State Key Laboratory of Biogeology and Environmental Geology, Wuhan, 430074, PR China; Hubei Key Laboratory of Yangtze Catchment Environmental Aquatic Science, China University of Geosciences, Wuhan, 430074, PR China.
State Key Laboratory of Biogeology and Environmental Geology, Wuhan, 430074, PR China; Hubei Key Laboratory of Yangtze Catchment Environmental Aquatic Science, China University of Geosciences, Wuhan, 430074, PR China.
Water Res. 2023 Apr 15;233:119734. doi: 10.1016/j.watres.2023.119734. Epub 2023 Feb 12.
Reactive oxygen species (ROS) are ubiquitous in O-perturbed aquifers, but their role in shaping ammonia-oxidizing microbial communities is not clear. This study examined the dynamic responses of ammonia-oxidizing microorganisms (AOMs) in redox-fluctuating aquifers to ROS via field investigation and in-lab verification using transcriptomes/ metatranscriptome and RT-qPCR. Ammonia-oxidizing archaea (AOA) dominated recharge aquifers with lower ROS levels, whereas ammonia-oxidizing bacteria (AOB) and heterotrophic nitrifying aerobic bacteria (HNB) predominated in discharge areas with higher ROS levels. Similar succession in AOM enrichments was found in that the dominant AOMs changed from AOA Nitrosopumilus to AOB Nitrosomonas with increasing ROS. Ammonia oxidation and antioxidant capacity differed significantly among three AOM isolates exposed to ROS. ROS decreased the amoA gene expression of AOA strain Nitrososphaera viennensis PLX03, accompanied by inhibited ammonia oxidation capacity. By contrast, the catalase and superoxide dismutase activities of the AOB strain Nitrosomonas oligotropha PLL12 and HNB strain Pseudomonas aeruginosa PLL01 increased, and the antioxidant genes katG, sodA, ahpC, and ahpF were significantly upregulated. These results demonstrate that ROS exert an important influence on AOMs in redox-fluctuating aquifers. This study improves our understanding of the ecological niches of AOMs in surface/subsurface environments.
活性氧(ROS)在受 O 干扰的含水层中普遍存在,但它们在塑造氨氧化微生物群落中的作用尚不清楚。本研究通过野外调查和使用转录组/宏转录组和 RT-qPCR 对实验室验证,研究了氧化还原波动含水层中氨氧化微生物(AOM)对 ROS 的动态响应。氨氧化古菌(AOA)在 ROS 水平较低的补给含水层中占优势,而氨氧化细菌(AOB)和异养硝化好氧细菌(HNB)在 ROS 水平较高的排放区占优势。在 AOM 富集物中也发现了类似的演替,随着 ROS 的增加,主要的 AOM 从 AOA 的 Nitrosopumilus 变为 AOB 的 Nitrosomonas。暴露于 ROS 下的三种 AOM 分离株的氨氧化和抗氧化能力有显著差异。ROS 降低了 AOA 菌株 Nitrososphaera viennensis PLX03 的 amoA 基因表达,伴随着氨氧化能力的抑制。相比之下,AOB 菌株 Nitrosomonas oligotropha PLL12 和 HNB 菌株 Pseudomonas aeruginosa PLL01 的过氧化氢酶和超氧化物歧化酶活性增加,抗氧化基因 katG、sodA、ahpC 和 ahpF 显著上调。这些结果表明,ROS 对氧化还原波动含水层中的 AOM 产生重要影响。本研究提高了我们对表面/地下环境中 AOM 生态位的理解。