Photochemical responses of three marine phytoplankton species exposed to ultraviolet radiation and increased temperature: Role of photoprotective mechanisms
Introduction
High intensities of solar radiation, which include ultraviolet (UVR, 280–400 nm) and visible (PAR, 400–700 nm) components may negatively affect some species in the surface layers of the water column. The UVR impact on phytoplankton cells comprises short- and long-term effects such as the decrease of photosynthesis and growth rates, and damage to different cellular targets, such as to the DNA molecule, among others [1], [2]. However, some phytoplankton species have evolved photoprotective mechanisms that can be selectively activated, depending on the exposure length and/or species-specific features, thus alleviating the impact of UVR in physiological processes such as photosynthesis. For motile species, one of these short-term mechanisms is the downward migration in the water column [3]. Radiation can trigger movement in flagellated species [4], [5]. Avoidance of excessive radiation can result from movement in response to high irradiance [6], [7] or also by a circadian response to daily light patterns [8]. In this way, flagellate cells maintain an appropriate level of light, and limit the loss of cells in the photic zone, if the water is not too turbulent [9]. However, under pronounced stratification, microorganisms are somewhat physically forced to stay close to the water surface, exposing cells to high radiation.
Another short-term mechanism includes the enzymatic conversion of xanthophylls which helps cells to cope with UVR and high levels of PAR [10], [11]. The de-epoxidation of diadinoxanthin, violaxanthin and antheraxanthin reduces any potential damage to PSII by enhancing the energy dissipation of excess light, measured as non-photochemical quenching, NPQ [12]. Over long-term (days) periods of exposure to high radiation levels, more permanent, physiological changes can occur, which are considered part of an acclimation process. One of such long-term mechanisms includes the synthesis of photoprotective compounds such as carotenoids, which act as antioxidants, and UV-absorbing compounds, UVACs – mainly mycosporine like amino acids, MAAs. UVACs exhibit absorption peaks within 310–360 nm [13] and are broadly distributed in tropical, temperate and polar environments, although not all the phytoplankton species synthesize them, e.g., they are less common in chlorophytes [14]. The acclimation ability under UVR is species-specific: Helbling et al. [15] found less photosynthetic inhibition and higher MAAs concentration in centric diatoms as compared to pennate species, whereas Hannach and Sigleo [16] demonstrated that MAAs synthesis was higher in dinoflagellates and haptophytes than in diatoms, chlorophytes and prasinophytes species.
This entire suit of individual and biochemical responses is in turn affected by temperature. For example, the dinoflagellates Lingulodinium polyedrum and Ceratium furca showed differences in swimming speeds at different temperatures: Between 22 and 26 °C, both species migrated at a rate of 0.7–1.0 m h−1, while temperatures below ca. 20 °C caused a marked decrease in swimming speed [17]. Moreover, Gyrodinium dorsum cells showed significant higher velocity at 32 °C than at 11 °C [18]. The synthesis of protective compounds is also affected by temperature, as it regulates the enzymatic cell machinery. In this regard, Halac et al. [19] demonstrated that the diatoms Chaetoceros gracilis and Thalassiosira weissflogii, at 23 °C and during short-term exposures to solar radiation showed lower photoinhibition as compared to samples exposed at 18 °C, mainly due to heat dissipation processes (NPQ) mediated by xantophyll pigments, which was more efficient at high temperatures.
So far, long-term studies about the interactive effects of UVR and temperature on phytoplankton photosynthesis and the associated photoprotective mechanisms are rather scarce. Sobrino and Neale [20] demonstrated that photosynthesis in phytoplankton exposed to UVR is highly dependent on temperature. Higher temperatures decreased the sensitivity to UVR due to the temperature dependence of repair mechanisms. However, Lionard et al. [21] did not find any significant effect of temperature or UV-B (280–315 nm) or their interaction, neither on photosynthetic performance nor in diadinoxanthin-based xanthophyll cycle pool size, likely associated to the presence of diatoms, the dominant algal group in the studied communities. This variability in the interactive effects of UVR and temperature on phytoplankton may be partly explained by other factors, such as the optimal temperature range for UVR sensitivity and the capacity of acclimation in each species under different temperatures.
In a context of climate change, it is essential to know the extent of these combined effects of different variables as well as the mechanisms that phytoplankton cells use to cope with their potential impact. Thus the aim of this study was to evaluate the long-term (days) photochemical responses to UVR of three phytoplankton species characteristic of Patagonian waters in terms of (a) effective photochemical efficiency, and (b) three key photoprotective mechanisms – dissipation of excess energy, synthesis of photoprotective compounds, i.e., carotenoids/UVACs, and vertical migration – that might help to mitigate the negative effects of UVR on the photosynthetic process. As temperature increase could interact antagonistically with UVR levels to reduce its negative effects, we also asked whether a potential increase in temperature, such as it may occur in a context of climate change [22], would influence the studied responses. Moreover, we also evaluated the effects of an attenuated irradiance condition such as occurring when cells are in deeper layers in the water column e.g. when the water column was mixed by wind. Because of the utmost importance of Patagonia within a photobiology context, i.e., the region normally receives high levels of UVR and it is periodically under the influence of ozone depletion events [23], this kind of studies are essential to assess the potential responses of local phytoplankton species under a scenario of climate change.
Section snippets
Culture collection/study site
Prorocentrum micans Ehrenberg (Dinophyceae), Dunaliella salina (Dunal) Teodoresco (Chlorophyceae) and Isochrysis galbana Parke (Prymnesiophyceae) from the Microalgae Culture Collection at Estación de Fotobiología Playa Unión (EFPU, Argentina) were grown in 1 l Erlenmeyer flasks in f/2 medium [24] with a photoperiod 12L:12D in a chamber (Sanyo model ML 350). Cells were pre-acclimated during two weeks prior to experimentation at the local oceanic mean surface temperature corresponding to the
Solar radiation conditions
In general, irradiances were quite similar within each experimental period (Fig. 1), with no significant differences determined among days. However, some differences in the mean irradiances among the experiments were found (Table 1). Mean irradiances were higher during D. salina experiments than in the ones with P. micans and I. galbana: PAR intensities were 19% and 26%, while UV-A was a 17% and 25% and UV-B was a 32% and 25% above the levels recorded during the P. micans and I. galbana
Discussion
The results of our study presented here contribute to understand the impact of temperature and UVR upon different phytoplankton species when exposed to solar radiation levels that normally occur in the Patagonia area and simulating an increase of temperature due to climate change as predicted by the year 2100 i.e., a scenario of increase in coastal surface temperature [22]. The first evident finding of our study is related to the species-specific nature of photochemical responses and
Acknowledgments
We thank V. Fiorda Giordanino, S. Guendulain-García, S. Strauch and S. Fernández (Estación Marítima) for their help during experiments; E. Heimsch analysed pigments and I. Albarracín helped with cultures. This work was supported by Agencia Nacional de Promoción Científica y Tecnológica (PICT 2012-0271); Ministerio de Ciencia, Tecnología e Innovación Productiva (Argentina) – Consejo Nacional de Ciencia y Tecnología (México) (Project No. MX/09/13) and Fundación Playa Unión, Argentina. This work
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