2017
DOI: 10.1016/j.quaint.2016.10.013
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New evidence for Paleolithic human behavior in Mongolia: The Kharganyn Gol 5 site

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Cited by 26 publications
(7 citation statements)
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“…21-18 ka, north China was a cold, arid desert and steppe, with permafrost extensive above 1000-1300 m (1000m lower than today), and annual temperatures 8-12 o C. colder than now (Cui et al, 2004). Mongolia may also have been largely depopulated as there is no record of occupation in the Tolbor or Kharganyn Gol valleys between 30,000 and 19,000 years ago (Khatsenovich et al, 2017). In southern Siberia, regions such as Transbaikalia were either abandoned or made archaeologically invisible for at least 2-3 kyr between about 24.8 ka and 22.7 ka (Graf and Buvit, 2017 Ma'anshan in the Nihewan Basin is dated at 18 ka but few details are available (Yang et al 2018).…”
Section: Was North China Depopulated In the Lgm?mentioning
confidence: 99%
“…21-18 ka, north China was a cold, arid desert and steppe, with permafrost extensive above 1000-1300 m (1000m lower than today), and annual temperatures 8-12 o C. colder than now (Cui et al, 2004). Mongolia may also have been largely depopulated as there is no record of occupation in the Tolbor or Kharganyn Gol valleys between 30,000 and 19,000 years ago (Khatsenovich et al, 2017). In southern Siberia, regions such as Transbaikalia were either abandoned or made archaeologically invisible for at least 2-3 kyr between about 24.8 ka and 22.7 ka (Graf and Buvit, 2017 Ma'anshan in the Nihewan Basin is dated at 18 ka but few details are available (Yang et al 2018).…”
Section: Was North China Depopulated In the Lgm?mentioning
confidence: 99%
“…Assemblages with these characteristics are distributed broadly across Eurasia, from the eastern Mediterranean to northeast Asia. In northeast Asia, IUP assemblages have been documented in Siberia, Mongolia, as well as northern China, with particular "hot spots" in the areas surrounding Baikal lake, in northern Mongolia, and in the Siberian Altai [16][17][18][19][20][21]. Our main aim here is to examine the intra-assemblage variation in the collection from the 1963 excavation at Shuidonggou locality 1 (SDG 1) in northern China, in an effort to situate the site and assemblage within the range of IUP variability in northeast Asia.…”
Section: Introductionmentioning
confidence: 99%
“…These Trans-Baikal IUP sites are Varvina Gora, Kandabaevo, Tolbaga, with the earliest material dating to ~41ka, 43ka and 34ka respectively [91, 92]. In addition, the sites 500km to the south in the Selenge River valley, which feeds into Lake Baikal, of Tolbor 4, Orkhon 1 & 7, and Kharganyn Gol 5 have similarly early dates of 41ka, 44ka and 48ka, respectively [93–96]. In proximity to Shuidonggou, the path also passes the surface IUP site of Yushuwan [97, 98].…”
Section: Discussionmentioning
confidence: 99%