Zhang Yuchen, Plymale Andrew, Son Jiyoung, Huang Qiaoyun, Chen Wenli, Yu Xiao-Ying
National Research Center for Edible Fungi Biotechnology and Engineering, Key Laboratory of Applied Mycological Resources and Utilization, Ministry of Agriculture, Shanghai Key Laboratory of Agricultural Genetics and Breeding, Institute of Edible Fungi, Shanghai Academy of Agricultural Sciences, Shanghai, China.
State Key Laboratory of Agricultural Microbiology, Huazhong Agricultural University, Wuhan, China.
Front Chem. 2023 May 25;11:1203314. doi: 10.3389/fchem.2023.1203314. eCollection 2023.
The interactions between soil microorganisms and soil minerals play a crucial role in the formation and evolution of minerals and the stability of soil aggregates. Due to the heterogeneity and diversity of the soil environment, the under-standing of the functions of bacterial biofilms in soil minerals at the microscale is limited. A soil mineral-bacterial biofilm system was used as a model in this study, and it was analyzed by time-of-flight secondary ion mass spectrometry (ToF-SIMS) to acquire molecular level information. Static culture in multi-wells and dynamic flow-cell culture in microfluidics of biofilms were investigated. Our results show that more characteristic molecules of biofilms can be observed in SIMS spectra of the flow-cell culture. In contrast, biofilm signature peaks are buried under the mineral components in SIMS spectra in the static culture case. Spectral overlay was used in peak selection prior to performing Principal component analysis (PCA). Comparisons of the PCA results between the static and flow-cell culture show more pronounced molecular features and higher loadings of organic peaks of the dynamic cultured specimens. For example, fatty acids secreted from bacterial biofilm extracellular polymeric substance are likely to be responsible for biofilm dispersal due to mineral treatment up to 48 h. Such findings suggest that the use of microfluidic cells to dynamically culture biofilms be a more suitable method for reducing the matrix effect arisen from the growth medium and minerals as a perturbation fac-tor for improved spectral and multivariate analysis of complex mass spectral data in ToF-SIMS. These results show that the interaction mechanism between biofilms and soil minerals at the molecular level can be better studied using the flow-cell culture and advanced mass spectral imaging techniques like ToF-SIMS.
土壤微生物与土壤矿物质之间的相互作用在矿物质的形成与演化以及土壤团聚体的稳定性方面发挥着关键作用。由于土壤环境的异质性和多样性,在微观尺度上对土壤矿物质中细菌生物膜功能的了解有限。本研究以土壤矿物质 - 细菌生物膜系统为模型,采用飞行时间二次离子质谱(ToF - SIMS)进行分析以获取分子水平信息。研究了生物膜在多孔板中的静态培养以及微流控中的动态流动池培养。我们的结果表明,在流动池培养的ToF - SIMS光谱中可以观察到更多生物膜的特征分子。相比之下,在静态培养情况下,生物膜特征峰被掩埋在矿物质成分之下。在进行主成分分析(PCA)之前,使用光谱叠加进行峰选择。静态培养和流动池培养的PCA结果比较表明,动态培养样本的分子特征更明显,有机峰的载荷更高。例如,细菌生物膜胞外聚合物分泌的脂肪酸可能在长达48小时的矿物质处理后导致生物膜分散。这些发现表明,使用微流控细胞动态培养生物膜是一种更合适的方法,可减少生长培养基和矿物质作为干扰因素产生的基质效应,以改善ToF - SIMS中复杂质谱数据的光谱和多变量分析。这些结果表明,使用流动池培养和ToF - SIMS等先进的质谱成像技术可以更好地研究生物膜与土壤矿物质在分子水平上的相互作用机制。