Abstract
The Lower Cretaceous/Upper Cretaceous boundary in Mexico is established at the base of the Thalmanninella ticinensis/Thalmanninella evoluta Interval-Zone, corresponding to the Zone with Stoliczkaia dispar of the ammonite scheme of zonation. The Vraconian is regarded as a valid stage and represents the time comprised by the zone with Stoliczkaia dispar. In Mexico the lower Cretaceous/Upper Cretaccous boundary lies within the Cuesta del Cura Limestone.
This work is licensed under a Creative Commons Attribution 4.0 International License.
Downloads
Download data is not yet available.