Protists regulate microbially mediated organic carbon turnover in soil aggregates

生态学 生物 环境科学 生态系统 土壤有机质 总有机碳 碳纤维 土壤微生物学 碳循环 土壤碳 土壤科学 环境化学 土壤水分 化学 材料科学 复合数 复合材料
作者
Hao Liao,Xiuli Hao,Yiting Li,Silin Ma,Shenghan Gao,Peng Cai,Wenli Chen,Qiaoyun Huang
出处
期刊:Global Change Biology [Wiley]
卷期号:30 (1): e17102-e17102 被引量:38
标识
DOI:10.1111/gcb.17102
摘要

Abstract Soil protists, the major predator of bacteria and fungi, shape the taxonomic and functional structure of soil microbiome via trophic regulation. However, how trophic interactions between protists and their prey influence microbially mediated soil organic carbon turnover remains largely unknown. Here, we investigated the protistan communities and microbial trophic interactions across different aggregates‐size fractions in agricultural soil with long‐term fertilization regimes. Our results showed that aggregate sizes significantly influenced the protistan community and microbial hierarchical interactions. Bacterivores were the predominant protistan functional group and were more abundant in macroaggregates and silt + clay than in microaggregates, while omnivores showed an opposite distribution pattern. Furthermore, partial least square path modeling revealed positive impacts of omnivores on the C‐decomposition genes and soil organic matter (SOM) contents, while bacterivores displayed negative impacts. Microbial trophic interactions were intensive in macroaggregates and silt + clay but were restricted in microaggregates, as indicated by the intensity of protistan‐bacterial associations and network complexity and connectivity. Cercozoan taxa were consistently identified as the keystone species in SOM degradation‐related ecological clusters in macroaggregates and silt + clay, indicating the critical roles of protists in SOM degradation by regulating bacterial and fungal taxa. Chemical fertilization had a positive effect on soil C sequestration through suppressing SOM degradation‐related ecological clusters in macroaggregate and silt + clay. Conversely, the associations between the trophic interactions and SOM contents were decoupled in microaggregates, suggesting limited microbial contributions to SOM turnovers. Our study demonstrates the importance of protists‐driven trophic interactions on soil C cycling in agricultural ecosystems.
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