© Stephen Plowright
Drug Referral and Information Centre, Canberra.
This method was designed by S. Plowright (1992) to be used by L. Martin in her paper investigating methods of extracting evidence of artificial deformation in the Australian Pleistocene cranial population (Martin, 1992). Martin's paper was inspired by work published by P. Brown (Brown, 1981), and was presented at the 1992 Conference of the Australasian Society for Human Biology. Martin used this method to complement other methods, and found evidence supporting Brown's assessment that artificial deformation was most likely present in the Australian Pleistocene cranial population.
This method was designed to quantify those features which are most easily observed as indicating induced deformity, ie. the curvature and symmetry of the cranial midline. It produces a number or index which reflects the degree of deformity and is easily extracted and calculated from any lateral photograph of a cranium.
The Frankfurt plane was calculated for use as a baseline. This baseline was then divided into ten equal parts, providing nine points from which to measure, giving measurements a 1, a 2, a 3, ...a 9 (a 0 and a 10 will always have values of 0). Lines were drawn perpendicular to the baseline to intersect with the top of the cranium, thereby constructing a plot of the cranial midline. Distances from the baseline to the midline were measured in units of one tenth of the baseline length thus eliminating the problem of variation in size and photographic scaling. Point 0 is at the front of the cranium and point 10 at the back.
Figure 1. Midline heights in 1/10 th baseline units.
From these nine measurements, information about curvature and symmetry were calculated. The curvature at each point was estimated by calculating the difference in angle between the lines connecting that point to the previous and next points (Figure 2).
Figure 2. Estimate of curvature at point 6 in radians per unit.
Deformed crania were observed to exhibit areas of low curvature at varying points, as well as a tendency to have increased curvature toward the back. One indicator of the deformity, therefore, was the difference in curvature between the lower values and the curvature toward the back. The most stable and reliable measurement was obtained by subtracting the average of the lowest four values from the average of the three hindmost values (Theta 7, 8, 9 ). This averaging across the cranial surface was necessary to prevent excessive sensitivity to normal lumps.
The resulting figure was then multiplied by a symmetry component, k , to reflect overall symmetry (Figure 3). The symmetry component was calculated by taking the ratio of the differences of the height toward the front and toward the back, from half the height at the mid point (a 5 ). For convenience, the calculation was multiplied by 10 to produce values ranging approximately between 2 and 20, which many people find easier to remember and compare.
Figure 3. The symmetry component.
The index is then calculated.
Where theta (a, b, c, d) are the four lowest curvatures. Examples of midline curve and index are shown in figures 4 and 5.
Figure 4. Plot of severely deformed Vanuatu cranium: I = 13.84
Figure 5. Plot of non-deformed Vanuatu Cranium: I = 4.48
A sample of 15 crania from the Coobool Creek population were sorted visually by Martin into two groups; deformed and non-deformed. The index was then calculated for each cranium and the two groups were tested statistically for a difference in the index. In table 1, specimens judged deformed by Martin are marked M, those judged by Brown as deformed are marked B.
The index produced by this method was found to discriminate quite well between deformed and non-deformed specimens. It was also found to agree well with the degree of deformity as determined visually. Martin found the method to be of use in assessing the likelihood of artificial deformation in the Australian Pleistocene cranial population (Martin, 1992).
Further studies need to be done to fully assess the value of this method. To assist those interested in such work, I have developed software for the Macintosh to perform the calculations and manage the resulting data. This software is available free of charge, contact Dr Colin Groves, Anthropology, ANU, or e-mail email@example.com.
Letresha Martin, for the inspiration, collaboration, and friendship.
Dr Colin Groves, for kind advice and support.
BROWN, P. (1981) Artificial Cranial Deformation: a component in the variation in Pleistocene Australian Aboriginal crania AO 16:156-167
MARTIN, L. (1992) Two Methodologies of Artificial Cranial Deformation Analysis.
Presented at the Conference of the Australasian Society for Human Biology. To be published.