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late pleistocene population interaction in western europe

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there has been a climatic deterioration dur<strong>in</strong>g the occupation of the site, possibly between<br />

the end of the Châtelperronian and the beg<strong>in</strong>n<strong>in</strong>g of the Aurignacian I.<br />

Figure 69. Proportions of re<strong>in</strong>deer (<strong>in</strong> NISP) <strong>in</strong> the macrofaunal samples from Sa<strong>in</strong>t-<br />

Césaire compared to proportions of narrow-skulled voles (<strong>in</strong> MNI) <strong>in</strong> the microfaunal<br />

samples from the same site. The wide dashed l<strong>in</strong>es <strong>in</strong> the narrow-skulled vole l<strong>in</strong>e <strong>in</strong>dicate<br />

small sample size. Re<strong>in</strong>deer data from Tables 13 and 14 and microfaunal data from Table<br />

18.<br />

Tak<strong>in</strong>g <strong>in</strong>to account the above cautionary notes about the stratigraphic <strong>in</strong>tegrity of<br />

this site, data for Roc de Combe also <strong>in</strong>dicate an <strong>in</strong>crease <strong>in</strong> abundance of the narrow-<br />

skulled vole, which rises from 12.9% (n=31) <strong>in</strong> the Châtelperronian to 29.2% (n=294) <strong>in</strong><br />

the Early Aurignacian occupations (Marquet 1993:73). The difference between the two<br />

375

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