Nitrogen availability is an important control of productivity and species composition in the alpine. Plant species can control the spatial variability in N availability, by influencing rates of litter decomposition and mineralization. As a result, plant species can affect the spatial variability in species composition, which can be demonstrated through the spatial cross-correlation of the relative abundances of dominant species to species diversity. In alpine tundra, soil beneath patches dominated by either of two abundant, codominant, species differ seven fold in net N mineralization rates, which is greater than variation associated with differences in soil microclimate. Three plant traits, phenolic:N ratio, C:N ratio, and fine root production vary between these two species. Variation in these traits accounts for 33% of the variability in soil N transformation rates among patches where one species or the other is dominant. Experimental results indicate that the phenolic:N ratio is a stronger control of N mineralized from litter than the C:N ratio. The spatial variability in the relative abundances of dominant species, which determine N availability by controlling quality of carbon inputs, thus has the potential to influence the spatial variability of other community characteristics such as plant and microbial species diversity.

Key words: Acomastylis rossii, community structure, Deschampsia caespitosa, nitrogen cycling, spatial heterogeneity, species effects