Possible impact of a primordial oil slick on atmospheric and chemical evolution

Frans Peder Nilson

Research output: Contribution to journalArticlepeer-review

28 Citations (SciVal)

Abstract

Low molecular weight liquid hydrocarbons from various sources, could have formed an oil layer covering the primeval ocean (present already 4.0-4.4 x 10(9) yr ago), preventing water from evaporating into the atmosphere. Water from other sources, precipitated by cold traps at higher altitude in the atmosphere, becomes trapped in the ocean. In a thereby more dry and presumably reducing atmosphere (before 3.9 x 10(9) yr ago) even more hydrocarbons, as well as reactive molecules will form. An oil layer can possibly act as a dry solvent for reactions, where the reactive molecules can produce monomers and condensing agents. Monomers and eventual polymers formed could become strongly concentrated at the oil-water interface, favouring molecular interactions at high mobility and low dilution, without exposure to the destructive action of UV-light. Increased water leakiness of the oil layer due to accumulation of polar molecules within, would lead to photo-oxidation of liquid hydrocarbons, and subsequent emulsification at the oil-water interface, forming cellular structures. The atmosphere would then have lost its reducing character.
Original languageEnglish
Pages (from-to)247-253
JournalOrigins of Life and Evolution of the Biosphere
Volume32
Issue number3
DOIs
Publication statusPublished - 2002

Subject classification (UKÄ)

  • Industrial Biotechnology

Keywords

  • reducing
  • oil layer
  • molecular interactions
  • dry solvent
  • hydrocarbons
  • atmosphere

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