How does the asteroid-impact hypothesis explain the extinction of the dinosaurs and other species?

THE KT-BOUNDARY IMPACT

Paintings and text copyright William K. Hartmann

Web page design by W. K. Hartmann and Daniel C. Berman

What Happened in Brief

According to abundant geological evidence, an asteroid roughly 10 km (6 miles) across hit Earth about 65 million years ago. This impact made a huge explosion and a crater about 180 km (roughly 110 miles) across. Debris from the explosion was thrown into the atmosphere, severely altering the climate, and leading to the extinction of roughly 3/4 of species that existed at that time, including the dinosaurs. Many asteroids of this type are now known; their orbits pass through the inner solar system and cross Earth's orbit. Some of these could potentially hit Earth in the future. Most, but not all are smaller than the one that hit us 65 million years ago.

Gaps in the Fossil Record

Fossils found in soil layers of different ages show a record of slow, gradual changes in species, with simple organisms gradually being replaced by more complex organisms, apparently by evolutionary processes driven by natural selection. For example, 1000 million years (abbreviate My) ago, the oceans held only simple organisms like algae, while the land was relatively lifeless. Fish fossils appear in strata after about 500-600 My ago; dinosaurs and giant reptiles were on the land by 200 My ago. Mammals were not common until after 65 My ago, and humanlike creatures appeared only in the last 4 My.

Ever since the fossil sequence began being mapped around 1800, geologists noticed that striking "breaks" occurred in the sequence, when one group of fossilized species gave way to other groups during short intervals. Indeed, these breaks were the basis for dividing geologic time into different eras with different names. For example, the Paleozoic era gave way to the Mesozoic era of middle life forms, which in turn gave way to the present Cenozoic era of recent life. Prior to the 1980s, the causes of the breaks were unknown...

How Was the Impact Event Discovered?

In the late 1970s, a team of geochemists headed by Luis Alvarez and his son Walter Alvarez, both with connections to the University of California at Berkeley, was studying chemical changes in soil layers corresponding to breaks in the fossil record. In the soil layer that separates the Mesozoic Era from the Cenozoic Era, dating 65 My ago, they found an excess of the element iridium, which is common in meteorites. Meteorites are believed to be fragments of asteroids. Therefore, the Alvarez team theorized that an asteroid had hit Earth at this time, and that the debris ejected from the explosion were spread in the soil layer.

For about ten years, this theory was extremely controversial. However, compelling evidence has accumulated to support the theory.

Evidence for the Impact Event

There are now many lines of evidence to prove that a relatively large impact happened 65 My ago.

1. The iridium excess in the 65 My-old soil layer has been confirmed at many points around the world.
2. The same soil layer contains grains of quartz that were deformed by high shock pressures, as would occur in a giant explosion. (The deformation is a microscopic structure called "twinning," in the crystals).
3. The same soil layer contains enough soot to correspond to burnding down all of the forests of the world. This suggests that massive fires were touched off at the time of impact.
4. The same soil layer, especially around the Gulf of Mexico, contains massive deposits of tumbled boulders, as would be generated in a large tsunami, or "tidal wave." The geographic distribution of tsunami deposits suggest the impact was in the Caribbean area.
5. After a decade of searching, scientists in 1990 identified the crater associated with this material. It is no longer visible on the surface of the Earth, but is buried under sediments. It straddles the coast of Yucatan. It is revealed by mapping the strength of the gravity field over that area, and by drilling; it has been dated to 65 My old.
6. Astronomers have charted numerous asteroids that cross Earth's orbit. From studies of orbit statistics, it is estimated that asteroids of 10 km size can hit the earth roughly every 100 My or so -- which fits with the idea that we actually did get hit 65 My ago by an object this size. (Smaller hits are much more common).

What Happened During the Impact?

Asteroids hit Earth typically at high speeds of 16 to 32 km/sec (10-20 miles/sec). During the impact, the kinetic energy in the asteroid (or energy of motion) is converted to explosive energy, blowing debris of dust, soil, and rocks not only into the atmosphere, but out into space, where it fell back into the top of the atmosphere. Early calculations in the 1980s (using in part ideas worked out by Carl Sagan and his colleagues) showed that so much dust entered the high atmosphere that the Earth was shrouded in a dust layer that blocked sunlight for several weeks or months. This would have killed some plants, disrupting the food chain.

  

 

Later calculations (especially by Jay Melosh at the University of Arizona) indicated that for the first few hours after the impact, rocky debris would have fallen back into the high atmosphere, creating a storm of glowing fireballs in the sky. The radiant energy from these would have heated the surface to boiling temperatures for some minutes, and would have been enough to kill many animals and plants on the surface. However, in regions of heavy rainstorms or snowstorms, these organisms would have survived the first few hours. Sea creatures would have been buffered from effects in the first hours, but plankton on the surface might have died out over the weeks of darkness, decreasing the food supply for small fish, which affected the bigger fish, and so on.

These examples show how hard it is to predict the exact effects of the impact. Many species who lived on the surface (such as dinosaurs) might have been decimated in hour or weeks. Species who lived in burrows, or hibernated (like some mammals) might have survived. This may explain why mammals replaced giant reptiles after the impact. Tiny primitive mammals may have emerged from their dens, to find that their giant reptile competitors were mostly gone.

Were All Breaks in the Evolutionary Record Caused by Asteroid Impacts?

Probably not. The biggest known break is the break between the Paleozoic Eara and the Mesozoic Era, about 230 to 250 My ago, when something like 90% of then-existing species died out. This has been called the "Great Dying," but has not been explained. So far there is no evidence of an asteroid impact at that time. The second greatest break is the one that we have discussed, 65 My ago, caused by an asteroid impact.

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What theory explains the extinction of dinosaurs and other plants and animals?