Red Deer Hunting in the Upper Paleolithic of South-West France: A Study in Seasonality

Author(s):  
Anne Pike-Tay
2012 ◽  
Vol 58 (3) ◽  
pp. 597-607 ◽  
Author(s):  
Jon Olaf Olaussen ◽  
Atle Mysterud
Keyword(s):  
Red Deer ◽  

1991 ◽  
Vol 57 (2) ◽  
pp. 1-8 ◽  
Author(s):  
S. J. Mithen ◽  
B. Finlayson

Knowing the source of the red deer in the Mesolithic shell middens on Oronsay is necessary for a reconstruction of the early post-glacial settlement patterns in the southern Hebrides. If they came from Colonsay, then it is conceivable that the combined resources of Colonsay and Oronsay could have supported a population on these small islands for extended periods of time — as the seasonally data from the middens suggests when taken at face value. If there were no red deer on Colonsay, it is more likely that the Oronsay middens result from many short intermittent visits to the island. Since early post-glacial faunal assemblages are unknown from Colonsay, and unlikely to be found, this paper discusses the relevance of lithic assemblages for inferring the hunting of red deer. It describes recent fieldwork on Colonsay and the discovery of the first Mesolithic sites, notably that of Staosnaig. It concludes that the microlithic elements within the assemblages are too small to indicate red deer hunting. If Mesolithic foragers went to Colonsay to hunt red deer, they probably left rather quickly and empty-handed.


2020 ◽  
Vol 29 ◽  
pp. 102049
Author(s):  
Ola Magnell ◽  
Sara Gummesson ◽  
Fredrik Molin ◽  
Peter Zetterlund ◽  
Jan Storå

2020 ◽  
Vol 37 (4) ◽  
pp. 107-125
Author(s):  
V. P. Chabai ◽  
D. V. Stupak ◽  
A. P. Veselsky ◽  
D. V. Dudnyk

The Upper Paleolithic site Barmaky, 2nd cultural layer from Volyhnia-Lublin upland is the most western manifestation of Epigravettian of the Mid Dnieper basin. During several field campaigns the 147 m2 of cultural deposits with three pits and one chalk / marl concentration were studied (fig. 1). The silty-loess deposits of Barmaky, 2 accumulated about 19 kyr cal BP (table 1) under the permafrost conditions. The fauna assemblage is represented by: mammoths, bison, reindeer, red deer, horse, bear, wolf, wolverine, polar fox, fox and hare. More than 100 thousand artifacts were recovered during the last two field campaigns. In essential account (without chips, chunks, unidentifiable debitage), the artifacts assemblage is represented by: cores and pre-cores — 0.87 %; flakes — 45.23; blades — 17.34; bladelets — 14.27; micro-blades — 7.34; burin spalls — 8.08; tools — 6.79 % (table 2). The reduction sequences are based on the flaking of uni-, bidirectional sub-cylindrical and narrow flaking surface unidirectional cores for blades and bladelets (table 3; fig. 2). There is no evidence of micro-blade technology implication. The structure of tool-kit is characterized by the dominance of burins — about 50 %; microliths — 25 %; and truncated pieces — about 18 % (table 4). The rest of tool classes are represented by a few percentages each. Among them are the end-scrapers on blades with truncated base (fig. 3). The most part of burins are represented by pieces made on obliquely truncated blades (table 5; fig. 4). Also, the obliquely truncated blades dominate the truncated pieces assemblage (table 6; fig. 5). The most representative type of microliths is the micro-points with abruptly retouched straight back and obliquely retouched base (table 7; fig. 6). The points, pendants, bracelet fragment made on tusk and perforated fossil marine shells from local chalk deposits are available. The composition of microliths, burins and end-scrapers in Barmaky, 2 tool-kit is characteristic to the cultural layers beyond the dwelling structures on such base-camps as Mezhyrich (fig. 7). Also, the presences of pits and fauna composition are close to what expected from Epigravettian base-camps. The artifacts assemblage of Barmaky, 2 belongs to the Mizyn industry. Also, Barmaky, 2 is the earliest manifestation of Epigravettian in the Mid Dnieper basin.


Author(s):  
D. G. Malikov ◽  
◽  
V. V. Sizova ◽  
N. E. Berdnikova ◽  
I. M. Berdnikov ◽  
...  

