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pubmed-article:17733683rdf:typepubmed:Citationlld:pubmed
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pubmed-article:17733683pubmed:dateCreated2010-6-8lld:pubmed
pubmed-article:17733683pubmed:abstractTextAmino acids have been found in aqueous extracts of a C2 carbonaceous chondrite recovered from Antarctica. The composition of the amino acids strongly suggests that they have a meteoritic origin. Comparison of these results with those obtained with other C2 chondrites supports the view that Antarctic meteorites have not been significantly altered by terrestrial processes since their fall.lld:pubmed
pubmed-article:17733683pubmed:languageenglld:pubmed
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pubmed-article:17733683pubmed:issn0036-8075lld:pubmed
pubmed-article:17733683pubmed:authorpubmed-author:CroninJ RJRlld:pubmed
pubmed-article:17733683pubmed:authorpubmed-author:PizzarelloSSlld:pubmed
pubmed-article:17733683pubmed:authorpubmed-author:MooreC BCBlld:pubmed
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pubmed-article:17733683pubmed:volume206lld:pubmed
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pubmed-article:17733683pubmed:pagination335-7lld:pubmed
pubmed-article:17733683pubmed:year1979lld:pubmed
pubmed-article:17733683pubmed:articleTitleAmino acids in an antarctic carbonaceous chondrite.lld:pubmed
pubmed-article:17733683pubmed:publicationTypeJournal Articlelld:pubmed