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Am. J. Hum. Genet.,
64:619-628, 1999
Fabrício R. Santos,1,2 Arpita Pandya,1 Chris Tyler-Smith,1 Sérgio D. J. Pena,2 Moses Schanfield,3 William R. Leonard,4 Ludmila Osipova,5 Michael H. Crawford,6 and R. John Mitchell7
1Department of Biochemistry, Oxford
University, Oxford; 2Departamento de Bioquímica, Universidade Federal
de Minas Gerais, Belo Horizonte, Minas Gerais, Brazil; 3Analytical
Genetic Testing Center, Inc., Denver; 4Department of Anthropology,
University of Florida, Miami; 5Institute of Cytology and Genetics,
Siberian Branch of the Russian Academy of Sciences, Novosibirsk, Russia;
6Department of Anthropology, University of Kansas, Lawrence; and
7School of Genetics and Human Variation, La Trobe University,
Bundoora, Australia
Summary
Y chromosomal DNA polymorphisms were used to investigate Pleistocene male
migrations to the American continent. In a worldwide sample of 306 men, we
obtained 32 haplotypes constructed with the variation found in 30 distinct
polymorphic sites. The major Y haplotype present in most Native Americans was
traced back to recent ancestors common with Siberians, namely, the Kets and
Altaians from the Yenissey River Basin and Altai Mountains, respectively. Going
further back, the next common ancestor gave rise also to Caucasoid Y
chromosomes, probably from the central Eurasian region. This study, therefore,
suggests a predominantly central Siberian origin for Native American paternal
lineages for those who could have migrated to the Americas during the Upper
Pleistocene.
Address for correspondence and reprints:
Dr. Fabrício R. Santos, Departamento de Biologia Geral, ICB/UFMG, Caixa Postal
486, 31.270-910 Belo Horizonte, MG, Brazil. E-mail: fsantos@mono.icb.ufmg.br
Introduction
The pre-Columbian settlers of the New World,
who gave rise to the present-day Native Americans, are commonly believed to have
come from Siberia, through the Bering land bridge, in the period 30,000-12,000
years before present (ybp). These conclusions are based on cultural,
morphological, and genetic similarities between populations of the New World and
Siberia (for a review, see Crawford 1998). Although affinities between Asians and Native Americans
have been acknowledged for a long time, no particular population in Siberia,
except for some Asian Eskimos and their relatives, has been pointed out as
directly descended from ancient groups related to the American founder
populations (Cavalli-Sforza et al. 1994). Morphological studies have suggested a place of origin for
Native Americans along the Amur River region (Crawford 1998),
and, more recently, the investigation of mtDNA lineages (Kolman et al. 1996; Merriwether et al. 1996), as well as of retrovirus infections (Neel et al. 1994), has suggested that Mongolia, instead of Siberia, is the
source of populations that share the more recent ancestors with the founding
population of the Americas.
Siberia is an inhospitable place for human
settlements, but the first hominids may have arrived as early as 260,000 ybp
(Waters et al. 1997). The population density has never been high, and it is
still vastly uninhabited. These conditions favor a high degree of population
isolation and genetic drift, which could have played an important role since the
first migrants left for the Americas. Furthermore, the number of indigenous
Siberian populations has been decreasing since the beginning of the Russian
territorial expansion in the seventeenth century (Forsyth 1996). Many populations have become extinct, and others--such as
the Kets, who are inhabitants of the Yenissey River Basin--are now reduced to
<1,000 individuals and are speakers of an isolated language unrelated to any
other extant languages (Grimes 1996).
The three-migrations theory (Greenberg et al.
1986) postulates that each of the major Native American
groups--namely, the Amerindians, Na-Denes, and Eskimo-Aleuts--came to the
Americas in three distinct migratory waves from Siberia, during the period
12,000-6,000 ybp. This theory received support a posteriori from the analysis of
mtDNA (Torroni et al. 1993) and several autosomal markers (Cavalli-Sforza et al. 1994), but
these data extended the entrance time of these groups to the Americas to
34,000-6,000 ybp. This model has been criticized mainly for the claims of the
existence of a genetic homogeneity in present-day Amerindians (Schanfield 1992), who are considered to be the descendants of the first
migrants. In addition, further mtDNA analyses have been shown to be consistent
with a single migration into the Americas (Merriwether et al. 1995) and with a single migration with further population
reexpansion (Forster et al. 1996; Bonnato and Salzano 1997). Some anthropometric studies have also revealed the
existence of skeletons not typical of Mongoloids among the oldest hominids in
the Americas, suggesting an earlier, non-Mongoloid migration (Neves and
Pucciarelli 1991; Lahr 1995).
