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通过大规模平行测序揭示北大西洋细菌群落的水体特异性。

Water mass-specificity of bacterial communities in the North Atlantic revealed by massively parallel sequencing.

机构信息

Department of Biological Oceanography, Royal Netherlands Institute for Sea Research (NIOZ), Den Burg, The Netherlands.

出版信息

Mol Ecol. 2011 Jan;20(2):258-74. doi: 10.1111/j.1365-294X.2010.04932.x. Epub 2010 Dec 9.

DOI:10.1111/j.1365-294X.2010.04932.x
PMID:21143328
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3057482/
Abstract

Bacterial assemblages from subsurface (100 m depth), meso- (200-1000 m depth) and bathy-pelagic (below 1000 m depth) zones at 10 stations along a North Atlantic Ocean transect from 60°N to 5°S were characterized using massively parallel pyrotag sequencing of the V6 region of the 16S rRNA gene (V6 pyrotags). In a dataset of more than 830,000 pyrotags, we identified 10,780 OTUs of which 52% were singletons. The singletons accounted for less than 2% of the OTU abundance, whereas the 100 and 1000 most abundant OTUs represented 80% and 96% respectively of all recovered OTUs. Non-metric Multi-Dimensional Scaling and Canonical Correspondence Analysis of all the OTUs excluding the singletons revealed a clear clustering of the bacterial communities according to the water masses. More than 80% of the 1000 most abundant OTUs corresponded to Proteobacteria of which 55% were Alphaproteobacteria, mostly composed of the SAR11 cluster. Gammaproteobacteria increased with depth and included a relatively large number of OTUs belonging to Alteromonadales and Oceanospirillales. The bathypelagic zone showed higher taxonomic evenness than the overlying waters, albeit bacterial diversity was remarkably variable. Both abundant and low-abundance OTUs were responsible for the distinct bacterial communities characterizing the major deep-water masses. Taken together, our results reveal that deep-water masses act as bio-oceanographic islands for bacterioplankton leading to water mass-specific bacterial communities in the deep waters of the Atlantic.

摘要

采用 V6 区 16S rRNA 基因(V6 焦磷酸测序)对大西洋北部分布从北纬 60°到南纬 5°的 10 个站位的近表层(100 m 水深)、中层(200-1000 m 水深)和深海-远洋(1000 m 水深以下)区的细菌进行了分析。在超过 830,000 个焦磷酸标签的数据集里,我们共鉴定出 10,780 个 OTUs,其中 52%为单峰。单峰在 OTU 丰度中占比小于 2%,而 100 和 1000 个最丰富的 OTUs 分别代表所有回收 OTUs 的 80%和 96%。排除单峰后对所有 OTUs 进行非度量多维标度分析和典范对应分析,发现根据水团细菌群落明显聚类。在 1000 个最丰富的 OTUs 中,超过 80%是变形菌,其中 55%是α变形菌,主要由 SAR11 群组成。γ变形菌随着深度的增加而增加,其中包括相对数量较多的属于交替单胞菌目和海洋螺旋菌目的 OTUs。深海区的分类均匀度高于上覆水,但细菌多样性变化显著。丰富和低丰度的 OTUs 均有助于形成独特的细菌群落,从而对大西洋深海的主要深水团进行了特征描述。总之,我们的研究结果表明,深水团充当了浮游细菌的生物海洋岛屿,导致了大西洋深海特定水团的特有细菌群落。

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