Vörös A. szerk.: Fragmenta Mineralogica Et Palaentologica 15. 1992. (Budapest, 1992)

1978 Libocedrites salicornioides (UNG.) ENDL.; Mai and Walther, pl. 14, figs. 1418, pl. 17, figs. 1-8. 1979 Libocedrites salicornioides (UNG.) ENDL.; Hably, pi. 2, fig. 1; pi. 3, fig. 2; pi. 4, fig. 2. 1980 Libocedrites salicornioides (UNG.) ENDL.; Zastawniak, p. 43, pl. 1, figs. 1, la. 1985 Libocedrites salicornioides (UNG.) ENDL.; Hably, p. 84, pi. 4, figs. 2-4. 1986 Tetraclinis salicornioides (UNGER) KVACEK; Kvacek, p. 48, Pl. 1, fig. 11; PI. 2, figs. 2-14; PI. 3, figs. 3,4, text-fig. 1. Material: sample No 849, depth 1691.4 m One whorl of leaves, 0.8 cm in length and 0.4 cm in width. At some Lower Oligocène localities of Hungary it occurs in large number while it is only scarcely found in the Upper Oligocène (Hably 1979, 1990). It was found in greatest abundance in the Lower Miocene (Ottnangian) tuff of Ipolytarnóc (Hably 1985). Lauraceae Daphnogene UNGER Daphnogene bilinica (UNGER) KVACEK et KNOBLOCH Pl. V, Figs. 4, 5; Pl. VI, Fig. 1. 1847 Ceanothus bilinicus UNGER; Unger, p. 145, pi. 49, fig. 9. 1914 Cinnamomum scheuchzeri HEER; Jablonszky, p. 256. 1950 Cinnamomophyllum scheuchzeri (HEER) KRÀUSEL and WEYLAND; Kràusel and Weyland, p. 68, pl. 11, fig. 7; pl. 16, figs. 1-6; pl.l7, fig. 1; pi. 18, figs. 2-4; text-fig. 25-26. 1971 Daphnogene bilinica (UNG.) KNOBLOCH and KVACEK; Kvacek, p. 67, pi. 2, figs. 1-4; pi. 9. figs. 4-6; text-fig. 14. 1979 Daphnogene bilinica (UNG.) KNOBLOCH and KVACEK; Hably, p. 56; textfig. 1. 1985 Daphnogene bilinica (UNG.) KVAC. and KNOBL.; Hably, p. 91, pi. 9, figs. 1, 46; pi. 10, figs. 1-7. Material: sample No 846, depth 1665.3 m, No 849, depth 1691.6 m, No 863, depth 1744.0 m, No 863, depth 1745 m, No 873, depth 1754.2 m. The leaves are small or moderate in size, simple, elongated ellipsoid in outline, 3.2-5.5 cm in length, 1.6-1.7 cm in width. The margin of the leaves is entire, the venation is suprabasal. The midvein is strong, the basal veins are slightly weaker or approximately as thick as the midvein. In Hungary it has been found in most of the Upper Oligocène localities (Hably 1988, 1989). It is the dominant species in the Lower Miocene flora of Ipolytarnóc (more than one thousand prints) (Hably 1985). It persists to the Sarmatian stage. Daphnogene cinnamomifolia (BRONG. in CUVIER) UNGER 1822 Phyllites cinnamomifolia BRONG. in CUVIER; Brongniart 2 Bd. 1850 Daphnogene cinnamomifolia UNGER; Unger, p. 168, PI. 39, Figs. 7-9.