Phytoplanktonic cells, and in particular cyanobacteria, experience dramatic daily fluctuations of solar radiations, which can become suboptimal for photosynthetic processes around midday. Photosystem II (PSII) is particularly sensitive to these changes in photon fluxes and under unfavorable or stressful conditions its activity can decline more rapidly than most other physiological processes (Berry and Björkman,
1980; Demmig-Adams and Adams,
1992; Aro et al.,
1993; Andersson and Aro,
2001). Photodamages to PSII are thought to start by the inactivation of the oxygen-evolving complex, which is caused by the dissociation of the Mn
4Ca
2+ cluster. This process leads to the production of long-lived P
680+, the oxidized form of the reaction center chlorophyll (Chl) pair, a particularly strong oxidant which in turn provokes the destruction of the PSII core protein D1 (Hakala et al.,
2006; Nishiyama,
2006). At low irradiances, the rate of photosynthetic electron transport is proportional to the photon flux density and damaged D1 polypeptides can be removed from the PSII reaction center and rapidly replaced by newly synthesized D1 proteins (Park et al.,
1995; Tyystjarvi and Aro,
1996; Nixon et al.,
2005; Ohnishi et al.,
2005). However, at higher irradiances, the rate at which the PSII reaction center is damaged can exceed its repair rate, which results in an increase of inactivated PSII centers and a subsequent decline of the quantum yield of photosynthesis, resulting from photoinhibitory fluorescence quenching (Powles,
1984; Prásil et al.,
1992; Aro et al.,
1993; Andersson and Aro,
2001).
Although the visible part of the solar spectrum (400–700

nm), also called photosynthetically active radiations (PAR), is responsible for most photoinhibitory effects, the contribution of UV-B (280–315

nm) and, to a least extent, UV-A (315–400

nm) is also notable in the uppermost layer of the ocean (Dring et al.,
2001; van de Poll et al.,
2001; He and Häder,
2002b). UV-B can indeed damage the photosynthetic apparatus about 100-fold more efficiently than visible light and these radiations might directly affect PSII proteins and the Mn
4Ca
2+ cluster (Sarvikas et al.,
2006; Caldwell et al.,
2007). UV and high visible radiations can also cause indirect photoinhibitory effects via the production of reactive oxygen species (ROS; He and Häder,
2002a,
b; Rastogi et al.,
2010), mainly formed within reaction centers (Asada,
1999) and light-harvesting complexes (Knox and Dodge,
1985; Zolla and Rinalducci,
2002). ROS are powerful oxidizing agents which can react with DNA, lipids, and proteins. Although these compounds are inevitably produced by cell metabolism, even under optimal growth conditions, their production is drastically enhanced when cells are exposed to a variety of stresses, including excess visible light and UV radiations (UVR; Latifi et al.,
2005; Ross et al.,
2006; Houot et al.,
2007; Allakhverdiev and Murata,
2008). The effect of ROS on PSII photoinhibition is thought to act primarily by inhibiting the
de novo synthesis of proteins, including those required for the repair of PSII (Nishiyama et al.,
2004; Nishiyama,
2006; Takahashi and Murata,
2008). A direct effect of ROS on the inactivation of PSII reaction center has also been suggested through triggering D1 degradation (Vass et al.,
1992; Aro et al.,
1993; Miyao et al.,
1995; Keren et al.,
1997; Lupinkova and Komenda,
2004). In any case, ROS clearly have a major role in light-mediated photoinhibition as well as in other environmental stresses (Nishiyama,
2006; Allakhverdiev and Murata,
2008; Latifi et al.,
2009). Thus, survival of phototrophic organisms depends upon the amount of ROS produced and their efficiency in scavenging these oxygen species.
In this context, marine picocyanobacteria belonging to the genera
Synechococcus and
Prochlorococcus constitute two relevant and complementary models to study acclimation processes to high light and UVR and their interrelationships with oxidative stress. In oceanic ecosystems, these two organisms numerically dominate the phytoplanktonic community (Partensky et al.,
1999a; Scanlan,
2003) and are considered to be the two most abundant photosynthetic organisms on Earth, with a substantial contribution to Chl biomass and primary production (Liu et al.,
1997; Partensky et al.,
1999a; Agawin et al.,
2000; Garcia-Pichel et al.,
2003). Members of the marine
Synechococcus genus are ubiquitously distributed and are most abundant in coastal regions and mesotrophic open ocean surface waters (Partensky et al.,
1999a; Zwirglmaier et al.,
2008), whereas
Prochlorococcus preferentially thrives in warm, stratified, oligotrophic tropical, and subtropical marine areas (Partensky et al.,
1999b; Zubkov et al.,
2000; Johnson et al.,
2006). In the field, these organisms experience large variations in irradiance, linked to the combination of the light/dark (L/D) cycle, water mixing, and a variable cloudiness (MacIntyre et al.,
2000). Moreover, their tiny size (0.5–0.8 and 0.8–1.2

μm diameter for
Prochlorococcus and
Synechococcus, respectively) confers them a high surface to volume ratio, optimizing their photon capture, and making them particularly sensitive to UVR (Llabres and Agusti,
2006,
2010).
Like other photosynthetic organisms, marine cyanobacteria have evolved a variety of protection mechanisms to ensure their growth and survival in highly illuminated habitats. These mechanisms include thermal dissipation of excess light excitation, structural changes of the photosynthetic machinery as well as enzymatic and non-enzymatic scavenging systems to eliminate ROS, in particular those produced in photosynthetic membranes (for reviews, see Bailey and Grossman,
2008; Latifi et al.,
2009). However, several pieces of evidence suggest that
Prochlorococcus and
Synechococcus lineages could deal differently with light stress. Indeed, two
P. marinus strains (PCC 9511 and SS120, a high light- and a low-light-adapted ecotype, respectively) were found to be more sensitive to a transient exposure to high irradiances than three
Synechococcus spp. strains representative of various trophic environments and exhibiting different pigmentation (RS9917, RCC307, and WH8102; Six et al.,
2007b). Similarly, measurements of cell abundances and/or mortality rates of field populations of picocyanobacteria exposed to different levels of natural solar radiations showed that
Prochlorococcus exhibited a lower resistance to UVR than
Synechococcus in surface waters of the central Atlantic Ocean (Llabres and Agusti,
2006; Agusti and Llabres,
2007) and the Mediterranean Sea (Sommaruga et al.,
2005; Llabres and Agusti,
2010).
In order to reveal potential differences in circadian metabolic rhythms between these two genera, the photophysiology of the model strains P. marinus PCC 9511 and Synechococcus sp. WH7803 was examined at different times of a modulated L/D cycle of visible light (hereafter VL) with or without UV. Additionally, the diel variability of the sensitivity of Prochlorococcus and Synechococcus to oxidative stress, as triggered by different H2O2 concentrations was investigated. Expression of key genes involved in photosynthesis, light, and oxidative stress response and a number of other processes were also monitored in order to get insights about the molecular bases of the observed physiological differences.