Field-growing silver birch (Betula pendula Roth) clones (clone 4 and 80) were exposed to elevated CO 2 and O 3 in open-top chambers for three consecutive growing seasons (1999)(2000)(2001). At the beginning of the OTC experiment, all trees were 7 years old. We studied the single and interaction effects of CO 2 and O 3 on silver birch below-ground carbon pools (i.e. effects on fine roots and mycorrhizas, soil microbial communities and sporocarp production) and also assessed whether there are any clonal differences in these belowground CO 2 and O 3 responses. The total mycorrhizal infection level of both clones was stimulated by elevated CO 2 alone and elevated O 3 alone, but not when elevated CO 2 was used in fumigation in combination with elevated O 3 . In both clones, elevated CO 2 affected negatively light brown/orange mycorrhizas, while its effect on other mycorrhizal morphotypes was negligible. Elevated O 3 , instead, clearly decreased the proportions of black and liver-brown mycorrhizas and increased that of light brown/ orange mycorrhizas. Elevated O 3 had a tendency to decrease standing fine root mass and sporocarp production as well, both of these O 3 effects mainly manifesting in clone 4 trees. CO 2 and O 3 treatment effects on soil microbial community composition (PLFA, 2-and 3-OH-FA profiles) were negligible, but quantitative PLFA data showed that in 2001 the PLFA fungi : bacteria-ratio of clone 80 trees was marginally increased because of elevated CO 2 treatments. This study shows that O 3 effects were most clearly visible at the mycorrhizal root level and that some clonal differences in CO 2 and O 3 responses were observable in the below-ground carbon pools. In conclusion, the present data suggests that CO 2 effects were minor, whereas increasing tropospheric O 3 levels can be an important stress factor in northern birch forests, as they might alter mycorrhizal morphotype assemblages, mycorrhizal infection rates and sporocarp production.