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386 BARYSHNIKOV & FORONOVA CAD. LAB. XEOL. LAXE 26 (2001) Based on the results of this analysis, we may conclude that p4 proportions in U. rossicus are similar to those of U. spelaeus, being different with those U. savini, and more sufficiently from U. deningeri. Among teeth of U. rossicus studied, the mean of the greatest length is at a maximum in Krasnodar and minimum in Kizel Cave (table 5), and the differences between them are reliable for this measurement (p
CAD. LAB. XEOL. LAXE 26 (2001) Pleistocene small cave Bear 387 Figure 10. Plot of centroids for each locality on the plane canonical variate 1 and 2 for m1. Table 7. Correlations of canonical variate for m1. samples with the exception of U. rossicus from Siberia/U. savini. Thus the m1 proportions among U. rossicus are rather different, but demonstrate more resemblance with those in U. savini, than with other cave bears (in the least degree with U. spe - laeus). In the samples of U. rossicus, the longest m1 has been recorded in Kizel Cave (table 5), however its differences in this measurement with Siberian and Krasnodar specimens are not statistically reliable. In U. spelaeus, the crown is most narrow at the trigonid and talonid junction but in U. rossicus, U. savini and U. deningeri, this place is approximately as wide as trigonid. U. etruscus, U. maritimus and U. arctos show the complicated metaconid and entoconid, the latter consisting of one or two cusps. Cave bears demonstrate a trend toward further development of entoconid portion. In U. rossicus, U. savini and U. deningeri, it is formed by two or three adjacent tubercles, while in U. spelaeus the entoconid more often has a shape of two large well-separated tubercles of almost equal height. Thus, U. rossi - cus demonstrates a rather primitive m1 structure. m2. This tooth is rectangular in shape, with talonid wider than trigonid. The
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282 VILA TABOADA et al. CAD. LAB. X
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290 WEINSTOCK, J. CAD. LAB. XEOL. L
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