Xinjiang Key Laboratory of Desert Plant Roots Ecology and Vegetation Restoration, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Chinese Academy of Sciences, Urumqi 830011, China; Cele National Station of Observation and Research for Desert-Grassland Ecosystems, Cele 848300, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Xinjiang Key Laboratory of Desert Plant Roots Ecology and Vegetation Restoration, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Chinese Academy of Sciences, Urumqi 830011, China; Cele National Station of Observation and Research for Desert-Grassland Ecosystems, Cele 848300, China.
Sci Total Environ. 2024 Nov 1;949:175129. doi: 10.1016/j.scitotenv.2024.175129. Epub 2024 Jul 30.
Soil salinization adversely affects soil fertility and plant growth in arid region worldwide. However, as the drivers of nutrient cycling, the response of microbial communities to soil salinization is poorly understood. This study characterized bacterial communities in different soil layers along a natural salinity gradient in the Karayulgun River Basin, located northwest of the Taklimakan desert in China, using the 16S rRNA Miseq-sequencing technique. The results revealed a significant filtering effect of salinity on the bacterial community in the topsoil. Only the α-diversity (Shannon index) in the topsoil (0-10 cm) significantly decreased with increasing salinity levels, and community dissimilarity in the topsoil was enhanced with increasing salinity, while there was no significant relationship in the subsoil. BugBase predictions revealed that aerobic, facultatively anaerobic, gram-positive, and stress-tolerant bacterial phenotypes in the topsoil was negatively related to salinity. The average degree and number of modules of the bacterial co-occurrence network in the topsoil were lower under higher salinity levels, which contrasted with the trends in the subsoil, suggesting an unstable bacterial network in the topsoil caused by higher salinity. The average path length among bacterial species increased in both soil layers under high salinity conditions. Plant diversity and available nitrogen were the main drivers affecting community composition in the topsoil, while available potassium largely shaped community composition in the subsoil. This study provides solid evidence that bacterial communities adapt to salinity through the adjustment of microbial composition based on soil depth. This information will contribute to the sustainable management of drylands and improved predictions and responses to changes in ecosystems caused by climate change.
土壤盐渍化会对世界干旱地区的土壤肥力和植物生长产生不利影响。然而,作为养分循环的驱动因素,微生物群落对土壤盐渍化的响应仍知之甚少。本研究采用 16S rRNA Miseq 测序技术,对位于中国塔克拉玛干沙漠西北部的卡拉玉尔滚河流域不同土层中微生物群落进行了特征描述,该流域存在自然盐度梯度。研究结果表明,盐分对表层土壤中细菌群落具有显著的过滤作用。只有表层土壤(0-10 cm)的α多样性(香农指数)随盐度的增加而显著降低,且随着盐度的增加,表层土壤的群落相似性增加,而在底层土壤中则没有显著的关系。BugBase 预测结果表明,表层土壤中好氧、兼性厌氧、革兰氏阳性和耐应激细菌表型与盐度呈负相关。在较高盐度条件下,表层土壤中细菌共生网络的平均模块度和数量均较低,与底层土壤的趋势相反,表明较高盐度导致表层土壤中细菌网络不稳定。在高盐条件下,两种土壤层中种间平均路径长度均增加。植物多样性和有效氮是影响表层土壤群落组成的主要驱动因素,而有效钾则主要影响底层土壤群落组成。本研究提供了确凿的证据,表明细菌群落通过基于土壤深度的微生物组成调整来适应盐分。这些信息将有助于干旱地区的可持续管理,并改善对气候变化引起的生态系统变化的预测和响应。