The term seed ferns (Pteridospermatophyta) are several groups of extinct seed plants (spermatophytes).
Late Devonian – End Cretaceous 376–66 mya
|Fossil seed fern leaves from the Pennsylvanian Carboniferous of northeastern Ohio.|
The oldest fossil evidence of plants of this type is from Upper Devonian strata. They flourished during the Carboniferous and Permian periods.
Pteridosperms declined during the Mesozoic Era and had mostly disappeared by the end of the Cretaceous. Some fossil pteridosperm-like plants seem to have survived into Eocene times in Tasmania.
History of the termEdit
The concept of the pteridosperms goes back to the late 19th century. Palaeobotanists saw that many Carboniferous fossils which looked like ferns had anatomical features like cycads.
British palaeobotanists made the discovery that some of these fronds were associated with seeds, and concluded that the fronds and seeds belonged to the same plants.
Initially it was still thought that they were intermediate between the ferns and cycads. In the English-speaking world they were referred to as "seed ferns" or "pteridosperms". Today, most palaeobotanists regard them as being only distantly related to ferns and that these names are misleading. The names have nevertheless stuck.
Later during the 20th century, the concept of pteridosperms was expanded to include various Mesozoic groups of seed plants with fern-like fronds. Some palaeobotanists also included seed plant groups with entire leaves such as Glossopteris and its relatives, which was clearly stretching the concept.
The seed ferns were by far the earliest seed plants, and must have included the ancestors of the later plants. They are spread across a number of clades, so many palaeobotanists today regard pteridosperms as little more than a paraphyletic 'grade-group'.
Does the concept of pteridosperms have any value today? Many palaeobotanists still use the term in an informal sense for the seed plants that are not angiosperms, coniferoids (conifers or cordaites), ginkgophytes or cycadophytes (cycads or bennettites).
This is useful for extinct seed plant groups, whose relationships are unknown. We can call them" pteridosperms" with no suggestion of their being a clade. Also, for curators or collectors, the term 'pteridosperm' is a useful shorthand for describing fern-like fronds probably produced by seed plants, which are often found in Palaeozoic and Mesozoic fossil floras.
- ↑ Rothwell G.W; Scheckler S.E. & Gillespie W.H. 1989. Elkinsia gen. nov., a late Devonian gymnosperm with cupulate ovules. Botanical Gazette, 150: 170-189.
- ↑ McLoughlin S; R.J. Carpenter, G.J. Jordan & R.S. Hill 2008. Seed ferns survived the end-Cretaceous mass extinction in Tasmania. American Journal of Botany, 95: 465-471.
- ↑ Oliver F.W. & Scott D.H. 1904. On the structure of the Palaeozoic seed Lagenostoma lomaxi, with a statement of the evidence upon which it is referred to Lyginodendron. Philosophical Transactions of the Royal Society of London, Series B, 197: 193–247.
- ↑ Hilton J. & Batemann R.M. 2007. Pteridosperms are the backbone of seed plant phylogeny. Journal of the Torrey Botanical Society, 33: 119-168. 119:PATBOS2.0.CO;2.short[permanent dead link]