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A possible energetic role of mineral surfaces in chemical evolution

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Mineral surfaces, particularly clays, are hypothesized to play a significant role in chemical evolution and the origin of life by interacting with various energy sources, which can enhance their catalytic properties and facilitate prebiotic chemistry. This study demonstrates novel luminescent properties of clays that indicate their capacity for energy storage and transfer, suggesting that these minerals could act as substrates for prebiological reactions and potentially serve as primitive life forms.

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Abstract

The postulated roles of clays and other minerals in chemical evolution and the origin of life are reconsidered in terms of the interaction of these minerals with penetrating sources of energy such as ionizing radiation and mechanical stress. This interaction, including such facets as excitation, degradation, storage, and transfer, is considered here with regard to its profound potential for altering the capabilities of minerals to serve both as substrates for prebiological chemistry and as inorganic prototypic life forms. The interaction of minerals and energy in relationship to surface chemistry is discussed in terms of the spectroscopic properties of minerals, the interaction of energy with condensed phases, some commonly accepted concepts of heterogeneous catalysis in the absence of electronic energy inputs, and some commonly accepted and novel means by which surface activity might be enhanced in the presence of energy inputs.

An estimation is made of the potential contribution of two poorly characterized prebiotic energy sources, natural radioactive decay and triboelectric energy. These estimates place a conservative lower limit on their prebiotic abundance. Also some special properties of these energy sources, relative to solar energy, are pointed out which might give them particular suitability for driving reactions occurring under geological conditions.

Skeletal support for this broadly defined framework of demonstrated and potential relationships between minerals, electronic excitation, and surface reactivity, as applied to chemical evolution, is provided from the results of our studies on 1/1 clays. We have discovered and partially characterized a number of novel luminescent properties of these clays, that indicate energy storage and transfer processes in clays. These luminescent properties are interpreted in relationship to the electron spin resonance phenomena, to provide a basis for estimating the potential significance of energy storage and transduction in monitoring or driving clay surface chemistry.

Consideration of the electronic structure of abundant minerals in terms of band theory and localized defect centers provides a predictive theoretical framework from which to rationalize the capacity of these materials to store and transduce energy. The bulk crystal is seen as a collecting antenna for electronic energy, with the defect centers serving as storage sites.

The clay properties produced by isomorphic substitution appear to be intimately associated with all of the life-mimetic chemical processes that have been attributed to clays. It appears sensible to postulate that the energetic properties of these substitutional defect centers may also be influential in these biomimetic processes: the promotion of surface reactions, storage of information, replication with transfer of information, and asymmetric separation of electrical charges, as well as their more recently hypothesized roles in energy storage and transduction. The identity of the sites implicated in all of the biomimetic functions of clays as well as their capacity for energy storage is seen to offer significant potential for coupling these functions to an environmental energy source. A yet more specific and experimentally testable hypothesis is offered for a new biomimetic process performed by clays. This hypothesis is that energy stored near isomorphically substituted sites provides the energetic basis for the coupled transport of electrical charge and/or electronic energy through the clay layer, which operates via environmental activation of electron/hole mobility. This is to say that mobility of charge/electronic excitation between defect centers serves as the basis for a primordial inorganic electron transport chain.

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References

  • Anderson, D. L.: 1974, Earthquakes and the Rotation of the Earth,Science186, 49–50.

    Google Scholar 

  • Angel, B. R., Jones, J. P. E., and Hall, P. L.: 1974, Electron Spin Resonance Studies in Doped Synthetic Kaolinite,Clay Minerals10, 247–255.

    Google Scholar 

  • Aronowitz, S., Coyne, L., Lawless, J., and Rishpon, J.: 1982, Quantum Chemical Modelling of Smectite Clays,Inorganic Chemistry21, 3589–3593.

    Google Scholar 

  • Attix, F. H. and Roesch, W. C.: 1968,Radiation Dosimetry, 2nd Ed., Academic Press, New York, V.1: Fundamentals, Chapter 1.

    Google Scholar 

  • Banin, A.: 1972, Transfer Properties and Friction Coefficients for Salt and Water Flow Through Clays, inFundamentals of Transport Phenomena in Porous Media, Am. Elsevier, N.Y.: pp. 212–220, V.2, Developments in Soil Science.

  • Banin, A. and Margulies, L.: 1983, Simulation of Viking Biology Experiments Suggests Smectites, Not Palagonites, as Martian Soil Analogs,Nature305, 523–525.

    Google Scholar 

  • Bard, A. J.: 1979, Photoelectrochemistry and Heterogeneous Photocatalysis at Semiconductors,Journal of Photochemistry10, 59–75.

