Late Pleistocene molluscan assemblages from the coral reefs of the Kenya coast

Since the Last Interglacial, there have been profound changes in the nature of the fringing reef along the Kenya coast. These are most apparent in the back-reef region where a marked decline in habitat diversity has led to a significant reduction in the variety of molluscan assemblages. Despite dramatic changes in the composition of these assemblages, very few species have become extinct. The four late Pleistocene species apparently missing from the Recent fauna of the Kenya coast still occur further east in the Indonesia-West Pacific region. There is evidence to suggest that range retractions from the periphery to the core region occurred at the same time in other parts of the Indo-Pacific province too. The province's margins may well have been more susceptible to fluctuations in certain environmental parameters, such as temperature, during the Pleistocene climatic cycles.