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Radiocarbon and Stable Carbon Isotope Ratio Data from a 4.7-Mlong Sediment Core of Lake Baikal (Southern Siberia, Russia)

Published online by Cambridge University Press:  18 July 2016

Fumiko Watanabe Nara ,
Takahiro Watanabe ,
Toshio Nakamura ,
Takeshi Kakegawa ,
Fumitaka Katamura ,
Koji Shichi ,
Hikaru Takahara ,
Akio Imai  and
Takayoshi Kawai
Fumiko Watanabe Nara*
Affiliation:
Graduate School of Science, Tohoku University, 6-3 Aramaki Aza Aoba, Aoba-ku, Sendai 980–8578, Japan
Takahiro Watanabe
Affiliation:
Graduate School of Science, Tohoku University, 6-3 Aramaki Aza Aoba, Aoba-ku, Sendai 980–8578, Japan
Toshio Nakamura
Affiliation:
Center for Chronological Research, Nagoya University, Furo-cho, Chikusa, Nagoya 464-8602, Japan
Takeshi Kakegawa
Affiliation:
Graduate School of Science, Tohoku University, 6-3 Aramaki Aza Aoba, Aoba-ku, Sendai 980–8578, Japan
Fumitaka Katamura
Affiliation:
Graduate School of Agriculture, Kyoto Prefectural Univ., 1-5 Hangi-cho Shimogamo Sakyo-ku, Kyoto 606-8522, Japan
Koji Shichi
Affiliation:
Forestry and Forest Products Research Institute, 1 Matsunosato, Tsukuba, Ibaraki 305-8687, Japan
Hikaru Takahara
Affiliation:
Graduate School of Agriculture, Kyoto Prefectural Univ., 1-5 Hangi-cho Shimogamo Sakyo-ku, Kyoto 606-8522, Japan
Akio Imai
Affiliation:
National Institute for Environmental Studies, 16-2 Onogawa, Tsukuba, Ibaraki 305-8506, Japan
Takayoshi Kawai
Affiliation:
Graduate School of Environmental Studies, Nagoya University, Furo-cho, Chikusa, Nagoya 464-8602, Japan
*
Corresponding author. Email: narafumi@m.tains.tohoku.ac.jp.
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Abstract

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A sediment core (VER99G12; core length, 4.66 m) was taken from the Buguldeika Saddle of Lake Baikal in 1999. Radiocarbon measurements of total organic carbon (TOC) and pollen concentrate fractions from the VER99G12 core were performed by a Tandetron accelerator mass spectrometry (AMS) system (Model-4130, HVEE) at Nagoya University. The AMS 14C ages showed that the VER99G12 core spans the past ∼30 cal ka BP (from the MIS 3 to present), and the average sedimentation rate of this core was calculated to be 13.6 cm/kyr based on the calibrated ages. This means that the time resolution of VER99G12 sediment samples in this study is better than ∼70–80 yr/cm. Stable carbon isotope ratios of TOC (δ13CTOC) in the VER99G12 core varied widely from about 26.6‰ to 31.3‰ during the last glacial/post-glacial transition period (about 17–12 cal ka BP). Therefore, a rapid change in the carbon sources in Lake Baikal occurred in the last glacial/post-glacial transition period is concluded.

Type
Soils and Sediments
Information
Radiocarbon , Volume 52 , Issue 3: 20th Int. Radiocarbon Conference Proceedings , 2010 , pp. 1449 - 1457
Copyright
Copyright © 2010 by the Arizona Board of Regents on behalf of the University of Arizona 

