Hostname: page-component-cd9895bd7-lnqnp Total loading time: 0 Render date: 2024-12-28T13:41:16.389Z Has data issue: false hasContentIssue false
  • English
  • Français

Paleoclimatic implications of glacial and postglacial refugia for Pinus pumila in western Beringia

Published online by Cambridge University Press:  20 January 2017

Patricia M. Anderson ,
Anatoly V. Lozhkin ,
Tatiana B. Solomatkina  and
Thomas A. Brown
Patricia M. Anderson*
Affiliation:
Quaternary Research Center and Department of Earth & Space Sciences , Box 351310, University of Washington, Seattle, WA 98195-1310, USA
Anatoly V. Lozhkin
Affiliation:
North East Interdisciplinary Science Research Institute, Far East Branch Russian Academy of Sciences, 16 Portovaya St., Magadan, 685000 Russia
Tatiana B. Solomatkina
Affiliation:
North East Interdisciplinary Science Research Institute, Far East Branch Russian Academy of Sciences, 16 Portovaya St., Magadan, 685000 Russia
Thomas A. Brown
Affiliation:
Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, CA 94550, USA
*
*Corresponding author.E-mail address:pata@u.washington.edu (P.M. Anderson).
Get access Rights & Permissions [Opens in a new window]

Abstract

Palynological results from Julietta Lake currently provide the most direct evidence to support the existence of a glacial refugium for Pinus pumila in mountains of southwestern Beringia. Both percentages and accumulation rates indicate the evergreen shrub survived until at least ∼ 19,000 14C yr BP in the Upper Kolyma region. Percentage data suggest numbers dwindled into the late glaciation, whereas pollen accumulation rates point towards a more rapid demise shortly after ∼ 19,000 14C yr BP. Pinus pumila did not re-establish in any great numbers until ∼ 8100 14C yr BP, despite the local presence ∼ 9800 14C yr BP of Larixdahurica, which shares similar summer temperature requirements. The postglacial thermal maximum (in Beringia ∼ 11,000-9000 14C yr BP) provided Pinus pumila shrubs with equally harsh albeit different conditions for survival than those present during the LGM. Regional records indicate that in this time of maximum warmth Pinus pumila likely sheltered in a second, lower-elevation refugium. Paleoclimatic models and modern ecology suggest that shifts in the nature of seasonal transitions and not only seasonal extremes have played important roles in the history of Pinus pumila over the last ∼ 21,000 14C yr BP.

