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 closer examination of the fossil record and geological evidence suggests that volcanic activity, specifically the Deccan Traps eruptions in India, was the primary driver of this mass extinction. Three key lines of evidence support this volcanic hypothesis. First, the Deccan Traps eruptions began well before the asteroid impact, approximately 66.3 million years ago, and lasted for nearly a million years. This prolonged volcanic activity would have released enormous quantities of sulfur dioxide and carbon dioxide into the atmosphere, causing severe global cooling followed by long-term warming, ocean acidification, and disrupted photosynthesis. Such environmental stress would have gradually weakened dinosaur populations long before the impact. Second, the fossil record shows a gradual decline in dinosaur diversity in the few million years leading up to the extinction event, not a sudden die-off that would be expected from an instantaneous asteroid strike. For example, studies of dinosaur teeth and eggshells from the latest Cretaceous reveal signs of physiological stress, such as reduced thickness and abnormal morphology, indicating chronic environmental deterioration. Third, the timing of the main phase of Deccan volcanism coincides with the extinction horizon more precisely than the impact. Recent radiometric dating places the peak eruption phase at 66.0 million years ago, exactly at the Cretaceous-Paleogene boundary, whereas the Chicxulub impact occurred slightly earlier, possibly 66.04 million years ago, leaving a gap of several tens of thousands of years. This temporal mismatch suggests that volcanic eruptions, not the impact, delivered the final lethal blow.

🎧 Bài giảng

The reading presents a compelling case for volcanic activity as the main cause of dinosaur extinction, but its arguments do not hold up under scrutiny. First, while the Deccan Traps eruptions indeed began before the impact, the intensity of those earlier eruptions was relatively low. The most voluminous and explosive phase of volcanism did not occur until after the impact, as evidenced by the massive lava flows that overlay the impact layer in India. In fact, the impact may have triggered a surge in volcanic activity by causing seismic shaking that altered magma chamber pressures. Thus, the prolonged but mild volcanism before the impact was unlikely to have caused a global catastrophe. Second, the claim of a gradual dinosaur decline is based on incomplete sampling. Many fossil sites from the latest Cretaceous are poorly preserved or have not been thoroughly studied, and recent discoveries in the Hell Creek Formation show that dinosaur diversity remained high until just a few thousand years before the boundary. The apparent decline is an artifact of the Signor-Lipps effect, where the last appearance of fossils appears earlier than the true extinction due to incomplete preservation. Third, the radiometric dates cited in the reading are not as precise as suggested. While the peak Deccan volcanism may coincide with the boundary, the Chicxulub impact is now dated to 66.043 million years ago, with an uncertainty of only 11,000 years, whereas the Deccan peak spans a wider range. More critically, the impact generated a global dust cloud that blocked sunlight for months, causing a sudden collapse of photosynthesis on both land and sea, and a rapid drop in temperature. Such a rapid, catastrophic event is more consistent with the abrupt extinction pattern seen in the fossil record, including the disappearance of ammonites and many marine plankton groups exactly at the boundary. Volcanic eruptions, while significant, released gases and aerosols over tens of thousands of years, which would have allowed ecosystems to adapt gradually, not cause a sudden mass extinction. Therefore, the evidence strongly supports the asteroid impact as the primary cause, with volcanism playing only a secondary role.