|A plot of data on mass extinctions in the past 250 million years.
Credit: University of Chicago
In geology as in cancer research, the silver bullet theory always gets the headlines and nearly always turns out to be wrong. For geologists who study mass extinctions, the silver bullet is a giant asteroid plunging to Earth.
But an asteroid is the prime suspect only in the most recent of five mass extinctions, said USC Earth scientist David Bottjer. The cataclysm 65 million years ago wiped out the dinosaurs.
"The other four have not been resolvable to a rock falling out of the sky," Bottjer said.
|The painting titled "K/T Hit" by artist Donald E. Davis. This impact occurred 65 million years ago, and many scientists believe it was linked to the demise of the dinosaurs.
Credit: Don Davis
The latest research from Bottjer’s group suggests a similar slow dying during the extinction 200 million years ago at the boundary of the Triassic and Jurassic eras.
At the 2008 Joint Annual Meeting of the Geological Society of America, USC doctoral student Sarah Greene drew similarities between ocean conditions at the Triassic-Jurassic boundary and after the end-Permian extinction. At both those times, bouquet-like structures of aragonite crystals formed on the ocean floor. Such structures are extremely rare in Earth’s history, Greene said.
"The fact that these deposits have only been found at these two specific times that are associated with mass extinction suggests at the very least that maybe there’s some shared ocean geochemistry that could be related to the cause of the extinctions," Greene said.
|Image of the Earth and Moon taken by Galileo spacecraft. The Earth is the only planet known to harbor life, and life’s future on Earth may depend on our understanding of climate change in the past, present and future.
"The Triassic-Jurassic extinction cause is totally up for grabs at the moment," she added.
Also at the meeting, USC doctoral student Rowan Martindale presented results from her studies of coral reefs during the Triassic-Jurassic extinction.
"The coral reefs look actually very similar to modern coral reefs," she said. "At the end-Triassic mass extinction, you lose all your reef systems. And nobody’s figured out why that is."
Martindale identified two distinct types of ancient reefs: one dominated by coral and another consisting mainly of mud and debris, possibly held together by bacteria. A theory for the end-Triassic extinction needs to explain how both types of reefs could have been killed off, Martindale said. Any knowledge about end-Triassic reef death could be useful in understanding the current reef crisis, widely attributed to climate change.
"We’re looking at it as a model to give us any insight that we might have for today’s decline for coral reefs," Bottjer said.
Related Web Sites
Astrobiology Roadmap Goal 4: Earth’s Early Biosphere and its Environment
Astrobiology Roadmap Goal 6: Life’s Future on Earth and Beyond
Great Impact Debate I: Benefits of Hard
Debating the Dinosaur Extinction
Extinction Followed Eruption
Reflecting on Climate Change