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Pectin drives microbial phosphorus solubilization in soil: Evidence from isolation-based and community-scale approaches

机译:果胶驱动土壤中的微生物磷溶解:来自孤立和社区规模方法的证据

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A considerable part of soil phosphorus is bound to metal cations or metal oxides, and cannot be used in these forms by soil microbes and plants. Phosphate-solubilizing bacteria (PSB) are abundant in pectin-rich rhizosphere, and their pectin-degrading activity has been reported. Therefore, we hypothesized that pectin activates PSB and promotes soil phosphorus solubilization. To test this hypothesis, we first tested the phosphate-solubilizing activity of pectin-degrading bacteria. PSB were more frequently isolated from pectin-containing medium, compared with other media (P 0.001). Further in a soil microcosm experiment, we examined whether pectin amendment accelerated soil phosphate solubilization. Pectin amendment decreased the concentrations of labile metallophosphate but increased the content of microbial biomass phosphorus in soils, meaning that phosphate solubilization was promoted by pectin amendment. In addition, PSB-like clades of bacteria increased by up to three times in response to pectin addition. This indicated that pectin amendment encouraged proliferation of PSB, accelerating soil phosphorus turnover processes initiated by solubilization of metallophosphate. In line with these results, genomic analysis indicated the widespread distribution of pectin-degrading genes among PSB, suggesting the possible co-evolution of pectin-degrading and phosphate solubilizing functions.
机译:相当一部分的土壤磷是与金属阳离子或金属氧化物结合,并且不能通过土壤微生物和植物在这些形式中使用。磷酸盐溶解的细菌(PSB)含有富含果胶的根际,并报告了它们的果胶降解活性。因此,我们假设果胶激活PSB并促进土壤磷溶解。为了测试这个假设,我们首先测试了果胶降解细菌的磷酸盐溶解活性。与其他介质相比,PSB比含果胶培养基更频繁地分离出PSB(P <0.001)。此外,在土壤微科学实验中,我们检查了果胶修正案是否加速土壤磷酸盐溶解。果胶修正案降低了不稳定金属磷酸盐的浓度,但增加了土壤中微生物生物质磷的含量,这意味着果胶炔蛋白促进了磷酸盐溶解。此外,响应果胶加入,细菌的PSB样板状片状增加了三次。这表明果胶修正案促进了PSB的增殖,加速通过溶解金属磷酸盐引发的土壤磷的周转过程。符合这些结果,基因组分析表明了PEB中果胶降解基因的广泛分布,表明果胶降解和磷酸盐溶解功能的可能的共同演变。

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