Temporal genomic data hold great potential for studying evolutionary processes such as speciation. However, sampling across speciation events would, in many cases, require genomic time series that stretch well back into the Early Pleistocene subepoch. Although theoretical models suggest that DNA should survive on this timescale1, the oldest genomic data recovered so far are from a horse specimen dated to 780–560 thousand years ago2. Here we report the recovery of genome-wide data from three mammoth specimens dating to the Early and Middle Pleistocene subepochs, two of which are more than one million years old. We find that two distinct mammoth lineages were present in eastern Siberia during the Early Pleistocene. One of these lineages gave rise to the woolly mammoth and the other represents a previously unrecognized lineage that was ancestral to the first mammoths to colonize North America. Our analyses reveal that the Columbian mammoth of North America traces its ancestry to a Middle Pleistocene hybridization between these two lineages, with roughly equal admixture proportions. Finally, we show that the majority of protein-coding changes associated with cold adaptation in woolly mammoths were already present one million years ago. These findings highlight the potential of deep-time palaeogenomics to expand our understanding of speciation and long-term adaptive evolution.
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All sequence data (in .fastq format) for samples sequenced in this study are available through the European Nucleotide Archive under accession number PRJEB42269. Previously published data used in this study are available under accession numbers PRJEB24361 and PRJEB7929.
The custom code used in this study to evaluate read length cut-offs is available from GitHub (https://github.com/stefaniehartmann/readLengthCutoff).
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T.v.d.V., P.P., D.D.-d.-M., M.D. and L.D. acknowledge support from the Swedish Research Council (2012-3869 and 2017-04647), FORMAS (2018-01640) and the Tryggers Foundation (CTS 17:109). A.G. is supported by the Knut and Alice Wallenberg Foundation (1,000 Ancient Genomes project). A.B. and P.S. were supported by the Francis Crick Institute (FC001595), which receives its core funding from Cancer Research UK, the UK Medical Research Council and the Wellcome Trust. P.S. was supported by the European Research Council (grant no. 852558), the Wellcome Trust (217223/Z/19/Z) and the Vallee Foundation. M.H., J.A.T., I.B., A.M.L. and G.X. were supported by NERC (grant no. NE/J010480/1) and the ERC StG grant GeneFlow (no. 310763). B.S. and J.O. were supported by the US National Science Foundation (DEB-1754451). P.N. was supported by RFBR (grant no. 13-05-01128). The authors also acknowledge support from Science for Life Laboratory, the Knut and Alice Wallenberg Foundation, the National Genomics Infrastructure funded by the Swedish Research Council, and Uppsala Multidisciplinary Center for Advanced Computational Science for assistance with massively parallel sequencing and access to the UPPMAX computational infrastructure. N. Clark at the Hunterian Museum provided access to the Scotland mammoth sample. Finally, we thank our late friend and colleague A. Sher, who defined and described the Olyorian sequence, collected large quantities of fossil vertebrate material (including all of the Early and Middle Pleistocene specimens studied here) and consistently promoted multidisciplinary studies on his finds.
The authors declare no competing interests.
Peer review information Nature thanks Gloria Cuenca-Bescós, David Lambert, Krishna Veeramah and the other, anonymous, reviewer(s) for their contribution to the peer review of this work.
