| Abstract: | It is well-known that in water phosphate readily reacts with calcium, precipitating as insoluble apatite. How phosphorus could have been available for prebiotic reactions is still an open problem. We suggest that phosphorus-containing compounds might have accumulated in a hydrophobic medium, since the absence of calcium ions would have prevented them from precipitating as apatite. Hydrophobic compounds may have been synthesized on the early Earth through the polymerization of methane or through Fischer-Tropsch-type reactions. Moreover, hydrophobic compounds would have been delivered to the early Earth by extraterrestrial infall. In previous articles (Morchio and Traverso 1999], Morchio et al. 2001]) we suggested that such hydrophobic material would have formed a hydrophobic layer on the surface of the sea, which would have provided an environment thermodynamically more suitable than water for the concentration and polymerization of organic molecules fundamental to life, particularly amino acids and (pyrimidine) bases. It may be hypothesized that elemental phosphorus or phosphorus-containing compounds (such as phosphite) deriving from volcanic eruptions would have ended up raining down into the hydrophobic layer, accumulating due to the absence of calcium ions, in an environment protected against hydrolysis. Phosphorus-containing compounds might have interacted with hydrophobic molecules in the layer giving rise to polymers. In particular, phosphite might have reacted with the hydrophobic amino acids, giving rise to phosphoamino acids, which, in turn, might have interacted with pyrimidine bases (relatively abundant in the layer) giving rise to peptides and oligonucleotide-like polymers. Indeed, it has been experimentally shown (Zhou et al. 1996]) that, in an anhydrous organic medium (pyridine), dialkilphosphite reacts with amino acids to form phosphoamino acids, which interact with pyrimidine nucleosides to give nucleotides, short oligonucleotides and phosphoryl peptides. |
