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中国西北贺兰山东坡不同海拔土壤微生物群落特征及其影响因素。

Soil microbial community characteristics and the influencing factors at different elevations on the eastern slope of Helan Mountain, Northwest China.

机构信息

Institute of Forestry and Grassland Ecology, Ningxia Agriculture and Forestry Science Academy/Key Laboratory of Desertification Control and Soil & Water Conservation of Ningxia, Yinchuan 750002, China.

Breeding Base for State Key Laboratory of Land Degradation and Ecological Restoration in Northwest China, Ningxia University, Yinchuan 750021, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2023 Jul;34(7):1957-1967. doi: 10.13287/j.1001-9332.202307.031.

Abstract

As an important bridge connecting aboveground communities and belowground biological processes, soil microorganisms play an important role in regulating belowground ecological processes. The altitudinal changes and driving factors of soil microbial community in mountain ecosystem in arid region are still unclear. We measured soil physicochemical properties at seven altitudes in the range of 1300-2800 m in Helan Mountains, and investigated the understory community composition, soil physicochemical properties, and soil microbial community. The driving factor for soil microbial community was explored by variance partitioning analysis and redundancy analysis. The results showed that the total amount of soil microorganisms and bacterial biomass first increased and then decreased with the increases of altitude, fungi, actinomyces, arbuscular mycorrhizal fungi, Gram-positive bacteria, and Gram-negative bacteria groups showed a gradual increase. The variation of fungal-to-bacterial ratio (F/B) along the altitude showed that the cumulative ability of soil bacteria was stronger than that of fungi at low altitudes, while the pattern is opposite at high altitudes. The ratio of Gram-positive bacteria to Gram-negative bacteria (GP/GN) showed an overall decreasing trend with the increases of altitude, indicating that soil bacteria and organic carbon availability changed from "oligotrophic" to "eutrophication" and from "low" to "high" transition as the altitude increased. Vegetation properties, soil physical and chemical properties jointly accounted for 95.7% of the variation in soil microbial community. Soil organic carbon (SOC), soil water content (SWC), and total nitrogen (TN) were significantly correlated with soil microbial community composition. Our results revealed the distribution pattern and driving factors of soil microbial communities at different elevations on the eastern slope of Helan Mountain, which would provide theoretical basis and data support for further understanding the interaction between plant-soil-microorganisms in arid areas.

摘要

作为连接地上社区和地下生物过程的重要桥梁,土壤微生物在调节地下生态过程中起着重要作用。干旱地区山地生态系统土壤微生物群落的海拔变化及其驱动因素仍不清楚。我们在贺兰山范围内的 1300-2800m 海拔高度上测量了七个海拔高度的土壤理化性质,并调查了林下群落组成、土壤理化性质和土壤微生物群落。通过方差分解分析和冗余分析探讨了土壤微生物群落的驱动因素。结果表明,土壤微生物总量和细菌生物量随海拔的升高先增加后减少,真菌、放线菌、丛枝菌根真菌、革兰氏阳性菌和革兰氏阴性菌呈逐渐增加的趋势。真菌与细菌比值(F/B)沿海拔的变化表明,在低海拔地区土壤细菌的累积能力强于真菌,而在高海拔地区则相反。革兰氏阳性菌与革兰氏阴性菌的比值(GP/GN)随海拔升高呈整体下降趋势,表明土壤细菌和有机碳的有效性随着海拔的升高从“贫营养型”向“富营养型”、从“低”向“高”发生转变。植被特性、土壤物理化学性质共同解释了土壤微生物群落变异的 95.7%。土壤有机碳(SOC)、土壤含水量(SWC)和总氮(TN)与土壤微生物群落组成显著相关。本研究揭示了贺兰山东坡不同海拔土壤微生物群落的分布格局及其驱动因素,为进一步理解干旱地区植物-土壤-微生物的相互作用提供了理论依据和数据支持。

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