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Another perspective on the age and origin of the Berelyokh mammoth site (northeast Siberia)

Published online by Cambridge University Press:  27 February 2018

Anatoly V. Lozhkin  and
Patricia M. Anderson
Anatoly V. Lozhkin
Affiliation:
North East Interdisciplinary Science Research Institute, Far East Branch Russian Academy of Sciences, Magadan, 685000, Russia
Patricia M. Anderson*
Affiliation:
Earth and Space Sciences and Quaternary Research Center, University of Washington, Seattle, Washington 98195, USA
*
*Corresponding author at: Earth and Space Sciences and Quaternary Research Center, University of Washington, Seattle, Washington 98195, USA. E-mail address: pata@u.washington.edu (P.M. Anderson).
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Abstract

The Berelyokh site includes an exceptional bone horizon consisting of 8431 remains of Mammuthus primigenius. Previous investigations, spanning ~40 years, concluded that the deaths and bone concentration were caused by spring flooding, possibly related to wetter Bølling climates. We review work from these studies with emphasis on under-reported palynological data to provide more detail on paleoenvironmental reconstructions and an alternative interpretation for the age and origin of the bone bed. Palynological results suggest the horizon formed under cool conditions of the last glacial maximum, rather than during a Bølling-type oscillation. Presence of permafrost features and associated tundra pollen taxa in the Berelyokh sections suggest that thermokarst processes, unrelated to climate change, could account for the formation of the bone horizon. The penetration of surface waters into frozen sediments of a high floodplain terrace resulted in the formation of hidden thaw sinks. As thaw continued, the pits expanded with surface soils supported by a viscous water-sediment mixture. The weakened surface gave way under the weight of the mammoths, with the hillside collapsing either due to the animals’ struggles or destabilization related to the thaw sinks. This scenario highlights the hazards of thermokarst terrain for present and future populations of northern animals.

Keywords

MammothPalynologyRadiocarbon chronologyPermafrostThermokarstWestern Beringia

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Type
Research Article
Information
Quaternary Research , Volume 89 , Issue 2 , March 2018 , pp. 459 - 477
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2018 

