Interpretación tafonómica de la malacofauna marina en el yacimiento neolítico de la Caserna de Sant Pau del Camp (Barcelona)

Abstract

The shell remains recovered at the ancient Neolithic site of Caserna de Sant Pau (Barcelona) are characterized by a large number of elements of the genus Glycymeris, many of them eroded by wave action. It is therefore surmised that the main part of the archaeomalacological record does not have an alimentary origin. Comparison with current taphonomic analyses could explain this archaeomalocological record as a natural accumulation of sea-borne deposits. However, geaoarchaeological studies demonstrate that the prehistoric seashore never reached the archaeological site, so this hypothesis must be invalidated. On the other hand, there is a clear spatial relationship between shells and Neolithic burials.