Wb. Herppich et M. Herppich, INFLUENCE OF LEAF WATER-CONTENT ON THE C-3-CAM TRANSITION IN MESEMBRYANTHEMUM-CRYSTALLINUM, New phytologist, 136(3), 1997, pp. 425-432
Changes in leaf water content, night-time accumulation of malic (Delta
-malate) and citric acid (Delta-citrate) and phosphoenolpyruvate carbo
xylase (PEPC, EC 4.1.1.31) activity were followed for 60 d after germi
nation in well watered and salt-stressed plants of the facultatively h
alophytic ephemeral Mesembryanthemum crystallium L. To separate the ef
fects of development, salt stress and water deficit on crassulacean ac
id metabolism (CAM) induction plants were stressed initially 10 d afte
r germination and then successively at l-wk intervals (five sets). Rel
ated to dry mass or organic matter (i.e. dry mass corrected for the ma
ss of inorganic ions) water content started to decrease during the lat
e embryonal phase of the life cycle. Water content on a dry mass basis
was always lower in salt-stressed than in well watered individuals. H
owever, on an organic matter basis no difference was detectable. This
indicated that salt treatment did not reduce leaf water content but fa
lsified the basis (dry mass). Increases in leaf succulence and in pres
sure potential prevented long-term water deficit in well watered and i
n salt-stressed plants. Instead, these changes displayed enhanced vacu
olisation, which is an essential prerequisite for the development of C
AM. The end of that differentiation process might allow the initiation
of nocturnal malic acid accumulation in a threshold response. At the
onset of each salt treatment, short-term water deficits occurred due t
o an incomplete osmotic adaptation independent of plant age. As Delta-
malate only appeared when plants were c. 35 d old this water deficit w
as unlikely to be a decisive CAM-inducing factor. About 2 wk after ger
mination water content began to decline during the light periods in pl
ants of all treatments. This pattern disappeared again when CAM had be
en fully established. Daytime transpirational water loss is therefore
unlikely to be the decisive factor because it failed to induce the met
abolic shift in young plants. Environmental stress (e.g. salt or draug
ht) can therefore only induce Delta-malate when leaf and plant differe
ntiation has reached a certain stage.