Hamatophyton verticillatum

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Hamatophyton verticillatum
Temporal range: Famennian–Tournaisian
Scientific classification OOjs UI icon edit-ltr.svg
Kingdom: Plantae
Clade: Tracheophytes
Division: Polypodiophyta
Class: Polypodiopsida
Subclass: Equisetidae
Order: Sphenophyllales
Genus: Hamatophyton
Species:
H. verticillatum
Binomial name
Hamatophyton verticillatum
L.-H. Deng, X.-X. Li, Z.-Y. Zhou, R. Xu, J.-N. Zhu, nom. inval. [1]
Synonyms [1] [2]
  • Sphenophyllostachys verticillata(L.-H. Deng, X.-X. Li, Z.-Y. Zhou, R. Xu, J.-N. Zhu) S.-N. Feng, J. Ma, nom. inval.

Hamatophyton verticillatum is a species of the extinct Sphenophyllales horsetails. [3]

Description

Axes of this plant are pseudomonopodial with axial trichomes or spines and nodal whorls of sterile leaves. Leaves are dimorphic and sometimes contain trichomes or spines. When mature, primary xylem is exarch and the secondary xylem lacks parenchyma. [3]

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<span class="mw-page-title-main">Vascular plant</span> Phylum of plants with xylem and phloem

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<span class="mw-page-title-main">Ginkgoales</span> Order of plants

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<span class="mw-page-title-main">Droseraceae</span> Family of carnivorous flowering plants

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<span class="mw-page-title-main">Trichome</span> Fine hair-like growth on plants

Trichomes are fine outgrowths or appendages on plants, algae, lichens, and certain protists. They are of diverse structure and function. Examples are hairs, glandular hairs, scales, and papillae. A covering of any kind of hair on a plant is an indumentum, and the surface bearing them is said to be pubescent.

<span class="mw-page-title-main">Paleobotany</span> Study of organic evolution of plants based on fossils

Paleobotany, also spelled as palaeobotany, is the branch of botany dealing with the recovery and identification of plant remains from geological contexts, and their use for the biological reconstruction of past environments (paleogeography), and the evolutionary history of plants, with a bearing upon the evolution of life in general. A synonym is paleophytology. It is a component of paleontology and paleobiology. The prefix palaeo- or paleo- means "ancient, old", and is derived from the Greek adjective παλαιός, palaios. Paleobotany includes the study of terrestrial plant fossils, as well as the study of prehistoric marine photoautotrophs, such as photosynthetic algae, seaweeds or kelp. A closely related field is palynology, which is the study of fossilized and extant spores and pollen.

<span class="mw-page-title-main">Winteraceae</span> Family of flowering plants

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<i>Psilophyton</i> Genus of fossil plants

Psilophyton is a genus of extinct vascular plants. Described in 1859, it was one of the first fossil plants to be found which was of Devonian age. Specimens have been found in northern Maine, USA; Gaspé Bay, Quebec and New Brunswick, Canada; the Czech Republic; and Yunnan, China. Plants lacked leaves or true roots; spore-forming organs or sporangia were borne on the ends of branched clusters. It is significantly more complex than some other plants of comparable age and is thought to be part of the group from within which the modern ferns and seed plants evolved.

<span class="mw-page-title-main">Polysporangiophyte</span> Spore-bearing plants with branched sporophytes

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<span class="mw-page-title-main">Lepidodendrales</span> Extinct order of vascular tree-like plants

Lepidodendrales or arborescent lycophytes are an extinct order of primitive, vascular, heterosporous, arborescent (tree-like) plants belonging to Lycopodiopsida. Members of Lepidodendrales are the best understood of the fossil lycopsids due to the vast diversity of Lepidodendrales specimens and the diversity in which they were preserved; the extensive distribution of Lepidodendrales specimens as well as their well-preservedness lends paleobotanists exceptionally detailed knowledge of the coal-swamp giants’ reproductive biology, vegetative development, and role in their paleoecosystem. The defining characteristics of the Lepidodendrales are their secondary xylem, extensive periderm development, three-zoned cortex, rootlike appendages known as stigmarian rootlets arranged in a spiralling pattern, and megasporangium each containing a single functional megaspore that germinates inside the sporangium. Many of these different plant organs have been assigned both generic and specific names as relatively few have been found organically attached to each other. Some specimens have been discovered which indicate heights of 40 and even 50 meters and diameters of over 2 meters at the base. The massive trunks of some species branched profusely, producing large crowns of leafy twigs; though some leaves were up to 1 meter long, most were much shorter, and when leaves dropped from branches their conspicuous leaf bases remained on the surface of branches. Strobili could be found at the tips of distal branches or in an area at the top of the main trunk. The underground organs of Lepidodendrales typically consisted of dichotomizing axes bearing helically arranged, lateral appendages serving an equivalent function to roots. Sometimes called "giant club mosses", they are believed to be more closely related to extant quillworts based on xylem, although fossil specimens of extinct Selaginellales from the Late Carboniferous also had secondary xylem.

<i>Pecopteris</i> Extinct genus of ferns

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<span class="mw-page-title-main">Thorns, spines, and prickles</span> Hard, rigid extensions or modifications of leaves, roots, stems or buds with sharp, stiff ends

In plant morphology, thorns, spines, and prickles, and in general spinose structures, are hard, rigid extensions or modifications of leaves, roots, stems, or buds with sharp, stiff ends, and generally serve the same function: physically defending plants against herbivory.

<span class="mw-page-title-main">Sphenophyllales</span> Order of plants

Sphenophyllales is an extinct order of articulate land plants and a sister group to the present-day Equisetales (horsetails). They are fossils dating from the Devonian to the Triassic. They were common during the Late Pennsylvanian to Early Permian, with most of the fossils coming from the Carboniferous period.

<i>Sphenophyllum</i> Extinct genus of ferns

Sphenophyllum is a genus in the order Sphenophyllales. It has been placed in the family Sphenophyllaceae.

<span class="mw-page-title-main">Rhacophytales</span> Extinct order of ferns

Rhacophytales are an extinct group of plants from the Devonian period.

Hamatophyton is a genus of the extinct Sphenophyllales horsetails. Unique to this genus among other Sphenophyllales is its lack of secondary xylem around the tips of the primary xylem arms. One of its species has also been placed in the genus Sphenophyllostachys, which is regarded as a synonym of Bowmanites by the Interim Register of Marine and Nonmarine Genera.

Rotafolia songziensis is a species of the extinct Sphenophyllales horsetails.

References

  1. 1 2 "Hamatophyton verticillata". International Fossil Plant Names Index. Retrieved 2024-02-24.
  2. "Sphenophyllostachys verticillata". International Fossil Plant Names Index. Retrieved 2024-02-24.
  3. 1 2 Taylor, T.N.; Taylor, E.L. & Krings, M. (2009). Paleobotany, The Biology and Evolution of Fossil Plants (2nd ed.). Amsterdam; Boston: Academic Press. ISBN   978-0-12-373972-8.