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Martian 'bacteria' matched to Earth

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Martian 'bacteria' matched to Earth
By BBC News Online Science Editor Dr David Whitehouse

Claims that the unusual features found on a Martian meteorite are those of
fossilised alien bacteria may be proved correct by new research.

When Nasa researchers first made their claims about Martian microfossils in
1996 they were greeted with scepticism by those who believed the shapes were
too small to have come from any bacteria-like organisms.

But in a new study, scientists have shown that the tiny fossilised structures
can be produced after microbes have died. The experiments have shown that
certain parts of Earth bacteria can also leave similar remains when they are
fossilised.

"We believe we have clearly shown that features similar in size and shape to
those in the Martian meteorite do exist within the biological record on
Earth," said Kathie Thomas-Keprta of Lockheed Martin Space Mission Systems and
Services in Houston, Texas.

But she warned that this does not prove definitively that the meteorite
features are fossilised organisms.

Fossilised filaments

The Earth bacteria, taken from rocks in Washington state, were bred in
conditions that simulated the environment deep beneath the Earth's surface.
When they died, they became fossilised in only eight weeks.


<Picture: [ image: width=150]>

Scientists saw that about 30% of the microbes grown in the laboratory had
filaments attached.

Crucially, filaments that were not attached to the organisms also became
fossilised. Researchers say it is the first time such tiny parts of bacteria
have been shown to become mineralised in the same way as whole microbe.

It suggests the structures on the Martian rock may also be the fossilised
remains of filaments.

Original findings

The longest shapes identified on the meteorite are approximately 1/25 the
diameter of a human hair. Dr Everett Gibson, a Nasa planetary scientist who
worked on the meteorite, says the new study supports the original findings.


<Picture: [ image: width=150]>

ALH84001, the potato-sized Martian meteorite is about 4.5 billion years, the
period when Mars formed. It is believed to have originated beneath the Martian
surface.

It is believed that billions of years ago Mars was warmer and wetter. The
water is believed to have penetrated fractures in the surface rock, forming an
underground water system. This system may have been the best location for life
during much of Mars's history.

The Earth bacteria used in this new experiment came from the Columbia River
basalt of Washington State. They are an example of life thriving at depth in
fractured rock where it is isolated from light and protected from any harsh
environment at the surface.

So it may be a good example of what life was like on Mars.

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