Wheat (Triticum aestivum L. cv Bannock), rice (Oryza sativa L.cv , and soybean (Glycine max [L.] Merr cv Essex) were grown in a factorial greenhouse experiment to determine if C02-induced increases in photosynthesis, biomass, and yield are modified by increases in ultraviolet (UV)-B radiation corresponding to stratospheric ozone depletion. The experimental conditions simulated were: (a) an increase in CO2 concentration from 350 to 650 microliters per liter; (b) an increase in UV-B radiation corresponding to a 10% ozone depletion at the equator; and (c) a and b in combination. Seed yield and total biomass increased significantly with elevated CO2 in all three species when compared to the control. However, with concurrent increases in UV-B and CO2, no increase in either seed yield (wheat and rice) or total biomass (rice) was observed with respect to the control. In contrast, CO2-induced increases in seed yield and total plant biomass were maintained or increased in soybean within the elevated C02, UV-B environment. Whole leaf gas exchange indicated a significant increase in photosynthesis, apparent quantum efficiency (AQE) and water-use-efficiency (WUE) with elevated CO2 in all 3 species. Including elevated UV-B radiation with high CO2 eliminated the effect of high CO2 on photosynthesis and WUE in rice and the increase in AQE associated with high CO2 in all species. Elevated CO2 did not change the apparent carboxylation efficiency (ACE) in the three species although the combination of elevated CO2 and UV-B reduced ACE in wheat and rice. The results of this experiment illustrate that increased UV-B radiation may modify C02-induced increases in biomass, seed yield and photosynthetic parameters and suggest that available data may not adequately characterize the potential effect of future, simultaneous changes in CO2 concentration and UV-B radiation.Current atmospheric levels of CO2 may double from 340 ,uL L-' to 680 ,uL L`by the middle of the 21st century (8).It is evident from a number of field and greenhouse experiments that increases in CO2 will have a significant effect on layer with subsequent increases in the amount of solar ultra- ( 17). In addition to CO2, other trace gases are also increasing as a result of industrialization. The rise of chlorofluorocarbons (CFCs), methane (CH4), and nitrous oxide (N20) may substantially deplete the stratospheric ozone violet-B radiation (UV-B, between 290-320 nm) reaching the earth's surface (1,3). Although this predicted increase is small relative to the entire electromagnetic spectrum, UV-B has a disproportionately large photobiological effect due to its absorption by proteins and nucleic acids. In UV-B sensitive plants, photosynthetic capacity may be reduced directly by the effect of UV-B radiation on photosynthetic enzymes or disruption of PSII reaction centers, or indirectly by effects on photosynthetic pigments and stomatal function (9,13,19,20).Both CO2 and UV-B radiation are expected to increase simultaneously with future changes in global climate. To date...