
A minuscule meteorite unlike any other we have discovered could help us understand the kinds of rocks that fill our solar system.
Maitrayee Bose at Arizona State University and her colleagues in a 2-millimetre meteorite found in Antarctica, called TAM19B-7. When they looked at the different carbon isotopes in the micrometeorite, they were in for a surprise.
“Some of the areas in the micrometeorite have the exact same composition as Earth,” says Bose. “But there were some regions that were carbon-13-rich hotspots, which is something that we didn’t expect to find at all.”
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The team spotted four of these little pockets of heavy carbon. The research was to have been presented at the now-cancelled Lunar and Planetary Science Conference in Texas.
The oxygen levels in the micrometeorite didn’t match any known asteroid. It is usually possible to match a micrometeorite to the asteroid family it belongs to, although not with this sample.
But we know its parent rock contained frozen water because of the abundance of other isotopes in the micrometeorite, primarily those of oxygen, says Bose.
“It comes from a body that has lots of ice, and when that ice melts it interacts with the rock,” she says. “The question is: can you make important, life-critical compounds by this interaction with water?”
On Earth, reactions between water and rocks can form sugars, amino acids and other chemicals important for life. Finding the micrometeorite’s mysterious parent could help us figure out if similar activity can occur on asteroids.
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