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Pleistocene to Holocene extinction dynamics in giant deer and woolly mammoth

An Erratum to this article was published on 17 March 2005

Abstract

The extinction of the many well-known large mammals (megafauna) of the Late Pleistocene epoch has usually been attributed to ‘overkill’ by human hunters, climatic/vegetational changes or to a combination of both1,2. An accurate knowledge of the geography and chronology of these extinctions is crucial for testing these hypotheses. Previous assumptions that the megafauna of northern Eurasia had disappeared by the Pleistocene/Holocene transition2 were first challenged a decade ago by the discovery that the latest woolly mammoths on Wrangel Island, northeastern Siberia, were contemporaneous with ancient Egyptian civilization3,4. Here we show that another spectacular megafaunal species, the giant deer or ‘Irish elk’, survived to around 6,900 radiocarbon yr bp (about 7,700 yr ago) in western Siberia—more than three millennia later than its previously accepted terminal date2,5—and therefore, that the reasons for its ultimate demise are to be sought in Holocene not Pleistocene events. Before their extinction, both giant deer and woolly mammoth underwent dramatic shifts in distribution, driven largely by climatic/vegetational changes. Their differing responses reflect major differences in ecology.

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Figure 1: Radiocarbon dated (red dots) M. giganteus finds, showing chronological changes in distribution.
Figure 2: Chart of Late Glacial and Holocene 14C dates for M. giganteus.
Figure 3: Chart of 14C dates <36 kyr for Mammuthus primigenius and Megaloceros giganteus in western Europe.
Figure 4: Chart of 14C dates <16 kyr for Megaloceros giganteus (red) and Mammuthus primigenius (blue) in Europe and selected areas of Siberia3,4,9–13,29 (and refs as Fig. 2).

References

  1. Martin, P. S. in Quaternary Extinctions: A Prehistoric Revolution (eds Martin, P. S. & Klein, R. G.) 364–403 (Univ. Arizona Press, Tucson, 1984)

    Google Scholar 

  2. Stuart, A. J. Mammalian extinctions in the late Pleistocene of northern Eurasia and North America. Biol. Rev. 66, 453–562 (1991)

    Article  CAS  Google Scholar 

  3. Stuart, A. J., Sulerzhitsky, L. D., Orlova, L. A., Kuzmin, Y. V. & Lister, A. M. The latest woolly mammoths (Mammuthus primigenius) in Europe and Asia: a review of the current evidence. Quat. Sci. Rev. 21, 1559–1569 (2002)

    Article  ADS  Google Scholar 

  4. Vartanyan, S. L., Garrut, V. E. & Sher, A. V. Holocene dwarf mammoths from Wrangel Island in the Siberian Arctic. Nature 382, 337–340 (1993)

    Article  ADS  Google Scholar 

  5. Barnosky, A. D. Big game extinction caused by late Pleistocene climatic change: Irish elk (Megaloceros giganteus) in Ireland. Quat. Res. 25, 128–135 (1986)

    Article  Google Scholar 

  6. Lister, A. M. The evolution of the giant deer, Megaloceros giganteus (Blumenbach). Zool. J. Linn. Soc. 112, 65–100 (1994)

    Article  Google Scholar 

  7. Kahlke, R. D. Die Entstehungs-, Entwicklungs- und Verbreitungsgeschichte des Oberpleistozänen Mammuthus-Coelodonta-Faunencomplexes in Eurasien (Groβsäuger). Abh. Senckenb. Natf. Ges. 546, 1–64 (1994)

    Google Scholar 

  8. Moen, R. A., Pastor, J. & Cohen, Y. Antler growth and extinction of Irish Elk. Evol. Ecol. Res. 1, 235–249 (1999)

    Google Scholar 

  9. Gould, S. J. The origin and function of ‘bizarre’ structures: antler size and skull size in the ‘Irish Elk’, Megaloceros giganteus. Evolution 28, 191–220 (1974)

    PubMed  Google Scholar 

  10. Mitchell, G. F. & Parkes, H. M. The giant deer in Ireland. Proc. R. Ir. Acad. B 52, 291–314 (1949)

    Google Scholar 

  11. Barnosky, A. D. Taphonomy and herd structure of the extinct Irish Elk Megaloceros giganteus. Science 228, 340–344 (1985)

    Article  ADS  CAS  Google Scholar 

  12. Markova, A. K. et al. Late Pleistocene distribution and diversity of mammals in northern Eurasia. Paleont. Evol. 28–29, 5–143 (1995)

    Google Scholar 

  13. Tzedakis, P. C. & Bennett, K. D. Interglacial vegetation succession: a view from southern Europe. Quat. Sci. Rev. 14, 967–982 (1996)

    Article  ADS  Google Scholar 

  14. Kaiser, K., De Klerk, P. & Terberger, T. Die “Riesenhirsch Fundstelle” von Endingen: geowissenschaftliche und archäologische Untersuchungen an einem spätglazialen Fundplatz in Vorpommern. Eiszeit. Ggw. 49, 102–122 (1999)

    Google Scholar 

  15. Aaris-Sørensen, K. & Liljegren, R. Late Pleistocene remains of giant deer (Megaloceros giganteus Blumenbach) in Scandinavia – chronology and environment. Boreas 33, 61–73 (2004)

