In general terms, the metabolic theory of ecology links rates of organism diversification (i.e., the metabolic rate of an organism) with the organisms' body size and body temperature, explained Dini-Andreote. Building upon the factors that are parametrized in the MTE, the researchers introduced variation in local pH as an additional variable that acts as a stringent selective filter of biodiversity in soils, impacting the species of microbes acting and surviving in the soil.
By considering all these factors—the metabolic rate, mass, and temperature as well as pH—the researchers were able to capture and account for previously unexplained variation in the relationship between soil edaphic properties (the physical, chemical, and biological properties of the soil), temperature, and biogeographical patterns of bacterial diversity. The team then continued to test and validate their models across multiple scales—such as single bacterial strain diversification rates, local and continental scale soil communities—yielding robust results.
"By layering these models, researchers can start to better understand patterns of microbial distribution in soils and start to answer long-standing questions in this field, such as: 'What determines variation in soil biodiversity?' and "How dynamic changes in soil biodiversity can be modeled and predicted?" said Dini-Andreote.
"With that, we will be able to better harness the genomic and functional potential of these soil microorganisms to effectively manipulate them for desirable outcomes. These outcomes vary from essential ecosystem functions, such as carbon storage in soil, to the manipulation of beneficial plant-associated microorganisms to enhance crop productivity in agriculture."
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