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


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.


Lagoon Diatom Paleoenvironmental change Paleoclimate Sediment core Korea 



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.


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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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