ABSTRACT
Here we describe a formerly unrecognized dry spell dated at between c. 4330 and 3950
radiocarbon years BP, and located in the Puerto de Mazarr�n (Murcia, southeastern Spain).
The palaeoclimatical inference is provided by halite levels within a long sequence of a
multiple core study carried in a palaeo-lagoon. The lithological inference is corroborated by
palynological records involving a forest depletion. The event is also linked to a population
decline in the study region