Variation of the schmelzmuster and other enamel characters in molars of the primitive Pliocene vole Ogmodontomys from Kansas.

Variation in enamel microhistology (the schmelzmuster) and other features were examined in adult Ogmodontomys poaphagus molars from the Meade Basin of southwestern Kansas. Measurements of total enamel thickness and thickness of tangential enamel were taken on individual triangles of first upper molar samples from the superposed Ripley B, Hornet and Rexroad 2A local faunas. Although thickness of total enamel layers and the tangential zone were not statistically different between triangles and sites, the quality of tangential enamel on the trailing edges increased, from incipient tangential and well-developed tangential enamel (Ripley B and Hornet) to solely well-developed tangential enamel (Rexroad 2A). The fundamental schmelzmuster of O. poaphagus is radial enamel on the leading edges and radial plus incipient or well-developed tangential enamel on the trailing edges. These results support the assertion that the schmelzmuster is a consistent and genetically controlled character mosaic, and confirm suggestions in the literature that Ogmodontomys is distinct from Mimomys. Paired sample Student’s t-tests of trailing/leading edge samples for each triangle were used to test for differentiation. Although the molars of Ogmodontomys poaphagus appear undifferentiated under the light microscope, and are indeed separable from the distinctly negatively differentiated molars of Mimomys by this technique, our results show that the M1s of O. poaphagus are slightly negatively differentiated, with various triangles being either undifferentiated or negatively differentiated. O. sawrockensis has a more primitive schmelzmuster than O. poaphagus, and the presence of discrete (primitive) lamellar enamel on the apices of at least one triangle in 55% of the sample from Fallen Angel B, combined with the absence of lamellar enamel in molars of O. poaphagus from Fox Canyon and all subsequent Ogmodontomys samples, conclusively demonstrates that the Fallen Angel B population of O. sawrockensis was not ancestral to O. poaphagus in the Meade Basin. A unique mosaic of dental and size features indicates that the early Blancan O. pipecreekensis from Indiana is a sister species to O. sawrockensis and not ancestral to O. poaphagus.