Journal of Molecular Evolution

, Volume 13, Issue 3, pp 179–183

Amino acids in a carbonaceous chondrite from Antarctica

Authors

  • R. K. Kotra
    • Laboratory of Chemical Evolution, Department of ChemistryUniversity of Maryland
  • Akira Shimoyama
    • Laboratory of Chemical Evolution, Department of ChemistryUniversity of Maryland
  • Cyril Ponnamperuma
    • Laboratory of Chemical Evolution, Department of ChemistryUniversity of Maryland
  • P. E. Hare
    • Carnegie Institution of Washington Geophysical Laboratory
Article

DOI: 10.1007/BF01739477

Cite this article as:
Kotra, R.K., Shimoyama, A., Ponnamperuma, C. et al. J Mol Evol (1979) 13: 179. doi:10.1007/BF01739477

Summary

A carbonaceous chondrite from the Antarctic, referred to as the Allan Hills meteorite 77306, appears to be free from terrestrial organic contamination. The presence of both protein and non-protein amino acids and an equal abundance of D- and L-enantiomers of amino acids, is testimony to the extraterrestrial nature of these compounds.

Key words

Carbonaceous chondrites Allan Hills meteorite Antartic meteorites Amino acids D, L-enantiomers

Copyright information

© Springer-Verlag 1979