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Ibérica na região de Trás-os-Montes (NE Portugal) - Universidade ...

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366 WITHALM, G. CAD. LAB. XEOL. LAXE 26 (2001)<br />

INTRODUCTION<br />

Since the work done by TORRES<br />

(1988) and KUNST (1989) there was not<br />

too much attention drawn to the metapodial<br />

bones of Ursus spelaeus and its pre<strong>de</strong>cessor,<br />

Ursus <strong>de</strong>ningeri.<br />

Torres tried to provi<strong>de</strong> a range of characters<br />

to differentiate U. spelaeus from U.<br />

<strong>de</strong>ningeri and U. arct<strong>os</strong> as well as a general<br />

<strong>de</strong>scription and comparison of the skeletal<br />

elements of these animals, collected in<br />

sites from Spain. Kunst tried to use the<br />

metapodial bones to exemplify differences<br />

between several cave bear sites of Austria.<br />

RESULTS<br />

The current investigation is aimed at<br />

the evolutio<strong>na</strong>ry changes of the metapodial<br />

bones throughout time by means of<br />

morphometrics. Therefore eight different<br />

measurements were taken and five indices<br />

were calculated from 4459 metapodial<br />

bones from U. spelaeus and U. <strong>de</strong>ningeri<br />

from eight different sites in Austria and<br />

Italy.<br />

The measurements are: proximal<br />

width and <strong>de</strong>pth, smallest diaphyseal<br />

width and <strong>de</strong>pth, distal width and <strong>de</strong>pth,<br />

distal epicondyleal width and greatest<br />

length. The indices are: proximal area,<br />

smallest diaphyseal area, distal area, in<strong>de</strong>x<br />

of robustness and K–in<strong>de</strong>x, the latter<br />

according to GUZVICA & RADANO-<br />

VIC–GUZVICA (2000).<br />

The sites from Austria and Italy are:<br />

Hundsheimer Spalte, Repolust cave,<br />

Schwabenreith cave, Ramesch cave,<br />

Conturines cave (Southern Ty r o l ) ,<br />

Figure 1. Measurements taken from metapodials.<br />

Graphics: from TORRES (1988), altered.<br />

Her<strong>de</strong>ngel cave, Win<strong>de</strong>ner Bärenhöhle<br />

and Gamssulzen cave.<br />

Basic statistical a<strong>na</strong>lysis was carried<br />

out on this data set to see wether there is<br />

a p<strong>os</strong>sibility to sex a population or not, for<br />

comparison with the results from<br />

OSWALD (1999). The obtained results<br />

are totally inhomogenous and so it is not<br />

p<strong>os</strong>sible to sex a cave bear fau<strong>na</strong> by means<br />

of metapodials. Further investigation showed<br />

that there is a correlation between the<br />

in<strong>de</strong>x of robustness, the K–In<strong>de</strong>x and the<br />

smallest diaphyseal area and the stratigraphic<br />

p<strong>os</strong>ition of the site. Therefore it is<br />

not only p<strong>os</strong>sible to predict the age of a<br />

cave bear population by a<strong>na</strong>lysing the evo-

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