การเขียนเชิงบูรณาการ TOEFL

📖 เนื้อเรื่อง

The extinction of the dinosaurs at the end of the Cretaceous period, about 66 million years ago, has long been debated. While the asteroid impact theory is widely accepted, a competing hypothesis suggests that massive volcanic eruptions in the Deccan Traps of India were the primary cause. This volcanic theory is supported by three main arguments. First, the Deccan eruptions lasted for approximately 30,000 years, releasing enormous amounts of sulfur dioxide and carbon dioxide. These gases would have caused rapid climate fluctuations, including volcanic winters and greenhouse warming, which could have stressed ecosystems long before the asteroid struck. Second, fossil evidence shows a gradual decline in dinosaur diversity over the last few million years of the Cretaceous, consistent with a slow environmental deterioration caused by volcanism, rather than a sudden catastrophic event. Third, the timing of the most intense volcanic phase, known as the Poladpur eruptions, appears to coincide with the mass extinction horizon in many sedimentary records, suggesting that volcanic activity was the direct trigger of the extinction.

🎧 การบรรยาย

The lecture challenges the volcanic theory presented in the reading. First, while the Deccan eruptions released gases, their duration was too long to cause abrupt extinction. Climate modeling shows that the effects were spread over tens of thousands of years, allowing many species to adapt. In contrast, the asteroid impact at Chicxulub generated a short-term but severe global cooling and darkness, which is more consistent with a sudden mass die-off. Second, the claimed gradual decline in dinosaur diversity is not supported by high-resolution fossil data. Recent studies in North America show that dinosaur populations were stable until the very end of the Cretaceous, with no evidence of a long-term decline. The apparent decline in other regions may be due to sampling biases or incomplete fossil records. Third, the timing of the Poladpur eruptions is not precisely aligned with the extinction. Radiometric dating places the main extinction event at 66.04 million years ago, while the most intense volcanic phase occurred about 300,000 years earlier. The extinction layer contains iridium and shocked quartz, which are uniquely associated with an asteroid impact, not volcanism. Thus, the lecture argues that the asteroid impact remains the more plausible cause.