Ulmipollenites sp.
publication ID |
https://doi.org/ 10.26879/465 |
persistent identifier |
https://treatment.plazi.org/id/66258796-FF82-FFED-3676-ED78D5C8FDC5 |
treatment provided by |
Felipe |
scientific name |
Ulmipollenites sp. |
status |
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Figure 5.18 View FIGURE 5
Material. Samples Pb-9137, Pb-9343, Pb-8896, Pb-8872, Pb-9141, Pb-9138, Pb-8898, Pb-9339, Pb-9340, and Pb-9147, Palynology Laboratory, IGLUNAM.
Description. Monad pollen, isopolar, radiosymmetric, amb subcircular. Tetraporate or pentaporate. Exine tectate, 1 µm thick, suprarugulate.
Dimensions. Equatorial diameter 17–33 µm, five specimens measured.
Comparisons. Considering dimensions and number of pores, Ulmipollenites sp. is similar to U. krempii from the Eocene of California, U.S.A. ( Frederiksen et al., 1983) and U. undulosus ( Jansonius and Hills, 1976: card number 3121); but the rugulae are less conspicuous in our specimens.
Other occurrences. Mexico - Ulmipollenites has been recovered from the late Eocene to early Oligocene Pie de Vaca Formation (Martíne–-Hernández and Ramírez-Arriaga, 1999); Oligocene San Gregorio Formation (Martínez-Hernández and Ramírez, 2006); Oligo-Miocene of Chiapas ( Biaggi, 1978); Neogene ( Palacios and Rzedowski, 1993); Pliocene, Paraje Solo, Veracruz ( Graham, 1975). U.S.A. – late Miocene Valentine Formation, Nebraska ( MacGinitie, 1962); late Eocene, Jackson Group, Mississippi and Alabama ( Frederiksen, 1980a); Eocene of California ( Frederiksen, 1989) and middle Miocene of Florida ( Jarzen and Klug, 2010). Initially found in the Tertiary of Germany by Wolff (1934) and Thomson and Plug (1953).
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