Soil bacterial diversity mediated by microscale aqueous-phase processes across biomes

Soil bacterial diversity varies across biomes with potential impacts on soil ecological functioning. Here, we incorporate key factors that affect soil bacterial abundance and diversity across spatial scales into a mechanistic modeling framework considering soil type, carbon inputs and climate toward...

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Bibliographic Details
Published in:Nature communications Vol. 11; no. 1; p. 116
Main Authors: Bickel, Samuel, Or, Dani
Format: Journal Article
Language:English
Published: London Nature Publishing Group UK 08-01-2020
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Summary:Soil bacterial diversity varies across biomes with potential impacts on soil ecological functioning. Here, we incorporate key factors that affect soil bacterial abundance and diversity across spatial scales into a mechanistic modeling framework considering soil type, carbon inputs and climate towards predicting soil bacterial diversity. The soil aqueous-phase content and connectivity exert strong influence on bacterial diversity for each soil type and rainfall pattern. Biome-specific carbon inputs deduced from net primary productivity provide constraints on soil bacterial abundance independent from diversity. The proposed heuristic model captures observed global trends of bacterial diversity in good agreement with predictions by an individual-based mechanistic model. Bacterial diversity is highest at intermediate water contents where the aqueous phase forms numerous disconnected habitats and soil carrying capacity determines level of occupancy. The framework delineates global soil bacterial diversity hotspots; located mainly in climatic transition zones that are sensitive to potential climate and land use changes. Numerous micro- and macro-scale factors influence soil microbial diversity. Here the authors create a model to demonstrate that fine scale soil moisture influences the carrying capacity of microbes, which then scales up to larger biogeographic patterns.
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ISSN:2041-1723
2041-1723
DOI:10.1038/s41467-019-13966-w