Praemurica uncinata displays pronounced allometry during its evolutionary t
ransformation into Morozovella angulata, an important species in Paleocene
planktic foraminiferal biostratigraphy. The allometry is such that smaller
specimens of P. uncinata resemble large specimens of the descendant, M. ang
ulata. Biometric analysis of populations spanning this paedomorphic evoluti
onary transition reveals that the event is recorded over an interval of 10.
69 meters in sediments from the DeSoto Canyon, Gulf of Mexico, and involves
specimens ranging in size from less than 100 to more than 300 mu m, Over t
his size range, failure to recognize the interdependence of size and shape
can lead to discordant zonations when biostratigraphers identify the first
appearance datum of Morozovella angulata after using different sieve sizes
during standard laboratory treatment of their samples.