AMINO ACIDS FROM THE YAMATO-791198 CARBONACEOUS CHONDRITE FROM ANTARCTICA

Abstract The Yamato-791198 carbonaceous chondrite yielded indigenous amino acids. These consitst of various structural and optical isomers, indicating abiotic in origin. The amount of these amino acids is the largest of carbonaceous chondrites studied so far. Terrestrial organic contamination was ni...

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Published in:Chemistry Letters
Main Authors: Shimoyama, Akira, Harada, Kaoru, Yanai, Keizo
Format: Article in Journal/Newspaper
Language:English
Published: Oxford University Press (OUP) 1985
Subjects:
Antarc*
Antarctica
Online Access:http://dx.doi.org/10.1246/cl.1985.1183
https://academic.oup.com/chemlett/article-pdf/14/8/1183/56249873/cl.1985.1183.pdf
id croxfordunivpr:10.1246/cl.1985.1183
record_format openpolar
spelling croxfordunivpr:10.1246/cl.1985.1183 2024-09-15T17:48:42+00:00 AMINO ACIDS FROM THE YAMATO-791198 CARBONACEOUS CHONDRITE FROM ANTARCTICA Shimoyama, Akira Harada, Kaoru Yanai, Keizo 1985 http://dx.doi.org/10.1246/cl.1985.1183 https://academic.oup.com/chemlett/article-pdf/14/8/1183/56249873/cl.1985.1183.pdf en eng Oxford University Press (OUP) https://academic.oup.com/pages/standard-publication-reuse-rights Chemistry Letters volume 14, issue 8, page 1183-1186 ISSN 0366-7022 1348-0715 journal-article 1985 croxfordunivpr https://doi.org/10.1246/cl.1985.1183 2024-08-27T04:16:45Z Abstract The Yamato-791198 carbonaceous chondrite yielded indigenous amino acids. These consitst of various structural and optical isomers, indicating abiotic in origin. The amount of these amino acids is the largest of carbonaceous chondrites studied so far. Terrestrial organic contamination was nil to this chondrite. Article in Journal/Newspaper Antarc* Antarctica Oxford University Press Chemistry Letters 14 8 1183 1186
institution Open Polar
collection Oxford University Press
op_collection_id croxfordunivpr
language English
description Abstract The Yamato-791198 carbonaceous chondrite yielded indigenous amino acids. These consitst of various structural and optical isomers, indicating abiotic in origin. The amount of these amino acids is the largest of carbonaceous chondrites studied so far. Terrestrial organic contamination was nil to this chondrite.
format Article in Journal/Newspaper
author Shimoyama, Akira
Harada, Kaoru
Yanai, Keizo
spellingShingle Shimoyama, Akira
Harada, Kaoru
Yanai, Keizo
AMINO ACIDS FROM THE YAMATO-791198 CARBONACEOUS CHONDRITE FROM ANTARCTICA
author_facet Shimoyama, Akira
Harada, Kaoru
Yanai, Keizo
author_sort Shimoyama, Akira
title AMINO ACIDS FROM THE YAMATO-791198 CARBONACEOUS CHONDRITE FROM ANTARCTICA
title_short AMINO ACIDS FROM THE YAMATO-791198 CARBONACEOUS CHONDRITE FROM ANTARCTICA
title_full AMINO ACIDS FROM THE YAMATO-791198 CARBONACEOUS CHONDRITE FROM ANTARCTICA
title_fullStr AMINO ACIDS FROM THE YAMATO-791198 CARBONACEOUS CHONDRITE FROM ANTARCTICA
title_full_unstemmed AMINO ACIDS FROM THE YAMATO-791198 CARBONACEOUS CHONDRITE FROM ANTARCTICA
title_sort amino acids from the yamato-791198 carbonaceous chondrite from antarctica
publisher Oxford University Press (OUP)
publishDate 1985
url http://dx.doi.org/10.1246/cl.1985.1183
https://academic.oup.com/chemlett/article-pdf/14/8/1183/56249873/cl.1985.1183.pdf
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Chemistry Letters
volume 14, issue 8, page 1183-1186
ISSN 0366-7022 1348-0715
op_rights https://academic.oup.com/pages/standard-publication-reuse-rights
op_doi https://doi.org/10.1246/cl.1985.1183
container_title Chemistry Letters
container_volume 14
container_issue 8
container_start_page 1183
op_container_end_page 1186
_version_ 1810290201579225088

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