N-CARBAMOYL-ALPHA-AMINO ACIDS RATHER THAN FREE ALPHA-AMINO-ACIDS FORMATION IN THE PRIMITIVE HYDROSPHERE - A NOVEL PROPOSAL FOR THE EMERGENCE OF PREBIOTIC PEPTIDES
J. Taillades et al., N-CARBAMOYL-ALPHA-AMINO ACIDS RATHER THAN FREE ALPHA-AMINO-ACIDS FORMATION IN THE PRIMITIVE HYDROSPHERE - A NOVEL PROPOSAL FOR THE EMERGENCE OF PREBIOTIC PEPTIDES, Origins of life and evolution of the biosphere, 28(1), 1998, pp. 61-77
Our previous kinetic and thermodynamic studies upon the reactional sys
tem HCHO/HCN/NH3 in aqueous solutions are completed. In the assumed pr
ebiotic conditions of the primitive earth ([HCHO] and [HCN] near 1 g L
-1, T = 25 degrees C, pH = 8, [NH3] very low), this system leads to 99
.9% of alpha-hydroxyacetonitrile and 0.1% of alpha-aminoacetonitrile (
precursor of the alpha-amino acid). The classical base-catalyzed hydra
tion of nitriles, slow and not selective, can not modify significantly
this proportion. On the contrary, we found two specific and efficient
reactions of alpha-aminonitriles which shift the initial equilibrium
in favor of the alpha-aminonitriie pathway. The first reaction catalyz
ed by formaldehyde generates alpha-aminoamides, precursors of alpha-am
inoacids. The second reaction catalyzed by carbon dioxide affords hyda
ntoins, precursors of N-carbamoyl-alpha-aminoacids. In the primitive h
ydrosphere, where the concentration in carbon dioxide was estimated to
be higher than that of formaldehyde, the formation of hydantoins was
consequently more efficient. The rates of hydrolysis of the alpha-amin
oacetamide and of the hydantoin at pH 8 being very similar, the synthe
sis of the N-carbamoyl-alpha-amino acid seems then to be the fatal iss
ue of the HCHO/HCN/NH3 system that nature used to perform its evolutio
n. These N-protected alpha-amino acids offer new perspectives in prebi
otic chemistry, in particular for the emergence of peptides on the pre
biotic earth.