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Ancient DNA research in the past decade has revealed that European population structure changed dramatically in the prehistoric period (14,000–3000 years before present, YBP), reflecting the widespread introduction of Neolithic farmer and Bronze Age Steppe ancestries. However, little is known about how population structure changed from the historical period onward (3000 YBP - present). To address this, we collected whole genomes from 204 individuals from Europe and the Mediterranean, many of which are the first historical period genomes from their region (e.g. Armenia and France). We found that most regions show remarkable inter-individual heterogeneity. At least 7% of historical individuals carry ancestry uncommon in the region where they were sampled, some indicating cross-Mediterranean contacts. Despite this high level of mobility, overall population structure across western Eurasia is relatively stable through the historical period up to the present, mirroring geography. We show that, under standard population genetics models with local panmixia, the observed level of dispersal would lead to a collapse of population structure. Persistent population structure thus suggests a lower effective migration rate than indicated by the observed dispersal. We hypothesize that this phenomenon can be explained by extensive transient dispersal arising from drastically improved transportation networks and the Roman Empire’s mobilization of people for trade, labor, and military. This work highlights the utility of ancient DNA in elucidating finer scale human population dynamics in recent history.

Ancient Rome was the capital of an empire of ~70 million inhabitants, but little is known about the genetics of ancient Romans. Here we present 127 genomes from 29 archaeological sites in and around Rome, spanning the past 12,000 years. We observe two major prehistoric ancestry transitions: one with the introduction of farming and another prior to the Iron Age. By the founding of Rome, the genetic composition of the region approximated that of modern Mediterranean populations. During the Imperial period, Rome’s population received net immigration from the Near East, followed by an increase in genetic contributions from Europe. These ancestry shifts mirrored the geopolitical affiliations of Rome and were accompanied by marked interindividual diversity, reflecting gene flow from across the Mediterranean, Europe, and North Africa.

Contamination from both present-day humans and postmortem microbial sources is a common challenge in ancient DNA studies. Here we present a suite of tools to assist in the assessment of contamination in ancient DNA data sets. These tools perform standard tests of authenticity of ancient DNA data including detecting the presence of postmortem damage signatures in sequence alignments and quantifying the amount of present-day human contamination.

Denisova Cave is located in the Altai mountains of Russia. Excavations from this cave have yielded two large hominin molars and three hominin phalanxes from the Pleistocene. One of the phalanxes (Denisova 3) had extraordinary DNA preservation allowing the sequencing of high quality nuclear and mitochondrial DNA (mtDNA) genomes and has been shown to belong to a young girl from hereto unknown sister group of Neandertals, called Denisovans. The mtDNA of Denisova 3 surprisingly split from the mtDNA ancestor of modern humans and Neandertals twice as long ago as the split of modern humans and Neandertals. The mtDNA of one of the molars (Denisova 4) was also sequenced and differs at only two positions from the mtDNA of Denisova 3. A second phalanx (Altai 1) also yielded a high quality genome, and was a Neandertal. While Neandertals show an admixture signal of 1-4% into present-day non-Africans, Denisovans show an admixture of up to 5% in present-day Oceanians, and to a much lesser extent East Asians. This thesis encompasses two studies. In the first study, we sequenced the complete mtDNA genome of the additional molar (Denisova 8), as well as a few megabases of nuclear DNA from Denisova 4 and Denisova 8. While the mtDNA of Denisova 8 is clearly of the Denisova type, its branch to the most recent common ancestor of Denisovans is half as long as the branch leading to Denisova 3 or Denisova 4, indicating that Denisova 8 lived many millenia before the other two. Both Denisova 4 and 8 fall together with Denisova 3 based on nuclear DNA, bringing the number of known Denisovans from one to three. In the second study, we sequenced an almost complete mtDNA and a few megabases of nuclear DNA from the third hominin phalanx from Denisova Cave, Altai 2. Both the mtDNA and the nuclear DNA show Altai 2 to be a Neandertal. The mtDNA also showed the presence of substantial Pleistocene spotted hyena contamination. Low levels of spotted hyena contamination were also found in Altai 1, Denisova

Denisova Cave is located in the Altai mountains of Russia. Excavations from this cave have yielded two large hominin molars and three hominin phalanxes from the Pleistocene. One of the phalanxes (Denisova 3) had extraordinary DNA preservation allowing the sequencing of high quality nuclear and mitochondrial DNA (mtDNA) genomes and has been shown to belong to a young girl from hereto unknown sister group of Neandertals, called Denisovans. The mtDNA of Denisova 3 surprisingly split from the mtDNA ancestor of modern humans and Neandertals twice as long ago as the split of modern humans and Neandertals. The mtDNA of one of the molars (Denisova 4) was also sequenced and differs at only two positions from the mtDNA of Denisova 3. A second phalanx (Altai 1) also yielded a high quality genome, and was a Neandertal. While Neandertals show an admixture signal of 1-4% into present-day non-Africans, Denisovans show an admixture of up to 5% in present-day Oceanians, and to a much lesser extent East Asians. This thesis encompasses two studies. In the first study, we sequenced the complete mtDNA genome of the additional molar (Denisova 8), as well as a few megabases of nuclear DNA from Denisova 4 and Denisova 8. While the mtDNA of Denisova 8 is clearly of the Denisova type, its branch to the most recent common ancestor of Denisovans is half as long as the branch leading to Denisova 3 or Denisova 4, indicating that Denisova 8 lived many millenia before the other two. Both Denisova 4 and 8 fall together with Denisova 3 based on nuclear DNA, bringing the number of known Denisovans from one to three. In the second study, we sequenced an almost complete mtDNA and a few megabases of nuclear DNA from the third hominin phalanx from Denisova Cave, Altai 2. Both the mtDNA and the nuclear DNA show Altai 2 to be a Neandertal. The mtDNA also showed the presence of substantial Pleistocene spotted hyena contamination. Low levels of spotted hyena contamination were also found in Altai 1, Denisova

DNA that survives in museum specimens, bones and other tissues recovered by archaeologists is invariably fragmented and chemically modified. The extent to which such modifications accumulate over time is largely unknown but could potentially be used to differentiate between endogenous old DNA and present-day DNA contaminating specimens and experiments. Here we examine mitochondrial DNA sequences from tissue remains that vary in age between 18 and 60,000 years with respect to three molecular features: fragment length, base composition at strand breaks, and apparent C to T substitutions. We find that fragment length does not decrease consistently over time and that strand breaks occur preferentially before purine residues by what may be at least two different molecular mechanisms that are not yet understood. In contrast, the frequency of apparent C to T substitutions towards the 5'-ends of molecules tends to increase over time. These nucleotide misincorporations are thus a useful tool to distinguish recent from ancient DNA sources in specimens that have not been subjected to unusual or harsh treatments.