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- W171420909 abstract "Publisher Summary This chapter discusses the present and future of the Miocene/Pliocene boundary. Aside from the fact that the definition and the location of a chronostratigraphic boundary is in the first place, a matter of nomenclature, one must not neglect its global importance as a reference point. In this way, the choice of a continuous boundary stratotype is a real scientific question. Nevertheless, such a choice is not devoid of a geopolitical aspect, all the Neogene stratotypes (including the boundary ones) being located in the northwestern and central Mediterranean region, and mostly in Italy. The first problem concerning the Miocene/Pliocene boundary, but not the least, is the large diachronism of the first appearance datum (FAD) of Globorotalia margaritae between the Atlantic Ocean and the Mediterranean Sea. There is no possibility to use the same biostratigraphic markers both in the Mediterranean and in the Atlantic for the recognition of the Miocene/Pliocene boundary. As a consequence, the present-day definition of the boundary in the Mediterranean region cannot have a worldwide significance." @default.
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- W171420909 date "1995-01-01" @default.
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- W171420909 title "Chapter A10 The miocene/pliocene boundary: Present and future" @default.
- W171420909 doi "https://doi.org/10.1016/s0920-5446(06)80014-2" @default.
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