Repository logo
 

Unusual nonterrestrial L-proteinogenic amino acid excesses in the Tagish Lake meteorite

Simple item page
dc.contributor.authorGlavin, Daniel P.
dc.contributor.authorElsila, Jamie E.
dc.contributor.authorBurton, Aaron S.
dc.contributor.authorCallahan, Michael P.
dc.contributor.authorDworkin, Jason P.
dc.contributor.authorHilts, Robert
dc.contributor.authorHerd, Christopher D. K.
dc.date.accessioned2022-05-27T01:13:59Z
dc.date.available2022-05-27T01:13:59Z
dc.date.issued2012
dc.description.abstractThe distribution and isotopic and enantiomeric compositions of amino acids found in three distinct fragments of the Tagish Lake C2-type carbonaceous chondrite were investigated via liquid chromatography with fluorescence detection and time-of-flight mass spectrometry and gas chromatography isotope ratio mass spectrometry. Large l-enantiomeric excesses (lee ∼ 43–59%) of the α-hydrogen aspartic and glutamic amino acids were measured in Tagish Lake, whereas alanine, another α-hydrogen protein amino acid, was found to be nearly racemic (d ≈ l) using both techniques. Carbon isotope measurements of d- and l-aspartic acid and d- and l-alanine in Tagish Lake fall well outside of the terrestrial range and indicate that the measured aspartic acid enantioenrichment is indigenous to the meteorite. Alternate explanations for the l-excesses of aspartic acid such as interference from other compounds present in the sample, analytical biases, or terrestrial amino acid contamination were investigated and rejected. These results can be explained by differences in the solid–solution phase behavior of aspartic acid, which can form conglomerate enantiopure solids during crystallization, and alanine, which can only form racemic crystals. Amplification of a small initial l-enantiomer excess during aqueous alteration on the meteorite parent body could have led to the large l-enrichments observed for aspartic acid and other conglomerate amino acids in Tagish Lake. The detection of nonterrestrial l-proteinogenic amino acid excesses in the Tagish Lake meteorite provides support for the hypothesis that significant enantiomeric enrichments for some amino acids could form by abiotic processes prior to the emergence of life.
dc.description.urihttps://library.macewan.ca/cgi-bin/SFX/url.pl/7PM
dc.identifier.citationGlavin, D. P., Elsila, J. E., Burton, A. S., Callahan, M. P., Dworkin, J. P., Hilts, R. W., & Herd, C. D. K. (2012). Unusual nonterrestrial L-proteinogenic amino acid excesses in the Tagish Lake meteorite. Meteoritics & Planetary Science, 47(8), 1347–1364. https://doi.org/10.1111/j.1945-5100.2012.01400.x
dc.identifier.doihttps://doi.org/10.1111/j.1945-5100.2012.01400.x
dc.identifier.urihttps://hdl.handle.net/20.500.14078/335
dc.languageEnglish
dc.language.isoen
dc.rightsAll Rights Reserved
dc.titleUnusual nonterrestrial L-proteinogenic amino acid excesses in the Tagish Lake meteoriteen
dc.typeArticle
dspace.entity.type

Files

Collections

Department of Physical Sciences