CORRELATING GEOCHRONOLOGY, LITHOSTRATIGRAPHY, BIOSTRATIGRAPHY, AND MAGNETOSTRATIGRAPHY: AN EXERCISE FROM THE MIOCENE BARSTOW FORMATION, CALIFORNIA
In preparation for the lab, brief introductions to argon-based and uranium-lead dating techniques, magnetostratigraphy, and the field area are presented. Students are provided with published lithostratigraphy, biostratigraphy (Woodburne et al., 1990), magnetostratigraphy, and K-Ar and 40Ar/39Ar geochronology (MacFadden et al., 1990), which have been correlated to the global magnetic polarity time scale and used to determine the ages of boundaries in North American land mammal stratigraphy (Woodburne, 1996). Students are also given new U-Pb ages of sedimentary carbonates (Cole et al., 2005) and unpublished 40Ar/39Ar ages of an important marker tuff.
Students are asked to evaluate the different data sets, draw their own correlations, and evaluate the robustness of their interpretations. For example, students compare the local magnetic polarity record and the dated ashes and carbonates to the global polarity time scale. In doing so, students uncover discrepancies between the data and are forced to exclude some of the data in order to construct stratigraphically-sound correlations.
This exercise provides the opportunity to discuss the differences between relative' and absolute' dating, presents data from a burgeoning geochronological technique, demonstrates real-world geologic complexity, and encourages problem solving with multiple data sets.