The researchers said the asteroid strike occurred 66.04 million years ago, plus or minus about 30,000 years. They said eruptions in a region called the Deccan Traps were already underway at a lower intensity but dramatically accelerated after the asteroid strike as if the powerful impact triggered it. The dating method they used found this acceleration began within 50,000 years of the impact, but it could have been in the mere days, months or years afterward. "Within measurement error, they're simultaneous," said volcanologist Loyc Vanderkluysen of Philadelphia's Drexel University. "The two processes in tandem caused the extinctions," added Paul Renne, director of the Berkeley Geochronology Center and a University of California, Berkeley geologist, who led the study in the journal Science.
Though many planetary scientists have discounted the Deccan Traps for decades, paleontologists have tended to favor it as a major factor in the extinction. This new study suggests that both were involved, which was the theory held by most of the more reasonable scientists in both fields. While many liked to push one or the other theory in the press, the better scientists considered both a possible factor and have been working to determine this possibility.
The cutting-edge facility was meant be ready for launches of Soyuz-2 rockets in December, but an unidentified space agency told the TASS news agency late Thursday that the rocket would not fit inside the assembly building where its parts are stacked and tested before launch. The building "has been designed for a different modification of the Soyuz rocket," the source said, according to news website Medusa, which picked up the story from TASS.
The rocket had just been delivered to Vostochny for assembly, so this report, though unconfirmed at this time, fits well with current events.
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