Edinger Evan N, Azmy Karem, Diegor Wilfredo, Siregar P Raja
Department of Geography, Memorial University, St. John's, NL, Canada.
Mar Pollut Bull. 2008 Sep;56(9):1553-69. doi: 10.1016/j.marpolbul.2008.05.028. Epub 2008 Jul 17.
Shallow marine sediments and fringing coral reefs of the Buyat-Ratototok district of North Sulawesi, Indonesia, are affected by submarine disposal of tailings from industrial gold mining and by small-scale gold mining using mercury amalgamation. Between-site variation in heavy metal concentrations in shallow marine sediments was partially reflected by trace element concentrations in reef coral skeletons from adjacent reefs. Corals skeletons recorded silicon, manganese, iron, copper, chromium, cobalt, antimony, thallium, and lead in different concentrations according to proximity to sources, but arsenic concentrations in corals were not significantly different among sites. Temporal analysis found that peak concentrations of arsenic and chromium generally coincided with peak concentrations of silica and/or copper, suggesting that most trace elements in the coral skeleton were incorporated into detrital siliciclastic sediments, rather than impurities within skeletal aragonite.
印度尼西亚北苏拉威西省布亚特-拉托托托克区的浅海沉积物和边缘珊瑚礁,受到工业金矿尾矿的海底处置以及使用汞齐化法的小规模金矿开采的影响。浅海沉积物中重金属浓度的站点间差异,部分反映在相邻珊瑚礁的珊瑚骨骼中的微量元素浓度上。珊瑚骨骼根据与源的接近程度记录了不同浓度的硅、锰、铁、铜、铬、钴、锑、铊和铅,但各站点珊瑚中的砷浓度没有显著差异。时间分析发现,砷和铬的峰值浓度通常与二氧化硅和/或铜的峰值浓度一致,这表明珊瑚骨骼中的大多数微量元素是被纳入碎屑硅质碎屑沉积物中,而不是骨骼文石中的杂质。