Pennicarpus tenuis E.M.FRIIS, K.R.PEDERSEN et P.R.CRANE, 2000
publication ID |
https://doi.org/10.37520/fi.2022.016 |
DOI |
https://doi.org/10.5281/zenodo.7535339 |
persistent identifier |
https://treatment.plazi.org/id/03FD87F2-FFD7-FFC2-FC3D-FB66C1B9FB65 |
treatment provided by |
Felipe (2023-01-10 20:28:08, last updated 2024-11-29 10:30:53) |
scientific name |
Pennicarpus tenuis E.M.FRIIS, K.R.PEDERSEN et P.R.CRANE, 2000 |
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Pennicarpus tenuis E.M.FRIIS, K.R.PEDERSEN et P.R.CRANE, 2000
Description and remarks. Two fruits, about 0.8–1.3 mm long and 0.5 mm broad, were recovered from Catefica sample 50. The fruits (not figured) are strongly flattened and elliptical in outline with a very thin fruit wall and thin, longitudinal ridges, probably from vascular bundles, that extend for the full length of the fruits.
Affinity and other occurrences.The fruits are closely similar in size, shape and texture to those of Pennicarpus tenuis described from the Vale de Água and Buarcos mesofossil floras ( Friis et al. 2000). The fruits from Catefica have not been studied using SEM and it is unknown whether they have adhering pollen of Pennipollis E.M.FRIIS, K.R.PEDERSEN et P.R.CRANE as is known for Pennicarpus tenuis from Vale de Água and Buarcos.
Pennicarpus and the associated Pennistemon E.M.FRIIS, K.R.PEDERSEN et P.R.CRANE and Pennipollis , collectively referred to as the Pennipollis plant (Friis et al. 2011), were placed in the monocots mainly based on the distinct acolumellate pollen wall ( Friis et al. 2000), although an affinity with Chloranthaceae has also been suggested (see Doyle and Endress 2014).
So far, only two fruits have been recovered from Catefica and Pennipollis grains have not been recognized in the palynological preparations. In the Vale de Água and Buarcos mesofossil floras remains of the Pennistemon plant are abundant. Dispersed Pennipollis pollen has also been reported in early Aptian to middle Albian palynological assemblages from coastal sections in Portugal ( Heimhofer et al. 2007) and from the dispersed palynoflora of Casal do Borracho (Torres Vedras) ( Mendes et al. 2018a). Pennipollis pollen is also widespread in Early Cretaceous palynofloras from other regions (see Friis et al. 2000).
Doyle, J. A., Endress, P. K. (2014): Integrating Early Cretaceous fossils into the phylogeny of living angiosperms: ANITA lines and relatives of Chloranthaceae. - International Journal of Plant Sciences, 175: 555 - 600. https: // doi. org / 10.1086 / 675935
Friis, E. M., Pedersen, K. R., Crane, P. R. (2000): Fossil floral structures of a basal angiosperm with monocolpate, reticulate-acolumellate pollen from the Early Cretaceous of Portugal. - Grana, 39: 226 - 245. https: // doi. org / 10.1080 / 00173130052017262
Heimhofer, U., Hochuli, P. A., Burla, S., Weissert, H. (2007): New records of Early Cretaceous angiosperm pollen from Portuguese coastal deposits: Implications for the timing of the early angiosperm radiation. - Review of Palaeobotany and Palynology, 144: 39 - 76. https: // doi. org / 10.1016 / j. revpalbo. 2005.09.006
Mendes, M. M., Barron, E., Dinis, P., Rey, J., Batten, D. J. (2018 a): A new palynoflora from upper Barremian-lower Aptian rocks at Casal do Borracho, Torres Vedras, western Portugal, and its palaeoecological significance. - Cretaceous Research, 90: 363 - 374. https: // doi. org / 10.1016 / j. cretres. 2018.06.012
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