Linum, Linnaeus, 1753

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 : 19-20

publication ID

https://doi.org/ 10.26879/465

persistent identifier

https://treatment.plazi.org/id/66258796-FF85-FFE8-3676-ED5AD6ABFE58

treatment provided by

Felipe

scientific name

Linum
status

 

Linum View in CoL pollen type

Figure 4.15 View FIGURE 4

Material. Sample Pb-9334, Palynology Laboratory, IGLUNAM.

Description. Monad pollen, isopolar, radiosymmetric, amb subcircular. Tricolpate, the broad and large colpi make a small polar area. Exine semitectate columellate, 3 µm thick, microreticulate to striate, supragemmate, gemmae 2–3.5 µm in diameter, distributed irregularly over the surface of the grain.

Dimensions. Equatorial diameter 48–53 µm, one specimen measured.

Comparisons. Tricolpate pollen grain characterized by large size ( Wingate, 1983: 44 x 49 µm) and gemmate ornamentation has been reported from the Elko Formation ( Wingate, 1983, plate 2, figure 12). The tricolpate pollen type 1 from the Elko Formation is not semitectate microreticulate like the Linum pollen type from the Cuayuca Formation, and has a thinner exine.

Other occurrences. This is the first mention of the genus in the Mexican fossil record. This taxon is also recorded from the European middle Eocene to early Oligocene, Ebro Basin, Spain ( Cavagnetto and Anadón, 1996).

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