Reworking processes and deposits in coral reefs during (very) high-energy events: Example from a Pleistocene coral formation (125Â ka), La Désirade Island, Lesser Antilles

The reworked deposits are interbedded between two coral reef levels, of which the main coral-species vertical succession should record the end of Marine Isotope Stage 5e sea-level rise. Thus, reworking is believed to occur during the transitional stage between a glacial and an interglacial period.