Redox-dependent phosphorus burial and regeneration in an offshore sulfidic sediment core in North Yellow Sea, China

Phosphorus (P) pollution can trigger severe marine eutrophication, which further leads to harmful algal blooms, and a deterioration of sea water quality. The P burial and regeneration in offshore sediments can directly affect the eutrophication levels of estuarine and coastal ecosystems. Although many researches on redox-dependent P burial and regeneration were studied, such process in the presence of silicate is still poorly understood, and the effects of pyrite formation on organic P (OP) burial and regeneration also remain unclear. In this study, a sulfidic sediment core was collected in the offshore of an estuary in the north Yellow Sea, China. Results indicated that indigenous biological input was found to be the primary source of organic matter in upper sediments. The regenerated P under reducing conditions was dominated by labile FeP and OP. The PO43− released from FeP and OP that could be captured by Al/Fe/Mn (oxyhydr) oxides in surface sediments and Ca minerals in deep sediments. CaP, AlP, unreactive Al/Fe-Si-P and some stable metal chelated OP were the main burial P fractions. Sulfate reduction and formation of insoluble metal sulfides including the pyrite promoted OP decomposition by anaerobic decomposition, removing metal ions from the “metal-OP” chelates and restoring the phosphatase activity. [Display omitted] •Marine algal debris is the primary source of organic P (OP) in the sediment core.•Free OP and reactive Al/Fe/Mn-P are the main regenerated P speciation.•CaP, AlP, Al/Fe-Si-P and OP-metal chelates are main buried fractions of P.•Sulfate reduction and the formation of metal sulfides promote OP regeneration.