Preliminary Results of the Excavation in the Karain B Cave near Antalya/Turkey : The Upper Palaeolithic Assemblages and the Upper Pleistocene Climatic Development

Paléorient ◽  
1988 ◽  
Vol 14 (2) ◽  
pp. 211-222 ◽  
Author(s):  
Gerd Albrecht
1964 ◽  
Vol 30 ◽  
pp. 382-399 ◽  
Author(s):  
C. B. M. McBurney

The following is a preliminary report on the results achieved during approximately six weeks' archaeological fieldwork in north-eastern Iran in July and August 1963. The primary objective was to explore the area for traces of the local Upper Pleistocene cultural sequence, and in particular to establish if possible the date and character of the local Upper Palaeolithic. In the event no traces of Upper Palaeolithic were obtained. However, a start was made towards defining the problem by the discovery of two well-stratified deposits, the one yielding a Middle Palaeolithic (Mousterian) industry with distinctive regional affinities, and the other an early Post-glacial Mesolithic industry. Reliable samples were obtained for defining the statistical properties of both, together with carbon samples, traces of vertebrate fauna, and some other climatic data.Representative collections were lodged with the Musée Iran Bastan at Teheran; and the expedition's share is to be offered in part to the Museum of Archaeology and Ethnology in Cambridge and in part to the British Museum. The expedition was financed mainly by a grant from the British Academy, supplemented by further grants from the Crowther-Beynon Fund and the British Museum.


1951 ◽  
Vol 8 ◽  
pp. 50-51
Author(s):  
Hallam L. Movius

The Lascaux Cave, one of the most important single sites of upper Palaeolithic art ever discovered, is located near Montignac (Dordogne), 16 miles up the Vézère River from the famous town of Les Eyzies. It was found in September 1940 by two French schoolboys out rabbit hunting. Called the “Versailles of Prehistoric Man,” Lascaux ranks among the world's oldest and most remarkable art galleries. It has been completely sealed off from the outside world since late upper Pleistocene times, and it is now generally believed that the majority of the paintings are upper Perigordian (Gravettian) in date—Phase 2 in the upper Palaeolithic art sequence of western Europe. That they were produced during a time of climatic amelioration, possibly the one known as the Achen retreat, is borne out by the fact that the animals depicted belong much more to a steppe and forest type of fauna, than they do to a colder tundra group. For example, there are no mammoths and no reindeer shown, but there are many horses, a considerable quantity of cattle, bison and several ibexes.


2000 ◽  
Vol 10 (1) ◽  
pp. 123-167 ◽  
Author(s):  
Francesco d'Errico ◽  
April Nowell

This article addresses the nature of the evidence for symbolling behaviour among hominids living in the Near East during the Middle and Upper Pleistocene. Traditionally, Palaeolithic art and symbolling have been synonymous with the Upper Palaeolithic of Europe. The Berekhat Ram figurine, a piece of volcanic material from a Lower Palaeolithic site in Israel, described as purposely modified to produce human features, challenges the view of a late emergence of symbolic behaviour. The anthropogenic nature of these modifications, however, is controversial. We address this problem through an examination of volcanic material from the Berekhat Ram site and from other sources, and by experimentally reproducing the modifications observed on the figurine. We also analyze this material and the figurine itself through optical and SEM microscopy. Our conclusion is that this object was purposely modified by hominids.With comments from Ofer Bar-Yosef, Angela E. Close, João Zilhão, Steven Mithen, Thomas Wynn, and Alexander Marshack followed by a reply from the authors.


2012 ◽  
Vol 276-277 ◽  
pp. 227-241 ◽  
Author(s):  
Teodor Obada ◽  
Johannes van der Plicht ◽  
Anastasia Markova ◽  
Afanasie Prepelitsa

2013 ◽  
Vol 316 ◽  
pp. 3-13 ◽  
Author(s):  
M.-H. Moncel ◽  
D. Pleurdeau ◽  
N. Tushubramishvili ◽  
R. Yeshurun ◽  
T. Agapishvili ◽  
...  

Author(s):  
Philip R. Nigst ◽  
Timothée Libois ◽  
Paul Haesaerts ◽  
Marjolein D. Bosch ◽  
Tansy Branscombe ◽  
...  

1964 ◽  
Vol 15 (1) ◽  
pp. 187-198
Author(s):  
Hugo Gross

Abstract. The Mid-Würmian "interstadial W I/II" plays a prominent part in the literature dealing with Pleistocene archaeology since 1931. This is not the case in the geological literature. Numerous strata dated by C14 measurement and sedimentanalysis, respectively, to be of Mid-Würmian age (between ca. 50000 and 30000 B.P.) in various Upper Pleistocene sequences are for the most part interstadial; ca. ten Würmian loess sequences dated by terrace morphology contain a Mid-Würmian considerable loam zone and a very weak vounger loam zone. These facts prove the reality of an interpleniglazial Mid-Würm between the two cold peaks of Early Würm and Young Würm. The interpleniglacial climate of Middle Würm was on the average rather a cool temperate one interrupted by warmer and colder oscillations. Within the Alps and in northern Europe the expansion of the Würmian and Weichselian ice-masses was stopped, they stagnated, their fronts oscillated more or less widely. At the close of the Middle Würm, the Würmian ice overflowed the northern Alpine passes and the Weichselian ice the Baltic basin, both as far as the Young Endmoraine girdle (Young Würm). In Central Europe Middle Würm divides the Middle and Upper Palaeolithic periods. To the Middle Würm has often been ascribed heretofore the well known loam stratum within the loess of Göttweig (Lower Austria), and with this loam has been correlated the basal loam zone of the triple Stillfried A complex of fossil soils displayed by loess sections of particularly arid regions (CSSR and eastern Lower Austria). Recent studies (the latest by palynology) of this loam have proved it to be of Riß/Würm Interglacial age. Till now, this correlation has not yet been demonstrated for the loam stratum of the type locality of Göttweig (also not datable by terrace morphology!). Therefore the term "Göttweig Interstadial" must be replaced by another name: Würmian Interpleniglacial.


2021 ◽  
Author(s):  
Nefeli Kafousia ◽  
Eleni Kaberi ◽  
Grigoris Rousakis ◽  
Maria Triantaphyllou ◽  
Eleni Koutsopoulou ◽  
...  

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