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Millennial-scale vegetation changes during the last 40,000 yr based on a pollen record from Lake Biwa, Japan

Published online by Cambridge University Press:  20 January 2017

Ryoma Hayashi ,
Hikaru Takahara ,
Akira Hayashida  and
Keiji Takemura
Ryoma Hayashi*
Affiliation:
Graduate School of Agriculture, Kyoto Prefectural University, 1-5 Hangi-cho, Shimogamo, Sakyo-ku, Kyoto, Kyoto 606-8522, Japan
Hikaru Takahara
Affiliation:
Graduate School of Life and Environmental Sciences, Kyoto Prefectural University, 1-5 Hangi-cho, Shimogamo, Sakyo-ku, Kyoto, Kyoto 606-8522, Japan
Akira Hayashida
Affiliation:
Department of Environmental Systems Science, Doshisha University, 1-3 Tatara Miyakodani, Kyotanabe, Kyoto 610-0321, Japan
Keiji Takemura
Affiliation:
Institute for Geothermal Sciences, Graduate School of Science, Kyoto University, Noguchibaru, Beppu, Oita 874-0903, Japan
*
⁎Corresponding author. Fax: +81 75 703 5683. E-mail address:hayashiryoma@gmail.com (R. Hayashi).
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Abstract

A high-resolution pollen record covering the last 40,000 yr (BIW95-4) from Lake Biwa, western Japan, shows regional vegetation responses to millennial-scale climate changes. From 40 to 30 ka, Cryptomeria japonica was dominant around the lake among pinaceous conifers and deciduous broad-leaved trees. During this period, fluctuations of C. japonica are correlated with Dansgaard–Oeschger (D–O) cycles recognized from the anhysteretic remanent magnetization (ARM) record. Increases in the abundance of this taxon may have been caused by wetter summer conditions influenced by the East Asian monsoon or increased snowfall on the Sea of Japan side of the Japanese archipelago. Between 29 and 14 ka, pinaceous conifer forests mainly composed of Pinus subgenus Haploxylon, Tsuga, and Picea trees developed. At approximately 23 ka, Picea trees increased in abundance as ARM values decreased. This expansion of Picea trees has been correlated with Heinrich event (HE) 2 in the North Atlantic. At about 14 ka, the distribution of broad-leaved forest (mainly composed of deciduous oaks) began to expand after D–O 1. Evidence of significant vegetation change related to the abrupt Younger Dryas cooling event has not been found.

Keywords

D–O cyclesEast Asian monsoonLake BiwaMillennial-scale vegetation changePollen recordCharcoal record
Type
Research Article
Information
Quaternary Research , Volume 74 , Issue 1 , July 2010 , pp. 91 - 99
Copyright
University of Washington

