Stories tagged Deccan Traps

Apr
30
2009

Killer asteroid?: Artist conception of impact event
Killer asteroid?: Artist conception of impact eventCourtesy NASA
The old “What really killed the dinosaurs” controversy is back in the news. And once again, it’s Princeton geophysicist Gerta Keller stirring up the pot.

Death from above?: Perhaps not.
Death from above?: Perhaps not.Courtesy Mark Ryan
Keller and her colleague Thierry Adatte of the University of Lausanne in Switzerland have published yet another paper challenging the prevailing theory that an asteroid was the major cause of the extinction of the dinosaurs at the end of the Cretaceous Period 65 million years ago. The extinction affected over 60 percent of animal species including all of the non-avian dinosaurs.

Actually a number of events were occurring around the end of the Cretaceous including long-term volcanic activity, rapid marine regression, and the infamous asteroid impact. There’s also evidence that some of the dinosaur population was already in decline 10 million years prior to the events. But the scenario is usually played out with the meteor coming late in the sequence and delivering the deathblow to an already weakened eco-system, and paving the way for mammals to take over the ecological gap.

K-T boundary layer: The Cretaceous-Tertiary boundary layer located near Trinidad, Colorado. The pale-gray 1-inch iridium layer (arrow) is sandwiched between coal layers and contains shocked quartz and other evidence of a large asteroid impact. The scale bar is 6 inches in length.
K-T boundary layer: The Cretaceous-Tertiary boundary layer located near Trinidad, Colorado. The pale-gray 1-inch iridium layer (arrow) is sandwiched between coal layers and contains shocked quartz and other evidence of a large asteroid impact. The scale bar is 6 inches in length.Courtesy Mark Ryan
The asteroid impact hypothesis was first proposed in 1980 by Luis Alvarez of the University of California after he and his son Walter discovered a claystone layer rich in the rare-earth element iridium and peppered with shocked quartz in many locations around the world. Iridium is a rare element not commonly found on the Earth’s surface but abundant in meteorites. Shocked quartz was first noticed in sand grains in craters created by nuclear test bombs and later in meteor impact sites. Alvarez hypothesized that the only other possible source for this naturally deposited strata would be from a large extraterrestrial object hitting the Earth. From studying the amount of iridium found in Cretaceous-Tertiary (K-T) boundary formations, he calculated that a bolide about 6 miles across would have been necessary to create that much iridium around the world. But at the time evidence of such an was unknown. It wasn’t until after Luis Alvarez’s death in 1988 that a crater on the Yucatan Peninsula near Chicxulub Mexico became the chief suspect. The Chicxulub impact crater was the right size and the right age fitting all the criteria of a Cretaceous extinction event.

But Keller claims the asteroid came too early to put the coup de grace on dinosaurs or any species for that matter. Her study of spherules in strata at localities in Mexico has convinced her that the asteroid collided with Earth 300,000 years before any mass extinction.

At El Penon, a location very near the impact crater site, Keller and Adatte studied a 30-ft layer of sandstone above the iridium layer that they calculated had been laid down at a rate of about 1-inch per thousand years. This means it took 300,000 years to pile up the entire section of sediment.

Fossils were analyzed on either side of the iridium layer and the researchers found that of 52 species counted below the iridium layer (meaning before the impact), the same 52 species were found above it, meaning the asteroid hadn’t caused any extinction. But at the top of the 30 feet of sandstone overlaying the iridium claystone things were different.

"The mass extinction level can be seen above this interval," Keller says. "Not a single species went extinct as a result of the Chicxulub impact."

The more likely culprit, according to Keller, is India’s Deccan Traps flood basalts which for several million years poured out tremendous amounts of lava and noxious fumes into the atmosphere that would have had put long and tremendous stress on the existing ecosystem. Keller seems to roll out a paper on the subject every year or so in the last decade. We covered some of her Deccan Traps research 2007 which you can read here.

Whatever the case we do know is that non-avian dinosaurs left the planet after the Cretaceous, as none of their fossils have been found above the K-T Boundary. Well, even that doesn’t appear to be the case anymore. Recent dinosaur fossils found in the San Juan Basin in northwestern New Mexico are suspected to come from a stratum that post-dates the Cretaceous extinction. More research needs to be done on the find, but even this wouldn’t be unexpected. Even after the host declares the party’s over, there are always some stragglers who just don’t want to leave.

Keller's paper was published this week in the Journal of the Geological Society.

