Pleistocene and Oligocene-Miocene calcareous nannofossils from the Sumisu Rift and Izu-Bonin Forearc Basin

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Abstract

During ODP Leg 126, three expanded Pleistocene sections were recovered from the active backarc rift (Sumisu Rift) and three expanded Oligocene-Miocene sections from the forearc basin of the Izu-Bonin volcanic island arc. Quantitative analysis of the Pleistocene nannofossils revealed five major assemblages between 0 and 1.0 Ma. These assemblages are largely synchronous with similar assemblages recognized from tropical and subtropical regions, and can be used for finer subdivision of the Pleistocene than that based on standard Pleistocene nannofossil datums. The Oligocene-Miocene sections contain several hiatuses. Biochronology of several nannofossil datums at Leg 126 sites indicate that Sphenolithus distentus, Sphenolithus ciperoensis, Cyclicargolithus floridanus, and Discoaster kugleri have diachronous occurrences compared with other sites in the western Pacific Ocean and Philippine Sea. -from Authors

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APA

Firth, J. V., & Isiminger-Kelso, M. (1992). Pleistocene and Oligocene-Miocene calcareous nannofossils from the Sumisu Rift and Izu-Bonin Forearc Basin. Proc., Scientific Results, ODP, Leg 126, Bonin Arc/Trench System, 237–262. https://doi.org/10.2973/odp.proc.sr.126.131.1992

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