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The global nannofossil zonations of Martini (1971), Bukry (1973, 1975, 1978), and Okada and Bukry (1980) have been successfully applied to thick Eocene sequences in the eastern Gulf (Siesser, 1983), Virginia (Gibson et al., 1980), and South Carolina (Hazel et al., 1977) Coastal Plains, resulting in detailed biostratigraphic subdivision of the Eocene strata in those areas. However, little more than reconnaissance nannofossil biostratigraphy has been accomplished in the North Carolina Eocene which is typically thin and poorly exposed (Turco et al., 1979; Worsley and Turco, 1979; Hazel et al., 1984). Furthermore, nannofossil assemblages in the Eocene Castle Hayne Limestone...

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