Recent studies of the human Y chromosome have
shown a major haplotype present in >90% of nonadmixed southern and central
Amerindians (Pena et al. 1995; Santos et al. 1995a), indicating a genetic homogeneity and a pronounced
founder effect in the formation of these populations. Later, some northern
Amerindians and also Na-Dene and Eskimo speakers were studied, and, despite
their higher level of admixture (Crawford 1998),
these populations also displayed the same major haplotype, although not in such
a high frequency (Santos et al. 1996b; Underhill et al. 1996). This major Native American haplotype initially was
identified as the combination of alphoid heteroduplex (h) type II and the
microsatellite DYS19 A allele (Pena et al. 1995;
Santos et al. 1995a),
and it subsequently was shown to also be defined by a CT transition in the
DYS199 locus (Underhill et al. 1996).
The study of several Siberian populations (Karafet et al. 1997; Lell et al. 1997) has identified the presence of the DYS199 T allele
only in Asian Eskimos and related tribes from the Beringia region. The presence
of the T allele in far northeastern Siberia was explained to be the result of
either a back migration of Native American populations bearing the DYS199
T allele or simply a split of populations inhabiting Beringia, after the
glaciation period. This suggests that the DYS199 T allele is a useful
marker for the identification of Y haplotypes originating after the first
migration to the Americas or Beringia but that more-informative (ancient)
markers are needed to trace the origin of these Y chromosomes within Asia.
In this study, the Y chromosomes of five
linguistically distinct Siberian populations, as well as of those of Native
Americans, Europeans, Indians, Mongolians, central East Asians, and Africans,
were analyzed with a set of seven polymorphic systems identifying 30 variable
loci in the nonrecombining portion of the Y chromosome. The worldwide
distribution of haplotypes and their evolutionary network shows the recent
common ancestry of Caucasoid and Native American Y chromosomes, as well as the
identification of intermediate Y haplotypes in Siberian populations from the
Altai Mountains and the Yenissey River Basin, namely, the Altaians and Kets,
respectively.
Material and Methods
DNA Samples
Most of the 306 male samples were obtained as
DNA or were extracted from plugs prepared for pulsed-field gel electrophoresis
(Mathias et al. 1994). Samples from Europeans (most were British), Indians (India
and Sri Lanka), Africans (Kenyans, Pygmies, and San), central East Asians
(Chinese and Japanese), Mongolians (Khalkhs), and Siberians (Buryats, Yakuts,
Evenkis, Altaians, and Kets) were subsets of those described elsewhere (Mathias
et al. 1994;
Zerjal et al. 1997). Ten samples, from south and central Amerindians and a
Na-Dene, were purchased from the National Institute of General Medical Science,
and an additional 10 Native American samples (not Aleut-Eskimos) came from
paternity tests in North America.
DNA Polymorphisms
The variants of 6-kb and 4.1-kb alphoid units
were first identified by hybridization with the pYl probe (Mathias et al. 1994) and
subsequently were checked by HindIII digestion of h PCR products (Santos
et al. 1995b), to avoid confusion because of the comigration of
4.1-kb bands on the gel from both the 6-kb and the 4.1-kb units. For most cases,
92R7 typing was performed by hybridization (Mathias et al. 1994),
but PCR was also used to type some individuals (M. Hurles, F. R. Santos, A.
Pandya, and C. Tyler-Smith, unpublished data).
