AnimaliaNot EvaluatedacceptedspeciesAccepted
Palaeobatrachus robustus

Palaeobatrachus robustus

Hossini & Rage, 2000

GBIF:203870985

0year

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Descriptions(3)

Description. Frontoparietals are flat and thin. They represent small-sized individuals. The parasagittal ridges are well-developed and build the limit between the flat dorsal surface of the bones and somewhat concave orbital margins. The parasagittal ridges are very closely located near the midpoint of the bone and form a sandglass shape at the dorsal surface of the bone. The dorsal surface of the bone between the parasagittal ridges is irregular and pierced by small foramina (pineal foramen sensu Villa et al. 2016) and pits (Fig. 9 L). Posteriorly, the surface of the frontoparietal table is flat and rather smooth. The irregularities, if present, are weakly pronounced. The parasagittal ridges reach the paroccipital processes posteriorly (Fig. 9 I, K). The latter are not fully preserved. Only their bases are observable, which in turn, possess a crest. A smaller posterior median crest is present along the anteroposterior axis of the bone which starts from the posterior margin of the frontoparietal table. The posterior margin of the bone between the median margin and paroccipital process is arched and forms a " bilobed " outline (Fig. 9 K). The median crest is lower than the paroccipital processes. Judging from the preserved portions of the paroccipital process and posterior median process, a shorter length of the former in comparison to the latter can be assumed. In ventral view, the frontoparietal incrassation, visible only in HLMD-Ez 2077 (Fig. 9 J), representing the posterior portion of the bone, has a round outline with slightly prominent margins. No structure similar to the lanceolate area (sensu Rocek et al. 2015) is observable on the available frontoparietals. Premaxillae, maxillae, vomer: all three bones are fragmentarily preserved and do not allow any detailed description. The preserved teeth and tooth pedicles display diagnostic characters, such as the conical and slightly lingually bent ankylosed teeth. At the tooth basis, large and deep pits are preserved. The bicuspid tooth has a small labial and large apical cusps (Fig. 9 N, O, HLMD-Ez 2084). Angulars: in total, two angulars can be clearly assigned to this taxon. They are elongated and curved bones. The coronoid process is compact and can be oval to drop-shape (Fig. 9 P, Q). Its surface is concave, rather smooth and can possess tubercles (muscle scars). The Meckelian groove behind the coronoid process is broad and opens dorsally, whereas anteriorly, it is open laterally or slightly dorsolaterally. Ilium: The acetabular region of the ilium is robust. The dorsal prominence (sensu Gomez and Turazzini 2015) is not well-developed. The drop-shape dorsal protuberance (sensu Gomez and Turazzinin 2015) is large (Fig. 9 R) and can be weakly to moderately developed (Fig. 9 V). Its surface is rather smooth, and its small posterior portion is located above the anterior margin of the acetabular crest. The ventral acetabular expansion (also known as pars descendens) does not project ventrally, but it is massive in ventral / dorsal views (Fig. 9 R). The dorsal acetabular expansion (also known as pars ascendens), even if only fragmentarily preserved, is moderately developed. The ventral half of the acetabular fossa is massive. The well-developed ventral portion of the acetabular crest projects laterally and contributes to the ventroanterior surface of the acetabular region of the ilia. In larger individuals (e. g. HLMD-Ez 2080), an oval knob-like flat surface is present in the lateroventral cornet between the iliac shaft and acetabulum (Fig. 9 V). It represents most probably the attachment surface for the muscle iliacus internus (sensu Gomez and Turazzini 2015). In posterior view, the well-pronounced interiliac groove and laterally projecting acetabular crest are observable. The iliac shaft is moderately developed, lateromedially flattened and has a rather smooth surface.
Vasilyan, Davit, Cernansky, Andrej, Szyndlar, Zbigniew, Moers, Thomas (2022): Amphibian and reptilian fauna from the early Miocene of Echzell, Germany. Fossil Record 25 (1): 99-145, DOI: http://dx.doi.org/10.3897/fr.25.83781, URL: http://dx.doi.org/10.3897/fr.25.83781
Fig. 9 I-W
Vasilyan, Davit, Cernansky, Andrej, Szyndlar, Zbigniew, Moers, Thomas (2022): Amphibian and reptilian fauna from the early Miocene of Echzell, Germany. Fossil Record 25 (1): 99-145, DOI: http://dx.doi.org/10.3897/fr.25.83781, URL: http://dx.doi.org/10.3897/fr.25.83781
Material. Four frontoparietals HLMD-Ez 2076 - 2078, five ilia HLMD-Ez 2079 - 2081, two angulars HLMD-Ez 2082, 2083, five jaw bones HLMD-Ez 2084, 2085.
Vasilyan, Davit, Cernansky, Andrej, Szyndlar, Zbigniew, Moers, Thomas (2022): Amphibian and reptilian fauna from the early Miocene of Echzell, Germany. Fossil Record 25 (1): 99-145, DOI: http://dx.doi.org/10.3897/fr.25.83781, URL: http://dx.doi.org/10.3897/fr.25.83781

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Media Files(1)

Figure 9. Frogs from Echzell locality. Ilia of Pelophylax sp. HLMD-Ez 2089 (A, B) and HLMD-Ez 2090 (C, D). Ilia of Rana sp. HLMD-Ez 2093 (E, F) and HLMD-Ez 2094 (G, H). Palaeobatrachus robustus (I-W). Frontoparietals HLMD-Ez 2077 (I, J), HLMD-Ez 2078 (K) and HLMD-Ez 2076 (L, M). Jaw bone HLMD-Ez 2084 (N, O). Angulars HLMD-Ez 2083 (P) and HLMD-Ez 2082 (Q). Ilia HLMD-Ez 2079 (R-T) and HLMD-Ez 2080 (V, W). Bones are figured in (A, D, E, G, M, R, V) lateral, (B, C, F, H, S) posterior, (I, K, L, P, Q) dorsal, (J, O) ventral, (N) labial and (T, W) medial views. Scale bars: 1 mm.

Imageimage/png© Vasilyan, Davit;Cernansky, Andrej;Szyndlar, Zbigniew;Moers, ThomasVasilyan, Davit;Cernansky, Andrej;Szyndlar, Zbigniew;Moers, Thomas

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Amphibian and reptilian fauna from the early Miocene of Echzell, Germany

checklist

This dataset contains the digitized treatments in Plazi based on the original journal article Vasilyan, Davit, Cernansky, Andrej, Szyndlar, Zbigniew, Moers, Thomas (2022): Amphibian and reptilian fauna from the early Miocene of Echzell, Germany. Fossil Record 25 (1): 99-145, DOI: http://dx.doi.org/10.3897/fr.25.83781, URL: http://dx.doi.org/10.3897/fr.25.83781

Vasilyan D, Cernansky A, Szyndlar Z, Moers T, pensoft (2022). Amphibian and reptilian fauna from the early Miocene of Echzell, Germany. Plazi.org taxonomic treatments database. Checklist dataset https://doi.org/10.15468/fvb6q2 accessed via GBIF.org on 2026-06-15.

CC0Published 5/10/2022View dataset
GBIF Usage Key
203870985
Dataset Key
879a081e-5c23-41a3-b500-84ae793fb677
Origin
source
Backbone Key
8544224
Taxon ID
46723D41ED3552F993EF2C528E0E5C40.taxon
Last Crawled
6/9/2026
Last Interpreted
6/9/2026