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MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109. TELEPHONE (818) 354-5011
http://www.jpl.nasa.gov
Contact: Diane Ainsworth, JPL Media Relations (818) 354-0850
Mimi Drummond, Monterey Bay Aquarium Media Relations
(831) 648-4918
FOR IMMEDIATE RELEASE
July 26, 1999
NEW JPL DEEP SEA PROBE TO BE TESTED IN MONTEREY AQUARIUM KELP
FOREST
A new aluminum deep sea probe, the prototype of one designed
to withstand crushing pressures and extreme temperatures, is set
to be lowered to depths of 9 meters (30 feet) in Monterey Bay
Aquarium's giant kelp forest July 28 as part of NASA's hunt for
clues to life's origins.
Scientists from NASA's Jet Propulsion Laboratory, Pasadena,
CA, will sink the new package of underwater cameras, temperature
sensors, optics and a spectrometer into the emerald waters of a
controlled aquatic environment to test the capabilities of more
advanced instruments to explore the interior of volcanic vents.
These cracks in the sea floor, occurring at depths of between 500
meters and 4,000 meters (1,650 feet and 13,200 feet), are known
to nurture a pageantry of macabre bottom-dwellers such as salps,
siphonophores, crustaceans and gelatinous animals only recently
discovered at such depths.
"These instruments will be able to record water temperatures
in the throat of a vent, capture video and low- and- high-
resolution still images of the walls of the vent, and record
spectral or fluorescent signatures of minerals and bioluminescent
life dwelling in these crevices," said Dr. Arthur Lane, manager
of the Underwater Volcanic Vent Mission probe at JPL. "The
experiment will demonstrate a more sophisticated set of
instruments that will be used in late August and September to
probe the Pitcairn, McDonald and Teahitia seamounts near Tahiti,
where hydrothermal vents range from 900 meters to 3,600 meters
(2,970 feet to 11,880 feet) in depth."
The mission will gather preliminary data and serve as a
stepping stone in the development of technology and instrument
housing required in the search for evidence of life in extreme,
high-pressure liquid environments. This information will aid in
NASA's proposed efforts to develop technologies capable of
exploring more extreme liquid and ice environments, such as Lake
Vostok in Antarctica, and eventually, to send instrumented probes
to the Martian polar caps and frozen oceans on Jupiter's moon,
Europa, and Saturn's moon, Titan.
The discovery of gelatinous material in underwater volcanic
vents has opened a new chapter in the search for life and
organisms that can survive in extreme environments. Hydrothermal
vents and the biological communities thriving in these remote
pockets of the sea floor are found primarily at tectonic plate
junctions at temperatures ranging from nearly 80 to almost 400
degrees Celsius (170 to 750 degrees Fahrenheit) and at pressures
as high as 6,000 pounds per square inch. Typical water
temperatures inside the vents range from 200 to more than 350
degrees C (392 to 662 degrees F) and drop quickly to ambient
temperatures of about 4 degrees C (39 degrees F) outside of the
vents.
To date, organisms living near the vents are known to
inhabit only the waters outside of the vents. Layers of
gelatinous material attached to the vents are presumed to be
organic and the product of living organisms. Researchers have
reported that on at least one occasion the gel appeared to
emanate directly from a vent throat.
"If there are indeed life forms present inside these vents,
their presence may challenge accepted notions of the temperature
ranges at which life can function," Lane said.
Last year, Lane and colleague Lloyd French of JPL, in
collaboration with Dr. Gary McMurtry of the University of Hawaii,
developed and deployed an instrumented probe into the Forbidden
Vent Fields near the summit of the Loihi seamount, an underwater
Hawaiian volcano.
That probe was tested last year in Monterey aquarium's kelp tank
before its deployment in Hawaii.
"The probe was capable only of limited visual imaging and
temperature determination at depths of approximately 1,500 meters
(4,950 feet)," French said. "Since that time, we've been able to
increase the depths at which these instruments can operate to
more than 4,000 meters (13,200 feet). The free-standing package
of instruments will be able to acquire temperature data, video
imaging and high-resolution digital stills. This year we're also
testing a new light source and spectrographic instrument to see
if we can gather more information about the bacterial growth --
what looked like thin veils of jellyfish-like material -- we
observed last year around the Loihi vent."
During the mission this August and September, scientists
will use the French research vessel L'Atalante to test their
instrument probe in several deep ocean volcanic vents in the
South Pacific. Using a deep submersible called Nautile, equipped
with a robotic arm, they will place the 142-centimeter (56-inch)
titanium tube housing the instruments inside several vents in the
area to investigate the presence and nature of organic matter.
Once the technology has been developed and demonstrated to
work at depths of 4,000 meters (13,200 feet), the probe's
external shell will be modified for use in sub-glacial lakes like
Lake Vostok, an ancient freshwater lake that appears to extend
about that deep beneath Antarctic's surface. The design may also
become a prototype for a probe that could penetrate Mars' icy
polar caps and search for microbial life, or explore a liquid
ocean thought to lie 7 kilometers to 8 kilometers (about 4 miles
to 5 miles) below the icy surface of Europa.
The Tahiti underwater volcanic vent mission is a
collaboration of the international POLYNAUT campaign in the South
Pacific, conducted by the French Institute of Research and
Exploitation of the Sea, with involvement from the University of
Hawaii and NASA/JPL. JPL's work on the project is conducted for
NASA's Office of Space Science, Washington, DC. JPL is a
division of the California Institute of Technology, Pasadena, CA.
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7/26/99 DEA
#99-061
This text derived from http://www.jpl.nasa.gov/releases/99/monterey.html
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