Viết tích hợp TOEFL

📖 Đoạn văn

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 in India, was the primary cause. First, the timing of the Deccan Traps eruptions aligns closely with the mass extinction event. Geochemical dating shows that the main phase of volcanic activity occurred just before and around the Cretaceous-Paleogene (K-Pg) boundary, and the eruptions lasted for hundreds of thousands of years, releasing enormous amounts of lava. This prolonged volcanic activity would have caused severe environmental stress, whereas an asteroid impact is a sudden, single event. Second, volcanic emissions of sulfur dioxide and carbon dioxide would have led to drastic climate changes, including global cooling from sulfate aerosols and subsequent warming from greenhouse gases. Such climate oscillations could have disrupted ecosystems long before any impact. Finally, the fossil record indicates a gradual decline in dinosaur diversity in the millions of years leading up to the K-Pg boundary, which is more consistent with a slow, ongoing stressor like volcanism rather than a sudden catastrophic impact. While an asteroid impact may have delivered the final blow, the volcanic activity was the primary driver of the extinction.

🎧 Bài giảng

The lecture challenges the idea that volcanic activity was the main cause of dinosaur extinction. While the Deccan Traps eruptions were indeed massive, their timing does not precisely match the extinction event. High-precision radiometric dating reveals that the most intense phase of volcanic activity occurred about 200,000 years before the K-Pg boundary, and by the time of the impact, volcanic emissions had largely subsided. This weakens the link between peak volcanism and the extinction. Furthermore, the climate effects of volcanic emissions were not as severe as the reading suggests. Studies of paleoclimate indicators, such as oxygen isotopes in marine sediments, show that temperature fluctuations during the Deccan Traps were relatively modest and occurred over long timescales, allowing many species to adapt. In contrast, the asteroid impact caused a sudden and extreme global cooling, known as an impact winter, which was far more lethal. Finally, the claim of a gradual dinosaur decline is not supported by recent fossil evidence. In fact, dinosaur fossil assemblages from the latest Cretaceous are diverse and abundant, indicating that dinosaurs were thriving right up to the impact. The apparent decline in earlier studies was likely due to sampling biases and incomplete fossil records. Thus, the asteroid impact remains the most plausible and immediate cause of the mass extinction.