Additional systems--namely, DYS199,
SRY-1532, Tat, the Y Alu polymorphism (YAP), and h--were scored,
after PCR, in a MJR PTC200 thermocycler, with a 12.5-l reaction volume, 1 M of
each primer, 200 M dNTPs, 1.5 mM MgCl2, 1 U Taq (Bioline) per
tube with 1× KCl buffer (Bioline), and other changes as follows. The locus
DYS199 (Underhill et al. 1996) was
amplified for 30 cycles at 94°C for 20 s, 61°C for 20 s, and 72°C for 30 s, with
a modified reverse primer, 5'-AGG TAC CAG CTC TTC CCA ATT-3', containing
a GC base change (underlined) that creates an artificial MfeI restriction
site when the DYS199 C allele is present. This PCR/RFLP protocol using
the MfeI enzyme (New England Biolabs), resolved in native polyacrylamide
gels stained by silver (Santos et al. 1996a), allowed us to determine without doubt the allele
state at this site that had been detected previously by an
allele-specific-primer protocol (Underhill et al. 1996).
The locus SRY-1532, with an AG mutation (Whitfield et al. 1995), was amplified for 30 cycles at 94°C for 20 s, 60°C for 20
s, and 72°C for 30 s, with the primers SRY1 (5'-TCC TTA GCA ACC ATT AAT
CTG G-3') and SRY2 (5'-AAA TAG CAA AAA ATG ACA CAA GGC-3') and 0.5 U
Taq per tube. The G allele was detected by the presence of the
DraIII (Boehringer) restriction site on a 1.5% agarose gel in
Tris/acetate/EDTA 0.5×. The YAP system was scored, as described elsewhere
(Hammer and Horai 1995), in the PCR conditions described above but with PROMEGA
enzyme and buffer. The Tat polymorphism (Zerjal et al. 1997) and
the h system (Santos et al. 1995b,
1996a)
were detected and classified as described previously. Most individuals were also
typed for the tetranucleotide microsatellite DYS19 (Santos et al. 1996a).
Population Genetics of Y
Chromosomes
Haplotype frequencies and gene diversities (Nei
1987) were calculated for all populations. A parsimonious network
was constructed either manually or by median network analysis (Bandelt et al. 1995), with the knowledge of the molecular mechanisms of the
h-system mutations (Santos et al. 1996a)
and other loci (Mathias et al. 1994;
Hammer and Horai 1995;
Jobling and Tyler-Smith 1995; Whitfield et al. 1995;
Underhill et al. 1996). On
the basis of this network, a haplotype distance matrix was constructed by use of
the number of mutation steps between each pair of Y haplotypes. The hierarchic
distribution of Y chromosome diversity, measured as the variance components
among individuals, populations, and geographic groups, was computed by use of
analysis of molecular variance (AMOVA) software. Genetic distances between
populations were calculated, and their significance was tested by use of a
permutation procedure (Excoffier et al. 1992). Population pairwise FST's and other
genetic distances (Excoffier et al. 1992) were
used to draw neighbor-joining and UPGMA trees, with the PHYLIP package
(Felsenstein 1993), that were visualized by use of TreeView software (Page 1996).
Results
Worldwide Distribution of Y
Haplotypes
This study comprised a sample of 306 men from
populations encompassing distinct linguistic affiliations. They are
representatives of different geographic areas expected to be informative for the
Americas settlement study. The analysis with seven polymorphic systems revealed
the variation at 30 distinct loci in the nonrecombining portion of the Y
chromosome, which allowed the discrimination of 32 haplotypes among 306 men. The
major Amerindian haplotype (Pena et al. 1995;
Underhill et al. 1996) is
described here as haplotype 31, which is associated with several markers, such
as h type II, the alphoid 4.1-kb units, the DYS199 T allele, the 92R7
HindIII- allele, and also the DYS19 microsatellite A allele (data
not shown), as well as with the ancestral states of the polymorphisms YAP and
Tat. Haplotype 10, differing from haplotype 31 only by the mutation at
DYS199, was very frequent (30%) in our Native American sample and was
found exclusively among the North American Indians; in addition, it was also
observed in a Mongolian and four Indians. Haplotype 20, which is similar to
haplotypes 10 and 31, was seen in a single North American Indian and in some
populations from the central region of Siberia. It was particularly frequent in
a sample of the rapidly disappearing Ket population (70%) and also was found in
some Altaians (17.4%) and a single Mongolian. Haplotype 23, which is very
different from haplotypes 31, 10, and 20, was seen in a single Na-Dene and could
be a more recent migrant haplotype from Asia, since it is most frequent in
Mongolia (42%) and also is seen in many Siberians. Haplotype 1, also similar to
haplotype 10 and the most frequent in Europe (53%), is also present in India
(14.5%) and was found in 20% of the Native Americans, exclusively in the samples
collected for paternity tests in North America, but it is absent from Siberia or
central East Asia. European ancestry was confirmed for at least one of these
Native American samples with haplotype 1 in the paternity-test report.
