![]() Tropical planktic foraminifera occur throughout each sequence at all sites. (1985) to provide an accurate chronology to compare interocean stratigraphic ranges of late Neogene planktic foraminifera. ![]() A consistent stratigraphy was developed between sites 214 and 586 B using graphic correlation and was integrated with the paleomagnetic time scale of Berggren et al. ÐDeep sea cores from sites 214 and 758 A (Ninetyeast Ridge, northeast Indian Ocean), 761 B (Wombat Plateau, northeast Indian Ocean) and 586 B (Ontong Java Plateau, Tropical Paci®c) are ideally located for comparison of late Neogene planktic foraminiferal bio-geography and paleoceanographic records of tropical Indian and Paci®c oceans to infer the timing of closing of the Indonesian Seaway. ![]()
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