F. Janowiak et K. Dorffling, CHILLING OF MAIZE SEEDLINGS - CHANGES IN WATER STATUS AND ABSCISIC-ACID CONTENT IN 10 GENOTYPES DIFFERING IN CHILLING TOLERANCE, Journal of plant physiology, 147(5), 1996, pp. 582-588
The objective of the present paper was to study the relationship betwe
en chilling tolerance and chilling-induced abscisic acid (ABA) accumul
ation in maize. Ten maize genotypes, five classified as chilling toler
ant and five as chilling sensitive, were used. Two of them, Co 125 and
F 7, with significant differences in chilling tolerance, were studied
in detail. Seedlings at the third leaf stage, without and with previo
us acclimation, were chilled at 5 degrees C and at relative humidities
(RH) of 65 and 100 %. Immediately before and during chilling the ABA
content in the third leaf was measured by RIA. Water content, osmotic
potential, and - after recovery - the degree of necrotic injuries were
also determined. Chilling of non-acclimated seedlings at 65 % RH caus
ed accumulation of ABA in all ten genotypes. The ABA accumulation was
significantly higher in the chilling tolerant genotypes than in the ch
illing sensitive ones. Chilling of non-acclimated seedlings at 100 % R
H, studied in the two inbreds, caused ABA accumulation only in the chi
lling tolerant inbred F 7, although there were no significant changes
in the water relations. Acclimation (4 days at 14/12 degrees C, 70 % R
H) had only marginal influence on the ABA content but increased the ch
illing tolerance markedly. The higher chilling tolerance of acclimated
seedlings was accompanied by the ability for greater ABA accumulation
during chilling, especially in the chilling tolerant inbred F 7. Thre
sholds of water content and osmotic potential for the rise of ABA were
higher in tolerant than in sensitive genotypes. It is suggested that
higher chilling tolerance is related to the ability for greater and fa
ster ABA accumulation and better stabilization of water status in resp
onse to chilling. Evidence is presented that the rise in ABA is induce
d indirectly by chilling-induced water deficit as well as directly by
the chilling temperature.