What Killed The Dinosaurs?

Scientists have long theorized that the dinosaurs met their demise at the hands of a giant asteroid, but the circumstances of such an event have thus far remained murky. Now, a team of American and European researchers have shed new light on the incident, lending extra weight to an already widely-adopted theory.

Researchers have spent years trying to find a direct connection between the Cretaceous-Tertiary extinction event (K-T, for short) and cosmic collision. They found a lead in the late 1970s, when geophysicist Glen Penfield discovered a giant prehistoric crater near the town of Chicxulub in Mexico. At more than 110 miles wide, the crater provided evidence of an utterly massive impact — one that would have released an explosion one billion times stronger than the atomic bombs dropped on Hiroshima and Nagasaki during World War II. The only problem, however, was figuring out whether this asteroid's collision actually coincided with the extinction of the dinosaurs.

Two main camps exist in paleontology today, each having a different view of what killed the dinosaurs and other organisms at the K-T boundary. Controversy has surrounded the topic since 1980; it has become difficult for the public (and the scientific world at large) to understand the issue due to the tangled assemblage of data which seems to point in many different directions. Luckily, the controversy has not harmed the study of mass extinction causation, but rather has made it a dynamic and interesting area. Every groundbreaking new hypothesis makes new headlines in the media, and excites researchers to delve further into the mystery.

The major sides of the schism can be broken down (greatly simplifying the issue, but making it more accessible) into "intrinsic gradualists" and "extrinsic catastrophists." We'll describe each generalized group in turn, and then try to synthesize the available information so you can form your own opinion. But first, let's outline what scientists generally agree that we know about the K-T boundary.

The common ground

• There was global climatic change; the environment changed from a warm, mild one in the Mesozoic to a cooler, more varied one in the Cenozoic. The cause of this climate change, and the speed at which it proceeded, are the major concerns of both schools of thought.
• As well as a permanent global climatic change, there is evidence that there were less lasting changes at the end of the Cretaceous period. These changes may have been the result of a massive terrestrial disturbance, which threw up soot into the air, causing short term acid rain, emission of poisonous gases, and cooling (similar to a nuclear winter). Long term consequences would have been a globalgreenhouse effect (warming and reduced sunlight).
• As discussed before, many organisms; both marine and terrestrial, vertebrate and invertebrate; went extinct. The reason for this extinction was probably this climate change.
• At or near the K-T boundary in several places around the globe, we have a thin layer of clay with an unusually high iridium (a rare metal similar to platinum) content. This may be evidence for the dust cloud in #2 above.

The "intrinsic gradualists"

Those scientists falling into this category believe that the ultimate cause of the K-T extinction was intrinsic; meaning of an Earthly nature; and gradual, taking some time to occur (several million years). Two main hypotheses exist today:

• Volcanism: We are quite certain that the end of the Cretaceous period that there was increased volcanic activity. Over a period of several million years, this increased volcanism could have created enough dust and soot to block out sunlight; producing the climatic change. In India during the Late Cretaceous, huge volcanic eruptions were spewing forth floods of lava which can be seen today at the K-T boundary (these ruptures in the Earth's surface are called the Deccan traps). The chemical composition of the lava rocks in India shows that they originated in the Earth's mantle, which is also relatively rich in iridium. This richness would explain the iridium layer.
• Plate Tectonics: Major changes in the organization of the continental plates (continental drift) were occurring at the K-T boundary. The oceans (especially the Interior Seaway in North America) were experiencing a regression; they were receding from the land. A less mild climate would have been the result, and this would have taken a long time. Large scale tectonic events did occur in the Mesozoic several times, and no extinction events have been conclusively associated with them yet.

Note that these two above hypotheses are inextricably tied together; volcanism cannot occur without the action of plate tectonics, and vice versa. If the extinction was intrinsic and gradual, both processes probably played a role. Also note that the basic theory here is an elaboration of the 'dinosaurs faded away' hypothesis from the invalid hypotheses section; it adds a factor of causation that is quite convincing.

The "extrinsic catastrophists"

This side of the controversy holds that the ultimate cause of the K-T extinction wasextrinsic, meaning of an extraterrestrial nature, and catastrophic, meaning fairly sudden and punctuated. The main hypothesis was proposed in 1980 by (among others) Luis and Walter Alvarez of the University of California at Berkeley.

The Alvarez Hypothesis: The original hypothesis is the basis for several subsequent variations on the theme that a large extraterrestrial object collided with the Earth, its impact throwing up enough dust to cause the climatic change. The iridium layer is what prompted the Alvarez team to blame an asteroid impact for the extinction — asteroids and similar extraterrestrial bodies are higher in iridium content than the Earth's crust, so they figured that the iridium layer must be composed of the dust from the vaporized meteor. No crater was found, but it was assumed that one existed that was about 65 million years old and 100 kilometers (about 65 miles) in diameter.

Later research found a likely candidate for the crater at Chicxulub, on the Yucatan Peninsula of Mexico. Other evidence was also reported: the presence of shocked quartzin the rocks of the K-T boundary (indicating the passage of a shock wave so powerful that it actually rearranged the crystal structure of quartz grains), glassy spheres that looked like impact ejecta (molten rock that solidified into droplets when cooled), and a soot layer was found in many areas (evidence for widespread forest fires). The likelihood that massive hurricanes and firestorms would have raged across the Earth was also hypothesized, adding to the destructive power of the catastrophe.

To reconcile the hypothesis with gradual data, it was suggested that rather than one impact, several impacts (of comets or meteors) could have occurred over a period of many years. Some evidence supported this — a hint of periodicity of mass extinctions in the fossil record was reported; mass extinctions seemed to occur roughly every 26 million years. Astronomers theorized that the Oort cloud of comets could cross the path of our solar system every 26 million years, and would possibly rain comets on our planet for a few million years. The existence of a tenth, as-yet unseen planet — or Nemesis, the twin star to our sun — both with large orbits were also contemplated. To date, no reliable evidence for periodicity or Nemesis-type celestial bodies has been found, but this does not render the hypothesis obsolete; it is accepted that any large extraterrestrial body impacting the Earth's surface could and would produce climatic changes similar to those thought to have occurred around the K-T boundary.

Previous studies have estimated that the Chicxulub asteroid struck some 300,000 years before the dinosaurs' demise, leading some to suspect alternative causes for their extinction. But a study published this week shows that the two events happened no more than 33,000 years apart — a small margin when considering time on such a large scale. Researchers arrived at their findings after conducting high-precision radiometric dating of debris near Chicxulub, providing strong evidence that the dinosaurs died off as a direct result of the asteroid's impact.

"We've shown the impact and the mass extinction coincided as much as one can possibly demonstrate with existing dating techniques," Paul Renne, study co-author and director of the Berkeley Geochronology Center, told LiveScience. The asteroid in question is believed to have been six miles wide, and its impacts were likely devastating, blocking out the sun with a thick cloud of dust, unleashing mega-tsunamis across the world, and possibly igniting massive firestorms. The collision alone is believed to have wiped out 75 percent of life on Earth.

Renne was quick to note, however, that the dinosaurs' extinction can't be attributed to the cosmos, alone. Earth's climate was already reaching a tipping point before the asteroid ever hit, leading to long cold snaps and volcanic eruptions. "The impact was clearly the final straw that pushed Earth past the tipping point," Renne said. "We have shown that these events are synchronous to within a gnat's eyebrow, and therefore, the impact clearly played a major role in extinctions, but it probably wasn't just the impact."