首页> 外文期刊>Geobiology >Spatiotemporal distribution of microbial communities in a coastal, sandy aquifer system (Donana, SW Spain)
【24h】

Spatiotemporal distribution of microbial communities in a coastal, sandy aquifer system (Donana, SW Spain)

机译:沿海沙质含水层系统中微生物群落的时空分布(西班牙西南部多纳纳)

获取原文
获取原文并翻译 | 示例
           

摘要

The aquifer system of Donana (SW Spain) represents the most important freshwater source in the Donana Natural Area. Its spatiotemporal dynamics favours the hydrological connection between surface and subsurface ecosystems, and promotes matter fluxes among the different terrestrial and aquatic systems present here. This aquifer has been intensively studied from a hydrogeological point of view but little is known from an ecological perspective. In order to understand the ecological roles played by microbial communities in this system, we conducted a long-term seasonal study of bacterial abundance, cell biomass, bacterial biomass and functional activities over a 2-year period. Bacterial abundance ranged between 2.11 +/- 1.79 x 10(5) and 8.58 +/- 6.99 x 10(7) bacteria mL(-1) groundwater, average cell biomass was estimated to be 77.01 +/- 31.56 fgC and bacterial biomass varied between 8.99 +/- 4.10 x 10(-2) and 5.65 +/- 0.70 microgC mL(-1). Iron-related bacteria showed the highest activities among the functional groups studied. Moreover, among the variables that usually control spatial distributions of microbial communities in aquifer systems, depth did not have a relevant effect on this aquifer, at least in the range of depths studied, but grain size, probably due to its direct effects on hydrogeological parameters, such as permeability or porosity, appeared to exert moderate control, principally in terms of bacterial abundance. Finally, significant seasonal differences in the means of these microbiological variables were also observed; temperature seems to be the main factor controlling the temporal distribution of microbial communities in this aquifer system.
机译:多纳纳(西班牙西南部)的含水层系统是多纳纳自然地区最重要的淡水水源。它的时空动力学有利于表层和地下生态系统之间的水文联系,并促进了这里存在的不同陆地和水生系统之间的物质通量。从水文地质学角度对该水层进行了深入研究,但从生态学角度了解甚少。为了了解微生物群落在该系统中的生态作用,我们进行了为期两年的细菌丰度,细胞生物量,细菌生物量和功能活动的长期季节性研究。细菌丰度介于2.11 +/- 1.79 x 10(5)和8.58 +/- 6.99 x 10(7)细菌mL(-1)地下水之间,平均细胞生物量估计为77.01 +/- 31.56 fgC,细菌生物量变化介于8.99 +/- 4.10 x 10(-2)和5.65 +/- 0.70 microgC mL(-1)之间。与铁有关的细菌在所研究的官能团中表现出最高的活性。此外,在通常控制含水层系统中微生物群落空间分布的变量中,深度对该含水层没有相关影响,至少在研究的深度范围内没有影响,但对晶粒大小可能是由于其对水文地质参数的直接影响诸如渗透性或孔隙度之类的细菌似乎表现出适度的控制,主要是在细菌丰度方面。最后,还观察到了这些微生物变量均值的明显季节性差异。温度似乎是控制该含水层系统中微生物群落时间分布的主要因素。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号