Keywords

RefugiumSeasonalityPollenNortheastern SiberiaBeringiaLate Quaternary
Type
Original Articles
Information
Quaternary Research , Volume 73 , Issue 2 , March 2010 , pp. 269 - 276
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Anderson, P.M., (1985). Late Quaternary vegetational change in the Kotzebue Sound area, northwestern Alaska. Quaternary Research 24, 307–321.Google Scholar
Anderson, P.M., Lozhkin, A.V., (2001). The stage 3 interstadial complex (Karginskii/middle Wisconsinan interval) of Beringia: variations in paleoenvironments and implications for paleoclimatic interpretations. Quaternary Science Reviews 20, 93–126.CrossRefGoogle Scholar
Anderson, P.M., Lozhkin, A.V., (2002). Palynological and radiocarbon data from late Quaternary deposits of northeast Siberia. Anderson, P.M., Lozhkin, A.V., Late Quaternary Vegetation and Climate of Siberia and the Russian Far East (Palynological and Radiocarbon Database). Russian Academy of Science Far East Branch North East Science Center and U.S. National Oceanic and Atmospheric Administration, Magadan., 27–34.Google Scholar
Anderson, P.M., Belaya, B.V., Glushkova, O.Yu., Lozhkin, A.V., (1997a). New data about the evolution of vegetation cover of northern Priokhot'ye during the late Pleistocene and Holocene. Gagiev, M.Kh, Late Pleistocene and Holocene of Beringia. North East Interdisciplinary Research Institute Far East Branch Russian Academy of Sciences, Magadan., 33–54.In Russian.Google Scholar
Anderson, P.M., Lozhkin, A.V., Belaya, B.V., Glushkova, O.Yu., Brubaker, L.B., (1997b). A lacustrine pollen record from near altitudinal forest limit, Upper Kolyma region, northeastern Siberia. The Holocene 7, 331–335.CrossRefGoogle Scholar
Anderson, P.M., Lozhkin, A.V., Belaya, B.V., Stetsenko, T.V., (1998). New data about the stratigraphy of late Quaternary deposits of northern Priokhot'ye. Simakov, K.V., Environmental Changes in Beringia during the Quaternary. North East Interdisciplinary Research Institute Far East Branch Russian Academy of Sciences, Magadan., 69–87.In Russian.Google Scholar
Anderson, P.M., Lozhkin, A.V., Belaya, B.V., Stetsenko, T.V., (2002a). Modern spore-pollen spectra from the mountain regions of the Kolyma and Indigirka rivers from lacustrine sediments. Simakov, K.V., Quaternary Paleogeography of Beringia. North East Interdisciplinary Science Research Institute, Far East Branch Russian Academy of Science, Magadan., 28–39.In Russian.Google Scholar
Anderson, P.M., Lozhkin, A.V., Belaya, B.V., Stetsenko, T.V., (2002b). Modern spore-pollen spectra of northern Priokhot'ye from lacustrine sediments. Simakov, K.V., Quaternary Paleogeography of Beringia. North East Interdisciplinary Science Research Institute, Far East Branch Russian Academy of Science, Magadan., 51–61.In Russian.Google Scholar
Anderson, P.M., Lozhkin, A.V., Brubaker, L.B., (2002c). 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.CrossRefGoogle Scholar
Andreev, V.N., (1980). Vegetation and Soils of Subarctic Tundra. Nauka Academy of Science Union Soviet Socialist Republics, Siberian Branch Yakutia Sub-branch, Novosibirsk., In Russian.Google Scholar
Bartlein, P.J., Anderson, K.H., Anderson, P.M., Edwards, M.E., Mock, C.J., Thompson, R.S., Webb, R.S., Webb, T.III, Whitlock, C., (1998). Paleoclimate simulations for North America over the past 21,000 years: features of the simulated climate and comparisons with paleoenvironmental data. Quaternary Science Reviews 17, 549–586.Google Scholar
Bennett, K.D., Provan, J., (2008). What do we mean by "refugia"?. Quaternary Science Reviews 27, 2449–2455.CrossRefGoogle Scholar
Binney, H.A, Willis, k.J, Edwards, M.E, Bhagwat, S.A, Anderson, P.M, Andreev, A.A, Blaauw, M, Damblon, F, Haesaerts, P, Kienast, F, Kremenetski, K.V, Krivonogov, S.K, Lozhkin, A.V, MacDonald, G.M, Novenko, E.Y, Oksanen, P, Sapelko, T.V, V"liranta, M, Vazhenina, L., (2009). The distribution of late-Quaternary woody taxa in northern Eurasia: evidence from a new macrofossil database. Quaternary Science Reviews 28, 2445"2464.Google Scholar
Birks, H.J.B., (1989). Holocene isochrone maps and patterns of tree-spreading in the British Isles. Journal of Biogeography 16, 503–540.Google Scholar
Brubaker, L.B., Anderson, P.M., Edwards, M.E., Lozhkin, A.V., (2005). Beringia as a glacial refugium for boreal trees and shrubs: new perspectives from mapped pollen data. Journal of Biogeography 32, 833–848.Google Scholar
Cwynar, L.C., (1982). A late Quaternary vegetation history from Hanging Lake, northern Yukon. Ecological Monographs 52, 1–24.Google Scholar
Dahl, E., (1946). On different types of unglaciated areas during the ice ages and their significance to phytogeography. New Phytologist 45, 225–242.CrossRefGoogle Scholar
