TOEFL 통합 작문

📖 읽기 지문

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 volcanic activity, specifically the eruption of the Deccan Traps in India, was the primary cause. First, volcanic eruptions release vast amounts of sulfur dioxide and carbon dioxide, which can cause rapid climate change. The Deccan Traps eruptions, which lasted for over a million years, would have produced enough greenhouse gases and aerosols to drastically alter global temperatures, leading to a collapse of ecosystems long before any asteroid struck. Second, the timing of the Deccan Traps eruptions aligns closely with the extinction event. Radioisotopic dating shows that the main phase of volcanic activity began about 66 million years ago, coinciding with the Cretaceous-Paleogene (K-Pg) boundary, whereas the asteroid impact occurred slightly later or at least its effects were not immediate enough to explain the gradual decline seen in fossil records. Third, the fossil record reveals a gradual decline in dinosaur diversity in the million years before the K-Pg boundary, which is more consistent with a slow, ongoing stressor like volcanic activity than with a sudden catastrophic impact. This pattern of decline is observed in many parts of the world, suggesting a global cause that predates the asteroid.

🎧 듣기 강의

The lecture challenges the volcanic theory presented in the reading. While volcanic activity did occur, the evidence strongly supports the asteroid impact as the primary cause. First, the climate effects of volcanic gases are not necessarily catastrophic. Sulfur dioxide can cause cooling, not just warming, and the Deccan Traps eruptions may have occurred in multiple pulses, some of which happened well before the extinction. In fact, some studies suggest that the most intense volcanic phase occurred about 300,000 years after the K-Pg boundary, not at it. Second, precise dating of the Chicxulub crater, the asteroid impact site, shows that it was formed exactly at the K-Pg boundary, with an error margin of only 30,000 years. This is a much more precise match than the volcanic record. Additionally, the impact would have released energy equivalent to billions of atomic bombs, causing immediate and global devastation, including wildfires, tsunamis, and a dust cloud that blocked sunlight for months, wiping out photosynthesizing organisms and collapsing the food chain. Third, the gradual decline in dinosaur fossils may be an artifact of incomplete fossil sampling. When scientists correct for sampling biases, the decline disappears, and dinosaurs appear to have been thriving right up to the impact. In contrast, the abrupt disappearance of many species at the boundary, including ammonites and marine reptiles, fits a sudden catastrophe. Therefore, the asteroid impact remains the most compelling explanation.