Abstract
Modern genetic data combined with appropriate statistical methods have the potential to contribute substantially to our understanding of human history. We have developed an approach that exploits the genomic structure of admixed populations to date and characterize historical mixture events at fine scales. We used this to produce an atlas of worldwide human admixture history, constructed using genetic data alone and encompassing over 100 events occurring over the past 4,000 years. We identify events whose dates and participants suggest they describe genetic impacts of the Mongol Empire, Arab slave trade, Bantu expansion, first millennium CE migrations in eastern Europe, and European colonialism, as well as unrecorded events, revealing admixture to be an almost universal force shaping human populations.
Diverse historical, archaeological, anthropological and linguistic sources of information indicate that human populations have interacted throughout history, due to the rise and fall of empires, invasions, migrations, slavery, and trade. These interactions can result in sudden or gradual transfers of genetic material, creating admixed populations. However, the genetic legacy of these interactions remains unknown in most cases, and the historical record is incomplete. We have developed an approach that provides a detailed characterization of the mixture events in the ancestry of sampled populations, based on genetic data alone.
Admixed populations should have segments of DNA from all contributing source groups (Fig. 1A), whose size decreases over successive generations due to recombination, and approaches have been developed to date admixture events by inferring the size of ancestry segments (1-5). Between-population frequency differences of individual alleles may provide information on ancestry sources (6, 7). Based on these principles we developed an integrated approach, using genome-wide patterns of ancestry to infer jointly both fine-scale information about groups involved in admixture, and its timing, allowing for the fact that migration and admixture events can occur at multiple times or involve numerous groups.
Our approach gains power and resolution by using alleles at multiple successive SNPs (haplotypes) (8). Given a focal population within a larger dataset containing many such groups, the chromosomes of individuals in this population share ancestors with those in other populations, resulting in shared “chunks” of DNA. We used CHROMOPAINTER (8) to decompose each chromosome as a series of haplotypic chunks, each inferred to be shared with an individual from one of the other groups, and colored (or painted) by this group (Fig. 1B). If the focal population is admixed, the changing colors along a chromosome noisily reflect true, but unknown, underlying ancestry (Fig. 1B), and so can be used to learn details of the source group(s) involved. To do this, we model haplotypes within each unsampled source group as being found across a weighted mixture of sampled “donor” populations (9). If a source group is genetically relatively similar to a single sampled population, then this population will dominate the inferred mixture. If there is no close proxy for the admixing group in the sample, especially likely for ancient admixture events or sparsely sampled regions, several donor populations will be needed to approximate its pattern of haplotype sharing. The focal population is then automatically a haplotypic mixture of the combined donors, because it is a mixture of the source groups. Inferring the reduced set of groups within the mixture allows us to produce a “cleaned” painting (Fig. 1B) using only these groups.
To assess the evidence for admixture and date events, informally we measure the scale at which the “cleaned” painting changes along the genome. Specifically, we produce a “coancestry curve” for each pair of donor populations, which plots genetic distance x against a measure of how often a pair of haplotype chunks, separated by distance x, come from each respective population (Fig. 1C), analogously to ROLLOFF curves (4), and averaging over uncertain, and typically computationally estimated, haplotypic phase (9). In theory, given a single admixture event, ancestry chunks inherited from each source have an exponential size distribution, resulting in an exponential decay of these coancestry curves (9). The rate of decay in all curves will be equal to the time in generations since admixture (Fig. 1C) (4, 9, 10), allowing estimation of this date: steeper decay corresponds to older admixture. Such a decay distinguishes true admixture from ancient spatial structure, and should only occur in recipient, but not donor, groups involved in non-reciprocal admixture events. We test for evidence to reject (p<0.01) a no-admixture null model, i.e. no exponential decay in (normalized) coancestry curves, via bootstrapping (9). Multiple admixture times result in a mixture of exponentials (9); so if admixture is detected, we test for evidence of multiple admixture times (e.g. two episodes of admixture, or more continuous admixture over a longer period; empirical p<0.05 in simulations), comparing the fit of a single exponential decay rate versus a mixture of rates.
