Cladophlebis
Fossil rangePermian to Campanian
~
RegnumPlantae
ClassisFilicopsida
OrdoFilicales
GenusCladophlebis
Genus authorityBrongniart 1849
Subdivision ranksSpecies
SubdivisionSee text

Cladophlebis is an extinct form genus of fern, which has been reported from the Permian to the end of the Cretaceous and from all continents of the world.[1][2]

Description

Some pinnules have smooth edges and some have serrated edges. The midrib is distinct and the lateral veins are dichotomous (two branches) to the end. This fern had rizoma. used to refer to Paleozoic and Mesozoic fern leaves that have "fern fronds with pinnules that are attached to the rachis, and have a median vein that runs to the apex of the pinnule, and veins from that are curved and dichotomise".[2][3][1]

Species

There were many species of Cladophlebis, including: C. akhtashensis, C. arctica, C. browniana, C. denticulata, C. dunberi, C. fukiensis. C. haiburnensis, C. heterophylla, C. hirta, C. impressa, C. kurtzi, C. lobifolia, C. nebbensis, C. patagonica, C. phlebopteris, C. porsildi, C. readi, C. remota, C. retallackii, C. roessertii, C. septentrionalis, C. simplicima, C. spectabilis, C. tenuis, C. wyomingensis, and C. yanschinii.

References

  1. ^ Holmes, W. B. Keith (2001). "The Middle Triassic megafossil flora of the Basin Creek Formation, Nymboida Coal Measures, New South Wales, Australia. Part 2. Filicophyta". Proceedings of the Linnean Society of New South Wales. 123: 39–87.
  2. ^ "Cladophlebis – New Zealand's Mesozoic Weed". Mike Pole. 2014-06-22. Retrieved 2020-11-24.
  3. ^ Cladophlebis at Fossilworks.org

Bibliography

  • McLoughlin, S.; Drinnan, A. N.; Rozefelds, A. C. (1995). "A Cenomanian flora from the Winton Formation, Eromanga Basin, Queensland, Australia". Memoirs of the Queensland Museum. 38 (1): 273–313.
  • Monje-Dussán, Camila; Martínez, Camila; Escapa, Ignacio; Madriñán, Santiago (1 June 2016). "Nuevos registros de helechos y coníferas del Cretácico Inferior en la cuenca del Valle Superior del Magdalena, Colombia" [New records of ferns and conifers from the lower Cretaceous in the Upper Magdalena Valley Basin, Colombia] (in Spanish). Boletín de Geología. 38 (4): 29–42. doi:10.18273/revbol.v38n4-2016002. hdl:11336/117867