"This is definitely the biggest thing I've ever been involved with in the Antarctic," said Eugene Domack, a professor at Hamilton College in New York and lead author of the report detailing the ecosystem. The article will be published in the 19 July issue of Eos, the weekly newspaper of the American Geophysical Union. "Seeing these organisms on the ocean bottom--it's like lifting the carpet off the floor and finding a layer that you never knew was there."
Domack suggests the strong possibility that new species of marine life may be uncovered in continuing analyses of the area as ecosystem experts sample the site. The international expedition was there on a U.S. Antarctic Program cruise to study the sediment record in the area vacated by the former ice shelf. The crew recorded a video of the seafloor at the end of its mission and only later discovered a thriving clam community, mud volcanoes, and a thin layer of bacterial mats.
The discovery could provide evidence for researchers to better understand the dynamics within the inhospitable sub-ice setting, which covers more than 1.5 million square kilometers [nearly 580,000 square miles] of seafloor, or an area of the same magnitude as the Amazon basin in Brazil or the Sahara Desert. The ecosystem, known as a "cold-seep" (or cold-vent) community, is fed by chemical energy from within the Earth, unlike ecosystems that are driven by photosynthesis or hot emissions from the planet's crust. Domack and his coauthors propose that methane from deep underwater vents likely provid
Source:American Geophysical Union