Aneurophyton
Aneurophyton is a genus of extinct vascular plants that belong to the Aneurophytales, a class of progymnosperms. The genus is primarily known from records of two well-known species found in mostly Middle Devonian and Upper Devonian (late Eifelian to Famennian) outcrops in Belgium, China (West Junggar), Germany, and the United States (New York).[1][2] Some uncertain species within the genus are also recorded from Middle Devonian outcrops in Kazakhstan, Russia (Timan and Siberia), and the Ukraine. While a number of species have been described in the paleobotanical literature, the genus likely only contains two well-circumscribed species, A. germanicum and A. doui,[1] and possibly a third species, A. olnense, from Fammenian outcrops in Belgium.[3] If the ages of the Early Devonian (Emsian) records of A. germanicum reported from Siberia are confirmed,[4] these would constitute the oldest records of this genus.
Aneurophyton | |
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Scientific classification | |
(unranked): | Archaeplastida |
Kingdom: | Plantae |
See also
References
- Jiang, Qing; Wang, Yi; Xu, Hong-he; Feng, Jing (2013). "A new species of Aneurophyton (Progymnospermopsida) from the Middle Devonian of West Junggar, Xinjiang, China, and its paleophytogeographical significance". International Journal of Plant Sciences. 174 (8): 1182–1200. doi:10.1086/671807.
- Hao, Shougang; Xue, Jinzhuang (2013). The Early Devonian Posongchong Flora of Yunnan - A Contribution to an Understanding of the Evolution and Early Diversification of Vascular Plants. Beijing: Science Press. pp. 244–245. ISBN 978-7-03-036616-0.
- Gerrienne, Philippe; Meyer-Berthaud, Brigitte; Lardeux, Hubert; Régnault, Serge (2010). "First record of Rellimia Leclercq & Bonamo (Aneurophytales) from Gondwana, with comments on the earliest lignophytes". Geological Society, London, Special Publications. 339 (1): 81–92. doi:10.1144/sp339.8.
- Korzhnev, Viktor N. (2014). "The appearance of the elements of the Protopteris floras: paleogeographic constraints". Stratigraphy and Geological Correlation. 22 (5): 465–478. doi:10.1134/s0869593814040066.