Dicroidium zuberi

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Dicroidium zuberi
Temporal range: Early Triassic–Late Triassic
Dicroidium zuberi leaf.jpg
Dicroidium zuberi leaf from the Early Triassic Gosford Formation of Terrigal, NSW, Australia.
Scientific classification Red Pencil Icon.png
Kingdom: Plantae
Clade: Tracheophytes
Division: Pteridospermatophyta
Order: Peltaspermales
Family: Corystospermaceae
Genus: Dicroidium
Species:
D. zuberi
Binomial name
Dicroidium zuberi
Holmes and Ash 1979

Dicroidium zuberi is a large bipinnate species of the seed fern Dicroidium with a forked rachis. The leaves are affiliated with Umkomasia feistmantellii megasporophylls and Petruchusbarrealensis microsporophylls. [1] [2]

Contents

D. zuberi was a common species in the coeval vegetation of the Sydney and Lorne Basins of New South Wales. Specimens have been found near Wairaki Hut and indicate that this species may have been as common in Scytho-Anisian vegetation of coastal New Zealand. In younger rocks younger than the late Anisian, they are outnumbered by unipinnate Dicroidium leaves such as those belonging to D. odontopteroides. [2]

Description

Leaf of Dicroidium zuberi from Brokvale, NSW in Hawkesbury Sandstone, Early Triassic. Specimen in Australian Museum, Sydney Dicroidium zuberi 2.jpg
Leaf of Dicroidium zuberi from Brokvale, NSW in Hawkesbury Sandstone, Early Triassic. Specimen in Australian Museum, Sydney

Dicroidium zuberi had large, bipinnate, thick and leathery leaves. The leaves were up to 21 cm long. The rachis is proximately forked once with opposite or sub-opposite pinnae that is imparipinnate. The largest pinnae found measure 8 cm long and 3 cm wide. The pinna rachis are between 2 and 5 cm wide with a distinct median ridge. The individual pinnules were closely spaced and frequently overlapping. The pinnules were rhomboidal or broadly oval, and usually slightly contracted at the base with entire or slightly lobed margins and an obtuse apex. The terminal pinnule of each frond was oval or oblong in shape. [1]

The stomatal frequency on both sides of the frond were similar, with irregularly oriented stomata evenly distributed over the entire surface of the leaves. Each of the stomata had typically 5 but sometimes 4 or 6 subsidiary cells that were rarely papillate and rarely in close contact with one another. The thinly cutinised guard cells were slightly sunken into the surface of the frond, appearing as an apature-like slit in a rectangular stomatal pit that was thickly cutinised on the lateral sides, with no encircling cells present. [1]

Location

D. zuberi is found in the southern hemisphere, from Australia, South Africa, India, and Argentina. It is the most consistently occurring species in the Triassic succession of Peninsular India, found in the Panchet Formation, Ramkola–Tatapani Coalfied, Balrampur District, Chhattisgarh, Tiki and Parsora formations, South Rewa Gondwana Basin and Pathargarh beds of Kamthi Formation, Mahanadi Valley Basin. [1] [2]

Taxonomy

After 1967, D. zuberi now unites four species previously categorized in the genus Zuberia, namely Z. sahnii, Z. barrealensis, Z. zuberi, and Z. feistmanteli. This combination was suggested by Sergio Archangelsky due to the lack of differences in size, shape, and venation of pinnules. These four species were described by Frenguelli in 1943 and 1944, and were originally united as a single species in the genus Dicroidium as D. feistmanteli by Bonetti in 1966. [3]

Neotype

The original type specimen of Zuberia zuberi was described by Szajnocha as Cardiopteris zuberi and under Archangelsky's combination of four Zuberia species should be the holotype for D. zuberi. However, a neotype (LP 9520) was selected by Archangelsky as he did not know where the holotype was located when he described D. zuberi. [3]

Related Research Articles

Pinnation

Pinnation is the arrangement of feather-like or multi-divided features arising from both sides of a common axis. Pinnation occurs in biological morphology, in crystals, such as some forms of ice or metal crystals, and in patterns of erosion or stream beds.

Frond collection of leaflets on a plant

A frond is a large, divided leaf. In both common usage and botanical nomenclature, the leaves of ferns are referred to as fronds and some botanists restrict the term to this group. Other botanists allow the term frond to also apply to the large leaves of cycads, as well as palms (Arecaceae) and various other flowering plants, such as mimosa or sumac. "Frond" is commonly used to identify a large, compound leaf, but if the term is used botanically to refer to the leaves of ferns and algae it may be applied to smaller and undivided leaves.

<i>Osmunda regalis</i> Species of fern

Osmunda regalis, or royal fern, is a species of deciduous fern, native to Europe, Africa and Asia, growing in woodland bogs and on the banks of streams. The species is sometimes known as flowering fern due to the appearance of its fertile fronds.

<i>Dryopteris affinis</i> Species of fern in the family Dryopteridaceae

Dryopteris affinis, the scaly male fern or golden-scaled male fern, is a fern native to western and southern Europe and southwestern Asia. It is most abundant on moist soils in woodlands in areas with high humidity, such as the British Isles and western France. In the Mediterranean region and the Caucasus it is confined to high altitudes.

Alsophila hornei is a species of tree fern in the Cyatheaceae family.

<i>Dicroidium</i> Extinct genus of seed ferns

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.

Pachypteris (Brongn.) T.M.Harris. is a Mesozoic pteridosperm leaf fossil probably belonging to the seed fern Order Peltaspermales.

