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Therefore, the results of the new study support the idea that primitive life could potentially have evolved on Ganymede. This is because places where water and rock interact are important for the development of life. For example, some theories suggest that life arose on our planet within hot, bubbling seafloor vents. Before the new study, Ganymede's rocky seafloor was believed to be coated with ice--not liquid. This would have presented a problem for the evolution of living tidbits. The "Dagwood sandwich" findings, however, indicate something else entirely--the first layer on top of Ganymede's rocky core might be made up of precious, life-sustaining salty water.



The Cassini-Huygens mission is a cooperative endeavor by NASA, the European Space Agency (ESA), and the Italian Space Agency. The Jet Propulsion Laboratory (JPL), a division of the California Institute of Technology in Pasadena, California, manages the mission for NASA.



Like our own Earth, Titan's atmosphere is mainly made up of nitrogen--but with the added ingredient of a small amount of methane. It is the only other world in our Solar System that is actually known to have a cycle of liquids that shower back down to the surface again, in Titan's case as large, lazy drops of hydrocarbon rain. The clouds of Titan pour torrential rains of gasoline down to the surface of this tormented moon. Even though the ingredients are different, this cycle is similar to our own planet's water cycle. Many planetary scientists propose that Titan contains a subsurface ocean of sloshing liquid water.