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The
meteorite ALH84001 may be the most important rock in the world.
This ancient fragment of the planet Mars may be the source of
what NASA claims are the fossilized remnants of primitive Martian
life-forms. Analysis of this extraterrestrial visitor has revealed
a remarkable history. Carbon-dated at 4.5 billion years old, the
rock was hurled from the Martian surface and into space by an
enormous asteroid impact 16 million years ago. After drifting
though space, it fell to Earth in Antarctica 13,000 years ago.
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ALH84001
METEORITE |
This
potato-sized gray meteorite launched the controversy over whether
there was once life on Mars. The rock probably originated beneath
the Martian crust when Mars formed some 4.5 billion years ago.
Its name encodes its discovery: ALH stands for Allan Hills, the
Antarctic ice field where it was the first meteorite found 1984
by the National Science Foundation's Antarctic Meteorite Program.
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Aliens
In Rock |
On
August 6,1996, NASA stunned the world. It announced that a research
team at the Johnson Space Center in Houston, Texas, had evidence
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produced photographs of what are claimed to be miniscule fossilized
bacteria from the Red Planet.
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NASA's
astonishing statement came after an intensive two-year-long analysis
of ALH84001a 4.2-pound chunk of glass-like Martian meteorite
that was discovered in Antarctica in 1984. ALH84001 is very different
from the 13 other Mars meteorites discovered up until then. Not
only is it three times older, but cracks and fissures inside the
rock contain tiny, disc-shaped globules of carbonatescompounds
that are deposited from water and which can fossilize and preserve
dead life-forms. The NASA team says that the globules were formed
about 3.6 billion years ago, at a time when water is believed
to have flowed on the surface of Mars. Within these carbonates,
the team found a combination of features that led them to their
startling conclusion that microbes may have once lived and
died in the rock.
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The
most striking of these features are tiny fossilized structures
called microfossils. At just one-thousandth the thickness of a
human hair, they are as small as any microfossils ever found on
Earth. Some of these so-called nanobacteria are worm-shaped, others
are egg-shaped. One type of microfossil appears to be segmented,
as if it were a filament composed of many separate cells.
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Telltale
Traces |
Other
telltale deposits found in ALH84001 include organic compounds
called PAHs (polycyclic aromatic hydrocarbons) and mineral deposits
of iron oxides and iron sulphides. On Earth, these are often the
only traces left behind by decomposed microorganisms.
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But
some scientists say that the evidence can be explained in other
ways. They point out that NASA used scanning electron microscopes,
which do not reveal either organic matter or structures such as
cell walls two signatures of life crucial to identifying
microfossils. They also argue that the PAHs could have entered
the rock while on Earth and that these carbon compounds are of
terrestrial origin. But PAHs are most plentiful deep within the
rock, contrary to what might be expected if the meteorite had
been contaminated on Earth. Others skeptics argue that the fossil
structures are too small to contain all the genetic material needed
for life. In any case, they may not be microfossils at alljust
odd-shaped crystals.
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Recently,
some members of the NASA team turned their attention to another
source of Martian rocka meteorite that struck the village
of Nakhia, Egypt, in 1911. An electron microscope revealed what
they claim is more microfossil evidence. One particular filament,
they say, is reminiscent of the thread-like trails left behind
by some bacteria on Earth. Unlike ALH84001, which lay on Earth
for 13,000 years before its discovery, this Nakhia fragment was
collected right after the impact, so contamination by terrestrial
bacteria is doubtful. I The controversy over whether the meteorites
contain Martian microfossils will not be easy to resolve. But
it may be settled after 2008, when NASA will send an unmanned
mission to Mars with a probe that will bring back fresh rocks.
Until then, the jury is out.
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TUCKED
AWAY |
After
its discovery, Martian meteorite ALH84001 languished in a storage
cabinet at NASA's Johnson Space Center for eight years. |



KEY
CHEMISTRY |
Of
the 20,000 meteorites found on Earth, only 14 match the unique
Martian chemistry sampled by the Viking probe, which landed
on Mars in 1976. |

ANCIENT
STONE |
At
4.5 billion years, ALH 84001 is one of the oldest rocks ever
studied. It probably came from one of Mars' oldest areas
the heavily cratered southern hemisphere. |
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