allochthonous (Fig. 3), with 34–60% (median = 49%)
Based on the δ13Corg (−29.5 to −23.9) and the C/N ratio (9–26.6), the sedimentary OM that accumulated in the central SAL is mainly allochthonous (Fig. 3), with 34–60% (median = 49%) derived from riverine sediment (Fig. 4)
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