The effects of high pressure (0.1-3.4 gigapascal (GPa)) on the ferrous heme active sites of human adult hemoglobin, sperm whale myoglobin, and Glycera dibranchiata hemoglobin (Fraction II) were probed using resonance Raman and absorption spectroscopies. High-to-low spin transitions of the heme iron occur for hemoglobin, myoglobin, and Glycera hemoglobin at 0.35, 0.75, and 0.50 GPa, respectively, for the deoxy species. These interspecies differences result from variations in the composition of the hemepockets and/or their rigidity to pressure-induced volume changes. Heme active sites initially bound to CO or O2 exhibit distinctive behavior at high pressures. For all proteins studied, O2 apparently dissociates from the heme at only moderately high pressure, while CO remains bound to the heme moiety even at extreme pressures. The Raman spectra demonstrate the differences in the ligated and deoxy species at 3.4 GPa in the high frequency region. Discrete changes (i.e. iron spin-state transitions and dissociation of O2) occur that are commensurate with the collapse of the distal pocket, while continuous shifts in the absorption and Raman spectra are observed at pressures above those required for pocket collapse.