Corystospermaceae

Corystosperms are a group of extinct seed plants (often referred to as " seed ferns") belonging to the family Corystospermaceae (also called Umkomasiaceae) assigned to the order Corystospermales or Umkomasiales. They were first described based on fossils collected by Hamshaw Thomas from the Burnera Waterfall locality near the Umkomaas River of South Africa. Corystosperms are typified by a group of plants that bore forked '' Dicroidium'' leaves, '' Umkomasia'' cupulate ovulate structures and '' Pteruchus'' pollen organs, which grew as trees that were widespread over Gondwana during the Middle and Late Triassic. Other fossil Mesozoic seed plants with similar leaf and/or reproductive structures have also sometimes been included within the "corystosperm" concept ''sensu lato'', such as the "doyleoids" from the Early Cretaceous of North America and Asia. A potential corystosperm ''sensu lato'', the leaf genus '' Komlopteris'', is known from the Eocene of Tasmania, around 53-50 million years old, over 10 million years after the Cretaceous–Paleogene extinction event.

Description

Classic Umkomasiaceae have helmet-like cupules around ovules born in complex large branching structures ('' Umkomasia''). The pollen organ ('' Pteruchus'') has numerous cigar-shaped pollen sacs hanging from epaulette-like blades, again in complex branching structures.

The architecture and size of '' Dicroidium'' leaves is highly variable, going from simple to tripinnate, to needle-like to lobed or dissected leaflets, however, all leaves are united by being bifurcated at the base.

The ''Dicroidium'' plant (which bore ''Dicroidium'' leaves, ''Umkomasia'' seed bearing structures and ''Pteruchus'' pollen organs) is thought to have grown as large trees, with trunks at least tall and over wide. Some other possible corystosperms like ''Pachypteris'' may have grown as shrubs.

Evolutionary history

The oldest fossils of corystosperms, belonging to ''Dicroidium, Pteruchus'' and ''Umkomasia'' date to the Late Permian in the low-latitudes of eastern Gondwana, including the Umm Irna Formation of Jordan, as well as the Indian subcontinent, though possible pollen belonging to the group is also known from the Late Permian of South Africa. During the Middle-Late Triassic, ''Dicroidium'' bearing corystosperms were widespread and dominant trees over temperate areas of southern Gondwana (including the Indian subcontinent, South America, Southern Africa, Antarctica, Australia and New Zealand) including wetland and forest environments, where they formed part of the canopy vegetation. ''Dicroidium-''bearing corystosperm ecosystems collapsed as a result of the end-Triassic extinction event. Late surviving ''Dicroidium''-bearing corystosperms are known from the Early Jurassic (Sinemurian) of East Antarctica. During the Jurassic, the possible corystosperms '' Pachypteris'' and '' Komlopteris'' were widespread over both hemispheres, with ''Komlopteris'' surviving in the Southern Hemisphere through the Cretaceous and into the early Eocene in Tasmania, making it the last surviving "seed fern" in the fossil record. A group of plants with corystosperm-like reproductive structures, either considered corystosperms or as belonging to the separate order Doyleales, were present in North America and Asia during the Early Cretaceous, with records of the group possibly extending back as far as the Early Jurassic.

List of genera

* '' Umkomasia'' ovulate structures
* '' Pteruchus'' pollen organs
* '' Dicroidium'' leaves
* '' Johnstonia'' leaves
* '' Komlopteris''? leaves
* '' Kurtziana''? leaves
* '' Pachypteris''? leaves
* '' Xylopteris'' leaves
* '' Antarcticoxylon'' wood
* '' Kyklyxylon'' wood
* '' Rhexoxylon'' wood
* "Doyleoids" (sometimes included)
** '' Doylea'' ovulate structures
** '' Jarudia'' ovulate structures
** '' Tevshiingovia'' ovulate structures
** '' Zirabia'' ovulate structures

Relationships to other seed plants

The relationships of corystosperms to other seed plants are contentious. It has been suggested that some " peltasperms" may be closely related to corystosperms. A 2016 paper suggested that they may be closely related to Ginkgoales, while a 2021 study suggested that based on the structure of their ovulate organs, corystosperms might form part of the " Anthophyte" clade more closely related to flowering plants than to living gymnosperms, alongside the Petriellales, Caytoniales, and glossopterids.

Nomenclature

Corystospermaceae is a family name which was not derived from a specific genus, an arrangement which is discouraged by the ICN. In light of this issue, Petriella (1981) proposed two solutions: either retain Corystospermaceae as a nomen conservandum, or replace it with a new name, Umkomasiaceae. Both names have been used frequently since then. Petriella additionally named a new order to encompass the family, Corystospermales. Doweld (2001) preferred a different name for the order, Umkomasiales. He also added a second family, Angaropeltidaceae (previously known as Cardiolepidaceae). Later sources generally classify Angaropeltidaceae (or its updated spelling, Angaropeltaceae) within Peltaspermales instead.

Gallery

Molteno Formation of South Africa)">
File:Umkomasia macleani.jpg, ''Umkomasia macleanii'' ovulate structure from Umkomaas
File:Pteruchus africanus.jpg, ''Pteruchus africanus'' pollen structure from Umkomaas
File:Dicroidium odontopteroides.jpg, ''Dicroidium odontopteroides'' leaf from Birds River

See also

* Evolution of plants

References

External links

*

{{Taxonbar, from=Q21588008

Pteridospermatophyta
Permian plants
Triassic plants
Prehistoric plant families
Permian first appearances
Triassic extinctions