The epiphytic plants in the fossil record and its example from in situ tuff from Pennsylvanian of Radnice Basin (Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10173863" target="_blank" >RIV/00216208:11310/13:10173863 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00228745:_____/13:#0000002

Výsledek na webu

<a href="http://dx.doi.org/10.3140/bull.geosci.1376" target="_blank" >http://dx.doi.org/10.3140/bull.geosci.1376</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.3140/bull.geosci.1376" target="_blank" >10.3140/bull.geosci.1376</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The epiphytic plants in the fossil record and its example from in situ tuff from Pennsylvanian of Radnice Basin (Czech Republic)

Popis výsledku v původním jazyce

Recognizing true epiphytes in the fossil record is still a major problem for palaeobotanists. Many indirect examples of evidence of epiphytic plants were previously published in palaeobotanical papers, especially from Pennsylvanian and Cenozoic times. Due to the special life strategy of epiphytes, which depends on presence of other plants for growth (so-called phorophytes), their preservation in the fossil record depends on the taphonomy of these phorophytes. Generally, the main factors for preservationof epiphytes are the type of environment in which the phorophyte grew, the habit-type of the epiphyte, the position of the epiphytes on the phorophyte, and the rapidity of burial. The ideal facies for preservation of epiphytes are in situ volcanic ash-fall deposits where plants were very quickly buried in the original place of growth. Vegetation buried in such deposits represents a single T-0 horizon that reveals the spatial distribution of plants including potential epiphytes. Examples

Název v anglickém jazyce

The epiphytic plants in the fossil record and its example from in situ tuff from Pennsylvanian of Radnice Basin (Czech Republic)

Popis výsledku anglicky

Recognizing true epiphytes in the fossil record is still a major problem for palaeobotanists. Many indirect examples of evidence of epiphytic plants were previously published in palaeobotanical papers, especially from Pennsylvanian and Cenozoic times. Due to the special life strategy of epiphytes, which depends on presence of other plants for growth (so-called phorophytes), their preservation in the fossil record depends on the taphonomy of these phorophytes. Generally, the main factors for preservationof epiphytes are the type of environment in which the phorophyte grew, the habit-type of the epiphyte, the position of the epiphytes on the phorophyte, and the rapidity of burial. The ideal facies for preservation of epiphytes are in situ volcanic ash-fall deposits where plants were very quickly buried in the original place of growth. Vegetation buried in such deposits represents a single T-0 horizon that reveals the spatial distribution of plants including potential epiphytes. Examples

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GAP210%2F12%2F2053" target="_blank" >GAP210/12/2053: Floristické změny jako důsledek vývoje klimatu v průběhu svrchnopaleozoické doby ledobé zaznamenané v pánvích Českého masívu</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název periodika

Bulletin of Geosciences

ISSN

1214-1119

e-ISSN

—

Svazek periodika

88

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

16

Strana od-do

401-416

Kód UT WoS článku

000319992000011

EID výsledku v databázi Scopus

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