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For more information about Dr. Barge, please visit her website
Prebiotic Chemistry in Hydrothermal Systems on Early Earth and Ocean Worlds
It is theorized that life on Earth could have begun at seafloor hydrothermal vents – if so, this also provides a possible way for life to emerge on ocean worlds such as Saturn’s moon Enceladus which may host hydrothermal systems. However, hydrothermal vents on Earth host a variety of chemical conditions, which can result in different outcomes of prebiotic organic reactions. In this talk I will discuss our group’s work on simulating prebiotic hydrothermal chimneys and sediments, and the organic chemistry that can occur within. Particularly I will present results from our recent studies investigating how changing geochemical conditions can lead to different prebiotic reactions, and discuss different types of vents in which these conditions may be found. Our origin of life investigations aim to bridge the gap between geochemistry and biochemistry in an early Earth context, as well as to inform the search for life and its origin on other planets.
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