November 3, 1995
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The bottom of the ocean may hold enough fuel to provide power to the
world for several centuries. But no one will know for certain until scientists
from the NSF Ocean Drilling Program (ODP) figure out a way of getting
so-called gas hydrates up to the surface. Gas hydrates -- gray crystals
formed from a combination of methane gas and water under pressure -- are estimated
to contain twice as much carbon as all the known deposits of oil, gas
and coal. The crystals are stored in the ocean crust under extremely high
pressures.
A team of ODP scientists is drilling four deep holes and seven shallow
ones off the North Carolina coast. When they succeed in getting a sample,
they will have to work quickly; the crystals will decompose within a few
hours. Gas hydrates decompose rapidly in conditions comfortable for humans,
say the scientists. Their "hostile" environment is the main reason geologists
know so little about gas hydrates. Most geologists, in fact, have never
seen a sample. [Cheryl Dybas]
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In a nationwide teleconference to discuss current issues in national
research policy, NSF Director Neal Lane called on the science community
to meet the challenges presented by a limited budget and changing national
rationale for science. He encouraged scientists and engineers to help
increase public understanding of science and to explain how budget reductions
can atrophy the R&D; enterprise in the same way that injury destroys muscle
tissue.
"Once inflicted, the damage cannot easily be reversed," said Lane. "The
original capability is almost never achieved again, often resulting in
a limp for the rest of one's life. We can't afford to have the U.S. limping
into the 21st century."
Lane opened the discussion during a November 1 teleconference organized
by the scientific research society Sigma Xi, during which participants
from nearly 90 universities and other research sites posed questions to
panel members. The conference highlighted the anxieties of a science community
struggling with change and a projected 30 percent cut in non defense R&D.;
Panelists strove for optimism in the face of an uncertain future. "The
Golden Age of Science may be over, but there are new and exciting opportunities," said
Thomas Meyer, a Vice Chancellor at the University of North Carolina-Chapel
Hill. [Mary Hanson]
Copies of Dr. Lane's remarks are available on NSF's www home page at
http://www.nsf.gov/ (under "overview" and "director").
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In a challenge to a major aspect of the theory of plate tectonics,
NSF-supported scientists have discovered the presence of an ancient conduit
deep in the Earth's mantle beneath Brazil.
The conduit appears to have remained geographically fixed with respect
to the overlying continent despite thousands of kilometers of South American
plate motion. This observation runs contrary to a major tenet of plate
tectonic theory -- that the motion of lithospheric plates is essentially
independent of flow in the upper mantle beneath the plates - - and implies
that the upper mantle and the overlying South American continent have
remained coupled since the break-up of the Gondwanaland supercontinent
and opening of the South Atlantic Ocean some 120 million years ago. This
result also implies that large-scale convection in the mantle may be responsible
for the motion of the great continental plates such as South America,
where the driving force for plate motion has not been well understood.
These findings are reported in the November 2nd issue of the journal
Nature by geophysicists John VanDecar and David James of the Carnegie
Institution in Washington, D.C. The data for their analysis were collected
from an array of state-of-the-art portable seismograph systems deployed
across southeastern Brazil. [Cheryl Dybas]
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