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Ice surrounds an island in the background.
Photo Credit: Maria Vernet
Ice surrounds Christensen Island in the Larsen A Embayment on the eastern side of the Antarctic Peninsula. The unusually thick ice conditions prevented the research vessel Nathaniel B. Palmer from reaching the Larsen B Embayment farther south.


There were also some scientific surprises along the way — though at least one discovery has potentially troubling implications for the fragile Antarctic ecosystem.

A remotely operated vehicle (ROV) brought by a Belgian team for the LARISSA project discovered a large number of invasive crabs moving up from deep water in a 1,500-meter-deep basin off Anvers Island referred to as the Palmer Deep.

Domack said that there must have been at least 100,000 crabs, which appear to have stripped the seafloor clean as they climbed to shallower waters made more inviting by climate change. “They’re decimating the Antarctic fauna. They’re an invasive species from Patagonia,” he said.

Craig Smith, University of Hawaii External Non-U.S. government site professor of oceanography on the LARISSA cruise, told the Honolulu Star-Bulletin in a recent interview External Non-U.S. government site that king crabs had been absent from cold Antarctic ecosystems for possibly millions of years, but with climate warming they are living far shallower than ever recorded.

“Climate warming in Antarctica is faster than anywhere on the globe,” he told the paper, and abundance of animals might decline as a result of warming, and “unique communities may change. Species may be lost.”

The ROV also spied less troublesome critters, like giant marine worms, an octopus, starfish and krill. The ROV, controlled by a three-person team from the Renard Center of Marine Geology at Ghent University External Non-U.S. government site in Belgium, carried a video camera to capture real-time images, as well as instruments to collect sediment, gas and water samples.

“The ROV was great,” Domack said. “We used it in as many situations as we could to resolve interesting problems that presented themselves as we worked through the cruise.”

Ship moves through sea ice.
Photo Credit: Maria Vernet
The Nathaniel B. Palmer pushes through sea ice on the eastern side of the peninsula.
Larsen B Ice Shelf after collapse.
Photo Credit: NASA
The Larsen B Ice Shelf after it first broke up.
Larsen B Ice Shelf after the ice cleared out.
Photo Credit: NASA
The Larsen B Ice Shelf after the ice cleared out.

Maria Vernet External Non-U.S. government site, a research biologist from Scripps Institution of Oceanography at UC San Diego External Non-U.S. government site, said the marine life on the seafloor was “extremely rich” on the western side of the peninsula. She said one hypothesis was that the plentiful phytoplankton in the upper surface of the waters fed the benthic communities below.

“Of course, we only had a snapshot in time,” she said.

Rocky road, good science

One problem the LARISSA team couldn’t solve was the thick pack ice in the Weddell Sea. The Palmer made a second effort to push into the Larsen B Embayment in February but again failed to penetrate to the former location of the ice shelf.

Domack said a later review of ice images since 1998, after the Larsen A Ice Shelf broke apart, showed enough open water every year that would have allowed the ship to reach most of its field targets. Only 2010 proved the exception to the rule.

“This was truly anomalous sea ice and weather year,” he said.

It was in that region five years ago that Domack and colleagues on a previous expedition found extraordinary signs of life on the floor of the continental shelf — bacteria so thick it was visible to the naked eye in what biologists call bacterial mats. The scientists had unexpectedly discovered a cold seep biological community, subsisting not on light, as most ecosystems, but on methane vented through the seafloor.

It was there that the researchers had hoped to return with the ROV and other instruments to study the cold seep community and drill into the sediments to learn more about the ice shelf collapse.

Domack said a follow-up LARISSA cruise is scheduled for 2012. Some of the unfinished work will be completed, he added, but other studies, such as of the bizarre bacterial mats, may not happen without an ROV.

A team of German researchers, who visited the region in 2007, is set to return to the Larsen Embayment next year, Domack noted. “We may just be beaten out of that even though we made the discovery. That’s the way it goes,” he said philosophically.

The ship and its crew had one last surprise as they steamed north back to Punta Arenas in Patagonian Chile. One of the world’s most powerful earthquakes had struck the morning of Feb. 27, creating widespread damage in the north of the country, including the gateway airport in Santiago.

The Palmer docked at Punta Arenas on March 1. The transportation disruptions stranded the crew and scientists for several more days. Domack lingered for a couple of more weeks to help with the scientific response to the earthquake after an exhausting two months at seas.

Despite what he called a “very difficult cruise,” Domack said he was pleased with the overall results, as well as the work ethic of personnel from Raytheon Polar Services Co. External Non-U.S. government site and Edison Chouest Offshore External Non-U.S. government site, the companies contracted to support the marine science program.

“It could have degenerated into a logistical waste of resources, but we were able to put it together, and I think we got some really good science out of it,” he said.

NSF-funded research in this story: Eugene Domack, Hamilton College, Award No. 0732467 External U.S. government site; Ted Scambos, University of Colorado at Boulder, Award No. 0732921 External U.S. government site; Ellen Mosley-Thompson and Lonnie Thompson, Ohio State University, Award No. 0732655 External U.S. government site; Maria Vernet, University of California-San Diego Scripps Institution of Oceanography, Award No. 0732983 External U.S. government site; Craig Smith, University of Hawaii, Award No. 0732711 External U.S. government site. Back   1 2 3