NY Times July 25, 2011
Blame for Extinction Spreads to Methane Gas
By SINDYA N. BHANOO
Two hundred million years ago, at the end of the Triassic period, a mass 
extinction, often attributed to major volcanic activity, wiped out half of all 
marine life on Earth. But new research published in the journal Science 
suggests that the extinction was more likely to have been caused by the release 
of at least 12,000 gigatons of methane from the seafloor into the atmosphere.

Volcanic activity occurred over a period of 600,000 years at the end of the 
Triassic, while the extinction took place over a period of just 10,000 to 
20,000 years, said Micha Ruhl, an earth scientist at the University of 
Copenhagen in Denmark and the study’s lead author.

Dr. Ruhl and his colleagues studied carbon isotopes of sediments from the 
period and found that the extinction event coincided with the giant release of 
methane into the atmosphere.

Volcanoes still played in a role in the process, Dr. Ruhl said.

“There was a release of CO2 from volcanic eruptions that warmed up global 
temperatures and also the ocean,” he said. “Methane is only stable under 
certain temperatures. If it gets warm, it is released.”

The study could be foreshadowing the effect of climate change on Earth, Dr. 
Ruhl said. An increase of carbon dioxide in the atmosphere from fossil-fuel use 
could warm up the planet enough to release methane from the ocean floors, he 
said.

“Methane is a much stronger greenhouse gas than CO2, so potentially that could 
result in a strong increase in temperature and climate change,” he said.

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