The oldest records of the stem amniote Discosauriscus (Seymouriamorpha, Discosauriscidae) from the European Carboniferous-Permian boundary
and references therein). The fossil record of Seymouriamorpha includes specimens in the pre-metamorphic stage (with external gills and found in the lacustrine sediments), as well as the post-metamorphic specimens of various grade of ossific ation, size, and age (Bulanov 2003 , Sanchez et al. 2008 , Klembara 2009) . The species of the family Discosauriscidae (Romer 1947) are so far known from the European localities in the Lower Permian of the Czech Republic, Poland, Germany and France: Discosauriscus austriacus, D. pul cherrimus, Makowskia laticephala, Spinarerpeton brevicephalum and one unidentified discosauriscid specimen (for review see Klembara 2016). The sixth discosauriscid species is Ariekanerpeton sigalovi from the Lower Permian of Tadzhikistan (Klembara & Ruta 2005). The stratigra phic ally oldest known seymouriamorph species is Utegenia spinari (Utegeniidae) from the upper Carboniferous(?)lower Permian of Kazakhstan (Klembara & Ruta 2004). However, there is no certainty as for the potential Upper Carboniferous age of Utegenia (Bulanov 2003). An another discosauriscid, Urumquia liudaowanensis (Zhang et al. 1984), is from China. According to the latest investig ations, the locality of Urumquia is of Middle Permian age (Jiang et al. 2020). Previously, no discosauriscid remains have been recorded in the upper Carboniferous sediments. The aims of the present paper are: 1) description of two new specimens belonging to Discosauriscus (Discosauriscidae) from the Czech Republic and Germany; and 2) their stratigraphic evaluation. Skull length of the specimen (NHMS-WP10870) from the locality Semily is about 28 mm (measured in the median plane). The postcranial skeleton of the specimen from the locality Sembachtal (NHMS-WP12069) may belong to a specimen with about 30 mm skull length. The study of the sequence of the ontogenetic stages of Discosauriscus shows that both here described specimens represent the larval ontogenetic stages (Klembara 1995 (Klembara , 1997 (Klembara , 2009)) . We used high-resolution X-ray microcomputed tomography to obtain the morphology of bones completely or partially embedded in the sediment and which are crucial for the determination of the specimen NHMS-WP10870. Microcomputed tomography (μ-CT) imaging was performed with phoenix v|tome|x L 240 device, developed by GE Sensing & Inspection Technologies at the Earth Science Institute of the Slovak Academy of Sciences in Banská Bystrica. Investigated specimen was analyzed by using 240 kV/320W microfocus tube. Scanning parameters were set as follows: voltage 200 kV, current 200 μA, projections 1900, average 3, skip 1, timing 333 ms, voxel size 40 μm, detector sensitivity 2, and 0.1Cu filter. The photographs of the postcranial skeleton of Discosauriscus from Sembachtal, Germany (NHMS-WP12069), was taken with Nikon D5100 camera. The drawing of this specimen was made with the help of a drawing mirror (ʻcamera lucidaʼ) on a Zeiss binocular Discovery.V12. Institutional abbreviations. -NHMS -Natur historisches Museum Schloss Bertholdsburg,
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