4.7 Article

Long-term organic fertilization promotes the resilience of soil multifunctionality driven by bacterial communities

期刊

SOIL BIOLOGY & BIOCHEMISTRY
卷 177, 期 -, 页码 -

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PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2022.108922

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Long-term fertilization; Temporal resilience; Soil multifunctionality; Copiotrophic taxa; Biodiversity loss; Microbial community

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Long-term intensive fertilization is a global practice that alters soil microbiome and affects the resilience of soil multifunctionality to biodiversity loss. This study found that organic fertilization promotes the resilience of both single functions and soil multifunctionality compared to mineral fertilization. Bacterial diversity is significantly and positively related to multifunctionality, and the diversity-multifunctionality relationships are stronger in organically fertilized soil.
Long-term intensive fertilization is a practice common around the world and gradually alters soil microbiome, however, its influences on the temporal resilience of soil multifunctionality to biodiversity loss and biodiversity-multifunctionality relationships remain poorly understood. Here, we manipulated soil biodiversity using the dilution-to-extinction approach to examine the temporal variability in individual functions, soil multi -functionality and their relationships with bacterial and fungal communities under different fertilization treat-ments during a 90-day re-colonization process. We found that organic fertilization accelerated the resilience of single functions and soil multifunctionality to biodiversity loss compared with mineral fertilization and unfer-tilized control. The fungal community was less resilient than bacterial community to disturbances caused by fertilization and dilution. Bacterial but not fungal diversity was significantly and positively related to multi -functionality, and the strength of the diversity-multifunctionality relationships in organic fertilized soil was 3 -and 67-fold higher than that in unfertilized and mineral fertilized soil, respectively. Both organic and mineral nutrient inputs promoted copiotroph-dominated bacterial assemblages (including Proteobacteria and Bacteroidetes members) and suppressed oligotrophs (mostly Acidobacteria and Chloroflexi), which paralleled multifunctionality resilience patterns in fertilized soils. beta-Diversity of bacterial copiotrophs alone or in combination was signifi-cantly related to changes in multifunctionality. Random forest analysis and structural equation modeling indi-cated that bacterial community diversity and composition along with soil carbon and nitrogen basically determined soil multifunctionality, with 70% of the variance in multifunctionality being explained. Rare taxa from the bacterial copiotrophs were particularly important for maintaining multifunctionality. Our results un-derline the importance of fertilization-induced shifts in microbial ecophysiological strategies for promoting the resilience of soil multifunctionality to biodiversity loss, and the need to preserve the diversity of rare copio-trophic taxa for stable provision of ecosystem functions under future environmental change.

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