- Open Access
Adaptively introgressed Neandertal haplotype at the OAS locus functionally impacts innate immune responses in humans
- Aaron J. Sams†1Email author,
- Anne Dumaine†2,
- Yohann Nédélec†2, 3,
- Vania Yotova2,
- Carolina Alfieri2, 4,
- Jerome E. Tanner2,
- Philipp W. Messer†1Email author and
- Luis B. Barreiro†2, 5Email author
© The Author(s). 2016
- Received: 28 May 2016
- Accepted: 4 November 2016
- Published: 29 November 2016
The 2’-5’ oligoadenylate synthetase (OAS) locus encodes for three OAS enzymes (OAS1-3) involved in innate immune response. This region harbors high amounts of Neandertal ancestry in non-African populations; yet, strong evidence of positive selection in the OAS region is still lacking.
Here we used a broad array of selection tests in concert with neutral coalescent simulations to demonstrate a signal of adaptive introgression at the OAS locus. Furthermore, we characterized the functional consequences of the Neandertal haplotype in the transcriptional regulation of OAS genes at baseline and infected conditions. We found that cells from people with the Neandertal-like haplotype express lower levels of OAS3 upon infection, as well as distinct isoforms of OAS1 and OAS2.
We present evidence that a Neandertal haplotype at the OAS locus was subjected to positive selection in the human population. This haplotype is significantly associated with functional consequences at the level of transcriptional regulation of innate immune responses. Notably, we suggest that the Neandertal-introgressed haplotype likely reintroduced an ancestral splice variant of OAS1 encoding a more active protein, suggesting that adaptive introgression occurred as a means to resurrect adaptive variation that had been lost outside Africa.
- Natural selection
- Innate immunity
Whole-genome sequencing of several archaic human genomes [1–5] representing Neandertals and an as yet geographically and paleontologically unknown population referred to as Denisovans has revealed gene flow between these populations and the ancestors of present-day humans. Neandertal ancestry makes up approximately 0.5–2% of the ancestry of most living humans, with higher amounts of Neandertal ancestry found outside of Africa [6–8]. While it seems that there may have been widespread purifying selection against Neandertal ancestry in humans [6, 8, 9], some positive selection on Neandertal genes (adaptive introgression) has also been observed [10, 11]. Neandertals and other archaic populations inhabited Eurasia for several hundred thousand years  and were likely well adapted to their environments. Therefore, some genetic variation inherited from these archaic humans may have been adaptive in modern humans, particularly across phenotypes that are strongly influenced by direct interactions with the surrounding environment , such as our immune response to infectious agents .
The oligoadenylate synthetase (OAS) locus on chromosome 12, which harbors three genes (OAS1, OAS2, OAS3) encoding the 2’-5’ OAS enzymes has received considerable attention due to its clear signatures of multiple archaic haplotypes in populations outside of Africa [14, 15] and the critical role of OAS genes in the innate immune response to viruses . Mendez et al.  first identified an introgressed haplotype of OAS1 from Denisovans that is restricted to individuals in Indonesia and Melanesia. Later, these authors  identified a Neandertal haplotype at the OAS locus that spans a ~190 kb region between two surrounding recombination hotspots.
We hypothesize that the overall lack of signals of selection in the OAS region stems from the low power of standard neutrality tests to detect adaptive introgression . Here we circumvent this issue by testing the hypothesis of adaptive introgression using extensive neutral coalescent simulations specifically tailored to match the genomic features of the OAS region in combination with several empirical observations of Eurasian genetic variation and ancient DNA data from Eurasia. We firmly demonstrate a population genetic signal of adaptive introgression at the OAS locus and characterize the functional consequences of the Neandertal haplotype in the transcriptional regulation of OAS genes in macrophages and peripheral blood mononuclear cells (PBMCs) at baseline and infected conditions. We note that the term “adaptive introgression” will be used in a broad sense, as our tests do not allow us to determine the exact timing when selection started to act on the Neanderthal alleles.
Mendez et al.  previously reported evidence of archaic introgression at the OAS locus. We first verified these results, using data from phase 3 of the 1000 Genomes Project , by examining the relationships of all modern human sequences at the OAS locus with the Altai Neandertal, Denisovan, and an inferred ancestral sequence. Clustering the human haplotypes resulted in 10 consensus sequences representing human haplotype clusters, which we combined with the archaic sequences in a neighbor-joining tree (Fig. 1a; see “Methods”). This tree confirms that the Denisovan haplotype is not present in the population samples represented in the 1000 Genomes Project dataset. In contrast, the Neandertal haplotype is found at relatively high frequencies outside of Africa, reaching highest frequencies in European population samples (up to 43 uc, Fig. 1b). Additionally, we corroborate the finding of Mendez et al.  that Neandertal-like haplotypes in the OAS region are too long to have resulted from incomplete lineage sorting (ILS) (P ≤ 2 × 10−3; see “Methods”).
