Ta. Elliott et Gw. Grime, EXAMINING THE DIAGENETIC ALTERATION OF HUMAN BONE MATERIAL FROM A RANGE OF ARCHAEOLOGICAL BURIAL SITES USING NUCLEAR MICROSCOPY, Nuclear instruments & methods in physics research. Section B, Beam interactions with materials and atoms, 77(1-4), 1993, pp. 537-547
The inorganic analysis of archaeological bone material can potentially
provide a wealth of information about the chronology, diet and palaeo
environment of past populations: for example, strontium and uranium le
vels are used in palaeodietary and dating studies, respectively. Howev
er, the extent to which the chemical composition of bone is subject to
diagenetic change during burial is open to controversy due, in part,
to differences in analytical technique, bone types and burial conditio
ns. To investigate this problem, archaeological human bone material fr
om a number of different geological environments including Pompeii and
a 12th century British ecclesiastical site, together with material fr
om two seawater burials (The ''Mary Rose'' and a 6th century Mediterra
nean wreck) have been studied using the nuclear microprobe facility at
the University of Oxford. Results using microbeam PIXE show that bone
is subject to contamination from a wide range of trace elements depen
ding on the burial conditions. Elemental maps are presented to demonst
rate the distribution of trace element accumulation under different bu
rial conditions, and the significance of this work to future trace ele
ment studies is discussed.