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News Release : Scientists Discover First Seafloor Vents on Ultraslow-Spreading Ridge |
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April 12, 2007
Media Relations Office
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Woods Hole Oceanographic Institution
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Enlarge Image The Chinese research vessel, Dayang 1, used in the discovery of the first hot vents in the Indian Ocean. (Photo by Mr. Huisheng Lu of R/V Dayang 1)
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Enlarge Image WHOI team members (from left to right: Al Duester, Andy Billings, and Christopher German) recover ABE from one of its three dives in the Indian Ocean. (Photo courtesy InterRidge)
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Enlarge Image Jian Lin (leader of the WHOI team, front right) with Mr. Songgang Zhen (R/V Dayang 1 Captain, front left) stand before the WHOI ABE vehicle. (Photo credit: R/V Dayang 1 science party)
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Enlarge Image Three members of the WHOI team: Christopher German, Jian Lin, and Dana Yoerger stand before the WHOI ABE underwater autonomous vehicle on the deck of the R/V Dayang 1.
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Enlarge Image The Southwest Indian Ridge is a spreading center between the African tectonic plate (top left, yellow-orange) and the Antarctic plate (bottom left, red). (Photo credit: NOAA Geophysical Data Center)
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| Source: Media Relations
Scientists have found one of the largest fields of seafloor vents
gushing super-hot, mineral-rich fluids on a mid-ocean ridge that, until
now, remained elusive to the ten-year hunt to find them.
“The discovery of the first active vents ever found on an
ultraslow-spreading ridge is a significant milestone event,” said Jian
Lin, leader of a team of Woods Hole Oceanographic Institution (WHOI)
scientists who participated in a Chinese expedition to the remote
Southwest Indian Ridge in the Indian Ocean in February and March.
Since deep-sea hydrothermal vents were first discovered 30 years ago in
the Pacific Ocean, scientists have studied them all along the Mid-Ocean
Ridge, a 40,000-mile-long mountain range that zigzags through the
middle of the world’s ocean basins like a giant zipper. The ridge marks
the area where the Earth’s giant tectonic plates spreads apart and new
ocean crust forms from hot lava rising from deep within Earth’s mantle.
Most studies of the chimney-like vent structures have taken place along
ridges in the “fast-spreading” East Pacific Rise (100 to 200
millimeters per year) and the “slow-spreading” Mid-Atlantic Ridge (20
to 40 millimeters per year). Only in recent years have scientists
explored “ultraslow-spreading ridges” (less than 20 millimeters per
year) in the Arctic and Indian Oceans—remote areas tough to get to, and
therefore the least studied.
Scientists initially thought ultraslow-spreading ridges would be too
cold to host large hot vents. But in the past decade, some scientists
began to hypothesize that the slower a ridge spreads, the fewer vents
it would have—but the bigger the vent fields would be.
“This cruise confirmed that hypothesis,” said Lin, a marine
geophysicist and U.S. Coordinator of the 20-day expedition aboard the
Chinese research vessel Dayang 1. “People have been looking for active hot vents on ultraslow ridges for more than 10 years,” Lin said.
In 2005-06, as part of China’s first around-the-world oceanographic expedition, Lin had sailed as a US chief scientist on Dayang 1
to the Southwest Indian Ridge, where scientists found tantalizing
evidence of active hydrothermal venting. They gathered critical data
that led them back to the site this year.
During the February-March expedition, the team nailed the discovery
with the aid of ABE, WHOI’s Autonomous Benthic Explorer, which has been
instrumental in recent years in helping scientists find vents on the
bottom of the ocean much quicker than ever before. ABE acts like a
robotic deep-sea bloodhound: In a sequence of dives, its sensors “sniff
out” clues indicating a plume of fluids emanating from a vent and
collect data scientists use to home in on the vent.
ABE also uses sonar to create maps of vent fields and takes photographs
about 5 meters above them. ABE snapped 5,000 images of the robust
Southwest Indian Ridge vent site, which is among the largest known to
date. It is larger than a football field (120 meters by 100 meters).
The discovery was a first for China. “This discovery reflects
China’s increasing contribution to ocean science in general, and ridge
science in particular,” Lin said.
The China Ocean Mineral Resources R&D Association (COMRA) in
Beijing, China, funded the 2005-06 expedition and ABE’s participation
in the current one. COMRA, which represents China in the International
Seabed Authority, has been exploring the deep sea for mineral resources
since the early 1990s.
China is increasing investments in ocean science, Lin said. COMRA’s
primary interests lay in the large sulfide deposits created by
hydrothermal vents, which are rich in copper, zinc, gold, and other
minerals, he said.
“Our Chinese colleagues were the happiest people I’ve ever seen at sea
when they brought the first samples aboard,” said Dana Yoerger,
scientist in the WHOI Deep Submergence Laboratory and co-designer of
ABE, who participated in the expedition. Once ABE pinpointed the site’s
exact location, the Chinese team sent down its “TV grab”— a grappling
device guided by a television camera—and retrieved a reddish chunk of a
vent chimney, Yoerger said.
The researchers outran a tropical cyclone and collected the data they
needed in just six days and three ABE dives. “It was the most
ruthlessly efficient science we’ve ever done,” said Christopher German,
chief scientist of the WHOI-operated National Deep Submergence
Facility, who also participated in the expedition. “We had no
margin for error.”
The Chinese science party was led by chief scientist Chunhui Tao, a
geophysicist at the Second Institute of Oceanography in Hanzhou, China.
“The two international teams worked exceedingly well for this kind of complex operation,” Lin said
Last updated: January 13, 2010 |
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