We next sought to examine the consistency of the simulation results described above using genetic data from a dataset of 230 ancient Eurasian individuals . Assuming neutrality, the expected frequency of an allele in contemporary European populations can be predicted as a linear combination of allele frequencies sampled from representative ancient populations that have contributed ancestry to present-day European populations in different proportions [26, 27] (see “Methods”). Using this approach, we calculated the expected allele frequency in four present-day European samples from the 1000 Genomes Project  at the 11 NLS falling within the bounds of the three OAS genes, based on the ancient allele frequencies estimated by Mathieson et al. To set up our null expectations we performed a similar analysis on a dataset of approximately 1 million SNPs scattered around the genome, generated by Mathieson et al. (by merging 213 ancient samples dated between 6500 and 300 BCE with sequencing data from four European samples from the 1000 Genomes Project). We found that the NLS at OAS are outliers in the genome with respect to deviations from ancient frequencies. More specifically, we found that the allele frequencies of 6/11 OAS SNPs tested in the OAS1–OAS3 region (those 6 SNPs fall within the block of SNPs with NLS frequency greater than 99% of neutral simulations) have increased above the frequency predicted by ancient Eurasian samples by more than 20%, significantly more than what we observed for other SNPs genome-wide with comparable present-day frequencies (lowest P = 0.00476, Fig. 2b, Additional file 2: Table S3). Our findings at this single locus are consistent with results from the genome-wide selection scan performed by Mathieson et al.  where the OAS region also showed evidence of selection (P < 10−7; Additional file 2: Table S3), even if it did not reach genome-wide significance after multiple test correction.
As an additional means of understanding whether Neandertal haplotypes at OAS are longer than would be expected if they had evolved neutrally, we followed up these empirical haplotype-based tests with a simulation approach using a simple test statistic, H D/A . This statistic (fully defined in “Methods”) compares pairwise haplotype homozygosity lengths within the set of haplotypes carrying a derived (Neandertal) allele and within those carrying the ancestral allele. We utilized the same demographic models described above for our frequency-based test to understand whether the haplotypes surrounding derived alleles at NLS are longer than expected under a neutral model, conditional on the map of recombination in the OAS region. Again, we found that several derived Neandertal-like alleles are associated with a haplotype that is significantly longer than observed in simulated loci and that these results were robust to a series of alternative simulation models tested, including the one-pulse and two-pulse models described above and two additional one-pulse models which varied the mutation and recombination rates (Fig. 3b, Additional file 2: Table S4). A caveat to this simulation-based approach is that the parameters of the true demographic history of Neandertal-modern human admixture remain uncertain. Therefore, comparisons of neutral demographic models of Neandertal introgression to tests of selection utilizing haplotype lengths, such as H D/A , are limited by the current state of demographic parameter estimates.
Finally, we calculated the levels of population differentiation between European and East Asian populations for all NLS in the OAS region. Interestingly, we found extreme levels of differentiation for most NLS (Fst as high as 0.6, P empirical < 0.01, Fig. 3c. Additional file 2: Table S5), except within the genomic region covering OAS1 and part of OAS3. These results suggest that NLS surrounding OAS1 have been positively selected in both European and East Asian populations but that distinct haplotypes, possibly recombinant forms of an original introgressed Neandertal haplotype, have been selected in Europe and Asia.
In addition to overall changes in expression, we took advantage of the power of RNA-seq data to test if NLS in the OAS regions influenced the ratio of alternative isoforms used for each of the OAS genes (i.e. alternative splicing QTL: asQTL). We found that SNPs associated with the Neandertal haplotype are significant asQTL for OAS1 and OAS2 in both infected and non-infected macrophages (FDR < < 1%; Fig. 4b, c). The effect of the splice site variant rs10774671 at determining what isoform is primarily encoded by OAS1 was particularly strong (P ≤ 2 × 10−32). This SNP is also a strong asQTL and protein QTL in lymphoblastoid cell lines [34, 35]. The ancestral G allele at this SNP (AG at acceptor site) retains the splice site whereas the derived allele, A, (AA at acceptor site) disrupts the splice site leading to the usage of a distinct isoform (Additional file 1: Figure S5). The Neandertal haplotype harbors the ancestral allele (encoding the p46 isoform), which is associated with high enzyme activity . Interestingly, despite the fact that this ancestral allele is found at ~ 60–70% in most sub-Saharan African populations, outside of Africa this allele is only found on individuals with the Neandertal haplotype (with rare exceptions; ~2% of all haplotypes; Additional file 1: Figure S6), suggesting that the Neandertal segment is effectively reintroducing an ancestral variant that was already present in other human groups. To validate that this SNP had the same impact at determining what OAS1 isoforms are expressed in African-descent individuals, we analyzed additional RNA-seq data collected from 41 African-American individuals. As among Europeans, rs10774671 is a strong asQTL for OAS1 in both non-infected and infected macrophages (P < 1 × 10−15; Additional file 1: Figure S7), despite laying in a non-Neandertal haplotype.
Because OAS genes are primarily involved in the control of viral infections, we decided to validate our functional findings on PBMCs from 40 individuals stimulated/infected with viral-ligands (polyI:C and gardiquimod) and live viruses (Influenza, Herpes simplex virus [HSV] 1, and HSV2). The individuals were chosen based on their genotype for the NLS rs1557866, a SNP that is a strong proxy for the presence or absence of the Neandertal haplotype in the OAS region (9 were homozygous for the Neandertal haplotype, 15 were heterozygous, and 16 homozygous for the modern human sequence).
The Neandertal lineage was present in Eurasia for at least 400,000 years , providing ample time for Neandertals to adapt to local disease environments. The admixture process, which likely fostered the transmission of pathogens between Neandertals and humans migrating out of Africa, could have also led to the exchange of genes useful in responding to local pathogens. Here, we have demonstrated that a previously reported case of Neandertal introgression at the OAS locus  displays population genetic signatures that are characteristic of positive selection in the European population. We note, however, that our results are limited by an incomplete knowledge of the demographic history of admixture between Neandertals and modern humans and the fact that the neutrality tests we used are not perfectly suited to detect adaptive introgression. Yet, we have strengthened the case for adaptive introgression by providing direct functional evidence of a role for the Neandertal OAS haplotype in the regulatory responses in innate immune cells to infectious agents.
