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Mid- to late Holocene cooling events in the Korean Peninsula and their possible impact on ancient societies

Published online by Cambridge University Press:  01 March 2019

Mark Constantine ,
Minkoo Kim  and
Jungjae Park
Mark Constantine
Affiliation:
Department of Geography, Seoul National University, 1 Gwanak-ro, Gwanak-gu, Seoul, 151-742, Republic of Korea
Minkoo Kim
Affiliation:
Department of Anthropology, Chonnam National University, 77 Yongbong-ro, Buk-gu, Gwangju 61186, Republic of Korea
Jungjae Park*
Affiliation:
Department of Geography, Seoul National University, 1 Gwanak-ro, Gwanak-gu, Seoul, 151-742, Republic of Korea Institute for Korean Regional Studies, Seoul National University, 1 Gwanak-ro, Gwanak-gu, Seoul 08826, Republic of Korea
*
*Corresponding author e-mail address: [email protected]
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Abstract

We present a multiproxy record using pollen, magnetic susceptibility, carbon isotopic composition, carbon/nitrogen ratio, and particle size of mid- to late Holocene environmental changes based on a sediment core from the Pomaeho lagoon on the east coast of Korea. The records indicate that climate deteriorations around 6400 cal yr BP and 4000 cal yr BP caused rapid vegetation changes in the study area, which were presumably attributable to low sunspot activity and strong El Niño–like conditions, respectively. These two cooling events were likely modulated by different climate mechanisms, as El Niño–Southern Oscillation activity began to strengthen around 5000 cal yr BP. These events may have had a substantial impact on ancient societies in the study area. Combining our results with archaeological findings indicated that climate deterioration led to drastic declines in local populations around 6400 cal yr BP, 4400 cal yr BP, and 4000 cal yr BP. Because of its high population, coastal East Asia (e.g., eastern China, Japan, and Korea) is particularly vulnerable to potential cooling events in the future. Therefore, there is a strong need for detailed paleoclimate information in this region.

Keywords

Ancient societiesCooling eventsHoloceneKoreaVegetation
Type
Research Article
Information
Quaternary Research , Volume 92 , Issue 1 , July 2019 , pp. 98 - 108
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2019 

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References

REFERENCES

Ahn, S.-M., 2010. The emergence of rice agriculture in Korea: archaeobotanical perspectives. Archaeological and Anthropological Sciences 2, 89–98.Google Scholar
Alley, R.B., Ágústsdóttir, A.M., 2005. The 8k event: cause and consequences of a major Holocene abrupt climate change. Quaternary Science Reviews 24, 1123–1149.Google Scholar
Alley, R.B., Mayewski, P.A., Sowers, T., Stuiver, M., Taylor, K.C., Clark, P.U., 1997. Holocene climatic instability: a prominent, widespread event 8200 yr ago. Geology 25, 483–486.Google Scholar
Barber, D., Dyke, A., Hillaire-Marcel, C., Jennings, A., Andrews, J., Kerwin, M., Bilodeau, G., McNeely, R., Southon, J., Morehead, M., 1999. Forcing of the cold event of 8,200 years ago by catastrophic drainage of Laurentide lakes. Nature 400, 344–348.Google Scholar
Bender, M.M., 1971. Variations in the 13C/12C ratios of plants in relation to the pathway of photosynthetic carbon dioxide fixation. Phytochemistry 10, 1239–1244.Google Scholar
Blaauw, M., Christen, J.A., 2011. Flexible paleoclimate age-depth models using an autoregressive gamma process. Bayesian Analysis 6, 457–474.Google Scholar
Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M.N., Showers, W., Hoffmann, S., Lotti-Bond, R., Hajdas, I., Bonani, G., 2001. Persistent solar influence on North Atlantic climate during the Holocene. Science 294, 2130–2136.Google Scholar
Bronk Ramsey, C., 2017. OxCal 4.3 Manual (accessed Feburuary 1, 2018). http://c14.arch.ox.ac.uk/oxcalhelp/hlp_contents.html.Google Scholar
Chang, N.K., 1986. Illustrated Flora & Fauna of Korea. Vol. 29, Pollen. [In Korean.] Ministry of Education, Seoul.Google Scholar
Chiba, T., Sugihara, S., Matsushima, Y., Arai, Y., Endo, K., 2016. Reconstruction of Holocene relative sea-level change and residual uplift in the Lake Inba area, Japan. Palaeogeography, Palaeoclimatology, Palaeoecology 441, 982–996.Google Scholar
Choe, C.P., Bale, M.T., 2002. Current perspectives on settlement, subsistence, and cultivation in prehistoric Korea. Arctic Anthropology 39, 95–121.Google Scholar
Clark, P.U., Marshall, S.J., Clarke, G.K., Hostetler, S.W., Licciardi, J.M., Teller, J.T., 2001. Freshwater forcing of abrupt climate change during the last glaciation. Science 293, 283–287.Google Scholar
Conroy, J.L., Overpeck, J.T., Cole, J.E., Shanahan, T.M., Steinitz-Kannan, M., 2008. Holocene changes in eastern tropical Pacific climate inferred from a Galápagos lake sediment record. Quaternary Science Reviews 27, 1166–1180.Google Scholar
Crawford, G.W., Lee, G.-A., 2003. Agricultural origins in the Korean Peninsula. Antiquity 77, 87–95.Google Scholar
Cullen, H.M., Hemming, S., Hemming, G., Brown, F., Guilderson, T., Sirocko, F., 2000. Climate change and the collapse of the Akkadian empire: evidence from the deep sea. Geology 28, 379–382.Google Scholar
Dixit, Y., Hodell, D.A., Petrie, C.A., 2014. Abrupt weakening of the summer monsoon in northwest India ~4100 yr ago. Geology 42, 339–342.Google Scholar
Donders, T.H., Wagner-Cremer, F., Visscher, H., 2008. Integration of proxy data and model scenarios for the mid-Holocene onset of modern ENSO variability. Quaternary Science Reviews 27, 571–579.Google Scholar
Faegri, K., Iversen, J., 1989. Textbook of Pollen Analysis. 4th ed. Wiley, Chichester, UK.Google Scholar
Fagan, B.M., 2000. The Little Ice Age: How Climate Made History, 1300–1850. Basic Books, New York.Google Scholar
Farquhar, G.D., Ehleringer, J.R., Hubick, K.T., 1989. Carbon isotope discrimination and photosynthesis. Annual Review of Plant Biology 40, 503–537.Google Scholar
Fujiki, T., Yasuda, Y., 2004. Vegetation history during the Holocene from Lake Hyangho, northeastern Korea. Quaternary International 123, 63–69.Google Scholar
Grimm, E.C., 1987. CONISS: a FORTRAN 77 program for stratigraphically constrained cluster analysis by the method of incremental sum of squares. Computers & Geosciences 13, 13–35.Google Scholar
Hu, C., Henderson, G.M., Huang, J., Xie, S., Sun, Y., Johnson, K.R., 2008. Quantification of Holocene Asian monsoon rainfall from spatially separated cave records. Earth and Planetary Science Letters 266, 221–232.Google Scholar
Innes, J.B., Zong, Y., Wang, Z., Chen, Z., 2014. Climatic and palaeoecological changes during the mid-to Late Holocene transition in eastern China: high-resolution pollen and non-pollen palynomorph analysis at Pingwang, Yangtze coastal lowlands. Quaternary Science Reviews 99, 164–175.Google Scholar
Katsuki, K., Nakanishi, T., Lim, J., Nahm, W.-H., 2017. Holocene salinity fluctuations of the East Korean lagoon related to sea level and precipitation changes. Island Arc 26, e12214.Google Scholar
