Department of Plant Physiology and Molecular Plant Biology, Eötvös Loránd University, Budapest 1117, Hungary.
J Plant Physiol. 2012 Nov 1;169(16):1615-22. doi: 10.1016/j.jplph.2012.04.012. Epub 2012 Jun 25.
Alkaline pH values and bicarbonate greatly reduce the mobility and uptake of Fe, causing Fe deficiency chlorosis. In the present work, the effects of pH and bicarbonate on the uptake and accumulation of Fe in the roots of cucumber were studied by Mössbauer spectroscopy combined with physiological tests and diaminobenzidine enhanced Perls staining. Mössbauer spectra of Fe-deficient cucumber roots supplied with 500 μM (57)Fe(III)-citrate at different pH values showed the presence of an Fe(II) and an Fe(III) component. As the pH was increased from 4.5 to 7.5, the root ferric chelate reductase (FCR) activity decreased significantly and a structural change in the Fe(III) component was observed. While at pH 4.5 the radial intrusion of Fe reached the endodermis, at pH 7.5, Fe was found only in the outer cortical cell layers. The Mössbauer spectra of Fe-deficient plants supplied with Fe(III)-citrate in the presence of bicarbonate (pH 7.0 and 7.5) showed similar Fe components, but the relative Fe(II) concentration compared to that measured at pH values 6.5 and 7.5 was greater. The Mössbauer parameters calculated for the Fe(II) component in the presence of bicarbonate were slightly different from those of Fe(II) alone at pH 6.5-7.5, whereas the FCR activity was similarly low. Fe incorporation into the root apoplast involved only the outer cortical cell layers, as in the roots treated at pH 7.5. In Fe-sufficient plants grown with Fe(III)-citrate and 1mM bicarbonate, Fe precipitated as granules and was in diffusely scattered grains on the root surface. The "bicarbonate effect" may involve a pH component, decreasing both the FCR activity and the acidification of the apoplast and a mineralization effect leading to the slow accumulation of extraplasmatic Fe particles, forming an Fe plaque and trapping Fe and other minerals in biologically unavailable forms.
碱性 pH 值和碳酸氢根会大大降低铁的流动性和吸收,导致缺铁性黄化。在本工作中,通过穆斯堡尔光谱结合生理测试和二氨基联苯胺增强 Perls 染色研究了 pH 值和碳酸氢根对黄瓜根系中铁吸收和积累的影响。在不同 pH 值下用 500 μM(57)Fe(III)-柠檬酸盐供应缺铁黄瓜根系的穆斯堡尔光谱显示存在 Fe(II)和 Fe(III) 组分。随着 pH 值从 4.5 增加到 7.5,根铁螯合还原酶(FCR)活性显著降低,并且观察到 Fe(III) 组分的结构变化。当 pH 值为 4.5 时,铁的径向侵入到达内皮层,而在 pH 值为 7.5 时,仅在外皮层细胞层中发现铁。在碳酸氢根存在下用 Fe(III)-柠檬酸盐供应缺铁植物的穆斯堡尔光谱显示出相似的铁组分,但与在 pH 值为 6.5 和 7.5 时测量的铁(II)浓度相比,相对铁(II)浓度更高。在碳酸氢根存在下计算出的 Fe(II) 组分的穆斯堡尔参数与在 pH 值为 6.5-7.5 时单独的 Fe(II) 略有不同,而 FCR 活性也同样较低。铁进入根质外体仅涉及外皮层细胞层,就像在 pH 值为 7.5 处理的根中一样。在含有 Fe(III)-柠檬酸盐和 1mM 碳酸氢根的铁充足植物中,铁沉淀为颗粒状,在根表面呈弥散分布的颗粒状。“碳酸氢根效应”可能涉及 pH 值成分,降低 FCR 活性和质外体酸化以及矿化效应,导致质外体铁颗粒缓慢积累,形成铁斑并将铁和其他矿物质固定在生物不可用的形式中。