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    青藏高原东南缘灰毛莸根际土壤细菌群落的海拔分布格局及驱动因子

    Altitudinal distribution patterns and driving factors of rhizosphere soil bacterial communities of Caryopteris forrestii on the southeastern edge of the Qinghai-Tibet Plateau

    • 摘要: 灰毛莸(Caryopteris forrestii)是青藏高原东南缘的典型乡土灌木,根系发达,在维持坡面稳定和防治水土流失中具有重要生态作用。其根际土壤细菌群落与植株生长密切相关,但不同海拔梯度下该群落的分布格局及其驱动因子仍缺乏系统研究。本研究在青藏高原东南缘沿2140–2750 m海拔设置7个梯度,利用16S rRNA基因高通量测序解析灰毛莸根际土壤细菌群落组成、多样性特征,并结合土壤理化性质探讨其环境驱动。结果表明,灰毛莸根际土壤含水率、pH、电导率和有机碳含量随海拔升高呈显著下降趋势,全磷含量沿海拔梯度呈单峰分布。根际土壤细菌共鉴定出48个菌门和114个菌纲,优势类群包括放线菌门、酸杆菌门、变形菌门、芽单胞菌门和绿弯菌门。在α多样性中,Shannon、Chao1和ACE指数均随海拔升高显著增加(P < 0.05)。β多样性分析显示,细菌群落结构沿海拔梯度发生显著分异,高、低海拔分离最为明显,而中间海拔聚集度较高。除土壤速效磷外,含水率、pH、有机碳、电导率、全氮、全磷以及海拔均显著影响细菌群落结构(P < 0.05),其中土壤pH和含水率是最关键的驱动因子。不同菌群表现出差异化的环境适应策略,绿弯菌门与pH呈显著正相关,而变形菌门和放线菌门则分别与含水率呈显著正、负相关(P < 0.05)。结构方程模型进一步揭示,海拔对细菌群落结构的影响以直接效应为主,并通过影响土壤理化特征产生一定的间接效应。本研究阐明了海拔与土壤环境因子对灰毛莸根际土壤细菌群落的调控机制,明确了pH和含水率的关键驱动地位,为后续利用灰毛莸开展高原的水土保持与生态恢复提供了理论支撑与实践参考。

       

      Abstract: Background Caryopteris forrestii is a typical native shrub in the southeastern margin of the Qinghai-Tibet Plateau, with a well-developed root system, and contributes significantly to slope stabilization and the mitigation of soil erosion. Its rhizosphere soil bacterial community is closely related to plant growth, but systematic research on the distribution pattern of this community and its driving factors under different altitude gradients is still lacking. Methods In this study, 7 elevation gradients were set along the 2140–2750 m altitude range on the southeastern edge of the Qinghai-Tibet Plateau. The rhizosphere bacterial community structure and diversity of Caryopteris forrestii were characterized via 16S rRNA gene high-throughput sequencing, followed by an investigation into their environmental drivers based on soil physical and chemical properties. Results The results showed that the soil water content, pH, electrical conductivity, and organic carbon content of the rhizosphere soil of Caryopteris forrestii decreased significantly with increasing altitude, while the total phosphorus content showed a unimodal distribution along the altitude gradient. A total of 48 bacterial phyla and 114 bacterial classes were identified in the rhizosphere soil, with the dominant groups including Actinobacteriota, Acidobacteriota, Proteobacteria, Gemmatimonadota, and Chloroflexota. Among the α-diversity indices, the Shannon, Chao1, and ACE indices all increased significantly with increasing altitude (P < 0.05). β-diversity analysis revealed that the bacterial community structure differed significantly along the altitude gradient, with the most obvious separation between high and low altitudes, while the middle altitudes showed a higher degree of aggregation. Except for soil available phosphorus, soil water content, pH, organic carbon, electrical conductivity, total nitrogen, total phosphorus, and altitude all significantly affected the bacterial community structure (P < 0.05), among which soil pH and soil water content were the most critical driving factors. Different bacterial groups exhibited differentiated environmental adaptation strategies: Chloroflexota showed a significant positive correlation with pH, while Proteobacteria and Actinobacteriota showed significant positive and negative correlations with soil water content, respectively (P < 0.05). The structural equation model further revealed that the effect of altitude on the bacterial community structure was mainly a direct effect, with a certain indirect effect through influencing soil physicochemical properties. Conclusions This study clarifies the regulatory mechanism of altitude and soil environmental factors on the rhizosphere soil bacterial community of Caryopteris forrestii, identifies the key driving role of pH and water content, and provides theoretical support and practical reference for the subsequent use of Caryopteris forrestii in soil and water conservation and ecological restoration on the plateau.

       

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