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向盐性的“弯曲”模型:纳入蛋白磷酸酶2A、ABCB转运蛋白和生长素代谢。

'Bending' models of halotropism: incorporating protein phosphatase 2A, ABCB transporters, and auxin metabolism.

作者信息

Han Eun Hyang, Petrella Dominic P, Blakeslee Joshua J

机构信息

Department of Horticulture and Crop Science, The Ohio State University/OARDC, Wooster, OH, USA.

Department of Horticulture and Crop Science, OARDC Metabolite Analysis Cluster (OMAC), The Ohio State University/OARDC, Wooster, OH, USA.

出版信息

J Exp Bot. 2017 Jun 1;68(12):3071-3089. doi: 10.1093/jxb/erx127.

Abstract

Salt stress causes worldwide reductions in agricultural yields, a problem that is exacerbated by the depletion of global freshwater reserves and the use of contaminated or recycled water (i.e. effluent water). Additionally, salt stress can occur as cultivated areas are subjected to frequent rounds of irrigation followed by periods of moderate to severe evapotranspiration, which can result in the heterogeneous aggregation of salts in agricultural soils. Our understanding of the later stages of salt stress and the mechanisms by which salt is transported out of cells and roots has greatly improved over the last decade. The precise mechanisms by which plant roots perceive salt stress and translate this perception into adaptive, directional growth away from increased salt concentrations (i.e. halotropism), however, are not well understood. Here, we provide a review of the current knowledge surrounding the early responses to salt stress and the initiation of halotropism, including lipid signaling, protein phosphorylation cascades, and changes in auxin metabolism and/or transport. Current models of halotropism have focused on the role of PIN2- and PIN1-mediated auxin efflux in initiating and controlling halotropism. Recent studies, however, suggest that additional factors such as ABCB transporters, protein phosphatase 2A activity, and auxin metabolism should be included in the model of halotropic growth.

摘要

盐胁迫导致全球农业产量下降,而全球淡水资源储备的枯竭以及受污染或循环水(即废水)的使用使这一问题更加严重。此外,由于耕地频繁进行灌溉,随后经历中度至重度的蒸发散,导致农业土壤中盐分不均匀聚集,从而引发盐胁迫。在过去十年中,我们对盐胁迫后期以及盐分从细胞和根部输出的机制的理解有了很大提高。然而,植物根系感知盐胁迫并将这种感知转化为远离盐分增加浓度的适应性定向生长(即向盐性)的确切机制尚不清楚。在这里,我们综述了目前关于盐胁迫早期反应和向盐性起始的相关知识,包括脂质信号传导、蛋白质磷酸化级联反应以及生长素代谢和/或运输的变化。目前的向盐性模型侧重于PIN2和PIN1介导的生长素外排在起始和控制向盐性中的作用。然而,最近的研究表明,向盐性生长模型应纳入其他因素,如ABCB转运蛋白、蛋白磷酸酶2A活性和生长素代谢。

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