The former Turbidite Research Group at the University of Aberdeen initiated pioneering research, and the BACAMS (Ancient Marine Systems of Baja California) project continues this legacy. The BACAMS project is dedicated to advancing our understanding of sedimentary processes and the resulting deposits in submarine channel systems.
Since 2019, we have been meticulously mapping the sedimentary architecture of various ancient sloping channel systems to unravel their complex structures. We have begun to explore and map areas that have never before been studied by sedimentologists due to their difficult access. The examination of coarse-grained facies distribution has been central to our research, revealing the dynamic interaction of channel architecture dominated by bypass. We are remapping the contacts between channel belts and levees, the latter characterized by thin-bed architectures, using vertical sequences as a crucial tool for identifying sloping channel architectures.
Our research has led to the discovery of new burned tree trunks within distinct stratigraphic units from previous findings, adding a new dimension to interpretations regarding the role of the Chicxulub Impact Event.
Through the BACAMS project, we are not only expanding our understanding of ancient marine systems but also pioneering innovative ideas about the geological history of the Baja California region.
A world wonder of coarse-grained sloping channel complexes interbedded with mass transport complexes.
