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Animals and humans in the European Russian Arctic towards the end of the last Ice Age and during the mid-Holocene time
被引:5
|作者:
Hufthammer, Anne Karin
[1
]
Svendsen, John Inge
[2
,3
]
Pavlov, Pavel
[4
]
机构:
[1] Univ Bergen, Univ Museum, Dept Nat Hist, Allegt 41, N-5007 Bergen, Norway
[2] Univ Bergen, Dept Earth Sci, Allegaten 41, N-5007 Bergen, Norway
[3] Bjerknes Ctr Climate Res, Jahnebakken 5, N-5007 Bergen, Norway
[4] Russian Acad Sci, Komi Sci Ctr, Inst Language Literature & Hist, Ural Div, Kommunist Skaya St 26, Syktyvkar 167000, Komi Republic, Russia
来源:
关键词:
LATE PLEISTOCENE;
EXTINCTION;
SHEETS;
D O I:
10.1111/bor.12343
中图分类号:
P9 [自然地理学];
学科分类号:
0705 ;
070501 ;
摘要:
Here, we present and discuss results from geo-archaeological and palaeo-zoological investigations at the Palaeolithic site Pymva Shor, in the Russian Arctic. As many as 3324 vertebrate fauna remains were recovered during two excavations. This includes bones of mammals, birds and fish. Radiocarbon dates were obtained from 26 specimens. The results show ages in the range 30-3cal. ka BP. Hare and reindeer are the best represented amongst the identified mammalian species, whilst ptarmigan and various wader species dominate the avian bones. The Pleistocene assemblage includes herbivorous herd animals such as horse, bison and musk ox. These species are typical of the treeless tundra-steppe landscape that existed during the Lateglacial. Of particular interest is a cave lion specimen that has been radiocarbon dated to approximately 15.5cal. ka BP. According to our knowledge, this is one of the latest dated examples of this species in Eurasia. The faunal composition in the Holocene assemblage is strikingly different and includes distinct forest taxa such as beaver and pine marten. The avifauna also supports a forested environment with the presence of black grouse. A few stone artefacts were found within the strata, and have been radiocarbon dated to 16-15cal. ka BP, suggesting that there were humans in the Pymva Shore area at that time. We identified impact notches and cut marks on some radiocarbon-dated reindeer and bison bones, showing that humans were present twice during the Younger Dryas period. A fourth occupation phase is identified during the mid-Holocene (6-5cal. ka BP). We also investigated river terraces and obtained a series of luminescence dates. These have been used to reconstruct the geological history and the relationship to the find-bearing strata.
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页码:387 / 406
页数:20
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