Despite the team's success in dating the water-rock interaction, the researchers don't think Mars was teeming with water at that time in history. Rather, they suspect the water came from permafrost melt, perhaps caused by molten rock moving through the planet's crust. The study appears in the Geochemical Perspectives Letters.

A sliver of Martian rock that once lay hidden in a university drawer has helped researchers better understand the Red Planet’s geological history. Using isotopic dating, a team at Purdue University has determined that the “Lafayette Meteorite” likely interacted with liquid water approximately 742 million years ago.

The unlikely journey that brought the Lafayette Meteorite to Purdue University’s Department of Earth, Atmospheric, and Planetary Sciences began 11 million years ago. An unknown object struck Mars with enough force to launch fragments of the planet into space.

The study identified when water interacted with the meteorite and established that the dating was unaffected by events after it left Mars.