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Constraining Holocene sea levels using U-Th ages of phreatic overgrowths on speleothems from coastal caves in Mallorca (Western Mediterranean)
(supprimer)
are in accord with an archaeologically estimated age for a drowned prehistoric construction at a depth of 1 m below current sea level in a cave from the same area. Speleothem δ13C and δ18O and chemical composition of cave pools provide supportive evidence
that phreatic overgrowths on speleothems (POS) reflect mixing between seawater and brackish water table.