Escritura integrada TOEFL

📖 Texto de lectura

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 eruptions in India, was the primary cause. First, the timing of the Deccan Traps eruptions aligns closely with the extinction event. Radioisotopic dating indicates that the main phase of eruptions began about 66 million years ago, just before the extinction, and continued for roughly 1 million years. In contrast, the Chicxulub impact occurred at the exact boundary, but its effects were short-lived (only a few years to decades), whereas volcanic emissions would have caused prolonged environmental stress. Second, volcanic eruptions release vast amounts of sulfur dioxide and carbon dioxide, leading to acid rain, global cooling followed by warming, and ocean acidification. These chemical effects match the observed patterns of selective extinction, where marine organisms with calcium carbonate shells were particularly hard hit. Finally, the fossil record shows a gradual decline in dinosaur diversity over the last few million years of the Cretaceous, consistent with the long-term, cumulative stress from volcanic activity, rather than a sudden, catastrophic impact.

🎧 Conferencia de audio

The lecture challenges the volcanic hypothesis presented in the reading. While the Deccan Traps eruptions were indeed massive, their timing does not support a causal role. The main phase of eruptions actually began about 66.5 million years ago, which is 500,000 years before the extinction, and the largest eruption pulse occurred after the extinction event, not before. This mismatch undermines the claim that volcanism drove the extinction. Furthermore, the environmental effects of the Deccan Traps were likely insufficient to cause a global catastrophe. Although they emitted sulfur and carbon dioxide, the aerosols would have been washed out of the atmosphere within a few years, and the total volume of gases was spread over hundreds of thousands of years, limiting their climatic impact. In contrast, the Chicxulub impact vaporized sulfate-rich rock and ejected dust and soot into the stratosphere, causing a sudden, severe global cooling and darkness that shut down photosynthesis for months. This explains the rapid extinction of land plants and dinosaurs. Finally, the gradual decline in dinosaur diversity cited in the reading is not supported by recent high-resolution fossil data. In fact, dinosaur fossils are abundant right up to the Cretaceous-Paleogene boundary, indicating that they were thriving until the impact. The apparent decline is an artifact of incomplete sampling.