Vipera berus (Linnaeus, 1758) remains from the Late Pleistocene of Slovakia

IVANOV, Martin and Andrej ČERŇANSKÝ. Vipera berus (Linnaeus, 1758) remains from the Late Pleistocene of Slovakia. Amphibia-Reptilia. LEIDEN: BRILL ACADEMIC PUBLISHERS, 2017, vol. 38, No 2, p. 133-144. ISSN 0173-5373. Available from: https://dx.doi.org/10.1163/15685381-00003095.

Basic information

• Original name: Vipera berus (Linnaeus, 1758) remains from the Late Pleistocene of Slovakia
• Authors: IVANOV, Martin (203 Czech Republic, guarantor, belonging to the institution) and Andrej ČERŇANSKÝ (703 Slovakia).
• Edition: Amphibia-Reptilia, LEIDEN, BRILL ACADEMIC PUBLISHERS, 2017, 0173-5373.

Other information

• Original language: English
• Type of outcome: Article in a journal
• Field of Study: 10600 1.6 Biological sciences
• Country of publisher: Netherlands
• Confidentiality degree: is not subject to a state or trade secret
• WWW: URL
• Impact factor: Impact factor: 1.105
• RIV identification code: RIV/00216224:14310/17:00096462
• Organization unit: Faculty of Science
• Doi: http://dx.doi.org/10.1163/15685381-00003095
• UT WoS: 000405024000002
• Keywords in English: Central Europe; Late Pleistocene; osteology; palaeoecology; Viperinae
• Tags: NZ, rivok

Abstract

Completely preserved specimens of fossil snakes are extremely rare and ophidian palaeontologists are usually dependent only on disarticulated elements of a postcranial skeleton. Here we present an unusually well-preserved specimen of a small viperid snake from the Late Pleistocene firm travertine at the famous Gánovce-Hrádok Neanderthal mound in Slovakia. The complex study of both cranial and axial skeleton with well-preserved maxilla and basiparasphenoid confirms the presence of a viper from the Vipera berus species group, and recent distribution of V. berus species complex members supports identification of these preserved remains as belonging to the common adder, V. berus (Linnaeus, 1758). Associated faunal assemblages of the MFG-C and D mammalian fauna groups reported from the firm travertine indicate a humid climate in a predominantly woodland environment with typical forest species in the Gánovce-Hrádok vicinity throughout the Eemian optimum, and mixed forest and steppe environments in the late Eemian to early Weichselian stages. Occurrence of V. berus documents the presence of open or semi-open biotopes with low vegetation. Although V. berus occurs in the Quaternary glacial/interglacial cycle and throughout the entire warm part, it never dominated herpetofaunal assemblages during the climatic optimum. Therefore, the presence of V. berus most likely indicates late Eemian or early Weichselian (interstadial) climatic conditions.