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Journal of Paleolimnology

, Volume 60, Issue 4, pp 553–570 | Cite as

Holocene climate and environmental changes inferred from sediment characteristics and diatom assemblages in a core from Hwajinpo Lagoon, Korea

  • Ara Cho
  • Daekyo Cheong
  • Jin Cheul Kim
  • Dong-Yoon Yang
  • Jin-Young Lee
  • Kaoru Kashima
  • Kota Katsuki
Original paper
  • 317 Downloads

Abstract

Hwajinpo is the largest lagoon in Korea and is located along the east coast of the country. It possesses Holocene sediments that provide an important record of past climate change. We studied the evolution of Hwajinpo Lagoon using grain size data and diatom assemblages in an 11.0-m core (HJ02), which was obtained at the mouth of a small river that drains into the lagoon. Core chronology was established with accelerator mass spectrometry 14C dates and optically stimulated luminescence dates. Diatom assemblages and grain size analysis revealed that estuarine conditions in the inner lagoon area transitioned to an open embayment ca. 8 ka as a result of sea-level rise. Around 7.8 ka, the open bay became a semi-closed bay as a consequence of development of a sand barrier. After the bay was semi-closed, marine water inflow was increasingly restricted as the sand barrier developed, and the semi-closed bay became a completely enclosed, low-salinity, brackish lagoon around 6 ka. There was an erosional hiatus between 5.5 and 1.7 ka (7.0 m depth), likely caused by river flooding and a switch in the location of drainage along the delta. The lagoon became oligohaline around 1.6 ka, likely because of increasing precipitation associated with an intensified Asian summer monsoon. This increase in precipitation resulted in expansion of the sand bar by sediment inflow, driven by agricultural development in the area. About 1000 years ago, the diatom assemblage was similar to the modern assemblage, suggesting the lagoon’s current geomorphic conditions had been established.

Keywords

Lagoon Diatom Paleoenvironmental change Paleoclimate Sediment core Korea 

Notes

Acknowledgements

This research was supported by a research grant from the Korean Ministry of Oceans and Fisheries (PJT300538). We are indebted to Professor Jonathan Woodruff of University of Massachusetts Amherst and Dr. Han Min of Seoul National University.

