Monocolpopollenites aff. texensis Nichols et al., 1973

Ramírez-Arriaga, Elia, Prámparo, Mercedes B. & Martínez-Hernández, Enrique, 2014, Angiosperm pollen grains from the Cuayuca Formation (Late Eocene to Early Oligocene), Puebla, Mexico, Palaeontologia Electronica 102 (8), pp. 1-38 : 9

publication ID

https://doi.org/ 10.26879/465

persistent identifier

https://treatment.plazi.org/id/66258796-FF9F-FFF3-32AE-E8CDD66EFB70

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Felipe

scientific name

Monocolpopollenites aff. texensis Nichols et al., 1973
status

 

Monocolpopollenites aff. texensis Nichols et al., 1973

Figure 4.7 View FIGURE 4

Material. Sample Pb-8872, Palynology Laboratory, IGLUNAM.

Description. Monad pollen, heteropolar, bilateral symmetry, amb oval. Monosulcate. Exine tectate, the structure of the wall is difficult to discern, 0.8 µm thick, psilate.

Dimensions. Length 32 µm, width 22.4 µm, one specimen measured.

Remarks. In a monographic discussion concerning monosulcate genera, Nichols et al. (1973) proposed that the shape of the sulcus differentiates the genus Monocolpopollenites from Arecipites . Arecipites includes monosulcate grains with a tapered sulcus, not expanded or gaping at the ends. Monocolpopollenites includes grains with flared or round-ended sulcus.

Comparison. M. aff. texensis (in this contribution) has the sulcus extending the entire long axis of the grain, with margins tending to overlap centrally, as in M. texensis . However, the Mexican specimen is larger (32 µm) than M. texensis ( Nichols et al. 1973: 17–19 x 24–28 µm) and presents a psilate instead of scabrate exine.

Other occurrences. There are no previous records of this taxon in Mexico. The genus has been reported from the US Gulf Coast ( Frederiksen, 1980a) and in England ( Wilkinson and Boulter, 1980).

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