Did an
extra-terrestrial impact over the Laurentian Ice Sheet cause
the extinction of North America’s mega-fauna, the disappearance
of Clovis culture and the onset of the Younger Dryas Cooling
?
Gilbert
N. Hanson
Department of Geosciences
Stony Brook University
Sunday,
May 18, 2008 at 2:00 P.M.
Room 319
American Museum of Natural History New York City
A
team of 26 scientists has proposed that 12,900 years ago a
comet broke up and exploded over the Laurentian Ice Sheet
with the force of millions of atomic bombs (Firestone et al,
2007). This impact event would have caused the extinction
of the North American mega-fauna which included animals such
as mammoths and saber tooth tigers; the disappearance of the
Clovis culture and the onset of a severe cooling of the North
Atlantic area known as the Younger Dryas.
The
extinctions of the mega-fauna would have been a result of
the impacts’ shock wave, then massive wildfires followed
by a dramatic reduction of food associated with climate change.
Evidence
for the impact includes a black algal mat that overlies the
latest Clovis sites throughout North America. The mat contains
charcoal, tiny spheres of carbon and metals, nanodiamonds,
and extraterrestrial concentrations of helium-3 and the element
iridium.
At
the time of the impact the climate had become warmer than
it had been for a few thousands of years after the Last Glacial
Maximum. The impact caused massive melting of the Laurentian
Ice sheet which produced fresh water which entered the North
Atlantic Ocean and stopped the thermohaline circulation. This
led to a ca 1000 year cold period when temperatures approached
those during the Last Glacial Maximum. This cooling period
is known as the Younger Dryas. After the Younger Dryas the
warm Holocene Epoch, that we are presently in, began.
In
this presentation we will consider the climatic and glacial
setting, the timing of the events and the evidence for an
extra terrestrial impact.
Reference
Cited Above:
R. B. Firestone, et al, 2008, Evidence for an extraterrestrial
impact 12,900 years ago that contributed to the megafaunal
extinctions and the Younger Dryas cooling, Proceedings of
the National Academy of Sciences, 104, 16016-16021.
N.Y.P.S. MEETING DATES FOR THE YEAR
These
are the meeting dates of the New York Paleontological Society
for the 2007-2008 season. We meet at 2:00 P.M. in room 319
at the American Museum of Natural History in New York City
(79th Street and Central Park West).