Villeneuve Karine, Turcotte-Blais Valérie, Lazar Cassandre Sara
Department of Biological Sciences, University of Québec at Montréal, UQAM, C.P. 8888, Succ. Centre-Ville, Montreal, QC H3C 3P8, Canada.
Microorganisms. 2023 Jun 8;11(6):1526. doi: 10.3390/microorganisms11061526.
Events of groundwater recharge are associated with changes in the composition of aquifer microbial communities but also abiotic conditions. Modification in the structure of the community can be the result of different environmental condition favoring or hindering certain taxa, or due to the introduction of surface-derived taxa. Yet, in both cases, the local hydrogeochemical settings of the aquifer is likely to affect the amount of variation observed. Therefore, in our study, we used 16S rRNA gene sequencing to assess how microbial communities change in response to snowmelt and the potential connectivity between subsurface and surface microbiomes in two distinct aquifers located in the region of Vaudreuil-Soulanges (Québec, Canada). At both sites, we observed an increase in groundwater level and decrease in temperature following the onset of snow melt in March 2019. Bacterial community composition of each aquifer was significantly different ( < 0.05) between samples collected prior and after groundwater recharge. Furthermore, microbial source tracking results suggested a low contribution of surface environments to the groundwater microbiome except for in the months associated with recharge (March 2019 and April 2019). Overall, despite differences in soil permeability between both sites, the period of snow melt was followed by important changes in the composition of microbial communities from aquifers.
地下水补给事件不仅与含水层微生物群落组成的变化有关,还与非生物条件的变化有关。群落结构的改变可能是由于不同的环境条件有利于或阻碍某些分类群,或者是由于引入了来自地表的分类群。然而,在这两种情况下,含水层的局部水文地球化学环境都可能影响观察到的变化量。因此,在我们的研究中,我们使用16S rRNA基因测序来评估微生物群落在融雪过程中的变化,以及位于加拿大魁北克省沃德勒伊 - 索朗热地区的两个不同含水层中地下和地表微生物群落之间的潜在连通性。在两个地点,我们都观察到2019年3月融雪开始后地下水位上升和温度下降。在地下水补给之前和之后采集的样本中,每个含水层的细菌群落组成都有显著差异(<0.05)。此外,微生物源追踪结果表明,除了与补给相关的月份(2019年3月和2019年4月)外,地表环境对地下水微生物群落的贡献较低。总体而言,尽管两个地点的土壤渗透率不同,但融雪期之后含水层微生物群落的组成发生了重要变化。