4.4 Article

Experimental and Theoretical Constraints on Amino Acid Formation from PAHs in Asteroidal Settings

Journal

ACS EARTH AND SPACE CHEMISTRY
Volume 6, Issue 3, Pages 468-481

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/acsearthspacechem.1c00329

Keywords

Polycyclic Aromatic Hydrocarbons; Amino Acids; Aqueous Alteration; Carbonaceous Chondrites; Meteorites; Equilibrium Thermodynamics

Funding

  1. Spinoza Prize
  2. NASA Astrobiology Institute [13-13NAI70032]
  3. Simons Foundation [302497]
  4. French government through the 3IA Cote d'Azur Investments [ANR-19-P3IA0002]
  5. European Union [819588]
  6. European Research Council (ERC) [819588] Funding Source: European Research Council (ERC)

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This study empirically and theoretically investigates whether polycyclic aromatic hydrocarbons (PAHs) are precursors to amino acids in carbonaceous chondrites. While the experiments did not show the formation of amino acids, the theoretical results suggest that PAHs could serve as precursors to amino acids at low temperatures.
Amino acids and polycyclic aromatic hydrocarbons (PAHs) belong to the range of organic compounds detected in meteorites. In this study, we tested empirically and theoretically if PAHs are precursors for amino acids in carbonaceous chondrites, as previously suggested. We conducted experiments to synthesize amino acids from fluoranthene (PAH), with ammonium bicarbonate as a source for ammonia and carbon dioxide under mimicked asteroidal conditions. In our thermodynamic calculations, we extended our analysis to additional PAH-amino acid combinations. We explored 36 reactions involving the PAHs naphthalene, anthracene, fluoranthene, pyrene, triphenylene, and coronene and the amino acids glycine, alanine, valine, leucine, phenylalanine, and tyrosine. Our experiments do not show the formation of amino acids, whereas our theoretical results hint that PAHs could be precursors of amino acids in carbonaceous chondrites at low temperatures.

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