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Comet
May Have Exploded Over North America 13,000 Years Ago
Tuesday, August 14, 2007
A
"black mat" of algal growth in Arizona marks a
line of extinction at 12,900 years ago; Clovis points and
mammoth skeletons were found at the line but not above it.
Credit:
Allen West, UCSB
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Caused wooly mammoth
extinction, global cooling and end of early human Clovis culture
New scientific findings suggest
that a large comet may have exploded over North America 12,900
years ago, explaining riddles that scientists have wrestled with
for decades, including an abrupt cooling of much of the planet
and the extinction of large mammals.
The discovery was made by
scientists from the University of California at Santa Barbara and
their colleagues. James Kennett, a paleoceanographer at the
university, said that the discovery may explain some of the
highly debated geologic controversies of recent decades.
The period in question is
called the Younger Dryas, an interval of abrupt cooling that
lasted for about 1,000 years and occurred at the beginning of an
inter-glacial warm period. Evidence for the temperature change is
recorded in marine sediments and ice cores.
According to the scientists,
the comet before fragmentation must have been about four
kilometers across, and either exploded in the atmosphere or had
fragments hit the Laurentide ice sheet in the northeastern North
America.
Wildfires across the continent
would have resulted from the fiery impact, killing off vegetation
that was the food supply of many of larger mammals like the
woolly mammoths, causing them to go extinct.
Since the Clovis people of
North America hunted the mammoths as a major source of their
food, they too would have been affected by the impact. Their
culture eventually died out.
The scientific team visited
more than a dozen archaeological sites in North America, where
they found high concentrations of iridium, an element that is
rare on Earth, and is almost exclusively associated with
extraterrestrial objects such as comets and meteorites.
They also found metallic
microspherules in the comet fragments; these microspherules
contained nano-diamonds. The comet also carried carbon molecules
called fullerenes (buckyballs), with gases trapped inside that
indicated an extraterrestrial origin.
The team concluded that the
impact of the comet likely destabilized a large portion of the
Laurentide ice sheet, causing a high volume of freshwater to flow
into the north Atlantic and Arctic Oceans.
"This, in turn, would have
caused a major disruption of the ocean's circulation, leading to
a cooler atmosphere and the glaciation of the Younger Dryas
period," said Kennett. "We found evidence of the impact
as far west as the Santa Barbara Channel Islands."
NSF's Paleoclimate Program
funded the research.
Source:
NSF

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