Newly discovered, unusual carbon on Mars could indicate life

© NASA/Caltech-JPL/MSSS

Science

NASA’s Curiosity rover has taken soil samples on Mars that may indicate life forms.

In samples from buried sediment, a Carbon isotope found at taken from half a dozen exposed sites. According to the researchers 3 plausible explanations

exist for the origin of carbon : cosmic dust, ultraviolet degradation of carbon dioxide, or ultraviolet degradation of biologically produced methane, which would be indicative of life on Mars. As the researchers note in the Proceeding of the National Academy of Sciences, all of these scenarios are unconventional and different from processes that are common on Earth.

No evidence for biological origin

As if from a broadcast by the research team around Christopher House from Pennsylvania State University, spectrographic analysis indicated a wide range Carbon 12 and Carbon 13 moieties. A portion was exceptionally poor in carbon 13 while other carbon samples were enriched.

“The Extremely depleted samples of carbon 13 are somewhat similar to samples from Australia, which come from 2.7 billion year old sediments,” House said. “These samples were caused by biological activity as methane was consumed by ancient microbial layers, but we can’t necessarily on Mars because it is a planet that may have formed from different materials and processes than Earth .” Thus, the evidence is not proof of life on the Red Planet.

Cosmic Dust

Another possible explanation for lower levels of carbon 13 is the ultraviolet conversion of carbon dioxide into organic compounds such as formaldehyde.

“All three possibilities point to a unusual carbon cycle in a way that doesn’t exist on Earth today,” says House. “But we need more data to figure out which of these is the correct explanation. It would be nice if the rover could detect a large methane plume and measure the carbon isotopes from it.” Methane plumes do exist, but most are small, and no rover was able to take a sample large enough to measure the isotopes.

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