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弧后盆地热液喷口沉积物中微生物群落的场间变异性。

Inter-field variability in the microbial communities of hydrothermal vent deposits from a back-arc basin.

机构信息

Department of Biology, Portland State University, Portland, OR, USA.

出版信息

Geobiology. 2012 Jul;10(4):333-46. doi: 10.1111/j.1472-4669.2012.00325.x. Epub 2012 Mar 23.

Abstract

Diverse microbial communities thrive on and in deep-sea hydrothermal vent mineral deposits. However, our understanding of the inter-field variability in these communities is poor, as limited sampling and sequencing efforts have hampered most previous studies. To explore the inter-field variability in these communities, we used barcoded pyrosequencing of the variable region 4 (V4) of the 16S rRNA gene to characterize the archaeal and bacterial communities of over 30 hydrothermal deposit samples from six vent fields located along the Eastern Lau Spreading Center. Overall, the bacterial and archaeal communities of the Eastern Lau Spreading Center are similar to other active vent deposits, with a high diversity of Epsilonproteobacteria and thermophilic Archaea. However, the archaeal and bacterial communities from the southernmost vent field, Mariner, were significantly different from the other vent fields. At Mariner, the epsilonproteobacterial genus Nautilia and the archaeal family Thermococcaceae were prevalent in most samples, while Lebetimonas and Thermofilaceae were more abundant at the other vent fields. These differences appear to be influenced in part by the unique geochemistry of the Mariner fluids resulting from active degassing of a subsurface magma chamber. These results show that microbial communities associated with hydrothermal vent deposits in back-arc basins are taxonomically similar to those from mid-ocean ridge systems, but differences in geologic processes between vent fields in a back-arc basin can influence microbial community structure.

摘要

深海热液喷口矿床上和内部栖息着多样的微生物群落。然而,由于之前的研究大多受到采样和测序工作的限制,我们对这些群落的场间变异性的了解甚少。为了探究这些群落的场间变异性,我们利用 16S rRNA 基因 V4 区的条码焦磷酸测序技术,对来自东劳厄斯扩张中心 6 个热液喷口场的 30 多个热液矿床样本的古菌和细菌群落进行了分析。总体而言,东劳厄斯扩张中心的细菌和古菌群落与其他活跃的热液喷口沉积物相似,具有高度多样性的 ε 变形菌和嗜热古菌。然而,最南端的马里纳喷口场的古菌和细菌群落与其他喷口场有显著差异。在马里纳, ε 变形菌属 Nautilia 和古菌科 Thermococcaceae 在大多数样本中普遍存在,而 Lebetimonas 和 Thermofilaceae 在其他喷口场更为丰富。这些差异似乎部分受到马里纳流体独特地球化学的影响,这是由于地下岩浆房的活跃脱气作用所致。这些结果表明,与弧后盆地热液喷口沉积物相关的微生物群落在分类上与中洋脊系统的微生物群落相似,但弧后盆地喷口场之间的地质过程差异会影响微生物群落结构。

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