It has been shown that Neanderthals contributed genetically to modern humans outside Africa 47,000–65,000 years ago. Here we analyse the genomes of a Neanderthal and a Denisovan from the Altai Mountains in Siberia together with the sequences of chromosome 21 of two Neanderthals from Spain and Croatia. We find that a population that diverged early from other modern humans in Africa contributed genetically to the ancestors of Neanderthals from the Altai Mountains roughly 100,000 years ago. By contrast, we do not detect such a genetic contribution in the Denisovan or the two European Neanderthals. We conclude that in addition to later interbreeding events, the ancestors of Neanderthals from the Altai Mountains and early modern humans met and interbred, possibly in the Near East, many thousands of years earlier than previously thought.
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We thank M. Slatkin, F. Racimo, J. Kelso, K. Prüfer, M. Stoneking and D. Reich for comments; the MPI-EVA sequencing group, B. Nickel and R. Schultz for technical support; A. Heinze, S. Sawyer and J. Dabney for sequencing library preparation; U. Stenzel and G. Renaud for help with sequence processing. M.J.H. was supported by the National Science Foundation Graduate Research Fellowship under grant DGE-1144153. Q.F. was funded in part by the Special Foundation of the President of the Chinese Academy of Sciences. T.M-B. was supported by ICREA, EMBO YIP 2013 and Fundació Barcelona Zoo. The Max Planck Society, the Krekeler Foundation, MINECO (grants BFU2014-55090-P FEDER, BFU2015-7116-ERC and BFU2015-6215-ERC to T.M-B. and BFU2012-34157 FEDER to C.L.-F.) and the US National Institutes of Health (grant GM102192 to A.S. and U01 MH106874 to T.M-B.) provided financial support.
The authors declare no competing financial interests.
Extended data figures and tables
Total migration rates estimated for 22 directional migration bands in five separate preliminary G-PhoCS runs. Rows correspond to source populations and columns to the target populations. The 20 migration bands between modern and archaic populations were considered in five separate runs, each containing the four bands associated with a different modern human population (Supplementary Fig. 15A). The two migration bands between the Denisovan and the Altai Neanderthal populations were considered in all five runs, and the values shown here correspond to an aggregate of all five runs. The estimates are as shown in Supplementary Fig. 15B. Shade indicates the posterior mean total migration rate (legend), which approximates the probability that a lineage in the target population originated in the source population. The 95% Bayesian credible intervals from 2,000 MCMC replicates are indicated for migration bands whose upper credible interval bound is above 0.3%. We identified four clusters of migration bands, corresponding to what were likely at least four different cases of introgression between populations: (1) Neanderthals into non-African modern humans (red box), (2) Denisovans into Oceanians (green box), (3) between Neanderthals and Denisovans (magenta), and (4) modern humans into Neanderthals (blue box). Alt, Altai Neanderthal; Chi, Chinese; Den, Denisovan; Fre, French; Pap, Papuan; Yor, Yoruba.
Simulated data were generated under the demographic model as inferred by G-PhoCS (Supplementary Table 13). Each simulated data set consisted of 10,000 loci of 1 kb length. We simulated the Altai Neanderthal, the Denisovan, and three modern human populations corresponding to the San, Yoruba, and French, with modern human demography consistent with recent studies (Supplementary information section 8). Three migration bands were simulated: (1) from the Altai Neanderthal to the Denisovan, (2) from a population that diverged from the ancestors of all present-day humans 300,000 years ago into the Altai Neanderthal, and (3) from a population that diverged from the ancestors of all modern and archaic humans roughly 2.6 million years ago into the Denisovan. a, Estimates of effective population sizes (theta, θ), population divergence times (tau, τ) and migration rates (m) from three G-PhoCS runs on data simulated with gene flow from modern humans into the Altai Neanderthal lineage. Each run analyses an individual from a different present-day population, using the exact same setup used in our main analysis (Supplementary Fig. 15A). Parameters are typically estimated accurately, with 95% Bayesian credible intervals containing the values used in simulations (horizontal red lines). Rates of archaic gene flow into Denisovan appear to be somewhat overestimated, and differences between analyses of African and non-African populations are consistent with those observed in the data analysis (Supplementary Fig. 15B). b, Similar analysis done on data simulated without gene flow from modern humans into the Altai Neanderthal lineage. Accurate estimates are obtained for all model parameters, and no gene flow is inferred from modern humans into the ancestors of the Altai Neanderthal. Error bars represent the 95% Bayesian credible intervals from 2,000 MCMC replicates.
Extended Data Figure 3 Simulation of different source populations for modern introgression into Neanderthals.
Estimated rates of migration from the modern human population to the Altai Neanderthal population obtained from 15 G-PhoCS runs on five simulated data sets. All demographic parameters are set according to the values inferred by G-PhoCS in our data analysis (Supplementary Table 13), and the five data sets differ by the source population for migration: no migration (none), population ancestral to all present-day humans (ancestral), population ancestral to Yoruba and Europeans (Yoruba), San population (San), and European population (European). The first two sets are the ones analysed in Extended Data Fig. 2. Each data set is analysed three times, using different present-day samples: European (French), Yoruba, or San. Significant differences in estimates are observed between the data sets with and without gene flow and the data set with gene flow from a source population related to Europeans. Only minor differences were observed between values inferred for the three data sets with source population diverging from African populations (San, Yoruba, and ancestral). We conclude from this that the source population likely diverged from an African human population before the divergence of present-day Eurasians. The shaded circle in Fig. 3a represents this conclusion. Error bars represent the 95% Bayesian credible intervals from 2,000 MCMC replicates.
