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洋中脊侧翼地壳流体中的微生物生命。

Microbial life in ridge flank crustal fluids.

作者信息

Huber Julie A, Johnson H Paul, Butterfield David A, Baross John A

机构信息

University of Washington, School of Oceanography, Center for Astrobiology and Early Evolution, Box 357940 Seattle, 98195, USA.

出版信息

Environ Microbiol. 2006 Jan;8(1):88-99. doi: 10.1111/j.1462-2920.2005.00872.x.

Abstract

To determine the microbial community diversity within old oceanic crust, a novel sampling strategy was used to collect crustal fluids at Baby Bare Seamount, a 3.5 Ma old outcrop located in the north-east Pacific Ocean on the eastern flank of the Juan de Fuca Ridge. Stainless steel probes were driven directly into the igneous ocean crust to obtain samples of ridge flank crustal fluids. Genetic signatures and enrichment cultures of microorganisms demonstrate that these crustal fluids host a microbial community composed of species indigenous to the subseafloor, including anaerobic thermophiles, and species from other deep-sea habitats, such as seawater and sediments. Evidence using molecular techniques indicates the presence of a relatively small but active microbial population, dominated by bacteria. The microbial community diversity found in the crustal fluids may indicate habitat variability in old oceanic crust, with inputs of nutrients from seawater, sediment pore-water fluids and possibly hydrothermal sources. This report further supports the presence of an indigenous microbial community in ridge flank crustal fluids and advances our understanding of the potential physiological and phylogenetic diversity of this community.

摘要

为了确定古老大洋地壳内的微生物群落多样性,采用了一种新颖的采样策略,在位于东北太平洋胡安德富卡海岭东翼的350万年历史的露头——小贝雷海山采集地壳流体样本。将不锈钢探针直接打入火成岩大洋地壳,以获取海岭侧翼地壳流体样本。微生物的基因特征和富集培养表明,这些地壳流体中存在一个微生物群落,该群落由海底原生物种(包括厌氧嗜热菌)以及来自其他深海栖息地(如海水和沉积物)的物种组成。使用分子技术的证据表明存在一个相对较小但活跃的微生物种群,以细菌为主导。在地壳流体中发现的微生物群落多样性可能表明古老大洋地壳中的栖息地存在变异性,有来自海水、沉积物孔隙水流体以及可能的热液源的营养物质输入。本报告进一步支持了海岭侧翼地壳流体中存在原生微生物群落,并增进了我们对该群落潜在生理和系统发育多样性的理解。

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