Abstract
Climate variability in the western Mediterranean is reconstructed for the last 4000 yr
using marine sediments recovered in the west Algerian-Balearic basin, near the Alboran
basin. Fluctuations in chemical and mineralogical sediment composition as well
as grain size distribution are linked to fluvial-eolian oscillations, changes in redox conditions
and paleocurrent intensity. Multivariate analyses allowed
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