Stable carbon isotope composition of amino acids in modern and fossil Mercenaria

Amino acids were extracted from the bivalve shells of modern and fossil Mercenaria and analyzed for δ 13C (PDB). These data were then compared to the expected impacts of diagenesis and contamination on the isotopic composition of fossilized proteins. The δ 13C of l-amino acids from modern specimens...

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Bibliographic Details
Published inOrganic geochemistry Vol. 38; no. 3; pp. 485 - 498
Main Authors O’Donnell, Thomas H., Macko, Stephen A., Wehmiller, John F.
Format Journal Article Conference Proceeding
LanguageEnglish
Published Oxford Elsevier Ltd 01.03.2007
Elsevier Science
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Summary:Amino acids were extracted from the bivalve shells of modern and fossil Mercenaria and analyzed for δ 13C (PDB). These data were then compared to the expected impacts of diagenesis and contamination on the isotopic composition of fossilized proteins. The δ 13C of l-amino acids from modern specimens had enriched glycine, glutamic acid, and isoleucine relative to leucine, and phenylalanine. The range of δ 13C in amino acids from modern Mercenaria collected from coastal Virginia (−1.6‰ to −29.6‰) and coastal Florida (−11.6‰ to −35.5‰) suggests the preservation of a diet signal. All of the fossil specimens had amino acids with the same δ 13C distribution pattern as modern specimens. Alanine in the fossil specimens however, was always relatively enriched and often had δ 13C values comparable to or more positive than glycine. Fossil specimens commonly contained glycine and glutamic acid with positive δ 13C values. The variation of δ 13C among the different enantiomers was not predictable. In some specimens, the d- and l-amino acids had the same δ 13C values, a feature attributed to the presence of original amino acids. In other specimens, one or more enantiomers had different δ 13C values, suggesting preferential loss of one enantiomer, the formation of secondary amino acids by the degradation of others, a diagenetic affect, or perhaps contamination.
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ISSN:0146-6380
1873-5290
DOI:10.1016/j.orggeochem.2006.06.010