Iron accumulation in root apoplasm of dicotyledonous and graminaceous species grown on calcareous soil

Citation
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
Citations number
10
Categorie Soggetti
Plant Sciences
Journal title
NEW PHYTOLOGIST
ISSN journal
0028646X → ACNP
Volume
141
Issue
1
Year of publication
1999
Pages
27 - 31
Database
ISI
SICI code
0028-646X(199901)141:1<27:IAIRAO>2.0.ZU;2-A
Abstract
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.