Our results show that the Neandertal haplotype at OAS is associated with several regulatory variants that reduce expression of OAS3 in response to infection, as well as encode alternate isoforms of OAS1 and OAS2. These dramatic functional implications of the Neandertal OAS haplotype support our case for adaptive introgression at OAS. Yet, because distinct functional polymorphisms segregate together in the same haplotype, inferring the exact variant(s) targeted by positive selection remains a daunting task. We speculate, however, that one of the strongest direct targets of selection is likely to have been the splice variant identified in OAS1.
The Neandertal haplotype carries the ancestral allele (G) of the OAS1 splice variant (rs10774671), which is common both inside and outside of Africa. However, outside of Africa, the only haplotypes carrying this ancestral splice site are closely related to the Neandertal haplotype, with a few exceptions being rare recombined haplotypes (~2% of all haplotypes with the ancestral allele). This pattern reflects the possibility that Neandertal introgression, in effect, served as a means to resurrect the ancestral splice site from local extinction outside of Africa, probably following the out-of-Africa exodus. Interestingly, the same ancestral splice site is found in the Denosivan genome and may similarly have impacted adaptive introgression into the ancestors of Melanesians. While we cannot at present confirm that the ancestral splice site was missing from the ancestral Eurasian population, the presence of this allele only on the Neandertal haplotype hints at the possibility that this splice site was lost to drift and subsequently re-introduced by Neandertals, providing beneficial genetic variation at the OAS locus (Additional file 1: Figure S6). The Neandertal-introgressed allele encodes a protein variant (p46) that is associated with higher enzymatic activity . The adaptive potential of this variant is supported by the observation that this variant (or other variants in strong LD with it) was shown to be associated with: (1) reduced infection and replication rates of West Nile virus (, but see ); (2) improved resistance to hepatitis C virus (HCV) infection [40, 41]; and (3) variable symptomology of tick-borne encephalitis (TBE) virus-induced disease (homozygous individuals for the Neandertal haplotype show the most severe symptoms of TBE). Strikingly, West Nile, hepatitis C, and TBE are all members of the Flaviviridae family, suggesting that Flaviviruses might have been the main drivers of selection in OAS1.
The differential responses of homozygous carriers of the Neandertal OAS haplotype to the different viruses described above suggest that the Neandertal haplotype is not uniformly beneficial in humans. Thus, it is plausible that both spatial and temporal fluctuations in virus populations could have led to fluctuating selection pressure on the Neandertal OAS haplotype, consistent with findings that genes in the immune system have been disproportionately targeted by positive selection since the dawn of agriculture .
Alternatively, and not mutually exclusively, alleles at OAS, and particularly the OAS1 splice variant, might be evolving under balancing selection. This hypothesis is supported by the observation that the OAS1 splice variant (rs10774671) is found at high frequency worldwide (0.11–0.7) and the significantly higher Tajima’s D values observed around OAS1, as compared to genome-wide expectations (Fig. 3d). Moreover, OAS1 is among the most diverse genes in both humans and non-human primates. Indeed, a recent analysis of genome-wide sequence data from a total of 55 individuals from four non-human ape species, chimpanzee (Pan troglodytes ellioti), bonobo (Pan paniscus), gorilla (Gorilla gorilla gorilla), and orangutan (Pongo abelii), identified OAS1 as in the top 1% of genes showing the largest levels of nucleotide diversity among ape species , consistent with a scenario of long-term balancing selection (OAS2 and OAS3 are ranked in the 60th and 36th percentile of the genome-wide distribution, respectively) or, as previous research has suggested, rapid evolution across the primate order . Further supporting the idea of balancing selection on the introgressed haplotype, our functional data suggest that the Neandertal haplotype contributes a range of gene expression responses in a cell-type and stimulus-specific manner.
Estimates of historical allele frequencies at the OAS locus, from ancient DNA samples dated between roughly 8500 and 2500 years ago, support the notion that the Neandertal haplotype did not follow a classic selective sweep model with constant directional selection. Under such a model, the observed present-day frequency of the Neandertal haplotype at the OAS locus of roughly 38% would suggest a codominant fitness effect of s ~ 0.0014–0.0017, when assuming an initial frequency of 0.02 at introgression approximately 2000–2400 generations ago (see “Methods”). However, the observed allele frequency shift of 0.26 over the past 200–340 generations (maximum shift in CEU from ancient samples; see Fig. 2b) suggests that the selection coefficient associated with the Neandertal haplotype during this recent human evolution would have been s ~ 0.0044–0.0075: 2.6–5.4 times larger than the above estimate. Therefore, both temporally varying selection and balancing selection could explain why the Neandertal haplotype at OAS did not show clear signatures of adaptive introgression in previous studies [15, 18].
