One answer to this question uses the facts that
there are two distinct stable isotopes of oxygen (O16 and O18),
and likewise of two of strontium. It turns out that O18, having two
extra neutrons, is roughly 12% heavier than O16 and so a water
molecule H2O18 is likewise heaver than H2O16.
When rain clouds drive in from the sea, the heavier rain falls first, causing a
decreasing gradient in the proportion of O18 in fresh water and
plants as you move inland, and a corresponding gradient in the take-up of the
two oxygen isotopes in the teeth of someone growing up there.
A second parameter that distinguishes your
region of origin is the proportion of two isotopes of the element strontium.
They have 48 and 49 neutrons respectively and their relative proportions in the
underlying rocks are mirrored in the top-soil and in the plants that grow
there. Ultimately the humans ingest the strontium in the same proportions
through the food chain and this can again be measured by the ratio of the two
isotopes deposited in their teeth.
Together, the values of these two isotope ratios,
for oxygen and strontium, are sensitive enough to locate where the owner of the
teeth was raised, on the assumption that most people don’t move far from
where they were born until they reach adulthood. This technique was used by Douglas Price and his team at the University of
Wisconsin in Madison to shed light on the geographical origins of sacrificial
victims cast into the Sacred Cenote, a sink hole in the limestone of the
Yucatán peninsula in Mexico believed by local Mayans to be the entrance to the
underworld. They analysed 40 ancient human teeth recovered from the lake and
concluded that half of them were locals, around a quarter had come from
somewhat farther afield, and the remainder from places hundreds of kilometres
away, in what are now western Honduras and Mexico’s central highlands. (Taken
from a report in The Economist, 3rd
August 2019.)
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