Abstract
Ten stenols and stanols were identified by TLC, GC and GC-MS-DS in a marine sediment core from Beibu Bay, the South China Sea. C27, C28 and C29 Δ5 stenols and 5α-stanols mainly come from zooplankton, algae and phytoplankton in marine environment. C29 24-ethylcholest-5-en-3β-ol is thought to indicate input of terrigenous organic matter. The increase of C27, C28 and C29 5α-stanol/Δ5 stenol ratios with sediment depth shows the evolution of stenols and stanols in the marine sediment core.
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The project was supported by the National Natural Science Foundation of China (48970111).
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Shanchun, J., Rongfen, J. & Zuofeng, L. The evolution of stenols and stanols in marine sediment core from Beibu Bay, the South China Sea. Chin. J. Ocean. Limnol. 10, 92–96 (1992). https://doi.org/10.1007/BF02844304
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DOI: https://doi.org/10.1007/BF02844304