4.1 Article

Intact archeological human bones and age at death studied with transmission x-ray diffraction and small angle x-ray scattering

Journal

INTERNATIONAL JOURNAL OF OSTEOARCHAEOLOGY
Volume 32, Issue 1, Pages 170-181

Publisher

WILEY
DOI: 10.1002/oa.3053

Keywords

age at death; carbonated hydroxyapatite; collagen D-period; crystallite size; diagenesis; human bone; lattice parameters; small angle x-ray scattering (SAXS); x-ray diffraction (wide-angle x-ray scattering; WAXS)

Funding

  1. DOE Office of Science by Argonne National Laboratory [DE-AC02-06CH11357]
  2. Northwestern University

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High-energy, wide-angle x-ray scattering (WAXS) and small-angle x-ray scattering (SAXS) were used to study intact human second metacarpal bones from two UK archeological sites. The study found that carbonated apatite lattice parameters were not correlated with age-at-death, and WAXS and SAXS could be used to select intact bones likely to retain unaltered tissue nanostructure.
High-energy, wide-angle x-ray scattering (WAXS, x-ray diffraction) and small-angle x-ray scattering (SAXS) were used to study intact human second metacarpal bones (mc2) from two UK archeological sites. A novel method correcting for irregular mass distribution was applied in these transmission geometry experiments done at beamline 1-ID of the Advanced Photon Source. The authors asked whether there were age-at-death-related changes in carbonated apatite (cAp) lattice parameters and whether SAXS could detect collagen D-period peaks in the archeological mc2. For each of the two sites, Ancaster and Wharram Percy in England, six female mc2s were studied; for each site, two were from each of three age-at-death cohorts (young, 18-29 years; middle, 30-49 years; old >= 50 years) along with a modern control mc2. The Rietveld method was applied to the WAXS patterns to provide precise lattice parameter values. The cAp lattice parameters did not correlate with age-at-death estimated from dental wear. From WAXS and the 00.2 diffraction peak widths, four archeological mc2s possessed coherently scattering domain lengths (crystallite c-axis sizes) that matched that of the modern mc2; SAXS revealed the same four archeological mc2 had D-period peak intensities equivalent to that of the modern mc2. The other eight archeological mc2s had significantly larger crystallite sizes (than the modern mc2) and weak or absent D-period peaks, differences attributed to diagenetic changes. Based on these data, the authors suggest that WAXS 00.2 peak width and SAXS D-period peak intensity can be used with intact bones to select those likely to retain largely unaltered tissue nanostructure, which might be required for other analyses. Taken as a whole, the results suggest detecting age-related deterioration in nanostructural features may be difficult in bone showing significant bioerosion.

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