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- W2181920524 abstract "A new integrated calcareous plankton biostratigraphy for the Mediterranean has been developed in the last few years which allows the continuous Plio-Pleistocene sedimentary sequence recovered at Site 653 to be rather precisely corre lated to other Leg 107 Sites and to sedimentary sequences on land. Although no magnetostratigraphy is available from Site 653, the biostratigraphic correlations to magnetostratigraphically controlled Mediterranean sections allow the se quence at Site 653 to be indirectly correlated to the geomagnetic reversal timescale. The correlation of the chronostratig raphy at Site 653 to the Plio-Pleistocene proposed stratotype sections indicates several anomalies in the time coverage of the stratotype sections. Hiatuses are present at the top of the Zanclean stratotype section at Capo Rossello and at the base of the Piacenzian stratotype section (in the Arda valley). In addition the Piacenzian stratotype section does not reach the Plio-Pleistocene boundary. There is therefore a gap of about 0.85 m.y. which is not covered by a stratotype section. As the top of the Piacenzian stratotype corresponds to a rather important climatic event (the onset of Northern Hemisphere Glaciation and the Glacial Pliocene), we advocate maintaining the Piacenzian as a chronostratigraphic unit and propose a threefold subdivision of the Pliocene. For the early Pleistocene, the previously proposed stratotype sections also do not adequately cover the time interval. For example, the Calabrian and Sicilian stratotype sections largely overlap. It has been suggested that the Calabrian stage be abandoned and that the Santernian, Emilian, and Si cilian be combined into a single stage, referred to as the Selinuntian." @default.
- W2181920524 created "2016-06-24" @default.
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- W2181920524 date "1990-02-01" @default.
- W2181920524 modified "2023-09-27" @default.
- W2181920524 title "Pliocene-Early Pleistocene Chronostratigraphy and the Tyrrhenian Deep-Sea Record from Site 653" @default.
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- W2181920524 doi "https://doi.org/10.2973/odp.proc.sr.107.185.1990" @default.
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