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New Images Show Additional Evidence Of Possible Ancient Life On Mars
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- Subject: New Images Show Additional Evidence Of Possible Ancient Life On Mars
- From: Ron Baalke <BAALKE@kelvin.jpl.nasa.gov>
- Date: Fri, 19 Mar 1999 20:31:34 GMT
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Life On Mars?
http://www.jsc.nasa.gov/pao/flash/marslife/photos.htm
A NASA research team of scientists at the Johnson Space
Center and at Stanford University has found evidence
that strongly suggests primitive life may have existed
on Mars more than 3.6 billion years ago.
The NASA-funded team found the first organic molecules
[Image] thought to be of Martian origin; several mineral
features characteristic of biological activity; and
possible microscopic fossils of primitive, bacteria-like
organisms inside of an ancient Martian rock that fell to
Earth as a meteorite.
New images show additional evidence of possible ancient
life on Mars from another, younger meteorite.
[Image] 1075 (Low-re JPG; Hire JPG TIF ) - These are
possible Martian fossilized microbial cells
attached to a mineral in the Egyptian meteorite Nakhla.
They range from about 1 to 2 micrometers in size and
each one is firmly attached to the crystal by clay
minerals which are know to commonly form on cells as
part of the mineralization or fossilization process. The
scale bar is 5 micrometers or abut 1/10 the thickness of
a human hair.
[Image] 2058 (Low-re JPG; TIF ) - This shows two
possible fossilized Martian cells and the
fragments of others. The cell in the center has the
remains of a fossilized biofilm partly covering its
surface. The cell to the right his partly embedded in
the clay mineral which fills veins or cracks in the
meteorite (NAKHLA). This clay mineral is now known to
have formed on Mars about 700 million years ago. If
these bumps are truly fossilized martian microbes, they
are then about 700 million years old.
[Image] 2060 (Low-re JPG; Hi-re JPG TIF ) - This shows
a possible elongated fossilized Martian cell on
the surface of a clay mineral which fills veins or
cracks in the meteorite (NAKHLA). Other possible
fossilized microbes are partly embedded in the clay
mineral. This clay mineral is now known to have formed
on Mars about 700 million years ago. If these embedded
bumps are truly fossilized Martian microbes, they are
then about 700 million years old. The elongated bump on
the surface may have formed later or it may be the same
age as the embedded bumps.
[Image] 2154e (Low-re JPG; Hire JPG TIF ) - This image
shows a series of partly embedded bumps in clay
minerals in the Nakhla meteorite. Our interpretation is
that these bumps are individual fossilized Martian
microbes. That interpretation must be checked by further
data on chemistry and structure of the bumps. Note the
three bumps lined up near the center. These bumps bear a
striking resemblance to earth microbes which are in the
process of reproduction. If the bumps are truly Martian
microbes, they are about 700 million years old, the age
of the surrounding clay minerals as dated by radioactive
isotope techniques.
[Image] 2165e (Low-re JPG; Hire JPG TIF ) - This image
shows a series of bumps partly embedded in a
tiny slab of Martian clay (Nakhla) . The slab is wrapped
and partially covered by another layer of Martian clay
free of bumps. We interpret that the bumps are
fossilized Martian microbes trapped the clay layers
about 700 million years ago on Mars. Our interpretation
must be checked by further detailed data to determine if
they are really fossilized microbes and to confirm that
they clay mineral formed on Mars, but the existing data
supports both of those theories.
[Image] 4181e (Low-re JPG; Hire JPG TIF ) - This image
shows a fossilized elongated microbe resting in
a hollow in clay minerals from the meteorite NAKHLA. The
microbe appears to be somewhat corroded and partly
covered with the remains of biofilm (slime generated by
living cells). It closely resembles many kinds of earth
bacteria.
Below are photographs of the evidence for the 1996
discovery announcement.
[Image] S96-12301 (Low-re JPG; Hire JPG TIF ) - In the
center of this electron microscope image of a
small chip from a meteorite are several tiny structures
that are possible microscopic fossils of primitive,
bacteria-like organisms that may have lived on Mars more
than 3.6 billion years ago. A two-year investigation by
a NASA research team found organic molecules, mineral
features characteristic of biological activity and
possible microscopic fossils such as these inside of an
ancient Martian rock that fell to Earth as a meteorite.
The largest possible fossils are less than 1/100th the
diameter of a human hair in size while most are ten
times smaller.
