Serpentinization is the hydrothermal alteration of ultramafic rock, which results in high pH, reducing fluids that are low in dissolved inorganic carbon, and have high levels of methane and hydrogen. While endemic microbial communities have been well-characterized from a variety of marine and terrestrial serpentinizing ecosystems, to date the ecological processes that contribute to microbial community assembly, community dynamics, and the impact of disturbances in serpentinizing environments have not yet been assessed. The work in this dissertation was performed at the Coast Range Ophiolite Microbial Observatory, CA, USA, where a series of wells were drilled in 2011 to access serpentinization-influenced fluids directly from the subsurface. Geochemical and 16S rRNA gene amplicon datasets were collected directly from these wells and a series of microcosm experiments were performed on fluids from the site. Samples collected over the course of six years were used to assess community assembly processes and the biogeochemical impacts of drilling fluid injection into the subsurface. A series of microcosm experiments were also performed to better understand the response of microbial populations to geochemical changes observed in situ following drilling. Results from this work will inform studies of biogeochemical dynamics relevant to modern and ancient Earth and extraterrestrial sites such as Mars. These data further our understanding of microbial community responses to environmental perturbations and provide information that will aid in the development of future drilling and monitoring projects focused on learning about life in the deep subsurface.
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