Edwards, M.E., Barker, E.D., (1994). Climate and vegetation in northern Alaska 18,000 yr-present. Palaeogeography, Palaeoclimatology, Palaeoecology 109, 127–135.Google Scholar
Edwards, M.E., Brubaker, L.B., Lozhkin, A.V., Anderson, P.M., (2005). Structurally novel biomes: a response to past warming in Beringia. Ecology 86, 1696–1703.CrossRefGoogle Scholar
Gallimore, R.G., Kutzbach, J.E., (1995). Snow cover and sea ice sensitivity to generic changes in earth orbital parameters. Journal of Geophysical Research 100, 1103–1120.CrossRefGoogle Scholar
Gorbarenko, S.A., Southon, J.R., Keigwin, L.D., Cherepanova, M.V., Gvozdeva, I.G., (2004). Late Pleistocene-Holocene oceanographic variability in the Okhotsk Sea: geochemical, lithological, and paleontological evidence. Palaeogeography, Palaeoclimatology, Palaeoecology 209, 281–301.CrossRefGoogle Scholar
Grichuk, V.P., (1984). Late Pleistocene vegetation history. Velichko, A.A., Late Quaternary Environments of the Soviet Union. University of Minnesota Press, Minneapolis., 155–179.Google Scholar
Heusser, C.J., (1955). Pollen profiles from the Queen Charlotte Islands, British Columbia. Canadian Journal of Botany 33, 429–449.CrossRefGoogle Scholar
Khomentovskii, P.A., (1995). The Ecology of Mountain Pine (Pinus pumila (Pall.) Regel) in Kamchatka: A General Review. Dal'nauka, Vladivostok., In Russian.Google Scholar
Kienast, F., Schirrmeister, L., Siegert, C., Tarasov, P., (2005). Palaeobotanical evidence for warm summers in the East Siberian Arctic during the last cold stage. Quaternary Research 63, 283–300.CrossRefGoogle Scholar
Kokorowski, H.D, Anderson, P.M, Sletten, R.S, Lozhkin, A.V, Brown, T.A., (2008). Post-glacial climatic changes in Northeast Siberia based on a multiproxy sediment record from Elikchan 4 Lake. Arctic, Antarctic and Alpine Research 40, 497"505.Google Scholar
Kozhevnikov, Yu.P, (1981). Ecology-floristics in middle part of the basin of the Anadyr River. Mazurenko, M.T., Biology of Plants and Flora of Northern Far East. Institute of Biological Problems of the North Far Eastern Branch United Soviet Socialist Republics Academy of Sciences, Vladivostok., 65–78.In Russian.Google Scholar
Krementski, C.V., Liu, K-L., MacDonald, G.M., (2000). The late Quaternary dynamics of pines in northern Asia. Richardson, D.M., Ecology and Biogeography of Pinus . Cambridge University Press, Cambridge., 95–106.Google Scholar
Kullman, J., (2002). The geoecological history of Picea abies in northern Sweden and adjacent parts of Norway: A contrarian hypothesis of postglacial tree immigration patterns. Geo-"ko 29, 141–172.Google Scholar
Kullman, L., (2002). Boreal tree taxa in the central Scandes during the late-glacial: implications for late Quaternary forest history. Journal of Biogeography 29, 1117–1124.Google Scholar
Kullman, L., (2008). Early postglacial appearance of tree species in northern Scandinavia: review and perspective. Quaternary Science Reviews 27, 2467–2472.Google Scholar
Kutzbach, J.E., Gallimore, R.G., (1988). Sensitivity of a coupled atmosphere/mixed-layer ocean model to change in orbital forcing at 9000 years B.P. Journal of Geophysical Research 93, 803–821.CrossRefGoogle Scholar
Kutzbach, J.E., Gallimore, R.G., Guetter, P.J., (1991). Sensitivity experiments on the effect of orbitally-caused insolation changes on the interglacial climate of high northern latitudes. Quaternary International 10-12 223–229.Google Scholar
Kutzbach, J., Gallimore, R., Harrison, S., Behling, P., Selin, R., Laarif, F., (1998). Climate and biome simulations for the past 21,000 years. Quaternary Science Reviews 17, 473–506.Google Scholar
Lozhkin, A.V., (1993). Geochronology of late Quaternary events in northeastern Russia. Radiocarbon 35, 429–433.Google Scholar
Lozhkin, A.V., Anderson, P.M., Belaya, B.V., Glushkova, O.Yu., Kozhevnikova, M.V., Kotova, L.N., (1996). Palynological characteristics and radiocarbon dates of sediments from Elgennya Lake, Upper Kolyma. Buchkov, M.Yu, Quaternary Climates and Vegetation of Western Beringia. North East Interdisciplinary Research Institute Far East Branch Russian Academy of Sciences, Magadan., 50–64.In Russian.Google Scholar
Lozhkin, A.V., (2001). Modern pollen rain in the arctic regions of Beringia and the reconstruction of vegetation during the glacial intervals of the Pleistocene. In: Simakov, K.V. (Ed.), Quaternary Paleogeography of Beringia, North East Interdisciplinary Science Research Institute, Far East Branch Russian Academy of Science, Magadan, pp. 13"27. In Russian.Google Scholar
Lozhkin, A.V., Anderson, P.M., (1995). A late Quaternary pollen record from Elikchan-4 Lake, northeast Siberia. Geology of the Pacific Ocean 14, 18–22.Google Scholar
Lozhkin, A.V., Anderson, P.M., Eisner, W.R., Ravako, 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.CrossRefGoogle Scholar
