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 Deccan Traps eruptions in India, played a more significant role. Proponents of the volcanic hypothesis argue three main points. First, the Deccan Traps eruptions began well before the asteroid impact and lasted for over a million years, releasing enormous amounts of sulfur dioxide and carbon dioxide. These gases would have caused severe global cooling and ocean acidification, stressing ecosystems long before the impact. Second, the timing of the most intense volcanic phase coincides with the mass extinction event, suggesting a causal link. Geochemical signatures from this period show a spike in mercury, a volcanic tracer, exactly at the extinction boundary. Third, volcanic eruptions could have produced enough dust and aerosols to block sunlight, leading to a 'volcanic winter' that disrupted photosynthesis and collapsed food chains, similar to the effects predicted for an asteroid impact. Thus, while an impact may have occurred, the prolonged volcanic activity was the primary driver of the end-Cretaceous extinction.

🎧 듣기 강의

The lecture challenges the volcanic hypothesis for the dinosaur extinction, arguing that the asteroid impact remains the most plausible cause. First, the Deccan Traps eruptions were not continuous but occurred in pulses, with long quiet intervals. The most intense phase actually happened about 200,000 years before the extinction, not at the boundary. This temporal mismatch weakens the causal link. Second, the mercury spike cited as volcanic evidence is not unique; it can also result from impact-related processes, such as vaporization of mercury-rich target rocks. Moreover, the abruptness of the extinction—occurring within a few thousand years—is inconsistent with the gradual, long-term effects of volcanism. Third, while volcanic aerosols can cause cooling, the geological record shows that the warming and cooling cycles during the Deccan eruptions were modest and did not lead to mass extinctions. In contrast, the asteroid impact at Chicxulub released energy equivalent to billions of atomic bombs, triggering a sudden global firestorm, a dust cloud that blocked sunlight for months, and a subsequent impact winter. These catastrophic effects, not gradual volcanism, best explain the rapid and selective extinction of large terrestrial animals and marine reptiles.