For Kids Current Volcano Activity Reports Volcano Topics Meet the folks behind VW
Lessons and Educator Resources Find Volcanoes Frequently Asked Questions Contact Us


Introduction
Volcanic Gases: Average Compositions and Minor or Trace Gases
Gas Compositions and Tectonic Setting
Gases: Man versus the Volcanoes
Volcanic Gases and the Origin of the Atmosphere
Global Impacts of Volcanic Eruptions
Some Important Eruptions
Deadly Gases
Dead Dinosaurs and Gas
Measuring Volcanic Gases
Quiz on Volcanic Gases
References on Volcanic Gases
Other Sources of Volcanic Gas Information

Return To:

Education Main






Back To VolcanoWorld Home




Dead Dinosaurs and Gases

The most widely accepted hypothesis for the extinction of the dinosaurs is the impact of an asteroid at Chicxulub, Mexico (Alverez and Asaro, 1990). An alternative hypothesis, that voluminous volcanic eruptions blocked the sun and caused extreme environmental conditions, has also been proposed (Officer and others, 1987; Courtillot, 1990). Photo of the dinosaur quarry at Dinosaur National Monument. Photo courtesy of the National Park Service.

The key to the volcanic hypothesis is the Deccan Traps, a flood basalt province in India. About 65 million years ago, coincident with the extinction of dinosaurs, a least one million cubic km of lava was erupted. Scaling upwards from the Laki eruption, the Deccan Traps eruption might have created 8-17x1012 tonnes of sulfur acid aerosol, about 100 times more than Laki.

Released suddenly, such a great volume of gas would produced dire environmental consequences, including mass extinctions. Critical to this hypothesis is the rate at which the lava was erupted and the gas released. Some evidence suggests the eruptions happened over a long period, perhaps allowing the atmosphere to recover between eruptions. Features within continental flood basalt lava flows (Self and others, 1997) and the presence of soil horizons at the Deccan Traps argue for a gradual emplacement of the lava flows. This could mean the impact of individual eruptions were no greater than that of Laki.

If the flux rate of iridium at Hawaiian volcanoes is representative of continental basaltic systems, the production rate of iridium by volcanoes cannot account for all of the iridium observed at the K/T boundary (Finnegan and others, 1990). This suggests another source of iridium was involved, possibly from an extraterrestrial source.

An even larger eruption of flood basalts (1.5 million cubic km) at the Siberian Traps at the end of the Permian is linked with the greatest mass extinction Earth's history.