Our study illustrates the difficulty of identifying strong candidates for adaptive introgression. In a genome-wide statistical framework, our use of neutral coalescent simulations as a null distribution for adaptive introgression likely would not have provided significant results after multiple test correction across loci. This suggests that other instances of less obvious adaptive introgression, especially those that did not follow a classic selective sweep model, may remain to be identified. Moving forward, novel methods must be developed to identify such cases. Some progress is now being made on this front. For example, Racimo et al.  recently developed a genome-wide statistical framework which relies on distributions of uniquely shared derived alleles between humans and Neandertals (as does our study) to identify candidate regions for adaptive introgression. This study also highlighted the OAS locus as a candidate for adaptive introgression. Additionally, estimates of historical allele frequencies with increased spatial and temporal resolution provided by the sequencing of ancient human genomes are likely to play an important role in illuminating candidates for adaptive introgression which do not conform to classical selective sweep models.
In conclusion, our study demonstrates that the frequency and haplotype distribution of Neandertal-like sites can be used in a neutral simulation framework that accounts for local genomic context to investigate the history of selection at a candidate locus for which genome-wide tests of selection provide ambiguous results. When combined with functional data, our results provide the strongest evidence to date in support of adaptive introgression in the OAS region. More generally, our study raises the possibility that adaptive introgression might not necessarily occur to select newly introduced variants but rather as a means to resurrect adaptive variation in modern human populations that had been lost due to demographic events.
Genome alignments and identification of Neandertal-like sites
Human/chimpanzee ancestral states were computed by parsimony using alignments from the UCSC Genome Browser for the human reference (hg19) and three outgroups chimpanzee (panTro2), orangutan (ponAbe2), and rhesus macaque (rheMac2) . Ancestral state was assumed to be the chimpanzee allele (if available) if its state was confirmed by matching either orangutan or macaque. All sites with no inferred ancestral state were removed from our analysis.
We filtered the Altai Neandertal genome  and Denisovan genome  using the map35_50 set of minimum filters provided at (https://bioinf.eva.mpg.de/altai_minimal_filters/). For the frequency analysis, we combined these filtered datasets with 10 samples from outside of Africa (5-Eur European: CEU, FIN, GBR, IBS, TSI; 5-East Asian: CDX, CHB, CHS, JPT, KHB; see Additional file 2: Table S7 for population codes) and one sub-Saharan African sample YRI (Yoruba in Ibadan, Nigeria) from the 1000 Genomes Project Phase 3 , which we downloaded from (https://mathgen.stats.ox.ac.uk/impute/1000GP%20Phase%203%20haplotypes%206%20October%202014.html).
We first extracted all bi-allelic variants in our human, Neandertal, and chimpanzee alignments. We considered as NLS only those variants where the African sample (YRI) had a derived allele frequency of zero and both the non-African sample and Neandertal carried the derived allele. We restricted the follow-up haplotype-based analysis to only the CEU sample. In that analysis, we required the derived allele to be present in CEU in at least two copies in order to calculate our haplotype-based test statistic (H D/A ).
Haplotype clustering in the 1000 Genomes Project data
To assess the relationships and frequencies of Neandertal-like haplotypes in the OAS region, we identified haplotype clusters based on sequence similarity. First, we filtered all 5008 haplotypes in the 1000 Genomes Project phase 3 dataset to include only SNPs within the bounds of the three OAS genes (hg19 chr12: 113344739–113449528) and at which the Altai Neandertal  and Denisovan  genomes carry homozygous genotypes. Next, we clustered the human haplotypes such that all haplotypes in a cluster had no more than 60 pairwise differences, which resulted in 10 clusters. We inferred a consensus haplotype for each cluster based on the majority allele at each position in the cluster. Finally, we produced a neighbor-joining tree of the human cluster consensus sequences and the Altai, Denisovan, and ancestral sequences using the R package “ape.” We estimated confidence values for nodes with 1000 bootstraps.
We then calculated haplotype frequencies for each of the 1000 Genomes Project population samples based on the assignment of each haplotype to the clusters described above.
Demographic model and neutral coalescent simulations
We performed coalescent simulations of the demographic history of the European, East Asian, African, and Neandertal populations applied by Vernot and Akey  based on previously inferred demographic models [23, 24]. In our first set of simulations, which were performed with ms , we extracted only allele frequencies at NLS. We gathered a total of 1 million simulation results. In each simulation run, a result was collected if a NLS was present in either the European or the East Asian population sample (or both). Therefore, null distributions specific to Europeans or East Asians included less than 1 million results (but typically > 800,000). Haplotype simulations were performed with macs  in order to explicitly simulate the genetic map (downloaded with the 1000 Genomes samples at the link above) of the 600 kb region centered on OAS (chr12:113100000–113700000). The general shape of the demographic model is illustrated in Additional file 1: Figure S1. Our baseline simulations were performed with the parameters specified in Additional file 2: Table S1, assuming 25 years per generation and a mutation rate of 2.5 × 10−8 per bp per generation. Additional file 2: Table S1 also provides all parameters used in one-introgression and two-introgression pulse simulations. Additionally, we examined the one-pulse model with a slower mutation rate (1.25 × 10−8) and a one-pulse model with a uniform recombination rate (1.3 × 10−8; a value conservatively lower than the average for the OAS region, 1.7 × 10−8). Sample ms and macs commands are given at the end of this section.
