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Hot Topic Solar System Mars Calibrated for Carbonates
 
Calibrated for Carbonates
Based on an Arizona State University news release
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Mars
Posted:   06/05/10

Summary: NASA's Mars Exploration Rover Spirit has identified an outcrop of rock that only could have formed in water that was not acidic. The finding is crucial in understanding the planet's early climate and the potential for habitable environments on ancient Mars.

ASU Instrument on NASA Rover Helps Identify Outcrop of Long-Sought Rare Rock on Mars

More than four years after Mars rover Spirit visited the Comanche outcrop in Gusev Crater's Columbia Hills, scientists armed with a new instrument calibration have discovered the rocks are rich in long-sought carbonate minerals. Comanche (left) and Comanche Spur (right) appear reddish-brown in this false-color image from Spirit's Pancam. (The bluish-wite rocks in the foreground belong to an unrelated outcrop.) Credit: NASA/JPL/Cornell University
It’s amazing what cleaning your glasses can reveal. A mineral-scouting instrument developed at Arizona State University has found an outcrop of rock rich in carbonate minerals in the Columbia Hills of Gusev Crater on Mars, according to a report published online June 3 in the journal Science. The instrument is onboard 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, or Mini-TES, developed at Arizona State University. Each of the two Mars rovers carries a Mini-TES to identify minerals in rocks nearby. The instrument was designed by its Principal Investigator, Philip Christensen, an ASU Regents’ Professor in the School of Earth and Space Exploration, part of the College of Liberal Arts and Sciences.

“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,” says Steve Ruff, research scientist at ASU’s Mars Space Flight Facility. Ruff is one of a team of scientists on the paper, whose lead author is Richard V. Morris of NASA’s Johnson Space Center in Houston. “We knew there was something weird about the outcrop’s spectrum as seen by Mini-TES, but couldn’t say what caused it.”

Ruff adds, “Spirit’s Mossbauer spectrometer indicated that carbonate was possible, but I didn’t believe it.”

Seen close up, the Comanche outcrop shows both a granular texture and multiple layers. Scientists think it is volcanic debris draped over preexisting terrain. After it was deposited, the rock was soaked in hydrothermal water rich in carbonate minerals. False-color Pancam image. Credit: NASA/JPL/Cornell University
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,” says 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,” says Ruff.

The difference this time, he says, “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 says they are part of a stack of volcanic sedimentary rocks, draped over the underlying terrain.

“They’re definitely a puzzle to understand,” says 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 preexisting landscape, then the entire stack was flooded with carbonate-rich water, probably from a hydrothermal source.

Thin blades protrude like fins from Comanche Spur just below Spirit's instrument arm (left). These mark where carbonate-rich water left fracture-filling deposits, which have proved somewhat more resistant to erosion than the surrounding rock. This image was taken by Spirit's Hazcam; for scale, the rover's wheels are 10 inches in diameter. Credit: NASA/JPL/Cornell University

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, as for example vinegar dissolves hard water deposits. Thus finding outcrops of carbonate rock shows that the hydrothermal water at Comanche was liquid, chemically neutral, and abundant.

While there’s no evidence for life, Ruff says, 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 says.

Looking at the big picture, Ruff notes, “the Comanche data have been available to scientists and the public for about four years now. The new finding shows that this data set still harbors potentially major discoveries.

“Do other surprises await us? Who knows? But I’ll make a strong prediction: More discoveries will be made with old data.”

 


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