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References

REFERENCES

Anderson, P.M., Lozhkin, A.V., 2001. The stage 3 interstadial complex (Karginski/middle Wisconsinan interval) of Beringia: variations in paleoenvironments and implications for paleoclimatic interpretations. Quaternary Science Reviews 20, 93–125.Google Scholar
Anderson, P.M., Lozhkin, A.V., 2002. Palynological and radiocarbon data from late Quaternary deposits of Northeast Siberia. In Simakov, K.V. (Ed.), Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database), pp. 27–34. Northeast Science Center Far East Branch Russian Academy of Sciences and National Oceanic and Atmospheric Administration (NOAA) Paleoclimatology Program, Magadan, Russia.Google Scholar
Anderson, P.M., Lozhkin, A.V., 2015. Late Quaternary vegetation of Chukotka (Northeast Russia), implications for Glacial and Holocene environments of Beringia. Quaternary Science Reviews 107, 112–128.Google Scholar
Anderson, P.M., Lozhkin, A.V., Belaya, B.V., Glushkova, O.Yu., Brubaker, L.B., 1997. A lacustrine pollen record from near altitudinal forest limit, upper Kolyma region, northeastern Siberia. The Holocene 7, 331–335.Google Scholar
Anderson, P.M., Lozhkin, A.V., Brubaker, L.B., 2002. Implications of a 24,000-yr palynological record for a Younger Dryas cooling and for boreal forest development in Northeastern Siberia. Quaternary Research 57, 325–333.Google Scholar
Arslanov, K.A., Vereschagin, N.K., Lyadov, V.V., Ukraintseva, V.V., 1980. On the chronology of the Karginsky interglacial, and on the reconstruction of Siberian landscapes based on the studies of mammoth corpses. In: Ivanova, I.K., Kind, N.V. (Eds.), Geochronology of the Quaternary Period. [In Russian.] Nauka Publishing House, Moscow, pp. 208–212.Google Scholar
Bartlein, P.J., Anderson, P.M., Edwards, M.E., McDowell, P.F., 1991. A framework for interpreting paleoclimatic variations in eastern Beringia. Quaternary International 10–12, 73–83.CrossRefGoogle Scholar
Billings, W.D., Peterson, K.M., 1980. Vegetation change and ice-wedge polygons through the thaw-lake cycle in arctic Alaska. Arctic and Alpine Research 12, 413–432.Google Scholar
Boeskorov, G.G., 2013. The natural monument “mammoth cemetery Berelyekh.”. [In Russian.] Bulletin of Samara Scientific Center of the Russian Academy of Sciences. Vol. 3–2, 806–809.Google Scholar
Binney, H., Macias-Fauria, M., Edwards, M., Anderson, P., Lozhkin, A., Kaplan, J., Nield, J., et al., 2017. Vegetation of Eurasia from the last glacial maximum to present: key biogeographic patterns. Quaternary Science Reviews 157, 80–97.Google Scholar
Edwards, M., Grosse, G., Jones, B.M., McDowell, P., 2016. The evolution of a thermokarst-lake landscape: Late Quaternary permafrost degradation and stabilization in interior Alaska. Sedimentary Geology 340, 3–14.Google Scholar
Edwards, M.E., Brubaker, L.B., Anderson, P.M., Lozhkin, A.V., 2005. Functionally novel biomes: a response to past warming in Beringia. Ecology 86, 1696–1703.Google Scholar
Faegri, K., Iversen, J., 1975. Textbook of Pollen Analysis. Hafner Press, New York.Google Scholar
Gladkova, A.N., Grichuk, V.P., Zaklinskaya, E.D., Sauer, V.V., Pokrovskaya, I.M., Radzevich, N.D., Samoilovich, S.R., Sedova, M.A., Stelmak, N.K., 1950. Pollen Analysis. [In Russian.] State Publishing House of Geological Literature, Moscow.Google Scholar
Grichuk, V.P., Zaklinskaya, E.D., 1948. Analysis of Fossil Pollen and Spores and Its Application in Paleogeography. [In Russian.] State Publishing House of Geographical Literature, Moscow.Google Scholar
Grigoriev, N.F., 1957. Finds of mammoths: overview of the materials received by the editorial board. [In Russian.] Prioda 5, 104–106.Google Scholar
Guthrie, R.D., 1990. Frozen Fauna of the 657 Mammoth Steppe: The Story of Blue Babe. The University of Chicago Press, Chicago.Google Scholar
Harington, C.R., 2011. Pleistocene vertebrates of the Yukon Territory. Quaternary Science Reviews 30, 2341–2354.Google Scholar
Harris, S.A., French, H.M., Heginbottom, J.A., Johnston, G.H., Ladanyi, B., Sego, D.C., van Everdingen, R.O., 1988. Glossary of Permafrost and Related Ground-Ice Terms. Permafrost Subcommittee, Associate Committee on Geotechnical Research, Technical Memorandum No. 192. National Research Council of Canada, Ottawa.Google Scholar
Haynes, G., 1991. Mammoths, Mastodonts, and Elephants: Biology, Behavior, and the Fossil Record. Cambridge University Press, Cambridge.Google Scholar
Higham, T.F.G., Jacobi, R.M., Ramsey, C.B., 2006. AMS radiocarbon dating of ancient bone using ultrafiltration. Radiocarbon 48, 179–195.Google Scholar
