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]
The Pliocene is the younger Neogene epoch, approximately to million years ago.[ref] 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]
The Miocene is the older Neogene epoch, approximately to million years ago.[ref] 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.

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