Polyadopollenites sp.1
publication ID |
https://doi.org/ 10.26879/465 |
persistent identifier |
https://treatment.plazi.org/id/66258796-FF98-FFEB-3195-EBA2D658FEA5 |
treatment provided by |
Felipe |
scientific name |
Polyadopollenites sp.1 |
status |
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Figure 5.2 View FIGURE 5 -3
Material. Sample Pb-9334, Palynology Laboratory, IGLUNAM.
Description. Polyad with 16 pollen grains: eight central grains and eight peripheral. Inaperturate. Exine atectate, 0.8–1.6 µm thick, regulate.
Dimensions. Polyad 48.8 µm x 46.4 µm. Monad: Equatorial diameter 16–20 µm, polar diameter 11.2 –14.4 µm, one specimen measured.
Comparisons. Polyadopollenites sp. 1 is distinguished by its suprarrugulate exine instead of a psilate tectum in Acaciapollenites from late Oligocene of New Zealand ( Pocknall and Mildenhall, 1984). Polyadopollenites sp. 1 presents similar ornamentation to Polyadopollenites mulleri ( Cavagnetto and Guinet, 1994) ; however, Polyadopollenites sp. 1 is not as big as P. mulleri ( Cavagnetto and Guinet, 1994: 65–72 µm). Furthermore, P. mulleri from the Oligocene of Spain has porate monads ( Cavagnetto and Guinet, 1994).
Other occurrences. This genus has been recovered in Mexico from the late Eocene to early Oligocene Pie de Vaca Formation ( Martínez-Hernández and Ramírez-Arriaga, 1999); Oligocene San Gregorio Formation, Baja California Sur (Martínez-Hernández and Ramírez-Arriaga, 2006); Oligo-Miocene of Chiapas ( Biaggi, 1978); Neogene ( Palacios and Rzedowski, 1993). Central America – early Miocene La Culebra Formation, Panamá ( Graham, 1988). Caribbean islands– Oligocene San Sebastián Formation, Puerto Rico ( Graham and Jarzen, 1969). Originally described from the Eocene-Oligocene in Germany ( Thomson and Pflug, 1953).
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