First record of a fossil chiton (Polyplacophora) from the Bohemian Cretaceous Basin (Late Cretaceous)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10192224" target="_blank" >RIV/00216208:11310/13:10192224 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

First record of a fossil chiton (Polyplacophora) from the Bohemian Cretaceous Basin (Late Cretaceous)

Popis výsledku v původním jazyce

The first record of a chiton (Polyplacophora) from the Bohemian Cretaceous Basin (Late Cretaceous) is described herein. It comes from the working quarry of Plaňany, located near the town Kolín. Excavated deposits are of the late Cenomanian - early Turonian. The poorly preserved specimen consists of a tail valve remain and two intermediate valves, it is associated herein only with order level - i.e. Lepidopleurida Thiele, 1910. The state of its preservation shows signs of corrosion of dorsal part causedprobably by biologic digestion (in stomach) and/or, more probably, by long exposure at the sea bottom. Stratigraphically, the layer yielding chiton shell is referred to be the late Cenomanian in age. The chiton living conditions are interpreted a very shallow water environment (not exceeding 20m) with irregular rocky basement possessing numerous caves and crevices.

Název v anglickém jazyce

First record of a fossil chiton (Polyplacophora) from the Bohemian Cretaceous Basin (Late Cretaceous)

Popis výsledku anglicky

The first record of a chiton (Polyplacophora) from the Bohemian Cretaceous Basin (Late Cretaceous) is described herein. It comes from the working quarry of Plaňany, located near the town Kolín. Excavated deposits are of the late Cenomanian - early Turonian. The poorly preserved specimen consists of a tail valve remain and two intermediate valves, it is associated herein only with order level - i.e. Lepidopleurida Thiele, 1910. The state of its preservation shows signs of corrosion of dorsal part causedprobably by biologic digestion (in stomach) and/or, more probably, by long exposure at the sea bottom. Stratigraphically, the layer yielding chiton shell is referred to be the late Cenomanian in age. The chiton living conditions are interpreted a very shallow water environment (not exceeding 20m) with irregular rocky basement possessing numerous caves and crevices.

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

2013

Kód důvěrnosti údajů

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

Název periodika

Folia Musei rerum naturalium Bohemiae occidentalis - Geologica et Paleobiologica

ISSN

1805-2371

e-ISSN

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Svazek periodika

47

Číslo periodika v rámci svazku

1-2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

6

Strana od-do

27-32

Kód UT WoS článku

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EID výsledku v databázi Scopus

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