DEPTHX Robot Dives Deep for Sinkhole  Slime  
STATUS REPORT
Date  Released: Thursday, January 17, 2008
Source: _Astrobiology Magazine_ (http://www.astrobio.net/) 
 
 
By Henry Bortman 
 
In May, researchers successfully conducted the third and final  field test of 
the autonomous underwater robot, _DEPTHX_ 
(http://www.stoneaerospace.com/products-pages/products-DEPTHX.php) .  Their 
objective was to explore Cenote 
Zacaton, the world's deepest water-filled  sinkhole.  
Zacaton lies near one end of a chain of sinkholes stretching  nearly half a 
mile across Rancho La Azufroza (Sulfur Ranch), located in  northeastern Mexico, 
roughly 20 miles from the Gulf Coast. Even without the  sinkholes, the 
biology of the region would make a fascinating subject of study.  The landscape 
is 
dotted with a muddle of tropical deciduous trees and bromeliads  growing 
side-by-side with agaves and cacti typical of desert climates. Each day,  as 
dawn 
approaches, a flock of green parrots takes wing, shrieking and squawking  as 
they circle the rim of Zacaton. Later in the day, the air grows thick with  
butterflies, more than a dozen different species, some with wingspans exceeding 
 
six inches. It is a languid, sun-drenched setting.  
But what lies below ground, in the dark waters of Zacaton, where  only 
microbial life can survive, is what has piqued the interest of scientists  and 
engineers from Stone Aerospace, the University of Texas at Austin, Carnegie  
Mellon 
University's Robotics Institute, the Colorado School of Mines, and other  
institutions, who make up the DEPTHX team.  
The DEPTHX project was funded by NASA's ASTEP (Astrobiology  Science and 
Technology for Exploring Planets) program. ASTEP projects typically  involve 
both 
technology and science components. The robot incorporates a number  of 
innovative technologies. It is the first underwater vehicle that can be  placed 
in an 
enclosed water-filled space and, without any previous knowledge,  safely 
navigate its way around, build a three-dimensional map of its  environment, and 
collect samples of scientific interest -- all without human  intervention.  
DEPTHX enabled investigators to explore an otherwise inaccessible  ecosystem 
that extends far below the Earth's surface. The robot had a mechanical  arm 
that could be extended 2 to 3 meters (6.5 to 10 feet); at its end was a  
spring-loaded penetrator that could sense when it came within a few inches of  
the 
cenote's wall. Once in position, it grabbed a gob of the microbial biofilm  
that 
coats the entire interior surface of the sinkhole, and brought it back to  
the surface for later laboratory analysis. Positioning the 1.5-ton robot  
precisely -- not too far from the uneven surface of the cenote wall to obtain a 
 
sample, but not so close that the penetrator slams into rock and gets bent --  
was challenging, particularly when the robot was doing its own navigation. But  
DEPTHX successfully obtained half a dozen samples of microbial Zacaton wall  
slime. The deepest of these came from close to the bottom of the cenote, at a  
depth of 272 meters (892 feet).  
Finding the bottom of Zacaton was another of DEPTHX's  accomplishments. 
Previously, no-one had been able to determine for certain how  deep the cenote 
was. 
As it turns out, the bottom is sloped, ranging from 315  meters (1033 feet) 
at its high end down to 320 meters (1050 feet). And it may go  even deeper. At 
the low end of the cenote, the robot found what appeared to be a  narrow 
tunnel that extended outward, and perhaps farther downward. Because the  
research 
team was pressed for time, however, and because they wanted to make  sure they 
could safely get the craft back to the surface, they told DEPTHX to  come home 
without exploring the tunnel.  
John Spear, the lead microbiologist on the DEPTHX team, speculates  that this 
deep channel is connected to an underground system of thermally heated  
water. About one million years ago, geologists believe, the Zacaton region was 
a  
site of intense hydrothermal activity, not unlike Mammoth Hot Springs in  
present-day Yellowstone National Park. Although thermal activity around Zacaton 
 
