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Tracing the Source of the Elephant And Hippopotamus Ivory from ...

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Koch et al. (1995) reported on several isotopes (carbon, nitrogen, and strontium)<br />

<strong>from</strong> elephants in Amboseli National Park, Kenya, to track dietary and habitat changes.<br />

Time series were ga<strong>the</strong>red by microsampling sequential growth laminations in molar<br />

roots (because tooth dentine grows by accretion in elephants). The results are presented<br />

in Table 5. There were no coherent temporal trends for <strong>the</strong> nitrogen isotopes, but <strong>the</strong><br />

δ 15 N values were as expected for elephants living in a semi-arid environment. The<br />

carbon isotopes did change with time, showing a switch in <strong>the</strong> diet <strong>from</strong> browse to grass.<br />

A negative correlation was observed between carbon and strontium isotope values<br />

(Figure 37) as a result <strong>of</strong> two isotopically distinct regions within <strong>the</strong> park: <strong>the</strong> C3 rich<br />

bushlands on Precambrian soils (low δ 13 C, high 87 Sr/ 86 Sr) and <strong>the</strong> C4 rich grassland on<br />

Plio-Pleistocene volcanic and lakebed soils (medium to high δ 13 C, low 87 Sr/ 86 Sr). The<br />

soils overlying <strong>the</strong> Proterozoic gneiss had Sr ratios <strong>of</strong> approximately 0.7067, whereas <strong>the</strong><br />

soils on <strong>the</strong> Plio-Pleistocene volcanic rocks were approximately 0.7048. At 0.70518 <strong>the</strong><br />

mean elephant Sr value is closer to <strong>the</strong> Plio-Pleistocene volcanic rocks, suggesting a<br />

greater residence time in this region (see Figure 38 for map <strong>of</strong> study area).<br />

The researchers also warn that ivory may be more isotopically variable than bone,<br />

as illustrated by <strong>the</strong> carbon isotope data. They suggest that “in <strong>the</strong> face <strong>of</strong> such high<br />

within-tusk variability, it may be difficult to characterize a tusk or ivory artifact on <strong>the</strong><br />

basis <strong>of</strong> a single, small (for example, 20 mg) isotopic sample. Isotopic discrimination<br />

between populations could probably be obtained if multiple samples <strong>of</strong> different<br />

geologically controlled isotopes (Sr, Nd, and Pb) were examined for each artifact” (Koch<br />

et al. 1995: 1343). While this may hold true for elephants (particularly with carbon<br />

isotopes) because <strong>of</strong> <strong>the</strong>ir seasonal diet and large home-range, hippopotami are much less<br />

115

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