Wu Xiaoqin, Wu Liyou, Liu Yina, Zhang Ping, Li Qinghao, Zhou Jizhong, Hess Nancy J, Hazen Terry C, Yang Wanli, Chakraborty Romy
Earth and Environmental Sciences, Lawrence Berkeley National Laboratory, Berkeley, CA, United States.
Institute for Environmental Genomics, Department of Microbiology and Plant Biology, The University of Oklahoma, Norman, OK, United States.
Front Microbiol. 2018 Jun 8;9:1234. doi: 10.3389/fmicb.2018.01234. eCollection 2018.
Knowledge of dynamic interactions between natural organic matter (NOM) and microbial communities is critical not only to delineate the routes of NOM degradation/transformation and carbon (C) fluxes, but also to understand microbial community evolution and succession in ecosystems. Yet, these processes in subsurface environments are usually studied independently, and a comprehensive view has been elusive thus far. In this study, we fed sediment-derived dissolved organic matter (DOM) to groundwater microbes and continually analyzed microbial transformation of DOM over a 50-day incubation. To document fine-scale changes in DOM chemistry, we applied high-resolution Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) and soft X-ray absorption spectroscopy (sXAS). We also monitored the trajectory of microbial biomass, community structure and activity over this time period. Together, these analyses provided an unprecedented comprehensive view of interactions between sediment-derived DOM and indigenous subsurface groundwater microbes. Microbial decomposition of labile C in DOM was immediately evident from biomass increase and total organic carbon (TOC) decrease. The change of microbial composition was closely related to DOM turnover: microbial community in early stages of incubation was influenced by relatively labile tannin- and protein-like compounds; while in later stages the community composition evolved to be most correlated with less labile lipid- and lignin-like compounds. These changes in microbial community structure and function, coupled with the contribution of microbial products to DOM pool affected the further transformation of DOM, culminating in stark changes to DOM composition over time. Our study demonstrates a distinct response of microbial communities to biotransformation of DOM, which improves our understanding of coupled interactions between sediment-derived DOM, microbial processes, and community structure in subsurface groundwater.
了解天然有机物(NOM)与微生物群落之间的动态相互作用不仅对于描绘NOM降解/转化途径和碳(C)通量至关重要,而且对于理解生态系统中微生物群落的演化和演替也至关重要。然而,地下环境中的这些过程通常是独立研究的,迄今为止尚未形成全面的观点。在本研究中,我们将沉积物来源的溶解有机物(DOM)投喂给地下水微生物,并在50天的培养期内持续分析DOM的微生物转化情况。为了记录DOM化学的精细尺度变化,我们应用了高分辨率傅里叶变换离子回旋共振质谱(FT-ICR MS)和软X射线吸收光谱(sXAS)。我们还监测了这段时间内微生物生物量、群落结构和活性的变化轨迹。这些分析共同提供了沉积物来源的DOM与本地地下水中微生物之间相互作用的前所未有的全面观点。DOM中不稳定碳的微生物分解从生物量增加和总有机碳(TOC)减少中立即显现出来。微生物组成的变化与DOM周转密切相关:培养早期的微生物群落受相对不稳定的单宁和蛋白质类化合物影响;而在后期,群落组成的演变与较不稳定的脂质和木质素类化合物最相关。微生物群落结构和功能的这些变化,加上微生物产物对DOM库的贡献,影响了DOM的进一步转化,最终导致DOM组成随时间发生显著变化。我们的研究证明了微生物群落对DOM生物转化的独特响应,这增进了我们对沉积物来源的DOM、微生物过程和地下水中群落结构之间耦合相互作用的理解。