Nitrous oxide (N2O) is a key atmospheric greenhouse gas that contributes to
global climatic: change through radiative warming and depletion of stratos
pheric ozone. In this report, N2O flux was monitored simultaneously with ph
otosynthetic CO2 and O-2 exchanges from intact canopies of 12 wheat seedlin
gs. The rates of N2O-N emitted ranged from <2 pmol(.)m(-2.)s(-1) when NH4was the N source, to 25.5 +/- 1.7 pmol(.)m(-2.)s(-1) (mean +/- SE, n = 13)
when the N source was shifted to NO3-. Such fluxes are among the smallest r
eported for any trace gas emitted by a higher plant. Leaf N2O emissions wer
e correlated with leaf nitrate assimilation activity, as measured by using
the assimilation quotient, the ratio of CO2 assimilated to O-2 evolved. N-1
5 isotopic signatures on N2O emitted from leaves supported direct N2O produ
ction by plant NO3- assimilation and not N2O produced by microorganisms on
root surfaces and emitted in the transpiration stream. In vitro production
of N2O by both intact chloroplasts and nitrite reductase, but not by nitrat
e reductase, indicated that N2O produced by leaves occurred during photoass
imilation of NO2- in the chloroplast. Given the large quantities of NO3- as
similated by plants in the terrestrial biosphere, these observations sugges
t that formation of N2O during NO2- photoassimilation could be an important
global biogenic N2O source.