|Most amino acids can have two different configurations, "D" or "L". Living organisms generally have amino acids in the "L" configuration, but when the organism dies, the ratio of D/L moves slowly toward equilibrium, a process called racemization. Measuring the ratio of D/L in a geologic sample containing preserved amino acids can therefore allow calculations of the age of the sample.|
|Albemarle Embayment and Central Arctic Ocean AAR sample locations:|
Downloaded Wednesday, 30-Jul-2014 07:14:43 EDT
Last Updated Wednesday, 26-Sep-2012 13:02:09 EDT by firstname.lastname@example.org
Please see the Paleoclimatology Contact Page or the NCDC Contact Page if you have questions or comments.