The extinction of the dinosaurs at the end of the Cretaceous period has long been attributed to a massive asteroid impact. However, recent evidence suggests that volcanic activity, specifically the Deccan Traps in India, may have been the primary cause. Three main arguments support this volcanic hypothesis. First, the Deccan Traps eruptions lasted for over a million years, releasing enormous amounts of sulfur dioxide and carbon dioxide. These gases would have caused severe global cooling followed by prolonged warming, creating climatic stress that could have disrupted ecosystems long before the asteroid impact. Second, geological records show that the dinosaur fossil record indicates a gradual decline in diversity over the last few million years of the Cretaceous, which aligns with the prolonged volcanic activity rather than a sudden impact. Third, the timing of the Deccan Traps eruptions coincides with the Cretaceous-Paleogene boundary, and some scientists argue that the eruptions reached their peak just before the mass extinction, suggesting that volcanic effects were the final blow. Therefore, a growing number of researchers contend that volcanic activity, not the asteroid, drove the dinosaurs to extinction.
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The lecture challenges the volcanic hypothesis presented in the reading. While the Deccan Traps eruptions were indeed massive, their climatic effects were not as severe as proposed. First, although sulfur dioxide can cause cooling, the Deccan Traps released gases over a long period, allowing natural processes like weathering and ocean absorption to buffer the climate. In contrast, an asteroid impact delivers a sudden, concentrated shock, which is far more disruptive. Second, the claim of gradual dinosaur decline is misleading. Many fossil sites show that dinosaur diversity remained high until the very end of the Cretaceous, and apparent declines in some regions may be due to sampling biases or incomplete fossil records. Third, the timing argument is flawed. Recent high-precision dating shows that the main phase of Deccan volcanism occurred about 300,000 years before the mass extinction, not at the boundary. Moreover, the Chicxulub impact in Mexico occurred exactly at the extinction layer, and its immediate effects—such as a global firestorm, tsunamis, and a dust cloud blocking sunlight—are consistent with a sudden mass kill. Thus, the lecture concludes that the asteroid impact remains the most plausible cause.
📝 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
Content Accuracy: Accurately capture the relationship between lecture and reading
Information Completeness: Cover all key counter-arguments from the lecture
Structure & Coherence: Logical organization and progression
Language Use: Grammar, vocabulary, expression accuracy
Scored 0-30 based on holistic scoring (original 0-5, scaled to 30).
