托福综合写作

📖 阅读文章

The extinction of the dinosaurs at the end of the Cretaceous period has long been attributed to a massive asteroid impact. However, a growing body of evidence suggests that intense volcanic activity in the Deccan Traps of India was the primary cause. First, the timing of the Deccan eruptions aligns closely with the extinction event. Radiometric dating shows that the main phase of volcanic activity occurred around 66 million years ago, coinciding with the Cretaceous-Paleogene boundary, whereas the Chicxulub impact occurred slightly earlier, about 300,000 years before the mass extinction. Second, volcanic emissions would have caused severe environmental stress. The Deccan eruptions released enormous quantities of sulfur dioxide and carbon dioxide, leading to acid rain, global cooling followed by warming, and ocean acidification—all of which could have disrupted ecosystems long before any impact. Third, the fossil record supports a gradual decline. In sediments just below the extinction boundary, paleontologists have found a decrease in dinosaur diversity and abundance, suggesting that dinosaurs were already struggling due to volcanic-induced climate change, not thriving until a sudden impact. Thus, the Deccan volcanism, not the asteroid, was the decisive factor in the dinosaurs' demise.

🎧 听力讲座

The lecture challenges the volcanic theory presented in the reading. While volcanic activity in the Deccan Traps is real, it was not the primary cause of dinosaur extinction. First, the timing argument is flawed. Although the Deccan eruptions began before the extinction, recent high-precision dating shows that the most intense phase of volcanism—the one that could release enough gas to alter climate—occurred after the extinction event, not at the boundary. The Chicxulub impact, in contrast, occurred exactly at the boundary, within a few thousand years of the fossil record's disappearance. Second, the environmental effects of volcanic gases were likely insufficient. Sulfur dioxide from the Deccan eruptions, while significant, would have been released over hundreds of thousands of years, allowing oceans and climate to buffer the changes. In contrast, the impact vaporized sulfate-rich rock and threw dust into the stratosphere, causing a sudden 'impact winter' that blocked sunlight for months, halting photosynthesis and collapsing food chains—a rapid and catastrophic effect that volcanism could not replicate. Third, the fossil evidence of gradual decline is misleading. The apparent decrease in dinosaur diversity near the boundary may be due to sampling bias or the Signor-Lipps effect, where the last fossils appear earlier than the true extinction time. In fact, when corrected for these biases, dinosaur fossils are found right up to the boundary, indicating healthy populations until the very end. Therefore, the asteroid impact, not volcanism, is the more plausible cause.