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References

Dansgaard, W., Johnsen, S.J., Clausen, H.B., Dahl-Jensen, D., Gundestrup, N.S., Hammaer, C.U., Hvidberg, C.S., Steffensen, J.P., Sveinbjornsdottir, A.E., Jouzel, J., and Bond, G. Evidence for general instability of past climate from a 250 kyr ice-core record. Nature 364, (1993). 218–220.Google Scholar
Danzeglocke, U., Jöris, O., and Weninger, B. CalPal-2007online. http://www.calpal-online.de (2009). accessed 2009-12-31 Google Scholar
Faegri, K., Kaland, P.E., and Krzywinski, K. Textbook of Pollen Analysis. 4th ed (1989). Wiley, New York.Google Scholar
Fuji, N. Pollen analysis. Horie, S. Lake Biwa. (1984). Dr. W. Junk Publishers, Dordrecht. 497–529.Google Scholar
Fujii, S. The development of the Kurobe Fan and submarine forests around the Toyama Bay (in Japanese, with English summary). Chikyu-Kagaku (Earth Science) 78, (1965). 11–20.Google Scholar
Fukui, E. The Climate of Japan. (1977). Elsevier, Amsterdam.Google Scholar
Grimm, E.C. CONISS: a Fortran 77 program for stratigraphically constrained cluster analysis by the method of incremental sum of squares. Computer & Geoscience 13, (1987). 13–35.CrossRefGoogle Scholar
Hayashi, Y. Taxonomical and Phytogeographical Study of Japanese Conifer (in Japanese). (1960). Norin-Shuppan, Tokyo.Google Scholar
Hayashida, A., Ali, M., Kuniko, Y., Kitagawa, H., Torii, M., and Takemura, K. Environmental magnetic record and paleosecular variation data for the last 40 kyrs from the Lake Biwa sediments, central Japan. Earth Planets and Space 59, (2007). 807–814.CrossRefGoogle Scholar
Hirayama, K., and Sakimoto, M. Regeneration of Cryptomeria japonica on a sloping topography in a cool-temperate mixed forest in the snowy region of Japan. Canadian Journal of Forrest Research 33, (2003). 543–551.CrossRefGoogle Scholar
Hughen, K., Lehman, S., Southon, J., Overpeck, J., Marchal, O., Herring, C., and Turnbull, J. 14C activity and global carbon cycle changes over the past 50,000 years. Science 303, (2004). 202–207.Google Scholar
Igarashi, Y. A late glacial climatic reversion in Hokkaido, northeast Asia, inferred from the Larix pollen records. Quaternary Science Review 15, (1996). 989–995.Google Scholar
Igarashi, Y., Igarashi, T., Daimaru, H., Yamada, O., Miyagi, T., Matsushita, K., and Hiramatsu, K. Vegetation history of Kenbuchi basin and Furano basin in Hokkaido, north Japan, since 32,000 yrs BP (in Japanese, with English summary). Daiyonki-Kenkyu (The Quaternary Research) 32, (1993). 89–105.Google Scholar
Inoue, J., Takahara, H., Yoshikawa, S., and Inouch, Y. Reconstruction of fire history during the last 130 ka by analysis of microscopic charcoal in Lake Biwa sediment (in Japanese, with English summary). Daiyonki-Kenkyu (The Quaternary Research) 40, (2001). 97–104.CrossRefGoogle Scholar
Irino, T., and Tada, R. High-resolution reconstruction of variation in aeolian dust (Kosa) deposition at ODP site 797, the Japan Sea, during the last 200 ka. Global and Planetary Change 35, (2002). 143–156.Google Scholar
Iwamoto, N., and Inouchi, Y. Reconstruction of millennial-scale variations in the East Asian summer monsoon over the past 300 ka based on the total carbon content of sediment from Lake Biwa, Japan. Environmental Geology 52, (2007). 1607–1616.CrossRefGoogle Scholar
Japan Meteorological Agency Normals for the Period 1971–2000 (CD-ROM). (2001). Japan Meteorological Business Support Center, Tokyo.Google Scholar
Kitagawa, H., and Van der Plicht, J. A 40,000 year varve chronology from Lake Suigetsu, Japan: extension of the radiocarbon calibration curve. Radiocarbon 40, (1998). 505–516.Google Scholar
Kumon, F., Kawai, S., and Inouchi, Y. Climate changed between 25,000 and 6,000 yrsBP deduced from TOC, TN, and fossil pollen analyses of a sediment core from Lake Nojiri, central Japan (in Japanese, with English summary). Daiyonki-Kenkyu (The Quaternary Research) 42, (2003). 13–26.CrossRefGoogle Scholar
