Geomicrobiology Laboratory, State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China; School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China.
Geomicrobiology Laboratory, State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China; Department of Geology and Environmental Earth Science, Miami University, Oxford, OH 45056, USA.
Environ Pollut. 2017 Apr;223:507-516. doi: 10.1016/j.envpol.2017.01.052. Epub 2017 Jan 26.
Acid mine drainage (AMD),characterized by strong acidity and high metal concentrations, generates from the oxidative dissolution of metal sulfides, and acidophiles can accelerate the process significantly. Despite extensive research in microbial diversity and community composition, little is known about seasonal variations of microbial community structure (especially micro eukaryotes) in response to environmental conditions in AMD ecosystem. To this end, AMD samples were collected from Nanshan AMD lake, Anhui Province, China, over a full seasonal cycle from 2013 to 2014, and water chemistry and microbial composition were studied. pH of lake water was stable (∼3.0) across the sampling period, while the concentrations of ions varied dramatically. The highest metal concentrations in the lake were found for Mg and Al, not commonly found Fe. Unexpectedly, ultrahigh concentration of chlorophyll a was measured in the extremely acidic lake, reaching 226.43-280.95 μg/L in winter, even higher than those in most eutrophic freshwater lakes. Both prokaryotic and eukaryotic communities showed a strong seasonal variation. Among the prokaryotes, "Ferrovum", a chemolithotrophic iron-oxidizing bacterium was predominant in most sampling seasons, although it was a minor member prior to September, 2012. Fe was the initial geochemical factor that drove the variation of the prokaryotic community. The eukaryotic community was simple but varied more drastically than the prokaryotic community. Photoautotrophic algae (primary producers) formed a food web with protozoa or flagellate (top consumers) across all four seasons, and temperature appeared to be responsible for the observed seasonal variation. Ochromonas and Chlamydomonas (responsible for high algal bloom in winter) occurred in autumn/summer and winter/spring seasons, respectively, because of their distinct growth temperatures. The closest phylogenetic relationship between Chlamydomonas species in the lake and those in Arctic and Alpine suggested that the native Chlamydomonas species may have been both acidophilic and psychrophilic after a long acclimation time in this extreme environment.
酸性矿山排水(AMD)的特征是强酸性和高金属浓度,由金属硫化物的氧化溶解产生,而嗜酸菌可以显著加速这一过程。尽管对微生物多样性和群落组成进行了广泛的研究,但对于微生物群落结构(尤其是微真核生物)对 AMD 生态系统环境条件的季节性变化知之甚少。为此,从 2013 年到 2014 年,在中国安徽南山 AMD 湖采集了 AMD 样品,进行了整个季节性周期的研究,研究了水化学和微生物组成。湖水的 pH 值在整个采样期间保持稳定(约 3.0),而离子浓度则变化剧烈。湖中金属浓度最高的是 Mg 和 Al,而不是常见的 Fe。出乎意料的是,在极其酸性的湖中测量到超高浓度的叶绿素 a,冬季达到 226.43-280.95μg/L,甚至高于大多数富营养化淡水湖中叶绿素 a 的浓度。原核生物和真核生物群落都表现出强烈的季节性变化。在原核生物中,“Ferrovum”是一种化能自养铁氧化细菌,在大多数采样季节都占主导地位,尽管在 2012 年 9 月之前它是一个次要成员。Fe 是驱动原核生物群落变化的初始地球化学因素。真核生物群落虽然简单,但比原核生物群落变化更为剧烈。光能自养藻类(初级生产者)与原生动物或鞭毛虫(顶级消费者)形成了一个食物网,横跨四季,而温度似乎是造成观察到的季节性变化的原因。Ochromonas 和 Chlamydomonas(导致冬季藻类大量繁殖)分别出现在秋季/夏季和冬季/春季,因为它们的生长温度不同。湖中 Chlamydomonas 物种与北极和高山的 Chlamydomonas 物种之间最接近的系统发育关系表明,在这种极端环境中经过长时间的适应后,本地 Chlamydomonas 物种可能既嗜酸又嗜冷。