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Facilitation in the soil microbiome does not necessarily lead to niche expansion

BACKGROUND: The soil microbiome drives soil ecosystem function, and soil microbial functionality is directly linked to interactions between microbes and the soil environment. However, the context-dependent interactions in the soil microbiome remain largely unknown. RESULTS: Using latent variable mod...

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Detalles Bibliográficos
Autores principales: Zhou, Xue, Leite, Márcio F. A., Zhang, Zhenqing, Tian, Lei, Chang, Jingjing, Ma, Lina, Li, Xiujun, van Veen, Johannes A., Tian, Chunjie, Kuramae, Eiko E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: BioMed Central 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8067652/
https://www.ncbi.nlm.nih.gov/pubmed/33902741
http://dx.doi.org/10.1186/s40793-021-00373-2
Descripción
Sumario:BACKGROUND: The soil microbiome drives soil ecosystem function, and soil microbial functionality is directly linked to interactions between microbes and the soil environment. However, the context-dependent interactions in the soil microbiome remain largely unknown. RESULTS: Using latent variable models (LVMs), we disentangle the biotic and abiotic interactions of soil bacteria, fungi and environmental factors using the Qinghai-Tibetan Plateau soil ecosystem as a model. Our results show that soil bacteria and fungi not only interact with each other but also shift from competition to facilitation or vice versa depending on environmental variation; that is, the nature of their interactions is context-dependent. CONCLUSIONS: Overall, elevation is the environmental gradient that most promotes facilitative interactions among microbes but is not a major driver of soil microbial community composition, as evidenced by variance partitioning. The larger the tolerance of a microbe to a specific environmental gradient, the lesser likely it is to interact with other soil microbes, which suggests that facilitation does not necessarily lead to niche expansion. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1186/s40793-021-00373-2.