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Extended data figures and tables
a, b, Upper third molars in lateral and cross-sectional views. c, Partial lower third molar in lateral and occlusal views. a, Chukochya (accession number PIN 3341-737). b, Krestovka (accession number PIN 3491-3) flipped horizontally. c, Adycha (accession number PIN 3723-511), occlusal view flipped horizontally. The lamellae are more closely spaced, and the enamel is thinner, in a (M. primigenius-like) than in b, c (M. trogontherii-like). d, Hypsodonty index versus lamellar length index of upper M3. e, Enamel thickness index versus basal lamellar length index of lower M3. Olyorian specimens that yielded DNA are labelled by site name. Green dashed line, convex hull summarizing Early to early Middle Pleistocene (about 1.5–0.5 Ma) North American Mammuthus samples (data points not shown). Green and blue squares, Early and Late Olyorian northeastern Siberian samples, respectively. Red and green circles, European M. meridionalis and M. trogontherii, respectively. Blue circles, M. primigenius from northeastern Siberia and Alaska. Note (i) the similarity of Krestovka and Adycha to other molars from the Early Olyorian, and to European steppe mammoths (M. trogontherii); (ii) the similarity of early North American mammoths to these (to molars of the Early Olyorian, in particular); and (iii) the similarity of Chukochya to M. primigenius. For site details, measurement definitions and data, see Supplementary Information section 1.
Extended Data Fig. 2 Sample age on the basis of biostratigraphy, palaeomagnetic reversals and genomic data.
Chart shows the stratigraphic position of the Kutuyakhian fauna, Phenacomys complex, and Early Olyorian and Late Olyorian faunas in relation to important European, northwest Asian and northern North American stratigraphic benchmarks. ELMA, European land mammal ages (small mammals); LMA, land mammal ages (large mammals); MN and MQ, European small mammal biozones; EEBU, East European biochronological units. Biostratigraphic- and palaeomagnetic-based chronological constraints for the specimens are provided, in comparison with the DNA-based age estimations.
Reads are aligned to the LoxAfr4 autosomes. For the three Early and Middle Pleistocene samples (Krestovka, Adycha and Chukochya), reads of 25–200-bp length are shown; 30–200-bp reads are shown for the remaining samples. Ultrashort reads (<35 bp) are denoted in red; these were shown to be enriched for spurious alignments, and therefore excluded from downstream analyses (Supplementary Information section 4). The mean read lengths (μ) were calculated using only the retained reads (≥35 bp).
The most ancient samples (Krestovka, Adycha and Chukochya) carry a greater frequency of cytosine deamination compared to younger permafrost-preserved woolly mammoth samples (Oimyakon and Wrangel) and the Columbian mammoth (M. columbi) specimen.
The statistics reflect relative divergence between the genomes on the left and the right side. Lower values indicate reduced derived allele-sharing between the sample indicated on the left and the right of the graph, at sites for which the genome on the right panel is heterozygous. The lower the value, the more drift has occurred between the genomes (and thus the older their genetic divergence).
The most parsimonious graph model (highest Bayes factor) of the phylogenetic relationships among mammoth lineages augmented with one admixture event. Branch lengths are given in f-statistic units multiplied by 1,000. Discontinuous lines show admixture events between lineages, and percentages represent admixture proportions.
a, The number of private alleles per 1,000 bp within genomic regions identified as woolly mammoth (M. primigenius) ancestry or ghost ancestry. b, Maximum-likelihood phylogenies for those genomic regions identified as ghost ancestry in the Colombian mammoth (M. columbi) genome. c, Maximum-likelihood phylogenies for regions identified as unadmixed ancestry.
Detailed description of methods and additional results, containing information on sample morphology and stratigraphy, laboratory methods for DNA extraction and sequencing, sequence data processing, and DNA authenticity assessment. Further information on mitogenome reconstruction, DNA-based dating, genetic phylogenies, and admixture analysis (f4-statistics, AdmixtureGraphs, TreeMix and ghost admixture) is also provided.
These tables contain information on sequencing data, specifically the number of sequence reads generated, and mapping and post-mortem DNA damage statistics. We also list all used priors and obtained posteriors from the mitochondrial BEAST analysis, all pairwise f4-statistics, and a list of all coding changes comparing mammoths to elephants.
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van der Valk, T., Pečnerová, P., Díez-del-Molino, D. et al. Million-year-old DNA sheds light on the genomic history of mammoths. Nature 591, 265–269 (2021). https://doi.org/10.1038/s41586-021-03224-9
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