Reconstruction of travel history using coupled δ18O and 87Sr/86Sr measurements of hair
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文摘
Oxygen isotope ratios (δ18O values) of hair largely reflect features of regional hydrology while strontium isotope ratios (87Sr/86Sr) are thought to reflect bedrock geology; combination of both isotope signatures may provide greater capacity for determining provenance and reconstructing travel history of an organism. To test this hypothesis, we compared the O-Sr isotope profiles of hair from domestic horses with known residency histories.

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