Increases in nitrogen uptake rather than nitrogen-use efficiency support higher rates of temperate forest productivity under elevated CO₂.
Authors:
Finzi, Adrien C. Norby, Richard J. Calfapietra, Carlo Gallet-Budynek, Anne Gielen, Birgit Holmes, William E. Hoosbeek, Marcel R. Iversen, Colleen M. Jackson, Robert B. Kubiske, Mark E. Ledford, Joanne Liberloo, Marion Oren, Ram Polle, Andrea Pritchard, Seth Zak, Donald R. Schlesinger, William H. Ceulemans, Reinhart USDA, FS
Source:
Proceedings of the National Academy of Sciences of the United States of America. 2007 Aug. 28, v. 104, no. 35 National Academy of Sciences, p. 14014-14019.
NALT Subjects:
temperate forests forest trees Pinus taeda Liquidambar styraciflua Populus tremuloides Betula papyrifera carbon dioxide elevated atmospheric gases primary productivity tree growth nitrogen fertilizers fertilizer application nutrient uptake nutrient use efficiency nutrient availability soil fertility forest soils North Carolina Wisconsin Tennessee Italy
Other Subjects:
free air carbon dioxide enrichment
Issue Date:
28-Aug-2007
Abstract:
Forest ecosystems are important sinks for rising concentrations of atmospheric CO₂. In previous research, we showed that net primary production (NPP) increased by 23 ± 2% when four experimental forests were grown under atmospheric concentrations of CO₂ predicted for the latter half of this century. Because nitrogen (N) availability commonly limits forest productivity, some combination of increased N uptake from the soil and more efficient use of the N already assimilated by trees is necessary to sustain the high rates of forest NPP under free-air CO₂ enrichment (FACE). In this study, experimental evidence demonstrates that the uptake of N increased under elevated CO₂ at the Rhinelander, Duke, and Oak Ridge National Laboratory FACE sites, yet fertilization studies at the Duke and Oak Ridge National Laboratory FACE sites showed that tree growth and forest NPP were strongly limited by N availability. By contrast, nitrogen-use efficiency increased under elevated CO₂ at the POP-EUROFACE site, where fertilization studies showed that N was not limiting to tree growth. Some combination of increasing fine root production, increased rates of soil organic matter decomposition, and increased allocation of carbon (C) to mycorrhizal fungi is likely to account for greater N uptake under elevated CO₂. Regardless of the specific mechanism, this analysis shows that the larger quantities of C entering the below-ground system under elevated CO₂ result in greater N uptake, even in N-limited ecosystems. Biogeochemical models must be reformulated to allow C transfers below ground that result in additional N uptake under elevated CO₂.