    Article  Google Scholar 

  16. Woodman, P., McCarthy, M. & Monaghan, N. The Irish Quaternary fauna project. Quat. Sci. Rev. 16, 129–159 (1997)

    Article  ADS  Google Scholar 

  17. Hoek, W. Z. Vegetation response to the 14.7 and 11.5 ka cal. BP climate transitions: is vegetation lagging climate? Global Planet. Change 30, 103–115 (2001)

    Article  ADS  Google Scholar 

  18. Litt, T., Schmincke, H.-U. & Kromer, B. Environmental response to climatic and volcanic events in central Europe during the Weichselian Lateglacial. Quat. Sci. Rev. 22, 7–32 (2003)

    Article  ADS  Google Scholar 

  19. Gamble, C., Davies, W., Paul Pettitt, P. & Richards, M. Climate change and evolving human diversity in Europe during the last glacial. Phil. Trans. R. Soc. Lond. B 359, 243–254 (2004)

    Article  Google Scholar 

  20. Woodman, P. C. in The Quaternary History of Ireland (eds Edwards, K. & Warren, W.) 251–278 (Academic, Orlando and London, 1985)

    Google Scholar 

  21. Gonzalez, S., Kitchener, A. C. & Lister, A. M. Survival of the Irish Elk into the Holocene. Nature 405, 753–754 (2000)

    Article  ADS  CAS  Google Scholar 

  22. Guenther, E. W. Funde von Ren und Riesenhirsch in nacheiszeitlichen Schichten aus der Nähe von Theriesenhof bei Plön. Schrift. Naturwiss. Ver. Schleswig-Holstein 30, 79–81 (1960)

    Google Scholar 

  23. Vereshchagin, N. K. & Baryshnikov, G. F. in Quaternary Extinctions: A Prehistoric Revolution (eds Martin, P. S. & Klein, R. G.) 483–516 (Univ. Arizona Press, Tucson, 1984)

    Google Scholar 

  24. Panova, N. K. The Forest Development Process in Urals and Trans-Urals [in Russian] 26–49 (Uralskoye Otdelenie Rossiiskoi Akademii Nauk, Ekaterinburg, 1996).

  25. Foronova, I.V. Quaternary Mammals of the South-East of Western Siberia (Kuznetsk Basin): Phylogeny, Biostratigraphy, and Palaeoecology [In Russian] 243 (United Institute of Geology Transactions 848, Publishing house of SB RAS Branch “GEO”, Russian Academy of Sciences, Siberian Branch, Novosibirsk, 2001).

  26. Serikov, Y. B. Paleolithic and Mesolithic of the Middle Trans-Urals [in Russian] 351 (Izdatelstvo Nizhne-Tagilskogo Pedagogicheskogo Instituta, Nizhny Tagil, 2000).

  27. Pavlova, M. V. Etudes sur l'Histoire paléontologique des Ongulés, IX Sélénodontes post tertiaires de la Russie. Mem. Acad. Sci. St Petersb. 20, 1–95 (1906)

    MathSciNet  Google Scholar 

  28. Guthrie, R. D. Radiocarbon dating evidence of Holocene mammoths on an Alaskan Bering Sea island. Nature 429, 746–748 (2004)

    Article  ADS  Google Scholar 

  29. Stuart, A. J. The extinction of woolly mammoth (Mammuthus primigenius) and straight-tusked elephant (Palaeoloxodon antiquus) in Europe. Quat. Int. (in the press)

Download references

Acknowledgements

The research was funded by the Natural Environment Research Council. We thank the following for their help in providing specimens and/or data: K. Aaris-Sørensen, J. Altuna, N. Benecke, P. Boscato, M. Breda, C. Bronk Ramsey, V. Cabrera, A. Currant, W. Davies, P. Doughty, I. V. Foronova, C. Gamble, M. Germonpré, S. Gonzalez, K. Hawkins, R. Hedges, B. Huntley, R. Jacobi, K. James, L. Kaagan, R. Kahlke, A. Kitchener, Y. V. Kuzmin, J. van der Made, A. K. Markova, D. Mol, D. Nagel, L. Niven, M. Palombo, M. Patou, P. Pettitt, A. Pinto, B. Sala, M. Street, A. Tagliacozzo, P. Tomlinson, E. Turner, A. A. Vorobiev and P. Wojtal. Special thanks to I. V. Foronova for agreeing to publication of the Chernigovo date in advance of further collaborative work on Siberian Megaloceros, and to P. Grootes for AMS radiocarbon dating of the Kamyshlov and Redut specimens. We are grateful to A. Mangione, B. Sala and Superintendenza per i Beni Archeologici dell'Umbria for permission to use the Megaloceros illustration in Figs 2, 3 and 4.

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Supplementary information

Supplementary Figure 1

Photo of Kamyshlov skeleton (DOC 776 kb)

Supplementary Tables 1 and 2

Table 1: Megaloceros radiocarbon date list, and calibrated values for dates <24 cal BP Table 2: Calibrated age ranges expressed in cal years BP for Megaloceros giganteus specimens <12.5 kyr BP. (XLS 137 kb)

Supplementary References (DOC 28 kb)

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Stuart, A., Kosintsev, P., Higham, T. et al. Pleistocene to Holocene extinction dynamics in giant deer and woolly mammoth. Nature 431, 684–689 (2004). https://doi.org/10.1038/nature02890

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