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Science & Technology

Did an Asteroid Cancel Dinosaurs? The Truth is in the Lava

February 26, 2019

Layered lava flows from the Bushe and Poladpur Formations near the village of Tail Baila. Image credit, Courtney Sprain.

Layered lava flows from the Bushe and Poladpur Formations near the village of Tail Baila. Image credit, Courtney Sprain.


About sixty-six million years ago a planet-wide catastrophe brought the non-avian dinosaurs to their demise, and the end of the Cretaceous period was marked by a mass extinction of its fauna and flora. New data, published in the journal Science, says it’s possible that intense volcanic eruptions in India coincided with the worldwide extinction – ultimately cementing the fate of the massive reptiles.   

Location map outlining exposed area of the Deccan Traps in modern day India. Image credit, Courtney Sprain.

“Our previous research presented the hypothesis that a large asteroid impact off the coast of Yucatan could have shaken the Earth globally, which could have disrupted the magmatic systems of volcanoes across the world, causing this transition,” said Loÿc Vanderkluysen, PhD, volcanologist and professor of geoscience in the College of Arts and Sciences at Drexel. However, this hypothesis remained very much untested and controversial, until now.

Vanderkluysen points at a red bole that marks the Bushe-Poladpur contact/Cretaceous-Paleogene boundary near the town of Poladpur in the Western Ghats. Image credit, Courtney Sprain.
Vanderkluysen points at a red bole that marks the Bushe-Poladpur contact/Cretaceous-Paleogene boundary near the town of Poladpur in the Western Ghats. Image credit, Courtney Sprain.

 

 

Vanderkluysen was among the group of researchers, primarily from the University of California, Berkeley, that dated the vast lava flows known as the Deccan Traps in India using radiation measurements. The team was able to date massive lava flows with far greater precision, whittling it down from around a million years to a period of tens of thousands of years. 

"We are able to recreate with great precision the order of events at the end of the Cretaceous period," said Vanderkluysen.

“Now that we have dated Deccan Traps lava flows in more and different locations, we see that the transition seems to be the same everywhere. I would say, with pretty high confidence, that the eruptions occurred within 50,000 years, and maybe 30,000 years, of the impact, which means they were synchronous within the margin of error,” said Paul Renne, a professor-in-residence of earth and planetary science at UC Berkeley, director of the Berkeley Geochronology Center and senior author of the study.

Lead author Courtney Sprain standing in front of an inflated sheet lobe in the Jawhar Formation, in a quarry north of Mumbai. Image credit, Loÿc Vanderkluysen.
Lead author Courtney Sprain standing in front of an inflated sheet lobe in the Jawhar Formation, in a quarry north of Mumbai. Image credit, Loÿc Vanderkluysen.

The new dates confirm earlier estimates that the lava flows continued for about a million years, but the data shows that three-quarters of the lava erupted after the impact. Previous studies suggested that about 80 percent of the lava erupted before the impact.

The close correlation of the two events, eruptions and extinction – don’t seem to be a coincidence, according to the researchers. “This bolsters the theory that the impact of the asteroid was the main cause,” said Vanderkluysen. “It’s like shaking a bottle of champagne, it can accelerate volcanic activity.”

Prof. Paul Renne inspects profile of a red bole within the Ambenali Formation near the town of Mahabaleshwar. Image credit, Loÿc Vanderkluysen.
Prof. Paul Renne inspects profile of a red bole within the Ambenali Formation near the town of Mahabaleshwar. Image credit, Loÿc Vanderkluysen.

This study also gleaned improved insights into the period’s climate record. The global climate warming in the years preceding the meteorite can’t be tied to an asteroid. Its likely, that volcanism is what caused this warming – and data from the study shows the climate hadn’t reached its peak intensity. Shell fragments and marine fossils prior to the extinction showed evidence of decline and stress prior to the impact of the meteorite.

“The ecosystem was primed to suffer a mass extinction and volcanism attributed to its weakened state and thwarted recovery,” said Vanderkluysen.


Media Contact:

Emily Storz

els332@drexel.edu

215.895.2705