FIGURE 1. Locality information for the holotype of Transylvanosaurus platycephalus gen. et sp. nov. A, Location of the type locality of Transylvanosaurus platycephalus gen. et sp. nov. south of Pui, in the eastern Hateg Basin, western Romania, alongside with that of other rhabdodontid posterior cranial remains (frontals and basicrania listed above, respectively below the horizontal line) discussed in the text; the holotype is LPB (FGGUB) R.2070, in bold (for details on specimen numbers, see text). Key: 1, uplifted pre-Alpine crystalline basement rocks bordering the Hateg Basin; 2, pre-uppermost Cretaceous sedimentary units of the Hateg Basin (mainly marine beds); 3–5, vertebrate-bearing uppermost Cretaceous (Maastrichtian) continental deposits: 3, Sînpetru Formation (spf); 4, Sînpetru Formation-correlative units ('Râul Mare Beds' in the central part of the basin, 'Pui Beds' in the eastern part); 5, Densus-Ciula Formation (dcf), with v—volcanoclastic 'lower member'; 6, Cenozoic (mainly Quaternary) sedimentary cover; 7, main fossiliferous localities with rhabdodontid posterior cranial material. B, Inset shows the position of the Hateg Basin within Romania (rectangle), as well as the approximate location of the rhabdodontid frontal MMIRS 780 in the southwestern part of the Transylvanian Basin (star).