COS 21-2 - Canopy photosynthesis drives diel patterns of fine root respiration in a loblolly pine (Pinus taeda) forest exposed to elevated CO2 and nitrogen deposition

Tuesday, August 7, 2007: 8:20 AM
J2, San Jose McEnery Convention Center
John E. Drake, Hawkesbury Institute for the Environment, University of Western Sydney, Australia, Gabriel G. Katul, Nicholas School of the Environment, Duke University, Durham, NC and Evan DeLucia, Plant Biology and Institute for Sustainability, Energy and Environment, University of Illinois, Urbana, IL
Recent research suggests that canopy photosynthesis drives soil respiration on short timescales (hours to days) in some temperate forests, presumably by affecting root respiration. However, measurements of fine root respiration (Rr) have lacked the sampling intensity and temporal precision to detect diel patterns, if present. We used a novel automated sampling system with temperature controlled cuvettes to make >7,000 measurements of Rr in a loblolly pine (Pinus taeda) forest exposed to elevated carbon dioxide and nitrogen fertilization. We detected diel patterns of Rr that track soil temperature as well as daily net ecosystem exchange (NEE) as measured by an on-site eddy-covariance tower. The direct response of Rr to temperature explained most of the diel variation in Rr on days with low NEE, but not on days with high NEE. The magnitude of the diel variation in Rr was correlated with the current and previous days’ NEE (r2=0.83, p<0.001 and r2=0.57, p<0.01, respectively), with no significant correlation with NEE from preceding days (p>0.1). Glucose additions to excised roots in solution consistently stimulated Rr measured in oxygen electrodes, suggesting that Rr was substrate limited and that the observed diel patterns in Rr could be explained by sugar supply from recent canopy photosynthesis. These results suggest a surprisingly close linkage between canopy and soil carbon processes, with implications for predicting Rr from measurements of NEE or photosynthesis. The combination of elevated [CO2] and N fertilization reduced basal Rr by 61% (p=0.07) indicating that Rr may be decreased by global change.
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