References

  1. Abu-Zied RH, Bantan RA (2015) Paleoenvironment, paleoclimate and sea-level changes in the Shuaiba Lagoon during the late Holocene (last 3.6 ka), eastern Red Sea coast, Saudi Arabia. Holocene 25:1301–1312CrossRefGoogle Scholar
  2. Bhattrai BD, Kwak S, Choi K, Heo W (2017) Assessment of long-term physicochemical water quality variations by PCA Technique in Lake Hwajinpo, South Korea. J Environ Prot 8:1636–1651CrossRefGoogle Scholar
  3. Bradbury JP (1989) Late quaternary lacustrine paleoenvironments in the Cuenca de Mexico. Q Sci Rev 8:75–100CrossRefGoogle Scholar
  4. Cho DY, Hong SH, Chwae U, Lee BJ, Choi P (1998) Geological report of the Goseong-Ganseong sheet (1:50,000). Korea Institute of Geology, Mining and Materials, Deajeon (in Korean) Google Scholar
  5. Chu G, Sun Q, Li S, Zheng M, Jia X, Lu C, Liu J, Liu T (2005) Long-chain alkenone distributions and temperature dependence in lacustrine surface sediments from China. Geochim Cosmochim Acta 69:4985–5003CrossRefGoogle Scholar
  6. Colombaroli D, Marchetto A, Tinner W (2007) Long-term interactions between Mediterranean climate, vegetation and fire regime at Lago di Massaciuccolo (Tuscany, Italy). J Ecol 95:755–770CrossRefGoogle Scholar
  7. Elwany MHS, Flick RE, Aijaz S (1998) Opening and closure of a marginal Southern California Lagoon Inlet. Estuaries 21:246–254CrossRefGoogle Scholar
  8. Folk RL, Ward WC (1957) Brazos river bar: a study in the significance of grain-size parameters. J Sediment Petrol 27:3–26CrossRefGoogle Scholar
  9. Genkal SI, Kiss KT (1993) Morphological variability of the diatom Cyclotella atomus Hustedt var. atomus and C. atomus var. gracilis var. nov. Hydrobiologia 269–270:39–47CrossRefGoogle Scholar
  10. Go A, Tanaka Y, Kashima K (2013) Sedimentary environment of Hwajinpo using diatom analysis. J Korea Geomorphol Assoc 20:15–25 (in Korean with English abstract) Google Scholar
  11. Hendey NI (1964) An introductory account of the smaller algae of British coastal waters, part V: Bacillariophyceae (Diatoms). Otto Koeltz Science, KoenigsteinGoogle Scholar
  12. Heo W-M, Kwon S, Lee J, Kim D, Kim B (2004) The limnological survey of a coastal lagoon in Korea (3): Lake Hwajinpo. Korean J Limnol 37:12–25 (in Korean with English abstract) Google Scholar
  13. Hong W, Park JH, Kim KJ, Woo HJ, Kim JK, Choi HW, Kim GD (2010a) Establishment of chemical preparation methods and development of an automated reduction system for AMS sample preparation at KIGAM. Radiocarbon 52:1277–1287CrossRefGoogle Scholar
  14. Hong W, Park JH, Sung KS, Woo HJ, Kim JK, Choi HW, Kim GD (2010b) A new 1MV AMS facility at KIGAM. Radiocarbon 52:243–251CrossRefGoogle Scholar
  15. Howell MW, Thunell RE, Tappa E, Rio D, Sprovieri R (1988) Late Neogene laminated and opal-rich facies from the Mediterranean region: geochemical evidence for mechanisms of formation. Palaeogeogr Paleoclimatol Palaeocol 64:265–286CrossRefGoogle Scholar
  16. Jo W (1980) Holocene sea-level changes on the east coast of Korea Peninsula. Geogr Rev Jpn 53:317–328CrossRefGoogle Scholar
  17. Joh GJ (2010) Algal Flora of Korea volume3 Number1 freshwater diatoms I. National Institute of Biological Resource, IncheonGoogle Scholar
  18. Joh GJ (2012) Algal Flora of Korea volume3 Number7 freshwater diatoms V. National Institute of Biological Resource, IncheonGoogle Scholar
  19. Kashima K (1985) Holocene diatom assemblages in Takagami Lowland, central part of Choshi Peninsula, and its relation to changes of sea-level. Q Res (Tokyo) 24:125–138 (in Japanese with English abstract) CrossRefGoogle Scholar
  20. Kashima K (1986) Holocene successions of diatom fossil assemblages in alluvium, and those relations to paleo-geographical changes. Geogr Rev Jpn Ser A 59:383–403 (in Japanese with English abstract) CrossRefGoogle Scholar