For haplotype-based simulations, data were thinned in a manner similar to Sankararaman et al.  to account for imperfect SNP ascertainment in the 1000 Genomes dataset, such that SNPs with minor allele count of 1, 2, 3, 4, 5, 6, 7, 8, 9, and > =10 were accepted with probabilities 0.25, 0.5, 0.75, 0.8, 0.9, 0.95, 0.96, 0.97, 0.98, and 0.99, respectively. Additionally, we only kept SNPs that were polymorphic in the simulated CEU sample. Finally, we performed an additional thinning of SNPs with uniform probability of 0.05 of removal to account for slightly elevated SNP density in the simulated data. The resulting simulated datasets had an average SNP density of 3.8 SNPs per kb compared to 2.5 in the real data. This is a slightly larger than ideal difference in SNP density, but we note that neither derived allele frequency nor our primary haplotype-based test statistic (described below) should be particularly sensitive to SNP density. In fact, Additional file 1: Figure S9 illustrates that our statistic is conservative with respect to SNP density. Additionally, our results hold in a simulation with half the mutation rate of our baseline simulation. This simulation resulted in an average SNP density of 1.9 SNPs per kb. So our observation of long haplotypes surrounding NLS is robust to SNP density across our simulations.
Sample ms command:
ms 752 1 -s 1 -I 4 250 250 250 2 0 -n 1 58.0027359781 -n 2 70.0410396717 -n 3 187.549931601 -n 4 0.205198358413 -eg 0 1 482.67144247 -eg 0 2 505.592963281 -eg 0 3 720.224280773 -em 0 1 2 0.358619661426 -em 0 2 1 0.358619661426 -em 0 1 3 0.111889334365 -em 0 3 1 0.111889334365 -em 0 2 3 0.446122858814 -em 0 3 2 0.446122858814 -en 0.00699726402189 1 1.98002735978 -eg 0.00699726402189 2 0.0 -eg 0.00699726402189 3 17.5076517287 -en 0.03146374829 2 2.03666547538 -en 0.03146374829 3 0.700185007205 -ej 0.0641347992705 3 2 -em 0.0641347992705 1 2 0.00015 -em 0.0641347992705 2 1 0.00015 -em 0.0839811779742 2 4 0.00075 -em 0.0846651725023 2 4 0 -ej 0.0957592339261 2 1 -en 0.202462380301 1 1.0 -ej 0.957592339261 4 1.
Sample macs command:
macs 416 600000 -t 0.000731 -R oas_recrates.txt -I 4 216 198 0 2 0 -n 1 58.0027359781 -n 2 70.0410396717 -n 3 187.549931601 -n 4 0.205198358413 -eg 0 1 482.67144247 -eg 1e-12 2 460.409556336 -eg 2e-12 3 720.224280773 -em 3e-12 1 2 0.4441436762 -em 4e-12 2 1 0.4441436762 -em 5e-12 1 3 0.138572826974 -em 6e-12 3 1 0.138572826974 -em 7e-12 2 3 0.552514733193 -em 8e-12 3 2 0.552514733193 -en 0.00699726402189 1 1.98002735978 -eg 0.00699727402189 2 0.0 -eg 0.00699728402189 3 18.896348561 -en 0.03146374829 2 2.79399962717 -en 0.03146375829 3 0.670250141711 -ej 0.051785044418 3 2 -em 0.051785054418 1 2 0.00015 -em 0.051785064418 2 1 0.00015 -em 0.0555806720117 2 4 0.00075 -em 0.0562646665398 2 4 0 -ej 0.0957592339261 2 1 -en 0.202462380301 1 1.0 -ej 0.957592339261 4 1 -h 1e3.
Frequency and haplotype-based tests of neutrality using simulations
We examined the consistency of genetic variation with our neutral model using several approaches. First, we examined the likelihood of observing (Neandertal) allele frequencies as high as the OAS locus. Under neutrality, allele frequency is not dependent upon recombination rate; therefore, we can estimate the likelihood of our observed NLS frequency in the OAS region. To create a distribution of expected NLS frequency in each introgression model, we first extracted derived allele counts (DAC) at simulated NLS for samples of 250 individuals each for Europeans and East Asians in the simulated model. Next, for each non-African population sample from the 1000 Genomes Project, we binomially sampled the DACs from the appropriate simulated population (European for CEU, GBR, IBS, TSI; East Asian for CDX, CHB, CHS, JPT, KHV) using the true population sample size to create a distribution of NLS frequencies that is specific to each population sample (Fig. 2a, Additional file 1: Figure S3). Minimum P values across the OAS locus for each population are listed in Additional file 2: Table S2.
Additionally, we wanted to examine if the haplotypes carrying NLS at the OAS locus are longer than expected under neutrality when conditioning on the observed frequencies and the underlying genetic map, which would provide an additional signature of selection on introgressed haplotypes beyond empirical haplotype signatures. For this purpose, we modified a simple haplotype statistic H , which measures the average length of pairwise homozygosity tracts in base pairs—a quantity that is very straightforward to interpret. As selective sweeps are expected to create long haplotypes around the selected site, the H statistic should be higher in samples containing positively selected haplotypes compared to samples containing neutrally evolving haplotypes, when frequency and recombination are properly controlled, similar to other statistics based on haplotype lengths, such as EHH, iHS, and nSL [28, 30, 49]. However, in contrast to these other statistics, H does not require specification of analysis parameters such as minimum haplotype homozygosity levels below which haplotypes are no longer extended.
where H D and H A are H calculated across haplotypes carrying derived NLS allele versus the ancestral allele (see Additional file 1: Figure S10).
