Rare taxa of alkaline phosphomonoesterase-harboring microorganisms mediate soil phosphorus mineralization

矿化(土壤科学) 根际 生态学 慢生型大豆根瘤菌 放线菌门 化学 缓生根瘤菌 相对物种丰度 微生物 农学 丰度(生态学) 植物 环境化学 磷酸酶 磷酸单酯酶 生物 根瘤菌 细菌 园艺 土壤水分 根瘤菌科 生物化学 共生 基因 接种 遗传学 16S核糖体RNA
作者
Xiaomeng Wei,Yajun Hu,Bahar S. Razavi,Juan Zhou,Jianlin Shen,P. Nannipieri,Jinshui Wu,Tida Ge
出处
期刊:Soil Biology & Biochemistry [Elsevier BV]
卷期号:131: 62-70 被引量:271
标识
DOI:10.1016/j.soilbio.2018.12.025
摘要

As a homologous gene encoding microbial alkaline phosphomonoesterase, the expression of phoD is critically controlled by P availability and thus contributes to the mineralization of soil organic P under P-depleted condition. However, its role in the regulation of soil P turnover is largely unknown due to the complex coupling of physiochemical and biological processes in the P cycle, especially in paddy field. We hypothesized that 1) P fertilization would decrease the abundance of phoD gene and change the composition of phoD-harboring microbial community and 2) the high abundance of phoD-harboring microorganisms in P-poor soil would stimulate the synthesis of alkaline phosphomonoesterase, thus mitigating P limitation via the mineralization of organic P. After 42 days of rice growth, the phoD abundance negatively correlated with soil P availability, and it was significantly higher in non-fertilized treatments than in P-fertilized treatments for both rhizosphere and bulk soils. A stronger competition among phoD-harboring microorganisms was detected in non-fertilized soil than in P-fertilized soil, with Bradyrhizobium, Methylobacterium, and Methylomonas being the dominant taxa in all samples. However, the high phoD gene abundance under P-poor condition was mainly due to the growth of rare operational taxonomic units (OTUs) affiliated to Actinobacteria and Cyanobacteria (relative abundance < 3%). Consistent with our hypothesis, the growth of phoD-harboring microorganisms stimulated the hydrolysis of organic P in non-fertilized soil. However, in the P-fertilized treatments, the increase in OTU abundance was accompanied by the depletion of exchangeable P and accumulation of microbial biomass P. Our findings suggest that phoD-harboring microorganisms have the potential to immobilize P in biomass when the supply is sufficient while mineralize organic P under P-poor condition, during which the rare taxa play an important role.
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