<i>Adiantum viridimontanum</i> A rare fern found only in outcrops of serpentine rock in New England and Eastern Canada

Adiantum viridimontanum, commonly known as Green Mountain maidenhair fern, is a rare fern found only in outcrops of serpentine rock in New England and Eastern Canada. The leaf blade is cut into finger-like segments, themselves once-divided, which are borne on the outer side of a curved, dark, glossy rachis. These finger-like segments are not individual leaves, but parts of a single compound leaf. The "fingers" may be drooping or erect, depending on whether the individual fern grows in shade or sunlight. Spores are borne under false indusia at the edge of the subdivisions of the leaf, a characteristic unique to the genus Adiantum.

<i>Cyathea borbonica</i> Species of fern

Cyathea borbonica is a tree fern endemic to Mauritius, Réunion and the islands of the south-western Indian Ocean. There are several natural forms and varieties.

<i>Asterotheca</i> Genus of plants

Asterotheca is a genus of seedless, spore-bearing, vascularized ferns dating from the Carboniferous of the Paleozoic to the Triassic of the Mesozoic.

<i>Lepidopteris</i> Extinct genus of seed ferns

Lepidopteris is a form genus for leaves of Late Permian to Late Triassic Period Pteridospermatophyta, or seed ferns, which lived from around 260 to 200 million years ago in what is now Australia, Antarctica, India, South America, South Africa, Russia and China. Nine species are currently recognized. Lepidopteris was a common and widespread seed fern, which survived the Permian-Triassic extinction event but succumbed to the Triassic-Jurassic extinction event. Lepidopteris callipteroides is especially common between the first two episodes of Permian-Triassic extinction event, and L. ottonis forms a comparable acme zone immediate before the Triassic-Jurassic extinction event. Lepidopteris would persist into the Early Jurassic in Patagonia, represented by the species Lepidopteris scassoi.

<i>Umkomasia</i> Extinct genus of seed ferns

Umkomasia is a genus of seed bearing organs produced by corystosperm seed ferns, first based on fossils collected by Hamshaw Thomas from the Burnera Waterfall locality near the Umkomaas River of South Africa. He recognized on the basis of cuticular similarities that the same plant produced pollen organs Pteruchus and the leaves Dicroidium. Various other corystosperm seed bearing organs from the Jurassic and Cretaceous have been assigned to this genus, but recently have been given distinct genera, with Umkomasia being restricted to the Triassic.

<i>Umkomasia feistmantelii</i> Extinct species of plant

Umkomasia feistmantelii is an unusually large species of Umkomasia from the Early Triassic of New South Wales, Australia.

<i>Pteruchus barrealensis</i> Extinct species of flowering plant

Pteruchus barrealensis is an unusually large species of Pteruchus with very elongate polleniferous heads from Early Triassic of Australia and Argentina.

<i>Pteruchus</i> Extinct genus of seed ferns

Pteruchus is a form genus for pollen organs of the seed fern (Pteridospermatophyta family Umkomasiaceae. It was first described by Hamshaw Thomas from the Umkomaas locality of South Africa. It is associated with the seed bearing organs Umkomasia and Dicroidium leaves.

Corystospermaceae Extinct family of seed ferns

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 The leaves of Dicroidium were recognized by Alex Du Toit 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, and also the Permian Umm Irna Formation of Jordan. 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. Corystospermaceae were also components of Jurassic and Cretaceous floras, declining in the Cretaceous presumably due to the rise of flowering plants, the last representative of the group, Komlopteris cenozoicus, is known from the Eocene of Tasmania.

Tupuangi Formation

The Tupuangi Formation is a geological formation in New Zealand, only exposed on Pitt Island in the Chatham Islands. It is the oldest exposed sedimentary unit within the archipelago. It was deposited in terrestrial deltaic to paralic conditions during the Cenomanian to Turonian stages of the Late Cretaceous. During this time period the Chatham Islands were attached to Antarctica within the Antarctic Circle, at approximately 70° to 80° south.

Argyrochosma connectens is a small cheilanthoid fern endemic to Sichuan, China. It is the only member of its genus known from Asia. Relatively rare, it is found growing in the crevices of limestone rocks in hot, dry valleys. The species was long classified in the genus Pellaea, but after a phylogenetic study in 2015 was transferred to Argyrochosma.

Ticoa is a genus originally assigned to the Cycadales from the Early Cretaceous of Argentina, Chile, and Antarctica. Other authors view this genus as a member of the poliphyletic "seed ferns".

Mesosingeria is a genus of fossil foliage attributable to the Cycadales. This genus is found in Early Cretaceous rocks from Argentina.

References

  1. 1 2 3 4 Anderson, Heidi M.; Barbacka, Maria; Bamford, Marion K.; Holmes, W. B. Keith; Anderson, John M. (2020-01-02). "Dicroidium (foliage) and affiliated wood Part 3 of a reassessment of Gondwana Triassic plant genera and a reclassification of some previously attributed". Alcheringa: An Australasian Journal of Palaeontology. 44 (1): 64–92. doi:10.1080/03115518.2019.1622779. ISSN   0311-5518. S2CID   199109037.
  2. 1 2 3 Retallack, Greg J. (1977). "Reconstructing Triassic vegetation of eastern Australasia: a new approach for the biostratigraphy of Gondwanaland". Alcheringa: An Australasian Journal of Palaeontology. 1 (3): 247–278. doi:10.1080/03115517708527763. ISSN   0311-5518.
  3. 1 2 ARCHANGELSKY, S.; BRETT, D. W. (1963). "Studies on Triassic Fossil Plants from Argentina". Annals of Botany. 27 (1): 147–154. doi:10.1093/oxfordjournals.aob.a083828. ISSN   1095-8290.