Abstract
Th e Nagyharsany Crystal Cave is a new, probably Late Pleistocene palaeovertebrate locality, from where this is the fi rst report on the herpetofauna. Th e study revealed the presence of Bufo viridis (Anura) and Natrix sp., the appearance of which taxa suggests that the fossilifer- ous sediments were probably accumulated at the beginning of an interglacial phase in a steppe or woody steppe environment. With 2 fi gures.
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