Yr. Qian et al., ABUNDANCE AND STABLE CARBON-ISOTOPE COMPOSITION OF AMINO-ACIDS IN MOLECULAR-WEIGHT FRACTIONS OF FOSSIL AND ARTIFICIALLY AGED MOLLUSK SHELLS, Geochimica et cosmochimica acta, 59(6), 1995, pp. 1113-1124
Amino acid abundances in molecular weight fractions (separated by ultr
afiltration) of artificially aged carbonate shells and fossil shells a
re reported. Hydrolyzable amino acids were primarily concentrated in t
he <500 Dalton fraction and in an acid insoluble fraction. With contin
ued heating, proteins hydrolyzed to free amino acids and peptides. The
amount of amino acids in the acid insoluble fraction diminished where
as the amount of amino acids in the <500 Dalton molecular weight fract
ion increased. The amount of soluble peptides in molecular weight frac
tions between 500 and 10,000 Daltons was minimal in both the heated an
d fossil shells. The extent of amino acid racemization was not uniform
throughout the molecular weight spectrum. Free amino acids and amino
acids in lower molecular weight peptides were racemized to the greates
t extent, whereas amino acids recovered from the insoluble residue fra
ctions were the least racemized. The deltaC-13 values of individual am
ino acids in the molecular weight fractions of the artificially aged s
hells generally varied by less-than-or-equal-to 2 - 3 parts per thousa
nd relative to their respective values in the total hydrolyzate of the
unheated shell. These differences may in part reflect fractionations
resulting from hydrolysis and decomposition.