Oxygen and carbon stable isotope records of the Lochkovian-Pragian boundary interval from the Prague Basin (Lower Devonian, Czech Republic)

2020 ◽  
Vol 560 ◽  
pp. 110036
Author(s):  
Hedvika Weinerová ◽  
Ondřej Bábek ◽  
Ladislav Slavík ◽  
Hubert Vonhof ◽  
Michael M. Joachimski ◽  
...  
2018 ◽  
Vol 364 ◽  
pp. 71-88 ◽  
Author(s):  
Ondřej Bábek ◽  
Martin Faměra ◽  
Jindřich Hladil ◽  
Jaroslav Kapusta ◽  
Hedvika Weinerová ◽  
...  

2017 ◽  
Vol 97 (3) ◽  
pp. 419-438 ◽  
Author(s):  
Petra Tonarová ◽  
Stanislava Vodrážková ◽  
Lenka Ferrová ◽  
G. Susana de la Puente ◽  
Olle Hints ◽  
...  

Author(s):  
Petr Budil ◽  
František Hörbinger ◽  
Robert Mencl

ABSTRACTA revision of the Lower Devonian dalmanitid trilobites of the Prague Basin (Czech Republic) is presented. The subfamily Odontochilinae Šnajdr is considered a synonym of Dalmanitidae Vogdes. Twenty-one previously and five newly described (three in open nomenclature) species and subspecies occur in the Prague Basin from the lowermost Pragian (one problematic specimen possibly comes from the uppermost Lochkovian) to the Lower Emsian; the last questionable record is from the Upper Emsian. The species have been assigned to four genera and subgenera: Odontochile Hawle & Corda, Reussiana Šnajdr, Zlichovaspis (Zlichovaspis) Přibyl & Vaněk and Zlichovaspis (Devonodontochile) Šnajdr. These trilobites are considered as scavengers or opportunistic predators, living most of their lives as vagrant benthos burying in the muddy substrate to find organic remains. The first undoubted adult-like meraspid specimens are described.


2014 ◽  
Vol 64 (4) ◽  
pp. 367-392 ◽  
Author(s):  
Karolína Lajblová ◽  
Petr Kraft

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.


2017 ◽  
Vol 12 (3) ◽  
pp. 201-208 ◽  
Author(s):  
Jingyu Huang ◽  
Eyram Norgbey ◽  
Philip N. Nkrumah ◽  
Prince A. Opoku ◽  
Theresa O. Apreku

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