Albicetus is inferred to have been a macroraptorial
predator specializing in hypercarnivorous feeding on large marine vertebrates, including small
cetaceans and
pinnipeds, based on its cranial morphology and dentition adapted for grasping and tearing flesh. The retention of functional,
enameled teeth in both upper and lower jaws, with conical
crowns and robust roots up to 20.5 cm long, indicates a biting mechanism suited for capturing and processing mobile prey such as seals or smaller whales, contrasting with the suction-feeding, squid-focused diet as seen in the modern
sperm whale. This
predatory specialization aligns with the high diversity of marine mammals in the middle Miocene
Monterey Formation, where
A. oxymycterus likely targeted abundant mid-sized vertebrates rather than soft-bodied cephalopods. This kind of macroraptorial predatory behavior is reconstructed as involving powerful jaw closure, facilitated by a structurally rigid
rostrum with a closed mesorostral groove that enhanced stability during biting. The enameled tips of the teeth, featuring coarse longitudinal striations, suggest repeated
occlusion and contact with hard tissues like bone or cartilage, implying a "grip-and-tear" strategy similar to that observed in coeval
macroraptorial sperm whales such as
Brygmophyseter. Wear patterns on preserved tooth fragments, including deep facets from tooth-to-tooth contact, further support frequent engagement with bony prey, though no direct evidence of gut contents or bite marks on associated fossils has been reported. As an
apex predator in
Miocene Pacific coastal ecosystems,
A. oxymycterus occupied a top trophic position, potentially competing with other
physeteroids like
Brygmophyseter for large vertebrate prey in nutrient-rich upwelling zones. It probably grew to be around in length and hypercarnivorous adaptations positioned it as a key regulator of marine mammal populations, contributing to the diverse predatory guilds of the era alongside sharks and early
pinnipeds, before the decline of such macroraptorial forms in the late Miocene. ==Paleoecology==