Abstract
The magnetostratigraphy of the mammal-bearing alluvial fan-fan delta sequences of the Fortuna basin (SE Spain) has
yielded an accurate chronology for the late Turolian (Messinian) basin infill. From early to late Messinian (at least between
6.8 and 5.7 Ma), the Fortuna basin records the sedimentation of alluvial-palustrine deposits over a confined shallow
basin.
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