The demise of the dinosaurs is the world's ultimate whodunit. Was it a
comet or asteroid impact? Volcanic eruptions? Climate change?
Team leader Paul Renne in Montana collecting a volcanic ash sample
from a coal bed within a few centimeters of the dinosaur extinction
horizon. Photo by Courtney Sprain.
In an attempt to resolve the issue, scientists at the Berkeley
Geochronology Center (BGC), the University of California, Berkeley, and
universities in the Netherlands and the United Kingdom have now
determined the most precise dates yet for the dinosaur extinction 66
million years ago and for the well-known impact that occurred around the
same time.
The dates are so close, the researchers say, that they now believe
the comet or asteroid, if not wholly responsible for the global
extinction, at least dealt the dinosaurs their death blow.
"The impact was clearly the final straw that pushed Earth past the
tipping point," said Paul Renne, BGC director and UC Berkeley professor
in residence of earth and planetary science. "We have shown that these
events are synchronous to within a gnat's eyebrow, and therefore the
impact clearly played a major role in extinctions, but it probably
wasn't just the impact."
The revised dates clear up lingering confusion over whether the
impact actually occurred before or after the extinction, which was
characterized by the almost overnight disappearance from the fossil
record of land-based dinosaurs and many ocean creatures. The new date
for the impact -- 66,038,000 years ago -- is the same within error
limits as the date of the extinction, said Renne, making the events
simultaneous.
He and his colleagues will report their findings in the Feb. 8 issue of the journal Science.
The crater of doom
The extinction of the dinosaurs was first linked to a comet or
asteroid impact in 1980 by the late UC Berkeley Nobel Laureate Luis
Alvarez and his son, Walter, who is a UC Berkeley professor emeritus of
earth and planetary science. A 110-mile-wide crater in the Caribbean off
the Yucatan coast of Mexico is thought to be the result of that impact.
Called Chicxulub (cheek'-she-loob), the crater is thought to have been
excavated by an object six miles across that threw into the atmosphere
debris still be found around the globe as glassy spheres or tektites,
shocked quartz and a layer of iridium-enriched dust.
A comet or asteroid impact 66 million years ago excavated a 110
mile-diameter crater, dubbed Chicxulub, centered off the coast of
Mexico's Yucatan peninsula. Courtesy of Wikipedia.
Renne's quest for a more accurate dating of the extinction began
three years ago when he noticed that the existing date conflicted with
other estimates of the timing of the extinction and that the existing
dates for the impact and the extinction did not line up within error
margins.
Renne and his BGC colleagues first went to work recalibrating and
improving the existing dating method, known as the argon-argon
technique. They then collected volcanic ash from the Hell Creek area in
Montana and analyzed them with the recalibrated argon-argon technique to
determine the date of the extinction. The formation below the
extinction horizon is the source of many dinosaur fossils and one of the
best sites to study the change in fossils from before and after the
extinction.
They also gathered previously dated tektites from Haiti and analyzed
them using the same technique to determine how long ago the impact had
occurred. The new extinction and impact dates are precise to within
11,000 years, the researchers said.
"When I got started in the field, the error bars on these events were
plus or minus a million years," said paleontologist William Clemens, a
UC Berkeley professor emeritus of integrative biology who has led
research in the Hell Creek area for more than 30 years, but was not
directly involved in the study. "It's an exciting time right now, a lot
of which we can attribute to the work that Paul and his colleagues are
doing in refining the precision of the time scale with which we work.
This allows us to integrate what we see from the fossil record with data
on climate change and changes in flora and fauna that we see around us
today."
Dinosaurs at the tipping point
Despite the synchronous impact and extinction, Renne cautions that
this doesn't mean that the impact was the sole cause. Dramatic climate
variation over the previous million years, including long cold snaps
amidst a general Cretaceous hothouse environment, probably brought many
creatures to the brink of extinction, and the impact kicked them over
the edge.
"These precursory phenomena made the global ecosystem much more
sensitive to even relatively small triggers, so that what otherwise
might have been a fairly minor effect shifted the ecosystem into a new
state," he said. "The impact was the coup de grace."
One cause of the climate variability could have been a sustained
series of volcanic eruptions in India that produced the extensive Deccan
Traps. Renne plans to re-date those volcanic rocks to get a more
precise measure of their duration and onset relative to the dinosaur
extinction.
xtinction level where impact debris is found. Photo by Paul Renne.
"This study shows the power of high precision geochronology," said
coauthor Darren F. Mark of the Scottish Universities Environmental
Research Center, who conducted independent argon-argon analyses on
samples provided by Renne. "Many people think precision is just about
adding another decimal place to a number. But it's far more exciting
than that. It's more like getting a sharper lens on a camera. It allows
us to dissect the geological record at greater resolution and piece
together the sequence of Earth history."
Renne's colleagues, in addition to Mark, are UC Berkeley graduate
student William S. Mitchell III; BGC scientists Alan L. Deino and Roland
Mundil; Leah E. Morgan of the Scottish Universities Environmental
Research Center in Kilbride, Scotland; Frederik J Hilgen of Utrecht
University; and Klaudia F. Kuiper and Jan Smit of Vrije University in
Amsterdam.

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