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蓝藻水华显著提高了亚热带分层水库中下层厌氧氨氧化细菌的丰度。

Cyanobacterial bloom significantly boosts hypolimnelic anammox bacterial abundance in a subtropical stratified reservoir.

作者信息

Xue Yuanyuan, Yu Zheng, Chen Huihuang, Yang Jun R, Liu Min, Liu Lemian, Huang Bangqing, Yang Jun

机构信息

Aquatic EcoHealth Group, Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, 361021, China.

University of Chinese Academy of Sciences, Beijing, 100049, China.

出版信息

FEMS Microbiol Ecol. 2017 Oct 1;93(10). doi: 10.1093/femsec/fix118.

Abstract

The degradation of freshwater quality induced by cyanobacterial blooms is a major global environmental concern. Microbially driven nitrogen removal could alleviate eutrophication to some degree in freshwater ecosystems. However, the response of anaerobic ammonium oxidizing (anammox) bacterial communities to cyanobacterial blooms remains poorly understood, especially in reservoir ecosystems. Here we compared the dynamics of anammox bacterial communities during and after a cyanobacterial bloom in a subtropical reservoir. Our data showed that a cyanobacterial bloom triggered a significant increase in bottom anammox bacterial abundance. During the bloom period, anammox bacterial abundance in bottom waters was 9-fold and 52-fold higher compared with non-bloom stratification and mixing periods, respectively. The community composition of anammox bacteria in surface waters changed substantially accompanied by the disappearance of the cyanobacterial bloom, and a shift of dominance from unidentified anammox genera to Ca. Brocadia was observed. Although Ca. Brocadia was always predominant in both middle and bottom waters, the non-bloom period had more unique taxa than the bloom period. Cyanobacterial bloom-related changes in environmental conditions (e.g. NH4-N and total organic carbon) and water stratification together influenced the distribution and dynamics of anammox bacteria. Altogether, our study lays the basis for a better understanding of the breakdown of cyanobacterial blooms in a stratified reservoir.

摘要

蓝藻水华引起的淡水水质退化是一个重大的全球环境问题。微生物驱动的氮去除在一定程度上可以缓解淡水生态系统的富营养化。然而,厌氧氨氧化(anammox)细菌群落对蓝藻水华的响应仍知之甚少,尤其是在水库生态系统中。在此,我们比较了亚热带水库蓝藻水华期间及之后厌氧氨氧化细菌群落的动态变化。我们的数据表明,蓝藻水华引发了底层厌氧氨氧化细菌丰度的显著增加。在水华期间,底层水体中厌氧氨氧化细菌的丰度分别比非水华分层期和混合期高9倍和52倍。随着蓝藻水华的消失,表层水体中厌氧氨氧化细菌的群落组成发生了显著变化,并且观察到优势地位从未鉴定的厌氧氨氧化菌属转变为“Ca. Brocadia”属。尽管“Ca. Brocadia”属在中层和底层水体中始终占主导地位,但非水华期比水华期有更多独特的分类群。与蓝藻水华相关的环境条件变化(如NH4-N和总有机碳)以及水体分层共同影响了厌氧氨氧化细菌的分布和动态。总之,我们的研究为更好地理解分层水库中蓝藻水华的分解奠定了基础。

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