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- W2893825934 abstract "ABSTRACT We describe two coastal paleosols recovered in sediment cores from the Oujiang Delta, Southeast China. These provide useful benchmarks for past sea level change on the East China Sea coast. Radiocarbon ( 14 C) dates on charcoal and plant matter show that one formed during Marine Isotope Stage 3 (MIS 3) and was exposed for perhaps 20 ka, during the Last Glacial Maximum. The other formed in the Early Holocene and was briefly exposed, during a period of fluctuating sea level. Similar paleosols have been described from the Changjiang (Yangtze) Delta, and at many other sites from the East China Sea. The MIS 3 paleosol records a regional relative sea level of about –27 m at the end of MIS 3. While this value is consistent with other paleo sea level estimates for the East China Sea region, it is much higher than predicted by eustatic sea level estimates." @default.
- W2893825934 created "2018-10-05" @default.
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- W2893825934 date "2018-09-25" @default.
- W2893825934 modified "2023-10-18" @default.
- W2893825934 title "Sea level implications from Late Quaternary/Holocene paleosols from the Oujiang Delta, China" @default.
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- W2893825934 doi "https://doi.org/10.1017/rdc.2018.77" @default.
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