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The extinction of the dinosaurs at the end of the Cretaceous period, about 66 million years ago, has long fascinated scientists. While the asteroid impact theory is widely accepted, a competing hypothesis proposes that massive volcanic eruptions in the Deccan Traps of India were the primary cause. This volcanic theory rests on three key arguments. First, the Deccan eruptions were prolonged, lasting over a million years, and would have released vast quantities of sulfur dioxide and carbon dioxide. These gases could have caused rapid climate fluctuations, including severe global cooling and warming, which would have stressed ecosystems long before the asteroid struck. Second, recent high-precision dating suggests that the most intense phase of volcanism occurred just before the mass extinction, with some eruptions continuing after, implying a temporal link between peak volcanic activity and the die-off. Third, volcanic emissions could have produced acid rain and ozone depletion, directly harming plant and marine life, and the resulting environmental stress may have already pushed many species to the brink, making them vulnerable to a final blow, whether from volcanoes or an asteroid.

🎧 听力讲座

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📝 작문 지시 Summarize the points made in the lecture, being sure to explain how they cast doubt on the specific points made in the reading passage.

📊 TOEFL Integrated Writing Rubric

Scored 0-30 based on holistic scoring (original 0-5, scaled to 30).

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