Abstract

It is now widely speculated that life originated at the “Black Smokers” of the undersea hydrothermal vents, where conditions exist for the formation of the primary ingredients and their subsequent transformation to higher biotic species such as amino acids, alcohols, etc. Any possible routes for the prebiotic oligomerization of simple compounds like amino acids, necessary for cell formation, has so far not been well understood. However, Leman et al. recently reported that under standard laboratory conditions carbonyl sulfide (COS) can “mediate” the oligomerization of simple amino acids in moderate yield. COS being a well-known volcanic gas points to its possible role in prebiotic peptide formation in the environment of the hydrothermal vents. Based on a previously developed and tested model for selective (vibrational) energy transfer (SET), we show that a COS-catalyzed condensation of α-amino-acids can lead to the formation of polypeptides. We also indicate that other agents can act as catalysts of the amino acid condensation, such as Fe(CN)63− and cyanamide (H2N-CN). This is related to the existence of vibrations with a frequency near to that of the critical vibration of the reactant, ρw (NH2). This wagging vibration occurs at 1048 ± 10 cm−1 (the mean value of Cu and Ni complexes) and, as the vibration of the presumed catalyst lies at 2079 cm−1, one notes that one quantum of the catalyst equals two quanta of the NH2 wagging: 2079/2 × 1048 = 0.9919. This is a good indication of a resonance.

Highlights

  • Among the chemical reactions of direct importance for life is the condensation of amino acids to give polypeptides or proteins

  • In volcanic eruptions [9], which in turn gave the catalyst a load of energy from the start. Such a reaction must have been conditioned by taking place in confined and restricted environments where selective catalyzed chemical reactions could proceed, forming progressively higher oligomeric chemicals

  • We suggest that the amino acid that reacts is the one that has a –COOH group firmly bonded to the metal atom as COO−

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Summary

Introduction

Among the chemical reactions of direct importance for life is the condensation of amino acids to give polypeptides or (depending on size) proteins. This is not an arbitrary choice; rather, we chose COS for two reasons, the first being the very strong infrared absorption of one of the three fundamental vibrations, at 2079 cm−1 [6,7], and the consequential strong emission [8] of importance for the catalytic process; the other reason is the appearance of COS in volcanic eruptions [9], which in turn gave the catalyst a load of energy from the start Such a reaction must have been conditioned by taking place in confined and restricted environments (e.g., the hydrothermal vents in mid-ocean ridges discovered in the 1970s) where selective catalyzed chemical reactions could proceed, forming progressively higher oligomeric chemicals. One can state that the SET model works well [19]

Peptide Bond Formation
COS and Resonance Conditions
Further Tests of SET Catalysis
Cyanamide Test
Conclusions
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