Paramblypterus, SAUVAGE, 1888

Štamberg, Stanislav, 2021, Actinopterygians Of The Broumov Formation (Permian) In The Czech Part Of The Intra-Sudetic Basin (The Czech Republic), Fossil Imprint 77 (1), pp. 73-101 : 86

publication ID

https://doi.org/ 10.37520/fi.2021.008

publication LSID

lsid:zoobank.org:pub:EEA2111C-2B5B-46E4-B267-8CF33DC54AB4

persistent identifier

https://treatment.plazi.org/id/895587F6-FFE8-FFC3-7800-F897FA44EA7C

treatment provided by

Felipe

scientific name

Paramblypterus
status

 

Paramblypterus cf. rohani

Text-figs 8b, c View Text-fig , 9–12 View Text-fig View Text-fig View Text-fig View Text-fig

M a t e r i a l. 210 fragments of bodies and isolated bones from the localities of the Otovice Limestone Horizon (Textfig. 1b).

R e m a r k s. Paramblypterus rohani (HECKEL in HECKEL et KNER, 1861) was first described from the Vrchlabí

Formation (Asselian) of the Krkonoše Piedmont Basin ( Heckel and Kner 1861, Fritsch 1895, Heyler 1969, Štamberg 1976). Heyler (1971) also documented this species from the Autun Basin in the French Massif Central. Numerous anatomical features such as the skull roof bones, maxilla and bones of the cheek correspond with the features described by Dietze (1999) in Paramblypterus duvernoyi ( AGASSIZ, 1833). It is likely that the species Paramblypterus rohani belongs within a synonymy of Paramblypterus duvernoyi ( Dietze 1999, Štamberg 2018). However, a thorough comparison of the two species has not yet been made and the species Paramblypterus rohani is still kept as valid. For this reason, the material described in the following article is compared with the specimens of Paramblypterus rohani known from the Vrchlabí Formation of the Krkonoše Piedmont Basin.

D e s c r i p t i o n. Bodies of fusiform shape and a total length up to 172 mm. None of studied specimens had a complete undeformed body shape ( Text-fig. 8b, c View Text-fig ). Body fragments exhibited the slightly arched anterior part of the body ( Text-fig. 10f View Text-fig ).

Rostral part and skull roof ( Text-figs 9 View Text-fig , 10a–d View Text-fig ). A large postrostral with short ridges and tubercles on the outer surface of the bone is preserved in specimen DP 4529. A ragment of the nasal and supraorbital anterior is situated laterally from the postrostral.

The skull roof bones are preserved in the specimens NM-M 4920 , P 64658, P 64665, P 64673 and others. The frontal is of oblong shape, the length being more than twice the width including the lateral process .

The anterior edge of the frontal is straight or slightly slopes medially, the lateral edge of the bone forms the lateral process in the posterior third of its length, the process extends between the dermopterotic and dermosphenotic. The interfrontal suture is without any large processes, and is straight or slightly wavy. The dorsal surface of the frontal bears well developed sculpture including tubercles and vermicularly arranged ridges. Prominent sculpture on the frontal sometimes overlaps the interfrontal suture ( Text-fig. 10a View Text-fig ). The supraorbital sensory canal traverses along the lateral margin of the frontal. The parietal is square shaped, and often the right and left parietal differ in shape ( Text-fig. 10a View Text-fig ). The anterior, medial and posterior pit lines are well-developed. The dorsal surface of the bone bears tubercles and short ridges. The triangular shaped dermosphenotic is slightly elongated posterolaterally along the anterior margin of the dermopterotic. Ridges which are parallel with the lateral border of the bone form the sculpture on the dermosphenotic. A short section of the infraorbital canal can be observed near to the lateral edge of the bone. The dermopterotic is oblong in shape, rounded anteriorly. It slightly extends in a posterior direction and continues as a large sharply pointed process posteriorly. The lateral edge of the bone is usually straight or slightly wavy in comparison to specimen P 30943 ( Text-fig. 10d View Text-fig ) which has a lateral process in the middle of the lateral edge length. Conspicuous ridges and tubercles form the sculpture similarly as on the other bones of the skull roof. The pores of the infraorbital sensory canal can be observed along the posterior part of the lateral edge of the bone. A small postparietal of oblong shape is preserved on DP 4529. A strip of extrascapular bones ( Text-fig. 9a View Text-fig ) which consists of the extrascapular medial and paired extrascapular

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