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小麦及其他重要作物在盐胁迫下的离子变化与信号传导

Ion Changes and Signaling under Salt Stress in Wheat and Other Important Crops.

作者信息

Lindberg Sylvia, Premkumar Albert

机构信息

Department of Ecology, Environment and Plant Sciences, Stockholm University, SE-114 18 Stockholm, Sweden.

Bharathiyar Group of Institutes, Guduvanchery 603202, Tamilnadu, India.

出版信息

Plants (Basel). 2023 Dec 22;13(1):46. doi: 10.3390/plants13010046.

Abstract

High concentrations of sodium (Na), chloride (Cl), calcium (Ca), and sulphate (SO) are frequently found in saline soils. Crop plants cannot successfully develop and produce because salt stress impairs the uptake of Ca, potassium (K), and water into plant cells. Different intracellular and extracellular ionic concentrations change with salinity, including those of Ca, K, and protons. These cations serve as stress signaling molecules in addition to being essential for ionic homeostasis and nutrition. Maintaining an appropriate K:Na ratio is one crucial plant mechanism for salt tolerance, which is a complicated trait. Another important mechanism is the ability for fast extrusion of Na from the cytosol. Ca is established as a ubiquitous secondary messenger, which transmits various stress signals into metabolic alterations that cause adaptive responses. When plants are under stress, the cytosolic-free Ca concentration can rise to 10 times or more from its resting level of 50-100 nanomolar. Reactive oxygen species (ROS) are linked to the Ca alterations and are produced by stress. Depending on the type, frequency, and intensity of the stress, the cytosolic Ca signals oscillate, are transient, or persist for a longer period and exhibit specific "signatures". Both the influx and efflux of Ca affect the length and amplitude of the signal. According to several reports, under stress Ca alterations can occur not only in the cytoplasm of the cell but also in the cell walls, nucleus, and other cell organelles and the Ca waves propagate through the whole plant. Here, we will focus on how wheat and other important crops absorb Na, K, and Cl when plants are under salt stress, as well as how Ca, K, and pH cause intracellular signaling and homeostasis. Similar mechanisms in the model plant will also be considered. Knowledge of these processes is important for understanding how plants react to salinity stress and for the development of tolerant crops.

摘要

盐碱土中经常发现高浓度的钠(Na)、氯(Cl)、钙(Ca)和硫酸盐(SO)。由于盐胁迫会损害植物细胞对钙、钾(K)和水分的吸收,农作物无法成功生长和产出。不同的细胞内和细胞外离子浓度会随着盐度变化,包括钙、钾和质子的浓度。这些阳离子除了对离子稳态和营养至关重要外,还作为胁迫信号分子。维持适当的钾钠比是植物耐盐性的一个关键机制,耐盐性是一个复杂的性状。另一个重要机制是将钠从细胞质中快速排出的能力。钙被确立为一种普遍存在的第二信使,它将各种胁迫信号传递到导致适应性反应的代谢改变中。当植物受到胁迫时,细胞质中游离钙的浓度可以从其50-100纳摩尔的静息水平上升到10倍或更多。活性氧(ROS)与钙的变化有关,并且是由胁迫产生的。根据胁迫的类型、频率和强度,细胞质中的钙信号会振荡、短暂出现或持续较长时间,并呈现出特定的“特征”。钙的流入和流出都会影响信号的长度和幅度。根据几份报告,在胁迫下,钙的变化不仅会发生在细胞的细胞质中,还会发生在细胞壁、细胞核和其他细胞器中,并且钙波会在整个植物中传播。在这里,我们将重点关注小麦和其他重要作物在盐胁迫下如何吸收钠、钾和氯,以及钙、钾和pH值如何引起细胞内信号传导和稳态。还将考虑模式植物中的类似机制。了解这些过程对于理解植物如何应对盐胁迫以及培育耐盐作物很重要。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/3678/10780558/98d0530916dc/plants-13-00046-g001.jpg

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