Kawahata, H., Yamamoto, H., Ohkushi, K., Yokoyama, Y., Kimoto, K., Ohshima, H., Matsuzaki, H., 2009. Changes of environments and human activity at the Sannai-Maruyama ruins in Japan during the mid-Holocene Hypsithermal climatic interval. Quaternary Science Reviews 28, 964–974.Google Scholar
Kim, J., 2002. The Late Neolithic-Early Bronze Age transition in South Korea: a new hypothesis. Journal of the Korean Archaeological Society 48, 93–133.Google Scholar
Kim, J.C., Bae, C.J., 2010. Radiocarbon dates documenting the Neolithic-Bronze Age transition in Korea. Radiocarbon 52, 483–492.Google Scholar
Kim, M., Park, J., 2011. Prehistoric rice cultivation and agricultural intensification in the Yeongdong region, Gwangwon, South Korea. [In Korean.] Journal of Korean Archaeological Society 79, 67–88.Google Scholar
Kim, M., Shin, H.N., Kim, S., Lim, D.J., Jo, K., Ryu, A., Won, H., Oh, S., Noh, H., 2015. Population and social aggregation in the Neolithic Chulmun villages of Korea. Journal of Anthropological Archaeology 40, 160–182.Google Scholar
Ko, D., 2012. Stratigraphic relationship of Osan-ri style and Yunggimun pottery of eastern coast. In: Jungang Institute of Cultural Heritage (Ed.), Characteristics and Developments of Korean Neolithic Period. [In Korean.] Seogyeong Munhwasa, Seoul, pp. 85–108.Google Scholar
Ko, D., Hong, S., 2007. Consideration on pottery excavated from the lower layer of Osan-ri II. [In Korean.] Journal of Gangwon Archaeological Society 9, 27–68.Google Scholar
Korean Archaeological Society, 2012. Lectures on Korean Archaeology. 2nd ed. Sahwe Pyeongron, Seoul.Google Scholar
Korea Meteorolgical Administration, 2018. Climate Information (accessed January 10, 2018). http://www.weather.go.kr/weather/main.jspGoogle Scholar
Koutavas, A., Olive, G.C., Lynch-Stieglitz, J., 2006. Mid-Holocene El Niño–Southern Oscillation (ENSO) attenuation revealed by individual foraminifera in eastern tropical Pacific sediments. Geology 34, 993–996.Google Scholar
Kunikida, D., Yoshida, K., 2007. Dating of Goseong Munam-ri pottery and opinion. Munhwajae 40, 431–438.Google Scholar
Li, G., Li, P., Liu, Y., Qiao, L., Ma, Y., Xu, J., Yang, Z., 2014. Sedimentary system response to the global sea level change in the East China Seas since the last glacial maximum. Earth-Science Reviews 139, 390–405.Google Scholar
Lim, J., Fujiki, T., 2011. Vegetation and climate variability in East Asia driven by low-latitude oceanic forcing during the middle to late Holocene. Quaternary Science Reviews 30, 2487–2497.Google Scholar
Liu, F., Feng, Z., 2012. A dramatic climatic transition at ~4000 cal. yr BP and its cultural responses in Chinese cultural domains. Holocene 22, 1181–1197.Google Scholar
MacDonald, G.M., Moser, K.A., Bloom, A.M., Potito, A.P., Porinchu, D.F., Holmquist, J.R., Hughes, J., Kremenetski, K.V., 2016. Prolonged California aridity linked to climate warming and Pacific sea surface temperature. Scientific Reports 6, 33325.Google Scholar
Mayewski, P.A., Rohling, E.E., Stager, J.C., Karlén, W., Maasch, K.A., Meeker, L.D., Meyerson, E.A., Gasse, F., van Kreveld, S., Holmgren, K., 2004. Holocene climate variability. Quaternary Research 62, 243–255.Google Scholar
McGranahan, G., Balk, D., Anderson, B., 2007. The rising tide: assessing the risks of climate change and human settlements in low elevation coastal zones. Environment and Urbanization 19, 17–37.Google Scholar
Meyers, P.A., 1994. Preservation of elemental and isotopic source identification of sedimentary organic matter. Chemical Geology 114, 289–302.Google Scholar
