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Paleoclimate Signals of Lake Hovsgol, Mongolia, Over the Last 19,000 Years Using Authigenic Beryllium Isotopes

Published online by Cambridge University Press:  26 July 2016

Yire Choi ,
Kyeong Ja Kim ,
Daekyo Cheong  and
Yong Ha Kim
Yire Choi
Affiliation:
Korea Institute of Geoscience and Mineral Resources, Daejeon 305–250, Korea University of Science and Technology, Daejeon 305–350, Korea
Kyeong Ja Kim*
Affiliation:
Korea Institute of Geoscience and Mineral Resources, Daejeon 305–250, Korea
Daekyo Cheong
Affiliation:
Department of Geology, Kangwon National University, Chuncheon, Kangwon-do 200–701, Korea
Yong Ha Kim
Affiliation:
Department of Astronomy and Space Science, Chungnam National University, Daejeon 305–764, Korea
*
3. Corresponding author. Email: [email protected].
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Abstract

The paleoclimatic signal of Lake Hovsgol in Mongolia was investigated using authigenic beryllium isotopes from 20 sediment samples. The beryllium isotopic records from this study indicate that there were three dry and cold periods at the lake around 9400, 12,700, and 17,100 cal yr BP. The significant 10Be signal during the Younger Dryas (YD) period is found to be lower. This indicates that the Lake Hovsgol area was subject to a period of cold and dry conditions with minimal dust input, which manifests itself as a low 9Be profile in this study. In warmer and wetter climatic conditions, the 10Be concentration was found to be higher, and this agrees with the sedimentation record of this study. The climatic signals from Lake Hovsgol appear to be similar to a decreased beryllium record during the deglacial period. The results of this study confirm that the Lake Hovsgol area also experienced the global paleoclimatic change associated with the YD event around 12,700 cal yr BP. Further investigation using worldwide lake records by the analytical technique of authigenic beryllium will be useful for understanding the global paleoclimatic change pattern in conjunction with lake-level change.

Type
Articles
Information
Radiocarbon , Volume 56 , Issue 3 , 2014 , pp. 1139 - 1150
Copyright
Copyright © 2014 by the Arizona Board of Regents on behalf of the University of Arizona 

