The early Aptian transgression event in the United Kingdom

In the United Kingdom the base of the Aptian transgression is located at the base of the Perna Beds (on the Isle of Wight), although recent work on the magnetostratigraphy has indicated that this dating may be in error. Micropalaeontological work on the Isle of Wight sections has shown that the Perna Beds represent a complex event at the transition from a non‐marine to a marine succession. Foraminiferal and palynological data agree on this transition, although no biostratigraphically diagnostic taxa are present. The base of the Aptian is tentatively moved downwards to the level of the Barnes, High Sandstone Member (Vectis Formation). If correct, this realignment of the boundary would necessitate a revision of many stratigraphic ranges and diversity calculations.