Casuarinidites sp.
publication ID |
https://doi.org/10.26879/465 |
persistent identifier |
https://treatment.plazi.org/id/66258796-FF87-FFEB-3670-EA6DD4D5FAF0 |
treatment provided by |
Felipe (2024-08-11 02:19:49, last updated 2024-08-12 12:53:37) |
scientific name |
Casuarinidites sp. |
status |
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Figure 3.4
Material. Samples Pb-9337, Pb-9340, Pb-8898, Pb-9141, Pb-9147, Pb-9136, Pb-9339, and Pb- 8896, Palynology Laboratory, IGLUNAM.
Description. Monad pollen, isopolar, radiosymmetric, amb triangular. Triporate, angulaperturate, aspidate pores, annulate, annulus with a 5.6 P m diameter. Exine tectate, granulate, 1.2 P m thick, scabrate. The granular infratectal structure gives a microreticulate pattern.
Dimensions. Equatorial diameter 26–37 µm, two specimens measured.
Comparisons. The size of the Casuarinidites sp. from the Cuayuca Formation is similar to that of C. granilabrata described by Srivastava (1972); however the exine of C. granilabrata is 2 µm thick.
Other occurrences. This genus has been reported in Mexico from the Oligocene San Gregorio Formation (Martínez-Hernández and Ramírez-Arriaga, 2006); Oligo-Miocene of Chiapas ( Biaggi, 1978). U.S.A. – Miocene, Massachussets ( Frederiksen, 1984); Paleocene, Alabama ( Srivastava, 1972).
Biaggi, R. E. 1978. Palynology and paleoecology of some Oligo - Miocene sediments from Chiapas, Mexico. MSc Thesis, Walla Walla College, WA, USA.
Frederiksen, N. O. 1984. Stratigraphic, paleoclimatic and paleobiogeographic significance of Tertiary sporomorphs from Massachusetts. U. S. Geological Survey Professional Paper, 1308: 1 - 25.
Ramirez-Arriaga, E., Martinez-Hernandez, E., and Pramparo, M. B. 2006. Palynology of the Paleogene Cuayuca Formation (stratotype sections), southern Mexico: chronostratigraphical and palaeoecological implications. Review of Palaeobotany and Palynology, 141: 259 - 275.
Srivastava, S. K. 1972. Systematic description of some spores from the Edmonton Formation (Maestrichtian), Alberta, Canada. Palaeontographica Abteilung B, 139: 1 - 46.
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