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The Deep Subsurface Biosphere in Igneous Ocean Crust: Frontier Habitats for Microbiological Exploration

机译:火成硬壳中的深层地下生物圈:微生物探索的前沿栖息地

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摘要

We discuss ridge flank environments in the ocean crust as habitats for subseafloor microbial life. Oceanic ridge flanks, areas far from the magmatic and tectonic influence of seafloor spreading, comprise one of the largest and least explored microbial habitats on the planet. We describe the nature of selected ridge flank crustal environments, and present a framework for delineating a continuum of conditions and processes that are likely to be important for defining subseafloor microbial "provinces." The basis for this framework is three governing conditions that help to determine the nature of subseafloor biomes: crustal age, extent of fluid flow, and thermal state. We present a brief overview of subseafloor conditions, within the context of these three characteristics, for five field sites where microbial studies have been done, are underway, or have been proposed. Technical challenges remain and likely will limit progress in studies of microbial ridge flank ecosystems, which is why it is vital to select and design future studies so as to leverage as much general understanding as possible from work focused at a small number of sites. A characterization framework such that as presented in this paper, perhaps including alternative or additional physical or chemical characteristics, is essential for achieving the greatest benefit from multidisciplinary microbial investigations of oceanic ridge flanks.
机译:我们讨论洋壳中的脊腹环境作为海底微生物生活的栖息地。海洋脊侧面,远离海床扩展的岩浆和构造影响,是地球上最大,勘探最少的微生物栖息地之一。我们描述了选定的脊胁腹地壳环境的性质,并提出了一个框架,用于描述可能对定义海底微生物“省”很重要的条件和过程的连续性。该框架的基础是三个控制条件,可帮助确定海底生物群落的性质:地壳年龄,流体流动程度和热状态。在这三个特征的背景下,我们对已经进行,正在进行或已提出微生物研究的五个现场进行了简要的海底条件概述。技术挑战仍然存在,并且很可能会限制微生物侧面生态系统研究的进展,这就是为什么选择和设计未来研究以充分利用针对少数地点的工作中尽可能多的一般理解至关重要。如本白皮书中所述,可能包括替代性或附加的物理或化学特性的表征框架,对于从多学科微生物对洋侧面的微生物研究中获得最大收益至关重要。

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