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Y chromosome sequences reveal a short Beringian standstill, rapid expansion, and early population structure of Native American founders

  • Thomaz Pinotti
  • , Anders Bergström
  • , Maria Geppert
  • , Matt Bawn
  • , Dominique Ohasi
  • , Wentao Shi
  • , Daniela R. Lacerda
  • , Arne Solli
  • , Jakob Norstedt
  • , Kate Reed
  • , Kim Dawtry
  • , Fabricio González-Andrade
  • , Cesar Paz-y-Miño
  • , Susana Revollo
  • , Cinthia Cuellar
  • , Marilza S. Jota
  • , José E. Santos
  • , Qasim Ayub
  • , Toomas Kivisild
  • , José R. Sandoval
  • Ricardo Fujita, Yali Xue, Lutz Roewer, Fabrício R. Santos, Chris Tyler-Smith

Research output: Contribution to journalArticlepeer-review

98 Citations (Scopus)

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, 2, 3, 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.
Original languageEnglish
Pages (from-to)149-157.e3
Number of pages9
JournalCurrent Biology
Volume29
Issue number1
DOIs
Publication statusPublished - 7 Jan 2019

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