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References

Aldahan, A, Ning, S, Possnert, G, Backman, J, Boström, K. 1997. 10Be records from sediments of the Arctic Ocean covering the past 350 ka. Marine Geology 144(1–3):147–62.Google Scholar
Bourlès, D, Raisbeck, GM, Yiou, F. 1989. 10Be and 9Be in marine sediments and their potential for dating. Geochimica Cosmochimica et Acta 53(2):443–52.Google Scholar
Bunch, TE, Hermes, RE, Moore, AMT, Kennett, DJ, Weaver, JC, Wittke, JH, DeCarli, PS, Bischoff, JL, Hillman, GC, Howard, GA, Kimbel, DR, Kletetschka, G, Lipo, CP, Sakai, S, Revay, Z, West, A, Firestone, RB, Kennett, JP. 2012. Very high-temperature impact melt products as evidence for cosmic airbursts and impacts 12,900 years ago. Proceedings of the National Academy of Sciences of the USA 109(28):11,066–7.Google Scholar
Carcaillet, J, Bourlès, D, Thouveny, N, Arnold, M. 2004. A high resolution authigenic 10Be/9Be record of geomagnetic moment variation over the last 300 ka from sedimentary cores of the Portuguese Margin. Earth Planetary Science Letters 219(3–4):397–412.CrossRefGoogle Scholar
Coto, B, Martos, C, Pena, JL, Rodriguez, R, Pastor, G. 2012. Effects in the solubility of CaCO3: experimental study and model description. Fluid Phase Equilibria 324:1–7.Google Scholar
Dunai, T. 2010. Cosmogenic Nuclides. Cambridge: Cambridge University Press.CrossRefGoogle Scholar
Eisenhauer, A, Spielhagen, RF, Frank, M, Hentzschel, G, Mangini, A, Kubik, PW, Dittrich-Hannen, B, Billen, T. 1994. 10Be records of sediment cores from high northern latitudes: implications for environmental and climatic changes. Earth and Planetary Science Letters 124(1–4):171–84.Google Scholar
Elsässer, W, Ney, EP, Winckler, JR. 1956. Cosmic-ray intensity and geomagnetism. Nature 178(4544):1226–7.Google Scholar
Fedotov, AP, Chebykin, EP, Yu, SM, Vorobyova, SS, Yu, OE, Golobokova, LP, Pogodaeva, TV, Zheleznyakova, TO, Grachev, MA, Tomurhuu, D, Oyunchimeg, T, Narantsetseg, T, Tomurtogoo, O, Dolgikh, PT, Arsenyuk, MI, Batist, M. 2004. Changes in the volume and salinity of Lake Khubsugul (Mongolia) in response to global climate changes in the upper Pleistocene and the Holocene. Palaeogeography, Palaeoclimatology, Palaeoecology 209(1–4):245–57.Google Scholar
Frank, M. 2000. Comparison of cosmogenic radionuclide production and geomagnetic field intensity over the last 200,000 years. Philosophical Transactions of the Royal Society of London A 358(1768):1089–107.CrossRefGoogle Scholar
Frank, M, Schwarz, B, Baumann, S, Kubik, PW, Suter, M, Mangini, A. 1997. A 200 kyr record of cosmogenic radionuclide production rate and geomagnetic field intensity from 10Be in globally stacked deep-sea sediments. Earth and Planetary Science Letters 149(1–4):121–9.Google Scholar
Goulden, CE, Tumurtogoo, O, Karabanov, E. 2006. The geological history and geography of Lake Hovsgol, Mongolia. In: Goulden, GE, Sitnikova, T, Gelhaus, T, Boldgiv, B, editors. The Geology, Biodiversity and Ecology of Lake Hovsgol (Mongolia). Leiden: Backhuys Publishers.Google Scholar
Graham, IJ, Ditchburn, RG, Whitehead, NE. 1998. 10Be spikes in Plio-Pleistocene cyclothems, Wanganui Basin, New Zealand: identification of the local flooding surface (LFS). Sedimentary Geology 122(1–4):193–215.CrossRefGoogle Scholar
Hill, JW, Petrucci, RH. 1999. General Chemistry. 2nd edition. Upper Saddle River: Prentice Hall.Google Scholar
Horiuchi, K, Goldberg, EL, Kobayashi, K, Oda, T, Nakamura, T, Kawai, T. 2001. Climate-induced variations of cosmogenic beryllium-10 in the sediments of Lake Baikal of the last 150 ky from AMS, SRXRF and NAA data. Nuclear Instruments and Methods in Physics Research A 470(1–2):396–404.Google Scholar
Jessen, CA, Rundgren, M, Bjorck, S, Muscheler, R. 2007. Climate forced atmospheric CO2 variability in the early Holocene: a stomatal frequency reconstruction. Global and Planetary Change 57(3–4):247–60.Google Scholar
Kim, KJ, Zolitschka, B, Jull, AJT, Ohlendorf, C, Haberzettl, T, Matsuzaki, H. 2012. Tracing environmental change in southern Patagonia using beryllium isotopes, Laguna Potrok Aike, Argentina. Quaternary Geochronology 9:27–33.Google Scholar
Laj, C, Kissel, C, Mazaud, A, Channell, JET, Beer, J. 2000. North Atlantic palaeointensity stack since 75ka (NAPIS-75) and the duration of the Laschamp event. Philosophical Transactions of the Royal Society of London A 358(1768):1009–25.Google Scholar
LeCompte, MA, Goodyear, AC, Demitroff, MN, Batchelor, D, Vogel, EK, Mooney, C, Rock, BN, Seidel, AW. 2012. Independent evaluation of conflicting microspherule results from different investigations of the Younger Dryas impact hypothesis. Proceedings of the National Academy of Sciences of the USA 109(44):17,738–9.Google Scholar
Masarik, J, Beer, J. 1999. Simulation of particle fluxes and cosmogenic nuclide production in the Earth's atmosphere. Journal of Geophysical Research 104(D10):12,099–13,012.CrossRefGoogle Scholar
