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281:. The earliest layer, Layer 3, is OSL dated to around 45,000 to 30,000 BP. While artefacts were found outside of Layer 3, the archaeologists who worked the site believe that all of the artefacts come from the assemblage associated with Layer 3. Paleo-environmental evidence suggests that the local climate was milder during the time of Layer 3 when compared against the present.
298:, through the use of prismatic cores. Archaeologists believe that Nwya Devu, with access to a good source of raw materials nearby, was likely the site of a lithic tool-making workshop, with a primary focus on creating long knives and scrapers that could be
302:. Some of the excavated blades were over 20 cm (8 in) in length. The lithic assemblage at Nwya Devu appears to be unique and not obviously related to any other sites in East Asia. It shows some similarities to sites from the Early
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3,683 lithic artefacts were excavated from the site. The lithic assemblage at Nwya Devu consists primarily of blade cores, flake cores, blades, flakes, chunks, and tools. All of the lithic artefacts at Newa Devu were sourced from black
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Zhang, X. L.; Ha, B. B.; Wang, S. J.; Chen, Z. J.; Ge, J. Y.; Long, H.; He, W.; Da, W.; Nian, X. M.; Yi, M. J.; Zhou, X. Y.; Zhang, P. Q.; Jin, Y. S.; Bar-Yosef, O.; Olsen, J. W.; Gao, X. (2018-11-29).
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that was locally derived, from nearby Nwya Devu Hill, which lies around 800 m (2,625 ft) east of the site. Blades found at the site were made using a non-
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ranges from around 12,700 to 12,400 BP, which shows concurrence with the OSL dating. Layer 2 is OSL dated from around 25,000 to 18,000 BP and corresponds with the
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region of Tibet. At around 4,600 m (15,092 ft) above sea level, Nwya Devu is the highest known archaeological site from the
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and provides evidence for one of the earliest known presences of humans at a high-altitude site, at around 40,000-30,000
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502:"The earliest human occupation of the high-altitude Tibetan Plateau 40 thousand to 30 thousand years ago"
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layers at the site and excavated around 170 cm (6 ft) worth of deposits in depth. Layer 1 is
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512:(6418). American Association for the Advancement of Science (AAAS): 1049–1051.
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462:(6418). American Association for the Advancement of Science (AAAS): 992–993.
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performed by the
Tibetan Cultural Relics Conservation Institute and the
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273:. Mollusc shells taken from the lowest part of Layer 1 yielded
454:(2018-11-29). "The last of Asia conquered by Homo sapiens".
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of Co Ngoin, a nearby freshwater lake to the site's north.
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Institute of
Vertebrate Paleontology and Paleoanthropology
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241:The site was discovered in 2013 during
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243:systematic archaeological surveying
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261:Archaeologists identified three
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569:2013 archaeological discoveries
249:. Nwya Devu lies on the former
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554:Archaeological sites in Tibet
153:4,600 m (15,092 ft)
376:, p. 4 (Supplementary).
344:, p. 3 (Supplementary).
269:from around 13,000 to 4,000
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564:Paleolithic sites in China
559:High-altitude archaeology
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422:Zhang & Dennell 2018
519:10.1126/science.aat8824
468:10.1126/science.aav6863
221:located in the eastern
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171:Excavation dates
279:Last Glacial Maximum
296:Levallois technique
251:lacrustrine terrace
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434:Zhang et al. 2018
401:Zhang et al. 2018
389:Zhang et al. 2018
374:Zhang et al. 2018
359:Zhang et al. 2018
342:Zhang et al. 2018
304:Upper Paleolithic
215:Nya-de'u gNa-shul
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134:31.467°N 88.800°E
81:Show map of China
78:Nwya Devu (China)
53:Show map of Tibet
50:Location in Tibet
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219:Tibetan Plateau
207:ཉ་དེའུ་གནའ་ཤུལ།
174:2013, 2016-2018
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306:in Siberia (
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227:Paleolithic
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113:Coordinates
548:Categories
318:References
237:Background
166:Site notes
528:0036-8075
476:0036-8075
323:Citations
312:Tolbor-21
285:Artefacts
267:OSL dated
223:Changtang
181:Nwya Devu
107:Changtang
17:Nwya Devu
536:30498126
492:54169275
484:30498110
308:Kara Bom
275:AMS date
150:Altitude
105:eastern
91:Location
506:Science
456:Science
203:Tibetan
185:Chinese
125:88°48′E
122:31°28′N
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300:hafted
198:Ní'ādǐ
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193:pinyin
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102:Region
574:Nagqu
488:S2CID
292:slate
211:Wylie
532:PMID
524:ISSN
480:PMID
472:ISSN
158:Type
514:doi
510:362
464:doi
460:362
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189:尼阿底
23:尼阿底
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408:^
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