Similar to humans, the bacteria and tiny plants living in the ocean need iron for energy and growth. But their situation is quite different than ours for one, they can't exactly turn to natural iron sources like leafy greens or red meat for a pick-me-up.
So where does their iron come from? New research published by "Nature Geoscience" points to a source on the seafloor: minute particles (called nanoparticles) of pyrite, or fool's gold, from hydrothermal vents at the bottom of the ocean.
Scientists already knew the vents' cloudy plumes emitted from the earth's interior include pyrite particles, but they thought they were solids that settled back on the ocean bottom. A University of Delaware team has shown that the vents emit a significant amount of pyrite as nanoparticles, which have a diameter that is one thousand times smaller than that of a human hair. Because the nanoparticles are so small, they are dispersed into the ocean rather than falling to the bottom.
Barbara Ransom, program director in the agency that funded the research, the National Science Foundation's Division of Ocean Sciences, called the discovery "very exciting."
"These particles have long residence times in the ocean and can travel long distances from their sources, forming a potentially important food source for life in the deep sea," she said.
UD Oceanography Professor and project collaborator George Luther explained the importance of the pyrite's lengthy residence times, or how long they exist in their current form. He said the pyrite, which consists of iron and sulfur as iron disulfide, does not rapidly react with oxygen in the seawater to form oxidized iron, or "rust," allowing it to stay intact and move throughout the ocean better than other forms of iron.
"As pyrite travels from the vents to the ocean interior and toward the surface ocean, it oxidizes gradually to release iron, which becomes available in areas where i
|Contact: Andrea Boyle|
University of Delaware