Corystospermaceae

Corystospermaceae is a natural family of seed ferns (Pteridospermatophyta) also called Umkomasiaceae, and first based on fossils collected by Hamshaw Thomas from the Burnera Waterfall locality near the Umkomaas River of South Africa [2] The leaves of Dicroidium were recognized by Alex Du Toit [3] to unite all the countries of the Gondwana supercontinent during the Triassic: Africa, South America, India, and Australia. Subsequently, Dicroidium was found in the Triassic of Antarctica and New Zealand,[4] and also the Permian of Jordan.[5] According to the form generic system of paleobotany, leaves are given separate generic names to ovulate and pollen organs, but the discovery of these reproductive organs in Africa by Thomas, and subsequently throughout Gondwana, strengthened Du Toit's concept of a continuous southern supercontinent.

Umkomasia macleanii ovulate structure from the Late Triassic, Molteno Formation of Umkomaas, South Africa

Corystospermaceae
Temporal range: Middle Permian–Late Triassic
Umkomasia macleanii reconstructed plant, Late Triassic, Molteno Formation, Umkomaas, South Africa.[1]
Scientific classification
Kingdom: Plantae
Clade: Tracheophytes
Division: †Pteridospermatophyta
Order: †Peltaspermales
Family: †Corystospermaceae
Thomas 1933
Genera
  • Umkomasia ovulate structures
  • Pteruchus pollen organs
  • Dicroidium leaves
  • Johnstonia leaves
  • Xylopteris leaves
  • Kyklyxylon wood
  • Antarcticoxylon wood
  • Rhexoxylon wood

Description

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.

Pteruchus africanus pollen structure from the Late Triassic, Molteno Formation of Umkomaas, South Africa

The leaves (Dicroidium) are tied to the fertile organs by similarities of cuticular structure, because their cuticles were robust like those of gymnosperms and unlike the thin leaves of ferns.

Dicroidium odontopteroides leaf from the Late Triassic, Molteno Formation of Birds River, South Africa
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See also
  • Evolution of plants

References
  1. Retallack, G.J.; Dilcher, D.L. (1988). "Reconstructions of selected seed ferns". Missouri Botanical Garden Annals. 75: 1010–1057. doi:10.2307/2399379.
  2. Thomas, H.H. (1933). "On some pteridospermous plants from the Mesozoic rocks of South Africa". Philosophical Transactions of the Royal Society B. 222: 193–265. doi:10.1098/rstb.1932.0016.
  3. Du Toit, A.L. (1937). Our wandering continents. Oliver and Boyd, London. pp. 366 pp.
  4. Retallack,G.J. (1977). "Reconstructing Triassic vegetation of Australasia: a new approach for the biostratigraphy of Gondwanaland". Alcheringa. 1: 247–278. doi:10.1080/03115517708527763.
  5. Hamad, A.A.; Kerp, H.; Vörding, B. & Bandel, K. (2008). "A late Permian flora with Dicroidium from the Dead Sea region, Jordan". Review of Palaeobotany and Palynology. 149: 85–130. doi:10.1016/j.revpalbo.2007.10.006.
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