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Three stages of the origin of life process: bifurcation, stabilization and inversion

Published online by Cambridge University Press:  04 January 2008

V.N. Kompanichenko
Affiliation:
Institute for Complex Analysis, 4 Sholom-Aleyhem Street, Birobidzhan 679016, Russia Department of Chemistry and Biochemistry, University of California, 1156 High Street, Santa Cruz CA 95064, USA e-mail: kompanv@yandex.ru

Abstract

The principal succession of transformations of a prebiotic microsystem leading to its transition into the primary living state is theoretically substantiated. For the first stage of the succession, a significant change in the external conditions constrains an organic microsystem to leave the current stable state with the following transition into a new stable state through the unstable critical (bifurcation) point. At the bifurcation point the microsystem acquires the original properties without which life cannot exist (self-maintaining heterogeneous structure, incessant fluctuations and rearrangement of molecules, exchange with the surroundings by matter and energy, etc.). During the second stage its unstable state stabilizes relatively by means of the balanced oscillations around the bifurcation point (the paradoxical state of ‘stabilized instability’ appears). The third stage is characterized with the radical turn in the network of chemical reactions: the free energy contribution begins to prevail over the entropy contribution. As a result, constructive transformations proceed faster than destructive transformations. At this stage the key properties of biological organization appear: the ability to concentrate free energy and information, intensified counteraction to external influences, expedient behaviour and persistent self-renovation. On the early Earth, such successive transformation of organic matter occurred in the changeable conditions of a hydrothermal medium. Some new methods for experimental and theoretical research in the origin of life field are suggested.