Masarik, J, Frank, M, Schäfer, JM, Wieler, R. 2001. Correction of in situ cosmogenic nuclide production rates for geomagnetic field intensity variations during the past 800,000 years. Geochimica et Cosmochimica Acta 65(17):2995–3003.Google Scholar
McHargue, L, Donahue, DJ. 2005. Effects of climate and the cosmic-ray flux on the 10Be content of margin sediments. Earth and Planetary Science Letters 232(1–2):193–207.Google Scholar
McHargue, L, Jull, AJT, Cohen, A. 2010. Measurement of 10Be from Lake Malawi (Africa) drill core sediments and implications for geochronology. Palaeogeography, Palaeoclimatology, Palaeoecology 303(1–4):110–9.Google Scholar
Mineral Resources Authority of Mongolia Geological Survey. 1998. Geological map of Mongolia (scale 1:1,000,000 summary). Mongolian Academy of Sciences, Institute of Geology and Mineral Resources. p 4–24.Google Scholar
Monaghan, MC, Krishnaswami, S, Turekian, KK. 1986. The global-average production rate of 10Be. Earth and Planetary Science Letters 76(3–4):279–87.CrossRefGoogle Scholar
Muscheler, R, Beer, J, Wagner, G, Laj, C, Kissel, C, Raisbeck, GM, Yiou, F, Kubik, PW. 2004. Changes in the carbon cycle during the last deglaciation as indicated by the comparison of 10Be and 14C records. Earth and Planetary Science Letters 219(3–4):325–40.Google Scholar
Nagai, H, Tada, W, Kobayashi, T. 2000. Production of 7Be and 10Be in the atmosphere. Nuclear Instruments and Methods in Physics Research B 172(1–4):796–801.Google Scholar
Namkhaijantsan, G. 2006. Climate of the Hövsgöl Lake region. In: Goulden, CE, Sitnikova, T, Gelhaus, J, Bazartseren, B, editors. The Geology, Biodiversity and Ecology of Lake Hövsgöl (Mongolia). Leiden: Backhuys Publishers. p 63–76.Google Scholar
Peters, B. 1955. Radioactive beryllium in the atmosphere and on the earth. Proceedings of the Indian Academy of Sciences A 41(2):67–71.Google Scholar
Pigati, JS, Latorre, C, Rech, JA, Betancourt, JL, Martinez, KE, Budahn, JR. 2012. Accumulation of impact markers in desert wetlands and implications for the Younger Dryas impact hypothesis. Proceedings of the National Academy of Sciences of the USA 109(19):7208–12.Google Scholar
Prokopenko, AA, Bonvento, AJ. 2009. Carbonate stable isotope signals in the 1-Ma sedimentary record of the HDP-04 drill core from Lake Hovsgol, NW Mongolia. Quaternary International 205(1–2):53–64.Google Scholar
Prokopenko, A, Kuzmin, M, Williams, D, Glelety, V, Kalmychkov, G, Gvozdkov, A, Solotchin, P. 2005. Basin-wide sedimentation change and deglacial lake-level rise in the Hovsgol basin, NW Mongolia. Quaternary International 136(1):59–69.CrossRefGoogle Scholar
Raisbeck, GM, Yiou, F, Bourlès, D. 1985. Evidence for an increase in cosmogenic 10Be during a geomagnetic reversal. Nature 315(6017):315–7.Google Scholar
Reimer, PJ, Baillie, MGL, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Bronk Ramsey, C, Buck, CE, Burr, GS, Edwards, RL, Friedrich, M, Grootes, PM, Guilderson, TP, Hajdas, I, Heaton, TJ, Hogg, AG, Hughen, KA, Kaiser, KF, Kromer, B, McCormac, FG, Manning, SW, Reimer, RW, Richards, DA, Southon, JR, Talamo, S, Turney, CSM, van der Plicht, J, Weyhenmeyer, CE. 2009. IntCal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 51(4):1111–50.Google Scholar
Solotchina, EP, Prokopenko, AA, Kuzmin, MI, Slotchin, PA. 2009. Climate signals in sediment mineralogy of Lake Baikal and Lake Hovsgol during the LGM-Holocene transition and the 1-Ma carbonate record from the HDP-04 drill core. Quaternary International 205(1–2):38–52.Google Scholar
Watanabe, T, Nakamura, T, Nara, FW, Kakegawa, T, Horiuchi, K, Senda, R, Oda, T, Nishimura, M, Matsumoto, GI, Kawai, T. 2009. High-time resolution AMS 14C data sets for Lake Baikal and Lake Hovsgol sediment cores: changes in radiocarbon age and sedimentation rates during the transition from the last glacial to the Holocene. Quaternary International 205(1–2):12–20.Google Scholar
Watanabe, T, Minoura, K, Nara, FW, Shichi, K, Horiuchi, K, Kakegawa, T, Kawai, T. 2012. Last glacial to post glacial climate changes in continental Asia inferred from multi-proxy records (geochemistry, clay mineralogy, and paleontology) from Lake Hovsgol, northwest Mongolia. Global and Planetary Change 88–89:53–63.Google Scholar
Wittke, JH, Weaver, JC, Bunch, TE, Kennett, JP, Kennett, DJ, Moore, AMT, Hillman, GC, Tankersley, KB, Goodyear, AC, Moore, CR, Daniel, IR Jr, Ray, JH, Lopinot, NH, Ferraro, D, Israde-Alcántara, I, Bischoff, JL, DeCarli, PS, Hermes, RE, Kloosterman, JB, Revay, Z, Howard, GA, Kimbel, DR, Kletetschka, G, Nabelek, L, Lipo, CP, Sakai, S, West, A, Firestone, RB. 2013. Evidence for deposition of 10 million tonnes of impact, spherules across four continents 12,800 y ago. Proceedings of the National Academy of Sciences of the USA 110(23):E2088–E2097.Google Scholar