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A biogenic-silica δ18O record of climatic change during the last glacial–interglacial transition in southwestern Alaska

Published online by Cambridge University Press:  20 January 2017

Feng Sheng Hu  and
Aldo Shemesh
Feng Sheng Hu*
Affiliation:
Departments of Plant Biology and Geology, University of Illinois, Urbana, IL 61801, USA
Aldo Shemesh
Affiliation:
Department of Environmental Sciences, The Weizmann Institute of Science, Rehovot 76100, Israel
*
*Corresponding author. Email Address:fshu@life.uiuc.edu
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Abstract

Despite growing evidence for environmental oscillations during the last glacial–interglacial transition from high latitude, terrestrial sites of the North Pacific rim, oxygen-isotopic records of these oscillations remain sparse. The lack of data is due partially to the paucity of lakes that contain carbonate sediment suitable for oxygen-isotopic analysis. We report here the first record of oxygen-isotopic composition in diatom silica (δ18OSi) from a lake in that region. δ18OSi increases gradually from 19.0 to 23.5‰ between 12,340 and 11,000 14C yr B.P., reflecting marked climatic warming at the end of the last glaciation. Around 11,000 14C yr B.P., δ18OSi decreases by 1.7‰, suggesting a temperature decrease of 3.5–8.9 °C at the onset of the Younger Dryas (YD) in southwestern Alaska. Climatic recovery began ca. 10,740 14C yr B.P., as inferred from the increase of δ18OSi to a maximum of 23.9‰ near the end of the YD. Our data reveal that a YD climatic reversal in southwestern coastal areas of Alaska occurred, but the YD climate did not return to full-glacial conditions.

Keywords

Younger DryasPaleoclimateOxygen IsotopesLake SedimentAlaskaNorth Pacific
Type
Articles
Information
Quaternary Research , Volume 59 , Issue 3 , May 2003 , pp. 379 - 385
Copyright
Elsevier Science (USA)