Lozhkin, A.V., Anderson, P.M., Brubaker, L.B., Kotov, A.N., Kotova, L.N., Prokhorova, T.P., (1998). The herb pollen zone from sediments of glacial lakes. Simakov, K.V., Environmental Changes in Beringia during the Quaternary. North East Interdisciplinary Research Institute Far East Branch Russian Academy of Sciences, Magadan., 96–111.In Russian.Google Scholar
Lozhkin, A.V., Anderson, P.M., Belaya, B.V., Glushkova, O.Yu., Stetsenko, T.V., (2000). Vegetation change in northeast Siberia at the Pleistocene-Holocene boundary and during the Holocene. Simakov, K.V., The Quaternary Period of Beringia. North East Interdisciplinary Research Institute Far East Branch Russian Academy of Sciences, Magadan., 53–75.In Russian.Google Scholar
Lozhkin, A.V., Anderson, P.M., Vartanyan, S.L., Brown, T.A., Belaya, B.V., Kotov, A.N., (2001). Late Quaternary paleoenvironments and modern pollen data from Wrangel Island (northern Chukotka). Quaternary Science Reviews 20, 217–234.Google Scholar
Lozhkin, A.V, Anderson, P.M, Belaya, B.V, Stetsenko, T.V., (2002). Reflections on modern pollen rain of Chukotka from bottom lake sediments. In: Simakov, K.V., (Ed.), Quaternary Paleogeography of Beringia, North East Interdisciplinary Science Research Institute, Far East Branch Russian Academy of Science, Magadan, pp. 40"50. In Russian.Google Scholar
Mann, D.H., Peteet, D.M., Reanier, R.E., Kunz, M.L., (2002). Responses of an arctic landscape to late glacial and early Holocene climatic changes: the importance of moisture. Quaternary Science Reviews 21, 997–1021.Google Scholar
Moskalyuk, T.A., (2008). On adaptations of trees and shrubs in the north of the Russian Far East. Russian Journal of Ecology 39, 73–82.Google Scholar
Mitchell, J.F.B., Grahame, N.S., Needham, K.H., (1988). Climate simulations for 9000 years before present: seasonal variations and the effect of the Laurentide ice sheet. Journal of Geophysical Research 93, 8283–8303.Google Scholar
Mock, C.J., Bartelin, P.J., Anderson, P.M., (1998). Atmospheric circulation patterns and spatial climatic variations in Beringia. International Journal of Climatology 18, 1085–1104.3.0.CO;2-K>CrossRefGoogle Scholar
(1994). PALE members. Research Protocols for PALE Paleoclimates of Arctic Lakes and Estuaries. PAGES Workshop Report Series, 1–94., IGBP.Google Scholar
Porter, S.C., Pierce, K.L., Hamilton, T.D., (1983). Late Wisconsin mountain glaciation in the western United States. Porter, S.C., Late Quaternary Environments of the United States Vol. 1 The Late Pleistocene. University of Minnesota Press, Minneapolis., 71–111.Google Scholar
Sepp", H., Hicks, S., (2006). Integration of modern and past pollen accumulation rate (PAR) records across the arctic tree-line: a method for more precise vegetation reconstructions. Quaternary Science Reviews 25, 1501–1516.Google Scholar
Sher, A.V., Kuzmina, S.A., Kuznetsova, T.V., Sulerzhitsky, L.D., (2005). New insights into the Weichselian environment and climate of the East Siberian Arctic, derived from fossil insects, plants, and mammals. Quaternary Science Reviews 24, 533–569.CrossRefGoogle Scholar
Shilo, N.A., (1970). The North of the Far East. Moscow, Nauka. Google Scholar
Shilo, N.A., Lozhkin, A.V., Anderson, P.M., Brown, T.A., Pakhomov, A.Yu., Solomatkina, T.B., (2007). Glacial refugium of Pinus pumila (Pall.) Regel in northeastern Siberia. Doklady Earth Sciences 412, 122–124.Google Scholar
Shilo, N.A, Lozhkin, A.V, Anderson, P.M, Vazhenina, L.N, Glushkova, O. Yu, Matrosova, T.V., (2008). New data about the expansion of Lairx gmelinii to arctic regions of Beringia during the early Holocene. Doklady Akademia Nauk 422, 1"3. In Russian.Google Scholar
Stewart, J.R., Lister, A.M., (2001). Cryptic northern refugia and the origins of the modern biota. Trends in Ecology and Evolution 16, 608–613.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., (1993). Extended 14C data base and revised CALIB 3.0 14C calibration program. Radiocarbon 350, 215–230.Google Scholar
Tarasov, P., Williams, J., Andreev, A., Nakagawa, T., Bezrukova, E., Herzschuh, U., Igarashi, Y., M"ller, S., Werner, K., Zheng, Z., (2007). Satellite- and pollen-based quantitative woody cover reconstructions for northern Asia: verification and application to late-Quaternary pollen data. Earth and Planetary Science Letters 264, 284–298.Google Scholar
Willis, K.J., Whittaker, R.J., (2000). The refugial debate. Science 287, 1406–1407.Google Scholar
Willis, K.J., van Andel, T.H., (2004). Trees or no trees? The environment of central and eastern Europe during the last glaciation. Quaternary Science Reviews 23, 2369–2387.Google Scholar
Willis, K.J., Rudner, E., S"megi, P., (2000). The full-glacial forests of central and southeastern Europe. Quaternary Research 53, 203–213.Google Scholar
Wright, H.E., Mann, D.H., Glaser, P.H., (1984). Piston corers for peat and lake sediments. Ecology 65, 657–659.Google Scholar