No mass extinction on Earth has been so tightly linked to an impact as the Chicxulub Crater which cuts across the northern Yucatan peninsula in Mexico in a mighty arc 170 kilometers (105 miles) across. The crater’s size implies an asteroid some 10 kilometers -seven miles- wide and reaching a depth as deep as the deepest ocean trench plunging the Earth into a global winter night that cut off photosynthesis for months, even years.
But one other may make the Chicxulub impact look like a 4th of July event: In 2006, NASA gravity and subsurface radar maps revealed a 500-kilometer-wide crater that lies hidden more than a mile beneath the East Antarctic Ice Sheet, created by a 50-kilometer wide object. The gravity measurements suggest that it could date back about 250 million years — the time of the Permian-Triassic extinction, when almost all animal life on Earth died out.
Its size and location — in the Wilkes Land region of East Antarctica, south of Australia — also suggest that it could have begun the breakup of the Gondwana supercontinent by creating the tectonic rift that pushed Australia northward.
Paleontologists believe that the Permian-Triassic extinction paved the way for the dinosaurs to rise to prominence. The Wilkes Land crater is more than twice the size of the Chicxulub crater, which marks the impact that may have ultimately killed the dinosaurs 65 million years ago. The void left at the K-T boundary created by the impact left the world to the mammals.
“This Wilkes Land impact is much bigger than the impact that killed the dinosaurs, and probably would have caused catastrophic damage at the time,” said Ralph von Frese, a professor of geological sciences at Ohio State University.
He and Laramie Potts, a postdoctoral researcher in geological sciences, led the team that discovered the crater. They collaborated with other Ohio State and NASA scientists, as well as international partners from Russia and Korea. They reported their preliminary results in a recent poster session at the American Geophysical Union Joint Assembly meeting in Baltimore.
The scientists used gravity fluctuations measured by NASA’s GRACE satellites to peer beneath Antarctica’s icy surface, and found a 200-mile-wide plug of mantle material — a mass concentration, or “mascon” — that had risen up into the Earth’s crust. Mascons form where large objects slam into a planet’s surface. Upon impact, the denser mantle layer bounces up into the overlying crust, which holds it in place beneath the crater.
When the scientists overlaid their gravity image with airborne radar images of the ground beneath the ice, they found the mascon perfectly centered inside a circular ridge some 300 miles wide — a crater easily large enough to hold the state of Ohio.
Taken alone, the ridge structure wouldn’t prove anything. But to von Frese, the addition of the mascon means “impact.” Years of studying similar impacts on the moon have honed his ability to find them.
“If I saw this same mascon signal on the moon, I’d expect to see a crater around it,” he said. “And when we looked at the ice-probing airborne radar, there it was.”
“There are at least 20 impact craters this size or larger on the moon, so it is not surprising to find one here,” he continued. “The active geology of the Earth likely scrubbed its surface clean of many more.”
He and Potts admitted that such signals are open to interpretation. Even with radar and gravity measurements, scientists are only just beginning to understand what’s happening inside the planet. Still, von Frese said that the circumstances of the radar and mascon signals support their interpretation.
“We compared two completely different data sets taken under different conditions, and they matched up,” he said.
To estimate when the impact took place, the scientists took a clue from the fact that the mascon is still visible.
“On the moon, you can look at craters, and the mascons are still there,” von Frese said. “But on Earth, it’s unusual to find mascons, because the planet is geologically active. The interior eventually recovers and the mascon goes away.” He cited the very large and much older Vredefort crater in South Africa that must have once had a mascon, but no evidence of it can be seen now.
“Based on what we know about the geologic history of the region, this Wilkes Land mascon formed recently by geologic standards — probably about 250 million years ago,” he said. “In another half a billion years, the Wilkes Land mascon will probably disappear, too.”
Approximately 100 million years ago, Australia split from the ancient Gondwana supercontinent and began drifting north, pushed away by the expansion of a rift valley into the eastern Indian Ocean. The rift cuts directly through the crater, so the impact may have helped the rift to form, von Frese said.
“All the environmental changes that would have resulted from the impact would have created a highly caustic environment that was really hard to endure. So it makes sense that a lot of life went extinct at that time,” he said.
The ultimate proof of the Antarctica impact theory lies in finding the shattered rock -the stuff of future expeditions and discovery.
Casey Kazan
Image above, combined image of gravity fluctuations and airborne radar in the Wilkes Land region of East Antarctica . The edges of the crater are colored red and blue; a concentration of mantle material is colored orange (center). Image courtesy of Ohio State University.
Source: http://www.spaceref.com/news/viewpr.html?pid=19996
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