Hopkins, D.M., 1949. Thaw lake and thaw sinks in the Imuruk Lake area, Seward Peninsula, Alaska. Journal of Geology 57, 119–131.Google Scholar
Hopkins, D.M., 1982. Aspects of the paleogeography of Beringia during the late Pleistocene. In: Hopkins, D.M., Matthews, J.V., Jr., Schweger, C.E., Young, S.B. (Eds.), Paleoecology of Beringia. Academic Press, New York, pp. 3–28.Google Scholar
Karavaev, M.N., 1958. The Synopsis of the Flora of Yakutia. [In Russian.] Izdatel’stbo USSR Akademii Nauk, Moscow.Google Scholar
Kartashov, I.P., 1966. Terrasouval and related unconsolidated deposits and placers. [In Russian.] Report USSR Academy of Sciences 166, 424–426.Google Scholar
Kokorowski, H.D., Anderson, P.M., Mock, C.J., Lozhkin, A.V., 2008. A re-evaluation and spatial analysis of evidence for a Younger Dryas climatic reversal in Beringia. Quaternary Science Reviews 27, 1710–1722.Google Scholar
Komarov, V.L. (Ed.), 1930. Proceedings of the Commission for the Study of the Yakut Autonomous Soviet Socialist Republic, Volume XV: Lena-Kolyma Expedition 1909 [In Russian.] Publishing House of the USSR Academy of Sciences, Leningrad.Google Scholar
Kozhevnikov, Yu.P., 1981. Ecology-floristics in middle part of the basin of the Anadyr River. In: Mazurenko, M.T. (Ed.), Biology of Plants and Flora of Northern Far East. [In Russian.] Institute of Biological Problems of the North Far Eastern Branch United Soviet Socialist Republics Academy of Sciences, Vladivostok, pp. 65–78.Google Scholar
Kremenetski, C.V., Sulerzhitsky, L.D., Hantemirov, R., 1998. Holocene history of the northern range of some trees and shrubs in Russia. Arctic and Alpine Research 30, 317–333.Google Scholar
Kuzmina, S.A., Sher, A.V., Edwards, M.E., Haile, J., Yan, E.V., Kotov, A.N., Willerslev, E., 2011. The late Pleistocene environment of the Eastern West Beringia based on the principal section of the Main River, Chukotka. Quaternary Science Reviews 30, 2091–2106.Google Scholar
Lavrov, A.V., Sulerzhitsky, L.D., 1992. Mammoths: their period of existence as evidenced by radiocarbon dates. In: Sukachev, V.N. (Ed.), Age-Old Dynamics of Biogeocenoses. [In Russian.] Nauka Publishing House, Moscow, pp. 46–51.Google Scholar
Lavrushin, Yu.A., Bessudov, A.N., Spiridonova, E.A., Kuralenko, N.P., Nedumov, R.I., Kholmovoy, G.V., 2015. Late Paleolithic Sedimentological-Paleozoological catastrophes in Eastern Europe: Essentials of a Concept of Appearance of Mammoth “Cemeteries.” [In Russian.] GEOS, Moscow.Google Scholar
Lisiecki, L.E., Raymo, M.E., 2005. A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records. Paleoceanography 20, PA 1003. http://dx.doi.org/10.1029/2004PA001071.Google Scholar
Lozhkin, A.V., 1977. Berelekh mammoth population environments. [In Russian.] Trudy Zoologicheskogo Instituta 72, 67–68.Google Scholar
Lozhkin, A.V., 2002. Boundaries of Beringia during the late Pleistocene and Holocene. In: Simakov, K.V. (Ed.), Quaternary Paleogeography of Beringia. [In Russian.] North East Interdisciplinary Science Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, pp. 4–12.Google Scholar
Lozhkin, A.V., Anderson, P.M., 2011. Forest or no forest: implications for climatic stability in Western Beringia during Oxygen Isotope Stage 3. Quaternary Science Reviews 30, 2160–2181.Google Scholar
Lozhkin, A.V., Anderson, P.M., 2016. About the age and habitat of the Kirgilyakh mammoth (Dima), Western Beringia. Quaternary Science Reviews 145, 104–116.Google Scholar
Lozhkin, A.V., Anderson, P.M., Eisner, W.R., Rovako, L.G., Hopkins, D.M., Brubaker, L.B., Colinvaux, P.A., Miller, M.C., 1993. Late Quaternary lacustrine pollen records from southwestern Beringia. Quaternary Research 39, 314–324.Google Scholar
Lozhkin, A.V., Anderson, P.M., Matrosova, T.V., Minyuk, P.S., 2007. The pollen record from El’gygytgyn Lake: implications for vegetation and climate histories of northern Chukotka since the late middle Pleistocene. Journal of Paleolimnology 37, 135–153.Google Scholar
Lozhkin, A.V., Glushkova, O.Yu., 1997. New palynological assemblages and radiocarbon dates from Quaternary deposits of northern Priokhot’ye. In: Gagiev, M.Kh., (Ed.) Pleistocene and Holocene of Beringia. [In Russian.] North East Interdisciplinary Science Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, pp. 70–79.Google Scholar
Lozhkin, A.V., Kotov, A.N., Ryabchun, V.K., 2000. Palynological and radiocarbon data of the Ledovyi Obryv exposure (south east Chukotka). In: Simakov, K.V. (Ed.), The Quaternary Period of Beringia. [In Russian.] North East Interdisciplinary Science Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, pp. 118–131.Google Scholar
