Leaf age affects the seasonal pattern of photosynthetic capacity and net ecosystem exchange of carbon in a deciduous forest

Citation
Kb. Wilson et al., Leaf age affects the seasonal pattern of photosynthetic capacity and net ecosystem exchange of carbon in a deciduous forest, PL CELL ENV, 24(6), 2001, pp. 571-583
Citations number
53
Categorie Soggetti
Plant Sciences","Animal & Plant Sciences
Journal title
PLANT CELL AND ENVIRONMENT
ISSN journal
01407791 → ACNP
Volume
24
Issue
6
Year of publication
2001
Pages
571 - 583
Database
ISI
SICI code
0140-7791(200106)24:6<571:LAATSP>2.0.ZU;2-I
Abstract
Temporal trends in photosynthetic capacity are a critical factor in determi ning the seasonality and magnitude of ecosystem carbon fluxes, At a mixed d eciduous forest in the south-eastern United States (Walker Branch Watershed , Oak Ridge, TN, USA), we independently measured seasonal trends in photosy nthetic capacity (using single-leaf gas exchange techniques) and the whole- canopy carbon flux (using the eddy covariance method). Soil respiration was also measured using chambers and an eddy covariance system beneath the can opy, These independent chamber and eddy covariance measurements, along with a biophysical model (CANOAK), are used to examine how leaf age affects the seasonal pattern of carbon uptake during the growing season. When the meas ured seasonality in photosynthetic capacity is represented in the CANOAK si mulations, there is good agreement with the eddy covariance data on the sea sonal trends in carbon uptake. Removing the temporal trends in the simulati ons by using the early season maximum value of photosynthetic capacity over the entire growing season overestimates the annual carbon uptake by about 300 g C m(-2) year(-1)-half the total estimated annual net ecosystem exchan ge. Alternatively, use of the mean value of photosynthetic capacity incorre ctly simulates the seasonality in carbon uptake by the forest. In addition to changes related to leaf development and senescence, photosynthetic capac ity decreased in the middle and late summer, even when leaf nitrogen was es sentially constant. When only these middle and late summer reductions were neglected in the model simulations, CANOAK still overestimated the carbon u ptake by an amount comparable to 25% of the total annual net ecosystem exch ange.