Young Mars Most Likely To Support Life, New Mineral History Shows
Mars started out relatively wet and temperate, underwent a major climate shift, and evolved into a cold, dry place strewn with acidic rock – less than ideal conditions for supporting life.
This is the finding of an international team of scientists who have created the most comprehensive mineral history of Mars, a history closely linked to the presence of liquid water on the planet. According to the mineral record, created with Mars Express mission data and detailed in Science, Mars would only have been hospitable to life in its infancy.
Starting about 3.5 billion years ago, conditions on Mars became increasingly dry and acidic – not a pleasant place for any form of life, even a microbe,” said John Mustard, a Brown University geologist and a primary author of the Science paper.
If any living organisms had formed on Mars, that evidence would likely be found in clay-rich rocks and soil north of the Syrtis Major volcanic plateau, in Nili Fossae and in the Marwth Vallis Regions, the team reports.
These areas make compelling targets for future lander missions, according to Mustard, a co-investigator on the Mars Express and Mars Reconnaissance Orbiter missions. In the meantime, the Compact Reconnaissance Imaging Spectrometer for Mars, or CRISM, aboard the Mars Reconnaissance Orbiter, will in September begin beaming mineralogical data on these clay-rich regions. The images will be 20 times more precise compared with those captured by Mars Express.
“I’m eager to get the CRISM data and explore the deposits found by OMEGA, as well as discover new sites and minerals,” Mustard said. “OMEGA shows that some of the most interesting sites are small – and CRISM is designed to find and characterize small deposits.”
Jean-Pierre Bibring, an astrophysicist from the University of Paris, led the team of scientists from France, Italy, Russia, Germany and the United States. The investigators pieced together the mineral history using data from Mars Express, a mission launched by the European Space Agency. An instrument aboard the spacecraft dubbed OMEGA – short for Observatoire pour la Minéralogie, l'Eau, les Glaces et l'Activité – determines mineral composition from visible and infrared light reflected from the Red Planet’s surface. The team used two years worth of data from OMEGA, which has mapped more than 90 percent of the planet’s surface.
The team found three distinct geological eras on Mars:
The team’s analysis led them to draw an intriguing conclusion: Liquid water didn’t make the Red Planet red. Instead, the team states, Mars most likely gets its glow from tiny grains of red hematite or possibly maghemite, both riddled with iron.
The Centre National d’Etudes Spatiales, Agenzia Spatiale Italiana
and the Russian Space Agency funded the OMEGA instrument. In the United
States, NASA supported OMEGA data analysis.
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