Fossils in Late Cretaceous to Early Palaeocene flint nodules embedded in Pleistocene glaciofluvial sediments near Fukov (Děčín District, Northern Bohemia)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00023272%3A_____%2F12%3A%230001826" target="_blank" >RIV/00023272:_____/12:#0001826 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985831:_____/12:00387231 RIV/44555601:13520/12:43884499

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Fossils in Late Cretaceous to Early Palaeocene flint nodules embedded in Pleistocene glaciofluvial sediments near Fukov (Děčín District, Northern Bohemia)

Popis výsledku v původním jazyce

Faunal and floral fossil remains of Late Cretaceous ? Early Palaeocene age were recovered from flint pebbles from glaciofluvial gravel sediments in the Fukov area, northern Bohemia, the Czech Republic. Sedimentology of these sediments is discussed. Suggestions are made regarding the origin of the flints and their possible sources. The recovered taphocoenosis consists of one fossil plant taxon, nineteen bryozoans, three molluscs, one sabellid, and seven echinoderms. This type of flint and fossil fauna may indicate a pioneer character of the association found in glaciofluvial sediments near Fukov, perhaps an unconsolidated environment on a continental shelf margin which is characteristic for North-western European chalk. The occurrence of plant fossil inthis type of deep shelf sediment is unique and suggests the existence of some land mass at a relatively close distance to the place of deposition.

Název v anglickém jazyce

Fossils in Late Cretaceous to Early Palaeocene flint nodules embedded in Pleistocene glaciofluvial sediments near Fukov (Děčín District, Northern Bohemia)

Popis výsledku anglicky

Faunal and floral fossil remains of Late Cretaceous ? Early Palaeocene age were recovered from flint pebbles from glaciofluvial gravel sediments in the Fukov area, northern Bohemia, the Czech Republic. Sedimentology of these sediments is discussed. Suggestions are made regarding the origin of the flints and their possible sources. The recovered taphocoenosis consists of one fossil plant taxon, nineteen bryozoans, three molluscs, one sabellid, and seven echinoderms. This type of flint and fossil fauna may indicate a pioneer character of the association found in glaciofluvial sediments near Fukov, perhaps an unconsolidated environment on a continental shelf margin which is characteristic for North-western European chalk. The occurrence of plant fossil inthis type of deep shelf sediment is unique and suggests the existence of some land mass at a relatively close distance to the place of deposition.

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

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Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2012

Kód důvěrnosti údajů

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

Název periodika

Sborník Národního muzea v Praze. Řada B, přírodní vědy

ISSN

0036-5343

e-ISSN

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Svazek periodika

68

Číslo periodika v rámci svazku

3-4

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

13

Strana od-do

119-131

Kód UT WoS článku

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EID výsledku v databázi Scopus

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