The curve heights (intercepts) provide complementary information to deconvolve the number and genetic composition of the ancestral sources prior to admixture (11). Fitted curves for all pairs of donor groups (Fig. 1C shows three examples) specify a pairwise intercept matrix which, following normalization, we decompose using a series of eigenvectors. Analogous to the standard use of eigenvector decomposition in principal components analysis (PCA) in genetics to estimate relative ancestry source contributions for different individuals (12), the eigenvectors allow us to estimate the relative contribution to different admixing sources (e.g. source 1 vs. source 2) for each different donor group (9). Also as for PCA, admixture between K distinct source populations produces K-1 significant eigenvectors (13), and we test for three or more admixing sources by testing (empirically) for evidence of two or more such eigenvectors (p<0.05) (9). Following iterative modeling to improve results, this allows us to attempt to “reverse” the admixture process (Fig. 1D) and infer the haplotypic makeup of admixing source groups as well as admixture date(s), in our method GLOBETROTTER.
To test our approach under diverse single, complex and no-admixture scenarios, incorporating many of the complexities – such as unsampled or admixed donor groups – likely to be present in real data, we simulated admixture scenarios involving real (but hidden to our analysis) human populations (4, 9) and populations generated under a coalescent framework (14) incorporating inferred (15-18) past demographic events. Admixture was simulated between 7 and 160 generations (200-4,400 years, assuming 28 years per human generation (19)) ago, with admixture fractions 3%-50%, and genetic differentiation (FST) between the admixing groups varying from 0.018 (similar to Europe vs Central Asia) to 0.185 (similar to West Africa vs. Europe). Results are detailed online (Fig. S3-7; Tables S1, S5). All populations simulated without admixture, including those with long-term migration, showed no admixture evidence (p>0.1). Power to detect admixture (p<0.01) when present was 94%, and 95% of our 95% bootstrapped confidence intervals contained the true admixture date, including cases with two distinct incidents of admixture or multiple groups admixing simultaneously. Inferred source accuracy was very high (9), with e.g. the mixture representation predicting a haplotype composition more correlated to the true, typically unsampled, source population than to any single sampled population >80% of the time. However source accuracy was lower for admixing sources contributing only 5% of DNA, with around 40% of such scenarios yielding elevated (>25%) rates of falsely inferring multiple admixture times and/or admixing groups. Further testing demonstrated robustness of GLOBETROTTER, in simulations and real data, to haplotypic phase inference approach used, inclusion/exclusion of particular chromosomes, genetic map chosen to provide genetic distances, and the presence of population bottlenecks since admixture, while GLOBETROTTER admixture dating was improved relative to ROLLOFF (4, 9).
Nevertheless, there are a number of settings which we believe are challenging for our approach. First, although the admixing sources need not be sampled – often impossible due to genetic drift, extinction, or later admixture into the sources themselves - source inference is improved when more similar extant groups are sampled, and GLOBETROTTER may miss events where we lack any extant group that can separate sources. Second, sampling of several genetically very similar groups can mask admixture events they share. Similarly, a caveat is that where genuine, recent bidirectional gene flow has occurred, admixture fractions are difficult to define and interpret. However, date estimation is predicted to still be useful, and in real data the majority of our inferred events do not appear to be bidirectional in this manner. Third, even in theory our approach finds it challenging to distinguish distinct continuous “pulses” of admixture and continuous migration over some timeframe (9), due to the difficulty of separating exponential mixtures (20). If the time frame were narrow, we expect to infer a single admixture time, within the range of migration dates. Where we infer two admixture dates, in particular with the same source groups, the exponential decay signal could also be consistent with more continuous migration, and so we conservatively refer to this as admixture at “multiple dates”. Finally, we only attempt to analyze populations with signals consistent with at most 3 groups admixing, and infer at most two admixture times, and we can provide only less precise inference of sources for the weaker/older admixture signal in these complex cases (9).
