
My contributions to Astrobiology research at UW have primarily been directed at exploring the ability of abiotic geochemical processes to support microbial life. I have done much of this research at deep-sea hydrothermal vents, some of the most primordial environments existing on present-day Earth. I study ridge-axis hydrothermal systems such as the Juan de Fuca Ridge about 300 miles off the coast of Washington State and the Lost City Hydrothermal Field near the Mid Atlantic Ridge.
Some of the exciting projects I have been able to participate in since arriving at UW include 1) Recovery of large pieces of hydrothermal vent chimneys (the largest such structures ever recovered from the seafloor); 2) Development of a high-pressure, high-temperature facility for incubating organisms under deep-sea conditions; and 3) Instrumenting black smoker chimneys for in situ thermal, chemical, and microbiological measurements. This research has allowed us to test criteria for life-detection, explore the upper temperature limits for life, and determine reliable biosignatures, all of which may be relevant to the search for extraterrestrial life.
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