Moy, C.M., Seltzer, G.O., Rodbell, D.T., Anderson, D.M., 2002. Variability of El Niño/Southern Oscillation activity at millennial timescales during the Holocene epoch. Nature 420, 162–165.Google Scholar
Nakanishi, T., Hong, W., Sung, K.S., Nakashima, R., Nahm, W.-H., Lim, J., Katsuki, K., 2017. Offset in radiocarbon age between plant and shell pairs in Holocene sediment around the Mae-ho Lagoon on the eastern coast of Korea. Quaternary International 447, 3–12.Google Scholar
National Research Institute of Cultural Heritage, 2014. Munam-ri at Goseong. Vol. 2, Analysis. [In Korean.] National Research Institute of Cultural Heritage, Daejeon, South Korea.Google Scholar
Nelson, S.M., 1993. The Archaeology of Korea. Cambridge University Press, New York.Google Scholar
Norton, C.J., 2000. Subsistence change at Konam-ri: implications for the advent of rice agriculture in Korea. Journal of Anthropological Research 56, 325–348.Google Scholar
Norton, C.J., 2007. Sedentism, territorial circumscription, and the increased use of plant domesticates across Neolithic-Bronze Age Korea. Asian Perspectives 46, 133–165.Google Scholar
Park, J., 2017. Solar and tropical ocean forcing of late-Holocene climate change in coastal East Asia. Palaeogeography, Palaeoclimatology, Palaeoecology 469, 74–83.Google Scholar
Park, J., Han, J., Jin, Q., Bahk, J., Yi, S., 2017. The link between ENSO-like forcing and hydroclimate variability of coastal East Asia during the last millennium. Scientific Reports 7, 8166.Google Scholar
Park, J., Shin, Y.H., 2012. Late-Holocene rice agriculture and palaeoenvironmental change in the Yeongdong region, Gangwon, South Korea. [In Korean.] Journal of the Korean Geographical Society 47, 641–653.Google Scholar
Park, J., Shin, Y.H., Byrne, R., 2016. Late-Holocene vegetation and climate change in Jeju Island, Korea and its implications for ENSO influences. Quaternary Science Reviews 153, 40–50.Google Scholar
Park, J., Yu, K.B., Lim, H.S., Shin, Y.H., 2012. Holocene environmental changes on the east coast of Korea. Journal of Paleolimnology 48, 535–544.Google Scholar
Parker, A.G., Goudie, A.S., Anderson, D.E., Robinson, M.A., Bonsall, C., 2002. A review of the mid-Holocene elm decline in the British Isles. Progress in Physical Geography 26, 1–45.Google Scholar
Prahl, F.G., Bennett, J.T., Carpenter, R., 1980. The early diagenesis of aliphatic hydrocarbons and organic matter in sedimentary particulates from Dabob Bay, Washington. Geochimica et Cosmochimica Acta 44, 1967–1976.Google Scholar
Rahmstorf, S., Feulner, G., Mann, M.E., Robinson, A., Rutherford, S., Schaffernicht, E.J., 2015. Exceptional twentieth-century slowdown in Atlantic Ocean overturning circulation. Nature Climate Change 5, 475–480.Google Scholar
Reimer, P.J., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Bronk Ramsey, C., Buck, C.E., Cheng, H., Edwards, R.L., Friedrich, M., 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55, 1869–1887.Google Scholar
Song, E.-S., 2006. Salmon and Osan-ri adaptations on the east coast of Korea. [In Korean.] Journal of the Korean Neolithic Research Society 11, 55–69.Google Scholar
Srokosz, M., Bryden, H., 2015. Observing the Atlantic Meridional Overturning Circulation yields a decade of inevitable surprises. Science 348, 1255575.Google Scholar
Stanley, J.D., Krom, M.D., Cliff, R.A., Woodward, J.C., 2003. Short contribution: Nile flow failure at the end of the Old Kingdom, Egypt: strontium isotopic and petrologic evidence. Geoarchaeology 18, 395–402.Google Scholar