Therefore, the presence of haplotype 1 in North American Indians can be
explained as a result of recent admixture with Europeans, whereas haplotypes 10,
20, and 23 cannot be explained in the same way, because they are absent from
Europe.
The Y Haplotype Network
The 32 different Y haplotypes were connected
into a parsimonious network assuming no recombination, because all markers were
located in the Y-specific region. Information on the mutation mechanisms that
characterize the variability of the h system (Santos et al. 1995a,
1995b,
1996a)
was used, as well as some additional information about the known ancestral
states for DYS199 (Underhill et al. 1996),
YAP (Hammer and Horai 1995),
Tat (Zerjal et al. 1997),
and SRY-1532 (Whitfield et al. 1995) and
also the inferred ancestral state for 92R7 (Mathias et al. 1994;
Jobling and Tyler-Smith 1995;
Jobling et al. 1997). Variability of the 6-kb and 4.1-kb alphoid units was
partially associated with the h system (Santos et al. 1995b),
and most of the Y chromosomes seemed to have both the 6-kb and 4.1-kb units
(Mathias et al. 1994;
Santos et al. 1995b;
F. R. Santos, A. Pandya, and C. Tyler-Smith, unpublished data). The deletion of
the 6-kb units can generate chromosomes bearing 4.1-kb divergent units only, and
further deletion of the 4.1-kb units generates chromosomes containing no
divergent units. Since deletion events that cause the loss of many units of
alphoid DNA are relatively frequent (Mathias et al. 1994;
Santos et al. 1995a,
1995b,
1996a),
we allowed these events to be recurrent on the network.
The occurrence of an extra reverse mutation at
the SRY-1532 locus is represented as a recurrent step in this parsimony
network, leading to haplotype 32. It is supported by the association with 92R7
alleles, by the specific association with h type II, and by analysis with an
additional 19 Y markers (F. R. Santos, A. Pandya, and C. Tyler-Smith,
unpublished data). In addition, the geographic distribution of haplotype 32 is
very similar to that of haplotype 1, its deduced immediate ancestor, and is
quite distinct from that of haplotype 19, which shares with haplotype 32 the
same allele A at SRY-1532. The same network was obtained with the
procedure of median network analysis (Bandelt et al. 1995),
which allows the resolution of networks containing such recurrent markers. Our
unique network shows the sequential accumulation of mutations used to trace
several Y lineages from the ancestral haplotype. The most likely root for this
network is haplotype 19, seen only in an African San, because it bears the
ancestral states for all the loci for which this information is known or
inferred . A recent study with several new biallelic Y markers (Underhill et al.
1997) also supports the conclusion that the San haplotype 19 is
the most ancestral Y chromosome. Following from the probable root, haplotypes 3,
13, and 10 are direct ancestors of the Native American haplotype 31, and other
related haplotypes, such as haplotypes 20 and 1, share with haplotype 31 the
common ancestor haplotype 10. The frequent and widespread haplotype 3 is
probably very old, because it gave rise to most, if not all, of the Y
chromosomes found outside Africa. Haplotype 13 also is probably old but is very
rare, which could indicate that the 92R7 mutation happened quite soon after the
origin of haplotype 13, producing haplotype 10. However, a simple deletion of
the 6-kb alphoid units in an individual with haplotype 3 can lead to a recurrent
haplotype 13. By using other Y markers (F. R. Santos, A. Pandya, and C.
Tyler-Smith, unpublished data), we found that the two Chinese individuals with
haplotype 13 are recurrent types, because of a de novo deletion of the 6-kb
units. Thus, interpretation of the distribution of the few haplotype 13
individuals should be made with care. Fortunately, haplotype 10, the immediate
ancestor of haplotype 31, is defined by the point mutation at 92R7 and, together
with all chromosomes derived from it, makes up the 92R7 lineage that is
important for the tracing of the major migrant Y chromosome to the Americas.
Global Diversity of Y Chromosome
Haplotypes
Our study used markers defining many branches
of the 92R7 lineage, with a consequent bias toward a better resolution of
populations containing this lineage, despite the fact that most variation was
found in the h polymorphism, with no such apparent bias (Santos et al. 1995b,
1996a).
