School of Metallurgy and Environment, Central South University, Changsha 410083, China.
School of Metallurgy and Environment, Central South University, Changsha 410083, China.
J Hazard Mater. 2024 Jul 15;473:134647. doi: 10.1016/j.jhazmat.2024.134647. Epub 2024 May 17.
Microbially-driven soil formation process is an emerging technology for the ecological rehabilitation of alkaline tailings. However, the dominant microorganisms and their specific roles in soil formation processes remain unknown. Herein, a 1-year field-scale experiment was applied to demonstrate the effect of nitrogen input on the structure and function of the microbiome in alkaline bauxite residue. Results showed that the contents of nutrient components were increased with Penicillium oxalicum (P. oxalicum) incorporation, as indicated by the increasing of carbon and nitrogen mineralization and enzyme metabolic efficiency. Specifically, the increasing enzyme metabolic efficiency was associated with nitrogen input, which shaped the microbial nutrient acquisition strategy. Subsequently, we evidenced that P. oxalicum played a significant role in shaping the assemblages of core bacterial taxa and influencing ecological functioning through intra- and cross-kingdom network analysis. Furthermore, a recruitment experiment indicated that nitrogen enhanced the enrichment of core microbiota (Nitrosomonas, Bacillus, Pseudomonas, and Saccharomyces) and may provide benefits to fungal community bio-diversity and microbial network stability. Collectively, these results demonstrated nitrogen-based coexistence patterns among P. oxalicum and microbiome and revealed P. oxalicum-mediated nutrient dynamics and ecophysiological adaptations in alkaline microhabitats. It will aid in promoting soil formation and ecological rehabilitation of bauxite residue. ENVIRONMENT IMPLICATION: Bauxite residue is a highly alkaline solid waste generated during the Bayer process for producing alumina. Attempting to transform bauxite residue into a stable soil-like substrate using low-cost microbial resources is a highly promising engineering. However, the dominant microorganisms and their specific roles in soil formation processes remain unknown. In this study, we evidenced the nitrogen-based coexistence patterns among Penicillium oxalicum and microbiome and revealed Penicillium oxalicum-mediated nutrient dynamics and ecophysiological adaptations in alkaline microhabitats. This study can improve the understanding of core microbes' assemblies that affect the microbiome physiological traits in soil formation processes.
微生物驱动的土壤形成过程是一种新兴的碱性尾矿生态修复技术。然而,主导微生物及其在土壤形成过程中的具体作用尚不清楚。在此,进行了为期一年的野外尺度实验,以证明氮输入对碱性铝土矿尾矿微生物组结构和功能的影响。结果表明,随着添加草酸青霉(P. oxalicum),营养成分的含量增加,表现在碳和氮矿化以及酶代谢效率增加。具体而言,酶代谢效率的增加与氮输入有关,这塑造了微生物的养分获取策略。随后,我们通过种间和种内的互作网络分析证实,草酸青霉通过塑造核心细菌分类群的组合以及影响生态功能,在塑造微生物组方面发挥了重要作用。此外,招募实验表明,氮增强了核心微生物群(亚硝化单胞菌、芽孢杆菌、假单胞菌和酿酒酵母)的富集,并可能有益于真菌群落生物多样性和微生物网络稳定性。总的来说,这些结果表明了草酸青霉和微生物组之间基于氮的共存模式,并揭示了草酸青霉介导的碱性小生境中的养分动态和生理生态适应。这将有助于促进铝土矿尾矿的土壤形成和生态修复。环境意义:铝土矿是拜耳法生产氧化铝过程中产生的一种高碱性固体废物。尝试使用低成本微生物资源将铝土矿尾矿转化为稳定的类似土壤的基质是一种很有前途的工程。然而,主导微生物及其在土壤形成过程中的具体作用尚不清楚。在这项研究中,我们证明了草酸青霉和微生物组之间基于氮的共存模式,并揭示了草酸青霉介导的碱性小生境中的养分动态和生理生态适应。本研究可以提高对影响土壤形成过程中微生物组生理特性的核心微生物组合的理解。