Ja. Silfer et al., STABLE CARBON-ISOTOPE COMPOSITIONS OF INDIVIDUAL AMINO-ACID ENANTIOMERS IN MOLLUSK SHELL BY GC C IRMS, Organic geochemistry, 21(6-7), 1994, pp. 603-609
Gas chromatography/combustion/isotope ratio mass spectrometry was used
to determine the stable carbon isotope composition of D- and L-enanti
omers of amino acids in a fossil Mercenaria shell and in modem samples
of Helix pomatia shell that were heated (80-degrees-C) for up to 289
days. The similarity in deltaC-13 values for the D- and L-enantiomers
of neutral amino acids in Mercenaria implies that these components are
indigenous. Whereas differences in the C-13 contents of the D- and L-
enantiomers of aspartic and glutamic acid in Mercenaria may indicate i
nputs from exogenous sources, similar discrepancies exist for the acid
ic amino acids in the heated samples of H. pomatia, suggesting more co
mplicated diagenetic pathways and concomitant isotope effects for the
acidic amino acid constituents of shell protein.