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Polypeptide formation on polar mineral surfaces: possibility of complete chirality

Published online by Cambridge University Press:  23 November 2015

Malcolm E. Schrader*
Affiliation:
Institute of Chemistry, Hebrew University of Jerusalem, Jerusalem, Israel

Abstract

In the present work, it is shown that thermodynamically feasible polymerization of cyanomethanol, which can be formed from formaldehyde and hydrogen cyanide, can lead to synthesis of polypeptides as well as to the previously reported synthesis of RNA. If the polymerization takes place on a one-dimensional feature of a mineral, such as for example a crack on its surface, the concept of quasi-chirality is introduced to describe the adsorbed polypeptide. This, in principle, would lead to formation of proteins that are completely homochiral in their alpha carbon groups. The concept of quasi-chirality can also be introduced in the condensation of glycine under similar conditions to form a polypeptide. This again leads to proteins completely chiral in their alpha carbon groups.

Type
Research Article
Copyright
Copyright © Cambridge University Press 2015 

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References

Bonner, W.A. (1991). The origin and amplification of biomolecular chirality. Orig. Life Evol. Biosph. 21, 59111.Google Scholar
Bonner, W.A. (1992). Terrestrial and extraterrestrial sources of molecular homochirality. Orig. Life Evol. Biosph. 21, 407420.Google Scholar
Bonner, W.A. (1995). Chirality and life. Orig. Life Evol. Biosph. 25, 59111.Google Scholar
Ferris, J.P. (1992). Chemical markers of prebiotic chemistry in hydrothermal systems. Orig. Life Evol. Biosph. 22, 109134.Google Scholar
Ferris, J.P. (2005). Mineral catalysis and prebiotic synthesis: montmorillonite-catalyzed formation of RNA. Elements 1, 145149.Google Scholar
Ferris, J.P. & Ertem, G. (1993). Montmorillonite catalysis of RNA oligomer formation in aqueus solution- a model for the prebiotic formation of RNA. J. Am. Chem. Soc. 115, 1227012275.Google Scholar
Gilbert, W. (1986). The RNA world. Nature 319, 618.Google Scholar
Goldschmidt, V.M. (1952). Geochemical aspects of the origin of complex organic molecules on the earth, as precursors to organic life. New Biol. 12, 97105.Google Scholar
Hazen, R.M. (2001). Life's rocky start. Sci. Am. 284(4), 6371.Google Scholar
Hazen, R.M. (2006). Mineral surfaces and the prebiotic selection and organization of biomolecules. Am. Mineral. 91, 17151729.Google Scholar
Hazen, R.M. & Sholl, D.S. (2003). Chiral selection on inorganic crystalline surfaces. Nat. Mater. 2, 367374.Google Scholar
Hennet, R.J.-C., Holm, N.G. & Engel, M.H. (1992). Abiotic synthesis of amino acids under hydrothermal conditions and the origin of life: a perpetual phenomenon. Naturwissenschaften 79, 361365.Google Scholar
Hill, A.R. Jr., Bohler, C. & Orgel, L.E. (1998). Polymerization on the rocks: negatively charged amino acids. Orig. Life Evol. Biosph. 28, 227.Google Scholar
Liu, R. & Orgel, L.E. (1998). Polymerization on the rocks: beta amino acids and arginine. Orig. Life Evol. Biosph. 28, 245257.Google Scholar
Lahav, N., White, D. & Chang, S. (1978). Peptide formation in the prebiotic era. Thermal condensation of glycine in fluctuating clay environment. Science 201, 6769.Google Scholar
Lane, N. (2011). Energetics and genetics across the prokaryote-eukaryote divide. Biol. Direct. 6, 35.Google Scholar
Martin, R.B. (1998). Free energies and equilibria of peptide bond hydrolysis and formation. Biopolymers 45, 351353.Google Scholar
Mayr, E. (1982). The Growth of Biological Thought. Harvard University Press, Cambridge.Google Scholar
Miller, S.L. (1953). A production of amino acids under possible primitive earth conditions. Science 117, 528.Google Scholar
Miller, S.L. (1955). Production of some organic compounds under possible primitive earth conditions. J. Am. Chem. Soc. 77, 23512361.Google Scholar
Mukhin, L.M. (1974). Evolution of organic compounds in volcanic regions. Nature 251, 5051.Google Scholar
Oparin, A.I. (1938). The Origin of Life, Macmillan, NY. Morgulis, S. (trans.).Google Scholar
Palyi, G., Zucchi, C. & Caglioti, L. (eds) (1999). Advances Biochirality, Elsevier, NY.Google Scholar
Pinto Joseph, P., Gladstone, G.R. & Yung, Y.L. (1980). Photochemical production of formaldehyde in earth's primitive atmosphere. Science 210, 183185.Google Scholar
Rimola, A., Ugliengo, P. & Sodupe, M. (2004). Formation versus hydrolysis of the peptide bond from a quantum mechanical viewpoint: the role of mineral surfaces and implications for the origin of life. Int. J. Mol. Sci. 10(3) 746760.Google Scholar
Schrader, M.E. (1968). Ultrahigh vacuum techniques in the measurement of contact angles. Methylene iodide on glass. J. Colloid Interface Sci. 27, 743750.Google Scholar
Schrader, M. E. (2006). Is life on Earth accidental? Natural selection and the second law of thermodynamics. In: Life as We Know it, ed. Seckback, J., Springer, Dordrecht, pp. 163178.Google Scholar
Schrader, M.E. (2009). The RNA world: conditions for prebiotic synthesis. J. Geophys. Res. 114, D15305.Google Scholar
Schrader, M.E. & Yariv, S. (1990). Wettability of clay minerals. J. Colloid Interface Sci. 136, 8594.Google Scholar
Smith, J.V. (1998). Biochemical evolution. 1. Polymerization on internal organophilic silica surfaces of dealuminated zeolites and feldspars. Proc. Natl. Acad. Sci. USA 95, 33703375.Google Scholar
Yariv, S. (1992). Wettability of clay minerals. In Modern Approaches to Wettability: Theory and Applications, ed. Schrader, M. E. & Loeb, G. I., Plenum Press, NY.Google Scholar
Zahnle, K.J. (1986). Photochemistry of methane and the formation of hydrocyanic acid (HCN) in the Earth's early atmosphere. J. Geophys. Res. 91, 28192834.Google Scholar