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酸性矿山排水微生物群落的季节性变化。

Seasonal variation in an acid mine drainage microbial community.

作者信息

Auld Ryan R, Mykytczuk Nadia C S, Leduc Leo G, Merritt Thomas J S

机构信息

a Department of Chemistry and Biochemistry, Laurentian University, Sudbury, ON P3E 2C6, Canada.

b School of the Environment, Laurentian University, Sudbury, ON P3E 2C6, Canada.

出版信息

Can J Microbiol. 2017 Feb;63(2):137-152. doi: 10.1139/cjm-2016-0215. Epub 2016 Sep 27.

DOI:10.1139/cjm-2016-0215
PMID:28071137
Abstract

Environmental oxidation and microbial metabolism drive production of acid mine drainage (AMD). Understanding changes in the microbial community, due to geochemical and seasonal characteristics, is fundamental to AMD monitoring and remediation. Using direct sequencing of the 16S and 18S rRNA genes to identify bacterial, archaeal, and eukaryotic members of the microbial community at an AMD site in Northern Ontario, Canada, we found a dynamic community varying significantly across winter and summer sampling times. Community composition was correlated with physical and chemical properties, including water temperature, pH, conductivity, winter ice thickness, and metal concentrations. Within Bacteria, Acidithiobacillus was the dominant genus during winter (11%-57% of sequences) but Acidiphilium was dominant during summer (47%-87%). Within Eukarya, Chrysophyceae (1.5%-94%) and Microbotrymycetes (8%-92%) dominated the winter community, and LKM11 (4%-62%) and Chrysophyceae (25%-87%) the summer. There was less diversity and variability within the Archaea, with similar summer and winter communities mainly comprising Thermoplasmata (33%-64%) and Thermoprotei (5%-20%) classes but also including a large portion of unclassified reads (∼40%). Overall, the active AMD community varied significantly between winter and summer, with changing community profiles closely correlated to specific differences in AMD geochemical and physical properties, including pH, water temperature, ice thickness, and sulfate and metal concentrations.

摘要

环境氧化和微生物代谢推动了酸性矿山排水(AMD)的产生。了解由于地球化学和季节特征导致的微生物群落变化,对于AMD的监测和修复至关重要。通过对加拿大安大略省北部一个AMD场地的微生物群落中的细菌、古菌和真核生物成员进行16S和18S rRNA基因的直接测序,我们发现了一个动态群落,其在冬季和夏季采样时间之间存在显著差异。群落组成与物理和化学性质相关,包括水温、pH值、电导率、冬季冰厚度和金属浓度。在细菌中,嗜酸氧化硫硫杆菌在冬季占主导地位(序列的11%-57%),但嗜酸菌在夏季占主导地位(47%-87%)。在真核生物中,金藻纲(1.5%-94%)和微球黑粉菌纲(8%-92%)在冬季群落中占主导地位,而LKM11(4%-62%)和金藻纲(25%-87%)在夏季占主导地位。古菌内部的多样性和变异性较小,夏季和冬季群落相似,主要由嗜热质体纲(33%-64%)和嗜热栖热菌纲(5%-20%)组成,但也包括很大一部分未分类的读数(约40%)。总体而言,活跃的AMD群落在冬季和夏季之间存在显著差异,群落概况的变化与AMD地球化学和物理性质的特定差异密切相关,包括pH值、水温、冰厚度以及硫酸盐和金属浓度

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