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Stable isotope analysis at the molecular level: A new approach for determining the origins of amino acids in the Murchison meteorite
A combined gas chromatography/isotope ratio mass spectrometry (GC/IRMS) method has been developed that permits the direct stable carbon isotope analysis of N(O)-trifluoroacetylisopropyl esters of individual amino acids and their respective enantiomers at nanomole abundances. Calculation of the origi...
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Published in: | Advances in space research 1995-03, Vol.15 (3), p.99-106 |
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Main Authors: | , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | A combined gas chromatography/isotope ratio mass spectrometry (GC/IRMS) method has been developed that permits the direct stable carbon isotope analysis of N(O)-trifluoroacetylisopropyl esters of individual amino acids and their respective enantiomers at nanomole abundances. Calculation of the original
δ
13C values of the amino acids is accomplished via a correction for the carbon introduced during the derivatization process. Previous GC/IRMS analyses of individual amino acids in the non-hydrolyzed water extract of an interior sample of a Murchison meteorite stone revealed an enrichment in
13C relative to terrestrial organic matter, in agreement with previous findings for bulk extracts. The range of amino acid
δ
13C values (+5 to +30 ‰, PDB) suggests possible kinetic effects during synthesis. In this study, an apparent kinetic isotope effect was also observed for the amino acid products of a spark discharge experiment. These preliminary results are supportive of a similar mechanism for the abiotic synthesis of amino acids in the Murchison meteorite. |
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ISSN: | 0273-1177 1879-1948 |
DOI: | 10.1016/S0273-1177(99)80069-6 |