Sea ice algal communities are naturally exposed to very high concentrations of dissolved oxygen, which are likely to lead to increasing stress levels and declines in productivity. To test this hypothesis, cultures of Fragilariopsis cylindrus (Grun?) Hasle, Pseudo-nitzschia sp., Fragilariopsis curta (Van Heurch), Porosira glacialis (Grunow), and Entomoneis kjellmannii (Cleve) from Antarctic sea ice and Nitzschia frigida from Arctic sea ice were exposed to elevated dissolved oxygen levels, and their growth, maximum quantum yield, relative maximum electron transport rate, and photosynthetic efficiency were measured. At oxygen concentrations equivalent to approximately four times air saturation (89% oxygen), the growth rate and maximum quantum yield were significantly reduced in all taxa. When the oxygen concentration was regularly allowed to drop, the effect on growth and quantum yield was reduced. At lower dissolved oxygen concentrations (52%), the declines in growth and quantum yield were reduced but were still mostly significantly different from the controls (21% oxygen). It is likely that the generation of excess active oxygen radicals in the presence of free oxygen is responsible for most of the decline in growth, maximum quantum yield, relative maximum electron transport rate, and photosynthetic efficiency in all species.Abbreviations: a, photosynthetic efficiency; dF/F m 0 , effective quantum yield; E k , minimum saturating irradiance; F v /F m , maximum quantum yield; NPQ, nonphotochemical quenching coefficient; rETR max , relative maximum electron transport rate; RLC, rapid light curve High dissolved oxygen concentrations under sea ice were first reported by McMinn et al. (2000). They noted that on bright sunny days, oxygen production by algae under the ice far exceeded its rate of removal by diffusion, leading to extensive oxygen bubble formation. Because of the increased solubility of oxygen in seawater at low temperatures, these organisms are likely to experience some of the highest dissolved oxygen concentrations on the planet, which is likely to be toxic to the sea ice algae. The question of how these algae cope with these high oxygen levels and other extreme conditions was also raised and discussed by Thomas and Dieckmann (2002). However, elevated dissolved oxygen concentrations are not unique to sea ice habitats but are found in the boundary layers of most microbial mat communities and frequently on the stapes or leaves of macrophytes and sea grasses. Oxygen concentrations as high as 560% air saturation, for instance, have been reported in boundary layers associated with seaweed stipes (Irwin and Davenport 2002), and similar dissolved oxygen concentrations have been observed above sediments dominated by diatoms (Raven 1991).Elevated oxygen levels are known to have an inhibitory effect on the metabolism and growth of plants (Raven 1991, Raven et al. 1994). There are two mechanisms thought to be largely responsible for these deleterious effects: the competitive effect of O 2 on RUBISCO (photorespiratio...