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The distributions of lipids in surface and subsurface sediments from the northern South China Sea were determined. The n‐alkanes were in bimodal distribution that is characterized by a centre at n‐C16–n‐C20 with maximum at C18 (or C19) and n‐C27–n‐C31 as well as at C29 (or C31). The short‐chain alkanes suffered from significant losses due to their slow deposition in the water column, and their presence...
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