Leaf cuticular analysis of the Upper Pennsylvanian and lower Cisuralian (Carboniferous - Permian) species of Cordaites UNGER from the Bohemian Massif, Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F24%3A10169145" target="_blank" >RIV/00025798:_____/24:10169145 - isvavai.cz</a>

Výsledek na webu

<a href="https://doi.org/10.1127/palb/2024/0083" target="_blank" >https://doi.org/10.1127/palb/2024/0083</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1127/palb/2024/0083" target="_blank" >10.1127/palb/2024/0083</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Leaf cuticular analysis of the Upper Pennsylvanian and lower Cisuralian (Carboniferous - Permian) species of Cordaites UNGER from the Bohemian Massif, Czech Republic

Popis výsledku v původním jazyce

Until now, poorly known cordaitalean leaves from the Stephanian and Permian of the Bohemian Massif have been studied through cuticular analysis that helped classify the known species and establish new species. Stomata arrangement patterns have enabled the cuticles to be classified into three principal groups: 1) Stomata dispersed more or less regularly over the cuticle [Cordaites rudnicensis, C. sudeticus and C. sudeticus (Kru &amp; scaron;ovice loc.)]; 2) Stomata arranged in simple or double stomatal rows (Cordaites malesicensis, C. radvanicensis, C. risutensis, C. roprachticensis sp. nov., C. setlikii, sp. nov. and C. pastuchovicensis sp. nov.); 3) Stomata arranged in stomatiferous bands consisting of several stomatal rows (Cordaites barthelii, C. melnicensis and C. cf. melnicensis). This new study brings new information on the spatial distribution of Cordaites species. The material studied came from coal mines, outcrops, and boreholes. The Cordaites leaves from boreholes are fragmentary, and cuticles help with their determination. The Cordaites came from different habitats: peat-forming swamps (samples from coal mines and some boreholes) and deltaic and lake deposits (mainly from outcrops). Cordaitaleans growing in peat-forming swamps indeed represent hygrophilous plants; the fragments found in the deltaic environment can be characterised as remains of mesophilous plants with less demand for water. The plants found in lake deposits could be either hygrophilous (nearly autochthonous that grew in coastal vegetation) or mesophilous (allochthonous, originally growing upstream, more or less far from the river that transported material to the lake). Cuticles of xerophilous cordaitaleans cannot be studied because their leaves have been found only as imprints in red deposits, and delicate cuticular structures are not preserved.

Název v anglickém jazyce

Leaf cuticular analysis of the Upper Pennsylvanian and lower Cisuralian (Carboniferous - Permian) species of Cordaites UNGER from the Bohemian Massif, Czech Republic

Popis výsledku anglicky

Until now, poorly known cordaitalean leaves from the Stephanian and Permian of the Bohemian Massif have been studied through cuticular analysis that helped classify the known species and establish new species. Stomata arrangement patterns have enabled the cuticles to be classified into three principal groups: 1) Stomata dispersed more or less regularly over the cuticle [Cordaites rudnicensis, C. sudeticus and C. sudeticus (Kru &amp; scaron;ovice loc.)]; 2) Stomata arranged in simple or double stomatal rows (Cordaites malesicensis, C. radvanicensis, C. risutensis, C. roprachticensis sp. nov., C. setlikii, sp. nov. and C. pastuchovicensis sp. nov.); 3) Stomata arranged in stomatiferous bands consisting of several stomatal rows (Cordaites barthelii, C. melnicensis and C. cf. melnicensis). This new study brings new information on the spatial distribution of Cordaites species. The material studied came from coal mines, outcrops, and boreholes. The Cordaites leaves from boreholes are fragmentary, and cuticles help with their determination. The Cordaites came from different habitats: peat-forming swamps (samples from coal mines and some boreholes) and deltaic and lake deposits (mainly from outcrops). Cordaitaleans growing in peat-forming swamps indeed represent hygrophilous plants; the fragments found in the deltaic environment can be characterised as remains of mesophilous plants with less demand for water. The plants found in lake deposits could be either hygrophilous (nearly autochthonous that grew in coastal vegetation) or mesophilous (allochthonous, originally growing upstream, more or less far from the river that transported material to the lake). Cuticles of xerophilous cordaitaleans cannot be studied because their leaves have been found only as imprints in red deposits, and delicate cuticular structures are not preserved.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10506 - Paleontology

Projekt

<a href="/cs/project/GF22-11661K" target="_blank" >GF22-11661K: Integrovaná stratigrafie mladšího paleozoika ve východní části tropické Pangey</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2024

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Palaeontographica. Beiträge zur Naturgeschichte der Vorzeit Abt. B. Palaeobotany-Palaeophytology

ISSN

2194-900X

e-ISSN

2509-839X

Svazek periodika

305

Číslo periodika v rámci svazku

5-6

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

71

Strana od-do

121-191

Kód UT WoS článku

001218860700001

EID výsledku v databázi Scopus

2-s2.0-85194277877