首页> 外文期刊>Applied Microbiology >Stratified Microbial Structure and Activity in Sulfide- and Methane-Producing Anaerobic Sewer Biofilms
【24h】

Stratified Microbial Structure and Activity in Sulfide- and Methane-Producing Anaerobic Sewer Biofilms

机译:产生硫化物和甲烷的厌氧下水道生物膜中的分层微生物结构和活性

获取原文
       

摘要

Simultaneous production of sulfide and methane by anaerobic sewer biofilms has recently been observed, suggesting that sulfate-reducing bacteria (SRB) and methanogenic archaea (MA), microorganisms known to compete for the same substrates, can coexist in this environment. This study investigated the community structures and activities of SRB and MA in anaerobic sewer biofilms (average thickness of 800 μm) using a combination of microelectrode measurements, molecular techniques, and mathematical modeling. It was seen that sulfide was mainly produced in the outer layer of the biofilm, between the depths of 0 and 300 μm, which is in good agreement with the distribution of SRB population as revealed by cryosection-fluorescence in situ hybridization (FISH). SRB had a higher relative abundance of 20% on the surface layer, which decreased gradually to below 3% at a depth of 400 μm. In contrast, MA mainly inhabited the inner layer of the biofilm. Their relative abundances increased from 10% to 75% at depths of 200 μm and 700 μm, respectively, from the biofilm surface layer. High-throughput pyrosequencing of 16S rRNA amplicons showed that SRB in the biofilm were mainly affiliated with five genera, Desulfobulbus , Desulfomicrobium , Desulfovibrio , Desulfatiferula , and Desulforegula , while about 90% of the MA population belonged to the genus Methanosaeta . The spatial organizations of SRB and MA revealed by pyrosequencing were consistent with the FISH results. A biofilm model was constructed to simulate the SRB and MA distributions in the anaerobic sewer biofilm. The good fit between model predictions and the experimental data indicate that the coexistence and spatial structure of SRB and MA in the biofilm resulted from the microbial types and their metabolic transformations and interactions with substrates.
机译:最近已观察到厌氧污水生物膜同时产生硫化物和甲烷,这表明在这种环境中可以共存硫酸盐还原细菌(SRB)和产甲烷古菌(MA)(已知与同一底物竞争的微生物)。这项研究结合了微电极测量,分子技术和数学模型,研究了厌氧污水生物膜(平均厚度为800μm)中SRB和MA的群落结构和活性。可以看出,硫化物主要在生物膜的外层产生,深度在0至300μm之间,这与冷冻切片荧光原位杂交(FISH)所揭示的SRB种群分布非常吻合。 SRB在表层的相对丰度较高,在400μm的深度处逐渐降低至3%以下。相反,MA主要居住在生物膜的内层。在距生物膜表面层200μm和700μm的深度处,它们的相对丰度分别从10%增加到75%。 16S rRNA扩增子的高通量焦磷酸测序表明,生物膜中的SRB主要与5个属有关,即脱硫球,脱硫微生物,脱硫弧菌,脱硫叶和脱硫古拉,而大约90%的MA种群属于Methanosaeta属。焦磷酸测序显示SRB和MA的空间组织与FISH结果一致。构建了生物膜模型来模拟厌氧污水生物膜中的SRB和MA分布。模型预测和实验数据之间的良好拟合表明,生物膜中SRB和MA的共存和空间结构是由微生物类型及其代谢转化以及与底物的相互作用引起的。

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