    Google Scholar 

  • Bar-Nun, A.: 1975, Shock Synthesis of Amino Acids II,Origins of Life6, 109–115.

    PubMed  Google Scholar 

  • Bar-Nun, A. and Chang, S.: 1983: Photochemical Reactions of Water and Carbon Monoxide in Earth's Primitive Atmosphere,J. Geophys. Res.88, 6662–6672.

    Google Scholar 

  • Bates, J. B., Wang, J. C., and Dudney, N.: 1982, Solid Electrolytes — theβ-Aluminas,Physics Today35, July, 46–53.

    Google Scholar 

  • Bernal, J. D.: 1952,The Physical Basis of Life, Routledge and Kegan Paul, London.

    Google Scholar 

  • Bolton, J. R.: 1978, Solar Fuels-Photochemical Reaction Kinetics and Energy Storage,Science202, 705–711.

    Google Scholar 

  • Bossard, A. R., Raulin, F., Mourey, D., and Toupance: 1982, Organic Synthesis from Reducing Models of the Atmosphere of the Primitive Earth with UV Light and Electric Discharges,J. Mol. Evol.18, 173–178.

    PubMed  Google Scholar 

  • Breslow, R.: 1959, On the Mechanism of the Formose Reaction,Tetrahedron Letters21, 22–26.

    Google Scholar 

  • Bube, R.: 1960,Photoconductivity of Solids, Wiley and Sons, New York.

    Google Scholar 

  • Bunch, T. E. and Chang, S.: 1980, Carbonaceous Chondrites II — Carbonaceous Chondrite Phyllosilicates and Light Element Geochemistry as Indicators of Parent Body Processes and Surface Conditions,Geochimica et Cosmochimica Acta44, 1543–1577.

    Google Scholar 

  • Cady, S. S. and Pinnavaia, T. J.: 1978, Porphyrin Intercalation in Mica-Type Silicates,Inorganic Chemistry17, 1501–1507.

    Google Scholar 

  • Cairns-Smith, A. G.: 1965, The Origin of Life and the Nature of the Primitive Gene,J. Theor. Biol.10, 53–88.

    Google Scholar 

  • Cairns-Smith, A. G.: 1975, A Case for an Alien Ancestry,Proc. Roy. Soc. Lond, B.189, 249–274.

    Google Scholar 

  • Cairns-Smith, A. G.: 1982,The Genetic Takeover and the Mineral Origins of Life, Cambridge University Press, Cambridge, N.Y.

    Google Scholar 

  • Caldwell, M. M.: 1979, Plant Life and Ultraviolet Radiation, Some Perspective in the History of the Earth's Climate,Bioscience29, 520–523.

    Google Scholar 

  • Canuto, V. M., Levine, J. S., Augustsson, T. R., and Imhoff, C. L.: 1982, U.V. Radiation from the Young Sun and Oxygen and Ozone Levels in the Prebiological Paleoatmosphere,Nature296, 816–820.

    Google Scholar 

  • Cariati, F., Erre, L., Micera, G., Piu, P., and Gessa, G.: 1981, Water Molecules and Hydroxyl Groups in Montmorillonites as Studied by Near Infrared Spectroscopy,Clay and Clay Minerals29, 157–159.

    Google Scholar 

  • Chang, S., Des Marais, D., Mack, R., Miller, S. L., and Strathearn, G.: 1983, Prebiotic Organic Synthesis and the Origins of Life, in Schopf, J. W. (ed),Earth's Earliest Biosphere: Its Origin and Early Evolution, Princeton University Press.

  • Chen, C. J. and Osgood, R. M.: 1983, Surface Catalyzed Photochemical Reactions of Physisorbed Molecules,Applied Physics A31, 171–182.

    Google Scholar 

  • Chen, Y., Shaked, D., and Banin, A.: 1979, The Role of Structural Iron (III) in the U.V. Absorption by Smectites,Clay Minerals14, 93–102.

    Google Scholar 

  • Childs, L. P. and Ollis, D. F.: 1980, Is Photocatalysis Catalytic?Journal of Catalysis66, 383–390.

    Google Scholar 

  • Chittendon, G. J. F. and Schwartz, A.: 1981, Prebiotic Photosynthetic Reactions,Biosystems14, 15–32.

    PubMed  Google Scholar 

  • Ciraci, S. and Batra, I. P.: 1983, Electronic Structure ofα-Alumina and its Defect States,Phys. Rev. B.28, 982–992.

    Google Scholar 

  • Corliss, J. B., Baross, J. A., and Hoffman, S. E.: 1981, An Hypothesis Concerning the Relationship Between Submarine Hot Springs and Origin of Life on Earth,Oceanologica Acta, 4, Supplement Proceedings of the 26th International Geological Congress, Paris, July 7–17, 1980, pp. 59–69.

