Abstract
Soils harbor the most diverse naturally evolved antibiotic resistance genes (ARGs) on Earth, with implications for human health and ecosystem functioning. How ARGs evolve as soils develop over centuries, to millennia (i.e., pedogenesis), remains poorly understood, which introduces uncertainty in predictions of the dynamics of ARGs under changing environmental conditions. Here we investigated changes in the soil resistome by analyzing 16 globally distributed soil chronosequences, from centuries to millennia, spanning a wide range of ecosystem types and substrate age ranges. We show that ARG abundance and diversity decline only after millions of years of soil development as observed in very old chronosequences. Moreover, our data show increases in soil organic carbon content and microbial biomass as soil develops that were negatively correlated with the abundance and diversity of soil ARGs. This work reveals natural dynamics of soil ARGs during pedogenesis and suggests that such ecological patterns are predictable, which together advances our understanding of the environmental drivers of ARGs in terrestrial environments.
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Acknowledgements
QL-C and HW-H thank the Australia Research Council (DP210100332, DE210100271) for the projects. We thank the researchers involved in the CLIMIFUN project for the help with soil sampling.
Funding
This project has received funding from the European Union’s Horizon 2020 research and innovation program under the Marie Sklodowska-Curie grant agreement no. 702057. MD-B is supported by a project from the Spanish Ministry of Science and Innovation (PID2020-115813RA-I00), and a project PAIDI 2020 from the Junta de Andalucía (P20_00879).
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QL-C, HW-H and MD-B conceived the idea of this study. MDB and HW-H conducted soil samplings and processing. QL-C conducted statistical analysis and modeling. The manuscript was written by QL-C, edited by HW-H and MD-B, and all co-authors contributed revisions.
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Chen, QL., Hu, HW., Yan, ZZ. et al. Cross-biome antibiotic resistance decays after millions of years of soil development. ISME J 16, 1864–1867 (2022). https://doi.org/10.1038/s41396-022-01225-8
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DOI: https://doi.org/10.1038/s41396-022-01225-8
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