Foraminiferal assemblages as flandrian palaeo-environmental indicators
Abstract The sediments deposited during the Flandrian Stage in Swansea Bay, South Wales, have been sampled by offshore gravity coring and drilling, and by drilling in the intertidal and supratidal zones. Sedimentological and microfaunal analyses have revealed that the late Devensian boulder-clay surface was progressively transgressed over the period 10,000–2,500 years B.P., and that a sequence of environments from the supralittoral marsh through high mudflats, low mudflats, littoral and sublittoral sandflats developed; each palaeoenvironment is characterised by its own, distinctive foraminiferal assemblage, with indigenous and allochthonous components.