Kuwae, M., Yoshikawa, S., Tsugeki, N., and Inouchi, Y. Reconstruction of a climate record for the past 140 kyr based on diatom valve flux data from Lake Biwa, Japan. Journal of Paleolimnology 32, (2004). 19–39.Google Scholar
Lisiecki, L.E., and Raymo, M.E. A Pliocene–Pleistocene stack of 57 globally distributed benthic d18O records. Paleoceanography 20, (2005). doi:10.1029/2004PA001071 PA1003 Google Scholar
MacDonald, G.M., Larsen, C.P.S., Szeicz, J.M., and Moser, K.A. The reconstruction of boreal forest fire history from lake sediments: a comparison of charcoal, pollen, sedimentological, and geochemical indices. Quaternary Science Reviews 10, (1991). 53–71.Google Scholar
Maekawa, F. General geography of Japan and its relationship to the flora. Numata, M. The Flora and Vegetation of Japan. Copublished. (1974). Kodansha, Tokyo. 2–20. Elsevier Scientific, Amsterdam Google Scholar
Matsui, T., Yagihashi, T., Nakaya, T., Tanaka, N., and Taoda, H. Climatic controls on distribution of Fagus crenata forests in Japan. Journal of Vegetation Science 15, (2004). 57–66.Google Scholar
Meyers, P.A., Takemura, K., and Horie, S. Reinterpretation of Late Quaternary sediment chronology of Lake Biwa, Japan, from correlation with marine glacial–interglacial cycles. Quaternary Research 39, (1993). 154–162.Google Scholar
Minaki, M., and Matsuba, C. Plant macrofossil assemblage from about 18 000 years ago in Tado-cho, Mie Prefecture, central Japan (in Japanese, with English summary). Daiyonki-Kenkyu (The Quaternary Research) 24, (1985). 51–55.Google Scholar
Miyoshi, N., Fujiki, T., and Morita, Y. Palynilogy of a 250 m core from Lake Biwa: a 430,000 year record of glacial–interglacial vegetation change in Japan. Review of Palaeobotany and Palynology 104, (1999). 267–283.Google Scholar
Nagashima, K., Tada, R., Matsui, H., Irino, T., Tani, A., and Toyoda, S. Orbital- and millennial-scale variations in Asian dust transport path to the Japan Sea. Palaeogeography, Palaeoclimatology, Palaeoecology 247, (2007). 144–161.Google Scholar
Nakagawa, T., Kitagawa, H., Yasuda, Y., Tarasov, P.E., Nishida, K., Gotanda, K., and Sawai, Y. Asynchronous climate changes in the North Atlantic and Japan during the Last Termination. Science 299, (2003). 688–691.Google Scholar
Nakagawa, T., Kitagawa, H., Yasuda, Y., Tarasov, P.E., Gotanda, K., and Sawai, Y. Pollen/event stratigraphy of the varved sediment of Lake Suigetsu, central Japan from 15,701 to 10,217 SG vyr BP (Suigetsu varve years before present): description, interpretation, and correlation with other regions. Quaternary Science Review 24, (2005). 1691–1701.CrossRefGoogle Scholar
Nakagawa, T., Tarasov, P.E., Kitagawa, H., Yasuda, Y., Gotanda, K., and Horie, S. Seasonally specific responses of the East Asian monsoon to deglacial climate changes. Geology 34, (2006). 521–524.Google Scholar
Nakashizuka, T., and Iida, S. Composition, dynamics and disturbance regime of temperate deciduous forests in Monsoon Asia. Vegitatio 121, (1995). 23–30.Google Scholar
North Greenland Ice Core Project members High-resolution record of Northern Hemisphere climate extending into the last interglacial period. Nature 431, (2004). 147–151.CrossRefGoogle Scholar
Ogden, J.G. III An alternative to exotic spore or pollen addition in quantitative microfossil studies. Canadian Journal of Earth Science 23, (1986). 102–106.Google Scholar
Sánchez Goñi, M.F., Landais, A., Fletcher, W.J., Naughton, F., Desprat, S., and Duprat, J. Contrasting impacts of Dansgaard–Oeschger events over a western European latitudinal transect modulated by orbital parameters. Quaternary Science Reviews 27, (2008). 1136–1151.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, G., Van der Plicht, J., and Spurk, M. INTCAL98 radiocarbon age calibration, 24,000–0 cal BP. Radiocarbon 40, (1998). 1041–1083.CrossRefGoogle Scholar
Tada, R., Irino, T., and Koizumi, I. Land–ocean linkages over orbital and millennial timescale records in late Quaternary sediments of the Japan Sea. Paleoceanography 14, (1999). 236–247.Google Scholar
