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The concentration of silica is very high at the centerlines of these halos,” said Jens Frydenvang, a scientist at Los Alamos National Laboratory and the University of Copenhagen and lead author of the new study. “What we’re seeing is that silica appears to have migrated between very old sedimentary bedrock and into younger overlying rocks. The goal of NASA’s Curiosity rover mission has been to find out if Mars was ever habitable, and it has been very successful in showing that Gale crater once held a lake with water that we would even have been able to drink, ... -thus further expanding the window for when life might have existed on Mars.”
originally posted by: Box of Rain
a reply to: Christosterone
How much wider is that time frame? I could not find a number that quantified how long the time of habitability should be lengthened.
I even skimmed through the actual scientific paper that this article references, and the best they say is:
"Consequently, the timescale for potential habitability, at least in the subsurface of Gale, must be substantially extended."
Extended by how much?
Granted, the paper also states that "Hence, this sequence of events implies that considerable amounts of neutral to alkaline groundwater were active in Gale crater well after Mount Sharp group lacustrine activity ceased", but I have no idea what "well after Mount Sharp group lacustrine activity ceased" means in terms of timescale.
originally posted by: stormcell
Probably life is still there, but moved underground. We've found life on Earth at the deepest ocean trenches, in isolated sealed off underground lakes and caves, so why not Mars?
originally posted by: stormcell
Probably life is still there, but moved underground. We've found life on Earth at the deepest ocean trenches, in isolated sealed off underground lakes and caves, so why not Mars?
originally posted by: MichiganSwampBuck
Come on now! We know there is life on Mars because Bugs Bunny and Daffy Duck have been there and met them.
I like Daffy and Bugs, but I don't like the Roadrunner.