Although the origin of life has been traditionally placed in water, this gi
ves rise to a number of thermodynamical problems. The hypothesis advanced i
n this work is that the first steps towards life took place in the hydrocar
bon layer that presumably covered the surface of the primordial ocean. Here
hydrophobic amino acids might have found a thermodynamically suitable ambi
ent where to concentrate and polymerize. Moreover, the low dielectric const
ant of such a hydrophobic superficial layer might have favoured possible el
ectrostatic interactions among peptidic chains. We suggest that this might
have constituted a thermodynamically favourable basis for the development o
f organized molecular systems.