Phosphorus is a key biogenic element and plays an essential role in global biogeochemical cycles. The geochemical characteristics of phosphorus as well as the controlling factors and the environmental marker function in Jiaozhou Bay sediments were presented. The different forms of sedimentary phosphorus were studied in three sediment cores, which are forms of inorganic phosphorus, exchangeable phosphorus, phosphorus bound to Al-Fe, and calcium, occluded phosphorus as well as total phosphorus and organic phosphorus, respectively. The vertical profiles of various forms of phosphorus in response to 210Pb chronological studies of sediment cores were investigated in order to reveal sedimentary environment changes. The results showed that inorganic phosphorus was the dominant form of total phosphorus and organic phosphorus was only the minor part. The detrital carbonate-bound phosphorus was the largest part of total phosphorus. The concentrations and burial fluxes of phosphorus were controlled by source and environmental factors including pH, salinity, temperature and grain size of sediments etc. Moreover, the analysis of OC/OP ratios suggested that the terrestrial inputs were the dominant source of Jiaozhou Bay sediments. The sedimentation fluxes of phosphorus increased in the past two decades, as a result, the pollution was still serious from the 1980 to 2000. But the state has greatly improved since 2000. The Fe-P,Al-P and Oc-P have close relationships with the degree of pollution and may act as good indicators for environment pollution in Jiaozhou Bay. |