scholarly journals Last Glacial Maximum landscape and Epigravettian horse hunting strategy in Central Europe: The case of Stránská skála IV

2020 ◽  
pp. 59-70
Author(s):  
Jiří Svoboda ◽  
Soňa Boriová ◽  
György Lengyel ◽  
Petr Pokorný ◽  
Antonín Přichystal ◽  
...  

With the end of MIS3, the unity of larger Gravettian settlements based predominantly on mammoth exploitation split into a mosaic of smaller Epigravettian sites with specific behaviors and economies. Based on C14 chronology, the site of Stránská skála IV (together with Grubgraben, Ságvár and Kašov), correlates with a brief warm period after the Last Glacial Maximum around 22 ka calBP. We detected two main accumulations of predominantly horse bones under a rock cliff suggesting that the site was not a regular settlement but rather a specialised hunting site. No features or hearths were recovered. Lithic raw materials were imported from long distances, and the horse hunting strategy profitted from the specific geographic qualitites of the site. Preferential location of Epigravettian sites in secluded valleys is a pattern generally recognized in Moravia and usually explained as a response to the harsh MIS2 climates.

2022 ◽  
pp. 223-228
Author(s):  
Leszek Marks ◽  
Albertas Bitinas ◽  
Mirosław Błaszkiewicz ◽  
Andreas Börner ◽  
Rimante Guobyte ◽  
...  

Author(s):  
Pawel Wasowicz ◽  
Maxime Pauwels ◽  
Andrzej Pasierbinski ◽  
Ewa M Przedpelska-Wasowicz ◽  
Alicja A. Babst-Kostecka ◽  
...  

The present study aimed to investigate phylogeographical patterns present within A. halleri in Central Europe, to propose hypotheses explaining the emergence of these patterns and to formulate hypotheses on the formation of the present day range of A. halleri in the region. 1281 accessions sampled from 52 populations within the investigated area were used in the study of genetic variation based on chloroplast DNA. Over 500 high quality species occurrence records were used in ecological niche modelling experiments. We evidenced the presence of a clear phylogeographic structure within A. halleri in Central Europe. Our results suggest that the species might have not survived the last glacial maximum in the Carpathians and Sudetes and that its range during the last glacial maximum might have consisted of at least two major parts: (1) a northern refugium consisting of vast refugial areas north and northeast of the Alps and (2) a southern refugium located in the Dinaric Alps and Balkan Mts. We postulate that the Sudetes and Western Carpathians were colonised mainly by plants originating from the northern refugium, whereas populations from the Eastern Carpathians originate from southern refugium. We also discuss our results in relation to the problematic taxonomy of the species.


2022 ◽  
pp. 381-388
Author(s):  
Leszek Marks ◽  
Albertas Bitinas ◽  
Mirosław Błaszkiewicz ◽  
Andreas Börner ◽  
Rimante Guobyte ◽  
...  

2002 ◽  
Vol 26 (4) ◽  
pp. 507-532 ◽  
Author(s):  
Cornelis (Kees) Kasse

Periglacial aeolian sand sheets and dunes of the last glacial cover extensive areas of northwest and central Europe. Four sedimentary facies have been described that could be related to fluvio-aeolian and cryogenic processes, moisture content of the depositional surface and surface morphology. Factors that favoured sand-sheet and low-dune formation were the abundance of unconsolidated sediments, absence of topographic barriers, sparseness of vegetation cover and the high ratio of wind energy to sand availability. Three phases of prominent aeolian sand deposition have been distinguished from the Last Glacial Maximum to the beginning of the Holocene. Phase I (c. 28-18 ka cal B.P.) with predominant fluvio-aeolian deposition was related to permafrost conditions of the Last Glacial Maximum. Phase II (c. 18-14 cal B.P.) represents the major period of sand-sheet or coversand formation at the waning stage of the last glacial (Late Pleniglacial and early Lateglacial). Phase III (c. 13-10 cal B.P.) with more localized deposition occurred in the later part of the Younger Dryas and early Holocene. It is stressed that the aeolian phases do not strictly coincide with glacial or stadial conditions. Climatic aridity, limited vegetation cover and delayed responses of the aeolian environment to climate change determine the timing of the aeolian phases.


2015 ◽  
Author(s):  
Pawel Wasowicz ◽  
Maxime Pauwels ◽  
Andrzej Pasierbinski ◽  
Ewa M Przedpelska-Wasowicz ◽  
Alicja A. Babst-Kostecka ◽  
...  

The present study aimed to investigate phylogeographical patterns present within A. halleri in Central Europe, to propose hypotheses explaining the emergence of these patterns and to formulate hypotheses on the formation of the present day range of A. halleri in the region. 1281 accessions sampled from 52 populations within the investigated area were used in the study of genetic variation based on chloroplast DNA. Over 500 high quality species occurrence records were used in ecological niche modelling experiments. We evidenced the presence of a clear phylogeographic structure within A. halleri in Central Europe. Our results suggest that the species might have not survived the last glacial maximum in the Carpathians and Sudetes and that its range during the last glacial maximum might have consisted of at least two major parts: (1) a northern refugium consisting of vast refugial areas north and northeast of the Alps and (2) a southern refugium located in the Dinaric Alps and Balkan Mts. We postulate that the Sudetes and Western Carpathians were colonised mainly by plants originating from the northern refugium, whereas populations from the Eastern Carpathians originate from southern refugium. We also discuss our results in relation to the problematic taxonomy of the species.


Sign in / Sign up

Export Citation Format

Share Document