Enrichment of the amino acid l-isovaline by aqueous alteration on CI and CM meteorite parent bodies

The distribution and enantiomeric composition of the 5-carbon (C5) amino acids found in CI-, CM-, and CR-type carbonaceous meteorites were investigated by using liquid chromatography fluorescence detection/TOF-MS coupled with o-phthaldialdehyde/N-acetyl-l-cysteine derivatization. A large l-enantiome...

Full description

Bibliographic Details
Published in:Proceedings of the National Academy of Sciences
Main Authors: Glavin, Daniel P., Dworkin, Jason P.
Format: Text
Language:English
Published: National Academy of Sciences 2009
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2667035
http://www.ncbi.nlm.nih.gov/pubmed/19289826
https://doi.org/10.1073/pnas.0811618106
id ftpubmed:oai:pubmedcentral.nih.gov:2667035
record_format openpolar
spelling ftpubmed:oai:pubmedcentral.nih.gov:2667035 2023-05-15T13:34:58+02:00 Enrichment of the amino acid l-isovaline by aqueous alteration on CI and CM meteorite parent bodies Glavin, Daniel P. Dworkin, Jason P. 2009-04-07 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2667035 http://www.ncbi.nlm.nih.gov/pubmed/19289826 https://doi.org/10.1073/pnas.0811618106 en eng National Academy of Sciences http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2667035 http://www.ncbi.nlm.nih.gov/pubmed/19289826 http://dx.doi.org/10.1073/pnas.0811618106 Physical Sciences Text 2009 ftpubmed https://doi.org/10.1073/pnas.0811618106 2013-09-02T12:10:45Z The distribution and enantiomeric composition of the 5-carbon (C5) amino acids found in CI-, CM-, and CR-type carbonaceous meteorites were investigated by using liquid chromatography fluorescence detection/TOF-MS coupled with o-phthaldialdehyde/N-acetyl-l-cysteine derivatization. A large l-enantiomeric excess (ee) of the α-methyl amino acid isovaline was found in the CM meteorite Murchison (lee = 18.5 ± 2.6%) and the CI meteorite Orgueil (lee = 15.2 ± 4.0%). The measured value for Murchison is the largest enantiomeric excess in any meteorite reported to date, and the Orgueil measurement of an isovaline excess has not been reported previously for this or any CI meteorite. The l-isovaline enrichments in these two carbonaceous meteorites cannot be the result of interference from other C5 amino acid isomers present in the samples, analytical biases, or terrestrial amino acid contamination. We observed no l-isovaline enrichment for the most primitive unaltered Antarctic CR meteorites EET 92042 and QUE 99177. These results are inconsistent with UV circularly polarized light as the primary mechanism for l-isovaline enrichment and indicate that amplification of a small initial isovaline asymmetry in Murchison and Orgueil occurred during an extended aqueous alteration phase on the meteorite parent bodies. The large asymmetry in isovaline and other α-dialkyl amino acids found in altered CI and CM meteorites suggests that amino acids delivered by asteroids, comets, and their fragments would have biased the Earth's prebiotic organic inventory with left-handed molecules before the origin of life. Text Antarc* Antarctic PubMed Central (PMC) Antarctic Murchison ENVELOPE(144.250,144.250,-67.317,-67.317) Proceedings of the National Academy of Sciences 106 14 5487 5492
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Physical Sciences
spellingShingle Physical Sciences
Glavin, Daniel P.
Dworkin, Jason P.
Enrichment of the amino acid l-isovaline by aqueous alteration on CI and CM meteorite parent bodies
topic_facet Physical Sciences
description The distribution and enantiomeric composition of the 5-carbon (C5) amino acids found in CI-, CM-, and CR-type carbonaceous meteorites were investigated by using liquid chromatography fluorescence detection/TOF-MS coupled with o-phthaldialdehyde/N-acetyl-l-cysteine derivatization. A large l-enantiomeric excess (ee) of the α-methyl amino acid isovaline was found in the CM meteorite Murchison (lee = 18.5 ± 2.6%) and the CI meteorite Orgueil (lee = 15.2 ± 4.0%). The measured value for Murchison is the largest enantiomeric excess in any meteorite reported to date, and the Orgueil measurement of an isovaline excess has not been reported previously for this or any CI meteorite. The l-isovaline enrichments in these two carbonaceous meteorites cannot be the result of interference from other C5 amino acid isomers present in the samples, analytical biases, or terrestrial amino acid contamination. We observed no l-isovaline enrichment for the most primitive unaltered Antarctic CR meteorites EET 92042 and QUE 99177. These results are inconsistent with UV circularly polarized light as the primary mechanism for l-isovaline enrichment and indicate that amplification of a small initial isovaline asymmetry in Murchison and Orgueil occurred during an extended aqueous alteration phase on the meteorite parent bodies. The large asymmetry in isovaline and other α-dialkyl amino acids found in altered CI and CM meteorites suggests that amino acids delivered by asteroids, comets, and their fragments would have biased the Earth's prebiotic organic inventory with left-handed molecules before the origin of life.
format Text
author Glavin, Daniel P.
Dworkin, Jason P.
author_facet Glavin, Daniel P.
Dworkin, Jason P.
author_sort Glavin, Daniel P.
title Enrichment of the amino acid l-isovaline by aqueous alteration on CI and CM meteorite parent bodies
title_short Enrichment of the amino acid l-isovaline by aqueous alteration on CI and CM meteorite parent bodies
title_full Enrichment of the amino acid l-isovaline by aqueous alteration on CI and CM meteorite parent bodies
title_fullStr Enrichment of the amino acid l-isovaline by aqueous alteration on CI and CM meteorite parent bodies
title_full_unstemmed Enrichment of the amino acid l-isovaline by aqueous alteration on CI and CM meteorite parent bodies
title_sort enrichment of the amino acid l-isovaline by aqueous alteration on ci and cm meteorite parent bodies
publisher National Academy of Sciences
publishDate 2009
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2667035
http://www.ncbi.nlm.nih.gov/pubmed/19289826
https://doi.org/10.1073/pnas.0811618106
long_lat ENVELOPE(144.250,144.250,-67.317,-67.317)
geographic Antarctic
Murchison
geographic_facet Antarctic
Murchison
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2667035
http://www.ncbi.nlm.nih.gov/pubmed/19289826
http://dx.doi.org/10.1073/pnas.0811618106
op_doi https://doi.org/10.1073/pnas.0811618106
container_title Proceedings of the National Academy of Sciences
container_volume 106
container_issue 14
container_start_page 5487
op_container_end_page 5492
_version_ 1766059628072796160