4.7 Article

Deciphering the dual role of bacterial communities in stabilizing rhizosphere priming effect under intra-annual change of growing seasons

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 903, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2023.166777

Keywords

Functional genes; Growing season; Microbial metabolic limitation; Multiple cropping; Rhizosphere priming effect; Soil organic carbon

Ask authors/readers for more resources

The rhizosphere priming effect (RPE) is a phenomenon that affects carbon turnover in plant-soil systems. This study investigated the impact of seasonal changes on RPE and soil carbon by planting maize in paddy soil during two growing seasons in southern China. The results showed that microbial metabolism was limited by different factors in different seasons, but both seasons exhibited positive RPE. The study also revealed the simultaneous response and adaptation of microbial communities to seasonal changes.
The rhizosphere priming effect (RPE) is a widely observed phenomenon affecting carbon (C) turnover in plantsoil systems. While multiple cropping and seasonal changes can have significant impacts on RPE, the mechanisms driving these processes are complex and not yet fully understood. Here, we planted maize in paddy soil during two growing seasons having substantial temperature differences [May-August (warm season, 26.6 degrees C) and September-November (cool season, 23.1 degrees C)] within the same calendar year in southern China to examine how seasonal changes affect RPEs and soil C. We identified sources of C emissions by quantifying the natural abundance of 13C and determined microbial metabolic limitations or efficiency and functional genes related to C cycling using an enzyme-based biogeochemical equilibrium model and high-throughput quantitative PCR-based chip technology, respectively. Results showed that microbial metabolism was mainly limited by phosphorus in the warm season, but by C in the cool season, resulting in positive RPEs in both growing seasons, but no significant differences (9.02 vs. 6.27 mg C kg-1 soil day-1). The RPE intensity remained stable as temperature increased (warm season compared to a cool season), which can be largely explained by the simultaneous increase in the abundance of functional genes related to both C degradation and fixation. Our study highlights the simultaneous response and adaptation of microbial communities to seasonal changes and hence contributes to an understanding and prediction of microbially mediated soil C turnover under multiple cropping systems.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available