The paper presents the detailed results of the archaeozoological study of the large mammals from the Shchapova 2 Upper Paleolithic site located in Irkutsk. Excavations in 2019 revealed four conditionally defined horizons with archaeological and faunal material; within the studied area subaerial sediments of deluvial origin were uncovered. Layers 3 and 4 were attributed to the Karginian period (MIS 3), layer 2 to the Early Sartanian period (MIS 2), layer 1 to the Holocene (MIS 1). The largest number of bone remains was obtained from layer 4. Altogether we recognized ten taxa: Spermophilus sp., Panthera spelaea, Mammuthus primigenius, Equus sp., Coelodonta antiquitatis, Cervus elaphus, Megaloceros giganteus, Alces alces, Rangifer tarandus, Bison priscus. The species composition of Shchapova 2 site is characteristic of the Late Pleistocene of region with a predominance of horse and steppe bison, diversity of cervids and presence of woolly mammoth and rhinoceros. Most of the bones have only slightly weathered surfaces. It indicates that the bulk of the bone remains were only exposed for a short time on the surface or in the soil prior to deeper burial. The analysis of the faunal material suggests that the accumulation of bones from layers 3 and 4 took place in the hunter camp. The subsistence strategy was based primarily on two game animals: horse and steppe bison. Horses and steppe bison were killed in the immediate vicinity of the site. Sometimes red deer and moose were hunted from remote areas. Large parts of horse and steppe bison carcasses were transported from a kill and initial butchering site to a residential and consumption site. Most likely the complete and unprocessed reindeer carcasses were brought to the camp. Reindeer skull fragments found in the layer 4 indicate that the Shchapova 2 site most likely was seasonally occupied during late autumn or winter. However, due to the small amount of bones these data are preliminary. The fauna from the Upper Paleolithic site Shchapova 2 is indicative of tundra-steppe. The presence of red deer and moose remains suggests the forest in the vicinity of the site, probably represented by floodplain forests.


Radiocarbon ◽  
2007 ◽  
Vol 49 (3) ◽  
pp. 1205-1214 ◽  
Author(s):  
Lawrence Guy Straus ◽  
Manuel R González Morales

This article expands the date list from the Stone Age cave site of El Mirón in the Cantabrian Cordillera of northern Spain to a total of 62 radiocarbon determinations, one of the longest series from a single prehistoric site in Iberia. All the assays (accelerator mass spectrometry [AMS] and conventional, run on charcoal and bone collagen) were done by a single laboratory (Geochron, GX). The 11 new dates confirm 1) the late spread of Neolithic economy and technology into the Atlantic environment of Cantabrian Spain by about 4500 cal BC; 2) the horizontally extensive, but not intensive, use of the whole cave vestibule by Upper Magdalenian foragers about 12,000–14,000 cal BC; 3) extensive and very intensive, repeated occupations of the cave during the Middle and Lower Cantabrian Magdalenian about 14,200–17,000 cal BC; and 4) a long, gradual technological transition from the Solutrean to the Archaic Magdalenian between about 20,000–17,000 cal BC. El Mirón joins a list of culturally very rich, frequently occupied, Lower Magdalenian residential hub sites—most of the rest of which (including Altamira) are located in the coastal lowlands of Cantabria—which have yielded distinctive red deer scapulae that are decorated with striated engraved images of game animals (mainly red deer hinds), now most precisely dated at El Mirón between 16,200–17,200 cal BC.


Author(s):  
Francisco Rosa Correia ◽  
Sofia Luís ◽  
Pedro Valente Fernandes ◽  
Maria João Valente ◽  
António Faustino Carvalho

The Pena d’Água Rock-shelter (Torres Novas, Portugal) was excavated in 1992–2000, revealing a long stratigraphic and cultural sequence including Middle Neolithic occupations. A preliminary study on its fauna was published by Valente (1998) based on the 1992–1994 material, but the 1997–2000 campaigns remained unstudied. The aim of this study is to present the full fauna analysis of the layer Db, dated from the earlier phases of that period. Like other assemblages from the same time frame in the area, the fauna collection understudy is small. Its bones showed several surface and chemical alterations due to sediment pressure, exposure to fire and water percolation. Regarding the taxonomical abundances, most remains were classified as rabbit (Oryctolagus cuniculus) and sheep and/or goat (Ovis aries/Capra hircus). A few specimens of cervid, fox (Vulpes vulpes) and bird were also identified. The other fauna assemblages from the region show either the prevalence of the caprine component (as in Pena d’Água) or a higher abundance of cervids. This trend may reflect a specialized animal exploitation and we propose that the Middle Neolithic human communities in the Limestone Massif had a subsistence strategy based on caprine exploration, supplemented by some cervid (red deer) hunting. These hunter-herders groups were probably highly mobile and may have practiced some kind of transhumance (or itinerant pastoralism), for which the details are still unknown.


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