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Y Chromosome Sequences Reveal a Short Beringian Standstill, Rapid Expansion, and early Population structure of Native American Founders.

Authors :
Pinotti T
Bergström A
Geppert M
Bawn M
Ohasi D
Shi W
Lacerda DR
Solli A
Norstedt J
Reed K
Dawtry K
González-Andrade F
Paz-Y-Miño C
Revollo S
Cuellar C
Jota MS
Santos JE Jr
Ayub Q
Kivisild T
Sandoval JR
Fujita R
Xue Y
Roewer L
Santos FR
Tyler-Smith C
Source :
Current biology : CB [Curr Biol] 2019 Jan 07; Vol. 29 (1), pp. 149-157.e3. Date of Electronic Publication: 2018 Dec 20.
Publication Year :
2019

Abstract

The Americas were the last inhabitable continents to be occupied by humans, with a growing multidisciplinary consensus for entry 15-25 thousand years ago (kya) from northeast Asia via the former Beringia land bridge [1-4]. Autosomal DNA analyses have dated the separation of Native American ancestors from the Asian gene pool to 23 kya or later [5, 6] and mtDNA analyses to ∼25 kya [7], followed by isolation ("Beringian Standstill" [8, 9]) for 2.4-9 ky and then a rapid expansion throughout the Americas. Here, we present a calibrated sequence-based analysis of 222 Native American and relevant Eurasian Y chromosomes (24 new) from haplogroups Q and C [10], with four major conclusions. First, we identify three to four independent lineages as autochthonous and likely founders: the major Q-M3 and rarer Q-CTS1780 present throughout the Americas, the very rare C3-MPB373 in South America, and possibly the C3-P39/Z30536 in North America. Second, from the divergence times and Eurasian/American distribution of lineages, we estimate a Beringian Standstill duration of 2.7 ky or 4.6 ky, according to alternative models, and entry south of the ice sheet after 19.5 kya. Third, we describe the star-like expansion of Q-M848 (within Q-M3) starting at 15 kya [11] in the Americas, followed by establishment of substantial spatial structure in South America by 12 kya. Fourth, the deep branches of the Q-CTS1780 lineage present at low frequencies throughout the Americas today [12] may reflect a separate out-of-Beringia dispersal after the melting of the glaciers at the end of the Pleistocene.<br /> (Copyright © 2018 The Authors. Published by Elsevier Ltd.. All rights reserved.)

Details

Language :
English
ISSN :
1879-0445
Volume :
29
Issue :
1
Database :
MEDLINE
Journal :
Current biology : CB
Publication Type :
Academic Journal
Accession number :
30581024
Full Text :
https://doi.org/10.1016/j.cub.2018.11.029