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Gone With the Wind
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- Subject: Gone With the Wind
- From: "Louis Varricchio" <varricch@aero.und.edu>
- Date: Mon, 22 Nov 1999 15:16:56 -0600
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News - November 19, 1999
NSF PR 99-69
Media contacts:
Cheryl Dybas (NSF)
(703) 306-1070
cdybas@nsf.gov
Sandra Lanman, Rutgers
University
(732) 932-7084, ext. 621
slanman@ur.rutgers.edu
Program contact:
J. Paul Dauphin
(703) 306-1581
jdauphin@nsf.gov
Geologists Pinpoint Source of Major Global Warming Event More
Than 55 Million Years Ago
For the first time, a team of scientists has identified the possible
methane release site and critical
sequence of events that precipitated Earth's bout with global warming, and
the extinction of many
deep-sea species and appearance of new mammalian orders, more than 55
million years ago.
The research project is part of the international Ocean Drilling Program,
which is funded by the National Science Foundation (NSF) and a consortium of
international partners.
In an article to be published this week in the journal Science, geologists
Miriam Katz and
Kenneth Miller of Rutgers University in New Brunswick, New Jersey, provide
support for a link
between the mass extinction millions of years ago and the massive release
of methane and carbon
dioxide into the earth's oceans and atmosphere, which is not unlike the
present input of fossil fuels
into the environment. "We haven't studied these major carbon influxes
before because we didn't
know about them," says NSF's Paul Dauphin, associate program director for
ODP.
In what is known as the latest Paleocene thermal maximum (LPTM), Earth's
climate and oceans
warmed significantly about 55.5 million years ago. Numerous mammalian
orders appeared while
many deep-sea species became extinct as water temperatures soared by 4 to
8 degrees Celsius.
Since the 1980s, scientists have tried to explain the rapid climate
warming apparent in
geochemical records from around the world.
"One approach to unraveling the possibilities of future climate change is
to study analogs from the
Earth's past," says Katz. "We have examined clues in the geologic record
of an ancient massive
release of carbon into the Earth's oceans and atmosphere." The clues came
from analyzing certain
geochemical and faunal changes in a group of microfossils known as
foraminifera - essentially
amoebas with shells - in order to reconstruct ancient oceanographic and
climatic conditions.
Working as part of an international scientific team onboard the Ocean
Drilling Program's vessel
the JOIDES (Joint Oceanographic Institutions for Deep-Earth Sampling)
Resolution, the
researchers recovered ocean sediments from the Blake Nose, 400 kilometers
(250 miles) east of
Tallahassee, Florida. Katz and her co-authors have pinpointed this region
as the first location to
be identified as a possible LPTM methane release site, where methane
appears to have escaped
from a pressure zone created by an underlying ancient reef.
Katz says "the triggering mechanism for methane release is still open to
debate," making it
impossible for scientists to predict whether a massive release from
today's 14,000 gigaton marine
gas hydrate reservoir could occur again.
"We know that 55.5 million years ago, carbon dioxide was added to the
atmosphere at a rate
comparable to present-day fossil fuel input, providing the potential for
using past changes in
carbon dioxide levels to shed light on future climate change
possibilities," Katz believes.
-NSF-
LOUIS VARRICCHIO
Environmental Information Specialist &
Producer/Writer, "Our Changing Planet"
(Visit OCP-TV on the Web at: www.umac.org/ocp)
Upper Midwest Aerospace Consortium
Odegard School of Aerospace Sciences
University of North Dakota
Grand Forks, N.D. 58202-9007 U.S.A.
Phone: 701-777-2482
Fax: 701-777-2940
E-mail: varricch@umac.org (in N.D.); morbius@together.net (in Vt.)
"Behind every man alive stand thirty ghosts, for that is the ratio by
which the dead outnumber the living. Since the dawn of time, a hundred
billion human beings have walked the planet Earth." -- Arthur C. Clarke
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