Evaluating an Alternate Method for Analysis of Meteoric Amino Acids Pia 1University 1 Sen , Jason P. 2 Dworkin Assessment and Optimization of GC-MS Method ▪ Carbonaceous chondrites are primitive stony meteorites that contain a diverse suite of soluble organic compounds, among them a variety of amino acids. ▪ More than 80 amino acids have been discovered in these meteorites Murchison Meteorite Jamie E. 2 Elsila , of Texas at Austin, Austin, TX 78712, USA. 2Catholic University of America, Washington, DC 20064, USA. 3NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA. Introduction β José C. 2,3 Aponte , Existing methods for GC-MS analysis of amino acids have drawbacks and require tradeoffs in reaction time, stability, ability to separate enantiomers, and number of carbon atoms added. Table 1. Comparison of derivatization methods for GC-MS analysis of amino acids. Derivatization Method Chlorofomate ester α α-Amino Acid Reaction time 10 s Stability (approx. time) > 72 h Chiral separation Y Water stable Y 2h 5 min 1h 1h <8h > 24 h <6h <2h Y Y N N N N N N α-Helix ▪ Many amino acids are chiral, meaning they can exist in two non-superimposable mirror image enantiomer forms. Abiotic processes create racemic mixtures (equal concentration of the two enantiomers), while creation of an enantiomeric excess requires the presence of a chiral force. Molecules are built using one enantiomer. Life on Earth uses primarily the Lenantiomer of amino acids. Abiotic processes produce racemic mixtures (L:D=1:1) Enantiomers: mirror image Evaluation of meteoritic amino acids is important because… ▪ L-Enantiomeric excesses of a few amino acids (e.g. isovaline) have been found in some carbonaceous chondrites. ▪ It is possible that there is a link between the delivery of enantiomerically enriched amino acids by meteorites and the origins of homochirality on Earth. Understanding the enantiomeric distribution of amino acids in extraterrestrial samples can help evaluate this link. Why use GC-MS for analysis? ▪ Amino acids are not volatile and derivatization is needed for analysis by gas chromatography-mass spectrometry (GC-MS), ▪ After derivatization, amino acids in meteorite extracts can be identified by retention time and mass spectrum, using standards as a comparison, ▪ Can be coupled to isotope ratio mass spectrometers to determine compound-specific isotopic composition which can be used to determine origin of organic compounds. Limitations of Method TFAA/IPA DMF/DMA MTBSTFA TMS Effectiveness of the chloroformate method is challenged by the formation of byproducts that add complexity to the chromatogram, and by the low reactivity of hindered compounds TFAA/IPA: Trifluoroacetic anhydride/isopropanol. DMF/DMA: N,N-dimethylformamide dimethylacetal. MTBSTFA: N-tert-butyldimethylsilyl-N-methyltrifluoroacetamide. TMS: Trimethylsilyl. We tested and optimized the chloroformate ester method using 35 amino acid standards, being able to separate 19 compounds (14 chiral, 5 achiral), at concentrations ranging between 20-36 nM. ▪ Meteorite extracts can be analyzed on either a non-chiral (does not separate enantiomers) or chiral (separates enantiomers) GC column. ▪ Chiral analysis provides more information, but has more potential for co-elutions. Conclusions ▪ We have evaluated a GC-MS method capable of resolving 19 meteoritic amino acids. The chloroformate ester derivatization has the following advantages: ▪ Quick procedure (10 sec. reaction) ▪ Doesn’t need heat (room temperature) ▪ Stable products (>72 hours at room temp.) ▪ High compound resolution possible ▪ Efficient at low concentrations ▪ Future work: ▪ Test chloroformate ester derivatives to determine suitability for liquid chromatographic analyses ▪ δ13C isotopic analysis of chloroformate-esterderivatized meteoritic amino acids Acknowledgements and References This work was supported by the NASA Astrobiology Institute and the Goddard Center for Astrobiology. [1] Cronin J. R. and Pizzarello S. (1997) Science, 275, 951-955. [2] Glavin D. P. and Dworkin J. P. (2009) Proc. Natl. Acad. Sci. USA, 106, 5487-5492. [3] Kvenvolden, K. et al. (1971) Proc. Natl. Acad. Sci. USA, 68, 486-490. [4] Zampolli M. et al. (2006) Chirality, 18, 279-295. [5] Myrgorodska I. et al. (2016) J. Chrom. A, 1433, 131-136. [6] Glavin D. P. et al. (2011) Met. Planet. Sci., 45, 1948-1972. [7] Villas-Bôas et al. (2011) Metabolites, 1, 3-20.
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