The response in intracellular dimethyl sulfoniopropionate (DMSP) and dissolved DMSP and dimethyl sulfide (DMS) concentrations when Emiliania huxleyi was exposed to acute (1-h) increases in photon flux densities of photosynthetically active radiation (PAR) and ultraviolet (UV) radiation was examined in cells acclimated to low light (LL, 30 mmol photons m 22 s 21 ) and high light (HL, 300 mmol photons m 22 s 21 ). LL-acclimated cells displayed greater photoinhibition, assessed as a decrease in maximum photochemical efficiency (F v : F m ). Photoinhibition was increased by exposure to UV wavelengths. LL-acclimated cells also exhibited more light dissipation through the xanthophyll cycle, evident as changes in de-epoxidation state. Greater photoinhibition in LL-acclimated cells corresponded with increased accumulation of DMSP of 21% 6 4% relative to initial concentrations, contrasting with a slight decrease of 5% 6 6% in HL-acclimated cells. Exposure to UV appeared to decrease the rates of intracellular accumulation of DMSP. Conversely, PAR + UV exposure stimulated the net production of dissolved DMSP and DMS in both HL-acclimated and LL-acclimated cultures, compared with high PAR alone. The results indicate a direct link between acute photo-oxidative stress and DMSP synthesis by E. huxleyi. The physiological basis for increased release of DMSP and DMS from cells due to high PAR + UV exposure is unclear. However, the timescales of changes in intracellular DMSP, dissolved DMSP, and DMS are consistent with variations in light intensity experienced by phytoplankton in a turbulent mixed layer and are similar to rates of change in photosynthetic parameters associated with photoacclimation.Emission of dimethyl sulfide (DMS) from the oceans may contribute to the nucleation and growth of aerosol particles, enhancing formation of cloud condensation nuclei in the marine boundary layer; and thereby increasing the Earth's albedo (Shaw 1983;Charlson et al. 1987). DMS is generally supersaturated in oceanic waters and its sea-toair flux is dictated to a large extent by surface seawater concentration and the gas transfer velocity. Understanding what drives the regional and temporal variability in surface seawater concentrations is a prerequisite to the development of either empirical relationships or mechanistic models capable of predicting DMS flux to the atmosphere.DMS is essentially a product of the enzymatic cleavage of the S-containing osmolyte, b-dimethyl sulfoniopropionate (DMSP), synthesized by a variety of phytoplankton (Challenger and Simpson 1948). DMSP appears to play multiple roles in phytoplankton, in addition to acting as an osmolyte or compatible solute (Stefels 2000;Sunda et al. 2002). Despite the increasing number of functions attributed to DMSP, there remains considerable uncertainty in why intracellular concentrations of DMSP vary from , 0.1 mmol L 21 to over 400 mmol L 21 between phytoplankton taxa (Keller et al. 1989) and in what drives spatial and seasonal variations in the proportion of energy invest...