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首页> 外文期刊>Environmental and experimental botany >Roots and leaves display contrasting osmotic adjustment mechanisms in response to NaCl-salinity in Atriplex nummularia
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Roots and leaves display contrasting osmotic adjustment mechanisms in response to NaCl-salinity in Atriplex nummularia

机译:根和叶表现出不同的渗透调节机制,以响应滨藜中的NaCl盐分

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This study reports contrasting mechanisms between the osmotic adjustment of roots and leaves from a typical halophytic species (Atriplex nummularia L.), in response to a large salinity range, resultant from the contribution of inorganic and organic solutes. Plants were grown in a greenhouse and irrigated with nutrient solution containing 0, 75, 150, 300, 450 and 600 mM NaCl during 7 weeks. The maximum leaf and root dry matter accumulation was observed at 300 and 150 mM treatments, respectively. The Na+ + Cl- concentrations in leaves were several times higher than in roots (ca. 760 and 90 mM in basis of tissue water, respectively at 300 mM NaCl treatment). Similar tendency was observed in the concentration of the most important organic solute involved with the osmotic adjustment, the glycinebetaine. The other analyzed solutes (K+, amino acids, soluble sugars and proline) also presented remarkably higher concentrations in leaves compared to roots, in all treatments. As a consequence, the leaf partial differential s was several times more negative than was in roots. Moreover, the osmotic adjustment of salt-treated plant leaves was approximately 3-fold higher than that found in roots. Surprisingly, under very high levels of external NaCl (450 and 600 mM), the root tissues exhibited partial differential s values less negative than those found in the external solution. The Na+ + Cl- were the major components to the leaves OA followed by K+ and GB, even in the untreated plants. In contrast to GB, the K+ participation in both leaves and roots decreased as the NaCl dose increased. In roots, K+ was the most important solute to OA of salt-untreated plants. Our data evidence that despite the A. nummularia leaves displayed an efficient osmotic adjustment, even under very high salinity levels, the same was not observed in its roots, which exhibit high partial differential s values. This fact probably complicates the root osmotic and water homeostasis in relation to the external medium. We can also conclude that glycinebetaine, followed by soluble sugars, plays a major role in the cytosol osmotic adjustment of both roots and leaves.
机译:这项研究报告了对典型盐生植物(Atriplex nummularia L.)的根和叶进行渗透调节的对比机制,这是由于无机和有机溶质的贡献而导致的较大盐度范围的结果。使植物在温室中生长,并在7周内用含有0、75、150、300、450和600 mM NaCl的营养液灌溉。在300和150 mM处理下分别观察到最大的叶和根干物质积累。叶片中Na + + Cl-的浓度是根部的几倍(分别以300 mM NaCl处理的组织水计分别约为760和90 mM)。在与渗透调节有关的最重要的有机溶质(甘氨酸甜菜碱)的浓度中也观察到了类似的趋势。在所有处理中,其他分析出的溶质(K +,氨基酸,可溶性糖和脯氨酸)在叶中的浓度也远高于根。结果,叶片偏微分s s的根数比根部的负数倍。此外,盐处理过的植物叶片的渗透调节比根部的渗透调节高约3倍。令人惊讶的是,在非常高的外部NaCl水平(450和600 mM)下,根部组织的偏微分s值小于在外部溶液中所发现的负值。 Na + + Cl-是叶片OA的主要成分,其次是K +和GB,即使在未经处理的植物中也是如此。与GB相反,随着NaCl剂量的增加,叶和根中的K +参与量均降低。在根部,K +是未经盐处理的植物的OA最重要的溶质。我们的数据证明,尽管农杆菌叶表现出有效的渗透调节,即使在非常高的盐度水平下,在其根部也未观察到相同的渗透,其表现出较高的偏微分s值。这一事实可能使根部渗透和与体内介质的水稳态平衡变得复杂。我们还可以得出结论,甘氨酸甜菜碱及其后的可溶性糖在根和叶的胞质渗透调节中起主要作用。

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