Cartoon by Chris Madden
Can sort through evidence and come up with a scientific theory that best fits the data.
Can recognize whether evidence is consistent with a scientific theory.
Can use geologic evidence to propose theories about past life on earth.
5 minute introduction
40-50 minutes to come up with theories
45-55 minutes to present theories and discuss conflicting theories
Groups of 3 students
There have been many mass extinctions throughout the history of the Earth. A mass extinction may be defined as an episode in geologic history where over half of the species in existence become extinct in a relatively short amount of time (just a few million years). The worst mass extinction came at the end of the Paleozoic Era 245 million years ago when nearly 95% of plant and animal life in the seas disappeared. Another mass extinction may be happening today. Evidence from the fossil record shows that, on average, only 10-100 species become extinct per year. Some estimates show that current rates of extinction are as high as 27,000 species per year.
Probably the most famous mass extinction happened 65 million years ago when the dinosaurs disappeared. This is generally called the K-T extinction since it occurred at the boundary between the Cretaceous (K) and Tertiary (T) periods. Whatever triggered the extinction of the dinosaurs also caused the death of nearly 60-70% of all the other species on Earth. Interestingly, not all groups of organisms were affected equally. Ocean species were hit harder than land-based species, with 90% of them becoming extinct. Birds were the only survivors of the dinosaur lineage. Interestingly, mammals, lizards, snakes, and other smaller terrestrial creatures were hardly affected. For some reason, ferns actually expanded and thrived during this time.
So what caused the dinosaur extinction? The clues can be found in the rocks that date from 65 million years ago. Some pieces of evidence are agreed upon by nearly all scientists:
Yet, even with an abundance of evidence, there is no consensus among scientists as to what happened at this time. Generally speaking, scientists are divided between two camps:
Gradualists – These scientists believe that the fossil record indicates a gradual decline over 5-10 million years. This time frame is more consistent with long term events such as plate tectonic forces and massive volcanic activity. These scientists believe that plate tectonic forces caused extensive volcanic activity in India and perhaps elsewhere that resulted in dense clouds of soot being released into the air. The soot darkened the skies resulting in global climate change and the reduced survival of plants, algae and plankton. In addition, the volcanoes likely released large quantities of carbon dioxide, further aggravating the climate through global warming and acid rain.
Catastrophists – These scientists believe that the fossil record indicates a sudden decline that is more consistent with a catastrophic event such as a massive asteroid impact. This theory was first proposed in 1980 by Walter Alvarez and is often referred to as the Alvarez Theory. He based his claims on the high iridium levels in rocks of that time period – suggesting that the isotopic profile of the iridium is more consistent with an extraterrestrial origin (a meteor or comet impact) than a volcanic origin. This is consistent with the presence of shocked quartz (metamorphically transformed quartz resulting from intense shock waves) in the rocks of that age. The resulting blast would have destroyed everything within 250-300 miles, including the object. Trillions of tons of debris (like dust, smoke, and steam) would have been thrown into the atmosphere when the object vaporized, darkening the sky around the globe in just a few weeks. Earthquakes, tsunamis, and wildfires would almost certainly have been triggered. The darkness may have only persisted for a few years but the effects on plant life would have been devastating.
The biggest problem with the catastrophic theory is that no conclusive crater has been identified. The most promising is evidence of an ancient crater called Chicxulub that was discovered in the Yucatan peninsula of Mexico. It is widely believed that Chicxulub is indeed the result of a massive asteroid nearly 6 miles across. Unfortunately, the crater itself is dated to 300,000 years before the K-T extinctions themselves. Could there have been another meteor impact or even a series of impacts? An even larger crater, the Shiva crater, was reported by Sankar Chatterjee under the Arabian Sea, off the coast of India. It is called the Shiva cater and dates from 65.0 million years ago. The Shiva crater is about 370 miles across and 7.5 miles deep. However, what created the crater is unknown. If it were made by an asteroid or meteoroid, the object must have been at least 25 miles wide. Other geologists claim the Shiva crater is the result of a sinkhole in the Earth’s surface, not an asteroid.
This ongoing debate offers an exciting opportunity for students to sort through the clues and propose a theory to explain the extinction of the dinosaurs. The key to this activity is for students to begin by organizing the evidence into sets of related information and then use the evidence to support a logical theory. Since there is no right answer students have an opportunity to engage in a true scientific debate over the same set of data that paleontologists, geologists, and astronomers argue over. Furthermore, there are endless directions in which the debate may travel, opening endless opportunities for further exploration.
Students should have an understanding of how fossils form and have experience with the geologic time scale. It is helpful to have a good foundation in the rock cycle and stratigraphy so as to better understand how the evidence provided may have been gathered.
There are many excellent websites that discuss the K-T extinction:
Earth and Life History (Earth Sciences)
4. Evidence from rocks allows us to understand the evolution of life on Earth. As a basis for understanding this concept:
a. Students know Earth processes today are similar to those that occurred in the past and slow geologic processes have large cumulative effects over long periods of time.
b. Students know the history of life on Earth has been disrupted by major catastrophic events, such as major volcanic eruptions or the impacts of asteroids.
e. Students know fossils provide evidence of how life and environmental conditions have changed.
g. Students know how to explain significant developments and extinctions of plant and animal life on the geologic time scale.