Cordaitales

Cordaitales are an extinct order of woody plants that may have been early conifers, or which may have given rise to the conifers (Pinophyta), ginkgos (Ginkgophyta) and cycads (Cycadophyta). They had cone-like reproductive structures reminiscent of those of modern conifers. The Cordaitales appeared during the Carboniferous Period forming large trees that seem to have been particularly abundant on drier ground, in tropical environments. Also, some tall trees but also shrubby and mangrove-like species of Cordaitales seem to have grown in the Carboniferous coal swamps. Cordaitales were also abundant during the Permian, but became less important during the Triassic and died out during the time of the end-Triassic mass extinction. Many Cordaitales had elongated strap-like leaves, resembling some modern-day conifers of the Araucariaceae and Podocarpaceae. Common genera from the Carboniferous include Mesoxylon and Cordaixylon. Other genera are Noeggerathiopsis and Sumaropsis.

Cordaitales Temporal range: Carboniferous–Late Triassic PreꞒ Ꞓ O S D C P T J K Pg N
Cordaites lungatus
Scientific classification
Kingdom:	Plantae
Clade:	Tracheophytes
Division:	Pinophyta
Class:	Pinopsida
Order:	†Cordaitales
Families
†Cordaitaceae

Features of the female cone (megastrobilus) of the members of Cordaitales indicate that the cone scales, possessed by themselves and their descendants, may correspond to short shoots, rather than leaves. This is because the cone consists of these short shoots, emerging from bracts. Among conifers, a leaf of any kind does not emerge from the axil of a bract.[1]^:55