Organic Matter from H2O and CO2 Dissolved in Minerals

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Scientific paper

Complex organic compounds must have been available on the early Earth. However, where they came from or how they formed has remained a subject of intense discussion. Our work looks at the solid Earth as a possible source. We have succeeded in extracting organic molecules from inside MgO and olivine in quantities sufficient to obtain not only IR, 1H- and 13C-NMR spectra but also to purify at least on of the compounds and to grow single crystals for x-ray structure determination. The MgO crystals used in these experiments had crystallized at 2860 degrees C from a melt equilibrated with CO/CO2/H2O at 1 bar in a carbon arc furnace. The olivine crystals originated from the high pressure environment of the upper mantle. Thermodynamics requires that, as a melt saturates with reactive gases such as CO, CO2 or H2O, the crystals growing from such a melt dissolve some of these gases. During cooling, the dissolved gases undergo a redox conversion by which solute CO2 reduces to C, and solute H2O reduces to H2, counterbalanced by an aliquot of O2- oxidizing to O_. As the solubility decreases with decreasing temperature, C and H2 segregate, concentrating along dislocation lines, subgrain boundaries etc.

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