Land use modified impacts of global change factors on soil microbial structure and function: A global hierarchical meta-analysis

• Published in: The Science of the total environment Vol. 935; p. 173286
• Main Authors: Wang, Mingyu, Li, Detian, Frey, Beat, Gao, Decai, Liu, Xiangyu, Chen, Chengrong, Sui, Xin, Li, Maihe
• Format: Journal Article
• Language: English
• Published: Netherlands Elsevier B.V 20.07.2024
• Subjects: Agriculture - methods; Biodiversity; Climate Change; Ecosystem; Functional genes; Global change; Land use; Meta-analysis; Microbiota; Nitrogen - analysis; Nitrogen Cycle; Nitrogen cycling; Soil - chemistry; Soil microbial alpha-diversity; Soil Microbiology; Soil microbial alpha-diversity; Functional genes; Land use; Nitrogen cycling; Global change; Meta-analysis
• ISSN: 0048-9697; 1879-1026
• DOI: 10.1016/j.scitotenv.2024.173286

Nitrogen cycling in terrestrial ecosystems is critical for biodiversity, vegetation productivity and biogeochemical cycling. However, little is known about the response of functional nitrogen cycle genes to global change factors in soils under different land uses. Here, we conducted a multiple hierarchical mixed effects meta-analyses of global change factors (GCFs) including warming (W+), mean altered precipitation (MAP+/−), elevated carbon dioxide concentrations (eCO2), and nitrogen addition (N+), using 2706 observations extracted from 200 peer-reviewed publications. The results showed that GCFs had significant and different effects on soil microbial communities under different types of land use. Under different land use types, such as Wetland, Tundra, Grassland, Forest, Desert and Agriculture, the richness and diversity of soil microbial communities will change accordingly due to differences in vegetation cover, soil management practices and environmental conditions. Notably, soil bacterial diversity is positively correlated with richness, but soil fungal diversity is negatively correlated with richness, when differences are driven by GCFs. For functional genes involved in nitrification, eCO2 in agricultural soils and the interaction of N+ with other GCFs in grassland soils stimulate an increase in the abundance of the AOA-amoA gene. In agricultural soil, MAP+ increases the abundance of nifH. W+ in agricultural soils and N+ in grassland soils decreased the abundance of nifH. The abundance of the genes nirS and nirK, involved in denitrification, was mainly negatively affected by W+ and positively affected by eCO2 in agricultural soil, but negatively affected by N+ in grassland soil. This meta-analysis was important for subsequent research related to global climate change. Considering data limitations, it is recommended to conduct multiple long-term integrated observational experiments to establish a scientific basis for addressing global changes in this context. [Display omitted] •GCFs do not always affect soil microbial structure and function.•Soil microbial α-diversity responds differently to GCFs in different ecosystems.•GCFs have different effects on certain functional genes involved in N cycling.•Effect values obtained using a hierarchical mixed-effects meta-analysis model.