For each model we generated 1000 simulated OAS regions containing NLS that reach a frequency greater than the 99th percentile for CEU in our frequency simulations. We calculated H D/A for every simulated NLS and for every NLS in our true sample. We then compared our simulation results to the observed data in two ways. First, to visually examine the distribution of true H D/A values to neutral simulations, we took the mean H D/A score across all NLS in each of 1000 simulations and calculated the 95th and 99th percentiles of those 1000 simulations (Fig. 3b). Second, to examine the probability under neutrality of the observed H D/A values at the peak of H D/A between chr12:113380000–113420000, we compared the mean H D/A score for SNPs in this window to the mean of SNPs in this window for each simulation that produced a NLS in that window. These results for all tested models are listed in Additional file 2: Table S4.
Analysis of ancient Eurasian data
We utilized supplementary data Table 3 from Mathieson et al. . This table includes maximum likelihood allele frequency estimates for three ancient population samples (HG: hunter-gatherer, EF: early farmer, SA: Steppe ancestry) and four present-day European samples from the 1000 Genomes Project (see the “Genome-wide scan for selection” section of methods in ). We intersect this table with allele frequencies for 1000 Genomes Yorubans (YRI) and the Altai Neandertal genotypes and only analyze sites for which we have data for all samples (1,004,612 SNPs).
Next, we calculated the absolute difference between observed and expected allele frequency in all four present-day European samples at all available sites. To test the null hypothesis that OAS NLS have not changed in frequency more than expected under neutrality at 11 SNPs in the central OAS region (chr12:113200000–113600000), we first calculated the fraction of all autosomal SNPs in the dataset at similar present-day frequency (within 1% in the folded frequency spectrum) of each OAS NLS. Finally, we calculated the fraction of autosomal SNPs with an absolute observed minus expected frequency difference greater than or equal to the OAS NLS. These results are given in Additional file 2: Table S3 and illustrated in Fig. 2b.
This test does not explicitly incorporate variance in estimated ancient allele frequency. However, any bias in ancient allele frequency estimation should be distributed randomly across the genome. Therefore, our comparison to a genome-wide distribution of SNPs at similar present-day frequency should incorporate most of this error. Nonetheless, the selection test performed by Mathieson et al.  does incorporate such error, so we can also look to the Ps from that test to ensure consistency with our results.
Estimation of selection coefficients
This equation can be easily solved to obtain s, given x 0 , x 1 , and Δt.
Probabilities that Neandertal haplotypes are shared due to incomplete lineage sorting
where L is the expected shared length, L = 1/(r × t) where r is recombination rate and t is time in generations.
We first estimated the maximum haplotype length observed in each of the 1000 Genomes Project population samples by identifying tracts of identity-by-state (IBS) that include NLS between the Altai Neandertal haplotype (considering only homozygous positions) and individual human haplotypes. We identified all tracts of IBS bounded by NLS (using YRI as the African reference) and took the maximum of these per-population sample IBS distributions.
We identified the maximum tract length (198,441 bp) in European (and some admixed Native American) samples. Maximum tract length for East Asian samples (54,385 bp) is notably shorter. As expected, no IBS tracts were identified in African population samples.
Assuming a conservatively low recombination rate for the OAS region (1.3 × 10−8) and a conservatively short divergence between Neandertals and humans of 300,000 years (and 25 years per generation), the probability of a length of at least 54,385 is P(54,385) = 0.002. The probability of the longest tracts is much smaller, P(198,441) = 1.15 × 10−12. Therefore, it is unlikely that Neandertal haplotypes are shared with non-Africans due to shared ancestral variation.
We repeated this analysis using the Denisovan genome and found no IBS tracts defined by Denisovan-like sites, suggesting that introgressed Denisovan haplotypes described by Mendez et al.  are not present in the 1000 Genomes Project Samples, consistent with our findings in Fig. 1a.
Neutrality tests in phase 3 of the 1000 Genomes data
We calculated iHS, DIND, Fst, and Tajima’s D on different populations from phase 3 of the 1000 Genomes project. The phased data were downloaded from Impute reference data panel (https://mathgen.stats.ox.ac.uk/impute/1000GP_Phase3.html) and were filtered for bi-allelic SNPs. Arlequin version 22.214.171.124  was then used to calculate Fst estimates derived from ANOVA among all pairs of European and Asian populations. DIND was calculated as previously described  and Tajima’s D was calculated for all SNPs using a window of 25 kb either side of each SNP (i.e. in window of 50 kb in total). iHS values were recovered from a genomic scan performed using hapbin  on the same phase 3 release of the 1000 Genomes dataset.
Buffy coats from 96 healthy European American donors and 41 African Americans were obtained from Indiana Blood Center (Indianapolis, IN, USA). Only individuals self-reported as currently healthy and not under medication were included in the study. The individuals recruited in this study were men aged 18–55 years old. For 80% of our samples, we have information on their exact age (for the remaining 20% of donors we only know that they were adults aged less than 55 years) and we found no association between the presence of the Neandertal haplotype (as measure by rs1557866) and age (P > 0.5). Thus, variation in age is not likely impact any of our conclusions. In addition to self-identified ancestry labels, we used the genome-wide genotype data (see the “DNA extraction and genotyping” section) to estimate genome-wide levels of European and African ancestry in each sample using the program ADMIXTURE . Consistent with previous reports, we found that self-identified European Americans showed limited levels of African admixture (mean = 0.4%, range 0–13%). The African Americans used in our study were selected on having at least 75% of African ancestry.
