Fig. 1 in Cetotheriidae (Cetacea, Mysticeti) From The Collections Of The National Geological Museum, Bucharest (Romania)

Fig. 1. Location of the studied area in Romania (left) and the geological structures and location of the fossiliferous localities (right) in Gorj County (modified after Codarcea et al., 1968): 1 — Igneous rocks; 2 — Sarmatian s. l.; 3 — Maeotian; 4 — Upper Besarabian–Maeotian; 5 — Holocene; 6 — Pleistocene; 7 — Volhynian–Lower richnessBessarabian(Bercia; 8 —et al., fossiliferous 1968). Theselocality. deposits are situated in the Novaci depression and continue to the east and to the west, as well as south of the Ciocadia–Săcel anticline (Bercia et al., 1968). The paleontological content is also represented by invertebrate species such as: Unio cf. subrecurvus Teisseyre 1907, Radix cf. velutina Deshayes 1838, and Congeria navicula Andrusov 1897 (Popescu, 1955; Bercia et al., 1968). The last sedimentary sequence, situated east of the Cerna River, on the northern rim of the Dacian Basin is composed of detritic deposits containing rare Mactra Linnaeus 1767 remains, characteristic of the Bessarabian and Khersonian, while eastwards, towards Râmnicu Vâlcea these detritic deposits overlay the Lower Bessarabian formations with C. pesanseris, and above these, the Maeotian deposits, predominantly detritic, composed of sands and sandy marls with gravel interlays follow (Bercia et al., 1968).