has calmed down considerably since those fiery days, there are clear signs that 
 
something is still stirring underground: a pervasive scent of sulfur hovers  
around the cenote, and Zacaton's water is a constant 30 degrees C (86 degrees  
F). In fact, says Spears, one of the surprising discoveries made by DEPTHX is 
 that the temperature in Zacaton is constant all the way through its  
thousand-foot water column. He expected to find temperature variation with  
depth, a 
more common scenario.  
"If we stuck DepthX in a place like Yellowstone Lake, for example,  you would 
see gradients of change in temperature. It would probably be warm on  the 
surface, cold in the middle, and then down at the thermal vents warm again,"  
Spear said. But something is keeping Zacaton unusually well-mixed. I asked 
Spear  
what caused the mixing. "Don't know," he replied, but in a later email he 
added  that "there is a large amount of geothermally heated water flowing 
through 
the  system."  
Whatever its cause, the unexpected uniformity put a kink in the  research 
team's sample-collection plans. They had hoped to use gradients in the  water's 
temperature, in its salinity and in its level of dissolved oxygen to  guide 
DEPTHX toward the best sampling locations. Places where such changes occur  are 
interesting because they are often accompanied by an ecological change.  
Different types of organisms thrive in cooler water than in warmer water, for  
example.  
Often, there is also a visual indicator of such changes. In  Yellowstone, 
where Spear has worked extensively, "I could walk up to a hot  spring and say, 
'I 
want a sample right there,' mainly because of my visual  interpretation of 
it, what I see," he says. Green, for example, indicates the  presence of 
photosynthetic organisms, which can survive only in relatively cool  water. 
Yellow-, 
orange- and red-hued organisms dominate in hotter waters.  
"You'd like the robot to do the same thing, use a visual cue to  understand a 
place," Spear says. He was hoping to be able to use "color changes  on the 
walls of the cenote," which "might correlate with chemistry," to guide  the 
robot toward good places to collect samples. But, apart from a shallow  
oxygenated 
zone near Zacaton's surface, the microbial life that clung to the  cenote 
walls was visually uniform, from top to bottom.  
Nevertheless, Spear expects the DNA analysis that his lab will  perform over 
the next few months on the Zacaton samples to yield valuable  results. 
Preliminary analysis of samples collected a couple of years ago by a  diver, at 
a 
depth of 85 meters (280 feet), turned up "six new groups of  bacteria." And by 
"six new groups" Spear emphasized, he didn't mean six new  species. "The 
bacteria domain [one of the three main branches on the tree of  life] has about 
100 
different divisions or phyla in it. So we found six new  ones, from here," he 
explained. "That's kind of equivalent to walking out your  door in the morning 
and finding plants for the first time." To be fair, Spear  points out that 
"you can often find new groups" even in places as pedestrian as  common garden 
soil. "It could even be something that's living between your  teeth." Still, 
six 
is a pretty good haul for one sinkhole. "And we think we can  find more," he 
adds.  
The samples that Spear's lab will analyze were collected while  DEPTHX was 
under human control. Because the robot's time in Zacaton was limited,  DEPTHX 
engineers had to choose between pursuing science goals or technology  goals, 
and 
they decided to tell the robot where to collect its samples, rather  than to 
let the craft's onboard computers make autonomous choices.  
But the robot's software-engineering team, which hails from  Carnegie 
Mellon's Robotics Institute, also got a chance to put the robot's  
sophisticated 
technology to the test. In Poza Verde (Spanish for "Green Pool"),  a wider but 
shallower cenote near Zacaton, DEPTHX was tested in "exploration  mode." In 
this 
mode, the robot is not given any instructions about where to go  or what to 
do. It's dropped into the water and simply told to go find  interesting stuff. 
It is responsible both for navigating its way around and for  deciding what is 
interesting. The engineering team judged this test a success.  
That is promising, because exploration mode will have to work well  for the 
next phase of the robot's life. Later this year, DEPTHX will morph into  
ENDURANCE, the same robot but with a slightly different configuration, and will 
 
transition from exploring balmy semitropical waters to swimming about in chilly 
 
ice-covered lakes.  
The first such cold-water test will take place in February 2008,  in the 
Midwest. That will be a trail run for an even more challenging mission  late in 
2008: autonomous exploration of the waters of Antarctica's Lake Bonney,  an 
ice-covered lake about 3 km (1.8 miles) long and 1.5 km (0.9 miles) wide.  
To date, very little is known about Lake Bonney. Peter Doran, a  University 
of Illinois at Chicago associate professor and the principal  investigator for 
the ENDURANCE project, and his colleagues have been studying  the lake for 
several years, measuring its temperature, salinity and a handful of  other 
parameters. But those measurements have all been made "in the center of  the 
lake," 
Doran says. "We go back to the same spot every year." ENDURANCE, he  says, 
will enable researchers for the first time to develop a portrait of the  lake - 
its temperature, its chemistry, and its microbial ecology - in three  
dimensions.  
_http://www.spaceref.com/news/viewsr.html?pid=26710_ 
(http://www.spaceref.com/news/viewsr.html?pid=26710) 



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