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Alanine enantiomers in the Murchison meteorite

Abstract

Engel and Macko1 have reported that alanine indigenous to the Murchison meteorite has an l-enantiomer excess of about 33%. Furthermore, they reported very similar δ15nitrogen values for l-alanine and d-alanine; these values are quite high in comparison with those of terrestrial amino acids. On this basis, they argued that contamination of the meteorite by terrestrial l-alanine can be ruled out because, if it contributed to the l-enantiomer excess, the lower 15N content of terrestrial l-alanine would significantly lower the δ15N value that they observed for l-alanine.

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Figure 1: Total ion chromatogram (Chirasil-l-Val, 50 m×025 mm, Alltech) of amino acids (N -trifluoroacetyl isopropyl esters) from a desalted Murchison water extract.

References

  1. Engel, M. & Macko, S. A. Nature 389, 265–268 (1997).

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  2. Kvenvolden, K. et al. Nature 228, 923–926 (1970).

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  3. Cronin, J. R. & Pizzarello, S. Science 275, 951–955 (1997).

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Pizzarello, S., Cronin, J. Alanine enantiomers in the Murchison meteorite. Nature 394, 236 (1998). https://doi.org/10.1038/28306

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