Abstract Amino acid racemization forms a basis for determining the chronology and paleotemperature of old plant constituents. Disparity in the extent of aspartic acid racemization was found in different taxa of plants subjected to the same environmental history and found in close proximity within an ancient packrat midden. One taxon showed different rates of aspartic acid racemization in two different anatomical sites. Temperature, pH and time being virtually identical in this one micro-environment within the midden, the differences in racemization rates may have been ultimately derived from physiological variants among the plants. Thus, at least, aspartic acid racemization data should be used selectively.