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沿碱性、高盐湖泊氧化还原梯度的微生物群落组成与活性

Composition and Activity of Microbial Communities along the Redox Gradient of an Alkaline, Hypersaline, Lake.

作者信息

Edwardson Christian F, Hollibaugh James T

机构信息

Department of Marine Sciences, University of Georgia, Athens, GA, United States.

Department of Microbiology, University of Georgia, Athens, GA, United States.

出版信息

Front Microbiol. 2018 Jan 31;9:14. doi: 10.3389/fmicb.2018.00014. eCollection 2018.

DOI:10.3389/fmicb.2018.00014
PMID:29445359
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5797777/
Abstract

We compared the composition of microbial communities obtained by sequencing 16S rRNA gene amplicons with taxonomy derived from metatranscriptomes from the same samples. Samples were collected from alkaline, hypersaline Mono Lake, California, USA at five depths that captured the major redox zones of the lake during the onset of meromixis. The prokaryotic community was dominated by bacteria from the phyla Proteobacteria, Firmicutes, and Bacteroidetes, while the picoeukaryotic chlorophyte dominated the eukaryotes. Most (80%) of the abundant (>1% relative abundance) OTUs recovered as amplicons of 16S rRNA genes have been reported in previous surveys, indicating that Mono Lake's microbial community has remained stable over 12 years that have included periods of regular, annual overturn interspersed by episodes of prolonged meromixis that result in extremely reducing conditions in bottom water. Metatranscriptomic sequences binned predominately to the Gammaproteobacteria genera (4-13%) and (0-14%); and to the Firmicutes genera (0-5%) and (1-4%), which were also abundant in the 16S rRNA gene amplicon libraries. This study provides insight into the taxonomic affiliations of transcriptionally active communities of the lake's water column under different redox conditions.

摘要

我们将通过对16S rRNA基因扩增子进行测序获得的微生物群落组成,与来自相同样本宏转录组的分类法进行了比较。样本采集于美国加利福尼亚州碱性、高盐度的莫诺湖,采集深度为五个,涵盖了混合湖形成初期湖泊的主要氧化还原带。原核生物群落主要由变形菌门、厚壁菌门和拟杆菌门的细菌组成,而微微型真核绿藻则在真核生物中占主导地位。作为16S rRNA基因扩增子回收的大多数(80%)丰富OTU(相对丰度>1%)在先前的调查中已有报道,这表明莫诺湖的微生物群落在12年中一直保持稳定,其中包括定期的年度水体翻转期,期间穿插着长时间的混合湖形成期,这导致底部水体处于极端还原条件。宏转录组序列主要归类于γ-变形菌属(4-13%)和 (0-14%);以及厚壁菌属(0-5%)和 (1-4%),这些在16S rRNA基因扩增子文库中也很丰富。这项研究为不同氧化还原条件下湖泊水柱转录活性群落的分类归属提供了见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/54dc617c9e6e/fmicb-09-00014-g0006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/39b057a5f869/fmicb-09-00014-g0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/044a88950943/fmicb-09-00014-g0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/4d041053d4f8/fmicb-09-00014-g0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/fef46795d8d7/fmicb-09-00014-g0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/40e065d664fd/fmicb-09-00014-g0005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/54dc617c9e6e/fmicb-09-00014-g0006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/39b057a5f869/fmicb-09-00014-g0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/044a88950943/fmicb-09-00014-g0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/4d041053d4f8/fmicb-09-00014-g0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/fef46795d8d7/fmicb-09-00014-g0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/40e065d664fd/fmicb-09-00014-g0005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6183/5797777/54dc617c9e6e/fmicb-09-00014-g0006.jpg

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