Jf. Saliege et al., PRESERVATION OF C-13 C-12 ORIGINAL RATIO AND C-14 DATING OF THE MINERAL FRACTION OF HUMAN BONES FROM SAHARAN TOMBS, NIGER/, Journal of archaeological science, 22(2), 1995, pp. 301-312
The remains of 40 skeletons from the necropolises of Iwelen and Adrar
Bous, situated in the massif of Air, southern Sahara (Niger) have been
investigated for their mineral content, carbon isotope ratio and C-14
activity. The impermeability of the graves allowed for a good preserv
ation of the bones, which are in fact devoid of secondary calcite. Fur
thermore, the necropolis of Iwelen gave the opportunity to study tombs
which cover a time interval of about four thousand years, which is ra
ther exceptional for sub-Saharan Africa. The good state of preservatio
n of the material enabled the study of the geochemical evolution of bo
ne carbonate hydroxylapatite through time, with a significant statisti
cal resolution. All analytical data allow us to conclude that the init
ial C-13/C-12 isotopic ratio of the carbonate hydroxylapatite, albeit
accompanied by a change in the crystallinity index, has been preserved
. Given the described local conditions, the increase in the crystallin
ity index cannot be linked to exchanges with the environment but clear
ly reflects the decrease of CO3 radicals in the bone material. A corre
lation is suggested between the crystallinity index and the residual c
ontent of organic matter. The C-14 dates obtained for the carbonate hy
droxylapatite are identical to those of the material of comparison (le
ather, charcoal and associated collagen samples). We can therefore con
clude that the potential carbon isotopic exchanges--either by adsorpti
on of by substitution--between the carbonate hydroxylapatite on the on
e hand and the total dissolved inorganic carbon (TDIC) on the other, a
re too insignificant to be detectable through analysis. These results
can be explained by the combining of two favourable factors: the water
proof nature of the graves and the arid climate. The dating of carbona
te hydroxylapatite in the restricted conditions already described open
s new prospects for establishing a chronology of the principal funerar
y monuments of the Sahara.