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Dorset and Thule divergence from east Central Asian roots
Author(s) -
Shields Edward D.,
Jones Gregory
Publication year - 1998
Publication title -
american journal of physical anthropology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.146
H-Index - 119
eISSN - 1096-8644
pISSN - 0002-9483
DOI - 10.1002/(sici)1096-8644(199806)106:2<207::aid-ajpa7>3.0.co;2-m
Subject(s) - beringia , arctic , geography , population , east asia , immigration , land bridge , archaeology , physical geography , ecology , pleistocene , demography , biology , china , biological dispersal , sociology
The history of the immigration of East Asians to America during the last glacial period remains controversial. In an attempt to add critical data to this problem, a large sample of whole teeth derived from Southeast Asian, Mongolian, Thule, Western Inuit, and pre‐Inca (Huari) people was quantified (N = 4,507 teeth from 495 individuals; ∼30 variables per tooth). Multivariate analysis helped establish that all Native Americans were likely derived from one ancient, extinct population that resided in the region of Mongolia (east Central Asia), and that Mongolians and Southeast Asians are two independent groups. A controversial and enigmatic Central Canadian Arctic “Thule culture Inuit” group on Southampton Island that survived until 1902 was identified as a relic, mainly Paleoeskimo Dorset community. Surprisingly, there was little, or no, indication of Dorset‐to‐Thule gene flow. Cumulatively, the data suggest that a small population of Paleoindian founders remained resident in Beringia, may have blocked further immigration, and were the antecedents to the Thule/Inuit. With the confluence of the Arctic and Pacific oceans at the breakup of Beringia, the resulting increased availability of marine animal food sources allowed this population to increase in size and expand throughout the eastern Arctic. Am J Phys Anthropol 106:207–218, 1998. © 1998 Wiley‐Liss, Inc.