  • Coyne, L.: 1979, Neurotransmitters as Ion Shuttles in Regulation of Neural Activity,J. Theor. Biol.79, 455–472.

    PubMed  Google Scholar 

  • Coyne, L., Lawless, J. G., Lahav, L., Sutton, S., and Sweeney, M.: 1981, Clays as Prebiotic Photocatalysts,Origin of Life: Proceedings of the Third ISSOL Meeting and Sixth ICOL Meeting, Jerusalem, Israel, June 22–27, 1980, Y. Wolman (ed.), D. Reidel, Dordrecht, Holland, pp. 115–124.

    Google Scholar 

  • Coyne, L., Lahav, N., and Lawless, J. G.: 1981, Dehydration Induced Luminescence in Clay Minerals,Nature292, 819–821.

    Google Scholar 

  • Coyne, L., Pollock, G., and Kloepping, R.: 1984, Room-Temperature Luminescence from Kaolin Induced by Organic Amines,Clays and Clay Minerals32, 58–66.

    PubMed  Google Scholar 

  • Coyne, L., Sweeney, M., and Hovatter, W.: 1983: Luminescence Induced by Dehydration of Kaolin — Association with Electron Spin Active Centers and with Surface Activity for Dehydration-polymerization of Glycine,Journal of Luminescence28, 395–409.

    Google Scholar 

  • Cundall, R. B. and Wyn-Jones, M.: 1978, Photophysical Processes in Condensed Phases, inPhotochemistry, Vol. 9, Chem. Soc. of London, U.K., Ch. 2, pp. 92–139.

  • Deamer, D. W. and Oró, J.: 1980, Role of Lipids in Prebiotic Structures,Biosystems12, 167–175.

    PubMed  Google Scholar 

  • Derr, J. S.: 1973, Earthquake Lights: A Review of Observations and Present Theories,Bulletins of the Seismological Soc. of America63, 2177–2187.

    Google Scholar 

  • Dollish, F. R. and Hall, K.: 1965, On the Interaction of Triphenylamine with Iodine and Silica-Alumina Catalysts,J. Phys. Chem.69, 2127–2129.

    Google Scholar 

  • Draganic, I. G. and Draganic, Z. D.: 1980, Radiation-Chemical Aspects of Chemical Evolution and Radiation Chemistry of Simple Cyano Compounds,Radiation Physics and Chem.15, 105–201.

    Google Scholar 

  • Ertem, G.: 1972, Irreversible Collapse of Montmorillonite,Clays and Clay Minerals20, 199–205.

    Google Scholar 

  • Faye, G. H.: 1968,Can. Mineral.9, 403–425.

    Google Scholar 

  • Ferraresso, G.: 1967, Thermoluminescence in Clay Minerals,American Minerologist52, 1288–1296.

    Google Scholar 

  • Finklea, H. O.: 1983, Photoelectrochemistry: Introductory Concepts,J. Chem. Ed.60, 325–329, and other articles in the State of the Art Symposium Proceedings.

    Google Scholar 

  • Folsome, C. and Brittain, A.: 1981, Model Photocells Photochemically Reduce Carbonate to Organic Carbon,Nature291, 482–484.

    Google Scholar 

  • Folsome, C., Brittain, A., Smith, A., and Chang, S.: 1981, Hydrazines and Carbohydrazides Produced from Oxidized Carbon in Earth's Primitive Environment,Nature294, 64–65.

    Google Scholar 

  • Fox, S. W.: 1973, Origin of the Cell — Experiments and Premises,Naturwissenschaften60, 359–368.

    PubMed  Google Scholar 

  • Fripiat, J. J. and Toussaint, F.: 1963, Dehydroxylation of Kaolinite II Conductometric Measurements and IR Spectroscopy,J. Phys. Chem.67, 30–36.

    Google Scholar 

  • Fripiat, J. J. and Cruz-Cumplido, M. I.: 1974, Clays as Catalysts for Natural Processes,Ann. Rev. Earth and Planetary Science2, 239–256.

    Google Scholar 

  • Gable, N. W. and Ponnamperuma, C.: 1967, Model for the Origin of Monosaccharides,Nature216, 453–455.

    PubMed  Google Scholar 

  • Gate, L. F.: 1971, The Determination of Light Absorption in Diffusing Materials by a Photon Diffusion Model,J. Phys., D. Applied Physics4, 1049–1056.

    Google Scholar 

  • Gaultier, J. P. and Mamy, J.: 1979, in M. M. Mortland and V. C. Farmer (eds.), Evolution of Exchange Properties and Crystallographic Characteristics of Bi-Ionic K-Ca Montmorillionite Submitted to Alternate Wetting and Drying, International Clay Conference (1978) Oxford Developments in Sentimentology, Vol. 27, Elsevier, Amsterdam, pp. 167–177.