DNA extraction and genotyping
DNA from each of the blood donors was extracted using the Gentra Pure Gene blood kit (Qiagen). Genotyping of each individual was then performed by Illumina’s HumanOmni5Exome bead Chip array and complemented with imputed data from the 1000 Genomes data using Impute2 . Here, we only focused on genetic diversity surrounding the OAS region – chr12:113229549–113574044 (~344 kb) spanning from the beginning of RPH3A to the end of RASAL1—for a total of 673 SNPs with a MAF above 10%. Genotypes can be found in Additional file 2: Table S8.
Isolation of monocytes and differentiation of macrophages
Blood mononuclear cells were isolated by Ficoll-Paque centrifugation. Monocytes were purified from PBMCs by positive selection with magnetic CD14 MicroBeads (Miltenyi Biotech) using the autoMACS Pro Separator. All samples had purity levels above 90%, as measured by flow cytometry using an antibody against CD14 (BD Biosciences). Monocytes were then cultured for seven days in RPMI-1640 (Fisher) supplemented with 10% heat-inactivated FBS (FBS premium, US origin, Wisent), L-glutamine (Fisher), and M-CSF (20 ng/mL; R&D systems). Cell cultures were fed every two days with complete medium supplemented with the cytokines previously mentioned. Before infection, we systematically verified that the differentiated macrophages presented the expected phenotype for non-activated macrophages (CD1a+, CD14+, CD83−, and HLA-DRlow (BD Biosciences)).
Bacterial preparation and infection of macrophages
The day prior to infection, aliquots of Salmonella typhimurium (Keller strain) were thawed and bacteria were grown overnight in Tryptic Soy Broth (TSB) medium. Bacterial culture was diluted to mid-log phase prior to infection and supernatant density was checked at OD600. Monocyte-derived macrophages were then infected with S. typhimurium at a multiplicity of infection (MOI) of 10:1. A control group of non-infected macrophages was treated the same way but using medium without bacteria. After 2 h in contact with the bacteria, macrophages were washed and cultured for another hour in the presence of 50 mg/mL of gentamycin in order to kill all extracellular bacteria present in the medium. The cells were then washed a second time and cultured in complete medium with 3 mg/mL gentamycin for an additional 2 h, the time point to which we refer in the main text.
Infection/stimulation of PBMC
PBMCs from a subset of 40 individuals used to derive macrophages were cultured in RPMI-1640 (Fisher) supplemented with 10% heat-inactivated FBS (FBS premium, US origin, Wisent) and 1% L-glutamine (Fisher). The 30 individuals were chosen based on their genotype for rs1557866, a SNP which derived allele is of Neandertal origin and that we used as a proxy to identify individuals harboring the Neandertal haplotype in the OAS region. From the 40 individuals, and based on this SNP, nine individuals were homozygous for the Neandertal haplotype, 15 were heterozygous, and 16 homozygous for the modern human sequence.
For each of the tested individuals, PBMCs (1 million per condition) were stimulated/infected with one of the following viral-associated immune challenges: polyI:C (10 μg/mL, TLR3 agonist), Gardiquimod (0.5 μg/mL, TLR7 and TLR8 agonist), Influenza PR8 WT (multiplicity of infection (MOI) of 0.05:1), HSV 1 (1.55 × 102 CPE), and HSV2 (19.5 × 104 CPE). PBMCs were stimulated/infected for 4 h with TLR ligands and Influenza and 6 h with HSV1 and HSV2. A control group of non-infected PBMC was treated the same way but with only medium.
RNA extraction, RNA-seq library preparation, and sequencing
Total RNA was extracted from the non-infected and infected/stimulated cells using the miRNeasy kit (Qiagen). RNA quantity was evaluated spectrophotometrically and the quality was assessed with the Agilent 2100 Bioanalyzer (Agilent Technologies). Only samples with no evidence of RNA degradation (RNA integrity number > 8) were kept for further experiments. RNA-seq libraries were prepared using the Illumina TruSeq protocol. Once prepared, indexed complementary DNA (cDNA) libraries were pooled (6 libraries per pool) in equimolar amounts and sequenced with single-end 100 bp reads on an Illumina HiSeq2500. Results based on the entire dataset are described elsewhere . Here, we only studied transcript-level and gene-level expression estimates for OAS1, OAS2, and OAS3. The transcript-level and gene-level expression data for these genes can be found in Additional file 2: Table S9.
Quantifying gene expression values from RNA-seq data
Adaptor sequences and low quality score bases (Phred score < 20) were first trimmed using Trim Galore (version 0.2.7). The resulting reads were then mapped to the human genome reference sequence (Ensembl GRCh37 release 65) using TopHat (version 2.0.6) and using a hg19 transcript annotation database downloaded from UCSC. Gene-level expression estimates were calculated using featureCounts (version 1.4.6-p3) and transcript-level expression values were obtained using RSEM under default parameters.
Quantitative real-time PCR
For the PBMC samples, we measured the expression levels of OAS and interferon genes using real-time PCR. A total of 100 ng of high-quality RNA was reverse-transcribed into cDNA using the qScript cDNA SuperMix (Quanta Biosciences). Quantitative real-time PCR was performed using 96.96 Dynamic Array™ IFCs and the BioMark™ HD System from Fluidigm. For the TaqMan gene assays, we used the following TaqMan Gene Expression Assay (Applied BioSystems) to quantify the expression levels of interferon genes: IFNA1 (Hs03044218), IFNA6 (Hs00819627), and IFNG (Hs00989291). To quantify the overall expression levels of OAS genes, we used probes that capture all common isoforms of OAS1 (Hs00973635), OAS2 (Hs00942643), and OAS3 (Hs00196324). Custom-made probes were designed to specifically target the short-isoform of OAS2 (Forward Primer Sequence CTGCAGGAACCCGAACAGTT; Reverse Primer Sequence ACTCATGGCCTAGAGGTTGCA; Reporter Sequence AGAGAAAAGCCAAAGAA). As housekeeping genes, we used: GAPDH (Hs02758991), GUSB (Hs99999908), HPRT1 (Hs99999909), and POLR2A (Hs00172187). The results reported in the manuscript used POLR2A as a reference but all conclusions remain unchanged when using any of the other housekeeping genes.