For this reason, the gene diversity (Nei 1987) for
each population usually was increased when different 92R7-lineage derivatives
were present, which also could have increased slightly the within-population
variance calculated with AMOVA (discussed below). Therefore, this study was
oriented toward a detailed investigation of Y lineages that are interesting with
regard to the peopling of the Americas and should not be considered a broad and
unbiased description of all worldwide Y lineages.
The genetic structure of this Y chromosome data
was analyzed in detail by use of AMOVA (Excoffier et al. 1992),
which allows an estimation of the relative distribution of genetic diversity in
three hierarchic levels: among individuals, among populations, and among
geographic groups. The AMOVA resulted in the values 59%, 25%, and 16%,
respectively, for worldwide Y chromosome diversity. The value of 59% of the
total Y chromosome variability found among individuals is relatively low,
compared with the value of 85% obtained for other autosomal DNA polymorphisms
(Barbujani et al. 1997). Thus, the higher degree of interpopulation and geographic
diversity (41%) of Y chromosomes observed in this study emphasizes the
usefulness of Y chromosome haplotype analysis, to discriminate between
populations and to elucidate past male migrations within and across continents
(Jobling and Tyler-Smith 1995;
Santos and Tyler-Smith 1996).
Y Chromosome Population Trees
AMOVA (Excoffier et al. 1992) also
generated a matrix of FST analogs between populations of Y
chromosomes. This procedure avoids the use of allele frequencies to calculate
genetic distances, since the loci in the nonrecombining portion of the Y
chromosome are not independent. Otherwise, if we used only the haplotype
frequencies (considering the Y chromosome as a single locus, as expected), we
would lose the information of shared ancestry. When running AMOVA, we computed
the similarity of populations sharing haplotypes related by descent, by taking
into account both haplotype frequencies and molecular differences between
haplotypes (see Material and
Methods). These pairwise FST's computed by AMOVA were used
to draw neighbor-joining and UPGMA gene trees (Felsenstein 1993), to
display the relationship of Y chromosome populations. Similar trees were
obtained with two other distances (data not shown). By use of a nonparametric
permutation test (Excoffier et al. 1992), the
calculated FST distances were shown to be significant
(P < .05), except between the Buryats and Yakuts, the closest groups
on the trees. In all the trees, the Native American Y chromosomes clustered with
Kets, Altaians, and Caucasoids (Europeans and Indians). European admixture
cannot explain this cluster, because if we exclude in the analysis all
haplotypes present in Siberians and Amerindians that are also found in Europe
(such as haplotype 1, which appears in four Native Americans), the tree remains
very similar (data not shown). This tree structure also did not change when we
used the inferred frequency 87% for haplotype 31 among 132 Native Americans,
published previously (Pena et al. 1995;
Santos et al. 1995a;
Underhill et al. 1996).
Although some Siberian and Native American Y
chromosomes show remarkably close association with Caucasoid Y chromosomes,
other Siberian populations are very distinct, clustering with other Asians. A
particular Siberian cluster is formed by Buryat and Yakut Y chromosomes, mainly
because of the common origin of most of their Y chromosomes, with the high
frequency of the Tat mutation (table 1;
Zerjal et al. 1997).
Thus, our findings from the haplotype distribution, the haplotype network , and
the Y chromosome population trees suggest a high interpopulation differentiation
in Siberia, probably because of distinct founder populations and subsequent
genetic drift. In addition, these data identify the group of Ket and Altaian Y
chromosomes that are related to those among Native Americans and Caucasoids,
whereas the Evenki Y chromosomes are related to those of Mongolians. Yakut and
Buryat Y chromosomes, which previously were shown to have a common origin with
Uralic Y chromosomes (Zerjal et al. 1997),
form another distinct cluster.
Discussion
A human Y chromosome phylogeny was used to
trace the origins of the major founder haplotype of the Americas, haplotype 31.
The worldwide distribution of Y haplotypes associated with the information of
sequential mutations, displayed in the network , allowed the construction of a
map showing the likely pathway of Y chromosomes migrating to the Americas. The
present-day distribution of haplotypes related to haplotype 31 can be explained
by a radiation from central Eurasia through a northern migration route to the
Americas and a southern route to the Indian subcontinent. This dichotomy is
supported by the absence of haplotypes 1, 10, 20, and 32 in China and Japan (table 1),
including in the analysis of another 56 Chinese and 138 Japanese samples (F. R.
