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Understanding the sea-level change in the geological past is helpful for the future coastal protection. Information of sea-level changes has been documented in various archives in the coasts. In this study, the well-preserved peat in three representative Holocene ditches in Dayanghe Plain in the Yellow Sea China were investigated using radiocarbon dating and diatom analysis. The widely distributed buried peats at elevation of ca. 2-10 m above sea-level (a.s.l.) in Dayanghe Plain are classified as marsh and limnological peats, which were formed after seawater receding from the drowned ditches. The peat layers lower than 4 m a.s.l., overlain the marine sediments conformably, correspond to the late-Holocene regression. Timing of the highstand sea-level in North Coast of North Yellow Sea is limited to 61825466 cal. a BP by radiocarbon dating. Shell banks at west of the Dagu Mountain which was at a 7-10 m height were thought not to be indicative of the Holocene highstand sea-level.

HIGHSTAND SEA-LEVEL IN THE HOLOCENE INFERRED FROM BURIED PEAT AND DIATOM ASSEMBLAGES FROM NORTH COAST OF THE YELLOW SEA, CHINA