The Neogene is the geological period from 23.04 to 2.58 million years ago in the consulted chart. It contains the Miocene and Pliocene, between the Palaeogene and Quaternary.[ref]
International Chronostratigraphic Chart by International Commission on Stratigraphy (2026-06). Cenozoic and Mesozoic columns; numerical ages in Ma
The Pliocene is the younger Neogene epoch, approximately to million years ago.[ref]
International Chronostratigraphic Chart by International Commission on Stratigraphy (2026-06). Pliocene row
It is included in the long marine oxygen isotope ratio stack used to compare earlier ocean conditions with those of the Pleistocene. Aligning records makes their temporal patterns comparable; it does not turn one isotope measurement into a unique independent temperature measurement.[ref]A Pliocene-Pleistocene stack of 57 globally distributed benthic oxygen-isotope records by Lorraine E. Lisiecki and Maureen E. Raymo. Abstract and introduction: Pliocene coverage and climatic interpretation
The Miocene is the older Neogene epoch, approximately to million years ago.[ref]
International Chronostratigraphic Chart by International Commission on Stratigraphy (2026-06). Miocene row
Dating a rock to this interval places it before the Pliocene; interpreting the environment in which it formed additionally requires observations such as sedimentary rock structure, composition and fossils. An age label and an environmental reconstruction answer different questions. Articles by others on the same topic
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