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Nannofossil and planktic foraminiferal evidence from three marginal-marine sections in the Indo-Pacific region challenges the timing of the Oligocene-Miocene boundary. The dataset suggests the planktic foraminiferal zones N.3 and N.4 should be combined, as the first appearance of Globigerinoides quadrilobatus primordius is depth-dependent and occurs earlier in shallow settings. It proposes a buffer zone between the extinction of Sphenolithus ciperoensis and the appearance of Sphenolithus belemnos to account for transitional biostratigraphic events.
Primary data format appears to be a journal article (HTML/PDF) rather than a structured data table; the actual dataset may be embedded within the publication.