    Google Scholar 

  • Gibbs, D. Lohrmann, and Orgel, L. E.: 1980, Template Directed Synthesis and Selective Adsorption of Oligoadenylates on Hydroxyapatite,J. Mol. Evol.15, 347–354.

    PubMed  Google Scholar 

  • Gillespie, J. B., Lindberg, J. D., and Smith, M. S.: 1974, Visible and Near Infrared Absorption Coefficients of Montmorillonites and Related Clays,American Minerologist59, 1113–1116.

    Google Scholar 

  • Gratzel, M.: 1982, Efficient Water Cleavage by Visible Light in Colloidal Solutions of Bifunctional Redox Catalysts,ACS Symp. Ser.177, 113–138.

    Google Scholar 

  • Grim, R.: 1978,Clay Minerology, McGraw Hill.

  • Grimshaw, R. W.: 1971,The Physics and Chemistry of Clays and Allied Ceramic Materials, 4th Edition, Earnest Benn, Ltd.

  • Hall, P. L.: 1980, The Application of Electron Spin Resonance Spectroscopy to Studies of Clay Minerals I. Isomorphous Substitution and External Surface Properties,Clay Minerals15, 321–335.

    Google Scholar 

  • Hardy, G. F., Kaska, W. C., Chandra, B. P., and Zink, J. I.: 1981, Triboluminescence-Structure Relationships in Polymorphs of Hexaphenylcarbodiphosphorane and Anthranilic Acid, Molecular Crystals and Salts,J. Am. Chem. Soc.103, 1074–1079.

    Google Scholar 

  • Hardy, G. F., Baldwin, C. C., Zink, J. I., Kaska, W. C., Po Hsin, Liu, and Dubois, L.: 1977, Triboluminescence Spectroscopy of Aromatic Compounds,Journal of the American Chemical Society99, 3552–3558.

    Google Scholar 

  • Hartman, H.: 1975, Speculations on the Origin and Evolution of Metabolism,J. Mol. Evol.4, 359–370.

    PubMed  Google Scholar 

  • Hatanaka, H. and Egami, F.: 1977, The Formation of Amino Acids and Related Oligomers and Formaldehyde and Hydroxylamine in Modified Sea Mediums Related to Prebiotic Conditions,Bull., Chem. Soc. Japan50, 1147–1156.

    Google Scholar 

  • Henglein, A.: 1984, Catalysis of Photochemical Reactions by Colloidal Semiconductors,Pure and Appl. Chem.56, 1215–1224.

    Google Scholar 

  • Hubbard, J. S., Hardy, J. P., Voecks, G. E., and Golub, E. E.: 1973, Photocatalytic Synthesis of Organic Compounds from CO and Water: Involvement of Surfaces in the Formation and Stabilization of Products,J. Molec. Evol.2, 149–166.

    PubMed  Google Scholar 

  • Hughes, R. C.: 1979, Generation, Transport and Trapping of Excess Charge Carriers in Czochralski-grown Sapphire,Phys. Rev. B, Condensed Matter, 1.19, 5318–5328.

  • Huguenin, R. L.: 1973, Photostimulated Oxidation of Magnetite Kinetics and Alternation Phase Identification,Journal of Geophysical Research78, 8481–8493.

    Google Scholar 

  • Hunt and Salisbury: 1970: Visible and Near Infrared Spectra of Minerals and Rocks I Silicate Minerals,Modern Geology1, 283–300.

    Google Scholar 

  • Huntress, W. T., Jr.: 1977, Ion-Molecule Reactions in the Evolution of Molecules in Interstellar Clouds and Planetary Atmospheres,Chem. Soc., Rev.6, 295–323.

    Google Scholar 

  • Iler, R. K.: 1979,Chemistry of Silica, Solubility, Polymerization, Colloid and Surface Properties and Biochemistry, Wiley Interscience, New York.

    Google Scholar 

  • Ingmanson, D. E. and Dowler, M. J.: 1977, Chemical Evolution and the Evolution of the Earth's Crust,Origins of Life8, 221–224.

    PubMed  Google Scholar 

  • Jewett, D. and Lawless, J.: 1979, Detection of Activated Acyl Groups Formed by Heating Carboxylic Acids with Silica,Naturwissenschaften68S: 570–571.

    Google Scholar 

  • Karickhoff, S. W. and Bailey, C. W.: 1973, Optical Absorption Spectra of Clay Minerals,Clays and Clay Minerals21, 59–70.

    Google Scholar 

  • Karplus, M. and Porter, R. N.: 1970, InAtoms and Molecules, an Introduction for Students of Physical Chemistry, W. A. Benjamin, Menlo Park, Calif., p. 434.

