Relevant bibliographies by topics / Lepidodendrales

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  1. Journal articles

Academic literature on the topic 'Lepidodendrales'

Author: Grafiati
Published: 4 June 2025
Last updated: 1 August 2025

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Journal articles on the topic "Lepidodendrales"

1

Đordjević, Milutinović. "Permo-Carboniferous flora of the Mlava-Pek coal basin (Eastern Serbia)." Bulletin of the Natural History Museum, no. 17 (2024): 7–69. https://doi.org/10.5937/bnhmb2417007d.

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Approximately 400 fossil plant remains from the Late Stephanian and Stephanian-Permian periods had been found in Eastern Serbia, in the area between the rivers Mlava and Pek. They were classified into two collections: 'Mlava-Pek sensu lato' and 'Borogin Potok, Ranovac village'. The fossil materials are remnants of a tropical Carboniferous forest that was dominated by seed ferns, primarily Alethopteris, Linopteris, Odontopteris, Neuropteris, Autunia, and tree ferns, mostly Pecopteris / Asterotheca, Cordaites, and to a much lesser extent by Lepidodendrales and Equisetidae. The 'Mlava-Pek sensu l
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2

Cichan, Michael A. "VASCULAR CAMBIUM AND WOOD DEVELOPMENT IN CARBONIFEROUS PLANTS. I. LEPIDODENDRALES." American Journal of Botany 72, no. 8 (1985): 1163–76. http://dx.doi.org/10.1002/j.1537-2197.1985.tb08369.x.

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3

Menezes, Nanuza L. de. "Rhizophores in Rhizophora mangle L: an alternative interpretation of so-called ''aerial roots''." Anais da Academia Brasileira de Ciências 78, no. 2 (2006): 213–26. http://dx.doi.org/10.1590/s0001-37652006000200003.

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Rhizophora mangle L., one of the most common mangrove species, has an aerial structure system that gives it stability in permanently swampy soils. In fact, these structures, known as "aerial roots" or "stilt roots", have proven to be peculiar branches with positive geotropism, which form a large number of roots when in contact with swampy soils. These organs have a sympodial branching system, wide pith, slightly thickened cortex, collateral vascular bundles, polyarch stele and endarch protoxylem, as in the stem, and a periderm produced by a phellogen at the apex similar to a root cap. They als
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4

Flores-Barragan, Miguel Angel, María Patricia Velasco-de León, and Josep Anton Moreno-Bedmar. "Avances en el conocimiento de la macroflora de la Formación Tuzancoa, Hidalgo, México, Pérmico inferior." Revista Mexicana de Ciencias Geológicas 40, no. 1 (2023): 1–15. http://dx.doi.org/10.22201/cgeo.20072902e.2023.1.1694.

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La paleoflora de la Formación Tuzancoa ha sido estudiada desde mediados del siglo pasado. Sin embargo, el constante descubrimiento de nuevos elementos florísticos y/o localidades hace necesaria una reevaluación del conocimiento actual de la paleoflora de esta formación. El objetivo de este trabajo es dar a conocer los nuevos reportes paleoflorísticos de tres localidades de la Formación Tuzancoa, así como analizar su distribución geográfica, cronológica y su relación con otras floras coetáneas de México. Las localidades aquí estudiadas se denominan Calnali 2, La Virgen y San Mateo 2, siendo est
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5

Ramanujam, C. G. K. "Origin and evolution of lycopods." Journal of Palaeosciences 41 (December 31, 1992): 51–57. http://dx.doi.org/10.54991/jop.1992.1106.

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The lycopods are known from as early as Sieginean Stage of the Lower Devonian. Lower and Middle Devonian lycopods were all herbaceous. Arborescent taxa appeared by Upper Devonian (e.g., Cyclostigma and Lepidosigillaria). The microphyllous foliage of lycopods seem to have originated from enations as well as telomic trusses. The lycopods attained peak of their evolution during the Upper Carboniferous. Towards the close of the Carboniferous and dawn of the Permian, with gradual dwindling and disappearance of swamps, the lepidodendrids suffered drastic decline numerically and phytogeographically.
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6

Thomas, Barry A., and Leyla J. Seyfullah. "A new look at Lepidodendron ophiurus Brongniart and the recognition of L. wingfieldense sp. nov. (Flemingitaceae, Lepidodendrales) from the Langsettian (Bashkirian) of Derbyshire, East Midlands, UK." Palaeontographica Abteilung B 292, no. 1-3 (2015): 23–32. http://dx.doi.org/10.1127/palb/292/2015/23.

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7

Wang, Shi-Jun, Bao-Lin Tian, and Gui-Ren Chen. "Anatomically preserved lepidodendralean plants from Permian coal balls of China: leaves of Lepidophylloides Snigirevskaya." Review of Palaeobotany and Palynology 122, no. 1-2 (2002): 63–76. http://dx.doi.org/10.1016/s0034-6667(02)00104-5.

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8

Zhou, Yi-Long, Shi-Jun Wang, Jason Hilton, and Bao-Lin Tian. "Anatomically preserved lepidodendralean plants from lower permian coal balls of northern China: Achlamydocarpon intermedium sp. nov." Plant Systematics and Evolution 273, no. 1-2 (2008): 71–85. http://dx.doi.org/10.1007/s00606-008-0013-3.

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9

Yi‐Long, Zhou, Wang Shi‐Jun, Jason Hilton, and Gar W. Rothwell. "Achlamydocarpon pingquanensis sp. nov. (Lycopsida): A Novel, Anatomically Preserved Lepidodendralean Disseminule from the Lower Permian of North China." International Journal of Plant Sciences 167, no. 3 (2006): 567–77. http://dx.doi.org/10.1086/501070.

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10

HILTON, JASON, WANG SHI-JUN, JEAN GALTIER, IAN GLASSPOOL, and LIL STEVENS. "An Upper Permian permineralized plant assemblage in volcaniclastic tuff from the Xuanwei Formation, Guizhou Province, southern China, and its palaeofloristic significance." Geological Magazine 141, no. 6 (2004): 661–74. http://dx.doi.org/10.1017/s0016756804009847.

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A new permineralized fossil plant assemblage is described from volcaniclastic tuff collected in the Upper Permian (Wuchiapigian to Changhsingian) Xuanwei Formation at Shanjiaoshu mine, Guizhou Province, China. The assemblage is fragmentary but contains a small sphenopsid strobilus, a partial strobilus of a lepidodendralean lycopsid, pinnae of the filicalean fern Anachoropteris and a filicalean non-laminate fertile pinna rachis, the marattialean ferns Eoangiopteris, Scolecopteris and Psaronius, hooked stems of probable gigantopterid affinity, and two kinds of cardiocarpalean ovules. This repres
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