
The data suggest yet another reason to think that Mars might once have sustained life.

Former Carnegie postdoctoral scientist Francis McCubbin, now at the University of New Mexico, led this research. The analysis was performed by Carnegie Institution investigator Erik Hauri and team.
Researchers analyzed what are called shergottite meteorites, thought to have been ejected from Mars approximately 2.5 million years ago. Erik explained why the researchers concluded that Mars’ interior has plentiful water:
"We analyzed two meteorites that had very different processing histories. One had undergone considerable mixing with other elements during its formation, while the other had not. We analyzed the water content of the mineral apatite and found there was little difference between the two even though the chemistry of trace elements was markedly different. The results suggest that water was incorporated during the formation of Mars and that the planet was able to store water in its interior during the planet’s differentiation."

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Interesting.
ReplyDeletethanks Raj :)
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