The Elbe Fault System in North Central Europe—a basement controlled zone of crustal weakness

2002 ◽  
Vol 360 (1-4) ◽  
pp. 281-299 ◽  
Author(s):  
Magdalena Scheck ◽  
Ulf Bayer ◽  
Volker Otto ◽  
Juliette Lamarche ◽  
Dirk Banka ◽  
...  
2005 ◽  
Vol 397 (1-2) ◽  
pp. 113-126 ◽  
Author(s):  
Yuriy Maystrenko ◽  
Ulf Bayer ◽  
Magdalena Scheck-Wenderoth

Antiquity ◽  
1964 ◽  
Vol 38 (151) ◽  
pp. 201-216 ◽  
Author(s):  
Joachim Werner

The centuries between A.D. 400 and 800, which make the transition between Antiquity and the Middle Ages, are sparsely documented and have often been called by the English the ‘Dark Ages’, the dark centuries of Western European history. This paucity of written historical sources is greatly to be regretted, for these were decisive centuries for the formation of European society and in them occurred events whose results are to be seen even to the present day. The Roman Empire with its ancient civilisation collapsed; the countries on the southern shore of the Mediterranean went over to Islam; the Slavs settled in the Balkans, North-Central Europe, and the territory around the Danube as far as Austria; and these Danube-lands came under the domination of the Mongolian Avars.


The record of palaeobotanical data from the Early and Middle Devensian (to 18000 B.P.) is reviewed, with additional pollen data from the Devensian type site at Four Ashes presented. Pollen and macrofossil assemblages derive principally from herb vegetation, but woodland episodes are known from the Early Devensian. Correlations of herb and woodland biozones are made with events in the Weichselian sequences of the Netherlands and north central Europe, and comparisons are made with the north American Wisconsin interstadial sequence and events in the North Atlantic cores. The environment of the herb and woodland biozones is discussed. The effect of a cool Atlantic as a modifying factor affecting the longitudinal zonation of Middle Weichselian vegetation across north central Europe is considered. The relation between environmental evidence based on flora/vegetation and that on fauna is discussed. Apparent discrepancies result from inadequate solutions of the problems associated with interpreting palaeoclimates from fossil assemblages. An interpretation of the data in the context of variation of assemblages of the same age across north Europe may offer better solutions for these problems.


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