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

地壳下方是地幔，由一种称为橄榄岩的超镁铁质岩石组成。橄榄岩通过大洋中脊的断层暴露在海底，在那里它们与流体反应形成蛇纹岩。反应流体可以是冷海水，也可以是源自海水的热液（350 摄氏度），并由深部玄武岩浆侵入产生的热量驱动。橄榄岩水合形成蛇纹石会产生氢气，为海底热液喷口周围的微生物群落提供支持。这些海底热液环境可能是地球生命起源的场所，并且微生物群落也发现了其他行星上生命的类似物。然而，关于这个地下生物圈的范围仍然存在主要问题，例如这个生物圈距离海底喷口有多远以及微生物生活在海底以下多远。除了生命之外，热液从海底橄榄岩排入海洋的地方也会形成金属沉积物。尽管这些沉积物及其相关流体已得到充分研究，但我们对地下基底的流体流动路径、对流体渗透和寄主橄榄岩蛇纹石化的控制及其与地下微生物活动的关系的了解还不够。这项研究研究了流体渗透和与橄榄岩反应形成蛇纹岩的地球化学，以及由此产生的水-岩石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）了解冷海水与海底循环的热热液的相对作用；（2）确定对海底橄榄岩中地下生物圈及其横向和深度范围的控制。这项工作的更广泛影响包括提高对海洋块状硫化物矿床的生成以及地热能行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路径、蛇纹石化以及微生物硫酸盐还原的分布和程度。 工作涉及对暴露在亚平宁山脉北部（意大利）蛇绿岩中的这些海底系统的模拟进行深入的现场和实验室研究。 通过对主量元素、微量元素以及硫同位素的分析，将区分岩石中热液的影响与海水的影响。结合岩相学、蛇纹石中微量元素的激光感应耦合质谱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；确定它们如何发展；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。 大块岩石分析将能够评估热液和海水以及微生物硫酸盐还原在基底中的总体影响。

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.