TOEFL 통합 작문

📖 읽기 지문

The extinction of the woolly mammoth (Mammuthus primigenius) at the end of the Pleistocene has long intrigued scientists. While climate change and human hunting are often cited, a recent hypothesis argues that a catastrophic comet impact was the primary cause. This theory posits that an extraterrestrial object struck the Earth around 12,800 years ago, triggering a sudden cooling event known as the Younger Dryas, which devastated mammoth populations. Three lines of evidence support this claim. First, a distinct layer of sediment dating to this period contains high concentrations of iridium, a rare element in Earth's crust but common in asteroids and comets. This iridium anomaly is analogous to the one found at the dinosaur-killing Chicxulub impact, suggesting a similar cosmic collision. Second, the same sediment layer contains microscopic diamonds, known as nanodiamonds, which are formed under extreme pressures and temperatures typical of an impact. These nanodiamonds have been recovered from multiple sites across North America, implying a widespread impact event. Third, the timing of the mammoth's extinction correlates remarkably with the onset of the Younger Dryas, a rapid return to near-glacial conditions. The impact would have thrown vast amounts of dust and aerosols into the atmosphere, blocking sunlight and causing a sudden drop in temperatures, which would have destroyed the mammoth's grazing habitat. Thus, the comet impact hypothesis provides a compelling, unified explanation for both the extinction event and the abrupt climate shift.

🎧 듣기 강의

The lecture challenges the comet impact theory, arguing that the evidence is far from conclusive. First, the iridium anomaly is not unique to impact events. Volcanic eruptions, such as those from the Deccan Traps, can also release significant amounts of iridium. Moreover, the concentration found in the Younger Dryas layer is much lower than that at Chicxulub, and it is not consistently distributed across all sites, casting doubt on a single massive impact. Second, the nanodiamonds are problematic. Recent studies have shown that nanodiamonds can form in non-impact processes, such as forest fires or even lightning strikes. Furthermore, the original findings have been difficult to replicate, and some researchers have identified the particles as common carbon spheres rather than impact-related diamonds. Third, the temporal correlation is overstated. Radiocarbon dating shows that woolly mammoths survived well after the start of the Younger Dryas, with populations persisting on remote islands like Wrangel Island until around 4,000 years ago. In mainland regions, some populations declined gradually over thousands of years, which is inconsistent with a sudden catastrophic kill. Instead, paleontological evidence suggests that a combination of human overhunting and gradual climate-driven habitat loss, as the steppe tundra gave way to forests, better explains the extinction. The lecture concludes that while an impact is an intriguing idea, the current evidence fails to support it as the primary driver.