Cortical surface patterns in human and nonhuman primates

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Abstract
An analysis of skulls from several primate species shows that a “worm‐track” surface pattern, first identified in the brow region in fossil adult hominids and subsequently in olive baboons, chimpanzees, and macaques, is also present in numerous other species. Fine cancellous bone and its attendant vermiculate surface pattern have been observed in subadult and adult gelada baboons, gibbons, gorillas, and orangutans as well as in modern Homo sapiens and several Plio‐Pleistocene fossil hominids. In contemporary primates, fine cancellous bone has been identified not only in the brow region, but also along the zygomatic arch, on the pterygoid plates, on the maxilla, along the temporal line, on the mastoid process, and in the region of inion. Given the widespread distribution of this trait, caution is advised when using it as a diagnostic indicator of the evolutionary or functional significance of craniofacial morphology.