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The vermiculate surface pattern in brow ridges of Australopithecines and other very ancient hominids
Author(s) -
Tappen N. C.
Publication year - 1980
Publication title -
american journal of physical anthropology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.146
H-Index - 119
eISSN - 1096-8644
pISSN - 0002-9483
DOI - 10.1002/ajpa.1330520408
Subject(s) - crania , paleontology , fibrous joint , paleobiology , geology , biology , anatomy
A convoluted surface pattern of fine ridges, pits, and grooves characterized the brow ridges of Australopithecines and other very ancient fossil hominids. This vermiculate configuration terminated rather abruptly just below the fronto‐zygomatic suture in Australopithecines. It was resistant to oriented cracking from weathering or fractures, contrasting with the smooth but structurally oriented zygomatic bone adjacent to it. The pattern apparently developed as individuals matured. The vermiculate pattern seems to have been a feature of brow surface in hominids through much of their identifiable history, despite substantial changes in shape and size of the supraorbital region during human evolution. Limitations on the area of vermiculate surface in Australopithecines suggest that the pattern was associated in some yet undetermined manner with overlying soft tissues. This gives evidence on the cause and functional significance of the vermiculate pattern in Neandertal and modern crania. Problems of describing surfaces as “vermiculate” are raised by observation of elaborations of surface relief on two individuals.