This study presents a high-resolution geochemical reconstruction of terrestrial biomarkers spanning the 320 Ma Carboniferous to 2026 AD Anthropocene. Utilizing a unified 800-sample matrix, I evaluated the evolutionary trajectory of wood-degrading fungal lineages—specifically the Paleancistrus-Phanerochaete transition—through the lens of Polycyclic Aromatic Hydrocarbon (PAH) molecular proxies. I introduce a multidimensional analytical framework that integrates the Combined PAH Flux Index (CPFI) and the Higher Plant Parameter (HPP) with planetary-scale drivers, including Inner Core Compositional Rayleigh Numbers (Rac), the Thermal Maturity Index (Im), and the Mathieu stability characteristic (a).Our results identify a primary metabolic pulse at 318 Ma, where a surge in the CPFI correlates with a high-energy state characterized by a CPFI of 0.78 and a calculated reflectance (Rc) of 0.87. Time-series analysis reveals that modern geochemical signatures have bypassed Pleistocene stable baselines, exhibiting a rapid regression to Paleozoic thermal maturity levels (Rc ≈ 0.86+). However, 3D surface modeling of Time, CPFI/HPP ratios, and Phylogenetic Diversity Scores (PDS) uncovers a critical high-frequency lag in modern biological complexity compared to the 318 Ma baseline. These findings suggest that contemporary terrestrial metabolism is currently over-revving in response to orbital excitation (q) and intensified geodynamic conductivity, marking a fundamental departure from planetary equilibrium.