Takahara, H., and Kitagawa, H. Vegetation and climate history since the last interglacial in Kurota Lowland, western Japan. Palaeogepgraphy, Palaeoclimatology, Palaeoecology 155, (2000). 123–134.Google Scholar
Takahara, H., and Takeoka, M. Buried forest of Cryptomeria japonica D. Don in Kurota, Mikata-cho, Mikata-gun, Fukui Prefecture. Bulletin of the Kyoto Prefectural University Forests 34, (1990). 75–81.Google Scholar
Takahara, H., and Takeoka, M. Vegetation history since the last glacial period in the Mikata lowland, the Sea of Japan area, western Japan. Ecological Research 7, (1992). 371–386.Google Scholar
Takahara, H., Uemura, Y., and Danhara, T. The vegetation and climate history during the early and mid last glacial period in Kamiyoshi Basin, Kyoto, Japan. Japanese Journal of Palynology 46, (2000). 133–146.Google Scholar
Takahara, H., Igarashi, Y., Hayashi, R., Kumon, F., Liew, P.M., Yamamoto, M., Kawai, S., Oba, T., Irino, T., in press. Millennial-scale variability in vegetation records from the East Asian Islands: Taiwan, Japan and Sakhalin. Quaternary Science Reviews, doi:10.1016/j.quascirev.2009.11.026.Google Scholar
Takemura, K., Hayashida, A., Okamura, M., Matsuoka, H., Ali, M., Kuniko, Y., and Torii, M. Stratigraphy of multiple piston-core sediments for the last 30,000 years from Lake Biwa, Japan. Journal of Paleolimnology 23, (2000). 185–199.CrossRefGoogle Scholar
Tinner, W., Conedera, M., Ammann, B., Ga¨ggeler, H.W., Gedye, S., Jones, R., and Sagesser, B. Pollen and charcoal in lake sediments compared with historically documented forest fires in southern Switzerland since AD 1920. Holocene 8, (1998). 31–42.Google Scholar
Toyoda, S., and Naruse, T. Eolian dust from Asian deserts to Japanese island since the last Glacial Maximum: the basis for the ESR method. Transactions, Japan Geomorphological Union 23, (2002). 811–820.Google Scholar
Tsukada, M. Vegetation and climate during the last glacial maximum in Japan. Quaternary Research 19, (1983). 212–235.Google Scholar
Tsukada, M. Map of vegetation during the last glacial maximum in Japan. Quaternary Research 23, (1985). 369–381.Google Scholar
Voelker, A.H.L. Global distribution of centennial-scale records for Marine Isotope Stage (MIS) 3: a database. Quaternary Science Review 21, (2002). 1185–1212.Google Scholar
Wang, Y.J., Cheng, H., Edwards, R.L., An, Z.S., Wu, J.Y., Shen, C.C., and Dorale, J.A. A high-resolution absolute-dated late Pleistocene monsoon record from Hulu Cave, China. Science 294, (2001). 2345–2348.Google Scholar
Wang, Y., Cheng, H., Edwards, R.L., Kong, X., Shao, X., Chen, S., Wu, J., Jiang, X., Wang, X., and An, Z. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature 451, (2008). 1090–1093.CrossRefGoogle Scholar
Wang, L., and Oba, T. Tele-connection between East Asian monsoon and high-latitude climate: a comparison between the GISP2 ice core record and the high resolution marine records from the Japan and the South China Seas. Daiyonki-Kenkyu (The Quaternary Research) 37, (1998). 211–219.CrossRefGoogle Scholar
Whitlock, C., and Larsen, C. Charcoal as a fire proxy. Smol, J.P., Birks, H.J.B., and Last, W.M. Tracking Environmental Change using Lake Sediments. Terrestrial, Algal, and Siliceous Indicators 3, (2001). Kluwer Academic Publisher, Dordrecht. 75–97.Google Scholar
Yamada, K. Last 40 ka climate changes as deduced from the lacustrine sediments of Lake Biwa, central Japan. Quaternary International 123–125, (2004). 43–50.Google Scholar
Yasuda, Y., Yamaguchi, K., Nakagawa, T., Fukusawa, H., Kitagawa, J., and Okamura, M. Environmental variability and human adaptation during the Lateglacial/Holocene transition in Japan with reference to pollen analysis of the SG4 core from Lake Suigetsu. Quaternary International 123, (2004). 11–19.CrossRefGoogle Scholar
Yuan, D., Cheng, H., Edwards, R.L., Dykoski, C.A., Kelly, M.J., Zhang, M., Qing, J., Lin, Y., Wang, Y., Wu, J., Dorale, J.A., An, Z., and Cai, Y. Timing, duration, and transitions of the last interglacial Asian monsoon. Science 304, (2004). 575–578.Google Scholar