Key Laboratory of Oasis Ecology Agriculture of Xinjiang Bingtuan, Shihezi University, Shihezi, 832003, Xinjiang, China.
Arch Microbiol. 2019 Nov;201(9):1219-1232. doi: 10.1007/s00203-019-01689-x. Epub 2019 Jun 12.
In recent years, understanding the impact of reclamation of abandoned salinized field on microbial community structure is of great importance for ecosystem restoration in arid regions. The aim of this work was to investigate the effects of reclamation years on soil properties, bacterial community composition and diversity based on field sampling and llumina MiSeq sequencing. The five reclamation years are: unreclaimed salinized and reclaimed (1, 5, 10, and 15 years) fields. The results showed soil properties are significantly altered by abandoned salinized field. In particular, reclamation significantly decreased soil electrical conductivity, Cl, SO, Na, and Ca, during 5 years of reclamation. In addition, reclamation increased the richness and diversity of the bacterial community, except for the 1-year field soils. There was a large difference in the abundant bacterial phyla in 1-year field soils compared with other field soils. Proteobacteria were the most abundant in all of the field soils. Principal coordinates analysis showed that the abandoned and 1-year field soils exhibited specific differences in bacterial community structures compared with other field soils. Statistical analyses showed that available phosphorus, SO, Mg, and Ca were the main physicochemical properties affecting the soil bacterial communities. Overall, reclamation improved soil physicochemical properties and altered the structure and composition of soil bacterial communities compared with unreclaimed salinized soil.
近年来,了解废弃盐碱地开垦对微生物群落结构的影响对于干旱地区的生态系统恢复至关重要。本研究旨在通过野外采样和 Illumina MiSeq 测序,研究开垦年限对土壤性质、细菌群落组成和多样性的影响。五个开垦年限分别为:未开垦盐碱地和开垦(1、5、10 和 15 年)地。结果表明,废弃盐碱地的土壤性质发生了显著变化。特别是在开垦的 5 年内,开垦显著降低了土壤电导率、Cl、SO、Na 和 Ca。此外,开垦增加了细菌群落的丰富度和多样性,但 1 年生土壤除外。与其他土壤相比,1 年生土壤中丰富的细菌门有很大差异。所有土壤中最丰富的是变形菌门。主坐标分析表明,与其他土壤相比,废弃地和 1 年生土壤的细菌群落结构存在特定差异。统计分析表明,有效磷、SO、Mg 和 Ca 是影响土壤细菌群落的主要理化性质。总体而言,与未开垦盐碱地相比,开垦改善了土壤理化性质,改变了土壤细菌群落的结构和组成。