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Seasonal Dynamics of Abundance, Structure, and Diversity of Methanogens and Methanotrophs in Lake Sediments.季节变化对湖底沉积物中产甲烷菌和甲烷营养菌丰度、结构和多样性的影响。
Microb Ecol. 2021 Oct;82(3):559-571. doi: 10.1007/s00248-021-01689-9. Epub 2021 Feb 4.
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Vertical stratification patterns of methanotrophs and their genetic controllers in water columns of oxygen-stratified boreal lakes.分层湖水中甲烷营养菌及其遗传调控因子的垂直分布模式。
FEMS Microbiol Ecol. 2021 Jan 26;97(2). doi: 10.1093/femsec/fiaa252.
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Ecological and genomic analyses of candidate phylum WPS-2 bacteria in an unvegetated soil.未植被土壤中候选门 WPS-2 细菌的生态和基因组分析。
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Growth and rapid succession of methanotrophs effectively limit methane release during lake overturn.甲烷氧化菌的生长和快速演替有效地限制了湖泊翻搅期间甲烷的释放。
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Niche partitioning of methane-oxidizing bacteria along the oxygen-methane counter gradient of stratified lakes.沿分层湖泊氧气-甲烷反梯度分层的甲烷氧化细菌的生态位分割。
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Large-scale biogeography and environmental regulation of methanotrophic bacteria across boreal inland waters.大尺度生物地理学和环境对北方内陆水域甲烷营养菌的调控。
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Temporal variations in turbidity in an oil sands pit lake.油砂矿坑湖浊度的时间变化
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北方油砂矿终坑湖中产甲烷菌的季节性动态。

Seasonal Dynamics of Methanotrophic Bacteria in a Boreal Oil Sands End Pit Lake.

机构信息

Department of Biological Sciences, University of Calgary, Calgary, Alberta, Canada.

Department of Geological Sciences, University of Saskatchewangrid.25152.31, Saskatoon, Saskatchewan, Canada.

出版信息

Appl Environ Microbiol. 2022 Feb 8;88(3):e0145521. doi: 10.1128/AEM.01455-21. Epub 2021 Nov 24.

DOI:10.1128/AEM.01455-21
PMID:34818104
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8824210/
Abstract

Base Mine Lake (BML) is the first full-scale demonstration end pit lake for the oil sands mining industry in Canada. We examined aerobic methanotrophic bacteria over all seasons for 5 years in this dimictic lake. Methanotrophs comprised up to 58% of all bacterial reads in 16S rRNA gene amplicon sequencing analyses (median 2.8%), and up to 2.7 × 10 cells mL of water (median 0.5 × 10) based on qPCR of genes. Methanotrophic activity and populations in the lake water were highest during fall turnover and remained high through the winter ice-covered period into spring turnover. They declined during summer stratification, especially in the epilimnion. Three methanotroph genera (, , and ) cycled seasonally, based on both relative and absolute abundance measurements. and populations peaked in winter/spring, when methane oxidation activity was psychrophilic. populations increased in the water column through summer and fall, when methane oxidation was mesophilic, and also predominated in the underlying tailings sediment. Other, less abundant genera grew primarily during summer, possibly due to distinct CH/O microniches created during thermal stratification. These data are consistent with temporal and spatial niche differentiation based on temperature, CH and O. This pit lake displays methane cycling and methanotroph population dynamics similar to natural boreal lakes. The study examined methanotrophic bacteria in an industrial end pit lake, combining molecular DNA methods (both quantitative and descriptive) with biogeochemical measurements. The lake was sampled over 5 years, in all four seasons, as often as weekly, and included sub-ice samples. The resulting multiseason and multiyear data set is unique in its size and intensity, and allowed us to document clear and consistent seasonal patterns of growth and decline of three methanotroph genera (, , and ). Laboratory experiments suggested that one major control of this succession was niche partitioning based on temperature. The study helps to understand microbial dynamics in engineered end pit lakes, but we propose that the dynamics are typical of boreal stratified lakes and widely applicable in microbial ecology and limnology. Methane-oxidizing bacteria are important model organisms in microbial ecology and have implications for global climate change.

摘要

贝塞矿湖(BML)是加拿大第一个油砂矿业全规模示范坑内湖泊。我们在这个二型湖的五年中,对所有季节的好氧甲烷氧化菌进行了研究。16S rRNA 基因扩增子测序分析中,甲烷氧化菌占所有细菌读数的高达 58%(中位数为 2.8%),根据基因的 qPCR,水中的甲烷氧化菌数量高达 2.7×10 个细胞 mL(中位数为 0.5×10)。在秋季翻转期间,湖泊水中的甲烷氧化活性和种群数量最高,并在冬季冰覆盖期和春季翻转期间保持高位。在夏季分层期间,特别是在真光层中,它们下降了。基于相对和绝对丰度测量,三种甲烷氧化菌属(,和)季节性循环。和属的种群在冬季/春季达到高峰,此时甲烷氧化是嗜冷的。属的种群在夏季和秋季通过水柱增加,此时甲烷氧化是中温的,并且在下面的尾矿沉积物中也占优势。其他,较少的属主要在夏季生长,可能是由于热分层期间形成了独特的 CH/O 小生境。这些数据与基于温度、CH 和 O 的时间和空间生态位分化一致。这个坑内湖显示出与天然北方湖泊相似的甲烷循环和甲烷氧化菌种群动态。该研究结合分子 DNA 方法(定量和描述性)和生物地球化学测量,在工业坑内湖中检查了甲烷氧化菌。该湖泊在 5 年内、所有四个季节、每周最多采样一次,包括冰下样品。由此产生的多年多季节数据集在规模和强度上都是独一无二的,使我们能够记录三个甲烷氧化菌属(,和)的清晰和一致的季节性生长和衰退模式。实验室实验表明,这种演替的一个主要控制因素是基于温度的小生境划分。该研究有助于了解工程坑内湖中的微生物动态,但我们提出,这些动态是北方分层湖泊的典型特征,在微生物生态学和湖沼学中具有广泛的应用。甲烷氧化菌是微生物生态学中的重要模式生物,对全球气候变化具有重要意义。