Title of article :
Estimating photosynthetic 13C discrimination in terrestrial CO2 exchange from canopy to regional scales
Author/Authors :
Chun-Ta، Lai, نويسنده , , R.، Ehleringer, James نويسنده , , Pieter، Tans, نويسنده , , C.، Wofsy, Steven نويسنده , , P.، Urbanski, Shawn نويسنده , , Y.، Hollinger, David نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2004
Abstract :
We determined (delta)13C values associated with canopy gross and net CO2 fluxes from four U.S. sites sampled between 2001 and 2002. Annual mean, flux-weighted (delta)13C values of net ecosystem CO2 exchange (NEE) were estimated for four contrasting ecosystems (three forests and one grassland) by analyzing daytime flask measurements collected at the top of canopies. Combining (delta)13C values associated with respiratory and net (respiration minus photosynthesis) fluxes, we demonstrate a method for estimating whole-canopy photosynthetic discrimination against 13C ((delta)A) in terrestrial ecosystems directly from field measurements. This experimental approach offers the possibility of examining interannual variability in (delta)A from ecosystem (delta)13C measurements. Our estimated (delta)13C values associated with photosynthetic fluxes are in agreement with those measured from foliar organic matter for C3 forests, and are within the range bounded by C3 and C4 grasses in a tallgrass prairie. The (delta)13C associated with NEE fluxes at our C3 forest sites ranges between -27.1+-2.7 and -28.3+-2.5‰, and is -22.6+-4.0‰ at the prairie site. These estimates differ from a previous study, particularly for C3 ecosystems at comparable latitudes. Sensitivity analyses indicate that our estimates of (delta)13C values of net CO2 fluxes are robust with respect to measurement errors, but can vary depending on the selection of background atmospheric values. Other factors (e.g., drought and sampling footprint) that might have influenced our (delta)13C measurements and calculations of (delta)A are also discussed. Our measurement-based analyses are particularly useful when both latitudinal and longitudinal variations in (delta)A are to be considered in the global inversion modeling studies.
Keywords :
1615 Global Change , Biogeochemical processes (4805) , 0315 Atmospheric Composition and Structure , Biosphere/atmosphere interactions , 0322 Atmospheric Composition and Structure , Constituent sources and sinks , 1040 Geochemistry , Isotopic composition/chemistry
Journal title :
GLOBAL BIOGEOCHEMICAL CYCLES
Journal title :
GLOBAL BIOGEOCHEMICAL CYCLES