Continental-scale drivers of soil microbial extracellular polymeric substances

Extracellular polymeric substances (EPS) are key microbial residues that contribute to soil organic carbon (SOC) and promote soil aggregation. Yet, their abundance and large-scale controls have only begun to be investigated. We conduct extensive soil sampling across a European transect spanning diverse climates, bedrocks, and land uses. Average soil EPS content is 956 ± 55 µg g<sup>-1</sup> soil (n= 92 sites), with EPS-carbon (EPS-C) contributing 1.6 ± 0.1% to SOC. Bedrock influences EPS content, EPS-C contribution to SOC, and the EPS-C/microbial biomass carbon (MBC) ratio, whereas land use mainly affects the latter two. The EPS-C/MBC ratio is negatively correlated with microbial growth and carbon use efficiency, and increases under water deficit, while EPS increases with MBC, clay content, and exchangeable calcium. Our results demonstrate that EPS represents a functionally important microbial residue, regulated by climatic, edaphic, microbial, and land-use factors, with significant implications for soil carbon cycling and sequestration.

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Publication Details

Journal
Nature Communications
Published
2026-03-02
DOI
https://doi.org/10.1038/s41467-026-70068-0
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
0.00

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article

Continental-scale drivers of soil microbial extracellular polymeric substances

Wolfgang D. Wanek, Lisa Noll, Yuntao Hu, Honghua Ruan et al.
Nature Communications
Soil Carbon and Nitrogen Dynamics
article

Continental-scale drivers of soil microbial extracellular polymeric substances

Wolfgang D. Wanek, Lisa Noll, Yuntao Hu, Honghua Ruan, Baorong Wang, Qing Zheng, Shasha Zhang, Ke Shi
article en

Abstract

Extracellular polymeric substances (EPS) are key microbial residues that contribute to soil organic carbon (SOC) and promote soil aggregation. Yet, their abundance and large-scale controls have only begun to be investigated. We conduct extensive soil sampling across a European transect spanning diverse climates, bedrocks, and land uses. Average soil EPS content is 956 ± 55 µg g<sup>-1</sup> soil (n= 92 sites), with EPS-carbon (EPS-C) contributing 1.6 ± 0.1% to SOC. Bedrock influences EPS content, EPS-C contribution to SOC, and the EPS-C/microbial biomass carbon (MBC) ratio, whereas land use mainly affects the latter two. The EPS-C/MBC ratio is negatively correlated with microbial growth and carbon use efficiency, and increases under water deficit, while EPS increases with MBC, clay content, and exchangeable calcium. Our results demonstrate that EPS represents a functionally important microbial residue, regulated by climatic, edaphic, microbial, and land-use factors, with significant implications for soil carbon cycling and sequestration.

Nature Communications
University of Vienna (AT), Nanjing Forestry University (CN), German Centre for Integrative Biodiversity Research (DE), Institute of Soil and Water Conservation (CN), Terrestrial Ecosystem Research Network (AU), Leipzig University (DE)
Austrian Science Fund, China Scholarship Council, National Key Research and Development Program of China
Openalex Percentile: Top 40%
Soil Carbon and Nitrogen Dynamics
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