Simulated windows of 100 kb for the Altai Neanderthal and Denisovan genomes with present-day human contamination of 5% at the genotype level. Windows are binned by their minimum divergence to Africans using derived alleles at >0.9 frequency in the simulated African population. The x and y axis as in Fig. 1. a, Gene flow from a deeply divergent archaic hominin into the Denisovan lineage (1%) and Altai Neanderthal gene flow into the Denisovan lineage (0.65%). b, Gene flow from a deeply divergent archaic hominin into the Denisovan lineage, Altai Neanderthal gene flow into the Denisovan lineage and modern human gene flow into the Altai Neanderthal lineage (1.8%). Error bars represent the 95% confidence intervals from 1,000 bootstrap replicates.
a, Distribution of ‘African’ haplotype ages in sequences simulated with introgression into the Altai Neanderthal lineage from modern humans 100,000 years ago. ‘African’ haplotypes are identified as in Fig. 2. Error bars represent the 95% Bayesian credible intervals from 302 MCMC replicates. b, Distribution of true haplotype ages for each of the estimated ages. The horizontal dotted lines show the estimated age. The plot is divided into four quadrants; the lower half represents ‘African’ haplotypes having true ages between 100,000 and 620,000 years ago (the divergence time between archaic and present-day humans), which are necessarily due to post-divergence gene flow from modern humans. The left side of the plot represents regions that would be identified as introgressed based on a threshold of ≤ 234,000 years. The counts in each quadrant are for Altai Neanderthal (red) and Denisovan (blue), respectively. The counts for the Denisovan in the lower two quadrants are zero because there was no simulated migration from modern humans into the Denisovan lineage. Note that this is a somewhat nonstandard plot of true age versus estimated age; a more standard, reversed view is given in Supplementary Fig. 33 and demonstrates that the estimated ages are largely unbiased. Error bars as in the standard Tukey box plot (R boxplot function).
Summary of the main demographic inference using G-PhoCS in a model with four archaic populations and one modern human population. a, The population phylogeny assumed in each of the G-PhoCS runs. Labels on internal edges indicate names of the four ancestral populations: population ancestral to the two Western Neanderthals (W.NEA), population ancestral to all three Neanderthals (NEA), population ancestral to all four archaic individuals (ARC), and population ancestral to all human samples (HUM). We augmented the phylogeny with 14 directional migration bands (arrows) between all pairs of sampled populations except for the pairs of Neanderthal populations. In one of the runs we added an unknown ‘ghost’ population and a migration band from that population into the Denisovan population. b, Parameter estimates obtained by G-PhoCS in six separate runs analysing 13,754 neutral and loosely linked loci, substituting samples in the ‘Modern’ population with pairs of present-day humans from five different modern populations (Supplementary Table 11). The last run has gene flow from the ‘ghost’ population and uses two Yoruba individuals in the modern human population. Bar heights indicate posterior mean and error bars correspond to 95% Bayesian credible intervals. Estimates of divergence times (τ) and effective population sizes (θ) are given in raw form, scaled by number of mutations per 10 kb (left axis), and calibrated to absolute units, 1,000 years for time, and 1,000 individuals for effective population size, (right axis) assuming an average mutation rate of 0.5 × 10−9 mutations per year per bp and an average generation time of 29 years. For each of the 14 migration bands, we are showing the estimated total migration rates (m). See Supplementary Information section 8 for more information on parameter calibration and setup for G-PhoCS. A graphical summary of these estimates is given in Fig. 3.
Total migration rates estimated for 46 directional migration bands in five separate G-PhoCS runs. Rows correspond to source populations and columns to the target populations. The 40 migration bands between modern (present-day) and archaic populations were considered in five separate runs, each containing the eight bands associated with a different modern human population (Extended Data Fig. 6a). The six migration bands between the Denisovan population and the three Neanderthal populations were considered in all six runs, and the values shown here were estimated as an aggregate of all five runs. The estimates are as shown in Extended Data Fig. 6. Shade indicates the posterior mean total migration rate (legend), which approximates the probability that a lineage in the target population originated in the source population. The 95% Bayesian credible intervals from 2,000 MCMC replicates are indicated for migration bands whose upper credible interval bound is above 0.3%. We identified four clusters of migration bands, corresponding to what were likely at least four different cases of introgression between populations: (1) Western (European) Neanderthals into non-African modern humans (red box), (2) Denisovans into East Asian and Oceanians (green box), (3) Neanderthals into Denisovans (magenta), and (4) modern humans into Eastern Neanderthals (blue box). Directed arrows in Fig. 3a depict these introgression events. Sid, El Sidrón Neanderthal; Vin, Vindija Neanderthal.
The putatively introgressed segments in the Altai Neanderthal genome, defined by derived alleles in two individuals from the San, Yoruba, Mbuti, Dinka or Mandenka populations. The introgressed segments show no clear affinity to one present-day African population. A, Altai Neanderthal; S, San; M, Mbuti; Y, Yoruba; D, Dinka; N, Mandenka.
Ratio of functional (putatively deleterious) to neutral polymorphism in archaic and present-day humans (Supplementary Information section 7). TFBS, transcription factor binding sites; upstream refers to 5 kb before the transcription start site of genes; UTRs, untranslated regions (in the mRNA). PhastCons ≥ 0.9 for a site to be used. Ne, Neanderthals; Af, Africans; As, Asians; Am, Americans.
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Kuhlwilm, M., Gronau, I., Hubisz, M. et al. Ancient gene flow from early modern humans into Eastern Neanderthals. Nature 530, 429–433 (2016). https://doi.org/10.1038/nature16544
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