作者: Vicente Marcano , Pedro Benitez , Ernesto Palacios-Prü
DOI: 10.1007/978-94-011-4313-4_27
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摘要: The origin of life is hardly understandable in the adverse conditions early Earth (Maher & Stevenson 1988, Zahnle Sleep 1997) unless formation different lengths carbon compounds, as well amino acids and primitive nucleobases aggregates, are conceived under effect a protective mechanism (Miller Bada et al. 1995, Levy Miller 1998). However, temperatures ≤ 350°C were possible 3600 Myr ago due to multiple impacts ~ 14 km bolides (Lyons Vasavada 1999) CO2 greenhouse effects (Kasting Ackerman 1986). During this age, hydrophobic coats alkanes ≥ n-C18 could served allowed yield long molecules avoiding its hydrolysis (Marcano 1999).