Clavatipollenites sp. 1

Friis, Else Marie, Crane, Peter R. & Pedersen, Kaj Raunsgaard, 2019, The Early Cretaceous Mesofossil Flora Of Torres Vedras (Ne Of Forte Da Forca), Portugal: A Palaeofloristic Analysis Of An Early Angiosperm Community, Fossil Imprint 75 (2), pp. 153-257 : 189

publication ID

https://doi.org/ 10.2478/if-2019-0013

persistent identifier

https://treatment.plazi.org/id/0396DC10-BF2B-C227-CC1F-B5FCE6CF1B72

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scientific name

Clavatipollenites sp. 1
status

 

Clavatipollenites sp. 1

Text-fig. 22a–g View Text-fig

D e s c r i p t i o n a n d r e m a r k s. The material comprises several fragments of small tetrasporangiate stamens with pollen in situ ( Text-fig. 22a, b View Text-fig ). The anthers are up to about 0.52 mm long. Pollen grains in situ within the stamens were described by Friis et al. (1999) as type J.1. The grains are monoaperturate and almost circular in equatorial outline, about 14–16 µm in diameter, semitectatereticulate with a homobrochate reticulum ( Text-fig. 22c–f View Text-fig ). Lumina are irregular and up to about 1.2 µm in diameter. Muri are ornamented with tiny verrucae arranged in two rows. Columellae are of medium size and widely spaced ( Text-fig. 22g View Text-fig ). The aperture is broad, rounded and covered by irregular verrucae that grade into the reticulum in the non-apertural regions of the grains ( Text-fig. 22c–e View Text-fig ) .

A f f i n i t y a n d o t h e r o c c u r r e n c e s. In their general shape, form of the pollen wall, and the indistinctly delimitated aperture, these pollen grains are similar to various dispersed pollen assigned to the genus Clavatipollenites . Pollen grains of Clavatipollenites are usually compared to pollen of extant Ascarina . However, the pollen described here differs from that of extant Ascarina in having a very broad and rounded colpus. Similar pollen to the fossil grains described here also occur in several stamens recovered from the Catefica mesofossil flora.

J

University of the Witwatersrand

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