Serpentinization processes in the subsurface of a seafloor ultramafic-hosted hydrothermal system

海底超镁铁质热液系统地下的蛇纹石化过程

• 批准号: 1536242
• 负责人: Jeffrey Alt
• 金额: $ 25.99万
• 依托单位: Regents of the University of Michigan - Ann Arbor
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2015
• 资助国家: 美国
• 起止时间: 2015-08-15 至 2020-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1536242&HistoricalAwards=false
• 关键词: Serpentinization; processes; subsurface; seafloor; ultramafic

Beneath Earth's crust lies the mantle, composed of an ultramafic rock called peridotite. Peridotites are exposed on the seafloor by faulting at mid-ocean ridges where they react with fluids to form serpentinites. The reacting fluids can be cold seawater or hot (350 degrees Celsius) hydrothermal fluids derived from seawater and driven by heat generated by intrusions of basaltic magma at depth. The hydration of peridotite to form serpentinite generates hydrogen, which supports microbial communities around hydrothermal vents at the seafloor. These seafloor hydrothermal environments are likely sites for the origin of life on Earth and the microbial communities found there are analogues for life on other planets. Major questions remain, however, about the extent of this subsurface biosphere, such as how far away from seafloor vents this biosphere extends and how far microbes live below the seafloor. In addition to life, metal deposits form where hot hydrothermal fluids vent into the ocean from peridotite on the seafloor. Although these deposits and their associated fluids are well studied, our understanding of the fluid flow pathways in underlying basement and the controls on fluid penetration and serpentinization of the host peridotite and their relationship to microbial activity in the subsurface is not. This research examines the geochemistry of fluid penetration and reaction with peridotite to form serpentinite and the impact of the resulting water-rock interactions on the deep biosphere. Two major goals of the project are: (1) understanding the relative roles of cold seawater versus hot hydrothermal fluids that circulate through the seafloor and (2) determining the controls on the subsurface biosphere and its lateral and depth extent in seafloor peridotites. Broader impacts of the work include improving understanding of the generation of marine massive sulfide ore deposits and processes of interest to the geothermal energy industry. The work also includes integration of research and education by training a student who is interested in a career in the mining industry. This research involves understanding fluid pathways, serpentinization, and the distribution and extent of microbial sulfate reduction in the subsurface of seafloor ultramafic-hosted hydrothermal systems. Work involves an intensive field and laboratory study of an analog of these seafloor systems that is exposed in an ophiolite in the northern Apennines (Italy). The effects of hydrothermal fluids in the rocks will be distinguished from those of seawater through analyses of major and trace elements and sulfur isotopes. Combined with petrography, micro-scale spot analyses by laser inductively coupled mass spectrometry of trace elements in serpentine, and the sulfur isotope compositions of individual sulfide grains, it will be possible to map the fluid flow pathways; determine how they developed; and understand how microbial processes affect and/or catalyze reactions in high-temperature ultramafic-hosted seafloor hydrothermal systems. Bulk rock analyses will enable evaluation of the overall effects of hydrothermal fluids and seawater and of microbial sulfate reduction in the basement.

地壳之下是地幔，由一种叫做橄榄岩的超镁铁质岩石组成。橄榄岩在洋中脊的断层作用下暴露在海底，与流体反应形成蛇纹岩。反应流体可以是冷的海水或热的（350摄氏度）来自海水的热液流体，并由玄武岩岩浆侵入体在深处产生的热量驱动。橄榄岩水合形成蛇纹岩产生氢，支持海底热液喷口周围的微生物群落。这些海底热液环境可能是地球上生命起源的场所，在那里发现的微生物群落与其他行星上的生命类似。然而，关于地下生物圈的范围仍然存在主要问题，例如该生物圈延伸到距离海底喷口多远的地方以及微生物生活在海底以下的多远。除了生命之外，金属矿床也是在热液流体从海底的橄榄岩排入海洋的地方形成的。尽管这些矿床及其伴生流体已得到很好的研究，但我们对下伏基底中的流体流动路径以及对流体渗透和寄主橄榄岩的蛇纹化的控制及其与地下微生物活动的关系的了解还不够。本研究探讨了流体渗透和橄榄岩反应形成蛇纹岩的地球化学，以及由此产生的水-岩相互作用对深层生物圈的影响。该项目的两个主要目标是：（1）了解冷海水与在海底循环的热液流体的相对作用;（2）确定对地下生物圈及其在海底橄榄岩中的横向和深度范围的控制。这项工作的更广泛影响包括增进对海洋块状硫化物矿床的生成和地热能工业感兴趣的过程的了解。 这项工作还包括通过培训对采矿业职业感兴趣的学生来整合研究和教育。这项研究涉及了解海底超镁铁质热液系统地下的流体通道、蛇纹石化作用以及微生物硫酸盐还原的分布和程度。 工作包括对这些海底系统的类似物进行密集的实地和实验室研究，这些海底系统暴露在亚平宁山脉（意大利）北方的蛇绿岩中。 通过对岩石中常量元素、微量元素和硫同位素的分析，将热液流体的作用与海水的作用区分开来。结合岩相学、用激光感应耦合质谱法对蛇纹石中的微量元素进行的微尺度点分析以及单个硫化物颗粒的硫同位素组成，将有可能绘制流体流动路径图;确定它们是如何形成的;并了解微生物过程如何影响和/或催化高温超镁铁质海底热液系统中的反应。 大量岩石分析将有助于评价热液流体和海水以及微生物在基底中硫酸盐还原的总体影响。