Using GLOBETROTTER, we analyzed 1,490 individuals from 95 worldwide human groups (Table S6, Fig. S11) (9), comprising 17 newly genotyped groups (21), 53 from the Human Genome Diversity Panel (HGDP) (22) and 25 from other sources (23, 24), filtered to 474,491 autosomal SNPs. We phased the individuals using IMPUTE2 (9, 25) and used fineSTRUCTURE (8) to verify homogeneity within labeled populations, identify genetically similar and clustered groups, and to remove outlying individuals (Figs. S12-S14; Tables S10-11). Of the 95 populations, 80 showed evidence (p<0.01) of admixture, although nine could not be characterized by our approach (Table S8). More than half of these have evidence of multiple waves of admixture (p<0.05), and estimated admixture times vary from <10 generations, to >150 generations (Fig. 2). We present individual results, for each population, via an interactive map online (26). We tested consistency of our results against a previous analysis of the 53 groups within the HGDP (11), which identified 34 groups with evidence of recent admixture. We identify (p<0.01) admixture evidence in all 34 cases (with multiple event evidence in 15 cases), and obtain 95% admixture date CIs narrower than, but consistent with, those estimated using ROLLOFF (9, 11). For 10 of 19 HGDP groups lacking previous support for recent admixture, GLOBETROTTER also identifies no events: in the remaining populations admixture is inferred as occurring between genetically similar sources (FST<0.02), a challenging setting where simulations suggest our method is more powerful (9).
In several instances, GLOBETROTTER clarifies or extends previous genetic analyses. For example, a previous study (27) inferred admixture in the Maya, with best source populations the Mozabites from North Africa and the Native American Surui, speculating based on historical events that this might actually represent a mixture of European, West African and Native American ancestry sources. GLOBETROTTER inferred admixture between three groups in the Maya dating to around 1670CE (9 generations ago) (28) (Figure 2A; Fig. 2D, hot pink box 1), with distinct sources from Europe (most genetically similar to the Spanish), West Africa (the Yoruba) and the Americas (the Pima, the nearest sampled group in the Americas). A different method – which aims to detect, but not date, admixture - concluded that Cambodians trace ~16% of their DNA to a group equally related to modern-day Europeans and East Asians (29). GLOBETROTTER infers a ~19% contribution from a similar source - related to modern-day Central, South and East Asians - and an ~81% contribution from a source related specifically to modern-day Han and Dai, the latter a branch of the Tai people who entered the region in historical times (30) (Fig. 2D, orange box 5). Further, this event dates to 1362CE (1194-1502CE), a period spanning the end of the Indianized Khmer empire (802-1431CE) (30), one of the most powerful empires in Southeast Asia whose fall was hypothesized to relate to a Tai influx (30).
A comparison with the historical record becomes progressively more difficult for older episodes. Even when events are well attested their exact genetic impacts (if any) are rarely if ever known, motivating our approach. Nevertheless, we have identified nine groups of populations showing related events, incorporating almost all (19/20) with the strongest GLOBETROTTER admixture evidence (9). Results are presented as online maps (26). Some events appear to match well with particular historical occurrences such as the Bantu Expansion into Southern Africa (9). Events affecting a group of seven populations (Fig. 2D, purple box 4) correspond in time to the rapid expansion led by Genghis Khan and the subsequent Mongol empire (1206-1368CE) (31), one of the most dramatic events in human history. These populations, including the Hazara (32, 33), Uygur (34) and the Mongola themselves, were sampled from within the range of the Mongol empire and show an admixture event dating within the Mongol Period, with one source closely genetically related to the Mongola that progressively decreases in proportion westward, to 8% in the Turkish (Fig. 2D).
Seventeen populations from the Mediterranean, Near East and countries bordering the Arabian Sea (Fig. 2D, blue box 3) show signals of admixture from sub-Saharan Africa, with most recent dates in the range 890-1754CE (Fig. 2B,D). We interpret these signals, consistent with overlapping results of previous studies (4, 20) as resulting from the Arab expansion and slave trade, which originated around the 7th century (35). Our event dates are highly consistent with this, but also imply earlier sub-Saharan African gene flow into e.g. the Moroccans. The highest-contributing sub-Saharan donor is West African for all 12 Mediterranean populations, and an East or South African Bantu-speaking group for all 5 Arabian Sea populations (Fig. 2D), confirming genetically different sources for these slave trades (35).
