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There is now a CONTENT FREEZE for Mercury while we switch to a new platform. It began on Friday, March 10 at 6pm and will end on Wednesday, March 15 at noon. No new content can be created during this time, but all material in the system as of the beginning of the freeze will be migrated to the new platform, including users and groups. Functionally the new site is identical to the old one. webteam@gatech.edu
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This talk will focus on how a series of continuously evolving science questions, spanning from geophysics to biogeography to astrobiology, have motivated a sustained body of work to explore the ocean floor for submarine venting.
Seafloor hydrothermal activity is now known to occur in all ocean basins and at all spreading rates. While early work suggested that most venting should coincide with where the most magmatic activity occurs, along Earth’s fastest spreading sections of Mid-Ocean Ridge, I will show how continuing robotics-based exploration of Earth’s slower spreading ridges have revealed a greater geologic diversity of conditions for seafloor fluid flow than previously anticipated, with societal relevance ranging from the future of seafloor mining to the prospects for habitability of other Ocean Worlds.
I will close with a discussion of future directions – both scientific (where else might life-sustaining seafloor fluid flow arise?) and technologic (what new methodologies might one might employ, blending autonomy with humans-in-the-loop, via telepresence?).