OOS 49-4 - Species controls over free-living nitrogen fixation in a tropical rain forest

Friday, August 10, 2007: 9:00 AM
C3&4, San Jose McEnery Convention Center
Sasha Reed, Southwest Biological Science Center, U.S. Geological Survey, Moab, UT, Cory C. Cleveland, Department of Ecosystem and Conservation Sciences, University of Montana, Missoula, MT and Alan R. Townsend, INSTAAR and Department of Ecology and Evolutionary Biology, University of Colorado at Boulder, Boulder, CO
Free-living nitrogen (N) fixation can be a significant source of N to terrestrial ecosystems. For plants capable of symbiotic associations, species-specific differences in N fixation rates are frequently documented, yet we have little understanding of how different plant species affect the free-living N fixation rates occurring on and beneath them. In particular, many species-rich tropical rain forests appear to support high rates of free-living N fixation, yet the degree to which tree species variation controls such rates is unknown. Here, we report results for surveys of canopy leaf, leaf litter, and soil N fixation rates on and beneath six species of trees from a lowland tropical rain forest in southwestern Costa Rica. The site contains 100-200 tree species per hectare, averages over 5 m of precipitation annually, and our six selected species represent six of the most common families in the region. Our data showed that rates of free-living N fixation varied by orders of magnitude along a vertical profile spanning the canopy to the soil. Moreover, free-living N fixation rates varied significantly by tree species within each profile component: showing sixty-, six-, and three-fold inter-specific rate differences for canopy leaves, leaf litter, and soils, respectively. Indices of phosphorus (P) availability such as foliar and litter P content, N:P ratios, and labile soil P pools also consistently varied by tree species, and were significantly correlated with rates of free-living N fixation. Thus, these data suggest that: 1) free-living N fixation in tropical forests varies considerably in both vertical and horizontal dimensions; 2) species-specific variation in N fixation rates may be predictable from standard ecosystem metrics such as foliar and soil P content and/or N:P ratios; and 3) variability in P availability and N inputs could drive inter-specific differences in other biogeochemical processes such as soil carbon storage.
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