The influence of prebiotic-type organic molecules on the crystallization of Al and Mg hydroxides.
It is now well accepted that clays could have concentrated prebiotic organic molecules, protected them from UV radiation and served as templates and catalysts in their prebiotic evolution. A complementary question is: How did prebiotic organics in the oceans, in ground water, or in hydrothermal solutions affect the formation and inorganic evolution of oxides, hydroxides, and clay minerals? In this study predominantly amorphous Al oxyhydroxides (Al gels) and crystalline Mg hydroxyoxides were synthesized, and then crystallized and recrystallized respectively, to Al and Mg hydroxides via wet and dry (w/d) cycling using both water and organic solutions. The products that resulted were examined using IR spectroscopy and X-ray diffraction (XRD). XRD scans of the products formed by w/d cycling of the Al gels with either water or 0.1 M aqueous solutions of methanol or formaldehyde showed that bayerite (alpha Al2O3) was the major phase formed. The acetonitrile treated sample exhibited the most defined XRD peaks, and no crystalline phase could be observed by XRD of the 0.1 M formamide solution treated sample. Cycling the Mg hydroxyoxide with water, or 0.1 M solutions of methanol, formamide, formaldehyde, or acetonitrile resulted in the formation of brucite (Mg(OH)2) (in varying amounts) and of three unidentified phases. One unidentified phase, 'phase II', was observed in the formaldehyde cycled sample (and tentatively identified in the methanol and formamide cycled samples), 'phase III' in the formamide and formaldehyde cycled sample, and 'phase IV' in only the formaldehyde. XRD peaks with a spacing of approximately 11.5 Angstrom (assigned to phase III) suggest intercalation of formamide and formaldehyde into the interlayer spaces of the brucite. Phosphate treatment, prior to w/d cycling with water, and also with the above mentioned organics, while totally preventing subsequent formation of any crystalline Al hydroxide, enhanced the formation of Mg phases, shown by XRD data. Formation of brucite was impeded only by w/d cycling using concentrated methanol solution, but even these effects were reversible. The XRD scans of the products resulting from the aqueous and organic solution cycling treatments of the Mg starting materials showed peaks due to brucite and three unidentified phases. Only the brucite is evident in oriented sample XRD scans of the Mg starting material when treated with methanol, formamide, and acetonitrile. In random powder sample XRD scans of the Mg starting material treated with: 1) methanol--the unidentified phase 11 is evident, 2) formamide--phase II and III are seen, and 3) formaldehyde--phases II, III, and IV are evident.
Costanzo
P M
PM
Department of Geological Sciences, State University of New York at Buffalo, Amherst 14226, USA.
Laszlo
P
P
D000097:Acetonitriles / Q000737:chemistry; D000536:Aluminum Hydroxide / Q000737:chemistry*; D000538:Aluminum Silicates / Q000737:chemistry; D000077215:Clay; D003460:Crystallization; D019418:Evolution, Chemical; D005557:Formaldehyde / Q000737:chemistry; D005559:Formamides / Q000737:chemistry; D005782:Gels; D008276:Magnesium Hydroxide / Q000737:chemistry*; D000432:Methanol / Q000737:chemistry; D013055:Spectrophotometry, Infrared; D014961:X-Ray Diffraction
D000097:Acetonitriles; D000538:Aluminum Silicates; D005559:Formamides; D005782:Gels; D005557:Formaldehyde; D000536:Aluminum Hydroxide; D008276:Magnesium Hydroxide; D000077215:Clay; D000432:Methanol; C032159:acetonitrile