About: Faunal turnover near the Katian/Hirnantian boundary in the Prague Basin (Czech Republic)     Goto   Sponge   NotDistinct   Permalink

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  • Faunal and environmental changes near the Katian/Hirnantian boundary are reviewed. After disappearance of the Foliomena Fauna, the glacioeustatic sea level drop brought the shallower fauna basinwards. The bryozoan-brachiopod-pelmatozoan fauna appeared in the highly fossiliferous calcareous claystone (?perník? bed). The ?Pernik? bed yields transported bioclasts and many subautochthonnous deep-water elements, namely small strophomenoids and some trilobites. This fauna was followed upward (at the summit of the Králův Dvůr) by the Hirnantia Fauna Formation due by drastic cooling at the beginning of the Hirnantian.
  • Faunal and environmental changes near the Katian/Hirnantian boundary are reviewed. After disappearance of the Foliomena Fauna, the glacioeustatic sea level drop brought the shallower fauna basinwards. The bryozoan-brachiopod-pelmatozoan fauna appeared in the highly fossiliferous calcareous claystone (?perník? bed). The ?Pernik? bed yields transported bioclasts and many subautochthonnous deep-water elements, namely small strophomenoids and some trilobites. This fauna was followed upward (at the summit of the Králův Dvůr) by the Hirnantia Fauna Formation due by drastic cooling at the beginning of the Hirnantian. (en)
Title
  • Faunal turnover near the Katian/Hirnantian boundary in the Prague Basin (Czech Republic)
  • Faunal turnover near the Katian/Hirnantian boundary in the Prague Basin (Czech Republic) (en)
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  • Faunal turnover near the Katian/Hirnantian boundary in the Prague Basin (Czech Republic)
  • Faunal turnover near the Katian/Hirnantian boundary in the Prague Basin (Czech Republic) (en)
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  • RIV/49777513:23420/11:43897349!RIV12-AV0-23420___
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  • 199432
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  • RIV/49777513:23420/11:43897349
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  • Glaciation, Ordovician, Hirnantia Fauna, Prague Basin (en)
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  • [E2228DC1FD7D]
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  • Mergl, Michal
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  • Instituto Geologico y Minero de Espana
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  • 978-84-7840-857-3
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  • 23420
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