18 October, 2005

None-organic natural methane production?

New research coauthored by Dudley Herschbach, Baird research professor of science and recipient of the 1986 Nobel Prize in chemistry, questions that thinking. Published last fall in the Proceedings of the National Academy of Sciences, the study describes how investigators combined three abiotic (non-living) materials -- water (H2O), limestone (CaCO3), and iron oxide (FeO) -- and crushed the mixture together with the same intense pressure found deep below the earth's surface. This process created methane (CH4), the major component of natural gas.

What about the dinosaurs? :(

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