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References

Abbott, M.B, and Stafford, T.W Radiocarbon geochemistry of modern and ancient Arctic lake systems, Baffin Island, Canada. Quaternary Research 45, (1996). 300 311.CrossRefGoogle Scholar
Alley, R.B The Younger Dryas cold interval as viewed from central Greenland. Quaternary Science Reviews 19, (2000). 213 226.CrossRefGoogle Scholar
Ammann, B, Eicher, U, von-Grafenstein, U, Hofmann, W, Lemdahl, G, Schwander, J, Tobolski, K, Wick, L, Birks, H.J.B, and Brooks, S.J Quantification of biotic responses to rapid climatic changes around the Younger Dryas—A synthesis. Palaeogeography, Palaeoclimatology, Palaeoecology 159, (2000). 313 347.CrossRefGoogle Scholar
Anderson, P.M, Bartlein, P.J, and Brubaker, L.B Late Quaternary history of tundra vegetation in northwestern Alaska. Quaternary Research 41, (1994). 306 315.CrossRefGoogle Scholar
Barker, P.A, Street-Perrott, F.A, Leng, M.J, Greenwood, P.B, Swain, D.L, Perrott, R.A, Telford, R.J, and Ficken, K.J A 14,000-year oxygen-isotope record from diatom silica in two alpine lakes on Mt. Kenya. Science 292, (2001). 2307 2310.CrossRefGoogle ScholarPubMed
Bigelow, N.H, and Edwards, M.E A 14,000 yr paleoenvironmental record from Windmill Lake, central Alaska. Evidence for high-frequency climatic and vegetation fluctuations. Quaternary Science Reviews 20, (2001). 203 215.CrossRefGoogle Scholar
Brandriss, M.E, O’Neil, J.R, Edlund, M.B, and Stoermer, E.F Oxygen isotope fractionation between diatomaceous silica and water. Geochemica et Cosmochimica Acta 62, (1998). 1119 1125.CrossRefGoogle Scholar
Briner, J.P, Kaufman, D.S, Werner, A, Caffee, M, Levy, L, Manley, W.F, Kaplan, M.R, and Finkel, R.C Glacier readvance during the late glacial (Younger Dryas?) in the Ahklun Mountains, southwestern Alaska. Geology 30, (2002). 679 682.2.0.CO;2>CrossRefGoogle Scholar
Briner, J.P, Swanson, T.W, and Caffee, M Late Pleistocene cosmogenic 36Cl glacial chronology of the southwestern Ahklun Mountains, Alaska. Quaternary Research 56, (2001). 148 154.CrossRefGoogle Scholar
Brubaker, L.B, Anderson, P.M, and Hu, F.S Vegetation ecotone dynamics in southwest Alaska during the late Quaternary. Quaternary Science Reviews 20, (2001). 175 188.CrossRefGoogle Scholar
Chapin, F.S, Shaver, G.R, Giblin, A.E, Nadelhoffer, K.J, and Laundre, J.A Responses of arctic tundra to experiemnetal and observed changes in climate. Ecology 76, (1995). 694 711.CrossRefGoogle Scholar
Cuffey, K.M, Clow, G.D, Alley, R.B, Stuiver, M, Waddington, E.D, and Saltus, R.W Large Arctic temperature change at the glacial-Holocene transition. Science 270, (1995). 455 458.CrossRefGoogle Scholar
Engstrom, D.R, Hansen, B.S.C, and Wright, H.E.J A possible Younger Dryas record in southeastern Alaska. Science 250, (1990). 1383 1385.CrossRefGoogle ScholarPubMed
Epstein, S The isotopic climatic records in the Allerod-Bolling-Younger Dryas and post-Younger Dryas events. Global Biogeochemical Cycles 9, (1995). 557 563.CrossRefGoogle Scholar
Hu, F.S, Brubaker, L.B, and Anderson, P.M Postglacial vegetation and climate change in the northern Bristol Bay region, southwestern Alaska. Quaternary Research 43, (1995). 382 392.CrossRefGoogle Scholar
Hu, F.S, Finney, B.F, and Brubaker, L.B Effects of Holocene Alnus expansion on aquatic productivity, nitrogen cycling, and soil development in southwestern Alaska. Ecosystems 4, (2001). 358 368.CrossRefGoogle Scholar
Hu, F.S, Lee, B.Y, Kaufman, D.S, Yoneji, S, Nelson, D.M, and Henne, P.D Response of tundra ecosystem in southwestern Alaska to YoungerDryas climatic oscillation. Global Change Biology 8, (2002). 1156 1163.CrossRefGoogle Scholar
Juillet-Leclerc, A, and Labeyrie, L Temperature dependence of the oxygen isotopic fractionation between diatom silica and water. Earth and Planetary Science Letters 84, (1987). 69 74.CrossRefGoogle Scholar
Levesque, A.J, Cwynar, L.C, and Walker, I.R Exceptionally steep north-south gradients in lake temperatures during the last deglaciation. Nature 385, (1997). 423 426.CrossRefGoogle Scholar
Levy, L.B., (2002). Late Holocene glacier fluctuations, northeastern Ahklun Moutnains, southwestern Alaska. Unpublished MS thesis, Northern Arizona University, Google Scholar
Manley, W.F, Kaufman, D.S, and Briner, J.P Pleistocene glacial history of the southern Ahklun Mountains, southwestern Alaska. soil-development, morphometric, and radiocarbon constraints. Quaternary Science Reviews 20, (2001). 353 370.CrossRefGoogle Scholar
Mayle, F.E, and Cwynar, L.C Impact of the Younger Dryas cooling event upon lowland vegetation of matitime Canada. Ecological Monographs 65, (1995). 129 154.CrossRefGoogle Scholar
Michaelson, G.J, Ping, C.L, and Kimble, J.M Carbon storage and distribution in tundra soils of Arctic Alaska, USA. Arctic and Alpine Research 28, (1996). 414 424.CrossRefGoogle Scholar
Peteet, D.M, and Mann, D.H Late-glacial vegetational, tephra, and climatic history of southwestern Kodiak Island, Alaska. Ecoscience 1, (1994). 255 267.CrossRefGoogle Scholar
Rietti-Shati, M, Shemesh, A, and Karlen, W A 3000-year climatic record from biogenic silica oxygen isotopes in an equatorial high-latitude lake. Science 281, (1998). 980 982.CrossRefGoogle Scholar
Rioual, P, Andrieu-Ponel, V, Rietti-Shati, M, Battarbee, R.W, Beaulieu, J.L.d, Cheddadi, R, M, M.R, Svobodova, H, and Shemesh, A High-resolution record of climate stability in France during the last interglacial period. Nature 413, (2001). 293 296.CrossRefGoogle ScholarPubMed
Rosqvist, G.C, Rietti-Shati, M, and Shemesh, A Late glacial to middle Holocene climatic record of lacustrine biogenic silica oxygen isotopes from a Southern Occan Island. Geology 27, (1999). 967 970.2.3.CO;2>CrossRefGoogle Scholar
Rozanski, K, Araguas-Araguas, L, and Gonfiantini, R Isotopic patterns in modern global precipitation. Swart, P.K, Lochmann, K.C, McKenzie, J, and Savin, S Climate change in continental isotopic records,. (1993). American Geophysical Union, Washington, D.C. 1 36.Google Scholar
Severinghaus, J.P, Sowers, T, Brook, E.J, Alley, R.B, and Bender, M.L Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice. Nature 391, (1998). 141 146.CrossRefGoogle Scholar
Shemesh, A, and Peteet, D Oxygen isotopes in fresh water biogenic opal—Northeastern US Allerod-Younger Dryas temperature shift. Geophysical Research Letters 25, (1998). 1935 1938.CrossRefGoogle Scholar
Shemesh, A, Bruckle, L.H, and Hays, J.D Late Pleistocene oxygen isotope records of biogenic silica from the Atlantic sector of the Southern Ocean. Paleoceanography 10, (1995). 179 196.CrossRefGoogle Scholar
Shemesh, A, Charles, C.D, and Fairbanks, R.G Oxygen isotopes in biogenic silica. global changes in ocean temperature and isotopic composition. Science 256, (1992). 1434 1436.CrossRefGoogle ScholarPubMed
Shemesh, A, Rosqvist, G, Rietti-Shati, M, Rubensdotter, L, Bigler, C, Yam, R, and Karlen, W Holocene climatic change in Swedish Lapland inferred from an oxygen-isotope record of lacustrine biogenic silica. The Holocene 11, (2001). 447 454.CrossRefGoogle Scholar
Sturm, M, Racine, C, and Tape, K Climate change—Increasing shrub abundance in the Arctic. Nature 411, (2001). 546 547.CrossRefGoogle ScholarPubMed
Wright, H.E Jr., Mann, D.H, and Glaser, P.H Piston corers for peat and lake sediments. Ecology 65, (1984). 657 659.CrossRefGoogle Scholar