Fig. 3 in Palynostratigraphic And Palaeoenvironmental Investigations Of The Maastrichtian From Oarda De Jos (Southwestern Transylvanian Basin)

Fig. 3. Terrestrial palynomorphs (cryptogam spores) recovered from the Oarda de Jos sample, uppermost Cretaceous continental Sebeș Formation, (scale bar 30 µm). a, b. Deltoidospora australis; c. Deltoidospora sp.; d. Microreticulatisporites uniformis; e. Polypodiaceoisporites hojrupensis; f. Densoisporites sp.; g. Gleicheniidites senonicus; h. Biretisporites potoniaei; i. Biretisporites sp.; j. Triplanosporites microsinuosus; k. Uvaesporites sp.; l. Zlivisporites blanensis; m. Laevigatosporites major; n. Laevigatosporites ovatus; o. Laevigatosporites sp.; p. Neoraistrickia sp.; q. Polypodiidites secundus.