May 6, 2013 in City

Rock Doc: Mass extinctions way more than just meteorites

E. Kirsten Peters
 

 

As any child can tell you, the Mesozoic Era ends with the extinction of the dinosaurs. Most geologists think the cause of that extinction was the impact of an enormous meteorite that hit the Yucatan Peninsula in Mexico. As the theory goes, the impact was so large it led to global changes in the composition of the atmosphere. Smoke and dust raised by the collision blocked the sun’s light for a time, making temperatures drop and plants die off. Many species of both plants and animals didn’t live through the crisis, as parts of the food web simply fell apart. As it happens, the dinos were one group that gave up the ghost and slipped into extinction.

 The extinction that carried off the dinosaurs is one of five mass extinctions in the geologic record during the last three eras of geologic time: the time marked by animals of sharply increasing complexity first in the seas and then on land. Because the dinosaurs are famous around the world, the extinction that killed them is often discussed in public circles. But the other mass extinctions’ causes interest scientists just as much.

 New evidence has come to light recently about the mass extinction that occurred during, rather than at the end of, the Mesozoic Era. The time in question stands at the boundary between the Triassic Period and the Jurassic Period (think of the movie “Jurassic Park” if you want a little help with these names). The extinction at issue saw the end of three-quarters of the species then living in the seas and on land. The massive die-off helped clear the ground for the dominance of the dinosaurs for more than the next 100 million years.

In the early Mesozoic, what is now North America was united with Europe as part of a supercontinent called Pangaea. Pangaea broke up into separate continents as geologic time unfolded. Volcanic rocks of the same type and age are found along the East Coast and in Morocco, areas next to each other in the Triassic. The rocks resulted from a giant rift in the crust of the Earth, one that ultimately grew to become the Atlantic Ocean.

 The massive eruptions that occurred in the late Triassic Period created what’s called the Central Atlantic magmatic province, or CAMP. Along with volcanic rock, the eruptions would have added carbon dioxide and other gases to the atmosphere, potentially triggering strong climate change.

 The new evidence about CAMP published in the journal Science relates to the age of the volcanic rocks in question. Sophisticated dating techniques now indicate the whole CAMP province of volcanic rocks was formed during a period of only 40,000 years. Geologically speaking, that’s nearly instantaneous. Such a massive outpouring of lava in such a short time could well have rapidly changed the atmosphere and climate.

 The more we learn about major extinctions, the more respect we must have for the ferocity of Mother Nature. Let’s hope we don’t live long enough to see her bare her volcanic claws once more.

Dr. E. Kirsten Peters, a native of the rural Northwest, was trained as a geologist at Princeton and Harvard universities. This column is a service of the College of Agricultural, Human and Natural Resource Sciences at Washington State University.


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