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This research paper investigates carbonate preservation changes in the deep sea of the eastern South China Sea over the last 600,000 years, using a multiproxy approach that includes planktonic foraminifera and total organic carbon measurements. The findings indicate that carbonate dissolution has been influenced by the deepening of the lysocline and Calcite Compensation Depth, with significant increases in planktonic foraminifera abundance and total organic carbon during specific marine isotopic stages. The
- Author
- dwi ayu
- Language
- EN