    Google Scholar 

  • Kasting, J. F., Zahnle, K. J., and Walker, J. C. G.: 1983, Photochemistry of Methane in the Earth's Early Atmosphere,Precambrian Research20, 121–148.

    Google Scholar 

  • Katchalsky, A.: 1973, Prebiotic Synthesis of Biopolymers on Inorganic Templates,Die Naturwissenschaften60, 215–220.

    Google Scholar 

  • Kenyon, D. and Steinman, G.: 1969,Biochemical Predestination, McGraw-Hill, New York.

    Google Scholar 

  • Kliewer, K. L. and Koehler, J. S.: 1965, Space Charge in Ionic Crystals I, General Approach with Application to NaCl,Phys. Rev.140 (4a, 1226–1240.

    Google Scholar 

  • Knobel, R., Freund, F., Breuer, H., Schroeder, M., and Nitz, G.: 1983, Formation of Organic Molecules from Carbon, Hydrogen and Nitrogen Dissolved in Minerals. Abstract Cl-23 from the 7th International Conference on the Origins of Life and the 4th Meeting of the Society for the Study of the Origin of Life, held in Mainz, Federal Republic of Germany, July 10–15, 1983.

  • Knozinger, H. and Ratnasamy, P.: 1978, Catalytic Aluminas: Surface Models and Characterization of Surface Sites,Catal. Rev.: Sci. & Eng.17, 31–70.

    Google Scholar 

  • Kuroda, P. K.: 1979, Origin of the Elements pre-Fermi Reactor and Plutonium-244 in Nature,Accts. of Chem. Res.12, 73–78.

    Google Scholar 

  • Lahav, N. and Chang, S.: 1976, The Possible Role of Solid Surface Area in Condensation Reactions During Chemical Evolution: Reevaluation,J. Molec. Evol.8, 357–380.

    PubMed  Google Scholar 

  • Lahav, N. and Chang, S.: 1982, The Possible Role of Soluble Salts in Chemical Evolution,J. Molec. Evol.19, 36–46.

    PubMed  Google Scholar 

  • Lahav, N. and White, D. H.: 1980, A Possible Role of Fluctuating Clay-Water Systems in the Production of Ordered Prebiotic Oligomers,J. Molec. Evol.16, 11–21.

    PubMed  Google Scholar 

  • Lahav, N., Coyne, L., and Lawless, J.: 1982, Prolonged Triboluminescence, in Clays and Other Minerals,Clays and Clay Minerals30, 73–75.

    Google Scholar 

  • Lahav, N., White, D. H., and Chang, S.: 1978, Peptide Bond Formation in the Prebiotic Era: Thermal Condensation of Glycine in Fluctuating Clay Environments,Science201, 67–69.

    PubMed  Google Scholar 

  • Lee, K. H. and Crawford, J. H.: 1977, Electron Centers in Single Crystal Al2O3,Phys. Rev. B, Solid State15, 4065–4070.

    Google Scholar 

  • Lehninger, A. L.: 1970,Biochemistry: The Molecular Basis of Cell Structure and Function, 1st ed., Worth, New York.

    Google Scholar 

  • Lehovic, K.: 1953, Space Charge Layer and Distribution of Lattice Defects at the Surface of Ionic Crystals,J. Chem. Phys.21, 1123–1128.

    Google Scholar 

  • Lemons, K. and McAtee, J. L.: 1982, Induced Thermoluminescence of Some Clay Minerals,Clays and Clay Minerals30, 311–314.

    Google Scholar 

  • Lichtin, N. and Vijaykumar, K. M.: 1983, The Reduction of N2 and CO2 with the Aid of Solid Photocatalysts, Abstract No. 353, Pacific Conference on Chemistry and Spectroscopy, Pasadena, Calif., Oct. 26–28, 1983.

  • Lin, S. H., Wutz, D., Ho, Z. Z., and Eyring, H.: 1980, Mechanisms of Triboluminescence,Proc. Natl. Acad. of Scien.77, 1245–1247.

    Google Scholar 

  • Lindberg, J. D. and Smith, D. G.: 1974, Visible and Near Infrared Absorption Coefficients of Kaolinite and Related Clays,American Minerologist59, 274–299.

    Google Scholar 

  • Little, L. H.: 1966,Infrared Spectra of Adsorbed Species, Academic Press, London, 96–99.

    Google Scholar 

  • Maiti, G. C. and Freund, F.: 1981, Dehydration-related Proton Conductivity in Kaolinite,Clay Minerals16, 395–413.

