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首页> 外文期刊>Hydrogeology journal >Environmental factors controlling the spatiotemporal distribution of microbial communities in a coastal, sandy aquifer system (Do_ana, southwest Spain)
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Environmental factors controlling the spatiotemporal distribution of microbial communities in a coastal, sandy aquifer system (Do_ana, southwest Spain)

机译:控制沿海沙质含水层系统中微生物群落的时空分布的环境因素(西班牙西南部的Do_ana)

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摘要

Currently, aquifers are considered to be ecosystems that interchange materials and energy with other systems located in their surroundings. The aquifer system of Do_ana (southwest Spain) has been studied over recent decades from a hydrogeological point of view, although nothing is known about its biological or ecological aspects. In order to describe the general characteristics of its microbial communities, bacterial abundance, cell biomass, bacterial biomass and microbial activities of functional groups were investigated by sampling, over a 2- year period, 13 wells located in the vicinity of four very productive shallow lakes in the most superficial part of this coastal, sandy aquifer system. Multivariate analysis of variance (MANOVA) indicated differences in abundance and biomass variables among sampling locations, seasons and sampling locations × seasons. Principal component analysis showed that temperature and dissolved oxygen appeared to be the most important factors controlling the temporal variability of microbial communities. Hydrological connectivity between surface water and groundwater was important in the control of the spatiotemporal distribution of microbial communities. Due to this hydrological connection, the aquifer system and the wetlands constitute a unique entity, a unique ecosystem, called the “hydroecosystem”, where microbial communities could play a central ecological role.
机译:当前,含水层被认为是与周围环境中的其他系统交换物质和能量的生态系统。尽管水生生物及其生态方面的信息尚不清楚,但近几十年来从水文地质学角度研究了多纳那(西班牙西南部)的含水层系统。为了描述其微生物群落的一般特征,通过在两年内对四个高产浅湖附近的13口井进行采样,研究了功能群的细菌丰度,细胞生物量,细菌生物量和微生物活性。在这个沿海的含沙含水层系统的最表面部分。多变量方差分析(MANOVA)表明,采样位置,季节和采样位置×季节之间的丰度和生物量变量存在差异。主成分分析表明,温度和溶解氧似乎是控制微生物群落时间变化的最重要因素。地表水和地下水之间的水文连通性对于控制微生物群落的时空分布很重要。由于这种水文联系,含水层系统和湿地构成了一个独特的实体,一个独特的生态系统,称为“水生态系统”,微生物群落可以在其中发挥核心的生态作用。

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