A new theory may explain how gold, platinum, and other precious metals found their way to shallow pockets within Earth’s mantle rather than deep in the planet’s core.
More broadly, the new theory offers insights into planet formation throughout the universe.
The new work provides valuable information about the story of gold.
It’s a story that begins with violent collisions of large objects in space, continues in a half-melted region of Earth’s mantle, and ends with precious metals finding an unlikely resting spot much closer to the planet’s surface than scientists would have predicted.
“Our research is a good example of making an unexpected discovery after re-examining conventional wisdom,” says Jun Korenaga, a professor of earth and planetary sciences at Yale University.
Korenaga and Simone Marchi, a researcher at SRI in Boulder, Colorado, are coauthors of the study in the Proceedings of the National Academy of Sciences.
Recent research from scientists around the world has established that precious metals such as gold and platinum came to Earth billions of years ago after the early proto-Earth collided with large, moon-sized bodies in space, which left behind deposits of materials that were folded into what is today’s Earth.
But that absorption process has remained something of a mystery.
Aside from being valued for their scarcity, aesthetic beauty, and use in high-tech products, gold and platinum are what is known as highly “siderophile” elements. They are drawn to the element iron to such a degree that they would be expected to collect almost entirely in Earth’s metallic core—either by merging directly with the metal core on impact or by sinking quickly from the mantle into the core.
By this logic, they should not have collected at or near the Earth’s surface. Yet they did.
“Working with Simone, who is an expert on impact dynamics, I was able to come up with a novel solution to this conundrum,” Korenaga says.
Korenaga and Marchi’s theory centers around a thin, “transient” region of the mantle, where the shallow part of the mantle melts and the deeper part remains solid. The researchers found that this region has peculiar dynamic properties that can efficiently trap falling metallic components and slowly deliver them to the rest of the mantle.
Their theory posits that this delivery is still ongoing, with the remnants of the transient region appearing as “large low-shear-velocity provinces”—well-known geophysical anomalies in the deep mantle.
“This transient region almost always forms when a big impactor hits the early Earth, making our theory quite robust,” Marchi says.
The researchers say the new theory not only explains previously enigmatic aspects of Earth’s geochemical and geophysical evolution, but it also highlights the wide range of time scales involved in Earth’s formation.
“One of the remarkable things we found was that the dynamics of the transient mantle region take place in a very short amount of time—about a day—yet its influence on subsequent Earth evolution has lasted a few billion years,” Korenaga says.
NASA and the National Science Foundation funded the work.
Follow us on Twitter for more articles about this topic.
