The Lower Palaeozoic palaeobiogeography of Bivalvia

Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F13%3A00000328" target="_blank" >RIV/00025798:_____/13:00000328 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1144/M38.16" target="_blank" >http://dx.doi.org/10.1144/M38.16</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1144/M38.16" target="_blank" >10.1144/M38.16</a>

Jazyk výsledku
angličtina
Název v původním jazyce
The Lower Palaeozoic palaeobiogeography of Bivalvia
Popis výsledku v původním jazyce
Bivalves appeared in Early Cambrian and were virtually cosmopolitan. In Early Ordovician the class was confined to Gondwana,their habitat was principally infaunal in the siliciclastic sediments. In the Mid Ordovician a few forms reached Baltica and Laurentia and in the Late Ordovician they become again cosmopolitan. The Silurian faunas were cosmopolitan and the major evolutionary event was caused by the appearance of a Gondwanana cephalopod limestone facies that provided sites for praecardiidinid bivalves.
Název v anglickém jazyce
The Lower Palaeozoic palaeobiogeography of Bivalvia
Popis výsledku anglicky
Bivalves appeared in Early Cambrian and were virtually cosmopolitan. In Early Ordovician the class was confined to Gondwana,their habitat was principally infaunal in the siliciclastic sediments. In the Mid Ordovician a few forms reached Baltica and Laurentia and in the Late Ordovician they become again cosmopolitan. The Silurian faunas were cosmopolitan and the major evolutionary event was caused by the appearance of a Gondwanana cephalopod limestone facies that provided sites for praecardiidinid bivalves.

Projekt
—
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

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