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By working with the simplest amino acids and elementary RNAs, physicists led by Rockefeller University's Albert J. Libchaber, head of the Laboratory of Experimental Condensed Matter Physics, have now generated the first theoretical model that shows how a coded genetic system can emerge from an ancestral broth of simple molecules.

The scientists suggest that life on Earth originated at photosynthetically-active porous structures, similar to deep-sea hydrothermal vents, made of zinc sulfide (more commonly known as phosphor). They argue that under the high pressure of a carbon-dioxide-dominated atmosphere, zinc sulfide structures could form on the surface of the first continents, where they had access to sunlight.

All of which could lend credence to the suggestion of biochemist Lawrence Henderson in 1913 that water is peculiarly favourable to the evolution of life. In the introduction to a 1958 edition of Henderson's book, Wald wrote 'we now believe that life… must arise inevitably wherever it can, given enough time.' But perhaps what it needs is not so much enough time, but the right amount of heat.