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Issue 2, April 2003
Lava Lamp Moon: The Search for Life on Europa May Just Have
Gotten Easier
Selby Cull
Planetary Sciences, Hampshire College
cull@jyi.org
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Lenticulae:
The odd reddish splotches in the center of this image may
be the key to finding life on Europa. The splotches, or lenticulae,
may represent areas of warm water from Europa's underground
ocean. (Click
to view larger image)
Courtesy
of
Galileo
Project, NASA
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The
surface of Jupiter's second moon is one of the most twisted, chaotic, and intriguing
surfaces in the solar system. Delicate, sinuous cracks weave across the whole
of Europa; tilted blocks of ice, miles high, break the surface. Scientists have
found evidence of cryo-volcanoes (volcanoes that erupt ice and slush instead of
lava) and the Galileo spacecraft has collected gravity measurements showing that
a deep ocean of liquid water exists under miles of icy crust. With so many phenomenal
surface features, it is no wonder that astronomers have overlooked the tiny dark
blotches that spot the face of the moon. Yet these blotches may be one of the
most interesting - and useful - aspects of Europa yet discovered.
Freckles blanketing Europa
The
Galileo spacecraft revealed these blotches, termed "lenticulae,"
from the Latin word for "freckles," when it photographed Europa
between 1997 and 2000. Only about 10 kilometers in diameter (a small
distance on a planetary scale), the lenticulae are a dusty red color,
and often bulge from the ice like elaborate igloos.
Until recently, astronomers have been unable to explain the lenticulae
blanketing Europa's surface. But in October 2002, a team of researchers
at the University of Colorado, Boulder, hypothesized that the lenticulae
are upwellings of warm water from Europa's ocean, 13 miles under
the surface. Beneath the dark red "freckles" may be narrow channels
that act as elevators, transporting warmer ocean waters up to the
surface, and colder surface water down under the ice in slow convection
currents.
The lava-lamp idea
"Europa
acts like a planetary lava lamp, carrying material from near
the surface down to the ocean."
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"Europa
acts like a planetary lava lamp, carrying material from near the
surface down to the ocean," said Dr. Robert Pappalardo, leader of
the Colorado team.
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Jagged
and broken surface: In addition to extensive ice ridges, enormous
blocks of ice chaotically break Europa's surface. This image
shows mountains of ice on the small moon. (Click
to view larger image)
Courtesy of Galileo
Project, NASA |
The team's
lava-lamp idea has interesting implications. Since the discovery of
Europa's underground ocean, numerous researchers have proposed countless
theories about ways in which life forms could survive under the ice.
If surface-to-ocean "elevators" exist, they could transport organisms
and nutrients from the ocean to the surface and back again, albeit
slowly. The elevators may provide nutrients to organisms living under
the ice sheet, or they may transport "hibernating" organisms to the
surface, where more sunlight is found.
On
Earth, scientists have long known that organisms living in Arctic
ice go into hibernation for long periods of time until conditions
improve. Similarly, Pappalardo has proposed that organisms living
under the Europa ice sheet may also go into hibernation for lack of
an energy source (such as sunlight). Yet, if such organisms were to
get caught in Europa's lava-lamp action, they could be transported
to the sunlit surface, where they may come out of hibernation and
flourish.
Proposed missions to the frozen moon
Theories
about life on Europa are necessarily speculative, but this has not
stopped researchers from formulating ways to test for life on this
enigmatic moon. Since the discovery of Europa's ocean, astronomers
have proposed several missions that would search for evidence of
life on and beneath the frozen moon's ice. One proposed mission
is a type of space-faring submarine that would land on Europa, then
heat itself until it melted through the ice. Once through to the
ocean below, it would make chemical measurements of the water, and
search for evidence of life. The problem with this lander is that
it would have to burn through the ice crust - 13 miles deep.
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Ice
ridges: Europa's surface is like a giant ball of twine - but
each thread is a ridge of solid ice, kilometers high. This
image shows many intersecting ice ridges. (Click
to view larger image)
Courtesy of Galileo
Project, NASA |
Yet fueled
by the new discovery of Europa's lava-lamp features, the lander's
13-mile crust excursion may be avoided altogether. Under the lenticulae,
the ice would be thin, and a lander would not have to burn far to
hit water. Once through the ice, the lander would be able to ride
the lava-lamp motions down into the ocean, where it would search for
evidence of life and analyze the chemistry and physics of the underground
realm.
Pappalardo and his team have proposed using a lander to search for
evidence of life on top of one of the "freckles." If organism-rich
waters are convected to the surface, then it is possible that organic
compounds or organisms themselves could be found on or near the lenticulae.
"If life exists in Europa's ocean, organisms might be carried on a
slow ride from the bottom to the top of Europa's icy crust," said
Pappalardo. "Sampling the surface composition may provide direct insights
into the nature of the ocean deep below, and could plausibly reveal
dormant organisms if they exist within Europa
One of NASA's top priorities
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"If
life exists in Europa's ocean, organisms might be carried
on a slow ride from the bottom to the top of Europa's icy
crust."
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Recently,
the National Research Council's Space Studies Board labeled the
proposed Europa Geophysical Explorer (EGE) mission one of NASA's
top priorities. Such a craft would orbit Europa, mapping its surface
and using U.S. Navy techniques to determine the varying depths of
the ocean beneath the ice. This explorer would also serve as a scout,
identifying possible landing sites for a future mission.
Ironically, funding for the EGE does not yet exist, and probably
won't for several years. Since the EGE's price tag was quickly rising
to over a billion dollars, NASA cut the last proposed Europa orbiter
in June 2002.
The price of any mission to Jupiter's second moon would be high.
While an orbiter would by far be the cheapest type of mission, it
would have little chance of finding direct evidence of life - one
of the primary reasons NASA is so anxious to go to the moon. Fortunately,
if researchers are able to verify Europa's lava-lamp action, the
costs and complexity of future lander proposals would be significantly
reduced, and a mission to the moon may become a real possibility
in the not too distant future.
Suggested Reading
"CU-Boulder
space team studying water, ice, and potential life on Jupiter's moon,
Europa." 24 October, 2002.
http://www.colorado.edu/NewsServices/NewsReleases/2002/2054.html
Martel, Linda. "Bands on Europa." Planetary Science Research Discoveries.
25 November 2002.
http://www.psrd.hawaii.edu/Nov02/EuropanBands.html
"Eavesdropping on Europa's Ice." 25 October 2002.
http://solarsystem.nasa.gov/whatsnew/pr/021025D.html
"The Frosty Plains of Europa." Science at NASA. 3 December 1998.
http://science.nasa.gov/newhome/headlines/ast03dec98_1.htm
Europa's Geophysical Explorer. 29 November 2002.
http://www.habitablezone.com/space/messages/27207.html
Galileo Home Page. 17 December 2002.
http://www.jpl.nasa.gov/galileo/
Journal of Young
Investigators. 2003. Volume Seven.
Copyright © 2003 by Selby Cull and JYI. All rights reserved.
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