References

Boës, X, Piotrowska, N, Fagel, N. 2005. High-resolution diatom/clay record in Lake Baikal from grey scale, and magnetic susceptibility over Holocene and Termination I. Global and Planetary Change 46(1–4):299–313.CrossRefGoogle Scholar
Brown, TA, Nelson, DE, Mathewes, RW, Vogel, JS, Southon, JR. 1989. Radiocarbon dating of pollen by accelerator mass spectrometry. Quaternary Research 32(2):205–12.CrossRefGoogle Scholar
Falkner, KK, Measures, CI, Herbelin, SE, Edmond, JM, Weiss, RF. 1991. The major and minor element geochemistry of Lake Baikal. Limnology and Oceanography 36(3):413–23.CrossRefGoogle Scholar
Fuchs, M, Buerkert, A. 2008. A 20 ka sediment record from the Hajar Mountain range in N-Oman, and its implication for detecting arid-humid periods on the southeastern Arabian Peninsula. Earth and Planetary Science Letters 265(3–4):546–58.CrossRefGoogle Scholar
Horiuchi, K, Minoura, K, Hoshino, K, Oda, T, Nakamura, T, Kawai, T. 2000. Palaeoenvironmental history of Lake Baikal during the last 23000 years. Palaeogeography, Palaeoclimatology, Palaeoecology 157(1–2):95–108.CrossRefGoogle Scholar
Hughen, KA, Southon, JR, Lehman, SJ, Overpeck, JT. 2000. Synchronous radiocarbon and climate shifts during the last deglaciation. Science 290(5498):1951–4.CrossRefGoogle ScholarPubMed
Huon, S, Grousset, FE, Burdloff, D, Bardoux, G, Mariotti, A. 2002. Sources of fine-sized organic matter in North Atlantic Heinrich Layers: δ13C and δ15N tracers. Geochimca et Cosmochimica Acta 66(2):223–39.CrossRefGoogle Scholar
Hutchinton, DR, Golmshtok, AJ, Zonenshain, LP, Moore, TC, Scholz, CA, Klitgord, KD. 1992. Depositional and tectonic framework of the rift basins of Lake Baikal from multichannel seismic data. Geology 20(7):589–92.Google Scholar
Kuzumin, MI, Williams, DF, Kawai, T. 2000. Baikal drilling project. In: Minoura, K, editor. A Mirror in Time and Space for Understanding Global Change Processes. Amsterdam: Elsevier. p 1–14.Google Scholar
Lang, A, Hönscheidt, S. 1999. Age and source of colluvial sediments at Vaihingen-Enz, Germany. Catena 38(2):89–107.CrossRefGoogle Scholar
Matsumoto, GI, Kosaku, S, Takamatsu, N, Akagi, T, Kawai, T, Ambe, Y. 2000. Estimation of paleoenvironmental changes in the Eurasian continental interior during the past 5 million years inferred from organic components in the BDP96 Hole1 sediment core from Lake Baikal. In: Minoura, K, editor. A Mirror in Time and Space for Understanding Global Change Processes. Amsterdam: Elsevier. p 119–35.Google Scholar
Meyers, PA. 1997. Organic geochemical proxies of paleoceanographic, paleolimnologic, and paleoclimatic processes. Organic Geochemistry 27(5–6):213–50.CrossRefGoogle Scholar
Nakamura, T, Oda, T, Tanaka, A, Horiuchi, K. 2003. High precision 14C age estimation of bottom sediments of Lake Baikal and Lake Hovsgol by AMS. Gekkan Chikyu No. 42. Tokyo: Kaiyoushuppan. p 20–31. In Japanese.Google Scholar
Nara, F, Tani, N, Soma, Y, Soma, M, Naraoka, H, Watanabe, T, Horiuchi, K, Kawai, T, Oda, T, Nakamura, T. 2005. Response of phytoplankton productivity to climate change recorded by sedimentary photosynthetic pigments in Lake Hovsgol (Mongolia) for the last 23,000 years. Quaternary International 136(1):71–81.CrossRefGoogle Scholar
Piotrowska, N, Bluszcz, A, Demske, D, Granoszewski, W, Heumann, G. 2004. Extraction and AMS radiocarbon dating of pollen from Lake Baikal sediments. Radiocarbon 46(1):181–7.CrossRefGoogle Scholar
Prokopenko, AA, Williams, DF. 2004. Deglacial methane emission signals in the carbon isotopic record of Lake Baikal. Earth and Planetary Science Letters 218(1–2):135–47.CrossRefGoogle Scholar
