High stability and metabolic capacity of bacterial community promote the rapid reduction of easily decomposing carbon in soil.

ABSTRACT: Irreversible climate change alters the decomposition and sequestration of soil carbon (C). However, the stability of C components in soils with different initial organic matter contents and its relationship with the response of major decomposers to climate warming are still unclear. In this study, we translocated Mollisols with a gradient of organic matter (OM) contents (2%-9%) from in situ cold region to five warmer climatic regions to simulate climate change. Soil C in C-rich soils (OM >5%) was more vulnerable to translocation warming than that in C-poor soils (OM ≤ 5%), with a major loss of functional groups like O-alkyl, O-aryl C and carboxyl C. Variations of microbial β diversity with latitude, temperature and precipitation indicated that C-rich soils contained more resistant bacteria

SUBMITTER: Huang R 

PROVIDER: S-EPMC8654823 | biostudies-literature | 2021 Dec

REPOSITORIES: biostudies-literature