MORE LINKS
ScienceDaily story
What Killed the Dinosaurs?
Gerta Keller's Chicxulub Debate
Dinosaur Killer May Have Been Volcanism

Dec
19
2007

Extreme volcanism may have put the kibosh on the Mesozoic: Unaware of their impending doom, dinosaur contemporaries frolic in the Late Cretaceous sea.
Extreme volcanism may have put the kibosh on the Mesozoic: Unaware of their impending doom, dinosaur contemporaries frolic in the Late Cretaceous sea.Courtesy Mark Ryan
The mass-extinction that signaled the end of the Cretaceous period, as well as the Age of Dinosaurs has long been blamed on an Earth-shaking collision with an asteroid that struck 65 million years ago near Chicxulub on Mexico’s Yucatan peninsula. Some scientists however have long argued that extreme episodes of volcanism around the same time played a significant if not major role in the event.

Now, a Princeton University paleontologist claims that evidence in the fossil record adds weight to the latter argument saying the volcanic activity that poured out massive amounts of toxic gases and the expansive flood basalts in India’s Deccan Traps may have been the real villain in the Mesozoic era’s demise.

In a recent presentation at the Geological Society of America, Gerta Keller explained that microfossils known as foraminifera show steep decline nearly half a million years before the Chicxulub asteroid event happened, and just when the Deccan event was beginning.

The volcanoes poured huge amounts of toxic gasses into the atmosphere, and flooded something like 600,000 square miles of south-central India with lava flows. To give you an idea of the magnitude of the outpouring, when Mount St. Helens erupted in 1980, the volcano unleashed a cubic kilometer of volcanic material. And the eruption of Mount Vesuvius that buried the city of Pompeii nineteen hundred years earlier had poured out something like 8 cubic kilometers. But the Deccan event is estimated to have produced 512,000 cubic kilometers!! Yikes!

Just prior to the end of the Cretaceous period, the Deccan eruptions would have released massive plumes of carbon dioxide and sulfur dioxide into the atmosphere – possibly ten times more toxic gases than generated by a meteor impact, according to one volcanologist. At any rate, it set off extreme global warming and acid rain, and significantly weakened the biosphere. When the asteroid arrived a half-million years later, the environment would have been ripe for collapse. Nearly thirty years ago, physicist Luis Alvarez and his geologist son, Walter, discovered the crater at Chicxulub, and claimed that asteroid that created it could be the one responsible for the dinosaurs’ demise. But Keller thinks it may have been a case of being in the wrong place at the wrong time.

"The Chicxulub impact could not have caused the mass extinction," she said, "because this impact predates the mass extinction and apparently didn't cause any extinctions."

Keller studied the sediments directly above and below the Chicxulub impact layer, in Mexico, Texas, and India, expecting to find evidence of a new bloom of plankton to fill the void left by a mass extinction. Instead, she found no significant change in the micro-marine environment.

"We cannot attribute any specific extinctions to this impact,” she said. But where she did find evidence of a new bloom was in strata that had been laid down 300,000 years after Chicxulub and just about the time when the output of the Deccan volcanoes would have been at its greatest.

In India, near the Bay of Bengal, about 1000 kilometers from the Deccan lava fields, Keller discovered two lava “traps” each with four lava layers. The telltale bloom of microfossils was found in nine meters of marine sediment located just above the lower trap, which marks the Deccan event’s climax.
"We've shown convincingly the mass extinction came about 300,000 years after the asteroid impact,” she said.

But what about the famous iridium layer found in the K-T boundary? If the Chicxulub impact didn’t produce it, then where did it come from?

Keller thinks a second asteroid impact – not the Chicxulub one- may have been responsible for laying down the worldwide iridium layer that divides the Cretaceous and Tertiary rock layers. Direct evidence of this later impact (such as a crater) has not yet been found.

But to add fuel to the fire –pun definitely intended- it may be that the iridium source isn’t even extraterrestrial at all. Volcanism could be another possible source of increased iridium in the rock layer. The Deccan eruptions were peaking right at the time of the dinosaurs’ demise and maybe that’s all that was needed to send them on their way into extinction.

At any rate, the case against the dinosaurs’ killer or killers is certainly not closed.

LINKS
Story at ScienceDaily
The Chicxulub debate on Gerta Keller's site
More on the Deccan Traps
More on the Deccan Traps Extinction Theory
The Cretaceous Extinction Event