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It was found in in a layer below the Jaramillo subchron and was attributed to loess L L15 in the Chinese loess-palaeosol sequence, with an estimated age of ca. Here, we demonstrate that there is a stratigraphical hiatus in the Gongwangling section immediately below loess 15, and the cranium in fact lies in palaeosol S S22 or S23, the age of which is ca. Closely spaced palaeomagnetic sampling at two sections at Gongwangling and one at Jiacun, 10 km to the north, indicate that the fossil layer at Gongwangling and a similar fossil horizon at Jiacun were deposited shortly before a short period of normal polarity above the Olduvai subchron. This is attributed to the Gilsa Event that has been dated elsewhere to ca. Our investigations thus demonstrate that the Gongwangling cranium is slightly older than ca.