Prokopenko, AA, Williams, DF, Karabanov, EB, Khursevich, GB. 1999. Response of Lake Baikal ecosystem to climate forcing and pCO2 change over the last glacial/interglacial transition. Earth and Planetary Science Letters 172(3–4):239–53.CrossRefGoogle Scholar
Prokopenko, AA, Khursevich, GK, Bezrukova, EV, Kuzmin, MI, Boës, X, Williams, DF, Fedenya, SA, Kulagina, NV, Letunova, PP, Abzaeva, AA. 2007. Paleoenvironmental proxy records from Lake Hovsgol, Mongolia, and a synthesis of Holocene climate change in the Lake Baikal watershed. Quaternary Research 68(1):2–17.CrossRefGoogle Scholar
Reimer, PJ, Baillie, MGL, Bard, E, Bayliss, A, Beck, JW, Bertrand, CJH, Blackwell, PG, Buck, CE, Burr, GS, Cutler, KB, Damon, PE, Edwards, RL, Fairbanks, RG, Friedrich, M, Guilderson, TP, Hogg, AG, Hughen, KA, Kromer, B, McCormac, G, Manning, S, Bronk Ramsey, C, Reimer, RW, Remmele, S, Southon, JR, Stuiver, M, Talamo, S, Taylor, FW, van der Plicht, J, Weyhenmeyer, CE. 2004. IntCal04 terrestrial radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon 46(3):1029–58.Google Scholar
Short, DA, Mengel, JG, Growley, TJ, Hyde, WT, North, GR. 1991. Filtering of Milankovitch cycles by Earth's geography. Quaternary Research 35(2):157–71.CrossRefGoogle Scholar
Soma, Y, Tani, Y, Soma, M, Mitake, H, Kurihara, R, Hashomoto, S, Watanabe, T, Nakamura, T. 2007. Sedimentary steryl chlorine esters (SCEs) and other photosyntehtic pigments as indicators of paleolimnological change over the last 28,000 years from the Buguldeika Saddle of Lake Baikal. Journal of Paleolimnology 37(2):163–75.CrossRefGoogle Scholar
Stuiver, M, Grootes, PM, Braziunas, TF. 1995. The GISP2 δ18O climate record of the past 16,500 years and the role of the sun, ocean and volcanoes. Quaternary Research 44(3):341–54.CrossRefGoogle Scholar
Watanabe, T. 2004. Environmental and biological changes in Eurasian continental interior by stable isotopes and organic geochemical records from Lake Baikal sediment core [PhD thesis]. Tokyo: Tokyo Metropolitan University. p 101–43.Google Scholar
Watanabe, T, Naraoka, H, Nishimura, M, Kawai, T. 2004. Biological and environmental changes at Lake Baikal during the late Quaternary inferred from carbon, nitrogen and sulfur isotopes. Earth and Planetary Science Letters 222(1):285–99.CrossRefGoogle Scholar
Watanabe, T, Tanaka, A, Nara, F, Nakamura, T, Senda, R, Nishimura, M, Kawai, T. 2005. Paleoproductivity changes in Lake Baikal over the past 250,000 years. Verhandlungen der Internationalen Vereinigung fur Theoretische und Angewandte Limnologie 29(2):903–6.Google Scholar
Watanabe, T, Nakamura, T, Kawai, T. 2007. Radiocarbon dating of sediments from large continental lakes (Lakes Baikal, Hovsgol and Erhel). Nuclear Instruments and Methods in Physics Research B 259(1):565–70.CrossRefGoogle Scholar
Watanabe, T, Nakamura, T, Nara, FW, Kakegawa, T, Horiuchi, K, Senda, R, Oda, T, Nishimura, M, Matsumoto, GI, Kawai, T. 2009a. 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.CrossRefGoogle Scholar
Watanabe, T, Nakamura, T, Nara, FW, Kakegawa, T, Nishimura, M, Shimokawara, M, Matsunaka, T, Senda, R, Kawai, T. 2009b. A new age model for the sediment cores from Academician Ridge (Lake Baikal) based on high-time-resolution AMS 14C data sets over the last 30 kyr: paleoclimatic and environmental implications. Earth and Planetary Science Letters 286(3–4):347–54.CrossRefGoogle Scholar
Watanabe, T, Matsunaka, T, Nakamura, T, Nishimura, M, Nara, FW, Kakegawa, T, Zhu, L. 2009c. Changes of organic matter sources in sediment cores from a high-altitude lake (Pumoyum Co, southeastern Tibetan plateau) over the last 19,000 years. Nuclear Instruments and Methods in Physics Research B 268(7–8):1070–2.Google Scholar
Yamamoto, S, Ishiwatari, R. 1995. Alkaline CuO oxidation of Lake Baikal sediments. Research in Organic Geochemistry 10:27–31. In Japanese.Google Scholar