Interactions between microbial diversity and substrate chemistry determine the fate of carbon in soil.

ABSTRACT: Microbial decomposition drives the transformation of plant-derived substrates into microbial products that form stable soil organic matter (SOM). Recent theories have posited that decomposition depends on an interaction between SOM chemistry with microbial diversity and resulting function (e.g., enzymatic capabilities, growth rates). Here, we explicitly test these theories by coupling quantitative stable isotope probing and metabolomics to track the fate of ¹³C enriched substrates that vary in chemical composition as they are assimilated by microbes and transformed into new metabolic products in soil. We found that differences in forest nutrient economies (e.g., nutrient cycling, microbial competition) led to arbuscular mycorrhizal (AM) soils harboring greater diversity of fungi

SUBMITTER: Raczka NC 

PROVIDER: S-EPMC8481224 | biostudies-literature | 2021 Sep

REPOSITORIES: biostudies-literature