Dwayne Brown
Headquarters, Washington
202-358-1726
dwayne.c.brown@nasa.gov
Natasha Metzler
Carnegie Institution of Washington
202-939-1142
nmetzler@carnegiescience.edu
WASHINGTON -- NASA-funded research on
Mars meteorites that landed on Earth shows strong evidence that very large
molecules containing carbon, which is a key ingredient for the building blocks
of life, can originate on the Red Planet. These macromolecules are not of
biological origin, but they are indicators that complex carbon chemistry has
taken place on Mars.
Researchers from the Carnegie
Institution for Science in Washington who found reduced carbon molecules now
have better insight into the chemical processes taking place on Mars. Reduced
carbon is carbon that is bonded to hydrogen or itself. Their findings also may
assist in future quests for evidence of life on the Red Planet. The findings
are published in Thursday's online edition of Science Express.
"These findings show that the
storage of reduced carbon molecules on Mars occurred throughout the planet's
history and might have been similar to processes that occurred on the ancient
Earth," said Andrew Steele, lead author of the paper and researcher from
Carnegie. "Understanding the genesis of these non-biological,
carbon-containing macromolecules on Mars is crucial for developing future
missions to detect evidence of life on our neighboring planet."
Finding molecules containing large
chains of carbon and hydrogen has been one objective of past and present Mars
missions. Such molecules have been found previously in Mars meteorites, but
scientists have disagreed about how the carbon in them was formed and whether
it came from Mars. This new information proves Mars can produce organic carbon.
"Although this study has not
yielded evidence that Mars has or once may have supported life, it does address
some important questions about the sources of organic carbon on Mars,"
said Mary Voytek, director of NASA's Astrobiology Program at the agency's
Headquarters in Washington. "With the Curiosity rover scheduled to land in
August, these new research results may help Mars Science Laboratory scientists
fine-tune their investigations on the surface of the planet by understanding
where organic carbon may be found and how it is preserved."
Scientists have theorized that the large
carbon macromolecules detected on Martian meteorites could have originated from
terrestrial contamination from Earth or other meteorites, or chemical reactions
or biological activity on Mars.
Steele's team examined samples from 11
Martian meteorites from a period spanning about 4.2 billion years of Martian
history. They detected large carbon compounds in 10 of them. The molecules were
found inside grains of crystallized minerals.
Using an array of sophisticated research
techniques, the team was able to show that at least some of the macromolecules
of carbon were indigenous to the meteorites themselves and not contamination
from Earth.
The team next looked at the carbon
molecules in relation to other minerals in the meteorites to see what kinds of
chemical processing these samples endured before arriving on Earth. The
crystalline grains encasing the carbon compounds provided a window into how the
carbon molecules were created. Their findings indicate that the carbon was
created by volcanic activity on Mars and show that Mars has been doing organic
chemistry for most of its history.
In a separate paper published by
American Mineralogist, Steele and his team report their findings on the same
meteorite announced in 1996 to contain possible -- but subsequently discounted
-- relics of ancient biological life on Mars. Called ALH84001, the meteorite
was found to also contain organic macromolecules of non-biological origin.
The Steele team's research indicates
that Mars does have a pool of reduced carbon. Their findings should help
scientists involved in current and future Mars missions distinguish
non-biologically formed carbon molecules from potential life.
For an image and more information about
the meteorite, visit http://1.usa.gov/mars052412.
- end -
No comments:
Post a Comment