Upton Warren, Worcestershire. The fossils occur in several extensive lenticular bands of silt
in the lower half of a gravel succession. From the stratigraphy and a radiocarbon age of 42
000 years, the deposits are ascribed to the beginning of the Gottweig Interstadial,
immediately following the maximum of the Midland Irish Sea Glaciation. The latter is thus
considered to belong to the last and most severe episode of the Early Würm. The silt bands …