Villafranchian

Villafranchian age (/ˌvɪləˈfræŋkiən/ VIL-ə-FRANK-ee-ən) is a period of geologic time (3.5–1.0 Ma)^[1][2]: 7 spanning the Late Pliocene and Early Pleistocene used more specifically with European Land Mammal Ages. Named by Italian geologist Lorenzo Pareto^[3] for a sequence of terrestrial sediments studied near Villafranca d'Asti, a town near Turin,^[4] it succeeds the Ruscinian age, and is followed by the Galerian.

Neogene ELMMZ
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−20 — – −10 — – 0 —	Messinian                     MN 1 MN 2 MN 3 MN 4 MN 5 MN 6 MN 9 MN 10 MN 11 MN 12 MN 13 MN 14 MN 15 MN 16 MN 17 MN 18	Mio- cene Plio- cene Pleistocene Aquitanian Burdigalian Langhian Serravallian Tortonian MN 7/8 Zanclean Piacenzian Gelasian Agenian Orleanian Astaracian Vallesian Turolian Ruscinian Villafranchian Chronostratigraphy ELMMZ Zones Age (Ma)

The Villafranchian is sub-divided into six faunal units based on the localities of Triversa, Montopoli, Saint-Vallier, Olivola, Tasso and Farnetta.^[2]: 149

A major division of both geological deposits and time, the Villafranchian is significant because the earliest hominids that clearly evolved into modern man (the australopithecines) appeared within it.^[4] The Villafranchian is partially contemporaneous with the Blancan Stage of North America.^[4]

Many animals and their extinct ancestors evolved during the Villafranchian, including the Red fox, Least weasel, Moorhen, Etruscan bear, and Panthera gombaszoegensis.

The beginning of the Villafranchian is typically defined by the first appearance of the bovid genus Leptobos in Italy, dated to around 3.5-3.6 million years ago (mya). The beginning of the Middle Villafranchian is defined by the "elephant–Equus event" denoting the first appearance of Mammuthus meridionalis and Equus stenonis, thought to be around 2.5-2.6 mya. The beginning of the Late Villafranchian was formerly typically defined by the "Wolf event", the first appearance of Canis etruscus , but this was later considered to be diachronous. It was later proposed that the boundary be placed at the first appearance of the giant hyena Pachycrocuta brevirostris approximately 1.8 mya.^[5]

References

1. Rook, Lorenzo; Martínez-Navarro, Bienvenido (2010). "Villafranchian: The long story of a Plio-Pleistocene European large mammal biochronologic unit". Quaternary International. 219 (1–2): 134–144. Bibcode:2010QuInt.219..134R. doi:10.1016/j.quaint.2010.01.007.
2. The Pleistocene Boundary and the Beginning of the Quaternary edited by John A. Van Couvering. Cambridge University Press 1997
3. Fossil Mammals of Asia: Neogene Biostratigraphy and Chronology, edited by Xiaoming Wang, Lawrence J. Flynn, Mikael Fortelius
4. "Villafranchian". archaeologywordsmith.com. Archived from the original on 2012-06-11.{{cite web}}: CS1 maint: unfit URL (link)
5. van Kolfschoten, T. (2013-01-01), "QUATERNARY STRATIGRAPHY | Continental Biostratigraphy", in Elias, Scott A.; Mock, Cary J. (eds.), Encyclopedia of Quaternary Science (Second Edition), Amsterdam: Elsevier, pp. 206–214, ISBN 978-0-444-53642-6, retrieved 2021-10-31