So, why an asteroid? What about the volcanic activity at the Deccan traps? The paleontolgists had several lines of evidence for this decision.
Shocked quartz, from Chicxulub |
- Shocked quartz: This is a rare form of quartz, that exists only at nuclear explosions and meteor impact. It is found world-wide through the layer of ash that marks the K-T boundary. This is a huge failing for the volcanic idea. There is simply no way any amount of eruption would create shocked quartz.
- Iridium layer: In that same layer of ash that the shocked quartz is found in, there is a huge spike in the iridium content. Iridium is a very rare element on the earth's surface, but shows up in asteroids fairly commonly. Some is also found in the earth's mantle, but not enough for volcanism to cause such a large spike.
- Speed of the extinction: In geologic time, the K-T boundary is an eyeblink. Dinosaurs and their compatriots, which had survived for 160 million years, were just gone. Poof. No more. Extreme volcanic activity would have significant short-term effects on climate, but it would have taken longer. The researchers found little evidence that many Mesozoic species were on the decline before the asteroid struck.
All this leads up to one conclusion: the Cretaceous-Tertiary mass extinction was caused by an asteroid. The evidence is overwhelming, especially upon reevaluation. One question, answered. Only infinitely many more to go.
Source: Science Daily- Asteroid Killed Off the Dinosaurs, Says International Scientific Panel