It’s amazing what cleaning your glasses can reveal. A mineral-scouting instrument developed at Arizona State University (ASU) has found an outcrop of rock rich in carbonate minerals in the Columbia Hills of Gusev Crater on Mars. The instrument is aboard NASA’s Mars Exploration Rover Spirit.
What makes the discovery unusual is that Spirit visited the outcrop, dubbed Comanche, back in December 2005. Yet the data pointing to the discovery languished since then because one of the instruments that detected the carbonate minerals was partly blinded by dust.
Dust in your eye
The instrument is the Miniature Thermal Emission Spectrometer (Mini-TES) developed at ASU. Each of the two Mars rovers carries a Mini-TES to identify minerals in rocks nearby. Philip Christensen, professor in the School of Earth and Space Exploration at ASU, designed the instrument.
“Mini-TES got dusted months before Spirit reached Comanche, and we didn’t have a good way to correct for the dust effects at the time,” said Steve Ruff, research scientist at ASU’s Mars Space Flight Facility. “We knew there was something weird about the outcrop’s spectrum as seen by Mini-TES, but couldn’t say what caused it.”
“Spirit’s Mossbauer spectrometer indicated that carbonate was possible, but I didn’t believe it,” Ruff said.
What finally did the trick was developing a calibration to remove the spectral effects of the dust on the instrument. Combined with the Mossbauer data and chemical data from a third spectrometer, “the Mini-TES spectra put the discovery over the edge,” said Ruff.
Warmer, wetter Mars?
Scientists have been searching for martian carbonate rocks for decades because such minerals are crucial to understanding the early climate history of Mars and the related question of whether the planet might once have held life.
“Small amounts of carbonate minerals have been detected on Mars before,” said Ruff. “The difference this time is that we’re seeing a couple of large outcrops of rock poking through the soil of the Columbia Hills. The rocks are about 25 percent carbonate by weight, by far the highest abundance we’ve seen on Mars.”
Born of water
Comanche and a neighboring small outcrop dubbed Comanche Spur have the same granular texture and Mini-TES spectral nature. Ruff said they are part of a stack of volcanic sedimentary rocks, draped over the underlying terrain.
“They’re definitely a puzzle to understand,” said Ruff. “The outcrops are very rich in olivine, a volcanic mineral, but they appear to have been soaked in water.” He explains that it’s as if the granular material settled over a pre-existing landscape, then the entire stack was flooded with carbonate-rich water, probably from a hydrothermal source.
NASA’s other Mars rover, Opportunity, has discovered ample evidence for alteration of rocks by water in Meridiani Planum, on the other side of Mars from Spirit’s Gusev Crater. But the water at Meridiani was strongly acidic. While life can evolve to survive in acidic conditions — such as in some of Yellowstone National Park’s geysers and hot springs — few scientists think it can start under those conditions.
Moreover, acidic water quickly destroys carbonate minerals, just like vinegar dissolves hard water deposits. The outcrops of carbonate rock show that the hydrothermal water at Comanche was liquid, chemically neutral, and abundant.
While there’s no evidence for life, Ruff said, the conditions would have been more favorable for it.
In plain view
Ironically, Ruff notes, the new finding complicates the story of the Columbia Hills. “This makes the geology harder to understand. It adds another environment to incorporate into the picture of how the Hills formed,” he said.
Looking at the big picture, Ruff said, “The Comanche data have been available to scientists and the public for about 4 years now. The new finding shows that this data set still harbors potential major discoveries.
“Do other surprises await us? Who knows? But I’ll make a strong prediction: more discoveries will be made with old data,” Ruff said.
