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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Published in | Organic geochemistry Vol. 38; no. 3; pp. 485 - 498 |
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Main Authors | , , |
Format | Journal Article Conference Proceeding |
Language | English |
Published |
Oxford
Elsevier Ltd
01.03.2007
Elsevier Science |
Subjects | |
Online Access | Get full text |
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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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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0146-6380 1873-5290 |
DOI: | 10.1016/j.orggeochem.2006.06.010 |