Carboniferous cuticles from the Lubná coal seam (Kladno Formation, Kladno-Rakovník Basin, Czech Republic)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F21%3A00000214" target="_blank" >RIV/00025798:_____/21:00000214 - isvavai.cz</a>
Výsledek na webu
<a href="https://www.schweizerbart.de/papers/palb/detail/prepub/100678/Carboniferous_cuticles_from_the_Lubna_coal_seam_Kladno_Formation_Kladno_Rakovnik_Basin_Czech_Republic" target="_blank" >https://www.schweizerbart.de/papers/palb/detail/prepub/100678/Carboniferous_cuticles_from_the_Lubna_coal_seam_Kladno_Formation_Kladno_Rakovnik_Basin_Czech_Republic</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1127/palb/2021/0076" target="_blank" >10.1127/palb/2021/0076</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Carboniferous cuticles from the Lubná coal seam (Kladno Formation, Kladno-Rakovník Basin, Czech Republic)
Popis výsledku v původním jazyce
More than 0 cuticle fragments have been selected from the Lubná coal seam section (Radnice Member, Kladno Formation, Pennsylvanian, Bolsovian, Czech Republic). The dispersed cuticles were classified into 25 informal categories (not including cordaitaleans). Among the dispersed cuticles, lycopsids dominate, namely sporangium walls of sub-arborescent Omphalophloios and cuticles from leaf cushions of arborescent lycopsids(Lepidodendron, Lepidophloios). Different kinds of stomata-less cuticles with polygonal and tetragonal cell imprints are difficult to assign to particular groups of ferns and pteridosperms. Some dispersed cuticles belong to the orders Lyginopteridales and Callistophytales. However, ferns and medullosans were not proven in the cuticular spectra, even though they probably grew in the original assemblage. Cordaitaleans were represented bydispersed leaf cuticles and also cuticles from fructification. Theyhave been found only in three samples and classified using the artificial system of dispersed cordaitalean cuticles as two new species of Cordaabaxicutis Šimůnek et Florjan. and a new species of Cordaadaxicutis Šimůnek et Florjan. Sphenopsids are represented only by very rare Sphenophyllum cuticles in two samples. Many cuticles with polygonal cell imprints belong to pteridosperm and cordaitalean seeds. The presence ofunidentified multicellular bodies is enigmatic. The dominance of lycopsids indicates a wet tropical forest, but the presence of Omphalophloios suggests perhaps seasonal alternation of wet and less humid periods. Cordaitaleans also grew in drier, more clastic, better-drained parts of the swamp. The cuticular assemblage from samples just below the roof-shales is the most diversified and probably contains also elements from the surroundings of the peat bog.
Název v anglickém jazyce
Carboniferous cuticles from the Lubná coal seam (Kladno Formation, Kladno-Rakovník Basin, Czech Republic)
Popis výsledku anglicky
More than 0 cuticle fragments have been selected from the Lubná coal seam section (Radnice Member, Kladno Formation, Pennsylvanian, Bolsovian, Czech Republic). The dispersed cuticles were classified into 25 informal categories (not including cordaitaleans). Among the dispersed cuticles, lycopsids dominate, namely sporangium walls of sub-arborescent Omphalophloios and cuticles from leaf cushions of arborescent lycopsids(Lepidodendron, Lepidophloios). Different kinds of stomata-less cuticles with polygonal and tetragonal cell imprints are difficult to assign to particular groups of ferns and pteridosperms. Some dispersed cuticles belong to the orders Lyginopteridales and Callistophytales. However, ferns and medullosans were not proven in the cuticular spectra, even though they probably grew in the original assemblage. Cordaitaleans were represented bydispersed leaf cuticles and also cuticles from fructification. Theyhave been found only in three samples and classified using the artificial system of dispersed cordaitalean cuticles as two new species of Cordaabaxicutis Šimůnek et Florjan. and a new species of Cordaadaxicutis Šimůnek et Florjan. Sphenopsids are represented only by very rare Sphenophyllum cuticles in two samples. Many cuticles with polygonal cell imprints belong to pteridosperm and cordaitalean seeds. The presence ofunidentified multicellular bodies is enigmatic. The dominance of lycopsids indicates a wet tropical forest, but the presence of Omphalophloios suggests perhaps seasonal alternation of wet and less humid periods. Cordaitaleans also grew in drier, more clastic, better-drained parts of the swamp. The cuticular assemblage from samples just below the roof-shales is the most diversified and probably contains also elements from the surroundings of the peat bog.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10506 - Paleontology
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2021
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Palaeontographica. Beiträge zur Naturgeschichte der Vorzeit Abt. B. Palaeobotany – Palaeophytology
ISSN
2194-900X
e-ISSN
—
Svazek periodika
303
Číslo periodika v rámci svazku
4-6
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
41
Strana od-do
77-117
Kód UT WoS článku
000723864500001
EID výsledku v databázi Scopus
2-s2.0-85120795162