Programmes > Par auteur > Koulakovska Larissa

Upper Palaeolithic environments in the loess plain of Central and East Europe. Contribution of charcoal and pollen records
Freddy Damblon  1, *@  , Paul Haesaerts  1@  , Vasile Chirica  2@  , Larissa Koulakovska  3@  , Andrei Sinitsyn  4@  , Philip Nigst  5@  
1 : Institut Royal des Sciences Naturelles de Belgique  (IRSNB)  -  Site web
Rue Vautier, 29 B-1000 Bruxelles -  Belgique
2 : Institut d'Archeologie de iASI  (IAI)  -  Site web
3 : National Academy of Science of Ukraine, Institute of Archaeology
Kiev -  Ukraine
4 : Institute of the History of Material Culture, Russian Academy of Sciences
St-Petersburg -  Russie
5 : University of Cambridge (UK)  (CAM)  -  Site web
Division of Archaeology Department of Archaeology and Anthropology University of Cambridge Downing Street Cambridge CB2 3DZ -  Royaume-Uni
* : Auteur correspondant

From Austria to Central Russia, several long loess sequences provided detailed paleoclimatic records for the period covering the middle and upper Pleniglacial. The high frequency of well-identified charcoal helped establish a precise and reliable chronology of the climate events for these periods in the continental area.

The reconstruction of paleo-environment of the Upper Palaeolithics in the loess area are based on pedostratigraphy and paleobiologic studies (pollen, charcoal, wood, bones, shells). When pollen records provide a regional picture of the landscapes, the presence of charcoal testifies to local and regional origin of the taxa and plays a main role in the physical identification of refuge areas for arboreal species during the Last Glacial.

In the loess of Central and Eastern Europe, paleobiologic data lead to recognize the predominance of steppe and steppe meadow environments and to detect the persistence of eurythermic and boreal trees in connection with the wet biotopes and streams. The extension of these populations fluctuated following the changes in the climate. Several hundred analyses of charcoal in this area have highlight no malacophyllous tree species of tempered character for the periods under consideration. On the contrary, the few fragments of these proved to be intrusive from Holocene material.

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