Type
Research Article
Copyright
Copyright © Cambridge University Press 2008

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References

Baltscheffsky, H. (1997). Major ‘anastrophes’ in the origin and early evolution of biological energy conversion. J. Theor. Biol. 187, 495501.CrossRefGoogle ScholarPubMed
Chaussidon, M. & Franquis, R. (2006). Constrains from silicon isotopic compositions on seawater temperature in the Archaean. Abstracts of 6th European Workshop on Astrobiology, Lyon, France.Google Scholar
Corliss, J.B., Baross, J.A. & Hoffman, S.E. (1981). An hypothesis concerning the relationship between submarine hot springs and the origin of life on the Earth. Oceanol. Acta SP4, 5969.Google Scholar
Deamer, D.W. (1986). Role of amphiphilic compounds in the evolution of membrane structure on early Earth. Origins Life 17, 325.CrossRefGoogle ScholarPubMed
Deamer, D.W. (2004). Prebiotic amphiphilic compounds. Origins, ed. Seckbach, J. Kluwer, Dordrecht, pp. 7589.CrossRefGoogle Scholar
Ehrenfreund, P., Rasmussen, S., Cleaves, J. & Chen, L. (2006). Experimentally tracing the key steps in the origin of life: the aromatic world. Astrobiology 6(3), 490520.CrossRefGoogle ScholarPubMed
Fox, S. & Dose, K. (1977). Molecular Evolution and the Origin of Life. Dekker, New York.Google Scholar
Fox, S., Balin, P., Pappelis, A. & Yu, B. (1996). Experimental retracement of terrestrial origin of an excitable cell: was it predictable? Chemical Evolution: Physics of the Origin and Evolution of Life, eds Chela-Flores, J. & Raulin, F., pp. 2132. Kluwer, Dordrecht.CrossRefGoogle Scholar
Gilbert, W. (1986). The RNA World. Nature 319, 618.CrossRefGoogle Scholar
Haken, H. (1978). Synergetics. Springer, Berlin.CrossRefGoogle Scholar
Holm, N. & Andersson, E. (2005). Hydrothermal simulation experiments as a tool for studies for the origin of life on Earth and other terrestrial planets: a review. Astrobiology 5(4), 444460.CrossRefGoogle ScholarPubMed
Holm, N. et al. (2006). Alkaline fluid circulation in ultramafic rocks and formation of nucleotide constituents: a hypothesis. Geochem. Trans. 7(7), 113.CrossRefGoogle ScholarPubMed
Huxley, I.S. (1942). Evolution: the Modern Synthesis. George Allen and Unwin, London.Google Scholar
Joice, G.F. & Orgel, L.E. (1993). Prospects for understanding the origin of the RNA world. The RNA World. pp. 125. Gold Spring Harbor Laboratory Press, New York.Google Scholar
Knauth, L.P. (1992). Origin and diagenesis of cherts: an isotopic perspective. Isotopic Signatures and Sedimentary Records (Lecture Notes in Earth Sciences, No 43), eds Clanet, N. & Chaudhuri, S., pp. 123152. Springer, Heidelberg.CrossRefGoogle Scholar
Knauth, L.P. & Lowe, D.R. (2003). High Archaean climatic temperature inferred from oxygen isotope geochemistry of cherts in the 3.5 Ga Swaziland Supergroup, South Africa. Geol. Soc. Amer. Bull. 115(5), 566580.2.0.CO;2>CrossRefGoogle Scholar
Kompanichenko, V.N. (1996). Transition of precellular organic microsystems to a biotic state: environment and mechanism. Nanobiology 4, 3945.Google Scholar
Kompanichenko, V.N. (2002). Life as high-organized form of the intensified resistance to destructive processes. Fundamentals of Life, eds Palyi, G., Zucci, C. & Caglioti, L., pp. 111124. Elsevier SAS, Paris.Google Scholar
Kompanichenko, V.N. (2003). Distinctive properties of biological systems: the all-round comparison with other natural systems. Frontier Perspectives 12(1), 2335.Google Scholar
Kompanichenko, V.N. (2004). Systemic approach to the origin of life. Frontier Perspectives 13(1), 2240.Google Scholar
Kompanichenko, V., Frisman, E., Fishman, B., Savenkova, E. & Shlufman, K. (2007). Exploration of thermodynamic fluctuations in the probable hydrothermal medium for the origin of life (on the example of Mutnovsky hydrothermal system in Kamchatka). Int. J. Astrobiol. 6(1), 74.Google Scholar
Kralj, Pt. & Kralj, Pol. (2000). Thermal and mineral waters in north-eastern Slovenia. Environ. Geol. 39(5), 488498.CrossRefGoogle Scholar
Luisi, P.L. (2000). The relevance of supramolecular chemistry for the origin of life. Adv. Supramol. Chem. 6, 287307.CrossRefGoogle Scholar
Nicolis, G. & Prigogine, I. (1977). Self-Organization in Nonequilibrium Systems. Wiley, New York.Google Scholar
Onsager, L. (1931). Reciprocal relations in irreversible processes. Phys. Rev. 38(12), 2265.CrossRefGoogle Scholar
Oparin, A.I. (1957). Origin of Life on the Earth. Nauka, Moscow.Google Scholar
Palyi, G., Zucci, C. & Caglioti, L. (eds) (2002). Fundamentals of Life. Elsevier SAS, Paris.Google Scholar
Prigogine, I. & Stengers, I. (1984). Order out of Chaos. Bantam, New York.Google Scholar
Russell, M.J., Hall, A.J., Boyce, A.J. & Fallick, A.E. (2005). On hydrothermal convection and the emergence of life. Econ. Geol. 100, 419438.Google Scholar
Schidlowski, M. (1997). Carbon isotopes and the oldest record of life: potential and limits. SPIE 3111, 462471.Google Scholar
Schwartzman, D.W. & Lineweaver, C.H. (2004). The hyperthermophilic origin of life revisited. Biochem. Soc. Trans. 32(2), 168171.CrossRefGoogle ScholarPubMed
Schopf, J.W., Kudryavtsev, A.B., Argesti, D.G., Wdowiak, T.G. & Czaja, A.D. (2002). Laser-Raman imagery of Earth's earliest fossils. Nature 416, 7376.CrossRefGoogle ScholarPubMed
Selye, H. (1974). Stress without distress. J.B. Lippincott Company, Philadelphia.Google Scholar
Stetter, K.O. (1995). Microbial life in hyperhermal environments. ASM News 61(6), 328340.Google Scholar
Westall, F. et al. (2006). The 3.466 Ga ‘Kitty's gap Chert’ an early Archaean microbial ecosystem. Processes on the Early Earth, vol. 405, eds Reymond, W.U. and Gibson, R.L., pp. 105131. Geological Society of America.Google Scholar
Woese, C.R. (1987). Microbial evolution. Microbial. Rev. 51, 221270.CrossRefGoogle Scholar
Wong, J.T.-F. & Xue, H. (2002). Self-perfecting evolution of heteropolymer building blocks and sequences as the basis of life. Fundamentals of Life, eds Palyi, G., Zucci, C. & Caglioti, L., pp. 473494. Elsevier SAS, Paris.Google Scholar
Xue, H., Tong, K.-L., Marck, C., Grosjean, H. & Wong, J.T.-F. (2003). Transfer RNA paralogs: evidence for genetic code-amino acid biosynthesis coevolution and an archaean root of life. Gene 310, 5966.CrossRefGoogle Scholar