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Extreme Life and Environments
hydrothermaldeepsea
09/01/09

 

The new hypothesis suggests that life on Earth originated at photosynthetically-active porous structures made of zinc sulfide similar to deep-sea hydrothermal vents.
Image credit: The Institute for Exploration, the University of Rhode Island (URI) Graduate School of Oceanography (GSO), and the URI Institute for Archaeological Oceanography



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