Neoproterozoic to early Cambrian Franciscan-type mélanges in the Teplá–Barrandian unit, Bohemian Massif: Evidence of modern-style accretionary processes along the Cadomian active margin of Gondwana?

2013 ◽  
Vol 224 ◽  
pp. 653-670 ◽  
Author(s):  
Jaroslava Hajná ◽  
Jiří Žák ◽  
Václav Kachlík ◽  
Wolfgang Dörr ◽  
Axel Gerdes
Keyword(s):  
Bohemian Massif ◽  
Early Cambrian ◽  
Active Margin ◽  
Modern Style

Diverse pelagic predators from the Chengjiang Lagerstätte and the establishment of modern-style pelagic ecosystems in the early Cambrian

2007 ◽  
Vol 254 (1-2) ◽  
pp. 307-316 ◽  
Author(s):  
Shixue Hu ◽  
Michael Steiner ◽  
Maoyan Zhu ◽  
Bernd-Dietrich Erdtmann ◽  
Huilin Luo ◽  
...  
Keyword(s):  
Early Cambrian ◽  
Modern Style ◽  
Chengjiang Lagerstätte ◽  
Pelagic Ecosystems

Vestige of an Early Cambrian incipient oceanic crust incorporated in the Variscan orogen: Letovice Complex, Bohemian Massif

2010 ◽  
Vol 167 (6) ◽  
pp. 1113-1130 ◽  
Author(s):  
Igor Soejono ◽  
Eliška Žáčková ◽  
Vojtĕch Janoušek ◽  
Matĕj Machek ◽  
Jan Košler
Keyword(s):  
Oceanic Crust ◽  
Bohemian Massif ◽  
Early Cambrian ◽  
Variscan Orogen

The earliest ostracods from the Ordovician of the Prague Basin, Czech Republic

2014 ◽  
Vol 64 (4) ◽  
pp. 367-392 ◽  
Author(s):  
Karolína Lajblová ◽  
Petr Kraft
Keyword(s):  
Czech Republic ◽  
Bohemian Massif ◽  
Massif Central ◽  
Central European ◽  
Middle Ordovician ◽  
Prague Basin ◽  
Barrandian Area ◽  
Fossil Assemblages ◽  
European Variscides

Abstract The earliest ostracods from the Bohemian Massif (Central European Variscides) have been recorded from the Middle Ordovician of the Prague Basin (Barrandian area), in the upper Klabava Formation, and became an abundant component of fossil assemblages in the overlying Šarka Formation. Both early ostracod associations consist of eight species in total, representing mainly eridostracans, palaeocopids, and binodicopids. The revision, description, or redescription of all species and their distribution in the basin is provided. Their diversification patterns and palaeogeographical relationships to ostracod assemblages from other regions are discussed.

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