    Google Scholar 

  • Marfunin, A. S.: 1979,Spectroscopy, Luminescence and Radiation Centers in Minerals (translated by V.V. Schiffer), Springer-Verlag, Berlin.

    Google Scholar 

  • Mason, B.: 1965,Principles of Geochemistry, 2nd ed., Ch. 3: The Structure and Composition of the Earth, pp. 28–66 (5th printing).

  • McBride, M.: 1979, Reactivity of Adsorbed and Structural Iron in Hectorite as Indicated by Oxidation of Benzidine,Clay and Clay Minerals27, 224–230.

    Google Scholar 

  • McBride, M. B. and Mortland, M. M.: 1974,Soil Sci. Soc. Am. Proc.38, 408–415.

    Google Scholar 

  • Miller, S. L. and Van Trump, J. E.: 1981, The Strecker Synthesis in the Primitive Ocean, in Y. Wolman (ed.),Origin of Life, D. Reidel, Dordrecht, Holland, pp. 135–141.

    Google Scholar 

  • Miller, S. L., Urey, H. C., and Oró, J.: 1976, Origin of Organic Compounds on the Primitive Earth and in Meteorities,J. Mol. Evol.9, 59–72.

    PubMed  Google Scholar 

  • Morrison, S. R.: 1980,Electrochemistry of Semiconductor and Oxidated Metal Electrodes, Plenum, N.Y.

  • Mortland, M. M.: 1984, Deamination of Glutamic Acid by CuII Smectite Catalysis,J. Molecular Catalysis27, 143–155.

    Google Scholar 

  • Mortland, M. M. and Halloran, L. J.: 1976, Polymerization of Aromatic Molecules on Smectite,Soil Sci. Soc., Am. J.40, 367–370.

    Google Scholar 

  • Myers, I. T.: 1968, Ionization, Ch. 7, in F. H. Attix and W. C. Roesch (eds),Radiation Dosimetry, Vol. I, Fundamentals, 2nd. ed., Academic Press, New York and London, pp. 325–328.

    Google Scholar 

  • Newman, M. J. and Rood, R. T.: 1977, Implications of Solar Evolution for the Earth's Early Atmosphere,Science198, 1035–1037.

    Google Scholar 

  • Newman, M. W., Neuman, W. F., and Lane, K.: 1970, On the Possible Roles of Crystals in the Origins of Life, IV — The phosphorylation of Nucleotides (and earlier papers),Currents in Modern Biology, North Holland Publishing Co., pp. 277–283.

  • Nishita, H. and Hamilton, M.: 1968, Some Thermoluminescent Characteristics of Gamma Irradiated Soils,Soil Science106, 76–84.

    Google Scholar 

  • Nishita, H. and Hamilton, M.: 1971, Spurious Thermoluminescence of Soils,Soil Science110, 371–378.

    Google Scholar 

  • Nishita, H. and Hamilton, M.: 1971, Influence of Temperature During the Gamma Irradiation Period on the Subsequent Thermoluminescence of Soils and LiF and CaF2 Dosimeters,Soil Science111, 393–395.

    Google Scholar 

  • Nishita, H. and Hamilton, M.: 1972, Soil Thermoluminescence in Relation to Radiation Exposure Under Field Conditions,Soil Science114, 430–439.

    Google Scholar 

  • Nishita, H. and Hamilton, M.: 1973, Effects of Some Chemical Treatment of Soils on Their Thermoluminescence,Soil Science115, 30–39.

    Google Scholar 

  • Nishita, H. and Hamilton, M.: 1975, Empirical Methods of Using Soils as Radiation Dosimeters,Soil Science120, 96–106.

    Google Scholar 

  • Nishita, H., Moore, R. H., Beckman, R. J., and Hamilton, M.: 1975, Decay Characteristics of Soil Thermoluminescence,Soil Science119, 259–268.

    Google Scholar 

  • Oparin, A. I.: 1957,The Origin of Life on Earth, 3rd Edition, translated by An Synge, Academic Press, New York.

    Google Scholar 

  • Paecht-Horowitz, M.: 1976, Clays as Possible Catalysts for Peptide Formation in the Prebiotic Era,Origins of Life7, 369–381.

    PubMed  Google Scholar 

  • Paecht-Horowitz, M., Gerger, J., and Katchalski, A.: 1970, Prebiotic Synthesis of Polypeptides by Heterogeneous Polycondensation of Amino Acid Adenylates,Nature228, 636–639.

    PubMed  Google Scholar 

  • Phillip, H. R.: 1966,Solid State Comm.4, 73.

    Google Scholar 

  • Pinnavaia, T. J.: 1983, Intercalated Clay Catalysts,Science220, 365–371.

