CONICET | Buscador de Institutos y Recursos Humanos

Coastal phytoplankton assemblages from Potter Cove in Antarctica were exposed to low salinity (S-) and hightemperature (T+) conditions to simulate oceanic changes resulting from global warming. The treatments were:low salinity (30) and high temperature (S-T+); low salinity and ambient temperature (1?2 °C) (S-T0); ambientsalinity (34) and increased temperature (4?5 °C) (S0T+) and ambient salinity with ambient temperature(control, S0T0). Experiments were conducted in 100-L microcosms and monitored for 6 days. Compared to thecontrol treatment, micro-size diatoms (25?50 μm) dominated the phytoplankton assemblages while prasinophyceae were less abundant at the end of the S-T+ and S0T+ treatments. Nano-size diatoms (10?20 μm) alsoincreased significantly at the end of the experiment but only when exposed to S0T+. In S- treatments, theproduction of reactive oxygen/ nitrogen species (ROS/RNS) increased while phytoplankton biomass decreased.Under T+ conditions, the production of ROS/RNS was significantly lower than in T0 treatments. Throughout theexperiment, α-Tocopherol (α-T) consumption may have prevented lipid damage, allowing for increases inphotosynthetic rate and growth when nutrients concentrations were sufficiently high. Our results indicate thatan increase in temperature can compensate for the lipid damage produced by low salinity, and stimulate carbonuptake in both conditions. This study demonstrated that the final composition of phytoplankton assemblages inall experimental treatments was strongly influenced by the original composition. Future changes in naturalphytoplankton assemblages in Antarctic coastal waters will therefore depend on the planktonic species present atthe time of the perturbation, which can strongly impact energy flow along food webs and the magnitude ofcarbon and nutrient fluxes in Antarctic waters.