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沿海加利福尼亚深叶绿素最大值中丰富的海洋古菌和细菌谱系的共现模式。

Co-occurrence patterns for abundant marine archaeal and bacterial lineages in the deep chlorophyll maximum of coastal California.

机构信息

Department of Biological Sciences and Wrigley Institute for Environmental Studies, University of Southern California, Los Angeles, CA, USA.

出版信息

ISME J. 2011 Jul;5(7):1077-85. doi: 10.1038/ismej.2010.204. Epub 2011 Jan 13.

Abstract

Microorganisms remineralize and respire half of marine primary production, yet the niches occupied by specific microbial groups, and how these different groups may interact, are poorly understood. In this study, we identify co-occurrence patterns for marine Archaea and specific bacterial groups in the chlorophyll maximum of the Southern California Bight. Quantitative PCR time series of marine group 1 (MG1) Crenarchaeota 16S rRNA genes varied substantially over time but were well-correlated (r(2)=0.94, P<0.001) with ammonia monooxygenase subunit A (amoA) genes, and were more weakly related to 16S rRNA genes for all Archaea (r(2)=0.39), indicating that other archaeal groups (for example, Euryarchaeota) were numerically important. These data sets were compared with variability in bacterial community composition based on automated ribosomal intergenic spacer analysis (ARISA). We found that archaeal amoA gene copies and a SAR11 (or Pelagibacter) group Ib operational taxonomic unit (OTU) displayed strong co-variation through time (r(2)=0.55, P<0.05), and archaeal amoA and MG1 16S rRNA genes also co-occurred with two SAR86 and two Bacteroidetes OTUs. The relative abundance of these groups increased and decreased in synchrony over the course of the time series, and peaked during periods of seasonal transition. By using a combination of quantitative and relative abundance estimates, our findings show that abundant microbial OTUs-including the marine Crenarchaeota, SAR11, SAR86 and the Bacteroidetes-co-occur non-randomly; they consequently have important implications for our understanding of microbial community ecology in the sea.

摘要

微生物使海洋初级生产力的一半再矿化和呼吸,但特定微生物群体占据的生态位,以及这些不同群体如何相互作用,还知之甚少。在这项研究中,我们确定了南加州湾叶绿素最大值中海洋古菌和特定细菌群体的共现模式。海洋组 1(MG1)古菌 16S rRNA 基因的定量 PCR 时间序列随时间变化很大,但与氨单加氧酶亚基 A(amoA)基因呈高度相关(r²=0.94,P<0.001),与所有古菌的 16S rRNA 基因相关性较弱(r²=0.39),表明其他古菌群体(例如,广古菌)在数量上很重要。这些数据集与基于自动核糖体基因间 spacer 分析(ARISA)的细菌群落组成的可变性进行了比较。我们发现,古菌 amoA 基因拷贝数和 SAR11(或 Pelagibacter)组 Ib 操作分类单元(OTU)随着时间的推移表现出强烈的共变(r²=0.55,P<0.05),古菌 amoA 和 MG1 16S rRNA 基因也与两个 SAR86 和两个拟杆菌门 OTU 共现。这些群体的相对丰度在时间序列的过程中同步增加和减少,并在季节性过渡期间达到峰值。通过使用定量和相对丰度估计的组合,我们的研究结果表明,丰富的微生物 OTU,包括海洋古菌、SAR11、SAR86 和拟杆菌门,非随机共现;因此,它们对我们理解海洋微生物群落生态具有重要意义。

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