In this paper, the small mammals recovered from sediments associated with the West Runton Elephant has been analysed and compared with sites in other parts of Europe. Major taxonomical problems are indicated and we suggest ways of utilising such morphological complexity to refine biostratigraphical and chronostratigraphic attributions.The micromammal assemblage from the West Runton Elephant Site so far totals 16 species from the West Runton Forest Bed (WRFB). There are strong similarities with the arvicoliG VSHFWUXP RI EDVDO OD\HU + LQ WKH .RQČSUXV\ & SURILOH &]HFK Republic), which accumulated under cooler conditions preceding the thermal maximum of an early Middle Pleistocene interglacial. Rare steppic indicators (e.g. Cricetus) at West Runton also imply a somewhat cooler and more continental climate than the present day, but overall the fauna is fully temperate in character. West Runton shares several stratigraphically significant small mammal taxa with Voigtstedt (Central Germany) and morphometric comparisons suggest that Voigtstedt may be slightly younger than West Runton. The presence of Mimomys savini, with a latest occurrence in the early part of Marine Isotope Stage (MIS) 15, together with the palaeomagnetic evidence suggests the WRFB may have been emplaced during the early part of MIS 17. However, given the complexity of the marine isotope curve during the early part of the Brunhes Chron and differences between global and A c c e p t e d m a n u s c r i p t A c c e p t e d m a n u s c r i p t -2 -25.10.2008 regional climatic evolution, it is difficult to assign the normally magnetized WRFB to a particular Marine Isotope Stage (MIS).