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Microbial community succession in soil is mainly driven by carbon and nitrogen contents rather than phosphorus and sulphur contents

氮气 肥料 环境化学 非生物成分 自行车 微生物种群生物学 肥料 大块土 氮气循环 营养循环 化学 土壤碳 农学 生态学 土壤有机质 营养物 土壤水分 生物 细菌 有机化学 遗传学 历史 考古
作者
Sheng Tang,Qian Ma,Karina A. Marsden,David R. Chadwick,Yu Luo,Yakov Kuzyakov,Lianghuan Wu,Davey L. Jones
出处
期刊:Soil Biology & Biochemistry [Elsevier]
卷期号:180: 109019-109019 被引量:19
标识
DOI:10.1016/j.soilbio.2023.109019
摘要

Organic manure is widely applied in agricultural systems to improve soil nutrient cycling and other physicochemical properties. However, the biotic and abiotic mechanisms that drive C, N, P, and S cycling following manure application are not completely understood. In this study, soil samples were collected from long-term experimental plots that had been amended with farmyard manure or mineral fertilisers since 1964. Isotope labelling with 15N, 33P, and 35S; metagenomics; and high-throughput sequencing were used to reveal the relationships between C, N, P, and S dynamics and microbial community composition and functions depending on fertilisation. A clear niche differentiation was observed between bacteria and fungi under mineral and manure regimes. A network analysis showed that long-term manure application reduced the complexity and stability of soil microbial network. Furthermore, a variation partitioning analysis based on redundancy analysis indicated that microbial community variation was mainly driven by soil Cand N contents. Dissolved organic C was the most important factor regulating microbial community structure. Soil C and N contents explained 43.5% of bacterial and 37.9% of fungal community variations. In contrast, soil P and S contents explained 29.9% of bacterial and 20.3% of fungal community variations. Long-term manure application increased the abundance of most functional genes related to C, N, P, and S cycling. This led to increased C and N cycling rates under manure application, which provided sufficient substrates for microbial growth. Partial least squares path modelling indicated that soil physicochemical properties, especially dissolved organic carbon, directly influenced C and S cycling, whereas the N and P cycles were indirectly affected by the changes in microbial community composition. These results provide a new perspective on both direct and indirect effects of organic manure and inorganic fertilisers on the soil nutrient cycling processes mediated by soil microbial community.
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