Origins of Life and Evolution of Biospheres

, Volume 42, Issue 6, pp 519–531 | Cite as

Abiotic Formation of Valine Peptides Under Conditions of High Temperature and High Pressure

  • Yoshihiro Furukawa
  • Tsubasa Otake
  • Takato Ishiguro
  • Hiromoto Nakazawa
  • Takeshi Kakegawa
Prebiotic Chemistry


We investigated the oligomerization of solid valine and the stabilities of valine and valine peptides under conditions of high temperature (150–200 °C) and high pressure (50–150 MPa). Experiments were performed under non-aqueous condition in order to promote dehydration reaction. After prolonged exposure of monomeric valine to elevated temperatures and pressures, the products were analyzed by liquid chromatography mass spectrometry comparing their retention times and masses. We identified linear peptides that ranged in size from dimer to hexamer, as well as a cyclic dimer. Previous studies that attempted abiotic oligomerization of valine in the absence of a catalyst have never reported valine peptides larger than a dimer. Increased reaction temperature increased the dissociative decomposition of valine and valine peptides to products such as glycine, β-alanine, ammonia, and amines by processes such as deamination, decarboxylation, and cracking. The amount of residual valine and peptide yields was greater at higher pressures at a given temperature, pressure, and reaction time. This suggests that dissociative decomposition of valine and valine peptides is reduced by pressure. Our findings are relevant to the investigation of diagenetic processes in prebiotic marine sediments where similar pressures occur under water-poor conditions. These findings also suggest that amino acids, such as valine, could have been polymerized to peptides in deep prebiotic marine sediments within a few hundred million years.


Amino acid Valine Peptide Diagenesis Early Earth Pressure 



The authors thank S. Ohara and K. Kawamura for helpful discussions. This study was supported by the Global COE program (Global Education and Research Center for Earth and Planetary Dynamics) of Tohoku University and by grants-in-aid for scientific research from the Japan Society for the Promotion of Science (JSPS) to T.K. (21244080), Y.F. (21840013), and H.N. (21340162).


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Copyright information

© Springer Science+Business Media B.V. 2012

Authors and Affiliations

  • Yoshihiro Furukawa
    • 1
  • Tsubasa Otake
    • 2
  • Takato Ishiguro
    • 1
  • Hiromoto Nakazawa
    • 1
    • 3
  • Takeshi Kakegawa
    • 1
  1. 1.Department of Earth Science, Graduate School of ScienceTohoku UniversitySendaiJapan
  2. 2.Division of Sustainable Resources Engineering, Faculty of EngineeringHokkaido UniversitySapporoJapan
  3. 3.National Institute for Materials ScienceTsukubaJapan

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