We start by doing a preamplification of the cDNA using the PreAmp Master Mix (Fluidigm). Preamplified cDNA was then diluted 2× on a solution of 10 mM Tris–HCl (pH 8.0) and 0.1 mM EDTA. In order to prepare samples for loading into the integrated fluid circuit (IFC), a mix was prepared consisting of 360 μL TaqMan Fast Advanced Master Mix (Applied BioSystems) and 36 μL 20× GE Sample Loading Reagent (Fluidigm). A total of 2.75 μL of this mix was dispensed to each well of a 96-well assay plate and mixed with 2.25 μL of preamplified cDNA. Following priming of the IFC in the IFC Controller HX, 5 μL of the mixture of cDNA and loading reagent were dispensed in each of the sample inlet of the 96.96 IFC. For the TaqMan gene assays, 5 μL of mixes consisting of 2.5 μL 20× TaqMan Gene Expression Assay (Applied BioSystems) and 2.5 μL 2× Assay Loading Reagent (Fluidigm) were dispensed to each detector inlet of the 96.96 IFC. After loading the assays and samples into the IFC in the IFC Controller HX, the IFC was transferred to the BioMark HD and PCR was performed using the thermal protocol GE 96 × 96 Fast v1.pcl. This protocol consists of a Thermal Mix of 70 °C, 30 min; 25 °C, 10 min, Hot Start at 95 °C, 1 min, PCR Cycle of 35 cycles of (96 °C, 5 s; 60 °C, 20 s). Data were analyzed using Fluidigm Real-Time PCR Analysis software using the Linear (Derivative) Baseline Correction Method and the Auto (Detectors) Ct Threshold Method.
To quantify the expression levels of the OAS1 isoform associated with the derived allele at the splicing variant rs10774671, we used SybrGreen and the following forward (GCTGAGGCCTGGCTGAATTA) and reverse (CCACTTGTTAGCTGATGTCCTTGA) primers. PCR was performed using the thermal protocol 50 °C, 2 min; 95 °C, 10 min, PCR cycle of 40 cycles of (95 °C, 15 s; 60 °C, 1 min). A melting curve was also performed to check for non-specific amplification.
Genotype–phenotype association analysis
eQTL and asQTL were performed against OAS1, OAS2, and OAS3. We examined associations between SNP genotypes and the phenotype of interest using a linear regression model, in which phenotype was regressed against genotype. In particular, expression levels were considered as the phenotype when searching for eQTL and the percentage usage of each isoform in each gene when mapping asQTL. To avoid low power caused by rare variants, only SNPs in the OAS region with a minor allele frequency of 10% across all individuals were tested (i.e. 673 SNPs within the region chr12:113229549–113574044). In all cases, we assumed that alleles affected the phenotype in an additive manner. For the eQTL and asQTL analyses on macrophages, we mapped Salmonella-infected and non-infected samples separately. We controlled for FDRs using an approach analogous to that of Storey and Tibshirani , which makes no explicit distributional assumption for the null model but instead derives it empirically null from permutation tests, where expression levels were permuted 1000 times across individuals. For the non-infected and infected/stimulated PBMCs we only tested expression levels against the SNPs identified as eQTL or asQTL in the macrophage data (specifically, the SNPs for which boxplots are shown in Fig. 4).
We thank all members from the Barreiro and Messer labs for helpful discussions and comments on the manuscript. We thank Dr. Silvia Vidal for the gift of the Influenza PR8 WT used in this study, Dr. Hugo Soudeyns and Doris Ransy for advice with the viral infections, and Marc Montero and George (PJ) Perry for sharing their analysis on nucleotide diversity levels of OAS genes in non-human primate species.
This study was funded by grants from the Canadian Institutes of Health Research (301538 and 232519), the Human Frontiers Science Program (CDA-00025/2012), and the Canada Research Chairs Program (950–228993) (to LBB). YN was supported by a fellowship from the Réseau de Médecine Génétique Appliquée (RMGA).
Availability of data and materials
The datasets supporting the conclusions of this article are included within the article and in Additional file 2 : Tables S8 and S9. The raw data were deposited under GEO accession numbers GSE73765 and GSE81046.
Conception and design: AJS, PWM, LBB; acquisition of data: AJS, AD, YN, VY, LBB; analysis and interpretation of data: AJS, AD, YN, PWM, LBB; contributed unpublished, essential data, or reagents: CA, JET; drafting or revising the article: AJS, PWM, LBB. All authors read and approved the final manuscript.
The authors declare that they have no competing interests.
Ethics approval and consent to participate
Institutional ethics (IRB) approval was obtained by the CHU Sainte-Justine Institutional Review Board (approved project #3557) and all subjects gave written informed consent prior to participation. Experimental methods comply with the Declaration of Helsinki.
Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated.
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