[Image] S96-12299 (Low-res JPG; Hi-res JPG; TIF ) -
This electron microscope image is a close-up of
the center part of photo number S96-12301. While the
exact nature of these tube-like structures is not known,
one interpretation is that they may be microscopic
fossils of primitive, bacteria-like organisms that may
have lived on Mars more than 3.6 billion years ago. A
two-year investigation by a NASA research team found
organic molecules, mineral features characteristic of
biological activity and possible microscopic fossils
such as these inside of an ancient Martian rock that
fell to Earth as a meteorite. The largest possible
fossils are less than 1/100th the diameter of a human
hair in size while most are ten times smaller.
[Image] S96-12298 (Low-res JPG; Hires JPG; TIF ) - This
electron microscope image shows extremely tiny
tubular structures that are possible microscopic fossils
of bacteria-like organisms that may have lived on Mars
more than 3.6 billion years ago. A two-year
investigation by a NASA research team found organic
molecules, mineral features characteristic of biological
activity and possible microscopic fossils such as these
inside of an ancient Martian rock that fell to Earth as
a meteorite. The largest possible fossils are less than
1/100th the diameter of a human hair in size while most
are ten times smaller. The fossil-like structures were
found in carbonate minerals formed along pre-existing
fractures in the meteorite in a fashion similar to the
way fossils occur in limestone on Earth, although on a
microscopic scale.
[Image] S96-12297 (Low -res JPG; Hi -res JPG;TIF ) -
This electron microscope image shows egg-shaped
structures, some of which may be possible microscopic
fossils of Martian origin as discussed by NASA research
published in the Aug. 16, 1996, issue of the journal
Science. A two-year investigation found organic
molecules, mineral features characteristic of biological
activity and possible microscopic fossils such as these
inside of an ancient Martian rock that fell to Earth as
a meteorite. The largest possible fossils are less than
1/100th the diameter of a human hair in size while most
are ten times smaller.
[Image] S96-12300 (Low-res JPG; Hires JPG; TIF ) - This
electron microscope image shows tubular
structures of likely Martian origin. These structures
are very similar in size and shape to extremely tiny
microfossils found in some Earth rocks. This photograph
is part of a report by a NASA research team published in
the Aug. 16, 1996, issue of the journal Science. A
two-year investigation by the team found organic
molecules, mineral features characteristic of biological
activity and possible microscopic fossils such as these
inside of an ancient Martian rock that fell to Earth as
a meteorite. The largest possible fossils are less than
1/100th the diameter of a human hair in size while most
are ten times smaller.
[Image] S96-12609 (Low-res JPG; Hires JPG; TIF) &
S96-12610 (JPG; TIF) - This high-resolution
scanning electron microscope image shows an unusual
tube-like structural form that is less than 1/100th the
width of a human hair in size found in meteorite
ALH84001, a meteorite believed to be of Martian origin.
Although this structure is not part of the research
published in the Aug. 16 issue of the journal Science,
it is located in a similar carbonate glob in the
meteorite. This structure will be the subject of future
investigations that could confirm whether or not it is
fossil evidence of primitive life on Mars 3.6 billion
years ago.
[Image] S94-032549 (Low-res JPG; Hires JPG; TIF ) -
This 4.5 billion-year-old rock, labeled
meteorite ALH84001, is believed to have once been a part
of Mars and to contain fossil evidence that primitive
life may have existed on Mars more than 3.6 billion
years ago. The rock is a portion of a meteorite that was
dislodged from Mars by a huge impact about 16 million
years ago and that fell to Earth in Antarctica 13,000
years ago. The meteorite was found in Allan Hills ice
field, Antarctica, by an annual expedition of the
National Science Foundation's Antarctic Meteorite
Program in 1984. It is preserved for study at the
Johnson Space Center's Meteorite Processing Laboratory
in Houston.
[Image] S95-00690 (JPG; TIF ) - This photograph shows
orange-colored carbonate mineral globules found
in a meteorite, called ALH84001, believed to have once
been a part of Mars. These carbonate minerals in the
meteorite are believed to have been formed on Mars more
than 3.6 billion years ago. Their structure and
chemistry suggest that they may have been formed with
the assistance of primitive, bacteria-like living
organisms. A two-year investigation by a NASA research
team found organic molecules, mineral features
characteristic of biological activity and possible
microscopic fossils inside of carbonate minerals such as
these in the meteorite.
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