Villanyian

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Villanyian age is a period of geologic time (3.4—1.8 Ma) within the Pliocene used more specifically with European Land Mammal Ages. It precedes the Ruscinian age and overlaps the early Piacenzian and Zanclean ages. [1]

The Pliocene Epoch is the epoch in the geologic timescale that extends from 5.333 million to 2.58 million years BP. It is the second and youngest epoch of the Neogene Period in the Cenozoic Era. The Pliocene follows the Miocene Epoch and is followed by the Pleistocene Epoch. Prior to the 2009 revision of the geologic time scale, which placed the four most recent major glaciations entirely within the Pleistocene, the Pliocene also included the Gelasian stage, which lasted from 2.588 to 1.806 million years ago, and is now included in the Pleistocene.

The Ruscian age is a period of geologic time within the Pliocene used more specifically with European Land Mammal Ages. It precedes the Villanyian age and follows the Turolian age. The Ruscian overlaps the early Piacenzian and Zanclean ages.

The Piacenzian is in the international geologic time scale the upper stage or latest age of the Pliocene. It spans the time between 3.6 ± 0.005 Ma and 2.588 ± 0.005 Ma. The Piacenzian is after the Zanclean and is followed by the Gelasian.

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