Archeocalamitaceae | |
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Archeocalamitaceae is a family of extinct sphenopsids related to horsetails. Archeocalamite fossils have been found in Siberia, Poland, and Brazil. The fossils date to the Middle Devonian-Carboniferous, lower Carboniferous (Dinantian), and the lower Permian respectively.[1][2][3] Given the distance of the fossil discoveries, archeocalamites may have had a subcosmopolitan distribution.
Taxonomy
Possible relationships archeocalamites has with other sphenopids is shown below.[4]
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References
- ↑ LESZCZYŃSKI, Krzysztof; WAKSMUNDZKA, Marta (2015-01-01). "ŚRODOWISKA SEDYMENTACJI I PALINOFACJE KREDY DOLNEJ W OTWORACH WIERTNICZYCH CIECHOCINEK IG 3, MSZCZONÓW IG 1 I KORABIEWICE PIG 1". Biuletyn Państwowego Instytutu Geologicznego. 457 (457): 1–14. doi:10.5604/08676143.1113252. ISSN 0867-6143.
- ↑ Faculty of Mining and Geology, Belgrade, Serbia; Radonjić, Miloš (2020-10-26). "Hyperpycnites within the Devonian-Carboniferous flysch of the Carpatho-Balkanides (Kostadinovica, eastern Serbia)". Geologia Croatica. 73 (3): 131–142. doi:10.4154/gc.2020.13.
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: CS1 maint: multiple names: authors list (link) - ↑ Boardman, Daiana Rockenbach; Iannuzzi, Roberto; Dutra, Tânia Lindner (2016-10-01). "A new genus of Sphenopsida from the Lower Permian of the Paraná Basin, Southern Brazil". Review of Palaeobotany and Palynology. 233: 44–55. doi:10.1016/j.revpalbo.2016.07.004. ISSN 0034-6667.
- ↑ "Systematics of the Sphenophyta". ucmp.berkeley.edu. Retrieved 2023-08-12.
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