A Combination of Genomics, Transcriptomics, and Genetics Provides Insights into the Mineral Weathering Phenotype of Pseudomonas azotoformans F77

• Published in: Applied and environmental microbiology Vol. 87; no. 24; p. e0155221
• Main Authors: Wang, Yuan-Li, Dong, Wen, Xiang, Kai-Xiang, Wang, Qi, He, Lin-Yan, Sheng, Xia-Fang
• Format: Journal Article
• Language: English
• Published: United States American Society for Microbiology 24.11.2021
• Subjects: Acids; Biosynthesis; Biotite; Efflux; Flagella; Genes; Genetics; Genomics; Geomicrobiology; Gluconic acid; Iron; Metabolic pathways; Metabolism; Minerals - metabolism; Mutants; Phenotype; Phenotypes; Protons; Pseudomonas; Pseudomonas - genetics; Pseudomonas - metabolism; Silicates - metabolism; Soil formation; Transcriptome; Transcriptomics; Weathering; transcriptomics; differentially expressed genes; genes involved in mineral weathering; genes related to acid tolerance; mineral-weathering Pseudomonas azotoformans
• ISSN: 0099-2240; 1098-5336
• DOI: 10.1128/AEM.01552-21

Silicate mineral weathering (dissolution) plays important roles in soil formation and global biogeochemical cycling. In this study, a combination of genomics, transcriptomics, and genetics was used to identify the molecular basis of mineral weathering activity and acid tolerance in Pseudomonas azotoformans F77. Biotite was chosen as a silicate mineral to investigate mineral weathering. The genome of strain F77 was sequenced, and the genes significantly upregulated when grown in the presence of biotite included mineral weathering-related genes associated with gluconic acid metabolism, flagellar assembly, and pilus biosynthesis and acid tolerance-related genes associated with neutralizing component production, reducing power, and proton efflux. The biotite-weathering behaviors of strain F77 and its mutants that were created by deleting the , , and genes, which are involved in gluconic acid metabolism, and the , , and genes, which are involved in acid tolerance, were determined. The Fe and Al concentrations in the strain F77-inoculated medium increased 2.2- to 13.7-fold compared to the controls. The cell numbers of strain F77 increased over time, while the pH values in the medium ranged from 3.75 to 3.90 between 20 and 36 h of incubation. The release of Al and Fe was significantly reduced in the F77 Δ , F77 Δ , F77 Δ , and F77 Δ mutants. Bacterial growth was significantly reduced in the presence of biotite in the F77 Δ and F77 Δ mutants. Our results demonstrated the acid tolerance of strain F77 and suggested that multiple genes and metabolic pathways in strain F77 are involved in biotite weathering and acid tolerance during the mineral weathering process. Acid production and tolerance play important roles in effective and persistent mineral weathering in bacteria, although the molecular mechanisms governing acid production and acid tolerance in bacteria have not been fully elucidated. In this study, the molecular mechanisms underlying biotite (as a silicate mineral) weathering (dissolution) and acid tolerance of F77 were characterized using genomics, transcriptomics, and genetics analyses. Our results showed that the genes and metabolic pathways for gluconic acid metabolism, flagellar assembly, and pilus biosynthesis may play important roles in mineral weathering by strain F77. Notably, the genes associated with neutralizing component production, reducing power, and proton efflux may be related to acid tolerance in strain F77. The expression of these acid production- and acid tolerance-related genes was observed to be increased by biotite in strain F77. Our findings may help to elucidate the molecular mechanisms governing mineral weathering and, especially, acid tolerance in mineral-weathering bacteria.