A population group centered around Eastern Europe shows signals of complex admixture. FineSTRUCTURE did not fully separate groups from this region, suggesting “masked” shared events might be present. We therefore repainted them excluding each other as donors: we performed similar re-analyses of five additional geographic regions for the same reason (Table S16; Figs. S16-21). The easterly Russians and Chuvash both show evidence (p<0.05) of admixture at more than one time (Fig. 2D), at least partially predating the Mongol empire, between groups with ancestry related to Northeast Asians (e.g. the Oroqen, Mongola and Yakut) and Europeans, respectively (Table S16). Six other European populations (Fig. 2D, pink/maroon box 2) independently show evidence following the repainting for similar admixture events involving more than two groups (p<0.02) at approximately the same time (Fig. 3). CIs for the admixture time(s) overlap, but predate the Mongol empire, with estimates from 440-1080CE (Fig. 3). In each population, one source group has at least some ancestry related to Northeast Asians with ~2-4% of these groups’ total ancestry linking directly to East Asia. This signal might correspond to a small genetic legacy from invasions of peoples from the Asian steppes (e.g. the Huns, Magyar and Bulgars) during the first millennium CE (36). The other two source groups appear much more local. One is more North-European in the repainting - when we exclude other East European groups as donors - and is largely replaced by northern Slavic-speaking groups in our original analysis (Fig. 2D; Table S12). The other source is more southerly (e.g. Greece, West Asians). This local migration could explain a recent observation of an excess of IBD sharing in Eastern Europe – including in the Greeks, in whom we infer admixture involving a group represented by Poland, at the same time -that was dated to a wide range between 1,000 and 2,000 years ago (37). We speculate that these events may correspond to the Slavic expansion across this region at a similar time, perhaps related to displacement caused by the Eurasian steppe invaders (38).
Finally, Central Asia shows a particularly complex inferred history following a reanalysis of 10 groups excluding each other as donors, with nine of ten groups showing diverse recent events (Fig. 4A). The exception are the Kalash, a genetically isolated (39) population from the Hindu Kush mountains of Pakistan (40). Distinct, ancient and partially shared admixture signals (always dated older than 90BCE) are seen in six groups (Fig. 4B), including the Kalash (Figure 2C), whose strongest signal suggests a major admixture event (990-210BCE) from a source related to present-day Western Eurasians, though we cannot identify the geographic origin precisely. This period overlaps that of Alexander the Great (356-323BCE) whose army, local tradition holds, the Kalash are descended from (40), but these ancient events predate recorded history in the region, precluding confident interpretation.
Our results demonstrate that it is possible to elucidate the effect of ancient and modern migration events, and to provide fine-scale details of the sources involved, complexity of events, and timing of mixing of groups, using genetic information alone. Where independent information exists from alternative historical or archaeological sources, our approach provides results consistent with known facts, and determines the amount of genetic material exchanged. In other cases, novel mixture events we infer are plausible, and often involve geographically nearby sources, supporting their validity. Admixture events within the past several thousand years affect most human populations, and this needs to be taken into account in inferences aiming to look at the more distant history of our species. Future improvements in whole-genome sequencing, greater sample sizes, and incorporation of ancient DNA – together with additional methodological extensions, are likely to allow better understanding of ancient events where little or no historical record exists, to identify many additional events, to infer sex biases, and to provide more precise event characterization than currently possible. We believe our approach will extend naturally to these settings, as well as to other species.
Supplementary Material
Acknowledgements
We are grateful for The John Fell Fund-University of Oxford, the NIH, the Wellcome Trust (SM, grant 098387/Z/12/Z), the BBSRC, the Royal Society/Wellcome Trust (GH, grant 098386/Z/12/Z), and The Istituto Italiano di Antropologia for funding. J.F.W. is a director, stockholder and employee of ScotlandsDNA (and formerly of EthnoAncestry). We thank S. Karachanak, D. Toncheva, P. Anagnostou, F. Cali, F. Brisighelli, V. Romano, G. LeFranc, C. Buresi, J. Ben Chibani, A. Haj-Khelil, S. Denden, R. Ploski, T. Hervig, T. Moen, P. Krajewski and R. Herrera for providing samples for our genotyping. We thank the blood donors and the staff of the Unità Operativa Complessa di Medicina Trasfusionale, Azienda Ospedaliera Umberto I, Siracusa (Italy). Data analyzed in this study may be downloaded via http://admixturemap.paintmychromosomes.com/.
References and Notes
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