Rc. Pausch et al., USE OF C-13 AND N-15 ISOTOPES TO INVESTIGATE O-3 EFFECTS ON C-METABOLISM AND N-METABOLISM IN SOYBEANS .1. C-FIXATION AND TRANSLOCATION, Agriculture, ecosystems & environment, 59(1-2), 1996, pp. 69-80
Short- and long-term C uptake/transaction dynamics were studied using
stable isotope techniques and leaf gas exchange to investigate the mec
hanism(s) of O-3 action on plant yield and C partitioning. Glycine mar
(L.) Merr. (soybean) plants were grown in open-top chambers and expos
ed to one of three O-3, regimes: half-ambient, ambient, or 2 x ambient
for nearly the entire growing season. The seasonal 7 h average O-3 co
ncentrations (nl l(-1)) were 25, 43, and 76 nl l(-1), respectively. Wh
ole plant C translocation was measured using pulse-labeled (CO2)-C-13
(99 atom %C-13) at two distant growth stages (R2 and R5). Translocatio
n parameters were as follows: %C-13 (sink strength), % C-13/g dry weig
ht (sink intensity), and % C-13/% Organ dry weight (relative specific
uptake). Single leaf photosynthesis (P-n) was measured at four growth
stages (V7, R2, R3, and R4). Ozone significantly affected translocatio
n, but the effect was dependent upon growth stage and the time followi
ng the C-13 pulse. At the stage of rapid seed fill within the pods (R5
), and at 42 h post-labeling, all three leaf translocation parameters
had a significant positive linear relationship with O-3 exposure. Conv
ersely, root nodule values were all inversely related to O-3 exposure.
Generally, at 0.5 h post-labeling, no significant effects were observ
ed for leaves and nodule translocation patterns, with the exception of
an inverse relationship between sink strength and O-3 exposure. No si
gnificant differences were observed for single leaf P-n among treatmen
ts. Our results indicate that the mechanism of chronic O-3 action invo
lves inhibition of translocation, implying reduced phloem loading and
the inhibition may be occurring without a concomitant reduction in the
amount of C fixed. In addition, C-13 pulse labeling appears to be a v
ery useful technique for investigating integrated long-term C transloc
ation dynamics which might not otherwise be evident using instantaneou
s methods such as short-term labeling or limited leaf gas exchange mea
surements.