| Erupting
Undersea Volcano Near Island of Guam Supports Unique Ecosystem
Scientists who
have just returned from an expedition to an erupting undersea
volcano near the Island of Guam report that the volcano appears
to be continuously active, has grown considerably in size
during the past three years, and its activity supports a unique
biological community thriving despite the eruptions.
An international
science team on the expedition captured dramatic new information
about the eruptive activity of NW Rota-1.
"This research allows us, for the
first time, to study undersea volcanoes in detail and close
up," said Barbara Ransom, program director in NSF's Division
of Ocean Sciences, which funded the research. "NW Rota-1
remains the only place on Earth where a deep submarine volcano
has ever been directly observed while erupting."
Scientists first observed eruptions at
NW Rota-1 in 2004 and again in 2006, said Bill Chadwick, an
Oregon State University (OSU) volcanologist and chief investigator
on the expedition. This time, however, they discovered that
the volcano had built a new cone 40 meters high and 300 meters
wide.
"That's as tall as a 12-story building
and as wide as a full city block," Chadwick said. "As
the cone has grown, we've seen a significant increase in the
population of animals that lives atop the volcano. We're trying
to determine if there is a direct connection between the increase
in the volcanic activity and that population increase."
Animals in this unusual ecosystem include
shrimp, crab, limpets and barnacles, some of which are new
species.
"They're specially adapted to their
environment," said Chadwick, "and are thriving in
harsh chemical conditions that would be toxic to normal marine
life.
"Life here is actually nourished
by the erupting volcano."
Verena Tunnicliffe, a biologist from the
University of Victoria, said that most of the animals are
dependent on diffuse hydrothermal venting that provides basic
food in the form of bacterial filaments coating the rocks.
"It appears that since 2006 the diffuse
venting has spread and, with it, the vent animals," Tunnicliffe
said. "There is now a very large biomass of shrimp on
the volcano, and two species are able to cope with the volcanic
conditions."
The shrimp reveal intriguing adaptations
to volcano living.
"The 'Loihi' shrimp has adapted to
grazing the bacterial filaments with tiny claws like garden
shears," said Tunnicliffe. "The second shrimp is
a new species--they also graze as juveniles, but as they grow
to adult stage, their front claws enlarge and they become
predators."
The Loihi shrimp was previously known
only from a small active volcano near Hawaii--a long distance
away. It survives on the fast-growing bacteria and tries to
avoid the hazards of the volcanic eruptions. Clouds of these
shrimp were seen fleeing volcanic bursts.
The other species attacks the Loihi shrimp
and preys on marine life that wanders too close to the volcanic
plumes and dies. "We saw dying fish, squid, etc., raining
down onto the seamount, where they were jumped on by the volcano
shrimp--a lovely adaptation to exploiting the noxious effects
of the volcano," Tunnicliffe said.
The new studies are important because
NW Rota-1 provides a one-of-a-kind natural laboratory for
the investigation of undersea volcanic activity and its relation
to chemical-based ecosystems at hydrothermal vents, where
life on Earth may have originated.
"It is unusual for a volcano to be
continuously active, even on land," Chadwick pointed
out.
"This presents us with a fantastic
opportunity to learn about processes we've never been able
to directly observe before," he said. "When volcanoes
erupt in shallow water they can be extremely hazardous, creating
huge explosions and even tsunamis. But here, we can safely
observe an eruption in the deep ocean and learn valuable lessons
about how lot lava and seawater interact."
Chadwick said that volcanic plumes behave
completely differently underwater than on land, where the
eruption cloud is filled with steam and ash, and other gases
are invisible.
"In the ocean, any steam immediately
condenses and disappears and what is visible are clear bubbles
of carbon dioxide and a dense cloud made of tiny droplets
of molten sulfur, formed when sulfur dioxide mixes with seawater,"
Chadwick said. "These volcanic gases make the eruption
cloud extremely acidic--worse than stomach acid--which is
another challenge for biological communities living nearby."
Ocean acidification is a serious concern
because of human-induced carbon dioxide accumulating in the
atmosphere. "Submarine volcanoes are places where we
can study how animals have adapted to very acidic conditions,"
Chadwick said.
During the April 2009 expedition, aboard
the University of Washington's R/V Thompson, the scientists
made dives with Jason, a remotely operated vehicle (ROV) operated
by the Woods Hole Oceanographic Institution.
Chadwick said that "it was amazing
how close Jason can get to the eruptive vent because the pressure
at a depth of 520 meters [about 1,700 feet] in the ocean keeps
the energy released from the volcano from becoming too explosive."
Some of the most intriguing observations came when the volcano
slowly pushed lava up and out of the erupting vent.
"As this was happening, the ground
in front of us shuddered and quaked, and huge blocks were
bulldozed out of the way to make room for new lava emerging
from the vent," Chadwick said.
Part of the evidence that the volcano
is in a constant state of eruption comes from an underwater
microphone--or hydrophone--that was deployed a year ago at
NW Rota-1 by OSU geologist Bob Dziak.
The hydrophone "listened" for
the sounds of volcanic activity. The data it recorded clearly
show that the volcano was active the entire year before the
latest expedition. Another hydrophone and other instruments
will monitor the volcano in the coming year.
The international team included scientists
from OSU, the University of Washington, University of Victoria,
University of Oregon, NOAA's Pacific Marine Environmental
Laboratory, New Zealand and Japan.
This research was funded by the National
Science Foundation (NSF).
Source: www.sciencedaily.com
Date: 5
May , 2009

|