J. Nyberg et al., Changes in the D- and L-content of aspartic acid, glutamic acid, and alanine in a scleractinian coral over the last 300 years, ORG GEOCHEM, 32(5), 2001, pp. 623-632
The D- and L-contents of aspartic acid (Asp), glutamic acid (Glu), and alan
ine (Ala) together with absolute and relative concentrations of 17 amino ac
ids (AAs) were determined in samples of aragonite skeletons of a scleractin
ian coral from the Caribbean through the last 308 years. Regular patterns o
f increasing D/L ratios with increasing age are seen for the last 300 years
. High and linear racemization rates occur through the first 250 years in A
sp, the first 150 years in Glu, and the first 250 years in Ala. An evaluati
on of the utility of the D/L ratios of these amino acids as a chronological
tool through the last 250 years yields standard errors for individual age
estimates ranging between 1.7 and 6.4 years. Thereafter the racemizations s
low down and in the 308-years old terminal sample the D/L values are discor
dant. A rapid decrease in the total amino acid concentration of 33% over ap
proximately the last hundred years is identified. The rapid rate of decreas
e in Asp and Glu may be responsible for this decrease in the total AA conce
ntration. The relative concentrations of Asp, Glu, and Ala (g AA/100 g prot
ein) show a general pattern of decrease, although not significant, through
the time interval analyzed. A regularity of the decrease in L-contents and
an irregularity of the decrease in D-contents are observed. This may imply
that, in addition to possible diagenetic alterations and/or leaching of ami
no acids, contamination of D-amino acids explains the discordant D/L values
. The D-amino acids could originate from peptidoglycans in bacterial cell w
alls. (C) 2001 Published by Elsevier Science Ltd.