US EPA

604620 

Journal Article 

Prebiotic chemistry: chemical evolution of organics on the primitive Earth under simulated prebiotic conditions 

Dondi, D; Merli, D; Pretali, L; Fagnoni, M; Albini, A; Serpone, N 

2007 

1 

Photochemical and Photobiological Sciences
ISSN: 1474-905X
EISSN: 1474-9092 

6 

11 

1210-1217 

English 

17973054 

10.1039/b709813h 

WOS:000250589200019 

A series of prebiotic mixtures of simple molecules, sources of C, H, N, and O, were examined under conditions that may have prevailed during the Hadean eon (4.6-3.8 billion years), namely an oxygen-free atmosphere and a significant UV radiation flux over a large wavelength range due to the absence of an ozone layer. Mixtures contained a C source (methanol, acetone or other ketones), a N source (ammonia or methylamine), and an O source (water) at various molar ratios of C:H:N:O. When subjected to UV light or heated for periods of 7 to 45 days under an argon atmosphere, they yielded a narrow product distribution of a few principal compounds. Different initial conditions produced different distributions. The nature of the products was ascertained by gas chromatographic-mass spectral analysis (GC-MS). UVC irradiation of an aqueous methanol-ammonia-water prebiotic mixture for 14 days under low UV dose (6 x 10(-2) Einstein) produced methylisourea, hexamethylenetetramine (HMT), methyl-HMT and hydroxy-HMT, whereas under high UV dose (45 days; 1.9 x 10(-1) Einstein) yielded only HMT. By contrast, the prebiotic mixture composed of acetone-ammonia-water produced five principal species with acetamide as the major component; thermally the same mixture produced a different product distribution of four principal species. UVC irradiation of the CH3CN-NH3-H2O prebiotic mixture for 7 days gave mostly trimethyl-s-triazine, whereas in the presence of two metal oxides (TiO2 or Fe2O3) also produced some HMT; the thermal process yielded only acetamide.