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  • Abiogenesis
  • Springer  (2)
  • MDPI Publishing
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  • Springer  (2)
  • MDPI Publishing
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  • 1
    Publication Date: 2020-10-20
    Description: Pyrite and organic matter closely coexist in some hydrothermally-altered gabbroic xenoliths from the Hyblean Plateau, Sicily. The representative sample consists of plagioclase, Fe-oxides, clinopyroxene, pyrite and minor amounts of many other minerals. Plagioclase displays incipient albitization, clinopyroxene is deeply corroded. Pyrite grains are widely replaced by spongy-textured magnetite, which locally hosts Ca-(and Fe-)sulfate micrograins and blebs of condensed organic matter. Whole-rock trace element distribution evidences that incompatible elements, particularly the fluid-mobile Ba, U and Pb, are significantly enriched with respect to N-MORB values. The mineralogical and geochemical characteristics of the sample, and its U-Pb zircon age of 216.9 ± 6.7 MA, conform to the xenolith-based viewpoint that the unexposed Hyblean basement is a relict of the Ionian Tethys lithospheric domain, mostly consisting of abyssal-type serpentinized peridotites with small gabbroic intrusions. Circulating hydrothermal fluids there favored the formation of hydrocarbons trough Fischer-Tropsch-type organic synthesis, giving also rise to sulfidization episodes. Subsequent variations in temperature and redox conditions of the system induced partial de-sulfidization, Fe-oxides precipitation and sulfate-forming reactions, also promoting poly-condensation and aromatization of the already-formed hydrocarbons. Here we show organic matter adhering to a crystal face of a microscopic pyrite grain. Pyrite surfaces, as abiotic analogues of enzymes, can adsorb and concentrate organic molecules, also acting as catalysts for a broad range of proto-biochemical reactions. The present data therefore may support established abiogenesis models suggesting that pyrite surfaces carried out primitive metabolic cycles in suitable environments of the early Earth, such as endolithic recesses in mafic rocks permeated by hydrothermal fluids.
    Description: Published
    Description: 19-47
    Description: 4V. Processi pre-eruttivi
    Description: JCR Journal
    Keywords: Abiogenesis ; FTT synthesis ; Hydrothermal system ; Pyrite ; Sicily ; Xenoliths
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    ISSN: 1432-1432
    Keywords: Abiogenesis ; Photocatalytic ; Surface Catalysis ; Ultraviolet Photosynthesis ; Chemical Evolution ; Mars
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary 14C-Formic acid and other14C-organic compounds are formed on surface materials when mixtures of14CO,12CO2 or N2 and water vapor are irradiated with ultraviolet light (UV) ofλ 〉 250 nm. The rate of organic formation is roughly proportional to the quantity of substratum irradiated. The available evidence suggests that14CO adsorbed to or in contact with the substratum is excited by the long wavelength UV and reacts with adsorbed H2O or surface hydroxyl groups yielding the organic products. Photodestruction of the14C-organics yields14CO2 and14CO. A steady state is attained when organic products reach a concentration such that the rate of photodestruction is equal to the rate of synthesis. The product accumulation is greater and the photodestruction is slower when N2 is used as diluent gas. Differences in the rates of synthesis, rates of photodestruction and amounts of product accumulation are observed with different silica and alumina substrata. The substrata with large surface areas are most effective for synthesis while maximum photoprotection of organics is afforded by substrata containing high concentrations of surface hydroxyl groups. The observation of the synthesis on a variety of substrata using realistic simulations of atmospheres and solar energies strengthens previous proposals that this process may occur on Mars and may have been important on the primitive Earth.
    Type of Medium: Electronic Resource
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