, Volume 132, Issue 4, pp 567–578

The nitrogen budget of a pine forest under free air CO2 enrichment


  • Adrien C. Finzi
    • Department of Biology, Boston University, 5 Cummington Street, Boston, MA 02215, USA
  • Evan H. DeLucia
    • Department of Plant Biology, University of Illinois, Urbana, IL 61801, USA
  • Jason G. Hamilton
    • Department of Plant Biology, University of Illinois, Urbana, IL 61801, USA
  • Daniel D. Richter
    • Nicholas School of the Environment, Duke University, Durham, NC 27708, USA
  • William H. Schlesinger
    • Nicholas School of the Environment, Duke University, Durham, NC 27708, USA
Ecosystems Ecology

DOI: 10.1007/s00442-002-0996-3

Cite this article as:
Finzi, A.C., DeLucia, E.H., Hamilton, J.G. et al. Oecologia (2002) 132: 567. doi:10.1007/s00442-002-0996-3


Elevated concentrations of atmospheric CO2 increase plant biomass, net primary production (NPP) and plant demand for nitrogen (N). The demand for N set by rapid plant growth under elevated CO2 could be met by increasing soil N availability or by greater efficiency of N uptake. Alternatively, plants could increase their nitrogen-use efficiency (NUE), thereby maintaining high rates of growth and NPP in the face of nutrient limitation. We quantified dry matter and N budgets for a young pine forest exposed to 4 years of elevated CO2 using free-air CO2 enrichment technology. We addressed three questions: Does elevated CO2 increase forest NPP and the demand for N by vegetation? Is demand for N met by greater uptake from soils, a shift in the distribution of N between plants, microbes, and soils, or increases in NUE under elevated CO2? Will soil N availability constrain the NPP response of this forest as CO2 fumigation continues? A step-function increase in atmospheric CO2 significantly increased NPP during the first 4 years of this study. Significant increases in NUE under elevated CO2 modulated the average annual requirement for N by vegetation in the first and third growing seasons under elevated CO2; the average stimulation of NPP in these years was 21% whereas the average annual stimulation of the N requirement was only 6%. In the second and fourth growing seasons, increases in NPP increased the annual requirement for N by 27–33%. Increases in the annual requirement for N were largely met by increases in N uptake from soils. Retranslocation of nutrients prior to senescence played only a minor role in supplying the additional N required by trees growing under elevated CO2. NPP was highly correlated with between-plot variation in the annual rate of net N mineralization and CO2 treatment. This demonstrates that NPP is co-limited by C availability, as CO2 from the atmosphere, and N availability from soils. There is no evidence that soil N mineralization rates have increased under elevated CO2. The correlation between NPP and N mineralization rates and the increase in the annual requirement for N in certain years imply that soil N availability may control the long-term productivity response of this ecosystem to elevated CO2. Although we have no evidence suggesting that NPP is declining in response to >4 years of CO2 fumigation, if the annual requirement of N continues to be stimulated by elevated CO2, we predict that the productivity response of this forest ecosystem will decline over time.

Elevated CO2 Nitrogen Net primary production N limitation Nutrient-use efficiency

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© Springer-Verlag 2002