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The Thompson heads into 30-knot winds.
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Was Grandma a Hyperthermophile?
by Peter Tyson
July 15, 1998
Yesterday a low-pressure zone swept in, bringing 30-knot
winds, ten-foot seas, and
ROPOS
operations to a screeching halt. It was as if Poseidon,
reading exhaustion in the faces of the scientific party after
a successful week of retrieving chimneys, suddenly declared,
"Whew, let's take a break." With the R/V Thomas G. Thompson
groaning through stomach-turning pitches, many retreated
shakily to their rooms. The main lab, library, and ROPOS room,
all usually buzzing with activity, were silent, and the
half-empty mess at meal-time revealed that a few of us were a
tad under the weather.
By this morning, the seas had calmed, and people began to
appear in the passageways again. While we waited for ROPOS to
get to the seafloor, I took the opportunity to catch up with
the biologists, who are studying the bizarre life forms living
in and around black smoker chimneys in search of clues as to
how life began on Earth. You haven't heard much about the
biologists, because the focus of the first fortnight was on
the engineers and geologists preparing and collecting the
chimneys. But they've been here all along, silently going
about their work and patiently waiting for the next "bio
dive."
One is taking place right now, as I write. It is led by Jozee
Sarrazin, a vibrant, French-speaking post-doc at the Woods
Hole Oceanographic Institution, and Istvan Urcuyo, a
gregarious, Nicaraguan-born graduate student at Pennsylvania
State University. They are collaborating on a project to
minutely characterize the community of life that lives on a
single sulfide chimney.
While biologists intimately know the denizens and workings of
tiny patches of rain forest and coral reef, they have
conducted few in-depth studies of this kind on hydrothermal
vent habitats. Such communities were only discovered 20 years
ago, and the environment they inhabit is extremely difficult
to work in, so many unknowns remain. For example, Urcuyo says
that of the more than 300 species of vent life discovered so
far, biologists can follow the life cycle of only about three
or four.
Jozee Sarrazin and Istvan Urcuyo examine tubeworms.
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Urcuyo and Sarrazin are working hard to fill such gaps in our
understanding. In previous work on the Juan de Fuca Ridge,
Sarrazin characterized six different types of biological
communities on sulfide chimneys. They range from Community 1,
distinguished by sulfide worms (Paralvinella sulfincola)
living on newly formed chimneys in water reaching 104°F,
to Community 6, a senescent type dominated by dead or dying
tubeworms (Ridgeia piscesae) in low-temperature water.
Sarrazin's goal is to determine what factors—including
temperature, chemical conditions, substrate type, and degree
of vent flow—control the development of those
communities.
Urcuyo is working with her to define, in addition to the
overall biomass, the composition, distribution, and abundance
of vent animals on selected chimneys. On a ROPOS dive two days
ago that he and Sarrazin directed, Urcuyo had the pilot on
duty scoop a sample off the biologically bristling chimney
Gwenen using a device called the Chimney Master. Like a
vacuum-cleaner bag with fingers, the Chimney Master grabs a
known surface area of material and delivers it to ROPOS'
biobox.
Later, in the main lab, a number of us chipped in to help
Urcuyo and Sarrazin sort the creatures by species. The sample
was from a high-flow Community 5, which is dominated by R.
piscesae tubeworms living in medium-high temperature water.
The tubeworms were there in abundance, along with tiny brown
limpets, scale worms, and several species of polychaete worms.
There was also a single sea spider and perhaps a thousand
snails of the wonderfully named species Depressigyra
globulus.
Meanwhile, Jon Kaye, a graduate student at the University of
Washington, told me about the microbial life he and his
advisor John Baross are focusing on. After each of the four
chimneys we collected was lifted onto the deck of the CCGS
John P Tully, Kaye and Baross cored them from edge to center.
They're hoping to find out what species live where within
different types of chimneys, and what their relationship is
with the geology. For example, do some microbes prefer living
on silica while others go for anhydrite?
When the Tully departed, Kaye joined us here on the Thompson
to continue his search for microbes that live in
high-temperature, high-salt-content conditions. No one had
ever seen these before, but already Kaye thinks he has
cultured some in his broth tubes. Pulled up from the deep sea,
these microscopic creatures have grown in his incubator at
temperatures reaching185°F—hence their technical
name, hyperthermophiles. Will they replicate? Do they prefer
or even require super salinity? The latter would prove they
were spewed out from some subsurface community that has those
conditions. Otherwise where did they come from?
"It's all based on Darwinian evolutionary theory, that they
exist for a reason," said Kaye, a lithe, rust-haired man in
his early 20s.
"And what might that reason be?" I asked. "Why would anything
willingly opt for hyper salinity?"
"Well, maybe they began there and later adapted to live
outside of vents. Perhaps we're all descended from
high-salt-tolerant hyperthermophiles."
Such talk has been floating about this ship since we left
port. I'd better listen in while I can, for the word's out
that another low-pressure system is on the way, with even
higher winds predicted. The ROPOS dive now underway may be our
last before we begin our 18-hour sail back to Seattle tomorrow
night.
Peter Tyson is Online Producer of NOVA.
The Tug of the Thompson (June 23)
The ROPOS Guys (June 25)
In the Juan de Fuca Strait (June 27)
Special Report: A Visit To Atlantis (June 29)
Dive 440 (July 1)
Rescue at Sea (July 2)
What's Your Position? (July 4)
Phang! (July 5)
20,000 Pounds of Tension (July 8)
Four for Four (July 11)
Thrown Overboard (July 13)
Was Grandma a Hyperthermophile? (July 15)
Swing of the Yo-Yo (July 18)
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