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一种独特的孔蛋白通过蓝藻外膜介导铁的选择性运输。

A unique porin meditates iron-selective transport through cyanobacterial outer membranes.

机构信息

School of Life Sciences, Hubei Key Laboratory of Genetic Regulation and Integrative Biology, Central China Normal University, Wuhan, China.

Department of Plant and Environmental Sciences, The Alexander Silberman Institute of Life Sciences, The Hebrew University of Jerusalem, Edmond J. Safra Campus, Givat Ram, Jerusalem, Israel.

出版信息

Environ Microbiol. 2021 Jan;23(1):376-390. doi: 10.1111/1462-2920.15324. Epub 2020 Nov 26.

DOI:10.1111/1462-2920.15324
PMID:33196124
Abstract

Cyanobacteria are globally important primary producers and nitrogen fixers with high iron demands. Low ambient dissolved iron concentrations in many aquatic environments mean that these organisms must maintain sufficient and selective transport of iron into the cell. However, the nature of iron transport pathways through the cyanobacterial outer membrane remains obscure. Here we present multiple lines of experimental evidence that collectively support the existence of a novel class of substrate-selective iron porin, Slr1908, in the outer membrane of the cyanobacterium Synechocystis sp. PCC 6803. Elemental composition analysis and short-term iron uptake assays with mutants in Slr1908 reveal that this protein is primarily involved in inorganic iron uptake and contributes less to the accumulation of other metals. Homologues of Slr1908 are widely distributed in both freshwater and marine cyanobacteria, most notably in unicellular marine diazotrophs. Complementary experiments with a homologue of Slr1908 in Synechococcus sp. PCC 7002 restored the phenotype of Synechocystis knockdown mutants, showing that this siderophore producing species also possesses a porin with a similar function in Fe transport. The involvement of a substrate-selective porins in iron uptake may allow cyanobacteria to tightly control iron flux into the cell, particularly in environments where iron concentrations fluctuate.

摘要

蓝藻是具有高铁需求的全球重要初级生产者和固氮生物。许多水生环境中环境溶解铁浓度低,这意味着这些生物必须维持足够且具有选择性的铁向细胞内转运。然而,蓝藻外膜中铁转运途径的性质仍不清楚。在这里,我们提出了多条实验证据,共同支持在集胞藻 PCC 6803 的外膜中存在一类新型的底物选择性铁孔蛋白 Slr1908。元素组成分析和 Slr1908 突变体的短期铁摄取实验表明,该蛋白主要参与无机铁摄取,对其他金属的积累贡献较小。Slr1908 的同源物广泛分布于淡水和海洋蓝藻中,在单细胞海洋固氮生物中尤为明显。与集胞藻 sp. PCC 7002 中的 Slr1908 同源物的互补实验恢复了集胞藻敲低突变体的表型,表明这种产生铁载体的物种也在铁转运中具有具有类似功能的孔蛋白。底物选择性孔蛋白在铁摄取中的参与可能使蓝藻能够严格控制铁流入细胞,特别是在铁浓度波动的环境中。

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