Letter
Nature advance online publication 30 September 2007 | doi:10.1038/nature06193; Received 15 March 2007; Accepted 23 August 2007; Published online 30 September 2007
Neanderthals in central Asia and Siberia
Johannes Krause1, Ludovic Orlando2, David Serre3, Bence Viola4, Kay Prüfer1, Michael P. Richards1, Jean-Jacques Hublin1, Catherine Hänni2, Anatoly P. Derevianko5 & Svante Pääbo1
1. Max Planck Institute for Evolutionary Anthropology, Deutscher Platz 6, D-04103 Leipzig, Germany
2. Paléogénétique et Évolution Moléculaire, Institut de Génomique Fonctionnelle de Lyon, Université de Lyon, Institut Fédératif Biosciences Gerland Lyon Sud, Université Lyon 1, CNRS, INRA, École Normale Supérieure de Lyon, 46 Allée d'Italie, 69364 Lyon, Cedex 07, France
3. McGill University and Genome Quebec Innovation Center, Montreal, Quebec H3A 1A4, Canada
4. Department of Anthropology, Faculty of Life Sciences, University of Vienna, Althanstrasse 14, 1090 Vienna, Austria
5. Paleolithic Department, Institute of Archaeology and Ethnography, Russian Academy of Sciences, Siberian Branch. Lavrentieva Prospekt, 17 Novosibirsk, 630090 Russia
Correspondence to: Svante Pääbo1 Correspondence and requests for materials should be addressed to S.P. (Email: mailto:paabo@eva.mpg.de).
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Abstract
Morphological traits typical of Neanderthals began to appear in European hominids at least 400,000 years ago1 and about 150,000 years ago2 in western Asia. After their initial appearance, such traits increased in frequency and the extent to which they are expressed until they disappeared shortly after 30,000 years ago. However, because most fossil hominid remains are fragmentary, it can be difficult or impossible to determine unambiguously whether a fossil is of Neanderthal origin. This limits the ability to determine when and where Neanderthals lived. To determine how far to the east Neanderthals ranged, we determined mitochondrial DNA (mtDNA) sequences from hominid remains found in Uzbekistan and in the Altai region of southern Siberia. Here we show that the DNA sequences from these fossils fall within the European Neanderthal mtDNA variation. Thus, the geographic range of Neanderthals is likely to have extended at least 2,000 km further to the east than commonly assumed.
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When the relationship of the Teshik Tash and Okladnikov mtDNA sequences to other Neanderthal mtDNA sequences is estimated (Supplementary Fig. 3), the Teshik Tash mtDNA sequence seems to be more closely related to the mtDNA sequence from Scladina in western Europe than to the sequence from Okladnikov. Further Neanderthal mtDNA sequences from across their range and from different time horizons will obviously be necessary to permit insights into how Neanderthals colonized both western and central parts of the Old World. However, the fact that no deep mtDNA divergence is seen between the central Asian Neanderthals and European and Caucasian Neanderthals shows that they were not separated for a long time. This supports the view that central Asia was colonized relatively recently by Neanderthals26. In fact, it has been suggested that Neanderthals did not colonize most of the Russian plains before an exceptionally warm episode 125,000 years ago27, during which the Caspian Sea was drastically reduced in size. This may have facilitated the expansion of Neanderthals into central Asia and Southern Siberia26. Intriguingly, their presence in southern Siberia raises the possibility that they may have been present even farther to the east, in Mongolia and China. Further work will be necessary to address this possibility.