    Google Scholar 

  • Ponnamperuma, C. and Chang, S.: 1971, The Role of Phosphates in Chemical Evolution, in R. Buvet and C. Ponnamperuma (eds.),Chemical Evolution and the Origin of Life, Proceedings of the 3rd International Conference on the Origin of Life, Pont-a-Mousson, France, 1970, North Holland Publishing Co., Amsterdam.

    Google Scholar 

  • Ponnamperuma, C., Shimoyama, A., and Friebele, A.: 1982, Clay and the Origin of Life,Origins of Life12, 9–40.

    PubMed  Google Scholar 

  • Powell, R. J. and Derbenwick, G. F.: 1971, Vacuum Ultraviolet Radiation Effects in SiO2,IEEE Trans. Nuc. Sci18, 99–105.

    Google Scholar 

  • Rao, M., Odom, D. G., and Oró, J.: 1980, Clays in Prebiotic Chemistry,J. Mol. Evol.15, 317–331.

    PubMed  Google Scholar 

  • Raulin, F.: 1981, Chemical Evolution in the Early Atmosphere of the Earth, Prebiotic Synthesis of Organic Precursors,Publication du Conseil de l'Europe 4AS/Science/CEP (32)1, 108–147, as presented at the Summer School ‘The Origins of and Early Evolution of Life’, Université d'Orleans, 17–20 September 1980.

  • Reid, C. and Orgel, L. E.: 1967, Synthesis of Sugars in Potentially Prebiotic Conditions,Nature216, 455.

    PubMed  Google Scholar 

  • Reilly, M. H.: 1970, Temperature Dependence of the Short Wavelength Transmittance Limit of Vacuum Ultraviolet Window Materials — II, Theoretical, Including Interpretations for U.V. Spectra of SiO2, GeO2 and Al2O3,J. Phys. Chem. Solids31, 1041–1056.

    Google Scholar 

  • Reisfeld, R.: 1983, Energy Transfer Between Dyes on Glass Surfaces and Ions in Glasses,Chemical Physics Letters95, 95–97.

    Google Scholar 

  • Rhodes, W.: 1979, Molecular Excited State Relaxation Processes,J. Chem. Ed.56, 562–567.

    Google Scholar 

  • Rideal, E. K.: 1968,Concepts in Catalysis, Academic Press, London and New York.

    Google Scholar 

  • Ring, D., Wolman, Y., Friedman, N., and Miller, S. L.: 1972, Prebiotic Synthesis of Hydrophobic and Protein Amino Acids,Proc. Nat. Acad. Sci. USA69, 765–768.

    PubMed  Google Scholar 

  • Robbins, D. W. and Strens, R. G. J.: 1972, Charge Transfer in Ferromagnesian Silicates: The Polarized Electronic Spectra of Trioctahedral Micas,Mminerological Magazine38, 551–563.

    Google Scholar 

  • Sanchez, R. A., Ferris, J. P., and Orgel, L. E.: 1967, Studies in Prebiotic Synthesis II, Synthesis of Purine Precursors and Amino Acids from Aqueous Hydrogen Cynanide,J. Molec. Biol.30, 223–252.

    PubMed  Google Scholar 

  • Schrauzer, G. W., Strampach, N., Liu, Nan Hu, Palmer, M. R., and Salehi, J.: 1983, Nitrogen Photoreduction on Desert Sands Under Sterile Conditions,Proc. Natl. Acad. Sci., USA80, 3873–3876 (Physical Sciences).

    Google Scholar 

  • Schwartz, A. W. and Goverde, M.: 1982, Acceleration of HCN Oligomerization by Formaldehyde and Related Compounds: Implications for Prebiotic Synthesis,J. Mol. Evol.18, 351–353.

    PubMed  Google Scholar 

  • Seigel, F. R., Vaz, J. E., and Ronca, L. B.: 1968, Thermoluminescence of Clay Minerals, Ch. 12,Thermoluminescence of Geological Materials, in D. J. McDougall (ed.), Proceedings of NATO Adv. Research Inst. on Applications of Thermoluminescence to Geological Problems, Academic Press, London, pp. 635–641.

    Google Scholar 

  • Smith, A., Folsome, C., and Bahadur, K.: 1981, Carbon Dioxide Reduction and Nitrogenase Activity in Organo-Molybdenum Microstructures,Experientia37, 357–359.

    PubMed  Google Scholar 

  • Somorjai, G. A.: 1972,Principles of Surface Chemistry, Prentice Hall, Englewood Cliffs, New Jersey.

    Google Scholar 

  • Swallow, A. J.: 1960,Radiation Chemistry of Organic Compounds, International Series of Monographs on Radiation Effects in Materials, V. 2, Pergamon Press, The Macmillan Co., New York, pp. 38, 244.

