NASA rover takes a closer look at organic carbon on Mars – World

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Using NASA’s Perseverance rover, scientists are getting a greater understanding of the nature of some of the organic carbon — the molecular backbone for all known ​living organisms — detected on Mars as they explore the question of whether Earth’s planetary neighbour ever harboured life.

New research describes the structure of the organic carbon ‌found last year by the rover in sedimentary rock that contained a potential biosignature — a possible sign of past microbial life. This mudstone formed perhaps between 3.2 and 3.8 billion years ago beneath a now-vanished body of water in Jezero Crater in the Martian northern hemisphere.

Organic carbon can be a clue as to whether Mars ever harboured life because it serves as the chemical underpinning for the molecules that build DNA, cells ​and proteins. But its presence is not proof of life because it also can arise in nonbiological processes such as chemical interaction between rock and water.

The detection of ​organic carbon in two rocks in Jezero Crater — given the names Cheyava Falls and Walhalla Glades — was disclosed last year when the researchers ⁠announced the discovery of a potential biosignature in one of them.

The two rocks were sampled by the rover at locations about 330 feet (100 meters) apart, according to planetary scientist Ashley ​Murphy of the Planetary Science Institute in Arizona, co-leader of the new research published in the journal Science Advances

Following last year’s discovery, NASA released an image of the Cheyava Falls rock showing a ​very fine-grained and rusty-red-colored mudstone bearing ring-shaped features resembling leopard spots as well as dark marks resembling poppy seeds.

Such features on Earth can be associated with microbial activity. A potential biosignature is defined as a substance or structure that may have a biological origin but needs more data or further study before a conclusion can be made about the absence or presence of life.

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