Contignisporites ugensis, Takahashi & Sugiyama, 1990
publication ID |
https://doi.org/ 10.5252/g2011n1a6 |
DOI |
https://doi.org/10.5281/zenodo.13942466 |
persistent identifier |
https://treatment.plazi.org/id/039A87FC-FFD8-6174-FF45-FC05FCC6FD02 |
treatment provided by |
Felipe |
scientific name |
Contignisporites ugensis |
status |
|
Callialasporites sp. cf. C. ugensis Takahashi & Sugiyama, 1990 ( Fig. 12N View FIG )
OCCURRENCE. — Ashikajima Fm (rare).
DESCRIPTION
Monosaccate pollen grain. Amb oval to subcircular. The central body is surrounded by a narrow and undulating equatorial saccus (5-8 µm). The exine is punctate on the thinned distal pole area. Equatorial diameter = 35-55 µm.
REMARKS
Two morphologically similar but larger species have been reported by Takahashi & Sugiyama (1990) from the Santonian of the Taneichi Formation, north-east Honshu, Japan (70-84 µm): Callialasporites ugensis Takahashi & Sugiyama , and by Kumar (1973) from the Lower Cretaceous of India (55-68 µm): Callialasporites doringii Kumar (previously named C. lenticularis (Döring, 1961) Venkatachala & Kar, 1969 by Singh & Kumar (1969): pl. 1, figs 15, 16). Deák (1962) reported a grain also showing similarities to ours: Inaperturopollenites undulatus Weyland & Greifeld, 1953 (pl. 12, figs 10, 13).
BOTANICAL AFFINITIES
Pinales . Archangelsky & Gamerro (1967) and Gamerro (1965, 1968)suggested similarities of grains of the genus Callialasporites with those observed in cones of Apterocladus lanceolatus Archangelsky (Podocarpaceae) from the Lower Cretaceous of Patagonia. Van Konijnenburg - Van Cittert (1971) reported abnormal grains of the same morphology in an Araucariaceae .
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
Kingdom |
|
Phylum |
|
Class |
|
Order |
|
Family |
|
Genus |