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Site 372 (40°01.86'N, 04°47.79'E) is on the East Menorca Rise (Figure 1). The present depth of the sea floor is 2734 meters. Forty-six cores were recovered from the site; the total penetration of 885 meters. The section penetrated includes four lithologic units: Unit I, Pliocene-Quaternary nannofossil marls; Unit II, upper Miocene gypsum and dolomitic marls; Unit III, lower to middle Miocene nannofossil marls to marlstones; and Unit IV, lower Miocene mudstones to nannofossil marlstones. Eleven samples were examined for dinoflagellate cysts from Cores 9, 12, 28 through 35, and 46. The transitional contact between Unit II (evaporitic unit) and Unit III(pre-evaporitic unit) occurs in Core 9. Core 12 and Cores 28 through 33 belong to Unit III (Serravallian to upper Burdigalian). This unit appears to be a transitional zone and consists mainly of nannofossil marls (the carbonate content ranges from 35% to 60%). The remaining cores comprise Unit IV(Burdigalian), and Core 46 was taken from the bottom of the hole. Unit IV is distinguished from Unit III by its high clay content (CaCO3 ranges from 15% to 30%). Samples of about 10 grams were processed by using a standard hydrofluoric acid/flotation technique and residues were mounted in glycerine jelly. Slides have been deposited at the Institute of Paleontology, Modena University, Italy, under Catalog Nos. 18842-18930.

Dinoflagellate Cysts in Deep-Sea Cores from DSDP Site 372, East Menorca Rise