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Terrestrial-marine sedimentary cycles in the South Yellow Sea, China: implications for paleoenvironmental reconstruction since MIS 5

Sedimentary records of the continental shelves since Marine Isotope Stage (MIS) 5 are valuable for paleoenvironmental reconstruction and decipherment of land–sea interactions. Since the 1990s, different perspectives on global glacioclimate magnitudes and the associated evolution of major sedimentary environments during the Late Pleistocene have caused a distinctive understanding of marine transgressions and coastal deposits during MIS 3 and MIS 5. | Terrestrial-marine sedimentary cycles in the South Yellow Sea, China: implications for paleoenvironmental reconstruction since MIS 5