taxonID	type	description	language	source
732A87EDFFB4FFD83C22FB58D2212694.taxon	description	(Figs 2 / 1, 3 – 7) B. viridis is represented on the slab by a partial skeleton and some isolated bones. The partial skeleton is exposed in ventral view (Fig. 2 / 1). Only a few skull bones are preserved from this specimen, as well as the almost complete vertebral column.	en	Szentesi, Z. (2014): Green toad (Anura: Bufonidae) skeleton from the Upper Pleistocene of Hungary (Nagyharsány Crystal Cave, Villány Hills). Fragmenta Palaeontologica Hungarica 31: 117-124, DOI: 10.17111/FragmPalHung.2014.31.117, URL: https://doi.org/10.17111/fragmpalhung.2014.31.117
732A87EDFFB4FFD83C22FB58D2212694.taxon	description	The isolated bones probably represent one or more specimens of green toads on this slab because they are significantly smaller than the bones of the above described partial skeleton. Differences in bone size and immaturity of these isolated bones suggest that these fossils belong to one or more younger specimens. The dorsal crest, similarly to other toads (e. g. HOLMAN 1998; SANCHÍZ 1998), is absent on this ilium (Fig. 2 / 3), and on the basis of the two-lobed dorsal protuberance this specimen belongs to Bufo viridis. The pars epicoracoidalis on the relatively elongat- ed coracoid (Fig. 2 / 4) is flat-rounded dorsoventrally while the bends of the margo fenestralis and posterior are similar. The deep, rounded fossa under the capitulum and laterally under the rim of the joint on the radio-ulna (Fig. 2 / 5) is typical of Bufo viridis (e. g. BAILON 1999) just like the distally well-defined sulcus longitudinalis (Fig. 2 / 5 – 7). The two isolated vertebrae (Fig. 2 / 6) are similar to those described above on the partial skeleton. These are vertebrae IV and V of the vertebral column of a green toad. Anura indet. (Fig. 2 / 2) The red clay slab also contains many fragmentary bones of Anura indet. by an angulosplenial, frontoparietals and mainly shin-bones, e. g. os cruris.	en	Szentesi, Z. (2014): Green toad (Anura: Bufonidae) skeleton from the Upper Pleistocene of Hungary (Nagyharsány Crystal Cave, Villány Hills). Fragmenta Palaeontologica Hungarica 31: 117-124, DOI: 10.17111/FragmPalHung.2014.31.117, URL: https://doi.org/10.17111/fragmpalhung.2014.31.117
