Eclogite subduction wedge intruded by arc-type magma: the earliest record of Variscan arc in the Bohemian Massif

2021 ◽  
Author(s):  
Piérig Deiller ◽  
Pavla Štípská ◽  
Marc Ulrich ◽  
Karel Schulmann ◽  
Stephen Collett ◽  
...  
2021 ◽  
Vol 559 ◽  
pp. 119919
Author(s):  
Prokop Závada ◽  
Pavla Štípská ◽  
Pavlína Hasalová ◽  
Martin Racek ◽  
Petr Jeřábek ◽  
...  

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.


Author(s):  
Karel Breiter ◽  
Michaela Vašinová_Galiová ◽  
Zuzana Korbelová ◽  
Michaela Vaňková ◽  
Viktor Kanický
Keyword(s):  

The Holocene ◽  
2021 ◽  
pp. 095968362110116
Author(s):  
Lucie Juřičková ◽  
Jakub Menšík ◽  
Jitka Horáčková ◽  
Vojen Ložek

The Alps are an important hotspot of species diversity and endemism, as well as a presumed glacial refugium of several species’ groups including land snails. The recent ranges of Alpine endemics are well known, but their fluctuations during the postglacial period mirroring local climate changes are understudied. By analysing five Late Glacial and Holocene mollusc successions from two areas in the southernmost part of the Bohemian Massif (Czech Republic) situated about 100 km north of the Alps, we reveal details of these fluctuations. The Alpine endemic rocky dweller Chilostoma achates had reached the southern part of the Bohemian Massif already in the Late Glacial and disappeared in the Mid-Holocene canopy forest optimum. On the contrary, the northern boundaries of Alpine canopy forest epigeic snails extended further north than today at the turn of the Middle and Late-Holocene, pointing to a more favourable forest microclimate. The earliest known occurrences of several temperate canopy forest central European species, especially Causa holosericea and Discus perspectivus, imply the role of different areas in the Alps as their glacial refugia.


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