Geosciences Journal

, Volume 20, Issue 4, pp 477–484 | Cite as

Climate change and human activities over the past millennium at Mt. Jeombong, central-eastern Korea

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Abstract

We present a multi-proxy record (pollen, microscopic charcoal, carbon-isotopic composition [δ13C], organic content, and particle size) of the late-Holocene climate change and human impact from central-eastern South Korea. The Medieval Climate Anomaly (MCA) and Little Ice Age (LIA), the most recent major climate events, have not been accurately investigated by paleolimnological studies in Korea, mainly due to a lack of undisturbed sediments and indifference to the past climate change. Our pollen records show late- Holocene centennial climate variations characterized by the successive solar minimums of the Oort, Wolf, Spörer, Maunder, and Dalton. We find paleoenvironmental evidence for shifting cultivation associated with serious droughts and consequent famines during the early 19th-century Dalton minimum. Our interpretation of human activities is well supported by Korean historical documents describing socioeconomic suffering induced by LIA climate deteriorations.

Keywords

Medieval Climate Anomaly Little Ice Age late Holocene human impact solar minimums climate change Korea 

References

  1. 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.CrossRefGoogle Scholar
  2. Berglund, B.E., 2003, Human impact and climate changes–synchronous events and a causal link? Quaternary International, 105, 7–12.CrossRefGoogle Scholar
  3. Bianchi, G.G. and McCave, I.N., 1999, Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland. Nature, 397, 515–517.CrossRefGoogle Scholar
  4. Blaauw, M., 2010, Methods and code for ‘classical’ age-modelling of radiocarbon sequences. Quaternary Geochronology, 5, 512–518.CrossRefGoogle Scholar
  5. Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., Priore, P., Cullen, H., Hajdas, I., and Bonani, G., 1997, A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science, 278, 1257–1266.CrossRefGoogle Scholar
  6. Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M.N., Showers, W., Hoffmann, S., Lotti-Bond, R., Hajdas, I., and Bonani, G., 2001, Persistent solar influence on North Atlantic climate during the Holocene. Science, 294, 2130–2136.CrossRefGoogle Scholar
  7. Büntgen, U., Tegel, W., Nicolussi, K., McCormick, M., Frank, D., Trouet, V., Kaplan, J. O., Herzig, F., Heussner, K.-U., and Wanner, H., 2011, 2500 years of European climate variability and human susceptibility. Science, 331, 578–582.CrossRefGoogle Scholar
  8. Chen, R., Shen, J., Li, C., Zhang, E., Sun, W., and Ji, M., 2015, Midto late-Holocene East Asian summer monsoon variability recorded in lacustrine sediments from Jingpo Lake, Northeastern China. The Holocene, 25, 454–468.CrossRefGoogle Scholar
  9. Choi, J.N., Yu, K.B., and Park, W.K., 1992, Paleoclimate reconstruction for Chungbu mountainous region using tree-ring chronology. The Korean Journal of Quaternary Research, 6, 21–32. (in Korean with English abstract)Google Scholar
  10. Chu, G., Sun, Q., Wang, X., Liu, M., Lin, Y., Xie, M., Shang, W., and Liu, J., 2012, Seasonal temperature variability during the past 1600 years recorded in historical documents and varved lake sediment profiles from northeastern China. The Holocene, 22, 785–792.CrossRefGoogle Scholar
  11. Clark, R.L., 1982, Point count estimation of charcoal in pollen preparations and thin sections of sediments. Pollen et spores, 24, 523–535.Google Scholar
  12. Delaygue, G. and Bard E., 2011, Antarctic last millennium 10Be stack and solar irradiance reconstruction. Climate Dynamics, 36, 2201–2218.CrossRefGoogle Scholar
  13. DeMenocal, P.B., 2001, Cultural responses to climate change during the late Holocene. Science, 292, 667–673.CrossRefGoogle Scholar
  14. Faegri, K. and Iverson, J., 1989, Textbook of pollen analysis. John Wiley & Sons, Chichester, 328 p.Google Scholar
  15. Farquhar, G.D., Ehleringer, J.R., and Hubrick, K.T., 1989, Carbon isotopic discrimination and photosynthesis. Annual Review of Plant Physiology and Plant Molecular Biolology, 40, 503–537.CrossRefGoogle Scholar
  16. Grimm, E.C., 1987, CONISS: a FORTRAN 77 p.ogram for stratigraphically constrained cluster analysis by the method of incremental sum of squares. Computers & Geosciences, 13, 13–35.CrossRefGoogle Scholar
  17. Hong, Y., Wang, Z., Jiang, H., Lin, Q., Hong, B., Zhu, Y., Wang, Y., Xu, L., Leng, X., and Li, H., 2001, A 6000-year record of changes in drought and precipitation in northeastern China based on a d13C time series from peat cellulose. Earth and Planetary Science Letters, 185, 111–119.CrossRefGoogle Scholar
  18. Keigwin, L.D., 1996, The little ice age and medieval warm period in the Sargasso Sea. Science, 274, 1504–1508.CrossRefGoogle Scholar
