Terebella phosphatica Leriche (Polychaeta) associated with phosphatic crusts and particles (Lower Turonian, Bohemian Cretaceous Basin, Czech Republic)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F13%3A00391032" target="_blank" >RIV/67985831:_____/13:00391032 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/00025798:_____/13:00000080
Výsledek na webu
<a href="http://dx.doi.org/10.1016/j.cretres.2012.11.003" target="_blank" >http://dx.doi.org/10.1016/j.cretres.2012.11.003</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.cretres.2012.11.003" target="_blank" >10.1016/j.cretres.2012.11.003</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Terebella phosphatica Leriche (Polychaeta) associated with phosphatic crusts and particles (Lower Turonian, Bohemian Cretaceous Basin, Czech Republic)
Popis výsledku v původním jazyce
The polychaete worm Terebella phosphatica Leriche occurs at the locality of Plaňany (Bohemian Cretaceous Basin) together with remains of the Atreta- Bdelloidina community, attached to the crystalline cobbles and boulders at the base of the Bílá Hora Formation, Whiteinella archaeocretacea Zone, the Lower Turonian. Terebella formed tubes with agglutinated phosphatic particles, mostly faecal pellets, firmly attached to the substrate. The surrounding phosphatic lag containing not only faecal pellets, but also coprolites, various indeterminate phosphatic particles and remains of phosphatized and unphosphatized macrofauna (ichthyolites, bivalves, sponges, crinoids) served as a source of phosphatic particles for the construction of the worm tubes. Formation of the phosphatic lag and the production and phosphatization of its components have been evaluated in relation to repeated phosphogenic episodes during which the phosphatic crusts covering the substrates encrusted by epifauna were formed.
Název v anglickém jazyce
Terebella phosphatica Leriche (Polychaeta) associated with phosphatic crusts and particles (Lower Turonian, Bohemian Cretaceous Basin, Czech Republic)
Popis výsledku anglicky
The polychaete worm Terebella phosphatica Leriche occurs at the locality of Plaňany (Bohemian Cretaceous Basin) together with remains of the Atreta- Bdelloidina community, attached to the crystalline cobbles and boulders at the base of the Bílá Hora Formation, Whiteinella archaeocretacea Zone, the Lower Turonian. Terebella formed tubes with agglutinated phosphatic particles, mostly faecal pellets, firmly attached to the substrate. The surrounding phosphatic lag containing not only faecal pellets, but also coprolites, various indeterminate phosphatic particles and remains of phosphatized and unphosphatized macrofauna (ichthyolites, bivalves, sponges, crinoids) served as a source of phosphatic particles for the construction of the worm tubes. Formation of the phosphatic lag and the production and phosphatization of its components have been evaluated in relation to repeated phosphogenic episodes during which the phosphatic crusts covering the substrates encrusted by epifauna were formed.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2013
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Cretaceous Research
ISSN
0195-6671
e-ISSN
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Svazek periodika
41
Číslo periodika v rámci svazku
April
Stát vydavatele periodika
GB - Spojené království Velké Británie a Severního Irska
Počet stran výsledku
16
Strana od-do
111-126
Kód UT WoS článku
000316582700011
EID výsledku v databázi Scopus
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