Britto D T, Kronzucker H J
University of Toronto, Canadian Centre for World Hunger Research, Canada.
University of Toronto, Canadian Centre for World Hunger Research, Canada.
J Plant Physiol. 2015 Aug 15;186-187:1-12. doi: 10.1016/j.jplph.2015.08.002.
The efflux of sodium (Na(+)) ions across the plasma membrane of plant root cells into the external medium is surprisingly poorly understood. Nevertheless, Na(+) efflux is widely regarded as a major mechanism by which plants restrain the rise of Na(+) concentrations in the cytosolic compartments of root cells and, thus, achieve a degree of tolerance to saline environments. In this review, several key ideas and bodies of evidence concerning root Na(+) efflux are summarized with a critical eye. Findings from decades past are brought to bear on current thinking, and pivotal studies are discussed, both "purely physiological", and also with regard to the SOS1 protein, the only major Na(+) efflux transporter that has, to date, been genetically characterized. We find that the current model of rapid transmembrane sodium cycling (RTSC), across the plasma membrane of root cells, is not adequately supported by evidence from the majority of efflux studies. An alternative hypothesis cannot be ruled out, that most Na(+) tracer efflux from the root in the salinity range does not proceed across the plasma membrane, but through the apoplast. Support for this idea comes from studies showing that Na(+) efflux, when measured with tracers, is rarely affected by the presence of inhibitors or the ionic composition in saline rooting media. We conclude that the actual efflux of Na(+) across the plasma membrane of root cells may be much more modest than what is often reported in studies using tracers, and may predominantly occur in the root tips, where SOS1 expression has been localized.
植物根细胞的质膜上,钠离子(Na⁺)外流到外部介质这一过程,令人惊讶地未被充分理解。然而,Na⁺外流被广泛认为是植物抑制根细胞质溶胶区室中Na⁺浓度升高从而获得一定程度耐盐性的主要机制。在本综述中,我们以批判性的眼光总结了有关根Na⁺外流的几个关键观点和证据。将过去几十年的研究结果应用于当前的思考中,并讨论了关键研究,包括“纯生理学”研究以及与SOS1蛋白相关的研究,SOS1蛋白是迄今为止唯一已在基因层面得到表征的主要Na⁺外流转运蛋白。我们发现,目前关于根细胞质膜上快速跨膜钠循环(RTSC)的模型,并未得到大多数外流研究证据的充分支持。另一种假设不能被排除,即在盐分范围内,从根中流出的大多数Na⁺示踪剂并非通过质膜,而是通过质外体。支持这一观点的研究表明,用示踪剂测量时,Na⁺外流很少受到抑制剂的存在或含盐生根培养基中离子组成的影响。我们得出结论,根细胞质膜上Na⁺的实际外流可能比使用示踪剂的研究中通常报道的要少得多,并且可能主要发生在已定位SOS1表达的根尖部位。