  19. Kim, D., 2008, Megadroughts in the Joseon dynasty (Daegigeun, Joseoneul duideopda). Blue history, 351 p. (in Korean)Google Scholar
  20. Korea National Park Research Institute, 2012, Investigation on natural resources of Seoraksan national park–Jeombongsan area. Korean National Park Research Institute research report 2012-17, 316 p. (in Korean)Google Scholar
  21. Lamb, H.H., 1965, The early medieval warm epoch and its sequel. Palaeogeography, Palaeoclimatology, Palaeoecology, 1, 13–37.CrossRefGoogle Scholar
  22. Lee, H. and Park, K., 1997, Climatic change and agricultural crisis in Choson Korea, 1799-1825. Journal of Choson Dynasty History, 2, 123–191. (in Korean with English abstract)Google Scholar
  23. Lee, U., 2003, Deforestation and Agricultural Productivity in Korea during the Eighteenth and Nineteenth Centuries. Review of Economic History, 34, 31–57. (in Korean with English abstract)Google Scholar
  24. Li, J., Mackay, A.W., Zhang, Y., and Li, J., 2013, A 1000-year record of vegetation change and wildfire from maar lake Erlongwan in northeast China. Quaternary International, 290, 313–321.CrossRefGoogle Scholar
  25. Liew, P.-M., Wu, M.-H., Lee, C.-Y., Chang, C.-L., and Lee, T.-Q., 2014, Recent 4000 years of climatic trends based on pollen records from lakes and a bog in Taiwan. Quaternary International, 349, 105–112.CrossRefGoogle Scholar
  26. Mann, M.E., Bradley, R.S., and Hughes, M.K., 1999, Northern hemisphere temperatures during the past millennium: Inferences, uncertainties, and limitations. Geophysical Research Letters, 26, 759–762.CrossRefGoogle Scholar
  27. Park, J., Kim, M., Lim, H.S., and Choi, J., 2013, Pollen and sediment evidence for late-Holocene human impact at the Seonam-dong archeological site, Gwangju, Korea. Review of Palaeobotany and Palynology, 193, 110–118.CrossRefGoogle Scholar
  28. Park, J., Yu, K.B., Lim, H.S., and Shin, Y.H., 2012, Multi-proxy evidence for late Holocene anthropogenic environmental changes at Bongpo marsh on the east coast of Korea. Quaternary Research, 78, 209–216.CrossRefGoogle Scholar
  29. Reimer, P.J., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Bronk Ramsey, C., Buck, C. E., Cheng, H., Edwards, R.L., and Friedrich, M., 2013, IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon, 55, 1869–1887.CrossRefGoogle Scholar
  30. Selvaraj, K., Wei, K.-Y., Liu, K.-K., and Kao, S.-J., 2012, Late Holocene monsoon climate of northeastern Taiwan inferred from elemental (C, N) and isotopic (d13C, d15N) data in lake sediments. Quaternary Science Reviews, 37, 48–60.CrossRefGoogle Scholar
  31. Sohn, J., Ahn, C., Choi, J., Park, K., Hahn, J., Jeon, J., Park, J., Hong, W., and Park, W., 2011, Flora and vegetation of forest genetic source reserve area in Mt. Jumbong. Proceedings of the 2011 Annual Meeting of the Korean Forest Society (Expanded Abstract), Gyungju, Feb. 17, p. 370–373. (in Korean)Google Scholar
  32. Wang, L., Rioual, P., Panizzo, V.N., Lu, H., Gu, Z., Chu, G., Yang, D., Han, J., Liu, J., and Mackay, A.W., 2012, A 1000 yrrecord of environmental change in NEChina indicated by diatom assemblages from maar lake Erlongwan. Quaternary Research, 78, 24–34.CrossRefGoogle Scholar
  33. Wang, L.-C., Behling, H., Chen, Y.-M., Huang, M.-S., Chen, C.-T., Lou, J.-Y., Chang, Y.-P., and Li, H.-C., 2014, Holocene monsoonal climate changes tracked by multiproxy approach from a lacustrine sediment core of the subalpine Retreat Lake in Taiwan. Quaternary International, 333, 69–76.CrossRefGoogle Scholar
  34. Wang, L.-C., Behling, H., Lee, T.-Q., Li, H.-C., Huh, C.-A., Shiau, L.-J., Chen, S.-H., and Wu, J.-T., 2013, Increased precipitation during the Little Ice Age in northern Taiwan inferred from diatoms and geochemistry in a sediment core from a subalpine lake. Journal of Paleolimnology, 49, 619–631.CrossRefGoogle Scholar
  35. Wanner, H., Beer, J., Buetikofer, J., Crowley, T.J., Cubasch, U., Flueckiger, J., Goosse, H., Grosjean, M., Joos, F., and Kaplan, J.O., 2008, Mid-to Late Holocene climate change: an overview. Quaternary Science Reviews, 27, 1791–1828.CrossRefGoogle Scholar
  36. Yoon, S.-O., Kim M., and Hwang S., 2013, Pollen analysis of alpine wetlands on Mt. Jeombong in Gangwon-do, South Korea and climate change during the late Holocene. Journal of the Korean Geomorphological Association, 20, 101–115 (in Korean).Google Scholar

Copyright information

© The Association of Korean Geoscience Societies and Springer-Verlag Berlin Heidelberg 2016

Authors and Affiliations

  1. 1.Department of GeographySeoul National UniversitySeoulRepublic of Korea
  2. 2.Institute for Korean Regional StudiesSeoul National UniversitySeoulRepublic of Korea

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