An outside researcher recently analyzed photos Curiosity took of an ancient sedimentary outcrop called Gillespie Lake, and noted some similarities to "microbially induced sedimentary structures" (MISS) here on Earth. Study author Nora Noffke, a geobiologist who is not a member of the Curiosity team, said the Gillespie Lake features could be consistent with a biological origin, but stressed repeatedly that this was just a hypothesis, and that she didn't regard the structures as proof of past Mars life.
Curiosity team members also noticed the Gillespie Lake structures (which include domes, cracks and pockets, among other shapes), said mission project scientist Ashwin Vasavada, of NASA's Jet Propulsion Laboratory in Pasadena, California. But the rover team arrived at a different interpretation.
"We really didn't see anything that can't be explained by natural processes of transporting that sand in water, and the nature of the rocks suggested that it was just a fluvial sandstone," Vasavada told Space.com.
"We do have several members of our team who are always keen to look out for things that might be caused by biological processes, but there was no reason, we felt, to explore that at that site," he added. "It came down to nothing exceptional, from our point of view, that wasn't just a consequence of erosion of this sandstone."
Vasavada also stressed that he and the rest of the Curiosity rover team welcome analyses by outside researchers such as Noffke.
If mission scientists had decided to study Gillespie Lake more closely, they could have taken up-close photos using Curiosity's Mars Hand Lens Imager, Vasavada said, or drilled the rock to deliver powder to the Sample Analysis at Mars (SAM) instrument, which is capable of detecting carbon-containing organic molecules.
The Curiosity team did decide to drill into a layer of fine-grained mudstone dubbed Sheepbed, which lies directly beneath Gillespie Lake within a broader region near the rover's landing site called Yellowknife Bay.
SAM's analysis of the Sheepbed mudstone, along with other Curiosity observations, allowed the rover team to determine that Yellowknife Bay could have supported microbial life in the ancient past. About 3.5 billion years ago, the area was part of a lake-stream system that may have been habitable for millions of years, mission scientists said.
SAM also detected organics in the Sheepbed sample, marking the first definitive detection of life's building blocks on Mars.
"We feel that choice paid off," Vasavada said of the focus on Sheepbed.
Read more at Discovery News
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