THE OCCURRENCE OF SUIDAE (ARTIODACTYLA, MAMMALIA) IN THE LATE VILLAFRANCHIAN FAUNA OF CRIMEA (TAURIDA CAVE, EARLY PLEISTOCENE) AND THE “SUID GAP” HYPOTHESIS
- Authors: Lopatin A.V.1
-
Affiliations:
- Borisyak Paleontological Institute, Russian Academy of Sciences
- Issue: Vol 524, No 2 (2025)
- Pages: 270–275
- Section: PALEONTOLOGY
- Submitted: 08.12.2025
- Published: 15.10.2025
- URL: https://journal-vniispk.ru/2686-7397/article/view/356837
- DOI: https://doi.org/10.7868/S3034506525100119
- ID: 356837
Cite item
Abstract
A fragment of the partially mineralized lower molar M1 of a fossil pig Sus sp. is described from the main bone level of the Taurida cave locality (central Crimea, Russia), dated to the Late Villafranchian (Early Pleistocene, MO1 zone, 1.8–1.6 Ma). Like the materials from the coeval Dmanisi locality in Georgia, this extremely rare find (so far the only one of many thousands of vertebrate remains from the Taurida cave) may indicate a sharp decline in number (but not complete disappearance) of Suidae in Eastern Europe and Western Asia around 1.8 Ma, which clarifies the ideas associated with the “suid gap” hypothesis about the absence of pigs in Europe in the interval of 1.8–1.2 Ma.
About the authors
A. V. Lopatin
Borisyak Paleontological Institute, Russian Academy of Sciences
Author for correspondence.
Email: alopat@paleo.ru
Academician of the RAS Moscow, Russia
References
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