Pseudoplicapollis peneserta ( Pflug, 1953 ) Krutzsch, 1967

Halamski, Adam T., Kvaček, Jiří, Svobodová, Marcela, Durska, Ewa & Heřmanová, Zuzana, 2020, Late Cretaceous mega-, meso-, and microfloras from Lower Silesia, Acta Palaeontologica Polonica 65 (4), pp. 811-878 : 851

Pseudoplicapollis peneserta ( Pflug, 1953) Krutzsch, 1967

Fig. 18H.

Remarks.—Found in almost all samples in the section RK-4 and in Palynoassemblage B ( Raniecka-Bobrowska 1984, 1989: pl. 218: 7). Known from the Coniacian ( Hradecká et al. 1999) through the Santonian ( Góczán and Siegl-Farkas 1990) to the Maastrichtian ( Góczán et al. 1967).

Genus Neotriangulipollis Góczán, Groot and Krutzsch in Góczán et al., 1967

Type: Neotriangulipollis piolencensis Groot and Krutzsch in Góczán et al., 1967; Santonian , Upper Cretaceous ; Piolenc, Vaucluse, southern France .

Neotriangulipollis sp.

Fig. 18I.

Remarks.—Representatives of Neotriangulipollis were known from the middle Santonian to the lower Campanian ( Góczán et al. 1967). However, Néraudeau et al. (2017) recently reported a Neotriangulipollis co-occurring with Cenomanian–Turonian forms like Atlantopollis microreticulatus Krutzsch in Goczán et al., 1967 or Complexiopollis praeatumescens Krutzsch, 1959a .

Genus Pecakipollis Krutzsch and Pacltová in Góczán et al., 1967

Type: Pecakipollis bohemiensis Krutzsch and Pacltová in Góczán et al., 1967; Turonian– Santonian , Upper Cretaceous ; borehole Pecák, Southern Bohemia, Czech Republic .

Pecakipollis sernoensis Pacltová and Krutzsch, 1970

Fig. 18N.

Remarks.—Two another species are reported under open nomenclature as Pecakipollis sp. ( Fig. 18R) and aff. Pecakipollis sp. ( Fig. 19J ). Representatives of Pecakipollis possibly occur from the upper Coniacian ( Góczán et al. 1967) to the middle Santonian (Pecák borehole, South Bohemian Basins; Pacltová 1981).

Genus Triangulipollis Krutzsch in Góczán et al., 1967

Type: Triangulipollis turonicus Krutzsch in Góczán et al., 1967; middle Turonian , Upper Cretaceous ; Zeichen near Pirna, Saxony, Germany .

Triangulipollis sp.

Fig. 18O.

Remarks.—Representatives of Triangulipollis are known possibly from the Cenomanian ( Durand and Louail 1976: 1721, under open nomenclature) and certainly from the Turonian( Batten1989:13)to the Paleocene ( Mikhelis 1981).

Genus Trudopollis Pflug, 1953 emend. Krutzsch in Góczán et al., 1967

Type: Trudopollis pertrudens Pflug, 1953 ; Danian ; Wehmingen near Sarstedt, Hannover, Germany .

Figures

Fig. 19. Spores (A–G, K, N–O) and pollen (H–J, L–M, P) from the North Sudetic Basin, Lower Silesia, Poland, Palynoassemblage B (lower–mid- dle Santonian). A. Cingutriletes clavus Dettmann, 1963, borehole KB18, depth 42.3 m. B. Echinatisporis sp., borehole KB18, depth 42.3 m. C. Baculatisporites parvopunctatus Weyland and Greifeld, 1953, borehole KB18, depth 29.8 m. D. Cicatricosisporites potomacensis Brenner, 1963, borehole KB13, depth 88.6 m. E. Klukisporites pseudoreticulatus Couper, 1958, borehole KB13, depth 94.5 m. F. Trilobosporites sp., borehole KB18, depth 38.3 m. G. Distaltriangulisporites perplexus (Singh, 1964) Singh, 1971, borehole KB13, depth 94.5 m. H. Catinipollis lwowekensis Raniecka- Bobrowska, 1984, holotype (slide 13/11, 48.5/110.2; repository unknown), borehole KB18, depth 35.0 m; equatorial focal plane (H1), focal plane on the surface (H2). I. Cerebropollenites mesozoicus (Couper, 1958) Nilsson, 1958, borehole KB17, depth 47.5 m. J. aff. Pecakipollis sp., borehole KB8, depth 77.5 mm. K. Clavifera cf. triplex (Bolkhovitina, 1953) Bolkhovitina, 1966, borehole KB13, depth 28.6 m. L. Piolencipollis sp., borehole KB16, depth 99 m; specimen illustrated by Raniecka-Bobrowska (1984, 1989: pl. 218: 2). M. Ephedripites virginiaensis Brenner, 1963, borehole KB18, depth 39.3 m. N. Cicatricosisporites dorogensis Potonié and Gelletich, 1933, borehole KB17, depth 38.0 m. O. Foveogleicheniidites sp., borehole KB18, depth 38.3 m. P. Podocarpidites sp., borehole KB8, depth 84.3 m. Photographs from the unpublished report by Raniecka-Bobrowska (1968).