4.4 Article

Intramolecular distribution of 13C/12C isotopes in amino acids of diverse origins

期刊

AMINO ACIDS
卷 52, 期 6-7, 页码 955-964

出版社

SPRINGER WIEN
DOI: 10.1007/s00726-020-02863-y

关键词

H-1 NMR; Position specific; Isotope analysis; Amino acids

资金

  1. Petroleum Research Fund New Directions grant (PRF) [61080-ND2]
  2. College of Natural Sciences Catalyst grant, University of Texas at Austin

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Carbon stable isotope analysis can provide information about the origin and synthetic pathways that produce organic molecules, with applications in chemical, medical and (bio)geochemical sciences. The(13)C/C-12 isotope ratios of organics such as amino acids are most commonly obtained as whole molecule averages. In this study, we apply proton nuclear magnetic resonance spectroscopy to conduct position-specific carbon isotope analyses ofl-/d-alanine,l-threonine andl-histidine from different sources, in addition to molecule average stable isotope analyses obtained via mass spectrometry. Our results demonstrate that carbon isotope ratios can vary significantly between the individual carbon positions within an amino acid. For example, the beta- and gamma- carbons ofl-threonine can differ in(13)C/C-12 ratio by > 20 parts per thousand. Comparisons of the position-specific and whole molecule average stable isotope abundances show that whole molecule analyses can mask the intramolecular isotope variation. These results provide the first experimentally measured position-specific isotope ratios for alpha and side chain carbons of alanine, threonine and histidine. Comparison with previous ab initio calculations of intramolecular equilibrium fractionation shows that the carbon isotope distributions are not at equilibrium, thus kinetic isotope effects play a significant role in amino acid synthesis. We hypothesize that position-specific(13)C/C-12 isotope ratios provide an isotopic fingerprint that can give insight into the origin or synthesis pathway that formed an amino acid, and that this emerging analytical field will be a valuable addition to traditional stable isotope analysis.

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