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Revising the archaeological record of the Upper Pleistocene Arctic Siberia: Human dispersal and adaptations in MIS 3 and 2
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Woolly mammoth was especially common and survived on island remnants of both the Great Arctic Plain and southern Bering Land Bridge into the mid Holocene.
“Woolly mammoth, which enjoyed a wide dietary niche, was especially common and survived on island remnants of both the GAP and southern BLB into the mid Holocene [4,31,36,39].”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
The earliest well-dated archaeological sites and human remains are represented by a cluster of open-air sites near the mouth of the Yana River.
“The earliest well-dated archaeological sites and human remains are represented by a cluster of open-air sites near the mouth of the Yana River that have yielded thousands of stone and non-stone artefacts, and a large quantity of associated faunal remains, including steppe bison, reindeer, hare and mammoth.”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
The immediate ancestors of ANE are found in the Arctic and western Beringia as early as 33 ka.
“The ANE population is present in southern Siberia during middle and late Upper Palaeolithic times at Mal'ta (24 ka) and Afontova Gora (17 ka), and their immediate ancestors (see below) are found in the Arctic and western Beringia as early as 33 ka [39,61,78].”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
A second regional population with roots in western Eurasia (Ancient North Eurasians (ANE)) expanded into Northeast Asia before 30 ka.
“A second regional population with roots in western Eurasia (Ancient North Eurasians (ANE)) expanded into Northeast Asia before 30 ka and contributed to the East Asian genome and—both indirectly and directly—to the Native American genome.”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
Calibration of a large sample of radiocarbon dates with the IntCal20 curve shows a concentration of ages around 34.5-31.5 ka, coinciding with two brief interstadials (GI 6 and GI 5).
“Calibration of a large sample of radiocarbon dates with the IntCal20 curve shows a concentration of ages around 34.5–31.5 ka, coinciding with two brief interstadials (Greenland Interstadial 6 [GI 6] and GI 5) [21,39,52].”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
ANE contributed to the East Asian genome and-both indirectly and directly-to the Native American genome.
“A second regional population with roots in western Eurasia (Ancient North Eurasians (ANE)) expanded into Northeast Asia before 30 ka and contributed to the East Asian genome and—both indirectly and directly—to the Native American genome.”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
The Yana River sites have yielded thousands of stone and non-stone artefacts, and a large quantity of associated faunal remains, including steppe bison, reindeer, hare and mammoth.
“The earliest well-dated archaeological sites and human remains are represented by a cluster of open-air sites near the mouth of the Yana River that have yielded thousands of stone and non-stone artefacts, and a large quantity of associated faunal remains, including steppe bison, reindeer, hare and mammoth.”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
The ANE population is present in southern Siberia during middle and late Upper Palaeolithic times at Mal'ta (24 ka) and Afontova Gora (17 ka).
“The ANE population is present in southern Siberia during middle and late Upper Palaeolithic times at Mal'ta (24 ka) and Afontova Gora (17 ka), and their immediate ancestors (see below) are found in the Arctic and western Beringia as early as 33 ka [39,61,78].”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
Evidence for a human presence in Beringia during the LGM is limited in comparison to the preceding interval.
“Evidence for a human presence in Beringia during the LGM is limited in comparison to the preceding interval [39,52].”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
Beringia itself may have been abandoned or have witnessed a severe decline in the human population after the GI 5 interstadial, which was followed by an episode of extreme cold climate (HE 3) at ca 30 ka.
“Beringia itself may have been abandoned or have witnessed a severe decline in the human population after the GI 5 interstadial, which was followed by an episode of extreme cold climate (HE 3) at ca 30 ka [39].”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
Most of the region between the north Eurasian and North American ice sheets was occupied by a dry plain that supported a relatively uniform steppe-tundra biome (the GAP) at least with respect to the fauna.
“Most of this region was occupied by a dry plain that supported a relatively uniform steppe-tundra biome (i.e. the GAP) at least with respect to the fauna, as described previously [36,37,39].”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
A credible archaeological proxy for APS (microblades) dates to approximately 15 ka.
“We are pursuing field research on both sides of the Bering Strait, including western arctic Beringia, which yields evidence for the presence of the west Eurasian lineage before the LGM, but has yet to produce definitive evidence for the East Asian lineage greater than 10 ka, although a credible archaeological proxy for APS (microblades) dates to approximately 15 ka [39,52]).”
From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [39]
Citations
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Self-citation
Metadata
- Authors
- Pitulko, V., Pavlova, E., & Nikolskiy, P.
- Venue
- Quaternary Science Reviews
- Publisher
- Elsevier BV
- Published
- 2017-06
- Volume
- 165
- Pages
- 127-148
- ISSN
- 0277-3791
- Cited by
- 77
- References
- 3
- Language
- en
- Funders
- Russian Academy of Sciences (1.11)
- Russian Foundation for Basic Research (N 13-06-12044)
- Russian Science Foundation (N 16-18-10265)
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