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根系-根尖质子通量在土壤胁迫适应中心。

Root-Apex Proton Fluxes at the Centre of Soil-Stress Acclimation.

机构信息

Center for Plant Water-Use and Nutrition Regulation and College of Life Sciences, Joint International Research Laboratory of Water and Nutrient in Crop, Fujian Agriculture and Forestry University, Jinshan Fuzhou 350002, China; Department of Plant Biotechnology and Bioinformatics, Ghent University, 9052 Ghent, Belgium; Center for Plant Systems Biology, VIB, 9052 Ghent, Belgium.

Département de Phytologie, Faculté des Sciences de l'Agriculture et de l'Alimentation, Université Laval, Québec, QC G1V 0A6, Canada.

出版信息

Trends Plant Sci. 2020 Aug;25(8):794-804. doi: 10.1016/j.tplants.2020.03.002. Epub 2020 Mar 30.

Abstract

Proton (H) fluxes in plant roots play critical roles in maintaining root growth and facilitating plant responses to multiple soil stresses, including fluctuations in nutrient supply, salt infiltration, and water stress. Soil mining for nutrients and water, rates of nutrient uptake, and the modulation of cell expansion all depend on the regulation of root H fluxes, particularly at the root apex, mediated primarily by the activity of plasma membrane (PM) H-ATPases. Here, we summarize recent findings on the regulatory mechanisms of H fluxes at the root apex under three abiotic stress conditions - phosphate deficiency, salinity stress, and water deficiency - and present an integrated physiomolecular view of the functions of H fluxes in maintaining root growth in the acclimation to soil stress.

摘要

植物根系中的质子(H)通量在维持根生长和促进植物对多种土壤胁迫的响应方面起着关键作用,这些胁迫包括养分供应波动、盐分渗透和水分胁迫。土壤中养分和水分的挖掘、养分吸收的速率以及细胞扩张的调节都取决于根 H 通量的调节,特别是在根冠,主要由质膜(PM)H-ATP 酶的活性介导。在这里,我们总结了在三种非生物胁迫条件下(磷缺乏、盐胁迫和水分亏缺)根冠 H 通量的调节机制的最新发现,并提出了 H 通量在适应土壤胁迫过程中维持根生长的生理分子综合观点。

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