Calcareous nannofossils were examined from 15 holes at nine sites, but Eocene to Miocene calcareous nannofossils were found only from Holes 782A, 784A, 786A, and 786B. An attempt was made to correlate the magnetochronological data with the first or last occurrences of the following species: Sphenolithus distentus, Reticulofenestra bisecta, Reticulofenestra reticulata, and Cyclicargolithus floridanus abisectus n. comb. Analyses of sediment-accumulation rates indicate that the rates increased gradually from the Eocene to Miocene. This is especially evident since the late Miocene in Hole 782A. In different parts of the Izu-Bonin forearc basin, however, the rate is not everywhere the same and appears to vary according to the import of volcanogenic materials. -from Authors
CITATION STYLE
Yulin Xu, & Wise, S. W. (1992). Middle Eocene to Miocene calcareous nannofossils of Leg 125 from the western Pacific Ocean. Proc., Scientific Results, ODP, Leg 125, Bonin/Mariana Region, 43–70. https://doi.org/10.2973/odp.proc.sr.125.142.1992
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