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Among the Cananéia mangrove swamp (extreme south of São Paulo's coastline), it was identified within the Archeological Programme of the Lower Ribeira Valley, eight shell middens within which could be found archeological submerged traces.Aiming at the understanding of these shell middens occurrence and the contextualisation in space and time in relation to the holocenic variations of the sea level, this monograph was based on an adaptation of the Vibracoring technique, underwater archeological methods and techniques, on the geoarcheological interpretation of Waters (1992), and on the studies of Formation Process adopted by Stein (1992).Thus, the shell middens preserving potential and distribution in this area shows a strong correlation with the sea related level changes, that occurred after the last holocenic regressive maximum.These evidences also indicated that not only were there real chances that completely submerged shell midden were preserved but also that it is not always that sites related to an ancient sea level ended up into being destroyed or kept submerged.In some cases, some that should have been destroyed or kept submerged, are seen in land covered by recent coast sediments or protected by any geological feature.Besides contributing to the development and maturation of the scientific underwater archeology and for the studies of the curves of the sea related level changes the research also identified some important evidences to the understanding of the shell middens phenomenon such as the occurrence of stratigraphic sequences that attach functional differences and an intention in building some sites, such as the one dated back to almost 8.000 years ago when Cananéia was first inhabited by the people of the shell middens.
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