    Google Scholar 

  • Theng, B. K. G.: 1974,The Chemistry of Clay Organic Reactions, John Wiley and Sons, New York, pp. 274–281.

    Google Scholar 

  • Tite, M. S.: 1966, Thermoluminescent Dating of Ancient Ceramics: A Reassessment,Archaeometry9, 155.

    Google Scholar 

  • Towe, K. M.: 1981, Environmental Conditions Surrounding the Origin and Early Archean Evolution of Life: A Hypothesis,Precambrian Research16, 1–10.

    Google Scholar 

  • Trukhin, A. N.: 1980, Study of Excitons in SiO2 Luminescent Centers as Exciton Detectors,Phys. Stat. Solidi D98, 541–549.

    Google Scholar 

  • Van Olphen, H.:An Introduction to Clay Colloid Chemistry, Wiley Interscience, New York.

  • Van Olphen, H. and Fripiat, J. J.: 1979,Data Handbook for Clay Materials and Other Non-Metallic Minerals, Pergamon Press, Oxford, England.

    Google Scholar 

  • Verhoogen, J.: 1980,Energetics of the Earth, National Academy Press, N.A.S., 2101 Constitution Avenue, N.W., Washington, D.C. 20418.

  • Voet, A. B. and Schwartz, A. W.: 1981, HCN Oligomerization Isolation and Preliminary Characterization of a New Precursor of Adenine, in Y. Wolman (ed.),Origin of Life, D. Reidel, Dordrecht, Holland, pp. 217–223.

    Google Scholar 

  • Volkov, A. I. and Sazonov, L. A.: 1982, Influence of Molecular Nitrogen and Irradiation Temperature on Radiolysis of N2O-Al2O3,System Reac. Kinet. Catal. Lett.20, 289–292.

    Google Scholar 

  • Volkov, A. I., Volkova, G. G., Yermolaev, V. K., and Sazonov, L. A.: 1982, Resonance Energy Transfer from Al2O3 to Adsorbed N2O,Reaction Kinet. Catal. Lett.20, 283–288.

    Google Scholar 

  • Volodin, A. M. and Cherkashin, A. E.: 1982, ESR Studies of N2O Interaction with Photoinduced Centers of ZnO and MgO,Reaction Kinet. Catal. Lett.20, 335–338.

    Google Scholar 

  • Wakita, H., Nakamura, Y., Kito, I., Fugii, N., and Notsu, K. K.: 1980, Hydrogen Release, New Indicator of Fault Activity,Science210, 188–190.

    Google Scholar 

  • Weaver, C. E. and Pollard, L. D.: 1973,The Chemistry of Clay Minerals, Developments in Sedimentology, No. 15, Elsevier.

  • Weiss, A.: 1981, Replication and Evolution in Organic Systems,Angew Chem. Int. Ed. Eng.20, 850–860.

    Google Scholar 

  • White, D. H., Macklin, J., and Kennedy, R. M.: 1983, Acyl Silicates as Activated Intermediates in Peptide Bond Formation on Clays. Abstract No. C2-16 from the International Conference on the Origins of Life and the 4th Meeting of the International Society for the Study of the Origin of Life, Mainz, Federal Republic of Germany, July 10–15.

  • White, J. L.: 1968, Proton Migration in Kaolinite, 9th International Congress of Soil Science Transactions, Vol. 1, Paper No. 71, pp. 701–707.

  • Wrighton, M. S.: 1979, Photoelectrochemical Conversion of Optical Energy to Electricity and Fuels,Accounts of Chemical Research12, 303–310.

    Google Scholar 

  • Wrighton, M. S.: September 3, 1979, Photochemistry,Chemical and Engineering News57, 29–47.

    Google Scholar 

  • Yanigawa, H. and Egami, F.: 1978(a), in H. Noda (ed.),Origin of Life, Center for Academic Publishing, Japan, p. 385.

    Google Scholar 

  • Yanigawa, H. and Egami, F.: 1978(b), Studies on Chemical Evolution Using Carbon Suboxide, from Proceedings of the 11th Lunar and Planetary Symposium, Japan, July 1978, pp. 259–261, NASA TM-76590.

  • Zahnle, K. J. and Walker, J. C. G.: 1982, The Evolution of Solar Ultraviolet Luminosity,Rev. Geophys. Space Phys.20, 280–292.

    Google Scholar 

  • Zink, J. T.: 1978, Triboluminescence,Accounts of Chem. Res.11, 289–295.

    Google Scholar 

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Authors and Affiliations

  1. Dept. of Chemistry, San Jose State University, NASA Ames Research Center, Mail Stop 239-12, 94035, Moffett Field, CA, USA

    Lelia M. Coyne

Authors
  1. Lelia M. Coyne

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