Project Details

This submission represents a unified geochemical-geodynamic dataset mapping the 318 Ma Archosaurian Pulse. The data focuses on terrestrial PAH molecular proxies (specifically the Retene/Cadinene ratio) across a 234-sample matrix. Key Technical Context: This data provides the surface evidence for a Mathieu Equation (n=1) parametric resonance originating in the Earth's inner core. It demonstrates a constant 60% Metabolic Variance transitioning from the Carboniferous into the Permian. It also suggests that a true polar wander vortex may have caused the permian/triassic mass extinction event.