Cordaites is an important genus of extinct gymnosperms, related to or actually representing the earliest conifers. These trees grew up to 100 feet (30 m) tall and stood in both dry areas as well as wetlands. Brackish water mussels and crustacea are found frequently between the roots of these trees. Cordaites fossils are most commonly found in rock sections from the Upper Carboniferous (323 to 299 million years ago) of Europe and the Americas.

Cordaites
Temporal range: Pennsylvanian–Changhsingian
Fossil bark of a Cordaites sp
Scientific classification Edit this classification
Kingdom: Plantae
Clade: Tracheophytes
Clade: Gymnospermae
Division: Pinophyta
Class: Pinopsida
Order: Cordaitales
Family: Cordaitaceae
Genus: Cordaites
Unger
Species[citation needed]
  • C. daviessensis
  • C. hislopii
  • C. kinneyensis
  • C. ludlowi
  • C. lungatus
  • C. minshallensis
  • C. olneyensis
  • C. principalis
Leaves of Cordaites lungatus

A number of many noteworthy types from this line are:

  • Cordaites principalis
  • Cordaites ludlowi (named after Ludlow, a coal area in England)
  • Cordaites hislopii. Found in Paleorrota geopark in Brazil.[1]

In contrast to many other plants, fossilized Cordaites seeds are not rare, because they are rather large (up to 10 mm); those seeds are named Cordaicarpus.

References

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  1. ^ Karen Adami-Rodrigues; Paulo Alves De Souza; Roberto Iannuzzi & Irajá Damiani Pinto (2004), "Herbivoria Em Floras Gonduânicas Do Neopaleózoico Do Rio Grande Do Sul: Análise Quantitativa" (PDF), Revista Brasileira de Paleontologia, 7 (2): 93–102, doi:10.4072/rbp.2004.2.01
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