Department of Microbiology, University of Granada, Campus Fuentenueva s/n 18071, Granada, Spain.
Sci Total Environ. 2024 Jan 15;908:168284. doi: 10.1016/j.scitotenv.2023.168284. Epub 2023 Nov 2.
Uranium (U) represents the preeminent hazardous radionuclide within the context of nuclear waste repositories. Indigenous microorganisms in bentonite can influence radionuclide speciation and migration in Deep Geological Repositories (DGRs) for nuclear waste storage. While bacterial communities in bentonite samples have been extensively studied, the impact of fungi has been somewhat overlooked. Here, we investigate the geomicrobiological processes in bentonite microcosms amended with uranyl nitrate and glycerol-2-phosphate (G2P) for six-month incubation. ITS sequencing revealed that the fungal community was mainly composed of Ascomycota (96.6 %). The presence of U in microcosms enriched specific fungal taxa, such as Penicillium and Fusarium, potentially associated with uranium immobilization mechanisms. Conversely, the amendment of U into G2P-suplemented samples exhibited minimal impact, resulting in a fungal community akin to the control group. Several fungal strains were isolated from bentonite microcosms to explore their potential in the U biomineralization, including Fusarium oxysporum, Aspergillus sp., Penicillium spp., among others. High Annular Angle Dark-Field Scanning Transmission Electron Microscopy (HAADF) analyses showed the capacity of F. oxysporum B1 to form U-phosphate mineral phases, likely mediated by phosphatase activity. Therefore, our study emphasizes the need to take into account indigenous bentonite fungi in the overall assessment of the impact of microbial processes in the immobilization of U within DGRs environments.
铀(U)是核废料处置库中首要的放射性危险核素。膨润土中的土著微生物会影响深地质处置库(DGR)中核废料储存的放射性核素形态和迁移。尽管膨润土样品中的细菌群落已经得到了广泛的研究,但真菌的影响却有些被忽视了。在这里,我们研究了添加硝酸铀酰和甘油-2-磷酸(G2P)的膨润土微宇宙中的地球微生物过程,进行了为期六个月的孵育。ITS 测序结果表明,真菌群落主要由子囊菌门(96.6%)组成。微宇宙中 U 的存在富集了特定的真菌类群,如青霉属和镰刀菌属,这些类群可能与铀的固定化机制有关。相反,将 U 加入到 G2P 补充的样品中,影响最小,导致真菌群落类似于对照组。从膨润土微宇宙中分离出了几种真菌菌株,以探索它们在 U 生物矿化中的潜力,包括尖孢镰刀菌、曲霉属、青霉属等。高角环形暗场扫描透射电子显微镜(HAADF)分析表明,尖孢镰刀菌 B1 有形成 U 磷酸盐矿物相的能力,可能是通过磷酸酶活性介导的。因此,我们的研究强调了在评估微生物过程对 DGR 环境中 U 固定化的影响时,需要考虑到土著膨润土真菌的作用。