Circumpolles

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Circumpolles
Temporal range: TriassicCretaceous
Scientific classification OOjs UI icon edit-ltr.svg
Kingdom: Plantae
Clade: Tracheophytes
Clade: Gymnospermae
Division: Pinophyta
Class: Pinopsida
Order: Pinales
Family: Cheirolepidiaceae
Genus: Circumpolles

Circumpolles is a gymnosperm pollen type that is important in biostratigraphy and paleoenvironmental reconstruction. [1] It characterizes the time between the middle Triassic to the middle Cretaceous Periods. This pollen has a unique morphology: it has a circular, equatorial colpus, which divides the pollen grain into two hemispheres. Circumpolles is also unique as it is the only gymnosperm with well developed nexinal columellae. [2]

Circumpolles is a synonym of Classopollis. Classopollis were produced by shrubs that tolerated semiarid conditions, and Classopollis is correlated with evaporites and are therefore associated with desert basins, but the shrubs may have also lived in xeric uplands. [3]

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Corystosperms are a group of extinct seed plants belonging to the family Corystospermaceae assigned to the order Corystospermales or Umkomasiales. They were first described based on fossils collected by Hamshaw Thomas from the Burnera Waterfall locality near the Umkomaas River of South Africa. Corystosperms are typified by a group of plants that bore forked Dicroidium leaves, Umkomasia cupulate ovulate structures and Pteruchus pollen organs, which grew as trees that were widespread over Gondwana during the Middle and Late Triassic. Other fossil Mesozoic seed plants with similar leaf and/or reproductive structures have also sometimes been included within the "corystosperm" concept sensu lato, such as the "doyleoids" from the Early Cretaceous of North America and Asia. A potential corystosperm sensu lato, the leaf genus Komlopteris, is known from the Eocene of Tasmania, around 53-50 million years old, over 10 million years after the Cretaceous–Paleogene extinction event.

Frenelopsis is a genus of extinct conifers belonging to the family Cheirolepidiaceae that lived throughout the Cretaceous period ranging from the Berriasian to the Maastrichtian stages, containing a total of 18 species. It is a form classification describing the shoots of the plant, and is accompanied by the genera Classopollis, Classostrobus, and Alvinia. These represent the pollen, male cones, and female cones respectively. They are likely to have been a major source of lignite in Cretaceous deposits.

References

  1. Pocock, S.A.J.; Vasanthy, G; Venkatachala, B.S (October 30, 1990). "Pollen of circumpolles — An enigma or morphotrends showing evolutionary adaptation". Review of Palaeobotany and Palynology. 65 (1–4): 179–193. Bibcode:1990RPaPa..65..179P. doi:10.1016/0034-6667(90)90069-U.
  2. Traverse, Alfred (1988). Paleopalynology. Unwin Hyman. ISBN   978-0045610013. OCLC   17674795.
  3. Srivastava, Satish K. (October 1976). "The fossil pollen genus Classopollis". Lethaia. 9 (4): 437–457. Bibcode:1976Letha...9..437S. doi:10.1111/j.1502-3931.1976.tb00985.x. ISSN   0024-1164.