By studying streams on the English Channel coast, researchers have calculated how much organic matter we might find on Mars.
Dorset, a county located in the South West England of the United Kingdom is home to highly acidic sulfur streams that host bacteria that thrive in extreme conditions. One such environment, in St Oswald’s Bay, mimics the conditions on Mars billions of years ago, researchers said.
Dorset, a county located in the South West England of the United Kingdom is home to highly acidic sulfur streams.
The scientists from London's Imperial College concluded that there could be nearly 12,000 Olympic sized pools of organic matter on Mars that could represent traces of past life. "Mars harbored water billions of years ago, meaning some form of life might have thrived there," said Mark Sephton, Head of Imperial's Department of Earth Science & Engineering.
"If life existed before the water dried up, it would probably have left remains that are preserved to this day in Martian rock," said Sephton. The scientists treated the landscape as a template for Mars and examined the organic matter preserved in rock deposits nearby.
The iron-rich mineral goethite transforms to hematite which is very common on Mars and gives the planet its red color. If these iron-rich minerals harbor traces of life on Earth, then they may hold clues to past microbial life on the red planet. The study, published in the journal Scientific Reports, found that goethite in the county’s St Oswald's Bay hosted many microbes as well as traces of their fossilized organic remains.
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The researchers applied these results to a martian environment. Based on how much rock is from acid environments on Mars, and assuming the concentration of fatty acids found in martian sediments matches that of Earth, there might be up to 2.86 1010 kg of fatty acids preserved within martian rock -equivalent to nearly 12,000 Olympic-size pools. Previous missions to find traces of life have used heat to inspect rock for the presence of organic matter.
Scientists suspect the heat might have caused minerals to react with any organic matter, explaining why we have not yet found traces of life. However, heating goethite or hematite does not destroy any organic matter that is there, meaning these minerals could be good life-search targets. "We have yet to find convincing traces of organic matter that would indicate previous life on the red planet," Sephton said.
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