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    Oparin-Haldane Theory

    Working independently, in the 1920s, Aleksandr Oparin and J. B. S. Haldane proposed similar theoretical schemes for how life may have originated on Earth (see life, origin). Hence, the term "Oparin-Haldane Theory" is sometimes used when referring to their views. The main similarities and differences between Oparin's and Haldane's suggestions are summarized below.


      Oparin Haldane
    primitive atmosphere Reducing, composed of methane, ammonia, hydrogen and water vapor Reducing, composed of carbon dioxide, ammonia and water vapor
    source of carbon for life Methane Carbon dioxide
    site of prebiotic evolution Atmosphere, then oceans Atmosphere, then oceans
    mechanism Spontaneous appearance of coacervates followed by evolution to cell-like state Synthesis of increasingly complex organic molecules in presence of ultraviolet light


    Related category

       • ORIGIN AND EVOLUTION OF LIFE




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