An international team of 38 scientists, including Rutgers’ Sonia Tikoo, has shown how large asteroid impacts deform rocks and possibly create habitats for early life on Earth and elsewhere.
Around 65 million years ago, a massive asteroid crashed into the Gulf of Mexico, causing an impact so huge that the blast and its aftermath wiped out about 75 percent of all life on Earth, including most of the dinosaurs. It’s known as the Chicxulub impact.
In April and May, scientists on an offshore expedition drilled deep into part of the Chicxulub impact crater. Their mission was to retrieve samples from the rocky inner ridges of the crater – known as the “peak ring” – drilling about 1,600 to 4,380 feet below the modern-day sea floor to learn more about the ancient cataclysmic event.
Now, the researchers have performed the first analysis of the core samples in a study published online today in the journal Science. They found that the impact deformed the peak ring rocks, making them more porous and less dense than models had predicted.
“Chicxulub crater is the only crater on Earth that has such a well-preserved peak ring and since we can’t get samples of peak rings from other planets yet, it’s really our best window into understanding the formation of large impact basins anywhere in the solar system,” said Tikoo, an assistant professor in the Department of Earth and Planetary Sciences in the School of Arts and Sciences. “We really didn’t know the exact physical mechanisms behind how peak ring craters form until this study.”
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