Fertilization regulates global thresholds in soil bacteria

Author:

Chen Cai12ORCID,Li Shu‐Le12ORCID,Chen Qing‐Lin123,Delgado‐Baquerizo Manuel4ORCID,Guo Zhao‐Feng13,Wang Fenghua5,Xu Yao‐Yang13ORCID,Zhu Yong‐Guan136ORCID

Affiliation:

1. Key Laboratory of Urban Environment and Health, Ningbo Observation and Research Station, Institute of Urban Environment Chinese Academy of Sciences Xiamen People's Republic of China

2. University of Chinese Academy of Sciences Beijing People's Republic of China

3. Zhejiang Key Laboratory of Urban Environmental Processes and Pollution Control CAS Haixi Industrial Technology Innovation Center in Beilun Ningbo People's Republic of China

4. Laboratorio de Biodiversidad y Funcionamiento Ecosistémico, Instituto de Recursos Naturales y Agrobiología de Sevilla (IRNAS) CSIC Seville Spain

5. School of Geographical Sciences, Hebei Normal University, Hebei Key Laboratory of Environmental Change and Ecological Construction Hebei Experimental Teaching Demonstrating Center of Geographical Science Shijiazhuang People's Republic of China

6. State Key Laboratory of Urban and Regional Ecology, Research Center for Eco‐Environmental Sciences Chinese Academy of Sciences Beijing People's Republic of China

Abstract

AbstractGlobal patterns in soil microbiomes are driven by non‐linear environmental thresholds. Fertilization is known to shape the soil microbiome of terrestrial ecosystems worldwide. Yet, whether fertilization influences global thresholds in soil microbiomes remains virtually unknown. Here, utilizing optimized machine learning models with Shapley additive explanations on a dataset of 10,907 soil samples from 24 countries, we discovered that the microbial community response to fertilization is highly dependent on environmental contexts. Furthermore, the interactions among nitrogen (N) addition, pH, and mean annual temperature contribute to non‐linear patterns in soil bacterial diversity. Specifically, we observed positive responses within a soil pH range of 5.2–6.6, with the influence of higher temperature (>15°C) on bacterial diversity being positive within this pH range but reversed in more acidic or alkaline soils. Additionally, we revealed the threshold effect of soil organic carbon and total nitrogen, demonstrating how temperature and N addition amount interacted with microbial communities within specific edaphic concentration ranges. Our findings underscore how complex environmental interactions control soil bacterial diversity under fertilization.

Funder

National Natural Science Foundation of China

Publisher

Wiley

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