Dicroidium
Dicroidium is an extinct genus of fork-leaved seed ferns that were widely distributed over Gondwana during the Triassic (). Their fossils are known from South Africa, the Arabian Peninsula, Australia, New Zealand, South America, Madagascar, the Indian subcontinent and Antarctica. They were first discovered in Triassic sediments of Tasmania by Morris in 1845. Fossils from the Umm Irna Formation in Jordan and in Pakistan indicate that these plants already existed in Late Permian. Late surviving members of the genus are known from the Early Jurassic (Sinemurian) of East Antarctica. Within paleobotany, "Dicroidium" is a form genus used to refers  to the leaves, associated with ovuluate organs classified as "Umkomasia" and pollen organs classified as "Pteruchus," while "Dicroidum" is also used collectively to refer to the whole plant. Description. The leaves are similar to those of modern ferns but like all seed ferns (Pteridospermatophyta) were thick and had substantial cuticles. "Dicroidium" differs from other seed fern leaves in having a forked rachis; giving the appearance of two fern leaves joined at the base. These plants had male and female reproductive structures. Following the form generic nomenclature of paleobotany, male pollen-bearing structures are separately named "Pteruchus" and the female structures  Umkomasia. Whole plant reconstructions. Different organs attributed to the same original plant can be reconstructed from co-occurrence at the same locality and from similarities in the stomatal apparatus and other anatomical peculiarities of fossilized cuticles.