  21. Katsuki K, Yang DY, Seto K, Yasuhara M, Takata H, Otsuka M, Khim BK (2016) Factors controlling typhoons and storm rain on the Korean Peninsula during the Little Ice Age. J Paleolimnol 55:35–48CrossRefGoogle Scholar
  22. Kim BH, Won DH, Kim YJ (2012) Spring bloom of Skeletonema costatum and lake trophic status in the Hwajinpo Lagoon, South Korea. Korean J Ecol Environ 45:329–339 (in Korean with English Abstract) Google Scholar
  23. Kobayashi H, Idei M, Mayama S, Nagumo T, Osada K (2006) H. Kobayasi’s atlas of Japanese diatoms based on electron microscopy. Uchida Rokakuho Publishing Co., Ltd, TokyoGoogle Scholar
  24. Kosugi M (1988) Classification of living diatom assemblages as the indicator of environments, and its application to reconstruction of paleoenvironments. Q Res (Tokyo) 27:1–20 (in Japanese with English abstract) CrossRefGoogle Scholar
  25. Kraft JC, John CJ, Marx PR (1981) Clastic depositional strata in a transgressive coastal environment: Holocene epoch. Northeast Geol 3:268–277Google Scholar
  26. Kumano S, Ihira M, Kuromi Mm Maeda Y, Matsumoto E, Nakamura T, Matsushima Y, Sato H, Mtsuda I (1990) Holocene sedimentary history of some coastal plains in Hokkaido, Japan V. Sedimentary history of Kushu Lake and Akkeshi. Ecol Res 5:277–289CrossRefGoogle Scholar
  27. Lim J, Yu S, Nahm WH, Kim JY (2012) Holocene millennial-scale vegetation changes in the Yugu floodplain, Kongju area, central South Korea. Q Int 254:92–98CrossRefGoogle Scholar
  28. Matsubara A (2000) Holocene geomorphic development of coastal barriers in Japan. Geogr Rev Jpn Ser A 73:409–434 (in Japanese with English abstract) CrossRefGoogle Scholar
  29. Morton RA, Ward GH, White WA (2000) Rates of sediment supply and sea level rise in a large coastal lagoon. Mar Geol 167:261–284CrossRefGoogle Scholar
  30. Murray AS, Wintle AG (2000) Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiat Meas 32:57–73CrossRefGoogle Scholar
  31. National Geographic Information Institute (2006) Historical geography of Korea. Ministry of Land Infrastructure and Transport, SejeonGoogle Scholar
  32. Okutani T (2001) Marine mollusks in Japan. Tokai University Press, Kanagawa, Japan (in Japanese)Google Scholar
  33. Ota Y, Umitsu M, Matsushima Y (1990) Recent Japanese research on relative sea-level changes in the Holocene, and related problems. Q Res (Tokyo) 29:31–48 (in Japanese with English abstract) CrossRefGoogle Scholar
  34. Park SC, Hong SK, Kim DC (1996) Evolution of late quaternary deposits on the inner shelf of the South Sea of Korea. Mar Geol 131:219–232CrossRefGoogle Scholar
  35. Park J, Yu KB, Lim HS, Shin YH (2012) Multi-proxy evidence for late Holocene anthropogenic environmental changes at Bongpo marsh on the east coast of Korea. Q Res 78:209–216CrossRefGoogle Scholar
  36. Pernetta JC, Milliman JD (1995) Land-ocean interactions in the coastal zone: implementation plan. Oceanogr Lit Rev 42:801–805Google Scholar
  37. Peros M, Gregory B, Matos F, Reinhardt E, Desloges J (2015) Late Holocene record of lagoon evolution, climate change, and hurricane activity from southeastern Cuba. Holocene 25:1483–1497CrossRefGoogle Scholar
  38. Pirazzoli PA (1991) World atlas of Holocene sea-level changes. Elsevier, AmsterdamGoogle Scholar
  39. Reimer PJ, Bard E, Bayliss A, Beck JW, Blackwell PG, Ramsey CB, Buck CE, Cheng H, Edwards RL, FriedrichM Grootes PM, Guilderson TP, Haflidason H, Hajdas I, Hatte C, Heaton TJ, Hoffmann DL, Hogg AG, Hughen KA, Kaiser KF, Kromer B, Manning SW, Niu M, Reimer RW, Richards DA, Scott EM, Southon JR, Staff RA, Turney CSM, van der Plicht J (2013) IntCal13 and Marine13 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 55:1869–1887CrossRefGoogle Scholar
  40. Roy PS, Cowell PJ, Ferland MA, Thom BG (1994) Wave dominated coasts. In: Carter RWG, Woodroffc CD (eds) Coastal evolution: late quaternary shoreline morphodynamics. Cambridge University Press, Cambridge, pp 121–186Google Scholar