Santos and C. Tyler-Smith, unpublished data). A migration route from central
Eurasia to northeastern Siberia during the Upper Pleistocene was suggested
recently (Lahr and Foley 1994), and the occurrence of several Caucasoid lineages in the
Indian subcontinent can be explained by the immigration of Indo-European
speakers from central Eurasia after 5,000 ybp (Cavalli-Sforza et al. 1994).
The major Native American haplotype 31 is
present on both sides of Beringia, most likely because of an American or
Beringian origin of the mutation in the DYS199 locus (Karafet et al. 1997;
Lell et al. 1997).
Its immediate ancestor, haplotype 10, is a rare haplotype (11 of 306
individuals) seen only in North America (n = 6), India (n = 4),
and Mongolia (n = 1). An old population bearing haplotype 10, a Native
American/Siberian/Caucasoid common ancestor, has been placed somewhere in
central Eurasia . Haplotypes 1 (Caucasoid), 20 (Siberian and Native American),
and 31 (Native American) are derived from this ancestor. The most common
European chromosome, haplotype 1, appeared in four Native American samples from
paternity tests in North America; thus, they very likely could be due to recent
admixture. Haplotype 20, another descendant of haplotype 10 by a simple alphoid
locus-deletion step, is very frequent in Kets and was found in some Altaians,
all of whom were shown to also have the DYS19 A allele (data not shown),
which is also present in most individuals with haplotype 31 (Pena et al. 1995;
Santos et al. 1995a;
Underhill et al. 1996).
Recently, the Ket language was suggested to be closely related to the Na-Dene
language (Greenberg 1996), and the resemblance of Kets to Native Americans and
Caucasoids, with regard to physical appearance (Forsyth 1996) and
Y chromosomes (this study), makes them the most likely central Siberian
population to share the same recent ancestors. The Altaians, a common
denomination for seven formerly distinct Turkic populations, exhibit very
diverse Y haplotypes and could have acquired their Y chromosomes from many
neighboring tribes, including the Kets (Forsyth 1996).
Our study can be compared to current research
on the peopling of the Americas. Recent archeological and anthropological
studies of the first settlement of the Americas are revealing many alternative
migration routes and older dates for settlement (Roosevelt et al. 1996), as well as raising doubts about the Mongolian origins of
the first migrants (Neves and Pucciarelli 1991;
Lahr 1995).
The multiple-dispersals model, suggested recently by paleoanthropologists (Lahr
and Foley 1994),
claims that the first migrants to the Americas were from a Southeast Asian
stock, whereas our Y chromosome data suggest a northern Eurasian route of
migration. However, they also proposed two distinct dispersals from central
Eurasia to northeastern Siberia and Europe, one in the middle Upper Pleistocene
(50,000-15,000 ybp) and another in the late Upper Pleistocene (15,000 ybp to
present). The former could be the source of the Y chromosomes in those who first
migrated to the Americas through Siberia, as well as the source of the Y
chromosomes in those colonizing Europe in the Paleolithic.
The very recent find of the 9,400-year-old
skeleton of the Kennewick man, which displays some Caucasoid characteristics,
and his contemporary, the Spirit Cave mummy, suggests that the earliest migrants
could be distinct from present-day populations (Morell 1998b). Possible genetic relationships between Eurasians
and Native Americans are suggested by the presence of the rare mtDNA haplogroup
X in both population groups, which apparently is absent in Siberia (Morell 1998a). Alternatively, in our study, the Y chromosome data
reveal a common ancestor (haplotype 10) between Native Americans and Europeans,
who left some rare descendants in Siberia, among the Kets and Altaians. However,
the presence of the most common European haplotype 1 in the Americas can be
explained as a recent European admixture more likely than as a remnant of a
pre-Columbian migrant. Our Y chromosome data, when compared with morphological
and mtDNA data, could imply another migration of typically Mongoloid people, who
would have left phenotypic traces in their Native American descendants without
contributing many of their Y chromosomes. This pattern of unequal paternal and
maternal contributions in the gene pools of several populations has been
characterized and discussed in detail by Poloni et al. (1997).
