Magnetic heat capacity measurements of a high-quality single crystal of the dipole-octupole pyrochlore down to a temperature of are reported. These show a two-peaked structure, with a Schottky-like peak at , similar to what is observed in its sister Ce pyrochlores and . However, a second sharper peak is observed at , signifying the entrance to the ground state. The ground state appears to have gapped excitations, as even the most abrupt extrapolation to at fully accounts for the entropy associated with the pseudospin- doublet for in this environment. The ground state could be conventionally ordered, although theory predicts a much larger anomaly in at much higher temperatures than the measured for expectations from an all-in, all-out ground state of the XYZ Hamiltonian for . The sharp low-temperature peak could also signify a crossover from a classical spin liquid to a quantum spin liquid (QSL). For both scenarios, comparison of the measured with NLC calculations suggests that weak interactions beyond the nearest-neighbor XYZ Hamiltonian become relevant below . The diffuse magnetic neutron scattering observed from at low temperatures between and resembles that observed from , which is well established as a -flux quantum spin ice (QSI). Together with the peak in the heat capacity at , this diffuse scattering from is suggestive of a classical spin liquid regime above that is distinct from the zero-entropy quantum ground state below .