A summer voyage to investigate the
causes of one of the most devastating tsunamis in United States
history has uncovered new mysteries about biological and geological
processes off Alaska. Probing the depths below one of the world's most
important fisheries, scientists with Scripps Institution of
Oceanography at the University of California, San Diego, as well as
Indiana State University and their colleagues, conducted the first
exploration of deep seafloor biological communities in a sector of the
Alaskan margin off the Aleutian Islands along the northern part of the
Pacific Rim.

Scientists operating a remotely operated vehicle observed a jellyfish
near the ocean floor.
In addition to identifying previously undiscovered deep-sea
habitats, the researchers have stirred debate about the causes and
characteristics of a devastating 1946 tsunami. The Pacific Ocean-wide
event led to more than 150 deaths and widespread destruction as it
pounded shorelines from Alaska to Antarctica.
The July research cruise, aboard the Scripps research vessel Roger
Revelle, was sponsored by the National Oceanic and Atmospheric
Administration's West Coast National Undersea Research Program.
To achieve a complete picture of how the 1946 event impacted
seafloor habitats, the researchers extensively mapped the area,
collected sediment samples and probed the region with Woods Hole
Oceanographic Institution's Jason II remotely operated vehicle (ROV).
They charted new canyons and features of this previously unexplored,
remote region of the world.
Using multibeam mapping technology, the scientists produced
previously unavailable details of the area, a snapshot that gave them
new insight into the region's history. In one scenario, scientists had
predicted that an enormous undersea landslide in the area unleashed
the giant tsunami. The new images, however, counter this explanation
by showing no evidence of such a large landslide.

Tony Rathburn (left) and Lisa Levin led the first exploration of deep
seafloor biological communities in a sector of the Alaskan margin
off the Aleutian Islands.
"We found seafloor evidence that will cause tsunami modelers to
rethink the cause and characteristics of the 1946 tsunami," said Tony
Rathburn, a research associate scientist at Scripps and a faculty
member at Indiana State University. "Our findings make the causes of
the 1946 tsunami even more mysterious."
An earthquake may now emerge as the leading cause of the 1946
event, but the scientists say much more investigation is needed to
pinpoint the cause due to the new findings.
The ROV and sonar explorations revealed a complex set of
environments on the Alaskan margin, including deep canyons, steep
scarps (walls), sandy slopes and an unusual seamount. While exploring
the area, the scientists also discovered previously unknown cold
methane seeps and biological communities that exist in such
environments. The seeps, found 3,300 meters below the water's surface,
were unlike others that have been studied on the Pacific margin.
Though the researchers focused on worms, crustaceans and
single-celled creatures, they also found clams and other animals that
obtain their nutrition from the chemical discharges of the seeps, a
process known as chemosynthesis. These creatures contain bacteria that
provide nutrition for the "host" animal, while the host provides a
home and chemicals from the seep for the bacteria.

Scripps researcher Lisa Levin dubbed this the "weeping rock," which
featured organisms that grow in a downward direction.
"At several thousand meters deep, we would notice sparse evidence
of animal life, but then all of a sudden we would find, right next to
a seep, rocks just completely covered with organisms," said Lisa
Levin, a professor at Scripps. "There was 100 percent cover of animal
life on these rocks. On one of them that I call 'weeping rock,' the
organisms were growing down instead of up, possibly to reach down to
the chemical source."
The scientists also identified many new, previously unidentified
deep-sea coral habitats, some possibly associated with the methane
seeps.
The expedition included an interdisciplinary team of Scripps
researchers, including geologists, geochemists, biogeochemists,
biologists and paleoceanographers.
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Scripps Institution of Oceanography, at the University of California,
San Diego, is one of the oldest, largest, and most important centers
for global science research and graduate training in the world. The
National Research Council has ranked Scripps first in faculty quality
among oceanography programs nationwide. The scientific scope of the
institution has grown since its founding in 1903 to include
biological, physical, chemical, geological, geophysical, and
atmospheric studies of the earth as a system. Hundreds of research
programs covering a wide range of scientific areas are under way today
in 65 countries. The institution has a staff of about 1,300, and
annual expenditures of approximately $140 million from federal, state,
and private sources. Scripps operates one of the largest U.S. academic
fleets with four oceanographic research ships and one research
platform for worldwide exploration.
Source:
http://scrippsnews.ucsd.edu/article_detail.cfm?article_num=657