Evaluation of the Potential for Dissolved Oxygen Ingress into Deep Sedimentary Basins during a Glaciation Event

Figure 6

Spatial O₂(aq) concentration distributions at different times for the base case simulation (i.e., at 0, 17,000, 20,000, and 32,000 years), corresponding to the initial condition, the end of Stage II, Stage III, and the final condition. O₂ concentrations in mol l⁻¹.