Coupling isotopic signatures and partial extraction method to examine lead pollution in mangrove sediments

Elevated lead (Pb) has been widely observed in mangrove sediments due to human activities, yet understanding the sources of Pb in these sediments and the factors influencing Pb accumulation is challenging. Here, we combined Pb isotopes with partial extraction methods to study Pb contamination levels in mangrove sediments from the eastern and western parts of the Maowei Sea, China. Our results showed that the Pb in the leachate and residual fraction was mainly from anthropogenic and natural sources, respectively. The use of 204Pb isotope analysis can reveal some overlooked differences between anthropogenic and natural sources. Calculation by Bayesian mixing model showed no significant difference in the total anthropogenic contribution between the two sites, but the relative contribution of each end member differed. The contribution of Pb/Zn ores was much higher in the eastern sites (30.9 & PLUSMN; 5.1%) than in the west (18.4 & PLUSMN; 5.5%), while that of agricultural activities was much lower in the east (5.2 & PLUSMN; 3.1%) than in the west (13.5 & PLUSMN; 4.6%). The elevated anthropogenic Pb accumulation in mangrove sediments was ascribed to organic matter. This study provides more data on Pb isotopic composition and new insights into Pb biogeochemistry in the mangrove environment.

Automated summary

This study investigated the levels of lead contamination in mangrove sediments from the Maowei Sea in China using lead isotopes and partial extraction methods. The results showed that the lead in the sediments was primarily from anthropogenic and natural sources, and that the 204Pb isotope analysis revealed overlooked differences between these sources. The study also found differences in the contribution of different sources between the eastern and western parts of the Maowei Sea.