam, University of Hyderabad, India
Reviewed by
Milan Szabo, HUN-REN Biological Research Centre, Hungary
Ranay Mohan Yadav, University of Hyderabad, India
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© 2026 Croteau, Guérin, Savoie, Donaher, M. Amirian, Babin, Campbell and Lavaud.
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*Correspondence: Dany Croteau, dany.croteau.3@ulaval.ca
† Present address: Dany Croteau, Institute of Integrative Biology and Systems, Laval University, Québec, QC, Canada, Johann Lavaud, UMR6539 LEMAR- Laboratory of Environmental Marine Sciences, CNRS, University Brest, Ifremer, IRD, Institut Européen de la Mer, Institut Universitaire Européen de la Mer, Plouzané, France
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