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These numeric ages assign the interglacial with at Mauer definitely to MIS 15, which is in full accordance with the above-mentioned biostratigraphic and geological evidence.Taking into account that the find layer was deposited in an interglacial stage, the bracketing data of M0503 and Mau 3 give additional support to this correlation (i.e., it is confirmed by a set of five dates).Age estimates for the Mauer mandible have been advanced previously.The Mauer sands are overlain by several Middle and Late Pleistocene glacial loess layers with interstratified interglacial paleosoil horizons, which constrain the age of the fossil to older than 350 ka (3).Hence, the interglacial represented by the Mauer lower sands is usually correlated with MIS 13 or MIS 15, orbitally tuned dates of 478–533 ka and 563–621 ka, respectively (6).In view of the importance of this site for documenting the appearance of in Europe, more accurate dating is desirable.

Thus, they belong to the Brunhes chron and are younger than 780,000 y (3).

This procedure leads to an apparent systematic underestimation of the ESR-US ages in comparison with the other samples extracted from the same fluvial unit.

The results obtained should be treated as minimum ages and cannot be considered in the geochronological interpretation.

The ages obtained for the four other teeth are, respectively, 624 79/−73 and 627 73/−71 ka for the lower sands and 458 39/−37 and 502 43/−41 ka for the upper sands (Fig. in terms of bio- and lithostratigraphy, as well as depth in the deposits.

The two sand samples Mau 1 and Mau 2 were taken 0.5 m below and above the gravel bed.