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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, specifically the Deccan Traps in India, was the primary cause. Three main arguments support this volcanic hypothesis. First, the Deccan Traps eruptions occurred over a period of approximately 1 million years, coinciding with the gradual decline of dinosaur populations observed in the fossil record. This extended timeline aligns with a slow extinction, rather than a sudden catastrophe. Second, volcanic eruptions released enormous quantities of sulfur dioxide and carbon dioxide, leading to severe climate change, including global cooling and ocean acidification. These environmental stresses would have disrupted food chains and habitats, causing many species to dwindle before the final extinction event. Third, the fossil record shows that many dinosaur species were already declining in diversity well before the asteroid impact, suggesting that volcanic activity, not the impact, was the driving force. Thus, while an asteroid may have delivered the final blow, the Deccan Traps volcanism created the conditions that made dinosaurs vulnerable to extinction.

🎧 听力讲座

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📝 Hướng dẫn viết 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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