Konferenzpaper

Jahr der Veröffentlichung: 1994

Seiten: 275-283

Zeitschrift: Plant and Soil

Bandnummer: 165

Heftnummer: 2

ISSN: 0032-079X

DOI Link: https://doi.org/10.1007/BF00008070

Konferenz: 7th International Symposium on Iron Nutrition in Soils and Plants

Verlag: Springer

Abstract: 

The article describes factors and processes which lead to Fe chlorosis (lime chlorosis) in plants grown on calcareous soils. Such soils may contain high HCO3- concentrations in their soil solution, they are characterized by a high pH, and they rather tend to accumulate nitrate than ammonium because due to the high pH level ammonium nitrogen is rapidly nitrified and/or even may escape in form of volatile NH3. Hence in these soils plant roots may be exposed to high nitrate and high bicarbonate concentrations. Both anion species are involved in the induction of Fe chlorosis.

Physiological processes involved in Fe chlorosis occur in the roots and in the leaves. Even on calcareous soils and even in plants with chlorosis the Fe concentration in the roots is several times higher than the Fe concentration in the leaves. This shows that the Fe availability in the soil is not the critical process leading to chlorosis but rather the Fe uptake from the root apoplast into the cytosol of root cells. This situation applies to dicots as well as to monocots. Iron transport across the plasmamembrane is initiated by Fe-III reduction brought about by a plasmalemma located Fe-III reductase. Its activity is pH dependent and at alkaline pH supposed to be much depressed. Bicarbonate present in the root apoplast will neutralize the protons pumped out of the cytosol and together with nitrate which is taken up by a H+/nitrate cotransport high pH levels are provided which hamper or even block the Fe-III reduction.

Frequently chlorotic leaves have higher Fe concentrations than green ones which phenomenon shows that chlorosis on calcareous soils is not only related to Fe uptake by roots and Fe translocation from the roots to the upper plant parts but also dependent on the efficiency of Fe in the leaves. It is hypothesized that also in the leaves Fe-III reduction and Fe uptake from the apoplast into the cytosol is affected by nitrate and bicarbonate in an analogous way as this is the case in the roots. This assumption was confirmed by the highly significant negative correlation between the leaf apoplast pH and the degree of iron chlorosis measured as leaf chlorophyll concentration. Depressing leaf apoplast pH by simply spraying chlorotic leaves with an acid led to a regreening of the leaves.

Harvard-Zitierstil: MENGEL, K. (1994) IRON AVAILABILITY IN PLANT-TISSUES - IRON CHLOROSIS ON CALCAREOUS SOILS, Plant and Soil, 165(2), pp. 275-283. https://doi.org/10.1007/BF00008070

APA-Zitierstil: MENGEL, K. (1994). IRON AVAILABILITY IN PLANT-TISSUES - IRON CHLOROSIS ON CALCAREOUS SOILS. Plant and Soil. 165(2), 275-283. https://doi.org/10.1007/BF00008070