A team of University of Minnesota scientists has discovered how iron- and chromium-rich rocks can generate natural gas (methane) and related hydrocarbons when reacted with superheated fluids circulating deep beneath the floor of the Atlantic Ocean. Because the process is completely nonbiological, the hydrocarbons could have been a source of "food" for some of the first organisms to inhabit the Earth. Also, methane is a potent greenhouse gas, and this process may have contributed to global warming early in geologic time, the researchers said. The researchers - Dionysios Foustoukos and Fu Qi and their graduate adviser, professor W.E. Seyfried, Jr. - will present a portion of this work Monday, Dec. 13, at the American Geophysical Union meeting in the Moscone Convention Center, San Francisco.