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Several biostratigraphic intervals are distinguished in the Miocene of the Western Mediterranean temperate area (DSDP, Site 372, East Menorca Rise, Balearic Basin). Evolutionary trends in the Globorotalia scitula praescitula, Globorotalia archeomenardii, Globorotalia praemenardii, and Globorotalia menardii plexus from Langhian to early Tortonian are used in an attempt to define biostratigraphic intervals. Characteristics of the penultimate chamber and carinal development are analyzed. Evolution of thick-walled forms shows the same trends as in thinwalled forms. Broad scale correlations with tropical sequences are recognized. Several morphotypes seem to be restricted to temperate areas. One new species (Globorotalia magnified) is described and illustrated.

Morphological Investigations on the Genus Globorotalia from Site 372