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To test the hypothesis that fatty acids were formed in hydrothermal vents, the scientists reproduced in the laboratory the conditions that existed in the ancient oceans of the Earth, characterised by a high content of carbon dioxide. They also simulated mixing seawater with hot alkaline water from certain types of hydrothermal vents.
It turned out that when hot hydrogen-rich liquids were mixed with carbon dioxide-rich water in the presence of iron-based minerals, the types of molecules needed to form the membranes of primitive cells emerged. The authors suggest that a similar process may occur in the oceans beneath the surface of icy moons in the solar system, such as Europa, Ganymede or Callisto.