How will the public know when scientists have determined which scenario is right? Though geologists had bickered for 60 years before reaching a consensus on continental drift, Alvarez declared the extinction debate over and done within two years. Among those who disagreed with him was Keller. The impacters contend that the fossils of both marine- and land-dwelling organisms show an abrupt and instantaneous die-off at virtually the same moment, geologically speaking, that the asteroid hit. In the illustration, dinosaurs, gurgling lime-green vomit, writhe on a hill spotted with flames and charred tree stumps; just behind them, a diagonal gash in the ground blazes with lava and spews dark, swirling clouds. Big rock from sky hits the humans, and boom they go. We were snaking down a sinewy road one afternoon when Adatte hollered, the van screeched to a stop, and everyone scrambled out to inspect a steep hill in the elbow of a hairpin turn.
A priest came to administer last rites and, as Keller hovered in and out of consciousness, commanded her to confess her sins. This looked like circular logic to Keller, who in set out to investigate whether the two really were concurrent. More problematic still, Chicxulub did not appear to Keller to have been particularly deadly. Thierry Adatte and Wolfgang Stinnesbeck, who have worked with Keller for years, confirmed this. A mountain in the distance had been cut away, leaving a rectangular, unnatural pit. Keller fears that we are filling our environment with the same ingredients—sulfur, carbon dioxide, mercury, and more—that killed the dinosaurs and that, left unchecked, will catalyze another mass extinction, this one of our own devising. According to this well-established fire-and-brimstone scenario, the dinosaurs were exterminated when a six-mile-wide asteroid, larger than Mount Everest is tall, slammed into our planet with the force of 10 billion atomic bombs. People and animals developed deformed joints, softened bones, cracked gums, and strange growths on their bodies—all symptoms of fluorine poisoning. We were snaking down a sinewy road one afternoon when Adatte hollered, the van screeched to a stop, and everyone scrambled out to inspect a steep hill in the elbow of a hairpin turn. It is tempting, but unreliable, to trust what appears to be the majority opinion. Even the geologists, who had visited the Deccan Traps multiple times before, gaped at the landscape. Where we now stood was virtually within a blink of an eye of the mass extinction, she explained: Never before have I encountered someone so gleeful about catastrophe. Each one had its own mound of white earth beside it, as if waiting to be filled. An asteroid had crashed into the Earth, spewing iridium and pulverized rock dust around the globe and wiping out most life forms. They had found iridium—a hard, silver-gray element that lurks in the bowels of planets, including ours—deposited all over the world at approximately the same time that, according to the fossil record, creatures were dying en masse. Both sides accuse the other of ignoring data. The fifth extinction, the one that doomed the dinosaurs, occurred just as one of the largest volcanoes in history seethed in the Deccan Traps. She said impacters had warned some of her collaborators not to work with her, even contacting their supervisors in order to pressure them to sever ties. So what did cause it? The impacters contend that the fossils of both marine- and land-dwelling organisms show an abrupt and instantaneous die-off at virtually the same moment, geologically speaking, that the asteroid hit. Eddy licked a rock, to determine whether it was clay. The combination of carbon dioxide and methane would have eventually raised temperatures on land by as much as 46 degrees Fahrenheit, further acidifying oceans and making them inhospitable to plankton and other forams. No one could explain what they were. Throughout Europe, crops turned white and withered, and in June, desiccated leaves covered the ground as though it were October. At age 12, Keller wanted to become a doctor.
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