2015
DOI: 10.1051/bioconf/20150400012
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Origins of life: From the mineral to the biochemical world

Abstract: Abstract.In this brief review, we summarize the most influential scenarios in origins-oflife studies that have resorted to minerals surfaces. The influence of the pre-existing mineral world on the organization of matter towards the living state may have manifested at several steps in the rise towards higher complexity. Small biomolecules such as amino acids formed on mineral surfaces of interstellar dust, meteorites or comets prior to their delivery to the primordial Earth. Mineral surfaces are known to promot… Show more

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Cited by 16 publications
(12 citation statements)
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“…The origin of life (or abiogenesis) is among the most intriguing questions in science [64]. Although it is not possible to know all the details of this process, some scientific hypotheses attempt to explain the synthesis of the molecules which were necessary for the emergence of primitive forms of life in planet Earth 3.8 billion years ago [65] as deriving from a reducing atmosphere (Miller's experiment [66]), meteorites impacts [67] or from metal sulfides in deep-sea hydrothermal vents, as explained in the famous article of Russel [68].…”
Section: The Role Of Clays In the Origin Of Lifementioning
confidence: 99%
“…The origin of life (or abiogenesis) is among the most intriguing questions in science [64]. Although it is not possible to know all the details of this process, some scientific hypotheses attempt to explain the synthesis of the molecules which were necessary for the emergence of primitive forms of life in planet Earth 3.8 billion years ago [65] as deriving from a reducing atmosphere (Miller's experiment [66]), meteorites impacts [67] or from metal sulfides in deep-sea hydrothermal vents, as explained in the famous article of Russel [68].…”
Section: The Role Of Clays In the Origin Of Lifementioning
confidence: 99%
“…The pores generated in minerals that precipitate at the contact of heated water vents with the surrounding ocean water would ensure the concentration of organic compounds by thermophoresis (Baaske et al, 2007). Porous structures generated by mineral sulphides created the conditions of protometabolism and protected the first proto-organisms of "dilution and other damage" (Lambert, 2015). Deamer et al (2006) believe that a more suitable environment for life emergence would be an aqueous phase with moderate temperature oscillations (below 60°C), a pH close to neutral and very low (submillimolar) concentrations of divalent cations.…”
Section: Formation Of Complex Organic Molecules and Macromoleculesmentioning
confidence: 99%
“…Ice appears to be the less effective protector since it is easily perishable by climatic warming. In regard to molecular biosignatures, molecular binding to minerals, like phyllosilicates [60,73,74] and Al-Fe oxyhydroxides [115], has shown to enhance preservation. Amorphous materials have also demonstrated some preservation potential that can be ascribed to the possibility to incorporate and protect molecules within their porous structure.…”
Section: Preservation Of Biosignaturesmentioning
confidence: 99%