The major Native American Y haplotype occurs in
high frequencies among Amerindians, Na-Denes, and Aleut-Eskimos (Pena et al. 1995;
Santos et al. 1995a,
1996b;
Underhill et al. 1996;
Karafet et al. 1997;
Lell et al. 1997;
Rodriguez-Delfin et al. 1997; Underhill et al. 1997). It
represented 90% of 90 nonadmixed South American Indians in our previous studies
(Pena et al. 1995;
Santos et al. 1995a)
and 60% of 412 Native American Y chromosomes analyzed by other groups (Underhill
et al. 1996;
Karafet et al. 1997;
Lell et al. 1997;
Rodriguez-Delfin et al. 1997;
Underhill et al. 1997),
including Y chromosomes from tribes with a very high level of admixture,
especially in North America (Santos et al. 1996b;
Crawford 1998). The
presence of this founder Y haplotype in the Americas suggests a single major
migration and is compatible with a settlement model incorporating a population
differentiation of all Native Americans in Beringia, as suggested by recent
mtDNA studies (Forster et al. 1996;
Bonatto and Salzano 1997). The
first migrants bearing a proto-Caucasoid Y chromosome (haplotype 10) would have
come from the region of central Siberia to Beringia 30,000 ybp (Cavalli-Sforza
et al. 1994;
Underhill et al. 1996).
The mutation in the DYS199 locus, which produced haplotype 31, could have
happened in this Pleistocene Beringian population, which would have experienced
an expansion and migrated south to the Americas, through the Alberta ice-free
corridor. Subsequently, the collapse of this corridor 20,000-14,000 ybp
(reviewed in Bonatto and Salzano 1997)
would have isolated the population that was still in Beringia from the recent
migrants in the Americas, who, after a major founder effect, would give rise to
the Amerindians. During this time of isolation, new minor Siberian migrants
could have come to Beringia, and, at the end of the glaciation (12,000-10,000
ybp), these Beringians finally could have migrated to the Americas, originating
the Na-Dene and Eskimo-Aleut speakers, with both still retaining the major
haplotype 31 (Underhill et al. 1996;
Karafet et al. 1997;
Lell et al. 1997) and
other Y chromosome lineages in frequencies higher than those in Amerindians,
exemplified by haplotypes 10, 20, and 23 in North American Indians (table 1).
These chromosomes could represent later migrations from central Siberia or
Mongolia, despite the possibility that present-day individuals with haplotype 10
could be descendants of the first migrants prior to the acquisition of the
DYS199 mutation. Other scenarios, involving earlier dates (<15,000
ypb), for the first settlement of the Americas are likely, but it is difficult
to explain a single major migration with further differentiation for at least
three major Native American groups.
This study traces the major Native American Y
chromosome haplotype to the immediate ancestor shared with present-day Siberians
and to an older common ancestor shared with Caucasoids (Europeans and Indians).
This common ancestry of Native Americans and Caucasoids could explain the
existence of non-Mongoloid skeletons, such as the Kennewick man. Despite the
fact that the Y chromosome represents only 1 of 46 in the human male genome, in
numeric terms, its exclusive father-to-son inheritance allows us to study
patrilineages that reflect the past male migrations but that may not reflect the
global history of populations. However, the Y lineage is the largest of many
genomic lineages that compose the population history of modern Homo
sapiens, and it is the counterpart to mtDNA lineage studies. Furthermore,
the human Y chromosome seems to display an association with linguistics and
geography that is higher than that for mtDNA (Poloni et al. 1997),
and our data concur with some current views on the settlement of the Americas.
Further analysis of all Y lineages present in the Americas that uses
microsatellites (Santos and Tyler-Smith 1996;
Zerjal et al. 1997)
will be very useful in the detailed study of all trans-Bering Strait migrating
lineages, as well as to the more precise determination of their entry time into
the Americas.
Acknowledgments
We thank D. R. Carvalho-Silva and E.
Tarazona-Santos for comments on the manuscript. This work was supported by
grants from Conselho Nacional de Desenvolvimento Cientifico e Tecnologico and
Fundação de Amparo à Pesquisa do Estado de Minas Gerais, Brazil, and from the
Leverhulme Trust, United Kingdom.
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