Xk. Zhang et al., Iron accumulation in root apoplasm of dicotyledonous and graminaceous species grown on calcareous soil, NEW PHYTOL, 141(1), 1999, pp. 27-31
Solution culture studies have demonstrated that apoplasmic iron (Fe) deposi
ted in the roots of dicotyledonous and graminaceous plants can be mobilized
to improve plant iron status in conditions of limited Fe supply. The prese
nt study investigated the formation of the apoplasmic Fe pool in dicotyledo
nous (soybean and cucumber) and graminaceous (wheat) plants in a pot experi
ment. The pots had three compartments such that plants could take up Fe and
other nutrients from two calcareous soils treated with different Fe forms
without their roots touching with soil directly. In this way overestimating
Fe accumulation in rest apoplasm was avoided. The results showed that whil
e the root d.wt of wheat did not vary when soils were supplied with differe
nt Fe resources, the root d. wt of soybean and cucumber supplied with FeEDT
A decreased compared with the control (without Fe treatment). Supplying FeE
DTA in the side compartment increased shoot d. wt and Fe concentration in s
hoots of all species. However, supplying Fe(OH)(3) had no effect on shoot d
. wt of Fe concentration in the shoots of any species. Soybean and cucumber
accumulated little or no Fe in the root apoplasm in controls or in Fe(OH),
treatments. By contrast, a large amount of Fe was deposited in the root ap
oplasm of wheat grown in similar conditions. Remarkably, when FeEDTA was su
pplied in the soils, large apoplasmic iron pools were formed in the roots o
f all three species. Therefore, in dicotyledonous plants grown on calcareou
s soils, little or no apoplasmic iron pool forms, because there is not enou
gh available Fe in the soil solution and the plants have little ability to
mobilize Fe3+ in the soil. By contrast, a larger apoplasmic iron pool could
form in graminaceous plants at lower concentrations of available soil-Fe p
ossibly by enhancing the release of phytosiderophores which could mobilize
Fe3+ in the soil and then transfer the Fe3+-complexes to the foot apoplasm.