Lozhkin, A.V., Parii, V.P., 1985. Experimental Radiocarbon Dates from Late Quaternary Deposits. [In Russian.] North East Interdisciplinary Science Research Institute, Northeast Science Center, USSR Academy of Sciences, Magadan.Google Scholar
Lozhkin, A.V., Postolenko, G.A., 1989. New data about the environmental evolution of the mountain region of the Kolyma region during the late Anthropogene. [In Russian.] Doklady Akademii Nauk 307, 1184–1188.Google Scholar
Melles, M., Brigham-Grette, J., Minyuk, P.S., Nowaczyk, N.R., Wennrich, V., DeConto, R.M., Anderson, P.M., et al., 2012. 2.8 Million Years of Arctic Climate Change from Lake El’gygytgyn, NE Russia. Science 337, 315–320.Google Scholar
Mochanov, Yu.A, 1977. The earliest stages of human settlement in Northeast Asia. [In Russian.] Nauka Publishing House, Novosibirsk, Russia.Google Scholar
Murton, J.B., Edwards, M.E., Lozhkin, A.V., Anderson, P.M., Bakulina, N., Bondarenko, O.V., Cherepanova, M., Danilov, P.P., Boeskorov, V., Goslar, T., Stanislav, , Gubin, V., Korzun, J.A., Lupachev, A.V., Savvinov, G.N., Tikhonov, A., Tsygankova, V.I., Zanina, O.G. 2017. Preliminary palaeoenvironmental analysis of permafrost deposits at Batagaika megaslump, Yana Uplands, northeast Siberia. Quaternary Research 87, 314–330.Google Scholar
Murton, J.B., Goslar, T., Edwards, M.E., Bateman, M.D., Danilov, P.P., Savvinov, G.N., Gubin, S.V., et al., 2015. Palaeoenvironmental interpretation of yedoma silt (ice complex) deposition as cold-climate loess, Duvanny Yar, Northeast Siberia. Permafrost and Periglacial Processes 26, 208–288.CrossRefGoogle Scholar
Nikolskiy, P.A., Basilyan, A.E., Sulerzhitsky, L.D., Pitulko, V.V., 2010. Prelude to the extinction: revision of the Achchagyi-Allaikha and Berelekh mass accumulations of mammoth. Quaternary International 219, 16–25.Google Scholar
Nikolskiy, P.A., Sulerzhitsky, L.D., Pitulko, V.V., 2011. Last straw versus Blitzkrieg overkill: climate-driven changes in the arctic Siberian mammoth population and the Late Pleistocene extinction problem. Quaternary Science Reviews 30, 2309–2328.Google Scholar
Pitulko, V.V., 2011. The Berelekh quest: a review of forty years of research in the mammoth graveyard in northeast Siberia. Geoarchaeology 26, 5–32.Google Scholar
Pitulko, V.V., Basilyan, A.E., Pavlova, E.Y., 2014. The Berelekh mammoth “graveyard”: new chronological and stratigraphic data from the 2009 field season. Geoarchaeology 29, 277–299.Google Scholar
Reimer, P.J., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Bronch Ramsey, C., Buck, C.E., et al., 2013. IntCal13 and marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55, 1869–1887.Google Scholar
Sher, A.V., 1971. Mammals and stratigraphy of the Pleistocene of the Far North-East of the USSR and North America. [In Russian.] Nauka Publishing House, Moscow.Google Scholar
Sher, A.V., Kaplina, T.N., Giterman, R.E., Lozhkin, A.V., Arkhangelov, A.A., Kiselyov, S.V., Kouznetsov, Yu.V., Virina, E.I., Zazhigin, V.S., 1979. Scientific Excursion on Problem “Late Cenozoic of the Kolyma Lowland.” Tour XI Guide, XIV Pacific Science Congress. Academy of Sciences, USSR, Moscow.Google Scholar
Sher, A.V., Plakht, I.R., 1988. Radiocarbon dating and problems of the Pleistocene stratigraphy in lowlands of the Northeast USSR. [In Russian.] International Geology Review 30, 853–867.CrossRefGoogle Scholar
Shilo, N.A., Lozhkin, A.V., Anderson, P.M., White, B.V., Stetsenko, T.V., Glushkova, O.J., Brigham-Grette, J., et al., 2001. First continuous pollen chronicle of changes in climate and vegetation of Beringia for the last 300 thousand years. [In Russian.] Reports of the Russian Academy of Sciences 376, 231–234.Google Scholar
Shilo, N.A., Lozhkin, A.V., Titov, E.E., Shumilov, Y.V., 1983. Kirgilyakh Mammoth (Paleogeographic Aspect). [In Russian.] Nauka Publishing House, Moscow.Google Scholar
Sladkov, A.N., 1967. Introduction to Spore-Pollen Analysis. [In Russian.] Nauka Publishing House, Moscow.Google Scholar
Vasilchuk, Y., Punning, J.-M., Vasilchuk, A., 1997. Ages of mammoths in northern Eurasia: implications for population development and the late Quaternary environment. Radiocarbon 39, 1–18.Google Scholar
Vereshchagin, N.K., 1977. Berelekh Mammoth “Graveyard.” [In Russian.] Proceedings of the Zoological Institute, USSR Academy of Sciences, Leningrad.Google Scholar
Vereshchagin, N.K., Mochanov, Y.A., 1972. The world’s northernmost traces of the Upper Paleolithic. [In Russian.] Sovetskaya Arkheologia 3, 332–336.Google Scholar
Washburn, A.L., 1979. Geocryology. Edward Arnold, London.Google Scholar
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