Steinhilber, F., Beer, J., Fröhlich, C., 2009. Total solar irradiance during the Holocene. Geophysical Research Letters 36, L19704.Google Scholar
Stockmarr, J., 1971. Tablets with spores used in absolute pollen analysis. Pollen et Spores 13, 614–621.Google Scholar
Stott, L., Cannariato, K., Thunell, R., Haug, G.H., Koutavas, A., Lund, S., 2004. Decline of surface temperature and salinity in the western tropical Pacific Ocean in the Holocene epoch. Nature 431, 56–59.Google Scholar
Tanigawa, K., Hyodo, M., Sato, H., 2013. Holocene relative sea-level change and rate of sea-level rise from coastal deposits in the Toyooka Basin, western Japan. Holocene 23, 1039–1051.Google Scholar
Teller, J.T., Leverington, D.W., Mann, J.D., 2002. Freshwater outbursts to the oceans from glacial Lake Agassiz and their role in climate change during the last deglaciation. Quaternary Science Reviews 21, 879–887.Google Scholar
Thompson, L.G., Mosley-Thompson, E., Davis, M.E., Henderson, K.A., Brecher, H.H., Zagorodnov, V.S., Mashiotta, T.A., Lin, P.-N., Mikhalenko, V.N., Hardy, D.R., 2002. Kilimanjaro ice core records: evidence of Holocene climate change in tropical Africa. Science 298, 589–593.Google Scholar
Wang, J., Sun, L., Chen, L., Xu, L., Wang, Y., Wang, X., 2016. The abrupt climate change near 4,400 yr BP on the cultural transition in Yuchisi, China and its global linkage. Scientific Reports 6, 27723.Google Scholar
Wang, Y., Cheng, H., Edwards, R.L., He, Y., Kong, X., An, Z., Wu, J., Kelly, M.J., Dykoski, C.A., Li, X., 2005. The Holocene Asian monsoon: links to solar changes and North Atlantic climate. Science 308, 854–857.Google Scholar
Wanner, H., Mercolli, L., Grosjean, M., Ritz, S., 2015. Holocene climate variability and change: a data-based review. Journal of the Geological Society 172, 254–263.Google Scholar
Wanner, H., Solomina, O., Grosjean, M., Ritz, S.P., Jetel, M., 2011. Structure and origin of Holocene cold events. Quaternary Science Reviews 30, 3109–3123.Google Scholar
Yasuda, Y., Fujiki, T., Nasu, H., Kato, M., Morita, Y., Mori, Y., Kanehara, M., Toyama, S., Yano, A., Okuno, M., 2004. Environmental archaeology at the Chengtoushan site, Hunan Province, China, and implications for environmental change and the rise and fall of the Yangtze River civilization. Quaternary International 123, 149–158.Google Scholar
Yim, Y.-J., 1977. Distribution of forest vegetation and climate in the Korean peninsula: IV. Zonal distribution of forest vegetation in relation to thermal climate. Japanese Journal of Ecology 27, 269–278.Google Scholar
Yoon, S., Moon, Y., Hwang, S., 2008a. Pollen analysis from the Holocene sediments of Lake Gyeongpo, Korea and its environmental implications. [In Korean.] Journal of the Geological Society of Korea 44, 781–794.Google Scholar
Yoon, S.-O., Hwang, S.-I., Park, C.-S., Kim, H.-S., Moon, Y.-R., 2008b. Landscape changes of coastal lagoons during the 20th century in the Middle East coast, South Korea. [In Korean.] Journal of the Korean Geographical Society 43, 449–465.Google Scholar
Yu, J., Lee, J., Kwon, K., 2003. An analysis of forest community and dynamics according to elevation in Mt. Sokri and Odae. [In Korean.] Korean Journal of Agricultural and Forest Meteorology 5, 238–246.Google Scholar
Zhang, Q., Zhu, C., Liu, C.-L., Jiang, T., 2005. Environmental change and its impacts on human settlement in the Yangtze Delta, PR China. Catena 60, 267–277.Google Scholar
Zong, Y., 2004. Mid-Holocene sea-level highstand along the southeast coast of China. Quaternary International 117, 55–67.Google Scholar