Kempia longicolpites E.M.FRIIS, P.R.CRANE et K.R.PEDERSEN, 2019
publication ID |
https://doi.org/ 10.37520/fi.2022.016 |
DOI |
https://doi.org/10.5281/zenodo.7535341 |
persistent identifier |
https://treatment.plazi.org/id/03FD87F2-FFD1-FFC2-FF7D-F9D6C62AF994 |
treatment provided by |
Felipe |
scientific name |
Kempia longicolpites E.M.FRIIS, P.R.CRANE et K.R.PEDERSEN, 2019 |
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Kempia longicolpites E.M.FRIIS, P.R.CRANE et K.R.PEDERSEN, 2019
Text-fig. 30a–f View Text-fig
Description and remarks. The material comprises two adhering stamens (only one cut stamen illustrated) with dithecate, tetrasporangiate anthers ( Text-fig. 30a View Text-fig ) and in situ pollen. The stamens are about 1 mm long and 0.25 mm broad with a distinct, triangular apical extension of the connective. One stamen was cut transversely into two pieces to expose the pollen for SEM. The other stamen was removed for TEM. Stamens and anthers are closely similar to Kempia longicolpites described from the Torres Vedras locality ( Friis et al. 2019a) and the specimen is assigned here to the same species. Pollen grains are small, about 11– 12 µm long, monoaperturate and with the colpus extending beyond the full length of the grains. The exine is semitectatereticulate, columellate ( Text-fig. 30b–f View Text-fig ) with the reticulum and columellae only loosely attached to the foot layer ( Text-fig. 30f View Text-fig ). The muri have a rounded profile and a smooth surface ( Text-fig. 30c View Text-fig ). The foot layer is thick, and the endexine is restricted to the apertural region ( Text-fig. 30e View Text-fig ).
Affinity and other occurrences. Kempia longicolpites was first described from the Torres Vedras locality ( Friis et al. 2019a) and is currently known from only the Torres Vedras and Catefica mesofossil floras.
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.
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