Calcareous Plankton Pliocene-Pleistocene Biostratigraphy in the Tyrrhenian Sea (Western Mediterranean, Leg 107)

The distribution of stratigraphically important calcareous nannofossils and planktonic foraminifera has been investigated in the Pliocene-Pleistocene sequences of ODP Sites 652, 653, and 654. Semiquantitative and quantitative methods have been used, and an optimum relative sequence of bioevents base...

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Bibliographic Details
Main Authors: Glacon G., Sprovieri R., RIO, DOMENICO
Other Authors: Kastens K.A., Mascle J., Glacon, G., Rio, Domenico, Sprovieri, R.
Format: Book Part
Language:English
Published: ODP, Texas A&M University, College Station; UK distributors, IPOD Committe, NERC, Swindon 1990
Subjects:
Planktonic foraminifera
Online Access:http://hdl.handle.net/11577/2513662
https://doi.org/10.2973/odp.proc.sr.107.148.1990
Description
Summary:The distribution of stratigraphically important calcareous nannofossils and planktonic foraminifera has been investigated in the Pliocene-Pleistocene sequences of ODP Sites 652, 653, and 654. Semiquantitative and quantitative methods have been used, and an optimum relative sequence of bioevents based on the calcareous plankton groups has been established. About 30 bioevents in an interval of 5.0My are considered widely traceable in the area and resonably synchronous. On the basis of those events, a correlation among the three investigated sequences is presented.

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