  41. Ryu E, Ryu BJ, Yun H, Lee SJ (2003) Diatom floras of the Ulleung basin: implication for late quaternary paleoenvironment. J Geool Soc Korea 39:183–198 (in Korean with English abstract) Google Scholar
  42. Selivanov AO (1996) Morphological changes on Russian coasts under rapid sea-level changes: examples from the Holocene history and implications for future. J Coast Res 12:823–830Google Scholar
  43. Smol JP, Stoermer EF (2010) The diatoms: applications for the environmental and earth sciences, 2nd edn. Cambridge University Press, CambridgeCrossRefGoogle Scholar
  44. Stuiver M, Reimer JP (1993) Extended 14C base and revised calib 3.0 14C age calibration program. Radiocarbon 35:215–230CrossRefGoogle Scholar
  45. Sylvestre F, Guiral D, Debenay JP (2004) Modern diatom distribution in mangrove swamps from the Kaw Estuary (French Guiana). Mar Geol 208:281–293CrossRefGoogle Scholar
  46. Vos PC, de Wolf H (1993) Diatoms as a tool for reconstructing sedimentary environments in coastal wetlands: methodological aspects. Hydrobiologia 269:285–296CrossRefGoogle Scholar
  47. Woodward C, Shulmeister J, Bell D, Haworth R, Jacobsen G, Zawadzki A (2014) A Holocene record of climate and hydrological changes from Little Llangothlin Lagoon, south eastern Australia. Holocene 24:1665–1674CrossRefGoogle Scholar
  48. Yasui S, Kobayashi I (2001) Pleistocene-Holocene diatom flora of the Shiotsugata Lagoon in the Echigo Plain, central Japan. Sci Rep Niigata Univ Ser E (Geol) 16:47–81Google Scholar
  49. Yi S, Kim JY, Yang DY, Oh KC, Hong SS (2008) Mid- and Late-Holocene palynofloral and environmental change of Korean central region. Q Int 176:112–120CrossRefGoogle Scholar
  50. Yoon SO, Hwang S, Park C-S, Kim HS, Moon YR (2008) Landscape changes of coastal lagoons during the Twentieth century in the Middle East coast, South Korea. J Korean Geogr Soc 43:449–465Google Scholar
  51. Yum JG (1996) Characteristics of a coastal lagoon, Hwajinpo, in the eastern coast of Korea, and its comparison with coastal lagoons in Sanin region in Japan. M.Sc thesis, Shimane University, Matsue, pp 1–72Google Scholar
  52. Yum JG, Sampei T, Tokuoka T, Nakamura T, Yu KM (2002) Depositional environmental change during the last 400 years in Hwajinpo Lagoon on the eastern coast of Korea. J Geol Soc Korea 38:21–32Google Scholar
  53. Yum JG, Takemura K, Tokuoka T, Yu KM (2003) Holocene environmental changes of Hwajinpo Lagoon on the eastern coast of Korea. J Paleolimnol 29:155–166CrossRefGoogle Scholar
  54. Yum JG, Yu KM, Takemura K, Naruse T, Kitamura A, Kitagawa H, Kim JC (2004) Holocene evolution of the outer lake of Hwajinpo lagoon on the eastern coast of Korea; envrionmental changes with Holocene sea-level fluctuation of the East sea (Sea of Japan). Radiocarbon 46:797–808CrossRefGoogle Scholar
  55. Yum JG, Takamura K, Yu KM, Nahm WH, Hong SS, Yang DY, Katsuki K, Kim JY (2015) Late quaternary environmental changes of the Hwajinpo and Songjiho Lagoons on the Eastern Coast of Korea. In: Kashiwaya K, Shen J, Kim JY (eds) Earth surface processes and environmental changes in East Asia. Springer, Tokyo, pp 163–199CrossRefGoogle Scholar

Copyright information

© Springer Nature B.V. 2018

Authors and Affiliations

  • Ara Cho
    • 1
    • 2
    • 3
  • Daekyo Cheong
    • 3
  • Jin Cheul Kim
    • 2
  • Dong-Yoon Yang
    • 2
  • Jin-Young Lee
    • 2
  • Kaoru Kashima
    • 1
  • Kota Katsuki
    • 4
  1. 1.Department of Earth and Planetary Sciences, Faculty of SciencesKyushu UniversityFukuokaJapan
  2. 2.Geological Research DepartmentKorea Institute of Geoscience and Mineral ResourcesDaejeonRepublic of Korea
  3. 3.Division of Geology and GeophysicsKangwon National UniversityChuncheonRepublic of Korea
  4. 4.Estuary Research CenterShimane UniversityMatsueJapan

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